Your search returned 14 results
By Page Type
By Tag
- All
- blog (700)
- Blog (237)
- AMRI (159)
- First Nations (101)
- archives (92)
- Anthropology (86)
- podcast (84)
- International collections (77)
- fish (73)
- Ichthyology (68)
- staff (64)
- AMplify (54)
- Indonesia (54)
- climate change (47)
- Eureka Prizes (44)
- geoscience (43)
- lifelong learning (42)
- invertebrate guide (39)
- staff profile (39)
- Bali (38)
- Digivol (36)
- Ancient Egypt (33)
- Herpetology (32)
- earth sciences (30)
- media release (30)
- archaeology (29)
- frog (29)
- frogs (29)
- Earth and Environmental Science (28)
- biodiversity (27)
- geological processes (27)
- citizen science (26)
- Aboriginal and Torres Strait Islander (25)
- Explore (25)
- minerals (25)
- sustainability (25)
- Lizard Island (24)
- exhibition (24)
- marine invertebrates (24)
- education (23)
- fossils (23)
- geology (23)
- malacology (23)
- egypt (22)
- history (22)
- herpetology (21)
- Balinese Art (20)
- research (20)
- Great Barrier Reef (19)
- gemstone (19)
-
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.
-
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.
-
Crystallography
https://australian.museum/learn/minerals/what-are-minerals/crystallography/Minerals can be identified by the shape of their crystals: called crystallography. External crystallography measures the outside properties of crystals such as length of crystal surfaces and the angles between these surfaces.
-
Plate Tectonics
https://australian.museum/learn/minerals/shaping-earth/plate-tectonic-processes/Since the 1950s, several discoveries have led to a new understanding of how the Earth works.
-
Meteors and Meteorites
https://australian.museum/learn/minerals/shaping-earth/meteors-and-meteorites/Solid pieces of extraterrestrial debris (meteoroids) can stray from their orbits in outer space and be captured by Earth's gravity.
-
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.
-
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.
-
Limestone caves
https://australian.museum/learn/minerals/shaping-earth/limestone-caves/Caves form in limestone (calcium carbonate), and occasionally in dolomite (calcium magnesium carbonate), when water containing dissolved carbon dioxide (carbonic acid) seeps into rock crevices and joints.
-
Soils
https://australian.museum/learn/minerals/shaping-earth/soils/Soils are made up of three layers and are thickest where they are older and in warm and wet environments.
-
Classification of sedimentary rocks
https://australian.museum/learn/minerals/shaping-earth/classification-of-sedimentary-rocks/Sedimentary rocks are classified according to the predominant grain size present, as well as by their mineral content.
-
Jurassic World by Brickman
Tickets on sale now.
Open until 17 July. -
Burra
Opens Saturday 2 July
Permanent education space -
School programs and excursions
Virtual excursions
Educator-led tours