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Ringwood and District Historical Society
Archive - Biographical material, Maggs Family of Ringwood and District (Parent Record)
Transcript of the Maggs Family History, given by Joan Walker, former member of RDHS:- Pioneer Family - Maggs • James Maggs and wife Harriet Banfield migrated to Melbourne on the “Ticondergoa” which sailed from Birkenhead on 4th August 1852 with 812 assisted immigrants. • In 1856 James purchased 7 acres of land, part of section 75, in the parish of Nunawading where he developed an orchard. • Three children died young – Emma (before 1862), Jemima at Ticonderoga Bay and Mary Jane aged 3 weeks at Konung Creek. Three sons and a daughter survived them. Harriet died in 1875, James in 1888 both buried in Box Hill cemetery. • Their sons Joseph, Samuel and James all established orchards in the Ringwood/Croydon district. Samuel Maggs • Born 11 May 1851, Somerset, England and grew up on his fathers property in Springfield Road, Blackburn, one block east of Surrey Road. • On 4 October 1876 Sam married Eliza Ann Barnes. • 1881 purchased a block, Allot. 39 Parish of Warrandyte and developed an apple and cherry orchard. The orchard occupied the area between White Horse Road and Mullum Mullum Creek from Oban Rd east to where White Horse Road takes a slight turn to the right, near Burnt Bridge. • Son George b.28 December 1876 Warrandyte married Annie Smith d.9 May 1947. • Daughter Eliza Jane b.27 July 1878 Ringwood married William Dobbin, d.31 May 1946 Camberwell. • Son James b.15 May 1880, Lilydale married Catherine Atkins d.28 July 1940 Ringwood buried Box Hill. • Daughter Jemima b.16 December 1881 Warrandyte married Edward Lindsay in 1905, d.2 November 1955 and buried in Box Hill. • Daughter Jane b.22 May 1884 Warrandyte married Thomas S Knee in 1912 d.31 January 1971, buried at Box Hill. • Son Samuel William b.1 Jan 1889 Ringwood married Mina Lillian Schuhkraft in 1911 d.15 Jan 1955 Ringwood. Joseph Maggs • Born 5 June 1845, Somerset England. • Married Mary Ann Reid in April 1867 at Templestowe. • Bought Sec. 26a, in Ringwood on the corner of Eastfield Road an Mt Dandenong Road in February 1870. Planted 4 acres with fruit treet. Was also a wood carter. During the 1880s white clay was mined here, which he carted for the Victorian Porcelain Clay Coy. • Daughter Emma b.8 Jan 1868 Templstowe d. 3 August 1939, Richmond married May 1890 Fredrick W. McGinnis. • Daughter Agnes b.16 June 1869 Templestowe married John D Miller c.1894. d.3 February 1912 Heathmont, buried Box Hill. • Son Albert b.1 May 1871 Nunawading d.15 Nov 1893. • Son Hubert b.10 May 1873 Nunawading married Isabella Atkins in 1898 Ringwood d.11 August Wagga Wagga and buried there. • Daughter Harriet Annis b.13 August 1875 Box Hill d.21 Sept 1875. • Son Joseph b.25 Septenber 1876 Box Hill d.3 Oct 1900 Mitcham. • Daughter Harriet Annis b.18 Aug 1879, Ringwood married James R Miller d.8 May 1945. • Son William b.3 Sep 1881 married Mary E Hardidge. D.6 April 1950 South Melbourne. • Daughter Dora Jane Dulcie b.13 December 1883 Ringwood d.1973. • Daughter Delia Rose b.20 February 1886, Ringwood married William J Sharkie d.30 October 1914 James Maggs • Youngest (born 28 April 1862, Blackburn) and only Australian born son was also an orchardist. • Married Marianne Hardidge in 1880 (divorced in 1906) purchased land in what is now Kalinda Road, adjoining Sam’s land. • James lived with Teresa Shanks in the Hawthorn and Prahran districts and became a taxi driver. Died in 1925, buried at Box Hill. Marianne became a widwife who delivered over 500 babies in the area – was known as Nurse Polly Maggs, died in 1941 aged 81. • Daughter Mary Ann Hase Polly b.5 July 1881 Ringwood married Thomas Lawford d.9 November 1961 buried at Box Hill. • Daughter Jane Emma b.9 May 1883 Ringwood married Frederick Bloom 1910 d.28 July 1954. • Daughter James John b.17 Jan 1885 Ringwood married Johanna Ida Edith Bloom in 1912 d.24 August 1962 buried at Box Hill. • Daughter David Joseph b.31 Jan 1887 Ringwood married Violet Lepp married 1916, d.11 July 1966. • Son Samuel Arthur b.11 March 1888 Ringwood married Bertha Anna Pump in 1913 d.7 August 1957. • Son John William b.16 April 1890 Ringwood married Lillian Mabel May Smith in 1909 d.18 February 1959 Cobram. • Daughter Eliza Anne b.6 March 1892 Ringwood d.April 18 1892. • Son Robert Thomas b.7 March 1893 Ringwood married Edith E Britnell in 1919 d.12 March 1981 buried Box Hill. • Son Albert Edward b.12 April 1895 Ringwood married Florence Sarah Pearce in 1918 d.30 January 1976 buried at Springvale. • Daughter Evaleen Victoria b.28 Aug 1897, Ringwood married Sydney Till married 1920 d.5 September 1989 buried at Box Hill. • Daughter Harriet Banfield Chrissy b.14 December 1899 Ringwood d.28 Dec 1979 buried Box Hill. Jane Maggs • Born 19 December 1858 in Blackburn. Died 5 July 1926 buried at Box Hill. Married William Cook and had one child, Harriet Amy Cook who never married and lived in Whitehorse Road, Mitcham until her death in 1962. Details, extract from Family Tree Maker family tree:- Descendants of James Maggs Generation No. 1 1. JAMES5 MAGGS (JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)1 died 24 Sep 18881. He married (1) HARRIET MARTHA BANFIELD1 23 Dec 1841 in Bristol, Somerset, England1. She was born 19 Jun 1817 in Clutton, Somerset, England1, and died 12 May 1875 in Nunawading, Victoria, Australia1. He married (2) ROSENA MAHON1 09 Dec 1875 in Fitzroy, Victoria, Australia1. She was born in Deptford, London, England1. Notes for JAMES MAGGS: JAMES MAGGS, and his wife HARRIET BANFIELD, migrated to Melbourne on the "Ticonderoga", which sailed from Birkenhead 4th Aug 1852 with 812 assisted immigrants aboard. In the close confines of the ship fever broke out and by the time she arrived off Port Phillip Heads on or about 2nd Nov, 100 deaths had been recorded in the log and hundreds were too weak to help themselves. Captain Wylie of the coastal trader "Champion", informed Captain Ferguson, the harbourmaster at Williamstown, of the tragic plight of the passengers and crew, and he came with two doctors, in the "Empire", to their aid. They anchored just inside Port Phillip Heads on 5 Nov. at the "Sanatory Station", declared but not yet established by the local authorities. Those who were well enough were put ashore in tents made of spars and sails. The "Lysander" was despatched from Melbourne to act as a hospital ship, and 2 houses, built of the local limestone, were commandeered as a quarantine station. For six weeks the survivors were held near Point Nepean at a place still known as Ticonderoga Bay while the fever, propably typhus, a louse borne epidemic disease, ran its course and a further 68 passengers, 2 crew members and 4 newborn babes succumbed to the scourge. Among them was Jemima Maggs, 3 year old daughter of James and Harriet. The dead were buried at the waters edge, in a grove of titree, a site now marked by Heaton's monument. The remainder of the family, including Samuel, just one year old, lived through the ordeal to make a new life in Australia. James obtained work with Robert Wilson of Bulleen for a period of 3 months at a wage of 52 pounds per annum with rations. By 1856 he was able to purchase 7 acres of land, part of section 75, in the parish of Nunawading at 5 pounds per acre. Here he developed an orchard by means of various mortgages including one taken out 17 July 1872 for 50 pounds from the Victorian Permanent Property Investment & Building Society. Three of their seven children died young, Emma before 1862, Jemima at Ticonderoga Bay, and Mary Jane, the first of their three Australian born children, aged 3 weeks at Konung Creek.Three sons and a daughter survived them. Harriet died in 1875, James lived until 1888 and both are buried at the Box Hill Cemetery. Their sons, Joseph, Samuel, and James all established orchards in the Ringwood/Croydon district. Bur Reg 308 Box Hill Grave #64 Presbyterian More About JAMES MAGGS: Ancestral File Number: LN0V-G01 Burial: 26 Sep 1888, Box Hill, Victoria, Australia1 Christening: 20 Oct 1816, Clutton, Somerset, England1 Record Change: 03 Oct 20041 More About HARRIET MARTHA BANFIELD: Ancestral File Number: LN0V-N11 Burial: 14 May 1875, Box Hill, Victoria, Australia1 Christening: 31 Aug 18171 Record Change: 29 Nov 20041 More About ROSENA MAHON: Record Change: 01 Dec 20011 Children of JAMES MAGGS and HARRIET BANFIELD are: i. EMMA6 MAGGS1, b. 13 Nov 1843, Clutton, Somerset, England1. More About EMMA MAGGS: Record Change: 08 Jul 20031 2. ii. JOSEPH MAGGS, b. 05 Jun 1845, Clutton, Somerset, England; d. 24 Jun 1886, Ringwood, Victoria, Australia. iii. JEMIMA MAGGS1, b. 25 Oct 1848, Clutton, Somerset, England1; d. 1852, Ticonderoga Bay, Victoria, Australia1. More About JEMIMA MAGGS: Record Change: 24 Jan 20031 3. iv. SAMUEL MAGGS, b. 11 May 1851, Clutton, Somerset, England; d. 30 Aug 1942, Croydon, Victoria, Australia. v. MARY JANY MAGGS1, b. 03 Dec 1855, Konung Creek, Victoria, Australia1; d. 27 Dec 18551. More About MARY JANY MAGGS: Record Change: 23 Jan 20051 4. vi. JANE MAGGS, b. 19 Dec 1858, Blackburn, Victoria, Australia; d. 05 Jul 1926, , Victoria, Australia. 5. vii. JAMES MAGGS, b. 1862, Nunawading; d. 1925, Fitzroy. Generation No. 2 2. JOSEPH6 MAGGS (JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)1 was born 05 Jun 1845 in Clutton, Somerset, England1, and died 24 Jun 1886 in Ringwood, Victoria, Australia1. He married MARY ANN READ1 01 Apr 1867 in Templestowe, Victoria, Australia1. She was born Abt. 1847 in of Templestowe, Victoria, Australia1, and died 1925 in Ringwood, Victoria, Australia1. Notes for JOSEPH MAGGS: Joseph Maggs born 5 Jun 1845 at Clutton, Somerset, England, arrived in Australia age 7 years. He married Mary Ann Read, in Apr 1867 at Templestowe, selected land, Lot 26a,in Ringwood on the corner of Eastfield Road and Mt.Dandenong Road, approx 114 acres, at 11 o'clock 2 Feb 1870. He planted 4 acres with fruit trees valued at 80 pounds and by Sep 1874 his occupation was farmer and wood carter. A 4 room house of lathe and plaster with a paling roof, a kitchen, a slab and bark stable and a pigsty had been errected to a value of 71 pounds. A well, 3 dams, clearing and fencing valued at 96 pounds are also listed. He notes "from the nature of the land, being very poor and heavily timbered, I have not been quite able to clear the complement required, not having means sufficient to do so, neither will the land pay when cultivated." Traces of antimony were found on the land but not in commercial quantities, however during the 1880s white clay was mined here, which he carted for the Victoria Porcelain Clay Coy. In Mar 1880 he was granted freehold title at a price of one pound per acre. More About JOSEPH MAGGS: Burial: Box Hill, Victoria, Australia1 Record Change: 18 Feb 20011 More About MARY ANN READ: Burial: Box Hill, Victoria, Australia1 Record Change: 21 Jul 20021 Children of JOSEPH MAGGS and MARY READ are: 6. i. EMMA7 MAGGS, b. 08 Jan 1868, Templestowe, Victoria, Australia; d. 03 Aug 1939, Richmond, Victoria, Australia. ii. ALBERT MAGGS1, b. 01 May 1871, Nunawading, Victoria, Australia1; d. 15 Nov 1893, Ringwood, Victoria, Australia1. More About ALBERT MAGGS: Record Change: 12 Oct 19971 7. iii. HUBERT MAGGS, b. 10 May 1873, Ringwood, Victoria, Australia; d. 11 Aug 1956, Wagga Wagga, N.S.W., Australia. iv. HARRIET ANNIS MAGGS1, b. 13 Aug 1875, Box Hill, Victoria, Australia1; d. Ringwood, Victoria, Australia1. More About HARRIET ANNIS MAGGS: Burial: 21 Sep 1875, Box Hill, Victoria, Australia1 Record Change: 18 Feb 20011 v. JOSEPH MAGGS1, b. 25 Sep 1876, Box Hill, Victoria, Australia1; d. 03 Oct 1900, Mitcham, Victoria, Australia1. More About JOSEPH MAGGS: Record Change: 18 Feb 20011 8. vi. HARRIET ANNIS MAGGS, b. 18 Aug 1879, Ringwood, Victoria, Australia; d. 08 May 1945. vii. WILLIAM MAGGS1, b. 03 Sep 18811; d. 06 Apr 1950, South Melbourne, Victoria, Australia1; m. MARY ELIZA HARDIDGE1, 24 Dec 1912, Goulburn, N.S.W., Australia1; b. Abt. 1884, , of Victoria, Australia1; d. 1956, Lilydale, Victoria, Australia1. More About WILLIAM MAGGS: Record Change: 18 Feb 20011 More About MARY ELIZA HARDIDGE: Record Change: 18 Feb 20011 viii. DORA JANE DULCIE MAGGS1, b. 13 Dec 1883, Ringwood, Victoria, Australia1; d. 1973, Mitcham, Victoria, Australia1. More About DORA JANE DULCIE MAGGS: Record Change: 21 Jan 20021 9. ix. DELIA ROSE MAGGS, b. 20 Feb 1886, Ringwood, Victoria, Australia; d. 30 Oct 1914. 10. x. AGNES MAGGS, b. 16 Jun 1869, Templestowe, Victoria, Australia; d. 03 Feb 1912, Heathmont, Victoria, Australia. 