Colour photograph of chimneys at Basalt.basalt, ruins, chimneys

Colour photograph of ruins in the landscape near Basalt. basalt, ruin, chimney

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

This particular geological specimen was found in Mount Franklin or Lalgambook in Djadjawurrung, located between Daylesford and Newstead, approximately ninety minutes drive from Melbourne. The mountain is an example of a breached scoria cone (a steep conical hill of loose pyroclastic fragments) which was created by a volcanic eruption about 470,000 years ago, a date which may indicate the age of this geological specimen. The volcanic eruptions of Mount Franklin were most likely witnessed by members of the Dja Dja Wurrung Aboriginal tribe, who referred to this country as the 'smoking grounds'. Mount Franklin and the surrounding area appears to have been a place of considerable religious significance to Aboriginal people, there is evidence which indicates that frequent large ceremonial gatherings took place in the area. Basalt is the most common rock on Earth’s surface, more than 90% of all volcanic rock on Earth is basalt. Basalt is an aphanitic extrusive igneous rock formed from the rapid cooling of low-viscosity lava exposed at or very near the surface of a rocky planet or moon. Specimens are black in colour and weather to dark green or brown. Basalt is rich in iron and magnesium and is mainly composed of olivine, pyroxene, and plagioclase. Olivine is the name of a group of rock-forming silicate minerals with compositions ranging between Mg2SiO4 and Fe2SiO4. Unlike other minerals, Olivine has a very high crystallisation temperature which makes it the first of the minerals to crystallise from magma. As magma cools, the crystals begin to form and settle on the bottom of the lava and form basalts that are abnormally enriched in olivine in the lower part of lava flows. According to H. M. King (on geology.com) "Olivine is thought to be an important mineral in Earth's mantle. Its presence as a mantle mineral has been inferred by a change in the behaviour of seismic waves as they cross the boundary between Earth's crust and mantle". Lava from Mount Franklin and other volcanoes in the area filled valleys and buried the gold bearing streams that became the renowned ‘deep leads’ of the gold mining era. In 1852, as part of the Victorian gold rush, gold was discovered in the immediate area, this gold was created by lava flows during the Newer Volcanic period, which were mined intensively during the nineteenth century. Around 1865 the presence of a deep lead in Mount Franklin was established. Deep lead mining was initially unsuccessful, and it was not until the late 1870s that the Franklinford Gold Mining Company mined at Mount Franklin on a significant scale. A few years later the Mount Franklin Estate Gold Mining Company also struck gold, followed by the Shakespeare and Great Western companies in the mid-1880s. By the late 1880s, however, deep lead mining had ceased in the area. Soon after gold was discovered in 1851, Victoria’s Governor La Trobe wrote to the Colonial Office in London, urging ‘the propriety of selecting and appointing as Mineral Surveyor for this Colony a gentleman possessed of the requisite qualifications and acquaintance with geological science and phenomena’. Alfred Selwyn was appointed geological surveyor in Australia in 1852 which began the Geological Survey of Victoria. In 1853-69 the Geological Survey issued under Selwyn's direction sixty-one geological maps and numerous reports; they were of such high standard that a writer in the Quarterly Journal of the Geological Society of London bracketed the survey with that of the United States of America as the best in the world. During his years spent in Australia, Selwyn collected numerous significant geological specimens, examples of which are held in collections such as the Burke Museum.This geological specimen is an example of basalt and olivine which shows the volcanic lava activity and geographical specific nature of Mt Franklin as a significant volcanic site. According to Agriculture Victoria 'The crater is one of the deepest in the Central Highlands area. It is a major megacryst site with some of the largest known Victorian examples of megacrysts of augite and an orthoclase. The small parasitic mound of Lady Franklin on the western flanks adds to the geological interest of the site'. This specimen also highlights the locality as a significant place for both indigenous activity and Victorian gold rush era mining practices. 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.An angular, solid hand-sized piece of grey volcanic Basalt with green/brown Olivine phenocrysts along one flat edge.Olivine in basalt / - label is probably / correct. / C. Willman / 15/4/21burke museum, beechworth, indigo shire, beechworth museum, geological, geological specimen, mineralogy, basalt, igneous rock, igneous-volcanic, volcanic geology, volcanic, olivine, olivine specimen, basaltoid

Janefield Precinct: Basalt remains. The remains of this site are between Greensborough and Janefield. A RAAF Hygiene Training Camp was located on the Plenty River, just south of the Janefield community. It was in use from 1944 to 1946. The Camp was constructed from salvaged materials. Instruction included building and maintenance of grease traps, latrines, elementary plumbing and carpentry.Early remains of a WW2 training camp Digital colour photograph.

