Mount Chambers Gorge
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Mount Chambers Gorge
Mount Chambers Gorge (alternative name: Marlawadinha Inbiri) is a gorge in the Australian state of South Australia in the locality of Wertaloona about north-east of Blinman in the Flinders Ranges. Although on private land, they are a tourist attraction near to the road between Blinman and Balcanoona, Gammon Ranges National Park. They are part of the Wearing Hills.Glovebox Guide - ''The Flinders Ranges'', Australian Geographic, 2000, p135, Mount Chambers Gorge winds through the Wearing Hills toward Lake Frome. There is usually water in the bed of the creek, although less in recent years than formerly; while it is brackish it can be used by campers (given appropriate treatment). The upper part of the Gorge is accessible to most vehicles while the lower parts are now closed to all but foot traffic and can no longer be accessed by four-wheel-drive. There is signage at the car park indicating the closure of the lower gorge to vehicle traffic. Mount Chambers Chasm The upp ...
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Eastern End Of Mount Chambers
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Gorge
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's River source, headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examp ...
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South Australia
South Australia (commonly abbreviated as SA) is a state in the southern central part of Australia. It covers some of the most arid parts of the country. With a total land area of , it is the fourth-largest of Australia's states and territories by area, and second smallest state by population. It has a total of 1.8 million people. Its population is the second most highly centralised in Australia, after Western Australia, with more than 77 percent of South Australians living in the capital Adelaide, or its environs. Other population centres in the state are relatively small; Mount Gambier, the second-largest centre, has a population of 33,233. South Australia shares borders with all of the other mainland states, as well as the Northern Territory; it is bordered to the west by Western Australia, to the north by the Northern Territory, to the north-east by Queensland, to the east by New South Wales, to the south-east by Victoria, and to the south by the Great Australian Bight.M ...
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Blinman, South Australia
Blinman is a locality incorporating two towns located in the Australian state of South Australia within the Flinders Ranges about north of the state capital of Adelaide. It is very small but has the claim of being the highest surveyed town in South Australia. It serves as a base for large acre pastoralists and tourism. The town is just north of the Flinders Ranges National Park, is 60 kilometres north of Wilpena Pound. History Indigenous people This land belonged to the Adnyamathanha tribe, of Indigenous Australians prior to colonisation. One of their unique customs was burn offs (controlled bushfires) to promote plant growth in the future seasons. European settlement The first European settlement around the current Blinman, was firstly of Angorichina Station. This land was taken up for sheep farming in the 1850s. A shepherd employed by the station, Robert Blinman, discovered a copper outcrop on a hot December day in 1859. Blinman gambled some of his money on the prese ...
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Flinders Ranges
The Flinders Ranges are the largest mountain range in South Australia, which starts about north of Adelaide. The ranges stretch for over from Port Pirie to Lake Callabonna. The Adnyamathanha people are the Aboriginal group who have inhabited the range for tens of thousands of years. Its most well-known landmark is Wilpena Pound / Ikara, a formation that creates a natural amphitheatre covering and containing the range's highest peak, St Mary Peak (). The ranges include several national parks, the largest being the Ikara-Flinders Ranges National Park, as well as other protected areas. It is an area of great geological and palaeontological significance, and includes the oldest fossil evidence of animal life was discovered. The Ediacaran Period and Ediacaran biota take their name from the Ediacara Hills within the ranges. In August 2022, a nomination for the Flinders Ranges to be named a World Heritage Site was lodged. History The first humans to inhabit the Flinders ...
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Gammon Ranges National Park
The Vulkathunha-Gammon Ranges National Park is a protected area in the Flinders Ranges of South Australia, immediately south-west of and adjacent to the Arkaroola Protection Area. They encompass some of the most rugged and spectacular country in South Australia. Geography The central ranges are of a different topographical nature to the rest of the Flinders, being composed of roughly flat-lying strata, creating a high plateau into which spectacular gorges have been cut, instead of the buckled and folded strata further south which lead to the ubiquitous cuestas of Wilpena Pound. The Gammons are dominated by "The Plateau" in the southwest, which is contiguous with and of much the same height as the Blue Range further northeast, culminating in Benbonyathe Hill (1064m), the highest point in the Flinders north of Wilpena. Other summits on the largely flat range and plateau include Elephant Hill (with adjacent outliers North Tusk and South Tusk), Mount Changeweather, Four Winds Hil ...
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Australian Geographic
Australian Geographic is a media business that produces the ''Australian Geographic'' magazine, ''DMag'' magazine, specialist book titles, travel guides, diaries and calendars and online media. It published editions of the Australian Encyclopaedia. It previously operated the Australian Geographic retail chain stores and Australian Geographic Travel and Australian Geographic Adventures. ''Australian Geographic'' magazine, originally titled ''Dick Smith's Australian Geographic'', is a bi-monthly geographical journal created by Dick Smith in 1986. The magazine focuses mainly on stories about Australia, or about Australian people in other countries. The six editions published each year are available by subscription and on newsstands. They include posters or sheet maps in each edition, as well as photographs and detailed technical illustrations. Australian Geographic also has a website that includes the entire magazine digital archive. Each year, a portion of the profits is prov ...
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Lake Frome
Lake Frome / Munda is a large endorheic lake in the Australian state of South Australia to the east of the Northern Flinders Ranges. It is a large, shallow, unvegetated salt pan, long and wide, lying mostly below sea level and having a total surface area of . It only rarely fills with brackish water flowing down usually dry creeks in the Northern Flinders Ranges from the west, or exceptional flows down the Strzelecki Creek from the north. The Adnyamathanha name for the lake is ''Munda''. Europeans named the lake ''Frome'' after Edward Charles Frome, after he mapped the area in 1843. The lake was officially dual named Lake Frome / Munda in 2004. Description The lake adjoins Vulkathunha-Gammon Ranges National Park to its west and lies adjacent to Lake Callabonna linked by Salt Creek to its north, the southern Strzelecki Desert to its east, and the Frome Downs pastoral lease to its south. The ancient Lake Mega-Frome (Lakes Frome, Blanche, Callabonna and Gregory) was last conn ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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Mesa
A mesa is an isolated, flat-topped elevation, ridge or hill, which is bounded from all sides by steep escarpments and stands distinctly above a surrounding plain. Mesas characteristically consist of flat-lying soft sedimentary rocks capped by a more resistant layer or layers of harder rock, e.g. shales overlain by sandstones. The resistant layer acts as a caprock that forms the flat summit of a mesa. The caprock can consist of either sedimentary rocks such as sandstone and limestone; dissected lava flows; or a deeply eroded duricrust. Unlike ''plateau'', whose usage does not imply horizontal layers of bedrock, e.g. Tibetan Plateau, the term ''mesa'' applies exclusively to the landforms built of flat-lying strata. Instead, flat-topped plateaus are specifically known as '' tablelands''.Duszyński, F., Migoń, P. and Strzelecki, M.C., 2019. ''Escarpment retreat in sedimentary tablelands and cuesta landscapes–Landforms, mechanisms and patterns.'' ''Earth-Science Reviews, no. ...
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Mountains Of South Australia
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ...
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