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Glacial erratic boulders of Estonia
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・ Glacial erratic boulders of King County, Washington
・ Glacial erratic boulders of Kitsap County, Washington
・ Glacial erratic boulders of Snohomish County, Washington
・ Glacial erratic boulders of the Puget Sound region
・ Glacial erratics on and around Rügen
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Glacial erratic boulders of Estonia : ウィキペディア英語版
Glacial erratic boulders of Estonia

Glacial erratic boulders of Estonia are large boulders of rock which have been formed and moved into Estonia by glacial action during previous ice ages. Before the takeover of Estonia by the Soviet Union, these large boulders were a symbol of national identity. They are now registered and protected by the Estonian government.
These boulders are found in especially large quantities in Estonia. Most of the boulders greater than in circumference found in northern Europe are in Estonia. There are 62 known boulders of this size in Estonia. Some particular large ones have been found in the sea, including some near Osmussaar that are diameter. The Osmussaar boulders are believed to have been pushed there by glaciers from the Neugrund meteorite crater.〔Anto Raukos, "Evolution of the theory of continental glaciation in northern and eastern Europe" in R. H. Grapes, D. R. Oldroyd, A. Grigelis (eds), ''History of Geomorphology and Quaternary Geology'', pp. 79-86, Geological Society of London, 2008 ISBN 1862392552.〕
The Estonian boulders were important in the development of the idea that northern Europe was once covered in glaciers. The first to suggest that the boulders were moved by glaciers was Russian mineralogist Vasily Severgin who was led to this conclusion by their similarity to Finnish basement rock at the very early date of 1815. However, Severgin was later to retract this theory in favour of the drift theory of Charles Lyell who believed they had been carried by icebergs. However, in the following years of the 19th century the glaciation theory slowly gained the ascendancy.〔
==List of boulders==


抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)
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