Janefield Precinct: Basalt rubble. The remains of this site are between Greensborough and Janefield. A RAAF Hygiene Training Camp was located on the Plenty River, just south of the Janefield community. It was in use from 1944 to 1946. The Camp was constructed from salvaged materials. Instruction included building and maintenance of grease traps, latrines, elementary plumbing and carpentry.Early remains of a WW2 training camp Digital colour photograph.

Janefield Precinct: Basalt quarry remnants. The remains of this site are between Greensborough and Janefield. A RAAF Hygiene Training Camp was located on the Plenty River, just south of the Janefield community. It was in use from 1944 to 1946. The Camp was constructed from salvaged materials. Instruction included building and maintenance of grease traps, latrines, elementary plumbing and carpentry.Early remains of a WW2 training camp Digital colour photograph.

Janefield Precinct: View of edge of basalt flow. The remains of this site are between Greensborough and Janefield. A RAAF Hygiene Training Camp was located on the Plenty River, just south of the Janefield community. It was in use from 1944 to 1946. The Camp was constructed from salvaged materials. Instruction included building and maintenance of grease traps, latrines, elementary plumbing and carpentry.Early remains of a WW2 training camp Digital colour photograph.janefield

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

MEYER COLLECTION - FALLS CREEK PHOTOS In 1947 a determined group of like-minded State Electricity Commission (SEC) staff including Ray Meyer, the chief surveyor of the Kiewa Hydro-Electric Scheme, had a common interest that revolved around the skiing potential of the snow-covered high plains which included what is now the resort of Falls Creek. The six SEC employees, Toni St Elmo, Ray Meyer, Jack Minogue, Lloyd Dunn, Adrian Ruffenacht and Dave Gibson (together with their families) banded together to secretly build a 'hut' that was the first ski lodge at Falls Creek. Using a road built in 1930s to gain access to Falls Creek, their hut project was carried out in secret as efforts by other skiers were blocked by H.H.C. Williams – the engineer in charge of the Hydro Scheme. In 1946 Ray Meyer made a trip to the Lands Office in Melbourne. He came away with a 99-year lease on three acres that was ideally suited for a hut designed by Lloyd Dunn. Adrian Ruffenacht (Design Engineer for the KHS) had suggested where the group should build because of easy access to a spring for water. Much of the building material required was scavenged from derelict huts on the high plains. Due to the need for secrecy, the determined group worked on the hut in the evenings and weekends to avoid detection. During the building period the group had met at Echidna Rock (now known as Eagle Rock) where Skippy St Elmo announced, "This is my favourite ‘Skyline’.” And so the first lodge in the area at Falls Creek Ski Resort came into existence. With the development of the International Poma in the 1970s, the Skyline Lodge, which was sited between the ski-lift’s pole one and pole two, was demolished. However, the legacy of Ray Meyer, Toni St Elmo, Jack Minogue, Lloyd Dunn, Adrian Ruffenacht and Dave Gibson and Skyline lives on in the vibrant atmosphere of Falls Creek Resort. The MEYER COLLECTION documents developments on the Kiewa Hydro Scheme and their life at Falls Creek from the mid 1930s to 1960s.These images are significant because they depict aspects of the life of a pioneering family of Falls Creek and the founders of "Skyline", the first lodge at Falls Creek.Two black and white images of John Meyer skiing near Wilkie and Basalt Hill, Bogong High Plains. Wilkinson’s Hut (Wilkie) was built for the SEC in the summer of 1932-3 to accommodate the snow research program manager. The cottage was sited next to a hydro-meteorological station, set on stilts above the snow. It was not a refuge hut but a permanent residence for all of the year. The work carried out there included operation of a meteorological station at the cottage, measuring the snow depth and density along two pole lines, and operating stream gauging stations in the area. The engineers stationed there included Adrian Rufenacht (1934-6), and Norwegian Martin Romuld (1936-42) Romuld was a champion skier, constructing a ski-jump and a grass tennis court near the hut during his residency. Adrian was one of the founders of 'Skyline". The hut was sold in 1948 to the Victorian Ski Club and renamed Wilkinson Lodge. Robert Wood Wilkinson, best known as 'Wilkie, was the 'Father figure' of Victorian skiing. Robert Wood Wilkinson died on May 22, 1939. The hut was resold some 12 years later to the Melbourne Bushwalkers club. In 1983, the National Parks Service described the building as an old SEC hut which had been purchased and, afterwards, maintained and occupied solely by the Melbourne Bushwalking Club. Wilkie Hut survived the 2003 bushfires but burnt down one year later (January 2004) in a cooking accident.falls creek, ray meyer, skyline