3. SAMUEL6 MAGGS (JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)1 was born 11 May 1851 in Clutton, Somerset, England1, and died 30 Aug 1942 in Croydon, Victoria, Australia1. He married ELIZA ANN BARNES1 04 Oct 1876 in Nunawading, Victoria, Australia1. She was born 19 Sep 1848 in St Lukes, London, England1, and died 17 Feb 1923 in Croydon, Victoria, Australia1. Notes for SAMUEL MAGGS: SAMUEL MAGGS grew up on his father's property in Springfield Road, Blackburn, one block east of Surrey Road. West of Surrey Road and fronting to White Horse Road was James Barnes' property, so by walking through the Maggs land and crossing Surrey Road, one might enter the back of the Barnes land, an easy way to visit ELIZA ANN BARNES. On the 4 Oct 1876 Sam and Eliza were married at her father's house. Sam wrote to the Secretary for Lands on the 29 Sep 1880, requesting that Allot. 39 Parish of Warrandyte be made available for selection. This block had been refused for selection earlier on the objection of the Mines Department as it was believed that the area was auriferous. When told that the block was available, Sam marked it at 5 o'clock December 3rd and applied for a lease of 12 acres 3 rods and 34 perches on the 6th December. On the application it is noted that he already had leasehold of 104 acres. His license was approved 7 Mar 1881 at a rate of 6 shillings and 6 pence per halfyear. Previously paid fees and rental came to 3 pounds 18 shillings, and he paid another pound for a certificate fee, a pound lease fee, plus the first half years rental, then proceeded to develop the land into an apple and cherry orchard.In 7 Mar 1898 he had succeeded in securing the freehold grant of the area by paying 2 pounds 18 shillings 6 pence fees due,plus a 1 guinea grant fee and assurance fund contribution of 7 pence, a total of 4 pounds and 1 penny. The orchard occupied the area between White Horse Rd and Mullum Mullum Creek,from Oban Rd east to where White Horse Road, now the Maroondah Highway, takes a slight turn to the right, near the Burnt Bridge. Sam and Eliza built a house on Sec38 and planted Fivecrown apples grafted on a Maggs Seedling stock at 24 ft spacing. Trees put in about 1875 were yielding up to twenty bushells 30 years later. He didn't approve of regulations which required spraying for codlin moth and was reputed to have said when denied coolstorage space until he sprayed his trees, "No one is going to tell me how to grow apples and anyway a bit of codlin is good for you". More About SAMUEL MAGGS: Ancestral File Number: LN0V-8X1 Record Change: 20 Aug 19971 Notes for ELIZA ANN BARNES: ELIZA ANN BARNES married SAMUEL MAGGS, son of neighbouring land owner, James Maggs, 4 Oct 1876 and had 6 children. She had a stroke about 1921 but was able to attend her seventyfourth birthday party held at her daughter Jane Knee's home in Sep 1922 when over forty family members gathered for the celebration(see photo). She died 17 Feb 1923 at Croydon. More About ELIZA ANN BARNES: Ancestral File Number: LN0V-2W1 Record Change: 20 Aug 19971 Children of SAMUEL MAGGS and ELIZA BARNES are: 11. i. GEORGE7 MAGGS, b. 28 Dec 1876, Warrandyte, Victoria, Australia; d. 09 May 1947, Ringwood, Victoria, Australia. 12. ii. ELIZA JANE MAGGS, b. 27 Jul 1878, Ringwood, Victoria, Australia; d. 31 May 1946, Camberwell, Victoria, Australia. 13. iii. JAMES MAGGS, b. 15 May 1880, Lilydale, Victoria, Australia; d. 28 Jul 1940, Ringwood, Victoria, Australia. iv. JANE MAGGS1, b. 22 May 1884, Warrandyte, Victoria, Australia1; d. 31 Jan 19711; m. THOMAS SAMUEL KNEE1, 1907, , Victoria, Australia1; b. 07 Aug 1881, Lilydale, Victoria, Australia1; d. 19 Apr 19601. More About JANE MAGGS: Burial: Box Hill, Victoria, Australia1 Record Change: 18 Feb 20011 More About THOMAS SAMUEL KNEE: Burial: 21 Apr 1960, Box Hill, Victoria, Australia1 Record Change: 22 Aug 20031 14. v. SAMUEL WILLIAM MAGGS, b. 01 Jan 1889, Ringwood, Victoria, Australia; d. 15 Jan 1955, Ringwood, Victoria, Australia. 15. vi. JEMIMA MAGGS, b. 16 Dec 1881, Warrandyte, Victoria, Australia; d. 02 Nov 1955. 4. JANE6 MAGGS (JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)1 was born 19 Dec 1858 in Blackburn, Victoria, Australia1, and died 05 Jul 1926 in , Victoria, Australia1. She married WILLIAM COOK1 1880 in , Victoria, Australia1. He was born Abt. 1859 in Wickliffe, Victoria, Australia1, and died 09 Aug 19391. Notes for JANE MAGGS: Jane Maggs, the only surviving daughter of James and Harriet, married William Cook and had one child, Harriet Amy Cook, known to her relatives as Cousin Amy. She never married and lived in the house inWhitehorse Road, Mitcham built by her parents, for many years until her death in 1962. She took a keen interest in family history and was a great source of information and memorabilia about the early days of the Ringwood area. More About JANE MAGGS: Burial: Box Hill1 Record Change: 18 Feb 20011 More About WILLIAM COOK: Burial: 10 Aug 1939, Box Hill, Victoria, Australia1 Record Change: 05 Nov 20011 Child of JANE MAGGS and WILLIAM COOK is: i. HARRIET AMEY7 COOK1, b. 1881, Box Hill, Victoria, Australia1; d. 13 Sep 1962, Surrey Hills, Victoria, Australia1. More About HARRIET AMEY COOK: Burial: 17 Sep 1962, Box Hill, Victoria, Australia1 Record Change: 18 Feb 20011 5. JAMES6 MAGGS (JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)2,3 was born 1862 in Nunawading4, and died 1925 in Fitzroy4. He married (1) THERESA BROWN4 in Christchurch, New Zealand5. She was born 1869 in Clunes, Victoria, Australia5, and died 1930 in Prahran, Victoria, Australia5. He married (2) MARIANNE HARDIDGE6 1880 in Kew6. She was born 1860 in Doncaster6, and died 1941 in Mitcham6. He married (3) ADA JANE CROY7 19127. She was born 1883 in ,Victoria, Australia7. Notes for JAMES MAGGS: James Maggs, the youngest child and only Australian born son of James and Harriet, was an orchardist like his older brothers. He married Marianne Hardidge in 1880 and selected an area in what is now Kalinda Road, adjoining Sam's land. They constructed a four roomed house measuring 26 feet square valued at fifty pounds and stables valued at forty pounds. The buildings were made of palings with an iron roof. Here they raised ten children and lost a little girl, Eliza, aged three weeks. In 1900 James became seriously ill with a kidney disease and was visited during his illness by a wide section of his neighbours, including Mrs Theresa Shanks. He and Theresa became attracted to each other and broke up their marriages, with James and Marianne being divorced in 1906. James and Theresa lived in the Hawthorn and Prahran districts and he became a taxi driver. He contributed to the upkeep of his children although the divorce was a bitter affair. He died in 1925 in Fitzroy and Theresa only survived him by five years. They are buried in the same grave at Box Hill. Marianne became a midwife who delivered over 500 babies in the neighborhood. She was known as Nurse Polly Maggs and the people of Ringwood presented her with a wireless set in appreciation of her service to the community. She died at the age of 81 years in 1941. More About JAMES MAGGS: Burial: Box Hill Cemetery8 Record Change: 01 Sep 20018 Notes for THERESA BROWN: [Ringwood.ged] Theresa had a son Jim Shanks born1902 (father was James Maggs) Reg No 12243R More About THERESA BROWN: Burial: 05 Feb 1930, Box Hill, Victoria, Australia9 Record Change: 01 Sep 200110 More About MARIANNE HARDIDGE: Burial: Box Hill Cemetery10 Record Change: 01 Sep 200110 Marriage Notes for JAMES MAGGS and MARIANNE HARDIDGE: [Ringwood.ged] divorced in 1906 More About ADA JANE CROY: Burial: 15 Apr 1932, Geelong, Victoria, Australia11 Record Change: 10 Aug 200211 Child of JAMES MAGGS and THERESA BROWN is: i. JIM7 MAGGS12, b. 190212. More About JIM MAGGS: Record Change: 01 Sep 200112 Children of JAMES MAGGS and MARIANNE HARDIDGE are: ii. MARY ANN HASE7 MAGGS12, b. 188112. More About MARY ANN HASE MAGGS: Record Change: 01 Sep 200112 16. iii. JANE EMMA MAGGS, b. 1883; d. 28 Jul 1954. 17. iv. JAMES JOHN MAGGS, b. 1885; d. 24 Aug 1962, Parkville, Victoria, Australia. v. DAVID JOSEPH MAGGS12,13, b. 188714; d. 11 Jul 1966, Mt. Waverley, Victoria, Australia15; m. VIOLET ADELINE LEPP15, 1916, , Victoria, Australia15; b. 1888, Ballarat, Victoria, Australia15; d. 26 Mar 1966, ,Victoria, Australia15. More About DAVID JOSEPH MAGGS: Record Change: 01 Sep 200116 More About VIOLET ADELINE LEPP: Record Change: 21 Jan 200217 18. vi. SAMUEL ARTHUR MAGGS, b. 1888; d. 07 Aug 1957, Doncaster, Victoria, Australia. 19. vii. JOHN WILLIAM MAGGS, b. 1890; d. 18 Feb 1959, Cobram, Victoria, Australia. viii. ELIZA ANN MAGGS18, b. 189218; d. 189218. More About ELIZA ANN MAGGS: Burial: Box Hill Cemetery18 Record Change: 01 Sep 200118 20. ix. ROBERT THOMAS MAGGS, b. 1893; d. 12 Mar 1981. 21. x. ALBERT EDWARD MAGGS, b. 1895; d. 1976. 22. xi. EVALEEN VICTORIA MAGGS, b. 1897; d. 05 Sep 1989. xii. HARRIET BANFIELD MAGGS18, b. 189918. More About HARRIET BANFIELD MAGGS: Record Change: 01 Sep 200118 23. xiii. MARY ANN HASE POLLY MAGGS, b. 05 Jul 1881, Ringwood, Victoria, Australia; d. 09 Nov 1961. xiv. HARRIET BANFIELD CHRISSY MAGGS19, b. 14 Dec 1899, Ringwood, Victoria, Australia19; d. 28 Dec 1979, Blackburn, Victoria, Australia19. More About HARRIET BANFIELD CHRISSY MAGGS: Burial: Box Hill19 Record Change: 18 Feb 200119 Children of JAMES MAGGS and ADA CROY are: xv. CLENCIE JOAN7 MAGGS19, m. ARTHUR RODERICK PITTER19. xvi. CLYDE MAGGS19, b. 1917, Collingwood, Victoria, Australia19; d. 1917, Collingwood, Victoria, Australia19. More About CLYDE MAGGS: Record Change: 10 Aug 200219 Generation No. 3 6. EMMA7 MAGGS (JOSEPH6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)19 was born 08 Jan 1868 in Templestowe, Victoria, Australia19, and died 03 Aug 1939 in Richmond, Victoria, Australia19. She married FREDRICK WILLIAM MCGINNIS19 May 1890 in , Victoria, Australia19. He was born in , of Victoria, Australia19. More About EMMA MAGGS: Record Change: 18 Feb 200119 More About FREDRICK WILLIAM MCGINNIS: Record Change: 18 Feb 200119 Children of EMMA MAGGS and FREDRICK MCGINNIS are: i. RENIRA EDDA8 MCGINNIS19. ii. FREDRICK HENRY MCGINNIS19, b. 1894, , of Victoria, Australia19; d. 195819. More About FREDRICK HENRY MCGINNIS: Record Change: 18 Feb 200119 7. HUBERT7 MAGGS (JOSEPH6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)19 was born 10 May 1873 in Ringwood, Victoria, Australia19, and died 11 Aug 1956 in Wagga Wagga, N.S.W., Australia19. He married ISABELLA ATKINS19 09 Mar 1898 in Ringwood, Victoria, Australia19. She was born Abt. 1875 in St Arnaud, Victoria, Australia19. More About HUBERT MAGGS: Burial: Wagga Wagga, N.S.W., Australia19 Record Change: 23 Jan 200519 More About ISABELLA ATKINS: Record Change: 23 Jan 200519 Children of HUBERT MAGGS and ISABELLA ATKINS are: i. HUBERT CARLYLE8 MAGGS19. ii. ANNE THORA MAGGS19. iii. RAYMOND MAGGS19, b. 09 Jun 1905, Ringwood, Victoria, Australia19; d. 20 Jul 190519. More About RAYMOND MAGGS: Record Change: 18 Feb 200119 8. HARRIET ANNIS7 MAGGS (JOSEPH6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)19 was born 18 Aug 1879 in Ringwood, Victoria, Australia19, and died 08 May 194519. She married JAMES RICHARD MILLER19 26 Sep 1910 in Ringwood East, Victoria, Australia19. He was born 1878 in Collingwood, Victoria, Australia19. More About HARRIET ANNIS MAGGS: Record Change: 18 Feb 200119 More About JAMES RICHARD MILLER: Record Change: 18 Feb 200119 Children of HARRIET MAGGS and JAMES MILLER are: i. DUDLEY8 MILLER19. ii. IRENE DOROTHY MILLER19, b. 10 Nov 1913, , of Victoria, Australia19; d. 29 Sep 199019. More About IRENE DOROTHY MILLER: Burial: Lilydale, Victoria, Australia19 Record Change: 18 Feb 200119 iii. CYRIL MILLER19, b. 26 Sep 1915, , of Victoria, Australia19; d. 05 Apr 197319. More About CYRIL MILLER: Burial: Springvale, Victoria, Australia19 Record Change: 18 Feb 200119 9. DELIA ROSE7 MAGGS (JOSEPH6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)19 was born 20 Feb 1886 in Ringwood, Victoria, Australia19, and died 30 Oct 191419. She married WILLIAM JAMES SHARKIE19. More About DELIA ROSE MAGGS: Burial: Box Hill, Victoria, Australia19 Record Change: 18 Feb 200119 Child of DELIA MAGGS and WILLIAM SHARKIE is: i. RONALD8 SHARKIE19, b. Abt. 1914, , of Victoria, Australia19; d. Abt. 1964, , N.S.W., Australia19. More About RONALD SHARKIE: Record Change: 15 Oct 200119 10. AGNES7 MAGGS (JOSEPH6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)20,21 was born 16 Jun 1869 in Templestowe, Victoria, Australia21, and died 03 Feb 1912 in Heathmont, Victoria, Australia21. She married (1) JOHN DOMONIC MILLER22 189423,24, son of FRANK MILLER and KATE MADDEN. He was born 187025,26, and died 194227,28. She married (2) JOHN DOMINIC MILLER29 1894 in , Victoria, Australia30,31. He was born 1870 in Box Hill, Victoria, Australia31. More About AGNES MAGGS: Burial: Box Hill, Victoria, Australia31 Record Change: 11 Sep 200132 More About JOHN DOMONIC MILLER: Record Change: 11 Sep 200132 More About JOHN DOMINIC MILLER: Record Change: 18 Feb 200133 Children of AGNES MAGGS and JOHN MILLER are: i. ALBERT JOHN8 MILLER33, b. 1894, , of Victoria, Australia33. More About ALBERT JOHN MILLER: Record Change: 18 Feb 200133 ii. LOUIS NICHOLAS MILLER33, b. 1901, , of Victoria, Australia33; d. 197433; m. LILA MERTON33. More About LOUIS NICHOLAS MILLER: Record Change: 18 Feb 200133 iii. LESLIE DOMINIC MILLER33, b. 1904, , of Victoria, Australia33; d. 198933. More About LESLIE DOMINIC MILLER: Record Change: 18 Feb 200133 11. GEORGE7 MAGGS (SAMUEL6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)33 was born 28 Dec 1876 in Warrandyte, Victoria, Australia33, and died 09 May 1947 in Ringwood, Victoria, Australia33. He married ANNIE GRACE SMITH33 26 Mar 1902 in , Victoria, Australia33. She was born Abt. 1878 in of Ringwood, Victoria, Australia33, and died 1967 in Box Hill, Victoria, Australia33. More About GEORGE MAGGS: Record Change: 18 Feb 200133 More About ANNIE GRACE SMITH: Record Change: 21 Jan 200233 Children of GEORGE MAGGS and ANNIE SMITH are: i. CLYDE8 MAGGS33, m. VIOLET OXENBURY33. 