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Map all coordinates using OpenStreetMap. Download coordinates as: KML; GPX (all coordinates) GPX (primary coordinates) ... Pages in category "Lakes of North Carolina"
The bridge carries traffic on North Carolina Highway 24/27/73 across the river and Lake Tillery from Stanly County to Montgomery County. Swift Island Bridge , the water's old crossing parallels the newer two-lane bridge which accompanies it; the older bridge is a narrow one-lane concrete arch bridge built in 1922.
Mountain Island Hydro Station is a four-unit generating facility with a capacity of 60 megawatts located in Gaston County, North Carolina. It was built in 1923 to meet the growing demand for electricity by homeowners in the Carolinas. At the time, electricity was largely used by industrial customers.
As of the census [3] of 2000, there were 3,053 people, 1,201 households, and 887 families residing in the town. The population density was 1,327.2 inhabitants per square mile (512.4/km 2).
North Carolina Highway 27A (NC 27A) was established when mainline NC 27 was rerouted on a more direct route between Lake Tillery and Troy, in Montgomery County. NC 27A follows NC 73 east, through Pee Dee, then continues straight along Pee Dee Road, connecting with NC 109, in Wadeville. Going back north, it reconnected with NC 27 west from Troy.
Kuwohi, third highest mountain in North Carolina From left: Old Black, Mount Kephart, Mount Guyot and Mount Chapman, 9th, 16th, 4th, and 7th highest mountains, respectively, in North Carolina Richland Balsam, 8th highest mountain in North Carolina Waterrock Knob, 12th highest mountain in North Carolina
This place-name is derived from the English surname Albemarle.According to a 1905 publication by the United States Geologic Survey, based on research by University of North Carolina - Chapel Hill history professor Kemp P. Battle, it was named specifically for General George Monck, the first Duke of Albemarle and one of the original proprietors of the colony of Carolina, which included the town.
The Uwharries were once a coastal mountain range; [2] isostasy has slowly raised the eastern seabed until today they lie in the Piedmont of North Carolina over 150 miles (240 km) from the coast. Formed approximately 500 million years ago by accretion along the Gondwanan tectonic plate, they are thought to have once peaked at some 20,000 feet ...
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