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Map of "Europe" in the early Oligocene, some 30 million years ago. The formation of Europe as a coherent landmass dates to after the breakup of Pangaea , taking place during the Oligocene and completed by the early Neogene period, some 20 million years ago.
The final major cold spell occurred from 25,000 to 18,000 years ago and is known as the Last Glacial Maximum when the Fenno-Scandinavian ice sheet covered much of northern Europe while the Alpine ice sheet occupied significant parts of central-southern Europe. However, there were several less cold periods after this.
This is a list of named geological features on Europa, a moon of the planet Jupiter. Craters and lineae are listed on separate pages: list of craters on Europa and list of lineae on Europa . Cavi
Satellite image of Europe by night 1916 physical map of Europe Topography of Europe. Some geographical texts refer to a Eurasian continent given that Europe is not surrounded by sea and its southeastern border has always been variously defined for centuries. In terms of shape, Europe is a collection of connected peninsulas and nearby
The European Plain or the Great European Plain is a plain in Europe and is a major feature of one of four major topographical units of Europe – the Central and Interior Lowlands. [1] It is the largest mountain -free landform in Europe, although a number of highlands are identified within it.
Modern humans ventured into northern Europe under extremely cold climate conditions and were living side by side with Neanderthals more than 45,000 years ago, according to new evidence.
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The research identified Roman ancestry in individuals from southern Germany, Italy, Poland, Slovakia, and southern Britain, with one person in southern Europe exhibiting 100 per cent Scandinavian ...