Transverse section of the Virginia mine on the Garden Gully line of Reef at Eaglehawk, being Plate V of Bulletin No. 47 from the Geological Survey Office at BendigoGeological Survey Office Bendigogold, goldfields, virginia mine, gold mines, garden gully line of reef, virginia mine , eaglehawk

Geological Survey of Stawell 1875/76 by Norman Taylor, Geological SurveyorYellow Card Front and Rear Cover with B/W Picture of mining scene. with black Plastic spineGeological Survey of Victoria No.3 Geological Survey of Stawell Norman Taylor 1875/76stawell mining

In the early 1990s the KVHS applied for a grant to create the Mt Beauty Heritage Centre / Discovery Centre. This involved employing consultants and further research.This collection includes a lot of detail of the Kiewa Valley area.1. Bogong - The Alpine Discovery Centre 2. Heritage Centre - black folder 3. Heritage Centre - manila folder 4. High Country Heritage Centre - 1991 - green spiral folder 5. Six Heritage Centre - Matt Viney & Associates - white spiral folders 6. Landscape Consultants - Susan Campbell & son - red spiral folder 7. Plant List - Upper Kiewa Valley Water Supply Catchment 8. Geological Survey of Vic., Plates, Bulletin No. 44 - in battered paper 'bag' with front cover list of contents - 15 plates 9. Geological Survey - A3 photo copies of pages 106-117 10. Geological Survey of Vic. - Report of Progress No VII 1884 - bound book 11. Geological Survey of Vic. Bulletin 56 - includes nth east Vic. 1958 - bound book with green cloth spine 12. Department of Mines Report Vic. 1906 - booklet held with two staples 13. Royal Society of Vic book - The Geology of the Kiewa Area 1961 14. Miscellaneous papers - Geological Survey, Reports of Fossil Specimens and maps of local area 15. Gold - Appendix K and Appendix 111, Part C - photocopied pages from Vic Mining Registrars Report 1888 - manila foldermt beauty heritage centre, mt beauty discovery centre, geological surveys

Drawing with Longitudinal Section through the Saddle Reefs along portion of Hustler's Line of Reefs, Bendigo. Map shows the depth of the mines, reef numbers and Datum 700 ft above sea level. North and South is also noted on the map. Map signed by H. S, Whitelaw, Underground Survey Office, Bendigo, September 1913. Bulletin No 33, Plate No XXXIV. Bendigo Creek, Ironbark Creek and Long Gully are also noted. Mines are: Fortuna Hustlers, Hustler's Royal Reserve No 2 Main Shaft, Hustler's Royal Reserve No 2 Park Shaft, Royal Hustler's, Imperial Hustler's, Extended Hustler's Freehold, Great Extended Hustler's Tribute (Pups), Old Shaft, Great Extended Hustler's Reef No 2, Great Extended Hustler's Main Shaft, Old Shaft, Hustler's Reef, Hustler's Reef No 1, Comet, K. K., United Hustler's & Redan, Old Shaft and Hustler's Consols. Has Geological Survey of Victoria Crest and underneath is: H. Herman, Director, W. Dickson, Secretary for Mines, The Hon. J Drysdale Brown M L C. Minister of Mines.Geological Survey of Victoria Crestmining, hustler's reef maps, hustlers line of reefs, bendigo creek, royal hustler's, imperial hustler's, extended hustler's freehold, great extended hustler's tribute (pups), great extended hustler's reef no 2, great extended hustler's main shaft, hustler's reef, hustler's reef no 1, united hustler's & redan, old shaft and hustler's consols.h s whitelaw, underground survey office bendigo september 1913