35mm colour positive transparency Mount - Black and Whitebasalt manna gum, eltham-yarra glen road, kangaroo ground, significant tree, roads, infrastructure

35mm colour positive transparency Mount - Black and Whitebasalt manna gum, eltham-yarra glen road, kangaroo ground, significant tree, roads, infrastructure

35mm colour positive transparency Mount - Black and Whitebasalt manna gum, eltham-yarra glen road, kangaroo ground, significant tree, roads, infrastructure

35mm colour positive transparency (1 of 4) Mount - Kodak EktachromeProduction Code "MAR M"significant tree, basalt manna gum, eltham-yarra glen road, kangaroo ground

Like Purple Plain, Mernda and Mernda Heat Haze this painting was a further development from aspects of the Basalt Plains series of the 1990's as seen in Mernda Plains Landscape. This picture has a greater minimalist quality about it, having been painted in the studio during a particularly wet spring when some of the surrounding flats were indented by channels of water. Greens are not a colour harmony I work with often, but here help convey the essence of the seasonal landscape. A much more formal structure has been emphasized in this picture in which atmospheric space has been almost negated in favour of a much shallower field of colour and two dimensional surface rhythm, an actual effect one can sometimes see under certain conditions of nature, particularly in a flat country. I have always had some respect for one or two of the better colour field painters of America in the 1950's and 1960's who actually untilzed expressive broad bands of colour harmonies in their work, but didn't classify them as landscape paintings. My own feelings on the subject are to avoid the clinical precision that such an approach can bring, and thus indicate some actual reference to landscape in a work, a horizon, however subtle, or marks indicating actual forms that give some scale to the work. I suppose the idea first occurred to me when I saw J. M. W. Turner's wonderful painting, Evening Star, in the National Gallery in London many years ago. In this work a few bands of mysterious colour and exquisite harmonies with one or two references to figure, sand, sea and sky, transmogrify everything into a magical unity. It serves as a revelatory example of how all art is dependent on abstract qualities and how great artists like Turner are able to conceal those qualities without lapsing into a forced mannerism.Part of the John and Gillian Borrack Federation Bequest, donated to the City of Whittlesea in December 2001 by Gillian and John BorrackJohn Borrack '90mernda

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

largely unknown; ultimately originated as part of series of basaltic volcanic events across victoriaClearly a fragment of a river rock- one surface is smooth and curved the others planar. Mineralogy is basalt-"bluestone"-with white veins of secondary quartz minralisation

The main gate to the former Gaol is a monumental work. The arch keystone facing Lydiard Street is beautifully executed. The gates and the iron lacework over the top are distinctive.The arch under the flyover is also distinctive; the basalt keystone appears to have been cut from one single block of stone. Most of the gaol has been demolished to allow the School of Mines Ballarat to expand onto the site. The remaining structures at the site include the main gate, warden's residence and governor's residence. These buildings are now used by Federation University.The main gate to the former Gaol is a monumental work. The arch keystone facing Lydiard Street is beautifully executed. The gates and the iron lacework over the top are distinctive.The arch under the flyover is also distinctive; the basalt keystone appears to have been cut from one single block of stone. gate, gaol, arch keystone, lydiard street, iron lacework, flyover, stone, basalt, ballarat school of minesfederation university, warden's residence, governor's residence

