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The Yilgarn Craton is a large craton that constitutes a major part of the Western Australian land mass. It is bounded by a mixture of sedimentary basins and Proterozoic fold and thrust belts . Zircon grains in the Jack Hills , Narryer terrane have been dated at ~4.27 Ga , with one detrital zircon dated as old as 4.4 Ga. [ 1 ]
The Yarrabubba impact structure is the eroded remnant of an impact crater, situated in the northern Yilgarn Craton near Yarrabubba Station between the towns of Sandstone and Meekatharra, Mid West Western Australia. [2] [3] With an age of 2.229 billion years, it is the oldest known impact structure on Earth. [1]
Dalgaranga crater is a small meteorite impact crater located on Dalgaranga pastoral station 75 km (47 mi) northwest of Mount Magnet (or north of Yalgoo) in Western Australia. It is only 24 m (79 ft) in diameter and 3 m (9.8 ft) deep, making it Australia's smallest impact crater (with exception of the smallest members of the Henbury crater field).
This is an accepted version of this page This is the latest accepted revision, reviewed on 9 November 2024. Rock formation in Western Australia Not to be confused with The Wave, Arizona. Wave Rock Katter Kich Western Australia Wave Rock Coordinates 32°26′38″S 118°53′54″E / 32.44389°S 118.89828°E / -32.44389; 118.89828 (Wave Rock) Location 3 km (2 mi) E of Hyden 296 ...
The Gascoyne Complex is separated from the Yilgarn Craton to the south by a major fault, the Errabiddy Shear Zone. To the east and northeast rocks of the complex are overlain unconformably by fine-grained Mesoproterozoic sedimentary rocks of the Edmund Basin and Collier Basin (formerly known as the Bangemall Basin). Several inliers of granite ...
Yapungku orogeny – North Yilgarn craton margin, Western Australia, (c. 1765 Ma) Albany-Fraser orogeny – Mountain-forming period in Australia – Western Australia, (c. 1710–1020 Ma) Mangaroon orogeny – Gascoyne Complex , Western Australia, (c. 1680–1620 Ma)
Ah, the good ol’ Leica M3. This camera was first released in 1954 and became a game-changer in the 35mm camera market due to its unique build and design.
The Dryandra Woodland is found within the south-western province of the Yilgarn craton, "an ancient plateau composed mainly of granite, with intrusions of dolerite and capped with laterite. Past weathering of the plateau in the Dryandra area has produced a gently undulating countryside". [1]
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