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・ Geology of solar terrestrial planets
・ Geology of Somerset
・ Geology of South Australia
・ Geology of South Wales
・ Geology of southern North Sea
・ Geology of Suffolk
・ Geology of Sumatra Trench
・ Geology of Svalbard
・ Geology of Taiwan
・ Geology of Taranaki
・ Geology of Tasmania
・ Geology of Tennessee
・ Geology of Texas
・ Geology of the Alps
・ Geology of the Antarctic Peninsula
Geology of the Appalachians
・ Geology of the Auckland Region
・ Geology of the Australian Capital Territory
・ Geology of the Baltic Sea
・ Geology of the Bryce Canyon area
・ Geology of the Canyonlands area
・ Geology of the Capitol Reef area
・ Geology of the Dallas–Fort Worth Metroplex
・ Geology of the Death Valley area
・ Geology of the English counties
・ Geology of the Falkland Islands
・ Geology of the Faroe Islands
・ Geology of the Grand Canyon area
・ Geology of the Grand Teton area
・ Geology of the Himalaya


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Geology of the Appalachians : ウィキペディア英語版
Geology of the Appalachians

The geology of the Appalachians dates back to more than 480 million years ago. A look at rocks exposed in today's Appalachian Mountains reveals elongate belts of folded and thrust faulted marine sedimentary rocks, volcanic rocks and slivers of ancient ocean floor - strong evidence that these rocks were deformed during plate collision. The birth of the Appalachian ranges marks the first of several mountain building plate collisions that culminated in the construction of the supercontinent Pangaea with the Appalachians and neighboring Little Atlas (now in Morocco) near the center. These mountain ranges likely once reached elevations similar to those of the Alps and the Rocky Mountains before they were eroded.〔(【引用サイトリンク】url=http://geology.er.usgs.gov/eespteam/Mtleconte/website/geology.html?etoc )
==Geological history==


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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