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Vlei
A vlei () is a shallow minor lake, mostly of a seasonal or intermittent nature. It even might refer to seasonal ponds or marshy patches where frogs and similar marsh dwellers breed. Commonly, vleis vary in their extent, or even in the presence or absence of water, according to the fall of rain or dryness of the season."Compendium of South African history and geography", by George McCall Theal, Edition: 3 - 18779/ref> In terms of water salinity, vleis may be freshwater, saltwater, or brackish. Over time a vlei may degrade into a salt pan or clay pan, such as Dead Vlei or Sossusvlei. Ecoregions Ecology Vleis of various types can be of considerable local ecological importance, harboring many endemic and migratory species. Most vleis are too minor to be granted recognition in the form of a name. However, some major vleis are accorded names, for example Rondevlei and Zeekoevlei in the Cape Peninsula, which are permanent bodies of water. Indeed, Rondevlei is home to hippopot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lakes Of South Africa
This is a list of lakes of South Africa. It includes lakes that were formed naturally, and a few wetlands. For artificial lakes such as reservoirs, refer to List of dams and reservoirs in South Africa. For estuaries (river mouths) see List of estuaries of South Africa, or if they are more the lagoon type List of lagoons of South Africa, and for bays see List of bays of South Africa. * A Subterranean lake * B The name ''Sout Pan'' literally translates as ''Salt Pan'', but the lake is not used to harvest salt. See also * List of estuaries of South Africa * List of rivers of South Africa * List of dams and reservoirs in South Africa * List of lagoons of South Africa * List of bays of South Africa * Ports and harbours in South Africa References {{Authority control * South Africa Lakes Lakes A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes li ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sossusvlei Aus Der Vogelperspektive
Sossusvlei (sometimes written Sossus Vlei) is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring ''vlei''s such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia. The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River. Environment The Sossusvlei area belongs to a wider region of southern Namib with homogeneous features (about 32.000 km²) extending between rivers Koichab and Kuiseb. This area is characterized by high sand dunes of vivid pink-to- ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sossusvlei
Sossusvlei (sometimes written Sossus Vlei) is a salt and clay pan surrounded by high red dunes, located in the southern part of the Namib Desert, in the Namib-Naukluft National Park of Namibia. The name "Sossusvlei" is often used in an extended meaning to refer to the surrounding area (including other neighbouring ''vlei''s such as Deadvlei and other high dunes), which is one of the major visitor attractions of Namibia. The name "Sossusvlei" is of mixed origin and roughly means "dead-end marsh". Vlei is the Afrikaans word for "marsh", while "sossus" is Nama for "no return" or "dead end". Sossusvlei owes this name to the fact that it is an endorheic drainage basin (i.e., a drainage basin without outflows) for the ephemeral Tsauchab River. Environment The Sossusvlei area belongs to a wider region of southern Namib with homogeneous features (about 32.000 km²) extending between rivers Koichab and Kuiseb. This area is characterized by high sand dunes of vivid pink-to-or ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vlaie
In the Hudson Valley of eastern United States, a vlaie, vly or fly is a swamp or marsh. It also applies to creeks and areas in the vicinities. The term appears in place names in areas of Dutch influence, formerly New Netherland. Etymology The terms are from a dialectal form of the Middle Dutch word ' ("valley", spelled ' in Modern Dutch). Unabridged : "from obsolete Dutch dialect (Hudson valley) ''vlei'', from Middle Dutch ''valeye''" However, the meaning shifted to "swamp" when used by New Netherlanders. Variants such as ''vley'' and ''vlei'' are also found. The English spelling of ''vleigh'' is probably under influence of rhymes like ''sleigh'' and ''weigh''. The Afrikaans word ' ("shallow lake") is a cognate, descended from the same Middle Dutch word. The ''Vlie'', a channel in Frisia, may not be related, as it is likely from the Latin '' Flevo''. Place names Examples of names of swamps, streams, lakes, and mountains which contain ''vlaie'' or other variant spellings: N ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Peninsula
The Cape Peninsula ( af, Kaapse Skiereiland) is a generally mountainous peninsula that juts out into the Atlantic Ocean at the south-western extremity of the African continent. At the southern end of the peninsula are Cape Point and the Cape of Good Hope. On the northern end is Table Mountain, overlooking Table Bay and the city bowl of Cape Town, South Africa. The peninsula is 52 km long from Mouille point in the north to Cape Point in the south. The Peninsula has been an island on and off for the past 5 million years, as sea levels fell and rose with the Glacial period, ice age and interglacial global warming cycles of, particularly, the Pleistocene. The last time that the Peninsula was an island was about 1.5 million years ago. Soon afterwards it was joined to the mainland by the Geology of Cape Town#Tertiary to Recent events, emergence from the sea of the sandy area now known as the Cape Flats. The towns and villages of the Cape Peninsula and Cape Flats, and the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Intermittent Lake