The main gate to the former Gaol is a monumental work. The arch keystone facing Lydiard Street is beautifully executed. The gates and the iron lacework over the top are distinctive.The arch under the flyover is also distinctive; the basalt keystone appears to have been cut from one single block of stone. Most of the gaol has been demolished to allow the School of Mines Ballarat to expand onto the site. The remaining structures at the site include the main gate, warden's residence and governor's residence. These buildings are now used by Federation University.The main gate to the former Gaol is a monumental work. The arch keystone facing Lydiard Street is beautifully executed. The gates and the iron lacework over the top are distinctive.The arch under the flyover is also distinctive; the basalt keystone appears to have been cut from one single block of stone. gate, gaol, arch keystone, lydiard street, iron lacework, flyover, stone, basalt, warden's residence, governor's residence, ballarat school of mines, federation university, former ballarat gaol

Murrup Laarr translates as 'Ancestral Stones' in Wadawurrung. This artwork by Dr Deanne Gilson is located in the North Gardens Indigenous Sculpture Park. The park is a significant project for the City of Ballarat and features works by Aboriginal and Torres Strait Islander artists, celebrating the richness and diversity of culture and telling important cultural stories. Dr Deanne Gilson is a Wadawarrung Traditional Custodian and established artist. She installed the first artwork commissioned by the City of Ballarat for the Sculpture Park in early 2019. Murrup Laarr is a contemporary artwork consisting of a traditionally-built stone hut in the middle of a circle of basalt standing stones, marked with ceramic plates reflecting the stories and symbols of dreaming, memory, ceremony.The artwork is of aesthetic and cultural, social and spiritual significance to the people of Ballarat and to Wadawurrung peopleA traditional hut made from river stone and stacked rocks, with the hut surrounded by large basalt rocks with plaques featuring unique designs on stoneware plates imbedded into them. Murrup Laarr (Ancestral Stones), 2019 / By Deanne Gilson / Wadawurrung people have always used stones to mark places of ceremony and important business. The stones are the holders of memory and knowledge, Country and Spirit. They mark the cosmos and seasons. They follow the sun, marking the summer and winter solstice, important dates for planting and harvesting and telling stories of past, present and future. / The stones are alive and still present. Murrup Laar has been created using local basalt stones to tell Wadawurrung stories of dreaming, memory and ceremony. / “Creating Murrup Laarr (Ancestral Stones) at this time has placed Aboriginal people and practices back on Country and created a place to tell our stories. I am very honoured to have had this opportunity. An Aboriginal stone circle existed in Ballarat pre-colonisation; by putting back what was lost throughout colonisation I pay homage to my ancestors, past, present and emerging”/ – Deanne Gilson, March 2019 murrup laarr, wadawurrung

One of a collection of over 400 photographs in an album commenced in 1960 and presented to the Phillip Island & Westernport Historical Society by the Shire of Phillip IslandPhotograph of inter basaltic formations on basalt shore platform eastern end of Smith's Beachlocal history, photography, rock formations, black & white photograph, coastline, smith's beach, dr g baker, john jenner, bryant west

One of a collection of over 400 photographs in an album commenced in 1960 and presented to the Phillip Island & Westernport Historical Society by the Shire of Phillip IslandPhotograph of dense basalt headland near Smith's Beachlocal history, photography, basalt headland, black & white photograph, coastline, smith's beach, dr a b edwards, john jenner, bryant west

The obelisk is not on the original site. Coloured photograph of a basalt obelisk to mark the discovery of gold at Ballarat.ballarat gold discovery obelisk

One of a collection of over 400 photographs in an album commenced in 1960 and presented to the Phillip Island & Westernport Historical Society by the Shire of Phillip IslandPhotograph of the basalt cliffs and shore platform near Pyramid Rocklocal history, photography, cliffs and shoreline pyramid rock, black & white photograph, coastline, rock formations, pyramid rock, dr a b edwards, john jenner, bryant west

One of a collection of over 400 photographs in an album commenced in 1960 and presented to the Phillip Island & Westernport Historical Society by the Shire of Phillip IslandPhotograph of the basalt Jetty and geological feature near Surf Beachlocal history, photography, basalt jetty, surf beach, black & white photograph, coastline, geology, rock formations, john jenner, bryant west

Local Indigenous PlantWatercolour paintings - Indigenous Plants of the Basalt Plains. Part of series of 14 commissioned paintings.