24. ii. GEORGE ALBERT MAGGS, b. 17 Jul 1902, Ringwood, Victoria, Australia; d. 1974, Heidelberg, Victoria, Australia. iii. HILDA GLADYS BILLIE MAGGS33, b. 05 Sep 1903, Ringwood, Victoria, Australia33; d. 15 Oct 198733; m. LENARD DRYSDALE REID33. More About HILDA GLADYS BILLIE MAGGS: Burial: Springvale, Victoria, Australia33 Record Change: 18 Feb 200133 iv. MYRTLE OLIVE MAGGS33, b. 24 Dec 1905, Kew, Victoria, Australia33; d. 02 Jan 198333; m. ROBERT SAMUEL BOB HEAD33, 1924, , Victoria, Australia33; b. 1898, , of Victoria, Australia33; d. 15 Oct 1980, Mermaid Beach, Queensland, Australia33. More About MYRTLE OLIVE MAGGS: Record Change: 18 Feb 200133 More About ROBERT SAMUEL BOB HEAD: Burial: 17 Oct 1980, Nerang, Queensland, Australia33 Record Change: 18 Feb 200133 v. FREDERICK STANLEY MAGGS33, b. 10 Jul 1907, of, Victoria, Australia33; d. 26 Jan 1975, Box Hill, Victoria, Australia33; m. (1) RUBY EMILY BRIERLEY33; m. (2) SARAH MRS FREDERICK MAGGS33; m. (3) ISABEL WOOD33. More About FREDERICK STANLEY MAGGS: Record Change: 21 Jul 200233 vi. ALFRED FRANCIS MAGGS33, b. 19 Jun 1909, Ringwood, Victoria, Australia33; d. 06 Feb 198733; m. FRANCES ESTELLE WILLOUGHBY33. More About ALFRED FRANCIS MAGGS: Record Change: 18 Feb 200133 vii. ERIC RAYMOND MAGGS33, b. 29 Nov 1910, Ringwood, Victoria, Australia33; d. 29 Jan 198633; m. THELMA THOMPSON33. More About ERIC RAYMOND MAGGS: Record Change: 18 Feb 200133 viii. MARJORIE FLORENCE MAGGS33, b. 21 Jun 1912, Ringwood, Victoria, Australia33; d. 20 Aug 197433; m. COLIN ADDISON33. More About MARJORIE FLORENCE MAGGS: Record Change: 18 Feb 200133 ix. CLARICE MAGGS33, b. 20 Dec 1913, , Victoria, Australia33; m. RONALD STONE33. More About CLARICE MAGGS: Burial: , Queensland, Australia33 Record Change: 18 Feb 200133 12. ELIZA JANE7 MAGGS (SAMUEL6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)33 was born 27 Jul 1878 in Ringwood, Victoria, Australia33, and died 31 May 1946 in Camberwell, Victoria, Australia33. She married WILLIAM NEWCOMB DOBBIN33 14 Mar 1900 in Ringwood, Victoria, Australia34,35. He was born 02 Aug 1878 in Bendigo, Victoria, Australia35, and died 12 May 1960 in Brighton, Victoria, Australia35. More About ELIZA JANE MAGGS: Ancestral File Number: LN0T-NV35 Record Change: 20 Aug 199735 Notes for WILLIAM NEWCOMB DOBBIN: WILLIAM NEWCOMB DOBBIN, the second child of William Edward Jones Dobbin and Amelia Matilda Shoman, was born at Bendigo in the state of Victoria, on the 2 August 1878. He spent his early childhood years in the goldfields towns of Bendigo and Ballarat but by the time he was of age to start school his family had moved to Melbourne and he commenced his education at the Richmond State school. His first job as a baker's boy in Ringwood included delivering bread by bicycle to homes in that area, and that was how he met ELIZA JANE MAGGS. By the time he turned 17 he had decided to go to Western Australia so in 1895 he embarked on a ship named the "Inaminka" which carried a deck cargo of draught horses. While crossing the Great Australian Bight a severe storm was encountered and three of the fifteen horses on deck were killed. He found work in a timber camp in the south west,near Albany, and lived in a hut made of palings for a time with five other men. While he was there an itinerant Indian photographer named S.Bhan took a picture of the hut with its inhabitants standing outside. Approaching the turn of the century his mind turned to thoughts of marriage. He returned to Victoria and proposed to Eliza Jane. They were married on the 14 March 1900 at Lilydale Road Ringwood according to the rites of the Church of Christ by Thomas Hagger in the presence of George Maggs,the brother of the bride and Elizabeth Frances Bell. He and his bride returned to Western Australia on a ship called the "Oruba" and when their first child was born at Denmark, on the 18 January 1901 he named her VERA ORUBA DOBBIN. Eliza Jane found the living conditions very rough and because of poor health she returned to Victoria when Vera was three months old. William followed on a ship called the "Suvic". Their second child, Cyril William Dobbin was born at Ringwood in October 1902 where William worked an orchard owned by his father-in-law, Sam Maggs. He purchased from Sam an area in Wonga Park Rd, (now Kalinda Rd) north of the creek which had been planted as a cherry orchard and part of the area on the corner of Oban Road He also worked in a pottery and in the 1905 Sands and McDougall directory he is listed as a brick and tile maker. In 1917 he rented premises in Main Street (Whitehorse Road), Ringwood, then newly built by J.B.McAlpin, the estate agent, on the corner of Melbourne Street. The shop between A.C.Beilby's store and McAlpin's office on the corner was opened as "The Railway Fruit and Confectionary Palace" and a shop in Melbourne Street, which adjoined the Main Street shop at the rear, became "The Fernery Refreshment Rooms". Three more children were born at Ringwood, Leonard Suvic in 1905, Clarence Newcomb in 1907, and the youngest child, a daughter named Elvie Olive in 1909. A fruit shop in Melrose Street, Sandringham, "The Covent Garden Fruit Palace" was purchased in 1921 and later taken over by his son Cyril. During the early 1930's his marriage failed and he went to Williamstown and opened a florist shop in the name of Walter Dobson which did very well. He married again and settled down to a life of retirement in Prahran, but his second wife, Elsie Fritzlaff (formerly Mrs Wilson) died unexpectedly and he was left alone once more. His eyesight deteriorated badly in his later years and he eventually entered the Mair Street Home for the Blind in Brighton where he died on the 12 May 1960. More About WILLIAM NEWCOMB DOBBIN: Ancestral File Number: LN0S-PW35 Record Change: 31 Mar 200135 Children of ELIZA MAGGS and WILLIAM DOBBIN are: i. ELVIE OLIVE8 DOBBIN35, m. ROY STEWART35; b. 1904, Landsborough, Victoria, Australia35; d. 30 Jun 1992, , Victoria, Australia35. More About ROY STEWART: Record Change: 18 Feb 200135 ii. VERA ORUBA DOBBIN35, b. 18 Jan 1901, Denmark, W.A., Australia35; d. 16 May 1995, Warwick, W.A., Australia35; m. ALEXANDER FRANCIS LAIRD35, 16 May 1923, Hampton, Victoria, Australia35; b. 24 Sep 1898, Collingwood, Victoria, Australia35; d. 21 Jul 1981, Kallaroo, W.A., Australia35. More About VERA ORUBA DOBBIN: Record Change: 02 Sep 200435 More About ALEXANDER FRANCIS LAIRD: Ancestral File Number: LN0Q-QS35 Record Change: 02 Sep 200435 iii. CYRIL WILLIAM DOBBIN35, b. 22 Oct 1902, Ringwood, Victoria, Australia35; d. 10 Aug 1989, Frankston, Victoria, Australia35; m. FLORENCE CONSTANCE DAVIDSON35, 22 Mar 1925, Brighton, Victoria, Australia35; b. 08 Mar 1903, South Melbourne, Victoria, Australia35; d. Jun 1987, Australia35. More About CYRIL WILLIAM DOBBIN: Record Change: 18 Feb 200135 Notes for FLORENCE CONSTANCE DAVIDSON: Notes: written by Carol Humphrey (daughter) 2001 Florence Constance Davidson, born in South Melbourne, was the second eldest child in her family. Her father worked for the Victorian railways and while stationed in Hamilton, Victoria, had met and married her mother. The family moved to the city from Hamilton, in 1903. They spent a brief period in South Melbourne before taking up residence in Ringwood. Throughout her life Florence answered to many different versions of her name. When she was small could never manage to say her full name, the best she could come up with was “Wonnie Connie Davie”. All of her life her immediate family called her “Won” (a shortened version of “Wonnie”). Her husband, Cyril, called her Florrie and her close friends called her Flo. She attended State School 2997, at the corner of Whitehorse Road and Ringwood Street, Ringwood. In the later stages of her schooling, each Wednesday, she travelled to Glenferrie Technical College (now Swinburne College) in Burwood Road, to attended cooking and laundry classes. She travelled by train to attend these classes and was given 1/- (one shilling) to cover the expenses for the day. A three course meal, which she helped to prepare, cost 3d. (three pence), her train fare cost 8d. (eight pence), leaving her one penny. Depending on the family finances for that week, sometimes she was allowed to spend the change. After leaving school she signed up as an apprentice tailoress. She began her apprenticeship on 9th May 1919, with Charles Lane & Co., whose workroom was in Flinders Lane Melbourne, between Elizabeth and Market Streets; the shop was on the corner of Flinders Lane and Elizabeth Street. Her wages for the first six months were 7 shillings and 6 pence and they increased gradually over the four year period of the apprenticeship to 35 shillings. After completing her apprenticeship she worked at Jimmy Oliver’s workroom at the back of Melbourne Town Hall, in Little Collins Street. She left this position when she married Cyril Dobbin in 1925. During her married life Florence worked in the family business in Melrose Street, as well as raising a family of 6 children. She sewed and knitted for her children, was a great cook and she was very meticulous with her laundry, which was probably a reflection of her lessons in cooking and laundry taken years earlier. In later life, when she had more time to herself, she loved to read and was a wizard at crossword puzzles, cryptic crossword puzzles and Scrabble (a word game). More About FLORENCE CONSTANCE DAVIDSON: Record Change: 18 Feb 200135 iv. LEONARD SUVIC DOBBIN35, b. 04 Jan 1905, Ringwood, Victoria, Australia35; d. Jan 194435; m. ALMA WEBSTER35. More About LEONARD SUVIC DOBBIN: Record Change: 18 Feb 200135 v. CLARENCE NEWCOMB DOBBIN35, b. 17 Mar 1907, Ringwood, Victoria, Australia35; d. 22 Jun 1977, Prahan, Victoria, Australia35; m. ELLEN PEARL ISELIN35, 04 Jul 1936, Camberwell, Victoria, Australia35; b. 17 Nov 1910, Richmond, Victoria, Australia35; d. 24 Aug 1979, Burwood, Victoria, Australia35. More About CLARENCE NEWCOMB DOBBIN: Record Change: 18 Feb 200135 More About ELLEN PEARL ISELIN: Record Change: 18 Feb 200135 13. JAMES7 MAGGS (SAMUEL6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)35 was born 15 May 1880 in Lilydale, Victoria, Australia35, and died 28 Jul 1940 in Ringwood, Victoria, Australia35. He married CATHERINE ATKINS35 24 Apr 1901 in , Victoria, Australia36,37. She was born 04 Nov 1882 in St Arnaud, Victoria, Australia37, and died 11 Oct 1960 in Ringwood, Victoria, Australia37. More About JAMES MAGGS: Burial: 30 Jul 1940, Box Hill, Victoria, Australia37 Record Change: 23 Jan 200537 More About CATHERINE ATKINS: Burial: 18 Oct 1960, Box Hill, Victoria, Australia37 Record Change: 18 Feb 200137 Children of JAMES MAGGS and CATHERINE ATKINS are: i. RUBY ISABEL GENIVEVE8 MAGGS37, m. (1) RODERICK CASSIDY37; m. (2) CHARLES BRUCE37. ii. BEULAH LEAH DRUCILLA DAPHNE MAGGS37, m. HERBERT BOPPEL37. iii. OLIVER SAMUEL JAMES MAGGS37, b. 10 Jan 1903, Ringwood, Victoria, Australia37; d. 1974, Box Hill, Victoria, Australia37; m. RITA MARGUERITE PICKETT37; b. Abt. 1903, of, Victoria, Australia37; d. 1971, Ringwood, Victoria, Australia37. More About OLIVER SAMUEL JAMES MAGGS: Record Change: 22 Jul 200237 More About RITA MARGUERITE PICKETT: Record Change: 21 Jan 200237 iv. DOUGLAS LINDSAY GORDON MAGGS37, b. 30 Dec 1904, Ringwood, Victoria, Australia37; d. 1977, ,Victoria, Australia37; m. EDITH EMMA ANNE MEYLAND37, Abt. 1930, , Victoria, Australia37; b. 01 Oct 1905, of, Australia37; d. 1980, ,Victoria, Australia37. More About DOUGLAS LINDSAY GORDON MAGGS: Record Change: 21 Jul 200237 More