Eagle Lake
See
Eagle Lake (Maine) for the lake at the headwaters of the Allagash Wilderness Waterway.
Eagle Lake overflows into the Fish River in the southeast corner of Wallagrass 13 miles (21 km) upstream of the confluence with the Saint John River. From the outlet, the lake extends southward through the eastern part of the town of Eagle Lake and forms a "L" extending eastward through township 16, range 6, into township 16, range 5. Fish River enters Eagle Lake at the bend in the "L". The chain of lakes tributary to the Fish River enters Eagle Lake via the Eagle Lake Thoroughfare from Square Lake in township 16, range 5. Smaller tributaries to Eagle Lake include Clark Brook, Gilmore Brook, Brown Brook, Devoe Brook, and Pond Brook from the town of Eagle Lake, and Alec Brook, Miller Brook, and Last Brook from township 16. The Bangor and Aroostook Railroad follows the west shore of Eagle Lake through the town of Eagle Lake and then follows the Fish River into Fort Kent. [2] Eagle Lake provides good habitat for rainbow smelt, brook trout, lake trout, and land-locked salmon. [12] The entire eastern arm of Eagle Lake is within the 23,000-acre (9,300 ha) reserve of public land available for ATV riding, birding, camping, cross-country skiing, fishing, hiking, hunting, snowmobiling, snowshoeing, and swimming. [13]
The Sebasticook River is a 76-mile-long (122 km) river in the central part of Maine, in the United States. From its source in Dexter, the upper "Main Stream" section flows generally west and south 30 miles (48 km) to Great Moose Lake. From the outlet of the lake in Hartland, the Sebasticook flows 41 miles (66 km) south to the Kennebec River in Winslow.
The East Branch Mattawamkeag River is a tributary of the Mattawamkeag River in Aroostook County, Maine. From its source in Dudley, the river runs 36 miles (58 km) south and southeast to its confluence with the West Branch Mattawamkeag River in Haynesville, about 10 miles (16 km) west of the Canada–United States border.
The Fish River is a 69.9-mile-long (112.5 km) river in northern Maine in the United States. It is a tributary of the Saint John River, which flows to the Bay of Fundy in New Brunswick, Canada.
The Kennebago River is a 30-mile-long (48 km) river in northwestern part of the U.S. state of Maine. It is a tributary of Cupsuptic Lake, an arm of Mooselookmeguntic Lake. Via a chain of lakes and the Rapid River, it is part of the Androscoggin River watershed.
The Moose River is an 83-mile-long (134 km) river in Maine. Its source is in Beattie, on the Canada–United States border, which runs along the height of land between the watersheds of the Kennebec River in Maine and the Chaudière River in Quebec. From there, the river runs east through Attean Pond and Wood Pond, past the town of Moose River, then through Long Pond and Brassua Lake. The Moose River empties into Moosehead Lake, the source of the Kennebec River, in Rockwood Strip. The International Railway of Maine was built along Moose River in 1889.
The Roach River is a river in Piscataquis County, Maine. From the outlet of Third Roach Pond in Shawtown, the river runs 19.1 miles (30.7 km) west, through a chain of ponds. The Flow sequence through the ponds is from the Fourth Roach Pond through the Third Roach Pond, Second Roach Pond, and First Roach Pond to empty into Moosehead Lake, the source of the Kennebec River, in Spencer Bay. The Seventh Roach Pond drains through the Sixth Roach Pond in a separate tributary to the Third Roach Pond. No fifth Roach Pond is shown on modern maps.
Range Ponds State Park is a public recreation area wrapping around the eastern end of Lower Range Pond in the town of Poland in Androscoggin County, Maine. The state park offers a sandy beach with lifeguard-supervised swimming, kayaking, limited motorized boating, hiking trails, and fishing. Mountain biking trails, built with the help of local volunteers, provide intermediate level, single-track loops off a central double-track trail that winds through mature pine and hardwood forests.