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

Longitudinal section of the Comet Mine on the Hustler's Line of Reef Bulletin No 33, Plate No XXVI signed by H. S. Whitelaw, Underground Survey Office Bendigo, September 1913. Map shows datum lines, depths of levels, approximate boundaries and references to other plans. Note - Plates 4, 8, 13, 20, 26 and 31 form a Longitudinal Section from Fortuna Hustler's to Hustler's Consols Mine. Geological Survey of Victoriamining, parish map, hustler's line of reef, longitudinal section of comet mine bulletin no 33 plate no xxvi, h s whitelaw

Transverse section of the Comet Mine on the Hustler's Line of Reef Bulletin No 33, Plate No XXV signed by H. A. Whitdon, Underground Survey Office Bendigo September,1913. Map shows depth of the different levels, the type of stone and shaft about 2020 deep. A number of smaller drawings on the side. Reference explaining the different types of stone, etc. Geological Survey of Victoriamining, hustler's line of reefs, transverse section of comet mine bulletin no 33 plate no xxv, lightning hill line of reef

Plan of the Comet Mine on the Hustler's Line of Reefs Bulletin No 33, Plate No XXIV signed by H S Whitelaw, Underground Survey Office Bendigo, September 1913. Upper and Lower Levels and approximate boundaries shown. Depths shown.Geological Survey of Victoriamining, parish map, hustler's line of reefs, comet mine plan bulletin no 33 plate no xxiv

Plan of the Comet Mine on the Hustler's Line of Reefs Bulletin No 33, Plate No XXIII. Map shows depths, Lightning Hill Anticline, Hustler's Anticline and approximate Lease Boundary. Signed by H. S. Whitelaw, Underground Survey Office Bendigo, September 1913. United Hustler's & Redan Co and Hustler's Reef Co also named on map. Geological Survey of Victoriamining, hustler's line of reefs, comet line plan belletin no 33 plate no xxiii, lightning hill anticline, hustler's anticline, united hustler's & redan co, hustler's reef co, h s whitelaw

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

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

Agate occurs when amygdales (gas pockets) form in the upper levels of basaltic lava flows. If these pockets or bubbles are iniltrated by water bearing silica in solution, the fluid dries and hardens in layers, forming round or egg shaped nodules or geodes within the rocky matrix. Agate is formed of a silica mineral chalcedony similar to quartz. Although relatively common and semi-precious, agate has been prized since at least 1450 BC - an intricately carved agate seal was found in the 2015 excavation of a grave belonging to a Mycenaeum priest or warrior near Pylos in Greece. Agate is also used in jewellery and other decorative or ritual purposes due to its often striking appearance. Quartz is found all over Australia, including Beechworth in Victoria. It is formed in deep-seated igneous rocks and crystallized through hot aqueous solutions. It can have two forms; Microcrystalline quartz or Crystalline quartz. Microcrystalline quartz is a fine grain quartz where crystalline quartz is often a large crystal. The colour of quartz can vary. These specimens were collected in Victoria in the vicinity of the Burke Museum. Victoria and other regions of Australia were surveyed for sites of potential mineral wealth throughout the 19th Century. The identification of sites containing valuable commodities such as gold, iron ore and gemstones in a locality had the potential to shape the development and history of communities and industries in the area. The discovery of gold in Victoria, for instance, had a significant influence on the development of the area now known as 'the goldfields', including Beechworth; the city of Melbourne and Victoria as a whole.The specimens are significant as examples of surveying activity undertaken to assess and direct the development of the mineral resource industries in Victoria and Australia, as well as the movement to expand human knowledge of earth sciences such as mineralogy and geology in the nineteenth century.Geological specimens of Agate and Quartz respectively; the fist-sized piece of Agate has peach/coral colouring with grey concentric patterning and the smaller piece of quartz is a uniform yellow/orange shade. Existing label: Local pebbles / (agate and / quartz / (yellowish) / egg-shaped). / BB geological specimen, geology, geology collection, burke museum, beechworth, agate, quartz, north-east victoria, indigo shire, geological surveys

Map: County of Gladstone, Geological survey of Victoria. Geological mapmap, gladstone, geological, county of gladstone, geological map

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