About EDITH EMMA ANNE MEYLAND: Record Change: 21 Jul 200237 v. LAURENCE REGINALD VIVIAN MAGGS37, b. 26 Jun 1906, Ringwood, Victoria, Australia37; d. 04 Jul 1955, Ashburton, Victoria, Australia37; m. DOROTHY CLAIRE SKURRIE37. More About LAURENCE REGINALD VIVIAN MAGGS: Record Change: 18 Feb 200137 vi. BASIL RODERICK SYLVESTER MAGGS37, b. 06 Sep 191037; d. 04 Oct 1969, Aspendale, Victoria, Australia37; m. DOROTHY BURLOCK37. More About BASIL RODERICK SYLVESTER MAGGS: Record Change: 21 Jan 200237 vii. LEWIS KEVIN MAXWELL MAGGS37, b. 30 May 1912, , of Victoria, Australia37; d. 11 Nov 1948, Ringwood, Victoria, Australia37. More About LEWIS KEVIN MAXWELL MAGGS: Record Change: 13 Jul 200037 viii. RONALD ALBURY RUSSEL MAGGS37, b. 25 Sep 1914, , Victoria, Australia37; d. 20 Mar 1960, St Kilda, Victoria, Australia37; m. ELVIE MARY IRENE MAGGS37, Abt. 1946, , Australia37; b. 02 Jun 1920, , of Victoria, Australia37; d. 04 Feb 196837. More About RONALD ALBURY RUSSEL MAGGS: Burial: 23 Mar 1960, Springvale, Victoria, Australia37 Record Change: 18 Feb 200137 More About ELVIE MARY IRENE MAGGS: Record Change: 18 Feb 200137 ix. JAMES RALPH MCKENNA MAGGS37, b. 17 Nov 1921, , Victoria, Australia37; d. 18 Aug 1973, Ashwood, Victoria, Australia37; m. SYLVIA GRACE MAGGS37, Abt. 194237; b. 1925, of, Victoria, Australia37; d. 22 May 200237. More About JAMES RALPH MCKENNA MAGGS: Burial: 22 Aug 1973, Templestowe, Victoria, Australia37 Record Change: 18 Feb 200137 More About SYLVIA GRACE MAGGS: Record Change: 24 Mar 200337 14. SAMUEL WILLIAM7 MAGGS (SAMUEL6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)37 was born 01 Jan 1889 in Ringwood, Victoria, Australia37, and died 15 Jan 1955 in Ringwood, Victoria, Australia37. He married MINA LILLIAN SCHUHKRAFT37 21 Jun 1911 in , Victoria, Australia37. She was born 21 Jun 189037, and died 1974 in Leongatha, Victoria, Australia37. More About SAMUEL WILLIAM MAGGS: Record Change: 18 Feb 200137 More About MINA LILLIAN SCHUHKRAFT: Record Change: 21 Jan 200237 Children of SAMUEL MAGGS and MINA SCHUHKRAFT are: i. BRIAN LESLIE8 MAGGS37, m. JEAN AIRD37. ii. CLIVE LIONEL MAGGS37, m. ALBERTA HARRIS37. iii. DONALD FREDERICK MAGGS37, m. PAULEEN HIGGS37. iv. RUSSELL IAN MAGGS37, m. VINA ANDERSON MILLAR37; b. 21 Jan 1928, Kew, Victoria, Australia37; d. 04 Nov 199437. More About VINA ANDERSON MILLAR: Record Change: 10 Jul 200237 v. MINA LYLA MAGGS37, m. WILLIAM ERNEST MATTHEWS37. vi. NANCY ELIN MAGGS37, m. ROBERT JOHN BRUCE37. vii. KEITH ALAN MAGGS37. 15. JEMIMA7 MAGGS (SAMUEL6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)38,39 was born 16 Dec 1881 in Warrandyte, Victoria, Australia39, and died 02 Nov 195539. She married EDWARD LINDSAY40,41 190542, son of JAMES LINDSAY and HELEN CORMLEY. He was born 188242, and died 194243,44. More About JEMIMA MAGGS: Burial: 04 Nov 1955, Box Hill, Victoria, Australia45 Record Change: 16 Jul 200146 Notes for EDWARD LINDSAY: [Ringwood.ged] See Borough Visitors Book 14 Borough Voters Roll 1924 Borough of Ringwood Voters List 12,13 More About EDWARD LINDSAY: Burial: Box Hill Cemetery46 Record Change: 15 Aug 200146 Children of JEMIMA MAGGS and EDWARD LINDSAY are: i. MYRTLE IVY8 LINDSAY46,47, b. 190648; d. 197948; m. BERT QUICK49. More About MYRTLE IVY LINDSAY: Record Change: 15 Aug 200150 ii. EUNICE EVELYN LINDSAY50,51, b. 190952; d. 197552; m. ROY LONG53. More About EUNICE EVELYN LINDSAY: Record Change: 15 Aug 200154 iii. CLUTHA BRUCE LINDSAY54,55, b. 191156; d. 198156. More About CLUTHA BRUCE LINDSAY: Record Change: 15 Aug 200156 16. JANE EMMA7 MAGGS (JAMES6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)56,57 was born 188358, and died 28 Jul 195459. She married FREDERICK ALFRED BLOOM59 14 Oct 1910 in , Victoria, Australia59. He was born 1882 in Doncaster, Victoria, Australia59. More About JANE EMMA MAGGS: Record Change: 01 Sep 200160 More About FREDERICK ALFRED BLOOM: Record Change: 18 Feb 200161 Child of JANE MAGGS and FREDERICK BLOOM is: i. HAROLD GRIFFITHS8 BLOOM61, b. 25 Nov 191161; d. 18 Jun 200061; m. MARJORIE HORSBURGH61. More About HAROLD GRIFFITHS BLOOM: Burial: 23 Jun 2000, Anderson's Creek, Victoria, Australia61 Record Change: 13 Jul 200061 17. JAMES JOHN7 MAGGS (JAMES6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)62,63 was born 188564, and died 24 Aug 1962 in Parkville, Victoria, Australia65. He married JOHANNA IDA EDITH BLOOM65 23 Oct 1912 in , Victoria, Australia65. She was born 1880 in Doncaster, Victoria, Australia65, and died 22 Sep 1964 in Box Hill, Victoria, Australia65. More About JAMES JOHN MAGGS: Burial: Springvale, Victoria, Australia65 Record Change: 01 Sep 200166 More About JOHANNA IDA EDITH BLOOM: Record Change: 18 Feb 200167 Children of JAMES MAGGS and JOHANNA BLOOM are: i. MERLE ADRIENNE8 MAGGS67, m. EDWARD BARNFATHER67. ii. LINTON DAVID MAGGS67, b. 31 Jan 1915, , Victoria, Australia67; d. 28 Nov 198667; m. DOROTHY JEEVES67. More About LINTON DAVID MAGGS: Burial: , Queensland, Australia67 Record Change: 26 Feb 199967 iii. RALPH LINDSAY MAGGS67, b. 05 May 1921, , Victoria, Australia67; d. 1960, , N.S.W., Australia67; m. MAVIS HYLAND67. More About RALPH LINDSAY MAGGS: Record Change: 15 Oct 200167 iv. BETTINA MIRIAM MAGGS67, b. 30 Apr 1923, , Victoria, Australia67; d. 12 Feb 194967. More About BETTINA MIRIAM MAGGS: Burial: Box Hill, Victoria, Australia67 Record Change: 05 Mar 199967 18. SAMUEL ARTHUR7 MAGGS (JAMES6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)68,69 was born 188870, and died 07 Aug 1957 in Doncaster, Victoria, Australia71. He married BERTHA ANNA PUMP71 01 Oct 1913 in , Victoria, Australia71. She was born 1887 in Doncaster, Victoria, Australia71, and died 13 Nov 1963 in Box Hill, Victoria, Australia72,73. More About SAMUEL ARTHUR MAGGS: Record Change: 01 Sep 200174 More About BERTHA ANNA PUMP: Record Change: 18 Feb 200175 Children of SAMUEL MAGGS and BERTHA PUMP are: i. NELLIE8 MAGGS75, m. THOMAS WHITMORE75. ii. MARY MAGGS75, m. (1) HECTOR WHITMORE75; m. (2) THOMAS BAKER75. iii. LESLIE JOHN MAGGS75, m. PATRICIA BONNEY75. 19. JOHN WILLIAM7 MAGGS (JAMES6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)76,77 was born 189078, and died 18 Feb 1959 in Cobram, Victoria, Australia79. He married LILLIAN MABEL MAY SMITH79 20 Nov 1909 in Fitzroy, Victoria, Australia79. She was born 1888 in Walhalla, Victoria, Australia79, and died 18 Jul 1969 in Fitzroy, Victoria, Australia79. More About JOHN WILLIAM MAGGS: Record Change: 01 Sep 200180 More About LILLIAN MABEL MAY SMITH: Record Change: 21 Jan 200281 Children of JOHN MAGGS and LILLIAN SMITH are: i. BASIL ROBERT BOB8 MAGGS81, m. (1) FRANCES MAY CUNNINGHAM81; b. 05 May 1907, North Melbourne, Victoria, Australia81; d. 21 Jan 1947, Lilydale, Victoria, Australia81; m. (2) MARGARET JESSIE PEG LINCOLN81. More About FRANCES MAY CUNNINGHAM: Record Change: 21 Jul 200281 ii. RONALD JNO. MAGGS81. iii. GLADYS ELLA MAGGS81, m. CHARLES KEATING81. iv. EDNA LILLIAN MAGGS81, m. ALBERT ROWE81. v. CLIFFORD HENRY MAGGS81, m. SHIRLEY SMITH81. vi. EVELYN CHRISTINA MAGGS81, m. (1) FREDERICK HENRY CROSS81; b. 18 Aug 1928, of, Australia81; d. 25 Aug 196881; m. (2) LEONARD LLEWELYN HUGHES81; m. (3) RONALD FRANK BOLLARD81. More About FREDERICK HENRY CROSS: Record Change: 18 Feb 200181 vii. IVOR CYRIL EDWARD MAGGS81, b. 03 Mar 1910, Ringwood, Victoria, Australia81; d. 09 Mar 1992, Lilydale, Victoria, Australia81; m. ISABELLA CUNNINGHAM81. More About IVOR CYRIL EDWARD MAGGS: Record Change: 18 Feb 200181 viii. LORNA AGNES MAGGS81, b. 31 Jul 1915, , Victoria, Australia81; d. 1981, Ararat, Victoria, Australia81; m. ALBERT HUNTER81. More About LORNA AGNES MAGGS: Record Change: 18 Feb 200181 ix. EDWARD WILLIAM TINY MAGGS81, b. 08 Feb 1918, , Victoria, Australia81; d. 24 Aug 198281; m. MURIEL EMILY MORELAND81, 23 Jan 194381; b. 07 Dec 1917, of, Australia81; d. 27 Dec 2001, Bega, N.S.W., Australia81. More About EDWARD WILLIAM TINY MAGGS: Record Change: 07 Jan 200281 More About MURIEL EMILY MORELAND: Record Change: 07 Jan 200281 x. JOHN DAVID JACK MAGGS81, b. 05 Jun 192281; d. 04 Feb 1942, Rabaul, New Guinea, Ww281. More About JOHN DAVID JACK MAGGS: Record Change: 18 Feb 200181 xi. MAUREEN LESLEY MAGGS81, b. 12 Jul 1929, , Victoria, Australia81; d. 05 Jul 1989, Melbourne, Victoria, Australia81; m. STEPHEN BELL81. More About MAUREEN LESLEY MAGGS: Record Change: 18 Feb 200181 20. ROBERT THOMAS7 MAGGS (JAMES6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)82,83 was born 189384, and died 12 Mar 198185. He married EDITH ELLEN BRITNELL85 30 Mar 1919 in , Victoria, Australia85. She was born 1893 in , of Victoria, Australia85, and died 07 Sep 1973 in Box Hill, Victoria, Australia85. More About ROBERT THOMAS MAGGS: Burial: Box Hill, Victoria, Australia85 Record Change: 01 Sep 200186 More About EDITH ELLEN BRITNELL: Record Change: 18 Feb 200187 Children of ROBERT MAGGS and EDITH BRITNELL are: i. GRACE ANNIE8 MAGGS87, m. JACOB BENNETT87. ii. BERYL ELLEN MAGGS87. iii. DOROTHY OLIVE PAT MAGGS87, m. ARTHUR BRYAN87; b. 08 May 1928, of, Australia87; d. 06 Jun 2004, ,Victoria, Australia87. More About ARTHUR BRYAN: Record Change: 08 Jun 200487 iv. GORDON ROBERT MAGGS87, m. MARY ELIZABETH BETTY GRAHAM87; b. , , of Victoria, Australia87; d. 28 Oct 1995, Swan Hill, Victoria, Australia87. More About MARY ELIZABETH BETTY GRAHAM: Record Change: 18 Feb 200187 v. WINIFRED FLORENCE MAGGS87, m. FRANK MCMILLAN87. vi. ELVIE MARY IRENE MAGGS87, b. 02 Jun 1920, , of Victoria, Australia87; d. 04 Feb 196887; m. (1) JAMES ANDERSON87; m. (2) RONALD ALBURY RUSSEL MAGGS87, Abt. 1946, , Australia87; b. 25 Sep 1914, , Victoria, Australia87; d. 20 Mar 1960, St Kilda, Victoria, Australia87. More About ELVIE MARY IRENE MAGGS: Record Change: 18 Feb 200187 More About RONALD ALBURY RUSSEL MAGGS: Burial: 23 Mar 1960, Springvale, Victoria, Australia87 Record Change: 18 Feb 200187 vii. ALEXANDER NORMAN MAGGS87, b. 19 Jan 192787; d. 199387. More About ALEXANDER NORMAN MAGGS: Record Change: 18 Feb 200187 viii. ARTHUR THOMAS MAGGS87, b. 22 Jun 1936, , Victoria, Australia87; d. 15 Apr 1945, Ringwood, Victoria, Australia87. More About ARTHUR THOMAS MAGGS: Record Change: 21 Jan 200287 21. ALBERT EDWARD7 MAGGS (JAMES6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)88,89 was born 189590, and died 197690. He married FLORENCE SARAH PEARCE91 06 Jul 1918 in Box Hill, Victoria, Australia91. She was born Abt. 1898 in , of Victoria, Australia91, and died 1973 in Ringwood, Victoria, Australia91. More About ALBERT EDWARD MAGGS: Burial: Springvale, Victoria, Australia91 Record Change: 01 Sep 200192 More About FLORENCE SARAH PEARCE: Record Change: 21 Jul 200293 Children of ALBERT MAGGS and FLORENCE PEARCE are: i. JEAN EVELYN8 MAGGS93, b. 31 Oct 1918, Mitcham, Victoria, Australia93; d. 31 Mar 199093; m. ALBERT ERNEST BENNETT93. More About JEAN EVELYN MAGGS: Record Change: 18 Feb 200193 ii. STANLEY EDWARD MAGGS93, b. 17 Mar 1920, Ringwood, Victoria, Australia93; d. 26 Mar 1980, Ringwood, Victoria, Australia93. More About STANLEY EDWARD MAGGS: Record Change: 22 Jul 200293 iii. RUTH FLORENCE MAGGS93, b. 20 Dec 1923, , Victoria, Australia93; d. 15 Aug 197193; m. THOMAS BOYCE93. More About RUTH FLORENCE MAGGS: Record Change: 18 Feb 200193 22. EVALEEN VICTORIA7 MAGGS (JAMES6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)94,95 was born 189796, and died 05 Sep 198997. She married SYDNEY NORMAN TILL97 12 Jun 1920 in , Australia97. He died 10 Mar 193197. More About EVALEEN VICTORIA MAGGS: Burial: Box Hill, Victoria, Australia97 Record Change: 01 Sep 200198 More About SYDNEY NORMAN TILL: Record Change: 18 Feb 200199 Children of EVALEEN MAGGS and SYDNEY TILL are: i. ALISON8 TILL99. ii. ALWYN TILL99, b. 09 May 192199; d. 28 Aug 1944, , Ww299. More About ALWYN TILL: Record Change: 18 Feb 200199 23. MARY ANN HASE POLLY7 MAGGS (JAMES6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)99 was born 05 Jul 1881 in Ringwood, Victoria, Australia99, and died 09 Nov 196199. She married THOMAS CAREY LAWFORD99 1906 in , Victoria, Australia99. He was born 1883 in Box Hill, Victoria, Australia99. More About MARY ANN HASE POLLY MAGGS: Burial: Box Hill, Victoria, Australia99 Record Change: 18 Feb 200199 More About THOMAS CAREY LAWFORD: Record Change: 18 Feb 200199 Children of MARY MAGGS and THOMAS LAWFORD are: i. LINDA ISOBEL8 LAWFORD99, b. 14 May 190799; d. 08 Mar 199699. More About LINDA ISOBEL LAWFORD: Record Change: 26 Feb 199999 ii. MELBA LAWFORD99, b. 08 May 190899; d. 199599. More About MELBA LAWFORD: Record Change: 26 Feb 199999 iii. OLIVE LAWFORD99, b. 30 Apr 190999; d. 24 Mar 198799; m. ERIC BLANCHFLOWER99. More About OLIVE LAWFORD: Record Change: 26 Feb 199999 Generation No. 4 24. GEORGE ALBERT8 MAGGS (GEORGE7, SAMUEL6, JAMES5, JOSEPH4, WILLIAM3, WILLIAM2, SAMUEL1)99 was born 17 Jul 1902 in Ringwood, Victoria, Australia99, and died 1974 in Heidelberg, Victoria, Australia99. He married THELMA LILIAN SMITH99 17 Oct 1923 in , Australia99. She was born Abt. 1906 in of, Victoria, Australia99, and died 1974 in Melbourne, Victoria, Australia99. More About GEORGE ALBERT MAGGS: Record Change: 21 Jan 200299 More About THELMA LILIAN SMITH: Record Change: 22 Jul 200299 Child of GEORGE MAGGS and THELMA SMITH is: i. SYLVIA GRACE9 MAGGS99, b. 1925, of, Victoria, Australia99; d. 22 May 200299; m. JAMES RALPH MCKENNA MAGGS99, Abt. 194299; b. 17 Nov 1921, , Victoria, Australia99; d. 18 Aug 1973, Ashwood, Victoria, Australia99. More About SYLVIA GRACE MAGGS: Record Change: 24 Mar 200399 More About JAMES RALPH MCKENNA MAGGS: Burial: 22 Aug 1973, Templestowe, Victoria, Australia99 Record Change: 18 Feb 200199 This is the parent record for the archives collection of the Maggs family in the Ringwood area. -
