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  2. Natural Bridge (Virginia) - Wikipedia

    en.wikipedia.org/wiki/Natural_Bridge_(Virginia)

    Natural Bridge is a geological formation in Rockbridge County, Virginia, United States, comprising a 215-foot-high (66 m) natural arch with a span of 90 feet (27 m). It is situated within a gorge carved from the surrounding mountainous limestone terrain by Cedar Creek, a small tributary of the James River.

  3. Granite - Wikipedia

    en.wikipedia.org/wiki/Granite

    Granite (/ ˈ ɡ r æ n ɪ t / GRAN-it) is a coarse-grained intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase.It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground.

  4. Old Rag Mountain - Wikipedia

    en.wikipedia.org/wiki/Old_Rag_Mountain

    Old Rag Mountain is underlain by Old Rag Granite, named for its ubiquitous exposure on the mountain, formed during the Grenville Orogeny about a billion years ago. About 400 million years after the Grenville orogeny during the Catoctin Formation, deposition of basaltic magma occurred during the formation of the Iapetus Ocean, forming a layer of greenstone over the granite.

  5. Humpback Rock - Wikipedia

    en.wikipedia.org/wiki/Humpback_Rock

    Humpback Rocks is a massive greenstone outcropping near the peak of Humpback Mountain in the Blue Ridge Mountains of Augusta County and Nelson County, Virginia, United States, with a summit elevation of 3,080 feet (940 m).

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  7. Geology of Virginia - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Virginia

    At the same time, 250 to 300 quarries were producing limestone, granite, slate, soapstone and gravel. Willis Mountain, near US 15 between US 60 and US 460 hosts the largest kyanite mine in the world, supplying the automotive spark plug and high-temperature kiln industry. Virginia also has significant vermiculite production. [10]

  8. Atlantic Seaboard Fall Line - Wikipedia

    en.wikipedia.org/wiki/Atlantic_Seaboard_Fall_Line

    The Atlantic Seaboard Fall Line, or Fall Zone, is a 900-mile (1,400 km) escarpment where the Piedmont and Atlantic coastal plain meet in the eastern United States. [2] Much of the Atlantic Seaboard fall line passes through areas where no evidence of faulting is present.

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