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Vema Trainingship , Greek daily newspaper
{{Disambiguation ...
Vema may refer to: * Prolaya Vema Reddy, the first king of the Reddy dynasty in Andhra Pradesh, India * A Greek pace (unit of length) * Research Vessel Vema, a research ship of the Lamont–Doherty Earth Observatory used by J. Lamar Worzel and Marie Tharp, and some ocean phenomena discovered using it: ** Vema (mollusc), a genus of monoplacophoran molluscs ** The Vema Seamount, a seamount in the South Atlantic Ocean at 31°38' S 8°20' E. ** The Vema hotspot, a hotspot (geology) ** The Vema Fracture Zone a fracture zone in the equatorial Atlantic Ocean See also * To Vima ''To Vima'' ( el, Το Βήμα, lit=The Tribune) is a Greek weekly newspaper first published in 1922 by Dimitris Lambrakis, the father of Christos Lambrakis, as ''Elefthero Vima'' (Free Tribune). It was owned by Lambrakis Press Group (DOL), a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prolaya Vema Reddy
The Reddi kingdom or Kondavidu Reddi kingdom (1325–1448 CE) was established in southern India by Prolaya Vema Reddi. Most of the region that was ruled by the Reddi dynasty is now part of modern-day coastal and central Andhra Pradesh. Origin The fall of the Kakatiya Kingdom in 1323, after being subject to seizes by the Tughlaq dynasty, led to a political vacuum in the Andhras.The Islamic conquerors failed to keep the region under effective control and constant infighting among themselves coupled with the martial abilities of the local Telugu warriors led to the loss of the entire region by 1347. Whilst, this led to the rise of the Musunuris (initially were based in Coastal Andhra) and Recharlas in the Telangana region, the coastal belt saw the rise of a third warrior lineage—the Reddi''s'' of the Panta clan. Established in about 1325 by Prolaya Vema Reddi,(also known as Komati Vema), his territory extended along the coast to Nellore in the south and Srisailam, in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reddy Dynasty
The Reddi kingdom or Kondavidu Reddi kingdom (1325–1448 CE) was established in southern India by Prolaya Vema Reddi. Most of the region that was ruled by the Reddi dynasty is now part of modern-day coastal and central Andhra Pradesh. Origin The fall of the Kakatiya Kingdom in 1323, after being subject to seizes by the Tughlaq dynasty, led to a political vacuum in the Andhras.The Islamic conquerors failed to keep the region under effective control and constant infighting among themselves coupled with the martial abilities of the local Telugu warriors led to the loss of the entire region by 1347. Whilst, this led to the rise of the Musunuris (initially were based in Coastal Andhra) and Recharlas in the Telangana region, the coastal belt saw the rise of a third warrior lineage—the Reddi''s'' of the Panta clan. Established in about 1325 by Prolaya Vema Reddi,(also known as Komati Vema), his territory extended along the coast to Nellore in the south and Srisailam, in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andhra Pradesh
Andhra Pradesh (, abbr. AP) is a state in the south-eastern coastal region of India. It is the seventh-largest state by area covering an area of and tenth-most populous state with 49,386,799 inhabitants. It is bordered by Telangana to the north-west, Chhattisgarh to the north, Odisha to the north-east, Tamil Nadu to the south, Karnataka to the west and the Bay of Bengal to the east. It has the second longest coastline in India after Gujarat, of about . Andhra State was the first state to be formed on a linguistic basis in India on 1 October 1953. On 1 November 1956, Andhra State was merged with the Telugu-speaking areas (ten districts) of the Hyderabad State to form United Andhra Pradesh. ln 2014 these merged areas of Hyderabad State are bifurcated from United Andhra Pradesh to form new state Telangana . Present form of Andhra similar to Andhra state.but some mandalas like Bhadrachalam still with Telangana. Visakhapatnam, Guntur, Kurnool is People Capital of And ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
India
India, officially the Republic of India (Hindi: ), is a country in South Asia. It is the seventh-largest country by area, the second-most populous country, and the most populous democracy in the world. Bounded by the Indian Ocean on the south, the Arabian Sea on the southwest, and the Bay of Bengal on the southeast, it shares land borders with Pakistan to the west; China, Nepal, and Bhutan to the north; and Bangladesh and Myanmar to the east. In the Indian Ocean, India is in the vicinity of Sri Lanka and the Maldives; its Andaman and Nicobar Islands share a maritime border with Thailand, Myanmar, and Indonesia. Modern humans arrived on the Indian subcontinent from Africa no later than 55,000 years ago., "Y-Chromosome and Mt-DNA data support the colonization of South Asia by modern humans originating in Africa. ... Coalescence dates for most non-European populations average to between 73–55 ka.", "Modern human beings—''Homo sapiens''—originated in Africa. Then, int ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pace (unit Of Length)
A pace is a unit of length consisting either of one normal walking step (approximately ), or of a double step, returning to the same foot (approximately ). The normal pace length decreases with age and some health conditions. The word "pace" is also used for units inverse to speed, used mainly for walking and running, commonly ''minutes per kilometer''. The word "pace" is also used to translate similar formal units in other systems of measurement. Pacing is also used as an informal measure in surveying, with the "pace" equal to two of the surveyor's steps reckoned through comparison with a standard rod or chain. Standardized units Like other traditional measurements, the pace started as an informal unit of length, but was later standardized, often with the specific length set according to a typical brisk or military marching stride. In the United States the pace is an uncommon customary unit of length denoting a brisk single step and equal to .''U.S. Army Map Reading and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Research Vessel Vema
