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The Sturtian-Varangian is a late Precambrian world-wide glaciation episode ranging from 950Ma to 600Ma, represented by tillite deposits in Congo, Australia, China, North America, Sahara and Norway. Also known as the Cryogenian. Generally considered to be divisible into at least two (Sturtian around 800Ma and Minoan/Varanger 650Ma) or four significant glaciation extremes. The tillite deposits occurred also in what is believed to be low latitudes, which lead to the hypothesis of Snowball Earth

The population of acritarchs crashed during this glaciation and it is claimed that oxygen levels in the atmosphere increased after the glaciation. There are a number of enigmatic features with regard to this glaciation including indications of glaciation at very low latitudes and the presence of limestones -- normally warm water sediments above, below and intermixed with glacial deposits. Paleomagnetism seems to indicate very high continental drift rates leading some geologists to question whether some of the phenomena might be due to magnetic pole wandering rather than plate motion and low latitiude glaciation. Evidence of the glaciation is found in various places and times: The Congo River basin from 950-750Ma and 620-600Ma. Australia from 800-780Ma and 690-680Ma. China 800-760Ma, 740-700Ma and 600Ma; Western North America 850-800Ma, Sahara 730-650Ma, NorwayThe Kingdom of Norway is a Nordic country west of Sweden on the Scandinavian Peninsula. It has a very elongated form and has an extensive coastline along the North Atlantic Ocean, where Norway's famous fjords are found. In addition to Sweden, it borders R 650Ma. SpitsbergenSpitsbergen is the largest island in the Svalbard archipelago, which is situated in the Arctic Ocean and administered by Norway. The name Spitsbergen means Jagged Peaks and was given by the Dutch explorer Willem Barents, who discovered the island while se 593-573Ma.

Other known world wide glaciations include the Huronian from 2400Ma to 2100Ma, Andean-Saharan from 450-420Ma, the Karoo glaciation from 360Ma to 260Ma, and the CenozoicThe Cenozoic or Cainozoic Era (sometimes Caenozoic Era is the most recent of the four classic geological eras. It covers the 64 million years since the extinction event at the end of the Cretaceous that marked the demise of the last dinosaurs and the end glaciation which started 30Ma in AntarcticaAntarctica (from Greek nu;ταρκτικ&sigmaf opposed to the arctic) is a continent surrounding the Earth's South Pole. It is the coldest place on earth and is almost entirely covered by ice. It is not to be confused with the and are not over.

Geologic timescaleA timeline of geologic periods in accordance with the dates and nomenclature proposed by the International Commission on Stratigraphy. The Earth is thought by geologists to be 4. 6 billion years old. The geologic or "deep" time of Earth's past has been or

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