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The Department of Mines commenced in late 1874, and the Geological Survey of New South Wales was brought into existence on 1 January 1875. Charles Smith Wilkinson was its first supervisor. In the 1950s to 1970s the administering body for mines was the New South Wales Department of Mines or New South Wales Department of Mines and Agriculture.
Pages in category "Geology of New South Wales" The following 59 pages are in this category, out of 59 total. ... Browns Field (New South Wales) Budgong Sandstone ...
Newcastle Coal Measures is a major geologic formation in eastern Australia. Found in the Sydney Basin and Lachlan Orogen, this stratum is up to 1200 metres thick, consisting of dozens of different sub types. Formed between the Changhsingian and Wuchiapingian ages, around 256 to 252 Ma in the Permian. This formation includes coal seams, tuffaceous claystone, siltstone, sandstone, and ...
Scheibner E. 1996–1998. Geology of New South Wales – synthesis. Geological Survey of New South Wales Memoir geology: 13 (2 v.) AUSTRALIAN LITHOSPHERE Clitheroe G. et al. 2000. The crustal thickness of Australia, Journal Geophysical Research 105: 13,697–13,713. Hillis RR & Muller RD. (eds) 2003. Evolution and dynamics of the Australian Plate.
The Central Tablelands in New South Wales is a geographic area that lies between the Sydney Metropolitan Area and the Central Western Slopes and Plains. The Great Dividing Range passes in a north–south direction through the Central Tablelands and includes the Blue Mountains.
Aerial view of Long Reef Beach, headland, and golf course; Collaroy Beach at upper left. Long Reef is a prominent headland on the Northern Beaches of Sydney, Australia. ...
The Griman Creek Formation is a geological formation in northern New South Wales and southern Queensland, Australia whose strata date back to the Albian-Cenomanian stages of the mid-Cretaceous. [1] It is most notable being a major source of opal, found near the town of Lightning Ridge, New South Wales. Alongside the opal opalised fossils are ...
The Deniliquin multiple-ring feature is a distinct deeply buried structure in southeast Australia. It is named after the town of Deniliquin.Its characteristics suggest that it is associated with an asteroid impact structure of diameter 520 km (320 mi), which would make it the largest one on Earth, exceeding the largest known one, the Vredefort impact structure of about 300 km (190 mi) in diameter.