The Last Ice Age in Europe

www.stb806.de The last glacial period occurred from the period c. 115,000 – c. 11,700 years ago. Erratic boulders, till, drumlins, eskers, fjords, kettle lakes, moraines, etc., are typical features left behind by glaciers which make it possible to reconstruct the ice coverage during the last Ice Age. Many of today’s countries were entirely covered by thick ice sheets for thousands of years. These countries include Iceland, Ireland, Norway, Sweden, Finland, Estonia, Latvia, and Lithuania. The big Scandinavian and British ice sheet extended south as far as northern Poland and Germany while also covering almost all of Denmark. At the same time in the eastern regions, the ice spread into the territory of Russia (about 300km west from Moscow) and some northern parts of Belarus. In the west, ice covered almost the entire British Isles, leaving just a relatively small ice-free zone in the south of the United Kingdom. Today, about three-quarters of all the world’s freshwater (14,9 million km2) is stored in glaciers, while during the last Ice Age it was about 3 times more (44,4 Million km2).

www.deviantart.com The source populations of Paleolithic humans survived the last glacial period in sparsely wooded areas and dispersed through areas of high primary productivity while avoiding dense forest cover.

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Find cities with similar climate

This map has been created using The Global environmental stratification. The Global environmental stratification (GEnS), based on statistical clustering of bioclimate data (WorldClim). GEnS, consists of 125 strata, which have been aggregated into 18 global environmental zones (labeled A to R) based on the dendrogram. Interactive map >> Via www.vividmaps.com Related posts: - Find cities with similar climate 2050 - How global warming will impact 6000+ cities around the world?

The Appalachian Mountains, the Scottish Highlands, and the Atlas Mounts in Africa were the same mountain range

The Central Pangean Mountains was a prominent mountain ridge in the central part of the supercontinent Pangaea that extends across the continent from northeast to southwest through the Carboniferous , Permian Triassic periods. The mountains were formed due to a collision within the supercontinents Gondwana and Laurussia during the creation of Pangaea. It was comparable to the present Himalayas at its highest peak during the start of the Permian period. It isn’t easy to assume now that once upon a time that the Scottish Highlands, The Appalachian Mountains, the Ouachita Mountain Range, and the Atlas Mountains in northwestern Africa are the same mountains , once connected as the Central Pangean Mountains.

Moose population in North America

The moose population in North America is shrinking swiftly. This decrease has been correlated to the opening of roadways and landscapes into this animal's north range. In North America, the moose range includes almost all of Canada and Alaska, the northern part of New England and New York, the upper Rocky Mountains, northern Minnesota and Wisconsin, Michigan's Upper Peninsula, and Isle Royale. In 2014-2015, the North American moose population was measured at around one million animals. The most abundant moose population (about 700,000) lives in Canada. About 300 000 moose remains in nineteen U.S. states Alaska, Colorado, Connecticut, Idaho, Maine, Massachusetts, Minnesota, Montana, Michigan, Nevada, New Hampshire, New York, North Dakota, Oregon, Utah, Vermont, Washington, Wisconsin, and Wyoming. The largest moose specimens are found in Alaska 200 thousand moose. Below the map shows the size of US states scaled by the moose population. Via www.vividmaps.com

Ecoclimax

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