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Orothamnus
''Orothamnus'' (Greek 'oros' mountain, 'thamnos' bush) or marsh rose is a monotypic fynbos genus in the family Proteaceae occurring in the Kogelberg and Kleinrivier Mountains of Hottentots-Holland in the Western Cape Province of South Africa. It is an erect, sparsely branched shrub to 5 m tall and was first depicted by Jean Villet, a Capetonian artist and dealer in natural history specimens, in Curtis's Botanical Magazine 74: plate 4357 in 1848. ''Orothamnus zeyheri'' (after the botanist Karl Ludwig Philipp Zeyher) is extremely rare and endangered and appears on CITES Appendix I. The plants are short-lived, with an average lifespan of 10 years and a maximum of 20 years, and are readily killed by fire. The seeds, on the other hand, are long-lived and remain viable for over 35 years below ground, where they are deposited by ants, and paradoxically need summer fires to germinate. The pollinating agent is not known. Marsh Roses grow in peaty swamps and seeps at altitudes of 450â ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cognate
In historical linguistics, cognates or lexical cognates are sets of words in different languages that have been inherited in direct descent from an etymology, etymological ancestor in a proto-language, common parent language. Because language change can have radical effects on both the sound and the meaning of a word, cognates may not be obvious, and often it takes rigorous study of historical sources and the application of the comparative method to establish whether lexemes are cognate or not. Cognates are distinguished from Loanword, loanwords, where a word has been borrowed from another language. The term ''cognate'' derives from the Latin noun '':wikt:cognatus, cognatus blood relative'. Characteristics Cognates need not have the same meaning, which semantic drift, may have changed as the languages developed independently. For example English language, English ''wikt:starve#English, starve'' and Dutch language, Dutch ''wikt:sterven#Dutch, sterven'' 'to die' or German languag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Semantic Shift
Semantic change (also semantic shift, semantic progression, semantic development, or semantic drift) is a form of language change regarding the evolution of word usage—usually to the point that the modern meaning is radically different from the original usage. In diachronic (or historical) linguistics, semantic change is a change in one of the meanings of a word. Every word has a variety of senses and connotations, which can be added, removed, or altered over time, often to the extent that cognates across space and time have very different meanings. The study of semantic change can be seen as part of etymology, onomasiology, semasiology, and semantics. Examples in English * Awful — Literally "full of awe", originally meant "inspiring wonder (or fear)", hence "impressive". In contemporary usage, the word means "extremely bad". * Awesome — Literally "awe-inducing", originally meant "inspiring wonder (or fear)", hence "impressive". In contemporary usage, the word means "ext ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Middle Dutch
Middle Dutch is a collective name for a number of closely related West Germanic dialects whose ancestor was Old Dutch. It was spoken and written between 1150 and 1500. Until the advent of Modern Dutch after 1500 or c. 1550, there was no overarching standard language, but all dialects were mutually intelligible. During that period, a rich Medieval Dutch literature developed, which had not yet existed during Old Dutch. The various literary works of the time are often very readable for speakers of Modern Dutch since Dutch is a rather conservative language. Phonology Differences with Old Dutch Several phonological changes occurred leading up to the Middle Dutch period. * Earlier Old Dutch , , merge into already in Old Dutch. * Voiceless fricatives become voiced syllable-initially: > , > (merging with from Proto-Germanic ), > . (10th or 11th century) * > * > or . The outcome is dialect-specific, with found in more western dialects and further east. This results in later ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Afrikaans Language
Afrikaans (, ) is a West Germanic languages, West Germanic language that evolved in the Dutch Cape Colony from the Dutch dialects, Dutch vernacular of Holland, Holland proper (i.e., the Hollandic dialect) used by Dutch, French, and German settlers and Slavery in South Africa, their enslaved people. Afrikaans gradually began to develop distinguishing characteristics during the course of the 18th century. Now spoken in South Africa, Namibia and (to a lesser extent) Botswana, Zambia, and Zimbabwe, estimates circa 2010 of the total number of Afrikaans speakers range between 15 and 23 million. Most linguists consider Afrikaans to be a partly creole language. An estimated 90 to 95% of the vocabulary is of Dutch origin with adopted words from other languages including German language, German and the Khoisan languages of Southern Africa. Differences between Afrikaans and Dutch, Differences with Dutch include a more analytic language, analytic-type Morphology (linguistics), morphology ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