The Beechworth Burke Museum
Photograph, 1999
This photograph features three display board sections showing information and photographs from 'The Harvest' exhibition inside the Burke Museum at Beechworth in 1999. The boards are titled 'To the Market' and 'Orchards'; the accompanying text cannot be read. The two accompanying photographs depict a man and woman picking fruit.This photograph is of social significance to Burke Museum and the Beechworth community, documenting an exhibition, The Harvest, held in 1999 to communicate the importance of agricultural development, specifically of orchards, in the area. The expansion of vineyards and horticulture in the Beechworth district followed gold rush prosperity in the mid-1850s, with nearly ninety acres of gardens and small farms under vineyards by 1865. There were 400 Chinese market gardeners and hawkers in the area in 1868. The growth of agriculture in the Ovens district in the mid -1860s led to advocacy by local farmers for the extension of railway infrastructure from Melbourne to improve access to distant markets.Colour rectangular photograph printed on matte AGFA photographic paper.Obverse: TO THE MARKET / ORCHARDS/ Reverse: 2856beechworth, burke museum, promoting settlement, living in country towns, making regional centres, preserving traditions and commemorating, farming and agriculture, orchards, exhibitions, burke museum exhibitions, fruitpicking, building local economies, transforming land, victorian agricultural history, marketing and promoting agricultural products, growing fruit and vegetables, the harvest exhibition, harvests, vineyards, victorian gold rush towns -
The Beechworth Burke Museum
Geological specimen - Malachite, Unknown
Malachite is typically found as crystalline aggregates or crusts, often banded in appearance, like agates. It is also often found as botryoidal clusters of radiating crystals, and as mammillary aggregates as well. Single crystals and clusters of distinguishable crystals are uncommon, but when found they are typically acicular to prismatic. It is also frequently found as a pseudomorph after Azurite crystals, which are generally more tabular in shape. This particular specimen was recovered from the Burra Burra Copper Mine in Burra, South Australia. Otherwise known as the 'Monster Mine', the Burra Burra Copper Mine was first established in 1848 upon the discovery of copper deposits in 1845. Within a few short years, people from around the world migrated to Burra to lay their claim in the copper economy. By April 1848 the mine was employing over 567 people and supporting a population of 1,500 in the local township. Up until 1860, the mine was the largest metals mine in Australia, producing approximately 50,000 tonnes of copper between 1845 to its closure in 1877. The Burra Burra Mine was also famous for a number of other specimens, including; crystalline azurite, cuprite, and botryoidal and malachite. Malachite is considered a rare gemstone in that the original deposits for the stones have been depleted leaving behind very few sources. In addition, the use of Malachite as gemstones and sculptural materials remains just as popular today as they were throughout history. It is quite common to cut the stone into beads for jewellery. The fact that Malachite has such a rich colour and one that does not fade with time or when exposed to light makes it particularly rare. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A solid hand-sized copper carbonate hydroxide mineral with shades of blue and light green throughout. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, burra, burra burra mine, south australia, malachite, malachite specimen -
The Beechworth Burke Museum
Geological specimen - Malachite, Unknown
Malachite is a green copper carbonate hydroxide mineral and was one of the first ores used to make copper metal. Malachite has been utilised as a gemstone and sculptural material in the past as its distinctive green color does not fade when exposed to light or after long periods of time. Malachite is formed at shallow depths in the ground, in the oxidizing zone above copper deposits. The material has also been used as a pigment for painting throughout history. This particular specimen was recovered from the Burra Burra Copper Mine in Burra, South Australia. Otherwise known as the 'Monster Mine', the Burra Burra Copper Mine was first established in 1848 upon the discovery of copper deposits in 1845. Within a few short years, people from around the world migrated to Burra to lay their claim in the copper economy. By April 1848 the mine was employing over 567 people and supporting a population of 1,500 in the local township. Up until 1860, the mine was the largest metals mine in Australia, producing approximately 50,000 tonnes of copper between 1845 to its closure in 1877. The Burra Burra Mine was also famous for a number of other specimens, including; crystalline azurite, cuprite, and botryoidal and malachite.Malachite is considered a rare gemstone in that the original deposits for the stones have been depleted leaving behind very few sources. In addition, the use of Malachite as gemstones and sculptural materials remains just as popular today as they were throughout history. It is quite common to cut the stone into beads for jewellery. The fact that Malachite has such a rich colour and one that does not fade with time or when exposed to light makes it particularly rare. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A solid hand-sized copper carbonate hydroxide mineral with shades of yellow, blue, and light green throughout.geological, geological specimen, burke museum, indigo shire, malachite, malachite specimen, burra burra mine, burra, south australia, australian mines, mines, monster mine -
The Beechworth Burke Museum
Geological specimen - Galena Chalcopyrite, Unknown
Galena Chalcopyrite is the earth's primary ore of lead and is mined from a large number of deposits in many countries. It is also an important source of silver. Galena Chalcopyrite is one of the most abundant and widely distributed sulfide minerals across the world. The mineral is found in igneous and metamorphic rocks in medium- to low-temperature hydrothermal veins. This specific specimen was recovered from the mines in Broken Hill, New South Wales. The mines in Broken Hill were first established after Charles Rasp discovered a large amount of silver-lead-zinc ore-body in the area in 1883. BHP (Broken Hill Proprietary) mining company was then established in 1885 and quickly became the lead in Australia's mining industry after they began excavating and exporting the country's largest amount of lead, silver, and zinc. This feat generated over $100 billion in wealth for the company.Galena Chalcopyrite is signifiant as it represents the catalyst for the rise of Australia's most influential mining companies - BHP. The mineral was one of the first to be mined in the country and after being made into lead, was used for a variety of things such as paint, batteries, ammunition, and plumbing materials before it was known to be harmful to humans. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A grey, solid hand-sized lead sulfide mineral with a silver metallic luster.burke museum, beechworth, geological, geological specimen, galena, galena chalcopyrite, chalcopyrite, broken hill, bhp, bhp mining, broken hill mine, mine, australia mine, lead, lead mine -
The Beechworth Burke Museum
Geological specimen - Feldspathic Sandstone
Feldspathic arenites are sandstones that contain less than 90% quartz, and more feldspar than unstable lithic fragments, and minor accessory minerals.Feldspathic sandstones are commonly immature or sub-mature.These sandstones occur in association with cratonic or stable shelf settings. Feldspathic sandstones are derived from granitic-type, primary crystalline, rocks. If the sandstone is dominantly plagioclase, then it is igneous in origin Sandstone features prominently in public buildings throughout Victoria. Most of the sandstone used as dimension stone in the State came from three sources: the Heatherlie quarry in the Grampians (Silurian), the Bacchus Marsh area (Permian), and the Barrabool Hills near Geelong (Cretaceous).Sandstone features prominently in public buildings throughout Victoria, making this specimen special as it shows the materials used by Victorian building companies. Sandstone can also be crushed, crushed stone is used in the construction of roadways and road structures such as bridges, and in buildings, both commercial and residential. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A feldspar-rich sandstone, a sandstone intermediate in composition between an arkosic sandstone and a quartz sandstone, containing 10% to 25% feldspar and less than 20% matrix material of clay, sericite, and chlorite. Feldspathic arenite containing less than 90 percent of the composition of quartz. Feldspar is the main composition. Feldspathic arenite may contain fragments of unstable rock, and a little amount of other minerals such as mica and heavy minerals. Some feldspathic arenite have pink or red color because of the presence of potassium feldspar or iron oxide. There are also colored light gray to white. These sandstones are usually medium to coarse grained and can contain a high percentage of granules with angular until subangular roundness. The content of the matrix can appear as the rest up to more than 15 percent, and sorting of grains can present as moderate to poorly sorted. Feldspathic sandstones are generally immature in textural maturity. Feldspathic arenite can not be judged from the structure of the sediment. Bedding can emerge from the laminate parallel to the crossbed. Fossils may appear in the layer deposited on the sea. Feldspathic arenites usually appear on the craton or the continental shelf, which can be associated with conglomerate, quartz lithic arenite, carbonate rock, or evaporites. This sandstone may also appear on the succession of sedimentary basins deposited on an unstable or deep sea, and moving arc setting. According to Pettijohn (1963) Arkose make up about 15 percent of all sandstones. Some Arkose formed in situ when the granite and related rocks disintegrate and generate granular sediments. Most of the material feldspathic sandstones derived from primary crystalline granitic rocks, such as granite or metasomatic rocks containing abundant potassium feldspar. Mineral contained in sandstones is mostly a form of plagioclase feldspar derived from quartz diorite or volcanic rock. Feldspar contained on this sandstone comes from arid to cool climates when the chemical weathering process is reduced.sandstone, natural stone, feldspathic sandstone, burke museum, geology, geological, geological specimen -
The Beechworth Burke Museum
Geological specimen - Ilvaite
Ilvaite has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns . This specimen was retrieved from Broken hill, known as the world's richest and largest zinc-lead ore deposit. Because of Ilvaite's often unaesthetic crystal formations compared to other minerals, Ilvaite is uncommon in most rock collections, particularly specimens that are not well formed, such as this one. Ilvaite is also a member of the Sorosilicate subclass of the silicate minerals, which have an unusual basic unit of Si2O7, making Ilvaite a unique mineral. Given that Ilvaite is not commonly found in Australia, it marks a unique contribution to an Australian collection of minerals. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized ferrous iron analogue mineral with of black with shades of beige Ilvaite is a brittle, opaque rock formation that has acquired its name from Ilva (Latin for Elba) Island, Greece, where Ilvaite is most commonly found. The geological setting in which Ilvaite occurs is through contact with magnetite, zinc and copper ore deposits, along with contact metamorphic deposits and zeolite zones. llvaite crystallizes in the form of black prismatic crystals and columns rock, mineral, ilvaite, ilvaite specimen -
