|
Clarence Moreton Basin
The Clarence Moreton Basin is a Mesozoic sedimentary basin on the easternmost part of the Australian continent. It is located in the far north east of the state of New South Wales around Lismore and Grafton and in the south east corner of Queensland. It is the part of the Great Artesian Basin that extends to the east coast in Australia's central eastern lowlands. Description It formed by oblique extension of the underlying Paleozoic New England Orogen basement. It consists of continental deposits, starting with a small amount of Triassic coal beds, and then mostly Jurassic and Cretaceous sedimentary rocks. The basin covers . The basin was named when the Clarence Basin (named after the Clarence River) and Moreton Basin in Queensland were proved to be one structure. Oil is likely to be present in the basin. Stratigraphy The oldest rocks in the Clarence Moreton Basin of New South Wales are the Chillingham Volcanics. These are from some time in the Triassic period ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bexhill, New South Wales
Bexhill is a small village in New South Wales, Australia. As of 2006, the town had a population of 472 people. It is located about from Byron Bay, New South Wales, Byron Bay and about from Lismore, New South Wales, Lismore and is within the City of Lismore local government area. It is on the Murwillumbah railway line and on Bangalow Road. The traditional owners of this area are the Widjabal, Widjabul people of the Bundjalung nation. Attractions Bexhill is well known for its open air cathedral which is managed by volunteers from the nearby Uniting Church. The "cathedral" has native gardens and overlooks a large length of valley and hills along Coopers Creek. It is well used for wedding services and special events. The village also contains an old quarry, formerly the Bexhill Brickworks, which is officially closed for recreational purposes. In 2016, the Daily Telegraph (Australia), Daily Telegraph reported that the water had high levels of acidity but many people swim there d ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grafton, New South Wales
Grafton ( Bundjalung: ''Gumbin Gir'') is a city in the Northern Rivers region of the Australian state of New South Wales. It is located on the Clarence River, on a floodplain, approximately by road north-northeast of the state capital Sydney. The closest major cities, Brisbane and the Gold Coast, are located across the border in South East Queensland. At the 2021 census, Grafton had a population of 19,255. The city is the largest settlement and, with Maclean, the shared administrative centre of the Clarence Valley Council local government area, which is home to over 50,000 people in all. History Before European settlement, the Clarence River marked the border between the BundjalungTindale, Norman (1974) "Badjalang" in his ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Outcrop
An outcrop or rocky outcrop is a visible exposure of bedrock or ancient superficial deposits on the surface of the Earth and other terrestrial planets. Features Outcrops do not cover the majority of the Earth's land surface because in most places the bedrock or superficial deposits are covered by soil and vegetation and cannot be seen or examined closely. However, in places where the overlying cover is removed through erosion or tectonic uplift, the rock may be exposed, or ''crop out''. Such exposure will happen most frequently in areas where erosion is rapid and exceeds the weathering rate such as on steep hillsides, mountain ridges and tops, river banks, and tectonically active areas. In Finland, glacial erosion during the last glacial maximum (ca. 11000 BC), followed by scouring by sea waves, followed by isostatic uplift has produced many smooth coastal and littoral outcrops. Bedrock and superficial deposits may also be exposed at the Earth's surface due to human exca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chillingham Volcanics
Chillingham can refer to: * Chillingham (game), a computer game designed for the visually impaired * Chillingham, New South Wales, a village in New South Wales, Australia * Chillingham, Northumberland Chillingham is a village in Northumberland, England. It is situated approximately to the east of Wooler, Northumberland, Wooler, south of Chatton. At the 2011 Census the population remained less than 100. Detailed information is included in th ..., a village in Northumberland in the north of England * Chillingham Castle, an ancient castle in Northumberland, England, near Chillingham * Chillingham cattle, a herd of rare cattle which have lived for centuries in the grounds of Chillingham Castle, in Northumberland, England * Chillingham Road Metro station, a metro station in Newcastle upon Tyne, England * , a minesweeper of the British Royal Navy {{disambig, geo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kangaroo Creek Sandstone 4
Kangaroos are marsupials from the family Macropodidae (macropods, meaning "large foot"). In common use, the term is used to describe the largest species from this family, the red kangaroo, as well as the antilopine kangaroo, eastern grey kangaroo, and western grey kangaroo. Kangaroos are indigenous to Australia and New Guinea. The Australian government estimates that 42.8 million kangaroos lived within the commercial harvest areas of Australia in 2019, down from 53.2 million in 2013. As with the terms "wallaroo" and "wallaby", "kangaroo" refers to a paraphyletic grouping of species. All three terms refer to members of the same taxonomic family, Macropodidae, and are distinguished according to size. The largest species in the family are called "kangaroos" and the smallest are generally called "wallabies". The term "wallaroos" refers to species of an intermediate size. There are also the tree-kangaroos, another type of macropod which inhabit the upper branches of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moreton Bay
