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William Matthew Hart (1830-1908)
https://australian.museum/learn/collections/museum-archives-library/john-gould/william-matthew-hart-1830-1908/William Hart had a predilection for intense colours, an attribute that would have pleased Gould. Though he commenced medical training, Hart was forced to abandon his studies due to lack of finance. He then turned to making his living as a colourer.
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John Gould the artist
https://australian.museum/learn/collections/museum-archives-library/john-gould/gould-the-artist/As an artist, John Gould's skills were limited.
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John Gould - the age of collecting
https://australian.museum/learn/collections/museum-archives-library/john-gould/the-age-of-collecting/Learn more about how historical context shaped Gould's success in the field of natural history.
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Fossils in Talbragar, NSW
https://australian.museum/learn/australia-over-time/fossils/sites/talbragar/Talbragar is a well-known fossil site in Australia and contains one of the most significant Jurassic terrestrial fossil deposits in Australia. It is also the only Jurassic fish site found in New South Wales.
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Fossils in Murgon, QLD
https://australian.museum/learn/australia-over-time/fossils/sites/murgon/Murgon is significant as the only site in Australia that records a diverse vertebrate fauna dating from the early Tertiary Period (55 million years ago), approximately ten million years after the extinction of the dinosaurs.
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The Jurassic Period (201 - 145 million years ago)
https://australian.museum/learn/australia-over-time/evolving-landscape/the-jurassic-period-201-145-million-years-ago/The Jurassic was warm and wet with flourishing plant life supporting a diverse fauna.
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The Mesozoic Era (252 - 66 million years ago)
https://australian.museum/learn/australia-over-time/evolving-landscape/the-mesozoic-era/The Mesozoic Era spanned 252 to 66 million years ago. Australia in the Mesozoic was nothing like it is today. It did not exist as a separate landmass, its position on the globe was much further south and the climate and plants were very different.
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The late Miocene Epoch (10.4-5 million years ago)
https://australian.museum/learn/australia-over-time/evolving-landscape/the-late-miocene-epoch/The late Miocene was a time of global drying and cooling. As ice rapidly accumulated at the poles, sea-levels fell, rainfall decreased and rainforests retreated. Many plant and animal groups died out and other forms, better adapted to a drying world, took their place.
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The Eocene Epoch (56-33.9 million years ago)
https://australian.museum/learn/australia-over-time/evolving-landscape/the-eocene-epoch/By the beginning of the Eocene, Gondwana had almost split apart, but Australia, Antarctica and South America remained joined. The Antarctic portion of Gondwana straddled the South Pole but because the global climate was warmer it was free of ice and snow.
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Types of metamorphism
https://australian.museum/learn/minerals/shaping-earth/types-of-metamorphism/There are several different types of metamorphism, including dynamic, contact, regional, and retrogressive metamorphism, that form and shape rocks.
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Machu Picchu and the Golden Empires of Peru
Now open
Tickets on sale -
Tails from the Coasts
Special exhibition
Opening Saturday 10 May -
Wild Planet
Permanent exhibition
Open daily -
Minerals
Permanent exhibition
Open daily