The Beechworth Burke Museum
Geological specimen - Porphyritic Rhyodacite
This specimen was recovered from the Nigretta Falls (previously named the Upper Wannon Falls), Victoria. The falls are fed by the Wannon River that has its head waters in the Grampians mountains. Approx. 10km upstream of the Wannon Falls, Nigretta is a multi-channel segmented cascade of smaller drops and bounces guided by patterns of joints in a much older (Devonian) rhyolitic volcanic rock. Both the Wannon and Nigretta Falls are iconic landscape features, entrenched in the history and identity of the region. These falls are particularly rare as they are the product of volcanic activity, which is unique in the context of the Volcanic Plain of Victoria. Waterfalls of this capacity are generally associated with the Uplands areas of Victoria, rather than the edges of the Volcanic Plain. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. A solid, dark grey mineral specimen with pale terracotta coloured inclusions. Rhyodacite is a volcanic rock intermediate in composition between dacite and rhyolite. Rhyodacites form from rapid cooling of lava relatively rich in silica and low in alkali metal oxides.GEOLOGICAL SURVEY / R / S 55 FELSTONE PORPHYburke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, porphyritic rhyodacite, lava, nigretta falls, upper wannon falls, dacite, rhyolite, volcanic geology -
The Beechworth Burke Museum
Geological specimen - Loellingite in Rhodonite
Rhodonite is a reddish-pink manganese silicate material and often contains iron, magnesium and calcium. It is usually found in metamorphic rocks (rocks which have been altered by heat, pressure or chemical process). It can range in size from tiny to massive. Because of their composition they are not suitable for use in jewellery because they are hard enough. It is quite rare to find, though has been found in Australia, North America, South America and Europe.This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. This specimen is a palm shaped piece of loellingite within rhodonite. It is mostly reddish-pink coloured, with flecks of light and dark grey. Loellingite is a grey iron arsenide which often forms into crystal shapes. It is mostly found in mesothermal veins (caused by immense heat) with sulfides or in limestone. It is toxic when heated or struck. rhodonite, loellingite, burke museum, beechworth, geological survey of victoria -
The Beechworth Burke Museum
Geological specimen - Copper Ore
This specimen was recovered from Silverton Mine in Broken Hill, New South Wales. Otherwise known as the 'Day Dream Mine', the Silverton Mine was first established in 1883, when silver and lead deposits where discovered. Within a few short years, the population of Broken Hill reached 3000 people. As of today the Silverton Mine is still open, and has produced over 200 million tonnes of ore, which has generated over $100 billion. The Silverton Mine was also famous for a number of specimens such as silver, iron and zinc.Copper is considered to be a rare ore in that finding it in its pure form is rare. Nowadays when mining for Copper it is often found in mixed in with other minerals or it is recycled from use. Moreover, Copper is found in a range of everyday uses such as coins, cookware, pipes, heating conductors and anything that generate electricity. The fact that Copper is heat a heat conductor, electricity conductor and it does not corrode easily, makes this ore a versatile and useful. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid hand-sized cube-shaped sulfide and oxide with shades of green, grey and brown throughout. Copper is typically found as nuggets in the ground. It can be found in a range of forms such as its native state; mixed with other ores, such as zinc and iron; as porphyry copper deposits; and as major deposits. Porphyry deposits are when the mineral is scattered evenly throughout the rock. Major deposits are when the mineral is scattered amongst other minerals.burke museum, beechworth, indigo shire, beechworth musum, geological, geological specimen, mineraology, copper, copper ore, copper ore speciment, broken hill, new south wales -
The Beechworth Burke Museum
Geological specimen - Hyalite in Basalt
According to the 1912 Department of Mines Bulletin of the Geological Survey of Victoria, basalt covers a considerable portion of the Macedon area including Mount Macedon. Basalt is the most common form of rock underlying the earth's surface and is found in three kinds of rock forming environments: ocean divergent boundaries, oceanic hotspots, and mantle plumes and hotspots beneath continents.This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid mass, geological specimen in shades of grey and white. Hyalite is a colourless variety of opal. It occurs as globular and botryoidal masses and irregular crusts in volcanic and pegmatite environments where the silica deposits from the gas phase. Basalt is dark in colour, fine-grained igneous rock composed of plagioclase and pyroxene minerals. It is commonly formed as an extrusive rock, such as lava flow. It is one of the most common forms of rock underlying the earth's surface.burke museum, geological specimen, department of mines, geological survey of victoria, basalt, mount macedon, beechworth -
The Beechworth Burke Museum
Geological specimen - Brown coal
This particular specimen was recovered from the Lal Lal Coal and Iron Mine in Victoria, 19km from Ballarat. Brown Coal was discovered here in 1857, just alongside the Geelong to Ballarat Railway line. This discovery of lignite (brown coal) was the first in Victoria, which would bring important benefits to the region and state, both of which had previously been reliant on coal imports. In the 1860s, iron ore was found just 5km from Lal Lal, and the area was converted into an Iron Ore Mine. The Lal Lal Iron Mining Company took over operations in 1874, who then peaked iron production in 1884. This mine continued operations until June 1884, when the blast furnace was extinguished and never recommenced. The blast furnace at Lal Lal is considered one of the most important and highly significant sites ion early industrial history in Australia, as it is the only remaining best furnace from the nineteenth century in the Southern Hemisphere. The furnace ruins are 17 metres high, and are clearly visible today on Iron Mine Road, Lal Lal, near the Bungal Dam. This specimen of Lignite (brown coal) is significant, as it was mined from the area where brown coal was first discovered in Victoria, leading to an important and controversial future of the mining and use of brown coal in this State. The Victorian Heritage Database has listed the Lal Lal Coal Mine with local significance, with their Statement of Significance stating: "The Lal Lal coal mine is historically significant as the site of the first discovery of lignite (brown coal) in Victoria, and one that promised important benefits to regional and state industries that were reliant on coal imports at the time. The significance of the stie is reduced by the poor state of preservation of the coal mining and processing fabric". This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A hand-sized light-weight, soft and combustable sedimentary rock specimen, that is dark brown in colour. The specimen has jagged edges, as though parts of the rock have crumbled away. Brown coal, or Lignite, is formed naturally from compressed peat, and is typically found in natural basins. The stages to the formation of coal ('coalification') begin with plant material and wood, which will decay if it is not subjected to deep burial or heating, and turn into Peat. Peat, when sufficiently compressed naturally, will turn into Brown Coal (Lignite), and finally into Black Coal (sub-bituminous, bituminous and anthracite). Each successive stage has a higher energy content and lower water content. It is brownish-black in colour. Brown Coal has a high moisture content, between 50 and 75 percent, and a low carbon content. Some Brown Coals may be stratified, with layers of plant matter, which means little coalification has occurred beyond the peat natural processing stage. When Brown Coal is submerged in dilute nitric acid or boiling potassium hydroxide solution, it reacts to produce a reddish solution, of which higher-ranked coals do not. When brown coal is pulverised and burned in boilers, the steam is used to drive turbines, which generates electricity. It is the lowest rank of coal, as when burned, it creates a relatively low heat content, which in turn does not create a great output of steam. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, brown coal, brown coal specimen, lignite, lal lal, lal lal coal mine, lal lal iron mine, ballarat, blast furnace -
The Beechworth Burke Museum
Geological specimen - Granite
Gabo Island sits off the coast of East Gippsland in Victoria, with cliffs of granite in a relatively unique red/pink colour. Early attempts to build a lighthouse on the island were abandoned due to poor foundations, but when a ship ran aground on the nearby Tullaberga Island in 1853 and led to the death of 37 people, efforts were reignited. Construction of a new lighthouse was completed by 1858, using Gabo Island granite. The lighthouse is Australia's second tallest in Australia and continues to play an important role in guiding boats around the coast as they journey between Melbourne and Sydney. The distinct pink colour from the granite means the lighthouse continues to be a defining feature of the island. Gabo Island granite was also used to construct the Treasury Building at 117 Macquarie Street in Sydney, now the Intercontinental Hotel.Granite in the pink colour of this specimen is relatively rare. The connection to the lighthouse on Gabo Island also gives the specimen historic significance and social significance regarding the maritime history of Victoria. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid palm-sized mineral, coloured by flecks of pink, red, and grey. Granite is formed by the slow crystallisation of magma below the earth's surface. It is typically composed of a mix of quartz, feldspar, and other minerals, though syenitic granite like this sample has a smaller amount of quartz than typical granite. This different mineral composition leads to the more distinct pink and red colouring.First sticker: [torn]logical survey / R........ S........ / Loc Gabo Island / 1/4 Sheet / Second Sticker: 15 Third Sticker: Syenitic Graniteburke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, gabo island, gabo island lighthouse, lighthouse, granite, coast, coastal, granite specimen, victoria, coastal cliffs -
The Beechworth Burke Museum
Geological specimen - Precious Opal
