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The Giant's Causeway (Irish: Clochán an Aifir) [1] is an area of approximately 40,000 interlocking basalt columns, the result of an ancient volcanic fissure eruption. [3] [4] It is located in County Antrim on the north coast of Northern Ireland, about three miles (4.8 km) northeast of the town of Bushmills.
Basalt columns seen on Porto Santo Island, Portugal. Columnar jointing of volcanic rocks exists in many places on Earth. Perhaps the most famous basalt lava flow in the world is the Giant's Causeway in Northern Ireland, in which the vertical joints form polygonal columns and give the impression of having been artificially constructed.
The Eno River, named for the Eno Native Americans who once lived along its banks, is the initial tributary of the Neuse River in North Carolina, United States. Descendants of European immigrants settled along the Eno River in the latter 1740s and early 1750s, including many Quakers from Pennsylvania.
The Nantahala River (/ ˌ n æ n t ə ˈ h eɪ l ə /) [5] is a river in western North Carolina in the United States, within the Nantahala National Forest, and near the Great Smoky Mountains National Park. Two-lane U.S. Highway 19/74 runs along the river, picnic areas dotting the route.
The interlocking basalt columns on the north-east side of Fingal Head were called the "Giants Causeway", named after the famous Giants Causeway between Northern Ireland and Western Scotland. The Fingal Caves located on the south side of Fingal Head, were destroyed and used in the early 1900s for the Tweed Break water.
Little River (Horry County, South Carolina) Little River (Jacob Fork) Little River (Neuse River tributary) Little River (North Carolina-Virginia) Little River (Pee Dee River tributary) Little River (Roanoke River tributary) Little Tennessee River; Little Uwharrie River; Lockwood Folly River; Lower Little River; Lumber River; Lynch Creek ...
The Swannanoa River flows through the Swannanoa Valley of the region of Western North Carolina, and is a major tributary to the French Broad River. Its headwaters arise in Black Mountain, North Carolina ; however, it also has a major tributary near its headwaters: Flat Creek, which begins on the slopes of Mount Mitchell .
Looking Glass Dome. The geology of North Carolina includes ancient Proterozoic rocks belonging to the Grenville Province in the Blue Ridge.The region experienced igneous activity and the addition of new terranes and orogeny mountain building events throughout the Paleozoic, followed by the rifting of the Atlantic Ocean and the deposition of thick sediments in the Coastal Plain and offshore waters.