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    The portion west of the Weddell Sea and east of the Ross Sea is called West Antarctica and the remainder East Antarctica, because they roughly correspond to the Western and Eastern Hemispheres relative to the Greenwich meridian. In the dry valleysthe same effect occurs over a rock base, leading to a desiccated landscape. The sheet has been of recent concern because of the real, if small, possibility of its collapse. If the sheet were to break down, ocean levels would rise by several metres in a relatively geologically short period of time, perhaps a matter of centuries.

    Antarctica contains many other mountainson both the main continent and the surrounding islands.

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    Mount Erebus on Ross Island is the world's southernmost active volcano. Another well-known volcano is found on Deception Islandwhich is famous for a giant eruption in Minor eruptions are frequent and lava flow has been observed in recent years. Other dormant volcanoes may potentially be active. Lake Vostokdiscovered beneath Russia's Vostok Station inis the largest of these subglacial lakes. It was once believed that the lake had been sealed off forto one million years but a recent survey suggests that, every so often, there are large flows of water from one lake to another.

    The frozen surface of the lake shares similarities with Jupiter 's moon, Europa. If life is discovered in Lake Vostok, it would strengthen the argument for the possibility of life on Europa. If found, these resilient creatures could further bolster the argument for extraterrestrial life in extremely cold, methane-rich environments.

    Geology of Antarctica Subglacial topography and bathymetry of bedrock underlying Antarctica ice sheet The above map shows the subglacial topography of Antarctica.

    As indicated by the scale on left-hand side, blue represents portion of Antarctica lying below sea level. The other colours indicate Antarctic bedrock lying above sea level. Map is not corrected for sea level rise or isostatic reboundwhich would occur if the Antarctic ice sheet completely melted to expose the bedrock surface. Topographic map of Antarctica after removing the ice sheet and accounting for both isostatic rebound and sea level rise. Hence, this map suggests what Antarctica may have looked like 35 million years ago, when the Earth was warm enough to prevent the formation of large-scale ice sheets in Antarctica.

    Antarctica was not always cold, dry, and covered in ice sheets. At a number of points in its long history, it was farther north, experienced a tropical or temperate climate, was covered in forests, and inhabited by various ancient life forms. Palaeozoic era — Ma During the Cambrian periodGondwana had a mild climate. West Antarctica was partially in the Northern Hemisphereand during this period large amounts of sandstoneslimestones and shales were deposited.

    East Antarctica was at the equator, where sea floor invertebrates and trilobites flourished in the tropical seas. Sand and silts were laid down in what is now the EllsworthHorlick and Pensacola Mountains. During the Permian period, the land became dominated by seed plants such as Glossopterisa pteridosperm which grew in swamps.

    Over time these swamps became deposits of coal in the Transantarctic Mountains. Towards the end of the Permian period, continued warming led to a dry, hot climate over much of Gondwana. In Eastern Antarctica, seed ferns or pteridosperms became abundant and large amounts of sandstone and shale were laid down at this time.

    Synapsidscommonly known as "mammal-like reptiles", were common in Antarctica during the Early Triassic and included forms such as Lystrosaurus. Ginkgo trees, conifers, bennettites, horsetails, ferns and cycads were plentiful during this period. Ammonites were common in the seas around Antarctica, and dinosaurs were also present, though only three Antarctic dinosaur genera Cryolophosaurus and Glacialisaurusfrom the Hanson Formation[53] and Antarctopelta have been described to date.

    However, there is some evidence of antarctic marine glaciation during the Cretaceous period. Models of the changes suggest that declining CO2 levels became more important. This sediment uplift was accompanied by igneous intrusions and volcanism. The most common rocks in West Antarctica are andesite and rhyolite volcanics formed during the Jurassic period.

    There is also evidence of volcanic activity, even after the ice sheet had formed, in Marie Byrd Land and Alexander Island. The only anomalous area of West Antarctica is the Ellsworth Mountains region, where the stratigraphy is more similar to East Antarctica.

    It is composed of a metamorphic and igneous platform which is the basis of the continental shield. On top of this base are coal and various modern rocks, such as sandstoneslimestones and shales laid down during the Devonian and Jurassic periods to form the Transantarctic Mountains. In coastal areas such as Shackleton Range and Victoria Land some faulting has occurred. The main mineral resource known on the continent is coal.

    The Prince Charles Mountains contain significant deposits of iron ore. The most valuable resources of Antarctica lie offshore, namely the oil and natural gas fields found in the Ross Sea in Exploitation of all mineral resources is banned until by the Protocol on Environmental Protection to the Antarctic Treaty. Climate The blue ice covering Lake Fryxellin the Transantarctic Mountainscomes from glacial meltwater from the Canada Glacier and other smaller glaciers.

