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Emily Gap
Emily Gap / Anthwerrke is a natural attraction and significant cultural site to the Arrernte people in the East MacDonnell Ranges, eight kilometres to the east of Mparntwe/Alice Springs, in Australia's Northern Territory. Various sections of the Gap include Aboriginal rock art. It is a registered sacred site and sits within the Yeperenye / Emily and Jessie Gaps Nature Park. History Adjacent to Jessie Gap, Emily Gap is a significant site for the dreaming stories of three ancestral caterpillars, Yeperenye, Utnerrengatye and the Ntyarlke. The caterpillar dreaming is one of the most important creation stories for Mparntwe/Alice Springs and the surrounding region. Many Arrernte people conceived in Alice Springs consider themselves direct descendants of these caterpillars. From 1 April 1872 Emily Gap became part of the Undoolya Station pastoral lease and, when cattle first arrived as part of an overland droving trip from South Australia in March 1873 they first camped here. In doi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arrernte People
The Arrernte () people, sometimes referred to as the Aranda, Arunta or Arrarnta, are a group of Aboriginal Australian peoples who live in the Arrernte lands, at ''Mparntwe'' (Alice Springs) and surrounding areas of the Central Australia region of the Northern Territory. Many still speak one of the various Arrernte dialects. Some Arrernte live in other areas far from their homeland, including the major Australian cities and overseas. Arrernte spirituality focuses on the landscape and The Dreaming which the Arrernte name for is Altyerre. Altjira is the creator being of the Inapertwa that became all living creatures. Tjurunga are objects of religious significance. The Arrernte Council is the representative and administrative body for the Arrernte Lands and is part of the Central Land Council. Tourism is important to the economy of Alice Springs and surrounding communities. Arrernte languages "Aranda" is a simplified, Australian English approximation of the tradition ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orogeny
Orogeny () is a mountain-mountain formation, building process that takes place at a convergent boundary, convergent plate margin when plate motion compresses the margin. An or develops as the compressed plate crumples and is tectonic uplift, uplifted to form one or more mountain ranges. This involves a series of geological processes collectively called orogenesis. These include both structural deformation (physics), deformation of existing continental crust and the creation of new continental crust through volcanism. Magma rising in the orogen carries less dense material upwards while leaving more dense material behind, resulting in compositional differentiation of Earth's lithosphere (crust (geology), crust and uppermost mantle (geology), mantle). A synorogenic (or synkinematic) process or event is one that occurs during an orogeny. The word ''orogeny'' comes . Although it was used before him, the American geologist Grove Karl Gilbert, G. K. Gilbert used the term in 1890 to me ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inland Sea (geology)
An inland sea (also known as an epeiric sea or an epicontinental sea) is a continental body of water which is very large in area and is either completely surrounded by dry land (landlocked), or connected to an ocean by a river, strait or " arm of the sea". An inland sea will generally be brackish, with higher salinity than a freshwater lake but usually lower salinity than seawater. As with other seas, inland seas experience tides governed by the orbits of the Moon and Sun. Definition What constitutes an "inland sea" is complex and somewhat necessarily vague. The United States Hydrographic Office defined it as "a body of water nearly or completely surrounded by land, especially if very large or composed of salt water". Geologic engineers Heinrich Ries and Thomas L. Watson say an inland sea is merely a very large lake. Rydén, Migula, and Andersson and Deborah Sandler of the Environmental Law Institute add that an inland sea is "more or less" cut off from the ocean. It may be semi- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Siltstone
Siltstone, also known as aleurolite, is a clastic sedimentary rock that is composed mostly of silt. It is a form of mudrock with a low clay mineral content, which can be distinguished from shale by its lack of fissility. Although its permeability and porosity is relatively low, siltstone is sometimes a tight gas reservoir rock, an unconventional reservoir for natural gas that requires hydraulic fracturing for economic gas production. Siltstone was prized in ancient Egypt for manufacturing statuary and cosmetic palettes. The siltstone quarried at Wadi Hammamat was a hard, fine-grained siltstone that resisted flaking and was almost ideal for such uses. Description There is not complete agreement on the definition of siltstone. One definition is that siltstone is mudrock (clastic sedimentary rock containing at least 50% clay and silt) in which at least 2/3 of the clay and silt fraction is composed of silt-sized particles. Silt is defined as grains 2–62 μm in diam ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a Clastic rock#Sedimentary clastic rocks, clastic sedimentary rock composed mainly of grain size, sand-sized (0.0625 to 2 mm) silicate mineral, silicate grains, Cementation (geology), cemented together by another mineral. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar, because they are the most resistant minerals to the weathering processes at the Earth's surface. Like uncemented sand, sandstone may be imparted any color by impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Because sandstone beds can form highly visible cliffs and other topography, topographic features, certain colors of sandstone have become strongly identified with certain regions, such as the red rock deserts of Arches National Park and other areas of the Southwestern United States, American Southwest. Rock formations composed of sandstone usually allow the p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), 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 (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite ( ) is a coarse-grained (phanerite, phaneritic) intrusive rock, intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dike (geology), dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF diagram, QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) conta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quartzite
Quartzite is a hard, non- foliated metamorphic rock that was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts, and hence quartzite is a metasandstone. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals. The term ''quartzite'' is also sometimes used for very hard but unmetamorphosed sandstones that are composed of quartz grains thoroughly cemented with additional quartz. Such sedimentary rock has come to be described as orthoquartzite to distinguish it from metamorphic quartzite, which is sometimes called metaquartzite to emphasize its metamorphic origins. Quartzite is very resistant to chemical weathering and often forms ridges and resist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Charles Todd (pioneer)
Sir Charles Todd (7 July 1826 – 29 January 1910) worked at the Royal Greenwich Observatory 1841–1847 and the Cambridge University observatory from 1847 to 1854. He then worked on telegraphy and undersea cables until engaged by the government of South Australia as astronomical and meteorological observer, and head of the electric telegraph department. Early life and career Todd was the son of grocer Griffith ToddH. P. Hollis, 'Todd, Sir Charles (1826–1910)', rev. K. T. Livingston, Oxford Dictionary of National Biography, Oxford University Press, 2004 and Mary Parker; he was born at Islington, London, the second of five children. Shortly after Charles's birth the family moved to Greenwich, where his father set up as a wine and tea merchant. Charles was educated and spent most of his life in Greenwich before moving to Australia. In December 1841, he entered the service of the Royal Observatory, Greenwich, under Sir George Biddell Airy. He was fortunate that his school lea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
MacDonnell Ranges
The MacDonnell Ranges, or Tjoritja in Arrernte language, Arrernte, is a mountain range located in southern Northern Territory. MacDonnell Ranges is also the name given to an Interim Biogeographic Regionalisation for Australia, interim Australian bioregion broadly encompassing the mountain range, with an area of .IBRA Version 6.1 data The range is a long series of mountains in central Australia, consisting of parallel ridges running to the east and west of Alice Springs. The mountain range contains many spectacular gaps and gorges as well as areas of Indigenous Australian, Aboriginal significance. The ranges were named after Sir Richard Graves MacDonnell, Richard MacDonnell (the Governor of South Australia at the time) by John McDouall Stuart, whose 1860 expedition reached them in April of that year. The Horn Exped ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Australia
South Australia (commonly abbreviated as SA) is a States and territories of Australia, state in the southern central part of Australia. With a total land area of , it is the fourth-largest of Australia's states and territories by area, which includes some of the most arid parts of the continent, and with 1.8 million people. It is the fifth-largest of the states and territories by population. This population is the second-most highly centralised in the nation after Western Australia, with more than 77% 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 26,878. South Australia shares borders with all the other mainland states. 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 (state), Victoria, and to the s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Undoolya Station
Undoolya Station is a pastoral lease east of Alice Springs (Mparntwe) in the Northern Territory of Australia. It was one of the first two pastoral leases granted in the region with the lease for it, and Owen Springs Station, being granted on 1 April 1872; five months before the completion of the Overland Telegraph Line. It has been managed by the Hayes Family since 1906 and t is currently managed by Ben and Nicole Hayes. Early history The Central Arrernte people have lived on Undoolya Station and the surrounding region for thousands of years. Undoolya Station was established by South Australian pastoralist and stock agent Edward Mead Bagot. After working the southern section of the Overland Telegraph Line, Bagot applied for two leases adjoining the Alice Springs Telegraph Station in 1872. His friend Joseph Gilbert also applied for two blocks, closer to where Owen Springs Station is today. Bagot's son Ted, Churchill Smith and Joseph Gilbert's son William, select ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
