In the northern parts the rock is mostly friable sandstone, but in the south it is divided into conglomerate below and siltstone above. Just off Lockhart -The Rock Road, this is both easy to access and equipped with everything you need to make the most of sunny afternoons. In the southern part of the basin a delta formed the lower Illawarra Coal Measures. Coal has been the main focus for exploration within the basin since this time. Many NSW national park campgrounds, accommodation and visitor centres will start to reopen from 1 June but important changes are in place to keep visitors safe. They are called Precipice Sandstone,In the Cretaceous sea water entered and deposited shale from the Rolling Downs GroupMost of the basin is covered by alluvium and lake deposits from the The first rocks in the Clarence Moreton Basin of New South Wales are the Chillingham Volcanics. Early in the The oldest Jurassic rocks in the basin are found in the northeast near the Queensland border.

The area used to be an ancient lake bed, a part of a chain of lakes between Willandra Creek and Lachlan River. ): The Dinosauria, 2nd, Berkeley: University of California Press. The Erins Vale Formation interrupts this. But deepening seawater formed the Kulnura Marine Tongue and Bulga Formation. Red Rock headland is part of the Solitary Islands Coastal walk, and is a significant place to the local Gumbaingirr people. Extensive coal exploration drilling has been undertaken, mostly in the Coorabin area. In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.

In the Late Permian river and delta deposition formed the Tomago and Whittingham Coal Measures in the north. A rock formation is an isolated, scenic, or spectacular surface rock outcrop. 573–574.
It is approximately 25 km wide at Oaklands and approximately 15 km wide at its northern extent. The Laytons Range ConglomerateThe next layer of rocks in the basin forming a nested U shape in its exposure is the Kangaroo Creek Sandstone.During the Cainozoic, rifting along the east coast of Australia commenced and uplifted the eastern side of the Clarence Moreton Basin.After Australia separated from Antarctica the Murray basin was formed. Beach deposition then formed Waratah/Watts Sandstone and the Darkes Forest Sandstone and Angus Place Sandstone. Fingal Head, an amazing basalt rock formation Fingal Head, located on the Tweed Coast of northern NSW, is a place of natural beauty and is one of the areas hidden gems. The basin floor only subsided slowly over time.The Oaklands Basin covers approximately 3 800 square kilometres in the Riverina district of southern New South Wales, between the towns of Mulwala, Jerilderie, Griffith, Coleambly, Oaklands and Albury. These are from some time in the Triassic period, and for a band north and south of The Red Cliff Coal Measures are from late Triassic. Volcanic rocks.


In addition two coal drilling programs by the NSW Department of Industry, designed to help define the limits of the basin, have resulted in wide-spaced drilling coverage over most of the basin.

Eerie, unusual and utterly captivating, the Pinnacles really are the pinnacle of rock formations.

Their names are Meehni, Wimlah, and Gunnedoo. The Oaklands Basin hosts to more than 1000 m thick sediments. The Three Sisters at sunset Over the beach land formed again with the Newcastle and Wollombi Coal Measures in the north, and upper Illawarra Coal Measures in the south. In the north east major outcrops of volcanic rocks are found between Warialda to Glen Innes and south to Armidale, the Liverpool Range, Barrington Tops, Nandewar Range near Narrabri, the Warrumbungles, and the Tweed Volcano.

Petroleum exploration within the basin has been minimal, consisting of a small number of geophysical surveys and two stratigraphic wells. For directions, safety and practical information, see Subscribe to our Naturescapes e-newsletter which is packed with the latest information, experiences and events in NSW national parks.


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