Trove : Leader, Saturday April 9th, 1892, page 24, 'Suicide in St. Kilda', mentions chemist Ernest Daintree in the report as selling the laudanum used in the suicide. Victorian Government Gazette, no.67, Friday May 4th, 1894, page 1841. : 'Trademarks, CLASS 47. 3833. A liquid detergent for general domestic cleaning purposes. Ernest Daintree of High-street, St. Kilda, Victoria, wholesale and retail druggist. 30 April 1894. (As a distinctive label.)' Victorian Government Gazettes, Pharmaceutical Registers, Ernest Daintree is listed at the address 102 High Street St Kilda from 1898 until at 523 Malvern Road, Toorak in 1903. He was first entered on the Pharmaceutical Register in Victoria on 11 April 1888 and his qualification was from Gt. Britain, Major Exam, No.2138.Tall rectangular clear glass bottle with angled corners, for stopper seal. Text embossed on one side & logo on base.Embossed on side 'E. DAINTREE ST KILDA'. On base : ' M' inside cartouche shaped impression.druggist, wholesale., druggist, retail, ernest daintree

When Richard Daintree rejoined the Victorian Geological Survey as a field surveyor in January 1859, he pioneered the use of photography in field-work. The glass plates attributed to him by the State Library of Victoria show four images of the mines in Clunes, Victoria, Australia in the 1860'sBlack and white reproduction of Port Phillip Colonial & Gold Mining Co., Clunes, Victoria, Australia in a light wood timber frameOn Reverse: Handwritten in pencil Port Phillip Co. 1860's Nettleton Photography glass plate Latrobe Libraryport phillip and colonial gold mining co., richard daintree

A coloured geological sketch map of the Werribee Gorge, Bacchus Marsh, Rowlesy, Darley, Parwan. The scale is 1 mile to 1 inchwerribee gorge, bacchus marsh, darley, parwan, w.e. bennett, bennett, r.a.f. murray, c.c. brittlebank, rowsley

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

A3 and A4 sized photocopies showing map section of land title showing streets, easements and allotment numbers, some with handwritten names and pricing notations circa mid 1950s.Map includes Valley Road, Granard Avenue, Park Road, Arundel Avenue, Hylton Avenue, Aviemore Avenue, Bowmore Avenue, Hopetoun Road, Colin Avenue, Daintree Avenue, Brucedale Crescent, Feversham Avenue, Ennismore Crescent, Iona Grove, Elgin Crescent and Gosford Crescent, Park Orchards, Victoria.

Large linen backed map of the Park Orchards subdivision for private sale of residential sites and recreation club, highlighting local facilities, services and layout of the estate. Surveyors - Tuxen & Miller, 34 Queen Street, Melbourne. Agents - Wm Addey & Co., Pty Ltd., National Mutual Buildings, 395 Collins Street, Melbourne, Phone F3906. Terms £5 deposit balance monthly installments of £1 with the residue at the end of five years. Subdivision includes Alva Avenue, Arundel Road, Aviemore Avenue, Berringa Road, Bowmore Avenue, Brucedale Crescent, Brympton Avenue, Camber Avenue, Cawdor Avenue, Colin Avenue, Corriedale Crescent, Craithie Avenue, Daintree Avenue, Dalry Avenue, Dirlton Crescent, Drayton Crescent, Elgin Crescent, Enfield Avenue, Ennismore Crescent, Euston Avenue, Feversham Avenue, Frogmore Crescent, Gosford Crescent, Granard Avenue, Hopetoun Road, Hylton Avenue (later Knees Road), Jura Avenue, Park Road.

Date not confirmed, a farm in the Beechworth Warner property with a farmer overlooking calves, poultry and timber. This photograph depicts the farming and agriculture industry in Beechworth. The property, known as Daintree Stud or the Warner property, was formed a part of the town on Beechworth, Victoria. Beechworth became famous in the 19th century from a short- lived gold-rush. The town grew to the extent of building a hospital and mental hospital, court house, hotels, convent, and prison. During this time, the industrial growth of Beechworth was significant, seeing a rise in practices including tanning, cobbling, blacksmithing, and the selling of livestock. This photograph perhaps reveals a small degree of insight into the livestock business.Black and white rectangular photograph on matte photographic paper, unmountedReverse: 5896/ BMM 8093-1farm, agriculture, farming and agriculture, beechworth, beechworth farm, industry

Ventifacts are sand-blasted rocks that are typically faceted and often display parallel grooves carved by wind-blown sand. They are useful indicators of wind direction and strength in environments such as deserts, mountains, and coastal areas because they are usually not hidden by later sediment, soil or vegetation cover. In Antarctica ventifaction is strongly related to the composition or type of rock. Ventifacts are important because they provide evidence for abraders such as sand, dust or snow and ice crystals, and offer a unique understanding of past wind processes that are effective in the reconstruction of past wind flow conditions and can provides clues to weather and climate changes in the past. Interestingly ventifacts have also been found on the surface of Mars. They were a threat to the NASA rover due to the sharp angles of the facets, created by the Martian wind over the course of millions of years. These Martian ventifacts act like weathervanes for past wind and weather patterns on the red planet in a similar manner to those found on earth.The Geological Survey of Victoria was instigated in response to the Victorian Gold Rush which began around 1851 in the Beechworth, Castlemaine, Daylesford, Bendigo and Ballarat areas. The survey was conducted by Alfred Richard Cecil Selwyn from his arrival in December 1852 until his resignation in 1869and during this time he trained many notable geologists, e.g. Aplin, Wilkinson, Daintree, who went on to other State survey senior positions. This specimen was among those donated to the Burke Museum in 1868.A hand-sized solid mineral specimen in shades of dark and light browns with light lines visible in all configurations and a groove on configuration 2.light lines visible in all configurations and a groove on configuration 2burke museum, beechworth, geological, geological specimen, ventifact, antarctic region, antarctic, alfred richard cecil selwyn, alfred selwyn, wind direction, wind strength, abraders, wind flow, climate change, reconstruction of wind flow conditions, weather change, mars