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														Building Materials
 https://australian.museum/learn/minerals/geological-deposits/building-materials/Perhaps the most important geological deposits are those that we use for building purposes. These come from all geological environments. 
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														Wave Rock
 https://australian.museum/learn/australia-over-time/evolving-landscape/wave-rock/Wave Rock is in the wheat belt region of Western Australia, 350 km south-east of Perth. 
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														The 'Barratta' Meteorite
 https://australian.museum/learn/collections/natural-science/mineralogy/mineralogy-collection-the-barratta-meteorite/The story of the 'Barratta meteorite' has a rather uncertain beginning. One version claims that in 1859 a stockman witnessed spectacular light and sound effects at a place where pieces of the meteorite were later found. 
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														A Rock from Cape Horn
 https://australian.museum/learn/collections/natural-science/mineralogy/mineralogy-collection-a-rock-from-cape-horn/On 22 May 1826, two ships sailed from Plymouth, England on a major expedition to chart the southern coast of South America. 
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														Metamorphic rocks
 https://australian.museum/learn/minerals/shaping-earth/metamorphic-rocks/Metamorphic rocks form because of changes in temperature and depth of burial within the Earth in a solid state without actual melting. 
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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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														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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														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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														Where will the next volcano erupt in Australia?
 https://australian.museum/learn/news/blog/amri-where-next-volcano-erupt-in-australia/The volcanic future of Australia is revealed. 
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				Discover more2025 Australian Geographic Nature Photographer of the YearSpecial exhibition 
 Now open
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				Discover moreUnfinished BusinessSpecial exhibition 
 Opens 1 November
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				Discover moreWansolmoanaPermanent exhibition 
 Open daily
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				Find out moreBurraPermanent kids learning space 
 10am - 4.30pm![]()  
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				Discover moreMineralsPermanent exhibition 
 Open daily![]()  

 
							 
												 
												 
												