    Near the coast, December looks fairly temperate. Antarctica is the coldest of Earth 's continents. It used to be ice-free until about 34 million years ago, when it became covered with ice. Sunburn is often a health issue as the snow surface reflects almost all of the ultraviolet light falling on it.

    Given the latitude, long periods of constant darkness or constant sunlight create climates unfamiliar to human beings in much of the rest of the world. East Antarctica is colder than its western counterpart because of its higher elevation.

    Weather fronts rarely penetrate far into the continent, leaving the centre cold and dry. Despite the lack of precipitation over the central portion of the continent, ice there lasts for extended periods. Heavy snowfalls are common on the coastal portion of the continent, where snowfalls of up to 1.

    At the edge of the continent, strong katabatic winds off the polar plateau often blow at storm force. In the interior, wind speeds are typically moderate. During clear days in summer, more solar radiation reaches the surface at the South Pole than at the equator because of the 24 hours of sunlight each day at the Pole.

    Second, the Arctic Ocean covers the north polar zone: Third, the Earth is at aphelion in July i. The orbital distance contributes to a colder Antarctic winter and a warmer Antarctic summer but the first two effects have more impact. Another unique spectacle is diamond dusta ground-level cloud composed of tiny ice crystals.

    It generally forms under otherwise clear or nearly clear skies, so people sometimes also refer to it as clear-sky precipitation. A sun doga frequent atmospheric optical phenomenonis a bright "spot" beside the true sun. The number of people conducting and supporting scientific research and other work on the continent and its nearby islands varies from about 1, in winter to about 5, in the summer, giving it a population density between 70 and inhabitants per million square kilometres and per million square miles at these times.

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    Many of the stations are staffed year-round, the winter-over personnel typically arriving from their home countries for a one-year assignment. An Orthodox church — Trinity Churchopened in at the Russian Bellingshausen Station —is manned year-round by one or two priests, who are similarly rotated every year. During the whaling era, which lasted untilthe population of that island varied from over 1, in the summer over 2, in some years to some in the winter. Most of the whalers were Norwegian, with an increasing proportion of Britons.

    Managers and other senior officers of the whaling stations often lived together with their families. Among them was the founder of Grytviken, Captain Carl Anton Larsena prominent Norwegian whaler and explorer who, along with his family, adopted British citizenship in She was a daughter of Fridthjof Jacobsen, the assistant manager of the whaling station, and Klara Olette Jacobsen. Jacobsen arrived on the island in and became the manager of Grytviken, serving from to ; two of his children were born on the island.

    Several bases are now home to families with children attending schools at the station.
    Dan Andrews Some of the most lively discussions in our forum revolve around re-location to different places across Southeast Asia. Last week an entrepreneur in Thailand asked: Why are so many of you guys are down there — what am I missing?

    I could go on forever about this. There is no question that bandwidth in much of Thailand is profoundly better. If internet speed is a priority for you and your business, consider this speedtest I ran from my couch in Bali as I wrote this: So why would people give up all that Thailand has to offer plus fast internet to live in the Philippines or Bali? Here are some guesses. Thailand is famous for having many young women that would like to find a nice western guy to settle down with.

    Now amplify that phenomenon by 10x. Welcome to the Philippines. Most people you encounter in the Philippines will understand and speak English at a conversational level. That said, you can hang out for 2 years without leaving the country. Try that in Thailand! Cheers, Dan PS, if you like this post you can hear directly from me by putting your email address in to the form below.

    Just on the Phone calls — without knowing how theyd work in your area. There are some great SIP phones with addon codec for slower speeds. I dont make phone calls through skype. The call quality is crap for anything but skype to skype. You can also use Viber App for ipad quite well, I spoke between Philippines and a guy in Nepal and the voice quality was crystal clear.

    Hans Can you tell me a little about the cost. Of living in VN? I will not need employment but after awhile I may want to open a business or teach conversational English. Being from Florida, I am quite familiar with it. I was thinking Greece since the collapse of its economy or more remote parts of New Zealand could be experienced long-term on the cheap. Wilster Guys Malaysia is a big place, go to the tax free havens like Labuan island and Langkawi and alcohol is very cheap.

    Labuan is a fun place to base actually and there are a few good business opportunities on offer. Langkawi is a great place to base if you are interested in yachting, and Thailand is on your doorstep. Sayong that I do find that Malaysia is a bit too boring and straight for my liking, i have always preferred Thailand, Indo or PI.

    Just stumbled across this page and find it quite interesting. Especially this article and the comments! Man I love the people over there and the attitude of most of them well of those I met of course. Looking forward to checking out Malaysia shortly… David Just stumbled across this page and liking:

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