In Australia, precious opal is found in Cretaceous age sandstones and mudstones. These sedimentary rocks were deeply weathered and this weathering released silica into the groundwater.Australia is the only part of the world where opalised animal and plant fossils have been found. Opal artefacts several thousands of years old have been discovered in East Africa. As early as 250 BC the Romans prized opals, thought to have come from mines in Eastern Europe, the ancient world's main source of opals. There are many aboriginal dreamtime stories that feature opal. Australian opals discovered during the late 1800's found little favour with European markets but their commercial value increased in the 1900's and in 1932 Australia took over as the major producer of opals in the world and remains the largest producer to this day. Opal is found around the world (Brazil, Mexico, Honduras and the western US) however Australia produces 95% of the world's precious opal and it is our official national gemstone. Opal was first mined commercially at Listowel Downs in Queensland in 1875 and later at White Cliffs in NSW. Today, Coober Pedy (SA) is the main producer of white opal, though in recent years this field has expanded and all types of opals are found. Other centres in SA include Andamooka and Mintabe. Lightning Ridge (NSW) is renowned for black opal and formerly White Cliffs was a large producer of high quality opal. Boulder opals (opals in concretionary ironstone) are mined in Queensland from numerous localities in a zone extending from the Eulo and Cunnamulla district in the south and northwest for a distance of over 700 km to Kynuna in the north. The towns of Quilpie, Yowah and Winton are the main opal mining and wholesale centres. Opals are considered gemstones and have been used in jewellery for thousands of years.Throughout much of history, opals were actually believed to be good luck. The Romans thought that opals were one of the luckiest gemstones and a symbol of hope. In the Middle Ages, opals were believed to be bestowed with all the positive properties of coloured gemstones due to its rainbow-like play of colour. Finally, there is a superstition that you should not wear an opal unless it is your birthstone otherwise misfortune will befall you. This, of course, is far-fetched, but the notion could have been promoted in the late 19th and early 20th Centuries by diamond traders who were trying to increase sales of diamonds and deter people from buying opals. Possibly related to this is the thought that you should set opal jewellery with diamonds as their powers of good fortune will override any negativity held by the opal. The great majority of opal does not show play of colour and is called common opal or potch however this is not the case with a precious opal. Opal is a precious gemstone, like rubies, emeralds or diamonds. Opal is rare, and it is expensive to prospect and mine for.Silica is one of the most common minerals on the planet, but precious opal is very rare – far more rare than diamonds. Precious opal is rare because the natural processes that create it rarely occur.Most (at least 95%) of the opal found by miners is common opal without gem colour. In Australia we call it potch. It can be white, grey, black or amber coloured. Even when a miner finds gem-coloured opal, most of it can’t be cut into gemstones because it’s too thin, or sandy. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.It is not known where this opal originated, except that it is probably from Victoria, as it has been recorded from many localities in the State. Common Opal is formed from silica-rich water circulating through rocks near the Earth’s surface. It consists of minute spheres of silica arranged in different ways. In common opal, the spheres are of different sizes and randomly arranged, unlike in precious opal where the spheres are of similar size and uniformly arranged in three dimensions. These differences account for common opal generally being translucent to opaque and without the play of colours, or opalescence, displayed by precious opal. Common opal is found in many localities and different geological environments throughout Australia and the world. Precious opal requires special conditions to form and is much less common. Australia produces most to the world’s precious opal. burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, precious opal, opal, brazil, mexico, honduras, queensland, coober pedy, gemstones, jewellery, play-of-colour, light blue -
The Beechworth Burke Museum
Geological specimen - Basalt, Unknown
Basalt is a common igneous rock that composes most of the Earth's surface and can be found on the Moon and other rocky planets of the Solar System. It is generally composed minerals such as calcic plagioclase, clinopyroxene and iron ore which form grains that are indistinguishable to the naked eye. It can be dark grey or black in colouring and sometimes may contain holes left by gas bubbles. Most of the Earth's basalt was produced in environments such as oceanic divergent boundaries, oceanic hotspots, and mantle plumes and hotspots beneath continents. Basalt is commonly used in construction where it is crushed and used for multiple purposes such as concrete aggregate, road base, or railroad ballast. Thin slabs of basalt can also be cut and used for floor tiles, stone monuments, and building veneer. This particular specimen was excavated from Talbot in Victoria, which was a small gold mining town established in 1852. As basalt is a common rock, it is not specific to Talbot. However, this specimen can be assumed to be of the Cainozoic age due to previous geomorphic surveys of the area. This particular type of Basalt was used mainly for roads due to the durability of the rock.Basalt holds significance due to the continued use of the rock from historic until present times. The rock has been utilised for many types of construction and is still used for the same purposes today. Basalt also has significance to the Earth and other rocky planets of the Solar System as it makes up most of the planet's surface. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A smaller than hand sized rock specimen which is dark grey in colour with small holes and white deposits across its surface.Geological survey / [illegible] /burke museum, beechworth, geological specimen, geology, basalt, basalt specemin, indigo shire, talbot, cainozoic, igneous rock -
The Beechworth Burke Museum
Geological specimen - Basalt
This specimen was recovered from Creswick in Victoria. Basalt is dark in colour, often black and has a fine grain. It is composed of plagioclase and pyroxene minerals and an igneous rock. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A cylindrical fine-grained piece of igneous rockburke museum, geological survey of victoria, geological specimen, geology -
The Beechworth Burke Museum
Geological specimen - Black Coal
This specimen was recovered from Wonthaggi in Victoria. Coal is a sedimentary rock which is composed of peat after it has been exposed over millions of years. This is an example of Australian black coal which is used as either thermal or coking coal for electricity generation or manufacturing processes. It is predominantly composed of Carbon which is 'C' on the periodic table of elements. This early example of a coal sample, shows the important role that coal played/plays in Australia's energy generation and manufacturing processes. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Small piece of black coal with museum original labelGeological survey / R..... S...../ Locality Cape Patterson coal specimen, burke museum, geological survey of victoria, geological specimen, geology -
The Beechworth Burke Museum
Geological specimen - Gold-Sulphide Ore
This particular specimen was recovered from two hundred feet down in the Golden Mile in Kalgoorlie, Western Australia. The Golden Mile, named after the estimated sixty million ounces of gold worth around one hundred billion dollars, was the birthplace of the largest gold rush in Australia almost one hundred and thirty years ago when William Brookman and Samuel Pearce leased the Great Boulder mine. The Golden Mile is also the home of the Super Pit, Australia's most well-known mine.The majority of gold deposits will form as a native metal, however, on occasion, it can form a compound with another element, in this case, sulphur. Therefore, this specimen is a rare example of gold naturally forming into a compound mineral with sulphur. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A small gold-sulphide ore mineral specimen in shades of silver and grey with flecks of gold. Precious metals are often found in Sulphide Ores, as sulphides usually bind to these metals. They are also extremely symmetrical in crystaline form. Gold-Sulphide Ore occurs when gold forms a natural compound with other elements. In this form, gold can be present in one of two ways. It can be fully immersed in the sulphide, or a portion may be partially free. This specimen has minimal gold visible, with only a few flecks being partially visible.burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, gold-sulphide ore -
The Beechworth Burke Museum
Geological specimen - Chalcopyrite
This specimen originated from Mount Lyell on the west coast of Tasmania, where a large group of open cut and underground copper-silver-gold mines began operating in 1883. Between 1893-1994, the Mt Lyell Mining and Railway Company were responsible for operations. The Mt Lyell copper-gold mines produce some excellent crystallised specimens of chalcopyrite and other minerals. The deposits are generally considered to be of Cambrian volcanic origin, but there are indications of Devonian granitic influence on the ores, plus local remobilisation during Devonian deformation. Over 120 million tonnes of ore was produced from several workings, including the main Prince Lyell mine and the North Lyell mine, which was also of great importance. The Mount Lyell mines have a long history of human and environmental disasters, including the 1912 North Lyell fire that killed 42 miners, and two separate incidents in 2013 in which three people lost their lives. The environmental impacts from this complex of mines are extensive, with waste tailings and heavy metal contamination flowing directly into the King and Queen River catchments. In 1954, the eminent Australian historian, Geoffrey Blainey, published 'The Peaks of Lyell' which delves into the history of the 1912 North Mount Lyell Disaster.Chalcopyrite does not contain the most copper in its structure relative to other minerals, but it is the most important copper ore since it can be found in many localities and occurs in a variety of ore types. The brassy-yellow colours in Chalcopyrite mean it is often confused with pyrites and gold, leading to use of the term, "fool's gold." Chalcopyrite has been the primary ore of copper since smelting began five thousand years ago. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.This hand sized solid mineral specimen has shades of brass-yellow with spots of iridescent green-black tarnish. Chalcopyrite is a copper iron sulphide mineral and a major ore of copper common in sulphide veins and disseminated in igneous rocks. Chalcopyrite has a hardness of 3.5-4 on the Mohs Scale. It is a member of the tetragonal crystal system and has metallic lustre and opaque transparency.burke museum, beechworth, indigo shire, beechworth museum, geology, geological specimen, chalcopyrite, copper pyrites, copper mining, tasmanian geology, mount lyell, mount lyell mines, fools gold, mohs scale, crystals, minerals, historical geological collection, victorian geological survey, a.r.c selwyn, gold rush, van diemans land -
The Beechworth Burke Museum
Geological specimen - Yellow Sandstone
This specimen is from Barefoot Hills, Victoria. Sandstones are economically important as major reservoirs for both petroleum and water, as building materials, and as valuable sources of metallic ores. Most significantly, they are the single most useful sedimentary rock type for deciphering Earth history. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A sedimentary rock composed mostly of quartz sand. Sandstone is the second most common sedimentary rock after shale. Sandstones consist of sand-sized grains principally quartz, feldspar and rock fragments. The two major classes of sandstone are arenite and wacke. the colour of sandstone varies from grey, yellow, red and white reflecting the variation in mineral content and cement and is gritty to touch (like sandpaper).Geological survey / R.... S 61 / Loc Bareboot Hills / Sheet / 24SE / 94 /burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, sandstone, yellow sandstone, victoria, barefoot hills -
The Beechworth Burke Museum
Geological specimen - Chalcedony
This specimen was recovered from Philip Island in Victoria. Chalcedony is composed of Quartz and Silicon Dioxide represented as SIO2. It has and is still used as a gemstone for thousands of years. This is an excellent specimen Chalcedony that shows its aesthetic properties. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. Uniquely shaped piece of Chalcedony with opening in the centerburke museum, beechworth, geological, geological specimen -
The Beechworth Burke Museum
Geological specimen - Gold Telluride Ore
Gold usually is found as a native metal, but it also forms minerals with tellurium, sulphur, or selenium. The gold-bearing minerals that contain tellurium are called tellurides. Kalgoorlie, Western Australia contains greater than 1500 tonnes of gold.Seventy to seventy-five percent of the deposit occurs as native gold, but a further twenty percent appears as tellurides. What remains is in the form of 'invisible' gold. Extracting gold from telluride minerals, such as calaverite, which contains around forty-two percent gold, has produced approximately three hundred tonnes of gold. Prior to 1896, rocks containing tellurides were not recognised as rich gold ores, and were discarded.This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A hand-sized silvery to pyrite-yellow striated mineral containing tellurium and goldburke museum, beechworth, beechworth museum, geological, geological specimen, mineralogy, telluride, tellurite, gold-bearing, kalgoorlie, tellurium -
The Beechworth Burke Museum
Geological specimen - Rhodonite with Galena and Sphalerite
