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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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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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Peridot
https://australian.museum/learn/minerals/gemstones/peridot/Facts about Peridot.
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Rhodonite
https://australian.museum/learn/minerals/gemstones/rhodonite/Facts about Rhodonite.
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Nephrite jade
https://australian.museum/learn/minerals/gemstones/nephrite-jade/Facts about Nephrite jade.
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Garnet
https://australian.museum/learn/minerals/gemstones/garnet/Facts about Garnet
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Topaz
https://australian.museum/learn/minerals/gemstones/topaz/Facts about Topaz.
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Sapphire and Ruby
https://australian.museum/learn/minerals/gemstones/sapphire-and-ruby/Facts about Sapphire and Ruby.
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Igneous rock types
https://australian.museum/learn/minerals/shaping-earth/igneous-rock-types/Igneous rocks can be divided up into four groups, based on how they were formed and what they are made of.
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Volcanic landforms
https://australian.museum/learn/minerals/shaping-earth/volcanic-landforms/Each type of volcanic massif (structure) contains lavas, pyroclastic rocks and intrusions, but these differ in proportions and compositions.
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Ramses & the Gold of the Pharaohs
Special exhibition
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Wansolmoana
Permanent exhibition
Open daily -
School programs and excursions
Virtual excursions
Educator-led tours -
Burra
Permanent education space
10am - 4.30pm