The SV ''Mandalay'' is a three-masted schooner measuring pp, with a wrought iron hull. It was built as the private yacht ''Hussar (IV)'', and would later become the research vessel ''Vema'', one of the world's most productive oceanographic research vessels. The ship currently sails as the cruising yacht ''Mandalay'' in the Caribbean. E.F. Hutton's luxury yacht, ''Hussar IV'' ''Hussar'' (IV) was designed by Cox & Stevens and built in 1923 by Burmeister & Wain in Copenhagen for E. F. Hutton and his wife Marjorie Merriweather Post. The 585-ton luxury yacht had an iron-hull and represented the epitome of maritime luxury and glamour in her class. Interiors were designed by William Baumgarten & Co of New York, the first American firm to do the interior decoration of a ship abroad. Upon her completion in Denmark King Christian X was invited to inspect the ship prior to its maiden crossing to New York. It was one of the fastest yachts, breaking the transatlantic record in 10 days, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lamont–Doherty Earth Observatory
The Lamont–Doherty Earth Observatory (LDEO) is the scientific research center of the Columbia Climate School, and a unit of The Earth Institute at Columbia University. It focuses on climate and earth sciences and is located on a 189-acre (64 ha) campus in Palisades, New York, north of Manhattan on the Hudson River. History The Lamont–Doherty Earth Observatory (LDEO) was established in 1949 as the Lamont Geological Observatory on the weekend estate of Thomas W. and Florence Haskell Corliss Lamont, which was donated to the university for that purpose. The Observatory's founder and first director was Maurice "Doc" Ewing, a seismologist who is credited with advancing efforts to study the solid Earth, particularly in areas related to using sound waves to image rock and sediments beneath the ocean floor. He was also the first to collect sediment core samples from the bottom of the ocean, a common practice today that helps scientists study changes in the planet's climate and th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marie Tharp
Marie Tharp (July 30, 1920 – August 23, 2006) was an American geologist and oceanographic cartographer. In the 1950s, she collaborated with geologist Bruce Heezen to produce the first scientific map of the Atlantic Ocean floor. Her cartography revealed a more detailed topography and multi-dimensional geographical landscape of the ocean bottom. Tharp's discovery of the Mid-Atlantic Ridge caused a paradigm shift in earth science that led to acceptance of the theories of plate tectonics and continental drift.Lamont–Doherty Earth Observatory Bestows Heritage Award on Marie Tharp, Pioneer of Modern Oceanography Published Jul 10, 2001, Retrieved Oct 12, 2014 Early life and education Marie Tharp was born on Jul ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vema (mollusc)
''Vema'' is a genus of deep-sea molluscs, monoplacophora Monoplacophora , meaning "bearing one plate", is a polyphyletic superclass of molluscs with a cap-like shell inhabiting deep sea environments . Extant representatives were not recognized as such until 1952; previously they were known only from ...ns. The genus is named after the oceanographic Research Vessel ''Vema''. All ''Vema'' species have six pairs of gills. Species * '' Vema bacescui'' (Menzies, 1968) * '' Vema ewingi'' (Clarke & Menzies, 1959) * '' Vema levinae'' Warén, 1996 * '' Vema occidua'' B. A. Marshall, 2006 References Monoplacophora Mollusc genera {{Mollusc-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vema Seamount
Vema Seamount is a seamount in the South Atlantic Ocean. Discovered in 1959 by a ship with the same name, it lies from Tristan da Cunha and northwest of Cape Town. The seamount has a flat top at a mean depth of which was eroded into the seamount at a time when sea levels were lower; the shallowest point lies at depth. The seamount was formed between 15-11 million years ago, possibly by a hotspot. The seamount rises high enough that its summit is at shallow depth, allowing sunlight to reach it and thus permitting the growth of kelp and algae. A number of sea animals and fish are encountered on the seamount; active fisheries existed at Vema Seamount and caused the disappearance of some animal species. History Vema Seamount was discovered by the research ship RV Vema of the Lamont–Doherty Earth Observatory in 1959. Vema is one of the first seamounts to be the subject of scientific study, and the first seamount investigated by scuba divers without special equipment. Vema li ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Seamount
A seamount is a large geologic landform that rises from the ocean floor that does not reach to the water's surface (sea level), and thus is not an island, islet or cliff-rock. Seamounts are typically formed from extinct volcanoes that rise abruptly and are usually found rising from the seafloor to in height. They are defined by oceanographers as independent features that rise to at least above the seafloor, characteristically of conical form.IHO, 2008. Standardization of Undersea Feature Names: Guidelines Proposal form Terminology, 4th ed. International Hydrographic Organization and Intergovernmental Oceanographic Commission, Monaco. The peaks are often found hundreds to thousands of meters below the surface, and are therefore considered to be within the deep sea. During their evolution over geologic time, the largest seamounts may reach the sea surface where wave action erodes the summit to form a flat surface. After they have subsided and sunk below the sea surface such flat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vema Hotspot
Vema Seamount is a seamount in the South Atlantic Ocean. Discovered in 1959 by a ship with the same name, it lies from Tristan da Cunha and northwest of Cape Town. The seamount has a flat top at a mean depth of which was eroded into the seamount at a time when sea levels were lower; the shallowest point lies at depth. The seamount was formed between 15-11 million years ago, possibly by a hotspot. The seamount rises high enough that its summit is at shallow depth, allowing sunlight to reach it and thus permitting the growth of kelp and algae. A number of sea animals and fish are encountered on the seamount; active fisheries existed at Vema Seamount and caused the disappearance of some animal species. History Vema Seamount was discovered by the research ship RV Vema of the Lamont–Doherty Earth Observatory in 1959. Vema is one of the first seamounts to be the subject of scientific study, and the first seamount investigated by scuba divers without special equipment. Vema li ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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