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Looking inside the Earth
https://australian.museum/learn/minerals/shaping-earth/looking-inside-the-earth/The internal structure of the Earth consists of three main parts, the crust, mantle and core. The division between the crust and the mantle is called the Moho.
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Metamorphic processes
https://australian.museum/learn/minerals/shaping-earth/metamorphic-processes/Most minerals are only stable at particular temperatures and pressures, so changes in these result in the formation of new minerals.
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Jenolan Caves Minerals
https://australian.museum/learn/minerals/shaping-earth/mineralogy-collection-jenolan-caves-minerals/The Jenolan Caves are one of the premier tourist attractions of New South Wales. Nine caves are regularly shown to visitors, but several hundred of various sizes are known from the area.
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The Sydney Basin
https://australian.museum/learn/minerals/shaping-earth/the-sydney-basin/The Sydney Basin is a major structural basin containing a thick Permian-Triassic (290 Ma - 200 Ma (million years old)) sedimentary sequence that is part of the much larger Sydney-Gunnedah-Bowen Basin.
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What are minerals?
https://australian.museum/learn/minerals/what-are-minerals/Minerals are the building blocks of our planet. Discover what they reveal about the history of Earth and our solar system and what makes them so essential to our existence.
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Gemstones
https://australian.museum/learn/minerals/gemstones/Gemstones are prized for their beautiful colours and patterns and are used in a range of applications including jewellery, decorative items and as important features of mineral collections.
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The Molong Meteorite – a visitor from outer space.
https://australian.museum/learn/news/blog/the-molong-meteorite-a-visitor-from-outer-space/A story about a meteorite from the central west of NSW that has been part of the Australian Museum collection for 83 years.
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Water and sedimentary transport
https://australian.museum/learn/minerals/shaping-earth/water-and-sedimentary-processes/Water plays a vital role in most sedimentary processes. Pure water itself has little effect on rocks. It is the dissolved gases in water, particularly carbon dioxide, that cause the chemical decay of minerals and mineral dissolution.
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Sedimentary processes
https://australian.museum/learn/minerals/shaping-earth/sedimentary-processes/Sediments are formed by the breakdown (both physical and chemical) of pre-existing rocks, which may be of igneous, metamorphic or sedimentary origin.
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Oliver Chalmers – Curator of Minerals
https://australian.museum/about/history/people/oliver-chalmers-curator-of-minerals/The promising lad who became a highly regarded geologist.
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Burra
Permanent kids learning space
10am - 4.30pm![]()
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Wansolmoana
Permanent exhibition
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Minerals
Permanent exhibition
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