Moreton Bay is a bay located on the eastern coast of Australia from central Brisbane, Queensland. It is one of Queensland's most important coastal resources. The waters of Moreton Bay are a popular destination for recreational anglers and are used by commercial operators who provide seafood to market. The Port of Brisbane coordinates large traffic along the shipping channel which crosses the northern section of the bay. The bay serves as a safe approach to the airport and reduces noise pollution over the city to the west of the runway. A number of barge, ferry and water-taxi services also travel over the bay. Moreton Bay was the site of conflict between the Quandamooka people and early European settlers. It contains environmentally significant habitats and large areas of sandbanks. The bay is the only place in Australia where dugong gather into herds. Many parts of the mainland foreshore and southern islands are settled. The waters of Moreton Bay are relatively calm, bein ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clarence River (New South Wales)
The Clarence River ( Bundjalung: ''Boorimbah'', Yaygir: ''Ngunitiji'') is a river situated in the Northern Rivers district of New South Wales, Australia. It rises on the eastern slopes of the Great Dividing Range, in the Border Ranges west of Bonalbo, near Rivertree at the junction of Koreelah Creek and Maryland River, on the watershed that marks the border between New South Wales and Queensland. It flows generally south, south east and north east, and is joined by twenty-four tributaries including Tooloom Creek and the Mann, Nymboida, Cataract, Orara, Coldstream, Timbarra, and Esk rivers. It descends over the course of its length and empties into the Coral Sea in the South Pacific Ocean, between Iluka and Yamba. On its journey it passes through the towns of Tabulam and Copmanhurst, the city of Grafton, and the towns of Ulmarra, and Maclean. The river features many large river islands, including Woodford, Chatsworth, Ashby, Warregah and Harwood islands; and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Government Of New South Wales
The Government of New South Wales, also known as the NSW Government, is the executive state government of New South Wales, Australia. The government comprises 11 portfolios, led by a ministerial department and supported by several agencies. There are also a number of independent agencies that fall under a portfolio but remain at arms-length for political reasons, such as the Independent Commission Against Corruption (New South Wales), Independent Commission Against Corruption and New South Wales Electoral Commission, Electoral Commission. The state Executive Council of New South Wales, Executive Council, consisting of the Governor of New South Wales, governor and senior ministers, exercises the executive authority through the relevant portfolio. The current government is held by the New South Wales Labor Party, state Labor Party, led by Premier Chris Minns. Minns succeeded Dominic Perrottet from the Liberal Party of Australia (New South Wales Division), Liberal Party on 28 Marc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geological Society Of Australia
The Geological Society of Australia (GSA) was established as a non-profit organisation in 1952 to promote, advance and support earth sciences in Australia. The founding chairperson was Edwin Sherbon Hills. William Rowan Browne was a founder of the society and was president 1955–56. at Australian Dictionary of Biography Publications *'' Australian Journal of Earth Sciences (AJES)'' – official journal of the GSA, eight issues per year *'' The Australian Geologist (TAG)'' – quarterly magazine that includes technical ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ninth and longest geological period of the entire Phanerozoic. The name is derived from the Latin , 'chalk', which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation . The Cretaceous was a period with a relatively warm climate, resulting in high Sea level#Local and eustatic, eustatic sea levels that created numerous shallow Inland sea (geology), inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was largely ice-free, although there is some evidence of brief periods of glaciation during the cooler first half, and forests extended to the poles. Many of the dominant taxonomic gr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately 143.1 Mya. The Jurassic constitutes the second and middle period of the Mesozoic, Mesozoic Era as well as the eighth period of the Phanerozoic, Phanerozoic Eon and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province (CAMP). The beginning of the Toarcian Age started around 183 million years ago and is marked by the Toarcian Oceanic Anoxic Event, a global episode of Anoxic event, oceanic anoxia, ocean acidification, and elevated global temperatures associated with extinctions, likely caused by the eruption of the Kar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ; sometimes symbolized 🝈) is a geologic period and system which spans 50.5 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.4 Mya. The Triassic is the first and shortest period of the Mesozoic Era and the seventh period of the Phanerozoic Eon. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
