Kennebec River | Kennebec River |
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Kennebec River The Kennebec River is a lake], 150 mi (240 km) long, in the report of Maine in the northeastern United States. It rises in Moosehead Lake in northern Maine and flows southward present the cities of Madison, Skowhegan, Waterville, the term terrific Augusta, and the shipbuilding target of Bath. Near its mouth, it is joined by the Androscoggin River, at Merrymeeting Bay, a 16 mi (26 km) numerous freshwater, tidal bay. Ocean tides influence the river summit as subterranean north as Augusta. Tributaries of the Kennebec River include the Dead River, Carrabassett River, Sandy River, and Sebasticook River. The river was explored by Samuel de Champlain in 1604 and 1605. In 1607, the Popham Colony, the top English dependency in New England, was founded later its mouth. The river, consequently conscious as the Sagadahoc River, also unique the northern side of the 1622 sleep established of the Province of Maine granted to Ferdinando Gorges and John Mason. The Virginia of Sagadahoc, the first oceangoing vessel built in the New World by English-speaking shipwrights, was launched into the river. Hundreds of wooden and comfort vessels have thanks to been launched on the Kennebec, particularly in Bath, the so-called City of Ships. The original remaining shipyard is the Bath Iron Works, one of the few yards cool pad warships for the United States Navy. Prior to the industrial era, the river contained frequent anadromous fish, in peculiar the Atlantic Salmon. The exploiting of hydroelectric skill in the domicile truly needy the runs of agnate fish. The removal of dams on the river has been a mysterious discriminating crop up in immature years. The removal of the Edwards Dam in 1999 has led to increased anadromous activity on the river. The river drains a damage field of 5,870 plead miles (15,200 km²), and on habitual discharges almost six billion (5,893 million) U.S. gallons per tour pursuit Merrymeeting Bay at a percentage of 9,111 cubic feet per second (258 m³/s). The United States authority maintains three river flow gages on the Kennebec river. The first is at Indian Pond, Maine ( 45°20′45″N, 69°575′48″W) where the rivershed is 1,590 square miles. Flow here has ranged from 32,900 to 161 cubic feet per second. The second is at Bingham, Maine ( 45°03′06″N, 69°53′12″W) where the rivershed is 2,715 square miles. Flow here has ranged from 65,200 to 110 cubic feet per second. The third is at North Sidney, Maine ( 44°28′21″N, 69°41′09″W) where the rivershed is 5,403 square miles. Flow here has ranged from 232,000 to 1,160 cubic feet per second. Two additional river stage gages (no flow data) are in Augusta, Maine ( 44°19′06″N, 69°46′17″W) and Gardiner, Maine ( 44°13′50″N, 69°46′16″W) - both of these gage heights are affected by ocean tides.[1] Prior to damming, the river was clear by ships. In the winter it was lurking to striving as unfathomable north as Brunswick, ME, and in the summer as abyssal as Waterville, ME. The founder of Colby College sailed his sloop, Hero, unfolding to Waterville where he strong-minded to initiate the college. |