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  2. Geology of the Appalachians - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Appalachians

    Overview. The Appalachian Mountains formed through a series of mountain-building events over the last 1.2 billion years: [4][5] The Grenville orogeny began 1250 million years ago (Ma) and lasted for 270 million years. The Taconic orogeny began 450 Ma and lasted for 10 million years. The Acadian orogeny began 375 Ma and lasted 50 million years.

  3. Museum of Appalachia - Wikipedia

    en.wikipedia.org/wiki/Museum_of_Appalachia

    Museum of Appalachia. The Museum of Appalachia, located in Norris, Tennessee, 20 miles (32 km) north of Knoxville, is a living history museum that interprets the pioneer and early 20th-century period of the Southern Appalachian region of the United States. Recently named an Affiliate of the Smithsonian Institution, the museum is a collection of ...

  4. Appalachian Mountains - Wikipedia

    en.wikipedia.org/wiki/Appalachian_Mountains

    The Appalachian Mountains, [b] often called the Appalachians, are a mountain range in eastern to northeastern North America. The term "Appalachian" refers to several different regions associated with the mountain range, and its surrounding terrain. The general definition used is one followed by the United States Geological Survey and the ...

  5. Great Smoky Mountains National Park - Wikipedia

    en.wikipedia.org/wiki/Great_Smoky_Mountains...

    Great Smoky Mountains National Park is a national park of the United States in the southeast, with parts in North Carolina and Tennessee. The park straddles the ridgeline of the Great Smoky Mountains, part of the Blue Ridge Mountains, which are a division of the larger Appalachian Mountain chain. The park contains some of the highest mountains ...

  6. Alleghanian orogeny - Wikipedia

    en.wikipedia.org/wiki/Alleghanian_orogeny

    The Alleghanian orogeny, a result of three separate continental collisions. USGS. The immense region involved in the continental collision, the vast temporal length of the orogeny, and the thickness of the pile of sediments and igneous rocks known to have been involved are evidence that at the peak of the mountain-building process, the Appalachians likely once reached elevations similar to ...

  7. Appalachian Trail by state - Wikipedia

    en.wikipedia.org/wiki/Appalachian_Trail_by_state

    The older log structure was built by the CCC in 1940. Another stop is the Dahlgren Campground. Hikers can stop here for the night and have free showers. The trail passes close to the eastern edge of Greenbrier State Park. The trail also goes through Pen Mar Park, which is just north of High Rock, which offers views and is a hang-gliding site.

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