who was the first person who cover the south pole very first?
469767
The question doesnt make sense to me but the first person to reach the south pole was Roald Amundsen on the 14th December 1911.
180782
July 20, 1969...Neil Armstrong was first, Buzz Aldrin second.
1048421
The scientist who first discovered the microbial life was Antony Van Leeuwenhoek". He is called as the Father of Microbiology.
338303
An American man, Erik Weihenmayer, has become the first blind man to successfully reach the summit of Mount Everest. The following links will take you to websites with more information concerning this incredible story. If the google search is available to you simply type in his name and Mount Everest and it will give you many more websites to research.\n\nMommaToldMe...to reach for the sky.
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Uranus, the first planet discovered in modern times, was discovered by William Herschel while systematically searching the sky with his telescope on March 13, 1781. It had actually been seen many times before but ignored as simply another star (the earliest recorded sighting was in 1690 when John Flamsteed cataloged it as 34 Tauri). Herschel named it "the Georgium Sidus" (the Georgian Planet) in honor of his patron, the infamous (to Americans) King George III of England; others called it "Herschel". The name "Uranus" was first proposed by Bode in conformity with the other planetary names from classical mythology but didn't come into common use until 1850. \n\nGo to the site below.  It has all kinds of info, even on all of the moons.  I hope this helps :)
1159847
pole\nmagnetic pole, the two nearly opposite ends of the planet where the earth's magnetic intensity is the greatest, as the north and south magnetic poles. For the magnetic north, it is the direction from any point on the earth's surface linking the horizontal component of the magnetic lines of force with the observer and north magnetic pole; it is similar for magnetic south. The north magnetic pole, first located (1831) by English explorer Sir James C. Ross, is now about 78°N and 104°W in the Queen Elizabeth Islands of northern Canada. The south magnetic pole, reached (1909) by English geologists Sir T. W. E. David and Sir Douglas Mawson, is now about 66°S and 139°E on the Adélie Coast of Antarctica. The magnetic poles are not fixed but follow circular paths with diameters of about 100 miles (160 km). Studies of paleomagnetism also indicate that the earth's magnetic field has reversed its polarity many times in the geologic past. The best hypothesis to date for the origin of terrestrial magnetism is the self-exciting dynamo theory, where the earth's magnetic field is generated by the interaction of motion and electrical currents in the earth's liquid outer core.\n\n///\nMagnetic fields are produced by the motion of electrical charges. For example, the magnetic field of a bar magnet results from the motion of negatively charged electrons in the magnet. The origin of the Earth's magnetic field is not completely understood, but is thought to be associated with electrical currents produced by the coupling of convective effects and rotation in the spinning liquid metallic outer core of iron and nickel. This mechanism is termed the dynamo effect. \nRocks that are formed from the molten state contain indicators of the magnetic field at the time of their solidification. The study of such "magnetic fossils" indicates that the Earth's magnetic field reverses itself every million years or so (the north and south magnetic poles switch). This is but one detail of the magnetic field that is not well understood\n\n....\nIn order to explain the fact that ferromagnetic materials with spontaneous magnetisation could exist in the demagnetised state Weiss proposed the concept of magnetic domains. Weiss built on earlier work carried out by Ampère, Weber and Ewing suggesting their existence. The findings of this work revealed that within a domain large numbers of atomic moments are aligned  typically 1012-1018, over a much larger volume than was previously suspected. The magnetisation within the domain is saturated and will always lie in the easy direction of magnetisation when there is no externally applied field. The direction of the domain alignment across a large volume of material is more or less random and hence the magnetisation of a specimen can be zero.\n\nMagnetic domains exist in order to reduce the energy of the system. A uniformly magnetised specimen as shown in figure 5(a) has a large magnetostatic energy associated with it. This is the result of the presence of magnetic free poles at the surface of the specimen generating a demagnetising field, Hd. From the convention adopted for the definition of the magnetic moment for a magnetic dipole the magnetisation within the specimen points from the south pole to the north pole, while the direction of the magnetic field points from north to south. Therefore, the demagnetising field is in opposition to the magnetisation of the specimen. The magnitude of Hd is dependent on the geometry and magnetisation of the specimen. In general if the sample has a high length to diameter ratio (and is magnetised in the long axis) then the demagnetising field and the magnetostatic energy will be low.\n\nThe break up of the magnetisation into two domains as illustrated in figure 5(b) reduces the magnetostatic energy by half. In fact if the magnet breaks down into N domains then the magnetostatic energy is reduced by a factor of 1/N, hence figure 5(c) has a quarter
195557
It came from Captain George Vancouver of the British navy who surveyed the area in the early 1790's. He had earlier been a midshipman on board HMS Endeavour when Captain James Cook sailed up the West Coast of Canada.
452384
African-American Matthew A. Henson accompanied polar explorer Robert E. Peary on a U.S. expedition to the North Pole on April 6, 1909. In 2000,\n\nsource: http://news.nationalgeographic.com/news/2003/01/0110_030113_henson.html\n\nFollow the footsteps of the great explorers, Robert E. Peary\nsource: http://www.bbc.co.uk/northpole2001/explorers.shtml
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He was the first to come up with a good system of classifying all life on earth. His system, with variations, is still in wide use today. \n\nVery Important Person to scientists!
516963
he went to the south pole and i think its Byrd
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YURI GAGARIN WAS THE FIRST  MAN IN THE SPACE! OF COURSE I KNOW THIS, THAT'S BECAUSE I'M RUSSIAN.\n\n: )
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Antarctica\n\n Geography: Antarctica is the icy continent at the South Pole. It is covered by permafrost (permanently frozen ground), is surrounded by water, and is about 1 1/2 times larger than the United States. The world's largest desert is on Antarctica. 98 percent of the land is covered with a continental ice sheet; the remaining 2 percent of land is barren rock. Antarctica has about 87% of the world's ice. \nClimate: The South Pole is the coldest, windiest, and driest place on Earth. The coldest temperature ever recorded on Earth was at the South Pole; it reached -128.6°F (-88.0°C)! On average, most of Antarctica gets less than 2 inches of snow fall each year. \nPeople: Although scientific expeditions visit Antarctica, there are no permanent human residents (because of the extreme weather, which includes freezing temperatures, strong winds, and blizzards). There are about 4,000 seasonal visitors to Antarctica. \nLocation: Antarctica hasn't always been located at the South Pole. It has drifted, like the other continents, and has ranged from the equator (during the Cambrian period, about 500 million years ago) to the South Pole. During the time of the dinosaurs (the Mesozoic Era, about 65 million to 248 million years ago), Antarctica was more temperate and housed dinosaurs and many other life forms. Now, there is very little indigenous life.
181298
Jaques Cartier was the first... I don't remember the others, there was also Samuel De Champlain... and the others was some misionairy like Père Marquette... lol I should listen more in history class I learn this this year... well hope you are satisfied by the answer^^
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White.  You're at the South Pole.\n\nYawn.
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On April 12, 1961 Soviet cosmonaut Yuri Gagarin is the first person to orbit Earth. His flight in Vostok 1 lasts less than 2 hr.
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1953: First Summit: May 29, 1953: Tenzing Norgay & Sir Edmund Percival Hillary (New Zealand) via the South-East Ridge Route. (Western Cwn, Lhotse face to the South-East ridge.)
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Sputnik 1957\nhttp://en.wikipedia.org/wiki/Satellite#The_first_artificial_satellite