Kennebec River
The Kennebec River just south of Bath
Origin	Moosehead Lake
Mouth	Gulf of Maine, North Atlantic Ocean
Basin countries	United States
Length	149 mi (240 km)
Source elevation	1,024 ft (312 m)
Avg. discharge	9,111 ft³/s (258 m³/s) at its entrance to Merrymeeting Bay
Basin area	5,869 mi² (15,200 km²)

The course of the Kennebec River

The Kennebec River is a river, 150 mi (240 km) long, in the state of Maine in the northeastern United States. It rises in Moosehead Lake in west central Maine. The East and West Outlets join at Indian Pond and the river then flows southward where it is joined, at the The Forks by the Dead River, also called the West Branch ^[1] then continues southward past the cities of Madison, Skowhegan, Waterville, and the state capital Augusta. At Richmond, it flows into Merrymeeting Bay, a 16 mi (26 km) long freshwater, tidal bay into which also flow the Androscoggin River and five other smaller rivers. The Kennebec then runs past the shipbuilding center of Bath, thence to the Gulf of Maine in the Atlantic Ocean. Ocean tides affect the river height as far north as Augusta. Tributaries of the Kennebec River include the , Carrabassett River, Sandy River, and Sebasticook River.

History

The river was explored by Samuel de Champlain in 1604 and 1605. In 1607, the Popham Colony, the first English colony in New England, was founded near its mouth. The river, then known as the Sagadahoc River, also marked the northern border of the 1622 land patent of the Province of Maine granted to Ferdinando Gorges and John Mason.

Shipbuilding

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 steel vessels have since been launched on the Kennebec, particularly in Bath, the so-called City of Ships, including the Wyoming, one of the largest wooden schooners ever built. The sole remaining shipyard is the Bath Iron Works, one of the few yards still building warships for the United States Navy.

Ice Industry

In 1814 Frederic Tudor began to establish markets in the West Indies and the southern United States for Ice. In 1826 Rufus Page build the first large ice house near Gardiner to supply Tudor The ice was harvested by farmers and other made inactive by the winter weather. The ice was cut by hand, floated to an ice house on the bank where it was stored until spring. Then, packed in sawdust it was loaded aboard ships and send south. ^[2]

Natural Resources

Prior to the industrial era, the river contained many anadromous fish, in particular the Atlantic Salmon. The exploiting of hydroelectric power in the region reduced the runs of such fish. The removal of dams on the river has been a controversial local issue in recent years. The removal of the Edwards Dam in 1999 has led to increased anadromous activity on the river.

Statistics

The river drains a total area of 5,870 square miles (15,200 km²), and on average discharges nearly six billion (5,893 million) U.S. gallons per day into Merrymeeting Bay at a rate of 9,111 cubic feet per second (258 m³/s). The United States government 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.^[3]

Prior to damming, the river was was considered navigable as far as Augusta. The founder of Colby College sailed his sloop, Hero, up to Augusta and a longboat to Waterville where he decided to found the college.

On April 1st 1987 fast melting snow and 4-6 inchs of rain in the mountains forced the river to flood her banks. By April 2nd 1987 the peak of the flooding was at 34.1 ft. above flood stage. It caused approximately 1 millon dollors in damage(171 millon dollors in todays money) It flooded 2,100 homes destoying 215 and caused major damage to 240 others. To this day some sign of the flood can still bee found around the towns and cities that line the river.

See also

• List of Maine rivers

External links

• MaineRivers.org Kennebec River profile
• Real-time flow or stage data for the The Forks, Bingham, North Sidney, Augusta, and Gardiner gages.
• Kennebec-Chaudiere Kennebec-Chaudiere International Corridor

	State of Maine Augusta (capital)
Topics	Culture | Geography | Government | History | Images
Regions	Down East | Highlands | Lake Country | Mid Coast | North Woods | Penobscot Bay | Southern Coast | Western Mountains
Counties	Androscoggin | Aroostook | Cumberland | Franklin | Hancock | Kennebec | Knox | Lincoln | Oxford | Penobscot | Piscataquis | Sagadahoc | Somerset | Waldo | Washington | York
Cities	Auburn | Augusta | Bangor | Bath | Belfast | Biddeford | Brewer | Calais | Caribou | Eastport | Ellsworth | Gardiner | Hallowell | Lewiston | Old Town | Portland | Presque Isle | Rockland | Saco | South Portland | Waterville | Westbrook
Largest towns	Brunswick | Cape Elizabeth | Falmouth | Gorham | Kennebunk | Kittery | Lisbon | Orono | Sanford | Scarborough | Skowhegan | Standish | Topsham | Wells | Windham | Winslow | York

References

1. ^ The Upper Kennebec Valley By John F. Hall p 7 The main stem, from Indian pond was sometimes called the East Branch
2. ^ Maine's Ice Industry by Richard Judd in Maine The Pine Tree State form Prehistory to the present
3. ^ G.J. Stewart, J.P. Nielsen, J.M. Caldwell, A.R. Cloutier (2002). Water Resources Data - Maine, Water Year 2001 (PDF). Water Resources Data - Maine, Water Year 2001. Retrieved on 2006-05-07.

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