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The Maine Geological Survey began a continuing process of mapping sand and gravel aquifers beginning in 1978. Statewide, Maine receives an annual rainfall total of 42 inches or 24 trillion gallons. Up to 50% of rainfall runs off the landscape in rivers and streams, while an additional 30–40% evaporates or is transpired through vegetation.
The Webhannet River is an 8.3-mile-long (13.4 km) [1] river whose 8,963-acre (36.27 km 2) watershed is contained entirely within the town of Wells, Maine. [2] The river has five tributaries, including three with official names: Pope’s Creek, Depot Brook, and Blacksmith Brook.
Geological modelling from cross sections Geomodelr, Inc. SaaS - AGPL: Cross-platform: Python: Allows creation of public geological models in its web platform for free and query the model with an Open Source Python Package BGS Groundhog Desktop [29] Geological modelling from cross sections British Geological Survey: OGL - Open Government Licence ...
The Presumpscot formation is a late Pleistocene glacial deposit of predominantly submarine clays, located along the Maine and New Hampshire coast and inland along their major river valleys.
The following is a list of dams and reservoirs in Maine, USA. Major dams are linked below. The National Inventory of Dams defines any "major dam" as being 50 feet (15 m) tall with a storage capacity of at least 5,000 acre-feet (6,200,000 m 3 ), or of any height with a storage capacity of 25,000 acre-feet (31,000,000 m 3 ).
The Saint John Ponds are a chain of shallow lakes at the headwaters of the Baker Branch Saint John River in the North Maine Woods.The flow sequence is from the Upper First Saint John Pond, through the Lower First Saint John Pond, Second Saint John Pond, Third Saint John Pond, and Fourth Saint John Pond to the Fifth Saint John Pond.
The Swift River is a 26.7-mile-long (43.0 km) [1] river in western Maine. It is a tributary of the Androscoggin River , which flows to the Kennebec River near its mouth at the Atlantic Ocean . The Swift River rises in Franklin County at the outlet of Swift River Pond, a small water body southeast of the Rangeley Lakes .
Kenduskeag Stream is a 36.2-mile (58.3 km) [1] stream in the U.S. state of Maine. It is a tributary of the Penobscot River . The stream rises at the outlet of Garland Pond in the town of Garland , and flows southeast through Corinth , Kenduskeag , and Glenburn , before it reaches the city of Bangor .