This specimen is from Broken Hill, NSW. Galena is a natural mineral form of lead sulphide and is often found associated with sphalerite, calcite, and fluorite. Galena is an important lead ore mineral, and, in some regions, it is also an important mineral associated with silver ore. Sphalerite is a sulphide mineral that is the main ore of zinc. Rhodonite is an uncommon mineral once used as an ore of manganese in India, however today the scarcity and fragility of the crystals mean it is primarily used as lapidary materials or mineral specimens. In 1883, Charles Rasp who was a boundary rider at the time, discovered what he thought were deposits of tin but were in fact samples of silver and lead. He and six others went on to set up the first mining company in Broken Hill (BHP). The ore body became the largest and richest of its kind in the world mining ore worth more than 42,000 pounds in its first year. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study. Galena contains lead and silver, Sphalerite contains zinc. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A hand-sized piece of Sphalerite and Galena with Rhodonite crystalsburke museum, beechworth, geological, geological specimen, galena, rhodonite, sphalerite, silver ore, manganese, lead sulphide, lead ore, zinc ore, lapidary, mineral specimen, broken hill, nsw -
The Beechworth Burke Museum
Geological specimen - Fossiliferous Mudstone, Unknown
This specimen was found in Cape Patterson, Vic. Cape Paterson is a cape and seaside village located near the town of Wonthaggi, 132 kilometres southeast of Melbourne, in the Bass Coast Shire of Gippsland, Victoria, Australia. These dark, fossiliferous Mudstones were deposited in slow-moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon-rich material would remain unoxidised during subsequent deposition & diagenesis. it has an imprint of a leaf in the rock itself, displaying the fossil of the plant. This specimen is unique due to the leaf impression within the stone itself. Imprint fossils are formed from an organism moving in some way, leaving behind a trace or track. These tracks are preserved when the clay/silt dries slowly and is covered by other sediment. Plants can also leave imprint fossils when they are covered by sediment. The leaf tissue degrades, leaving an imprint of where the leaf once was. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.These dark, fossiliferous Mudstones were deposited in slow moving water associated with sedimentary basins & continental shelves. They are rich in carbon which makes them almost black. This is typical of an anoxic, reducing environment such as deep water or stagnant conditions where carbon rich material would remain unoxidised during subsequent deposition & diagenesis. FOSSILIFEROUS MUDSTONE / Locality: Cape Patterson, Victoria | Descriptive catalogue / Pg 27 No 95 / "Grey Clay, / Cape Paterson with leaf impressions' / 15/4/21 C. William /mudstone, cape patterson, leaf imprint, fossilised leaf, fossiliferous mudstone -
The Beechworth Burke Museum
Geological specimen - Granodiorite, Unknown
This specimen was found in Harcourt, Victoria. Harcourt is a small historic gold rush town located in a valley at the foot of Mount Alexander (741 m) in the Central Highlands of Victoria. In recent times the goldrush origins of the town have been replaced by a district known for apples, cider and wine. The Traditional owners of Harcourt are The Dja Dja Wurrung people. Granodiorite is a coarse-grained intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. Granodiorite has greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase. This piece is of significance due to its provenance in Harcourt, Vic. Granodiorite is commonly produced in volcanic arcs, and in mountain buildings where it emplaces as large batholiths in mountain roots. Granodiorite is the plutonic equivalent of dacite. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Granodiorite is a coarse-grained intrusive igneous rock similar to granite, but containing more plagioclase feldspar than orthoclase feldspar. According to the QAPF diagram, granodiorite has a greater than 20% quartz by volume, and between 65% and 90% of the feldspar is plagioclase.GRANDIORITE. / Locality: / Harcourt, Victoria / Other label: Geological survey / R S / Loc Harcourt quarries [?] Alexander / 1/4 Sheet. | 4 | Granite /granodiorite, granite, burke museum, harcourt, coarse-grained, igneous, plagioclase feldspar, orthoclase feldspar, quartz, mount alexander, the dja dja wurrung people, the traditional owners, central highlands of victoria, gold rush -
The Beechworth Burke Museum
Geological specimen - Slate (Metamorphic), Unknown
This particular specimen was found in the Moorabool Slate quarries in Victoria. The Moorabool Slate quarries was established in the 1860’s by a company of Welshmen with a crew of six who purchased land by the riverside to mine for slate. Under the promise of adding to existing recourses the crew mined the slate which was used for paving and roofing. Slate is a fine-grained, low-grade metamorphic rock that is formed by the transformation of mudstone, shale or sometimes volcanic ash under low pressure and temperatures. It dark colour is due to carbonaceous material or to finely divided iron sulphide. It is believed that Evan Rowlands and Theophilus Williams of Ballarat were the first to discover the slate veins. Slate is a one of the most common natural stones in general use. Being used as paving, flooring, roofing and more. However, its history of being mined in Australia is not common as it is considered that the best places to mine slate is Spain and parts of the United Kingdom. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A somewhat rectangular foliated metamorphic rock composed of quartz, sericite and minerals from the chlorite group that make up the compounds of slate. The rock is dark grey almost black.Geological survey / R S / Loc Moorabool /Slate quarries / 1/4 sheet | 78 | Roofing Slate /burke museum, beechworth, geological, slate, metamorphic, slate (metamorphic), geological specimen, slate specimen, indigo shire -
The Beechworth Burke Museum
Geological specimen - Spotted Slate, Unknown
This specimen was recovered from Sedgwick, VIC. Spotted slate is a fine-grained porphyroblastic metamorphic rock with a number of compounds including muscovite, quartz, graphite with cordierite poikiloblasts and more. The cordierite poikiloblasts are rounded crystals that size up to 2.5 mm. the growth of these crystals is in response to metamorphism of low to medium intensity. The town Sedgwick was named after British geologist Adam Sedgwick This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.A solid rectangular hand-sized spotted slate specimen in a shade of light grey with darker flecks throughout Spotted Slate / Locality: Sedgwick Victoria | This is an early specimen / from the Quarter sheet / map. See sample 62 / page 18. Described as 'Spotted Slate' but these / days we would call it spotted hornfels / C. William 15/4/21 slate, spotted slate, victoria, beechworth, burke museum, geological specimen, mineralogy, sedgwick, sedgwick victoria, spotted slate specimen -
The Beechworth Burke Museum
Geological specimen - Greenstone / Gabbro, Unknown
This specimen was recovered from Ceres West of Geelong, Victoria. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Greenstone is often formed through metamorphsis along a convergent plate boundary. In the rock cycle (the series of processes that creates the various types of rocks) there are identified three different types of rocks, which are the sedimentary, the igneous and the metamorphic. Metamorphic rocks started out as sedimentary, igneous or earlier metamorphic rocks but changed from their original condition under the effect of high heat, high pressure or hot, mineral-rich fluid. However, if pressure or heat is too high, then the rock will melt, resulting in the formation of an igneous rock. The name used to describe these types of rocks reflects this specific inherent trait of change, since the word “metamorphic” derives from the Greek word “metamorphosis”, meaning “change of form or structure”. Metamorphic rocks form in the Earth`s crust but can be also found on the surface, due to elevation of the Earth`s surface. They are divided into two categories: the foliated metamorphic and the non-foliated metamorphic rocks. Gabbro is a highly useful mineral that is often polished to create cemetery markers and kitchen benches. It is notable for its qualities of durability, being able to withstand extreme elements and wear. Whilst not rare, Gabbro is of great utility and has been highly desirable for its qualities. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Greenstone is a solid hand-sized metamorphic mineral of a green colour. Greenstone is the name for any metamorphosed basic igneous rock (in the case of this specimen, Gabbro) that gains its greenish colour to the presence of the minerals chlorite, actinolite, or epidote, hence the term 'green' and 'stone'. Gabbro is a medium to coarse grained rocks that consist primarily of plagioclase feldspar and pyroxene. Greenstone is often formed through metamorphsis along a convergent plate boundary. Gabbro forms due to cooling and crystallization of magma underneath Earth's surface. Greenstone/Gabbro/from Ceres west/of Geelong. Has old Geological Survey label/and probably collected by/Richard Daintree in 1861/C.Willam 15/4/21/ Other label: 62 /greenstone, metamorphosed, igneous rock, gabbro, chlorite, actinolite, epidote, metamorphsis, rock cycle, various types of rocks, sedimentary, high heat, high pressure, mineral-rich fluid, metamorphosis, foliated metamorphic, non-foliated metamorphic, convergent plate boundary, greenish colour, minerals -
The Beechworth Burke Museum
Geological specimen - Slate with Iron pyrites
This specimen was recovered from Moonambel, Donkey Hill, Victoria. Established in the early 1860's, Moonambel is a small town in the Pyrenees region of the Australian state of Victoria. In the 1850s the location of Moonambel was part of the ‘Mountain Creek’ pastoral run, but in 1860 reports began to appear of a gold-rush at McKinnon’s ‘Mountain Creek’ station. By 1861, a township had developed on the diggings site, and on 21 October 1861 the “municipal district of Moonambel, on Mountain Creek” was proclaimed. The name 'Moonambel' is believed to be an aboriginal word meaning 'hollow in the hills'. Slate is a stone with a fine grain that is noted for its persistent strength and ability to naturally split into slabs. It forms under low temperatures and is most often created from clay. Pyrite is a crystallising compound that occurs naturally in grey and blue-black slate that is colloquially referred to as slate-rust as it resembles regular rust. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Pyrite is iron sulphide (also known as “fool's gold”) which is commonly found in slates.Existing label: 53 /moonambel, slate, pyrite, burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, victoria -
The Beechworth Burke Museum
Geological specimen - Pyrite
This specimen was recovered from Adelong, NSW. The initial discovery of gold at Adelong by a Mr Williams took place in 1857. Much of the area is underlain by granitic rocks, while at Adelong itself a prominent norite intrusive body occurs. To the west of Adelong is a belt of intermediate to mafic igneous rocks and sediments which extends from Batlow in the south to at least as far north as the Snowy Mountains Highway. Around 26 tonnes of gold was found at the Adelong goldfield from its discovery in the 1850s until the last miners left in the 1940s. Pyrite has the formula of FeS2 and forms as an isometric (cube) form. It is a common occurring material and is often mistaken for gold, now colloquially known as ‘fool’s gold’. Pyrite that has strongly crystallised is considered stable, but the mineral has the potential to oxidise and decay. This specimen is part of a larger collection of geological and mineral specimens collected from around Australia (and some parts of the world) and donated to the Burke Museum between 1868-1880. A large percentage of these specimens were collected in Victoria as part of the Geological Survey of Victoria that begun in 1852 (in response to the Gold Rush) to study and map the geology of Victoria. Collecting geological specimens was an important part of mapping and understanding the scientific makeup of the earth. Many of these specimens were sent to research and collecting organisations across Australia, including the Burke Museum, to educate and encourage further study.Pyrite is iron sulphide (also known as “fool's gold”) which is commonly found in slates.Existing Label: 104 /burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, pyrite, adelong