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Constructive Forces of Mountain Building
Constructive Forces of Mountain Building

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... Run from Canada to Alabama down the east coast. Oldest mountains in the US. The area east of the Appalachian Mountains is called the Piedmont, and it is good farming soil. ...
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... B. Answer the following: 1. When did the formation of the Appalachians begin? 2. When did the plate movements reverse in forming the Appalachians? 3. According to Figure 20-11, when did the fragment that was to become the Blue Ridge Province attached to N. America? 4. According to Figure 20-11, what ...
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Appalachian Mountains



The Appalachian Mountains (/ˌæpəˈleɪʃɨn/ or /ˌæpəˈlætʃɨn/, French: les Appalaches), often called the Appalachians, are a system of mountains in eastern North America. The Appalachians first formed roughly 480 million years ago during the Ordovician Period and once reached elevations similar to those of the Alps and the Rocky Mountains before they were eroded. The Appalachian chain is a barrier to east-west travel as it forms a series of alternating ridgelines and valleys oriented in opposition to any road running east-west.Definitions vary on the precise boundaries of the Appalachians. The United States Geological Survey (USGS) defines the Appalachian Highlands physiographic division as consisting of thirteen provinces: the Atlantic Coast Uplands, Eastern Newfoundland Atlantic, Maritime Acadian Highlands, Maritime Plain, Notre Dame and Mégantic Mountains, Western Newfoundland Mountains, Piedmont, Blue Ridge, Valley and Ridge, Saint Lawrence Valley, Appalachian Plateaus, New England province, and the Adirondack provinces. A common variant definition does not include the Adirondack Mountains, which geologically belong to the Grenville Orogeny and have a different geological history from the rest of the Appalachians.
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