The Munsungan-Chase Lake Thoroughfare Archeological District encompasses a series of important archaeological sites in a remote area of northern Maine, United States. These sites offer evidence of human habitation dating to not long after the retreat of the glaciers following the Wisconsin glaciation, with extensive stone tool workshops working with red chert found in abundance in the area. Stone tools made from sources in this region have been found at archaeological sites across New England. The district was listed on the National Register of Historic Places in 1979.
Eagle Lake is the first, largest, and deepest lake of the Allagash Wilderness Waterway in the North Maine Woods. The lake covers the eastern side of Eagle Lake township. The southern end of the lake extends into Maine township 7, range 12, where it receives overflow from Indian Pond, and into Soper Mountain township where it receives overflow from Haymock Lake via Smith Brook. Other ponds in the Eagle Lake watershed include Woodman Pond via Woodman Brook, Pillsbury Pond and Little Pillsbury Pond via Smith Brook, Soper Pond and Upper Soper Pond via Soper Brook, and the Russell Ponds via Russell Brook. Eagle Lake originally received overflow from Chamberlain Lake, but Lock Dam has diverted most Chamberlain Lake overflow through Telos Cut to the Penobscot River since the 1850s.
Seboeis Lake extends from Lake View Plantation, Maine, north into Maine township 4, range 9. The lake is enclosed by rocky headlands and sandy beaches and contains several pine-covered islands. The inlet at the north end receives several tributaries from Long A township including Dean Brook, Jordan Brook, and West Seboeis Stream. Bear Brook flows into the northwest corner of the lake, and Northwest Pond overflows into the west side of the Lake. West Branch Sebois Stream overflows the east side of the lake through Dudley Rips into Endless Lake; and Endless Lake overflow reaches the Piscataquis River 15 miles (24 km) downstream, just 3 miles (4.8 km) upstream of the Piscataquis and Penobscot River confluence at Howland.
Upper Richardson Lake and Lower Richardson Lake are impounded as a single reservoir by Middle Dam at the outlet to Rapid River on the western shore of the lower lake. Rapid River flows 5 miles (8.0 km) to Umbagog Lake headwaters of the Androscoggin River. Upper Richardson Lake is in the western portion of Richardsontown township, and the lower lake is on the border of Magalloway Plantation and Maine township C. Primary inflow is discharge over Upper Dam on Mooselookmeguntic Lake on the eastern shore of the upper lake. Smaller tributaries entering the north end of the upper lake include Mill Brook draining the Richardson Ponds, Fish Brook draining Fish Pond, and Beaver Brook draining Beaver Pond, Little Beaver Pond, and Aziscohos Pond. Other small tributaries include Rand Brook on the western shore, and Mosquito Brook, Metallak Brook, and Bailey Brook on the eastern shore. The lake offers excellent habitat for adult trout, but with dams on the outlet and major inlet, fish populations are limited by the insufficient spawning and nursery areas of these small tributaries. The public boat launch area at the north end of the upper lake is 1 mile (1.6 km) off Maine State Route 16; and the boat launch area at the south end of the lower lake is accessed by driving 12 miles (19 km) north of Andover on South Arm Road.
Scopan Lake is a "V" shaped lake in northern Maine. The lake was known as Squa Pan Lake by early European settlers, but was renamed in 2011 to eliminate what Native Americans in the United States interpreted as a racial slur. The lake is mostly in Scopan township, but the north end of the eastern arm of the "V" extends into Maine township 11, range 4; and the north end of the western arm extends into Masardis and Ashland. The lake discharges to Scopan Stream through a dam in Masardis. Scopan Stream flows into the Aroostook River 4 miles (6.4 km) downstream of the dam, and the Aroostook River is a tributary to the Saint John River. The Bangor and Aroostook Railroad crosses the northern tip of both arms of the lake.
The Belgrade Lakes are a chain of lakes around Belgrade, Maine. The flow sequence is from East Pond to North Pond to Great Pond to Long Pond to Messalonskee Lake and thence via Messalonskee Stream to the Kennebec River at Waterville. The lakes have long been an important resort area for fishing, boating, and swimming; and shoreline development includes residences for individuals employed in the cities of Waterville and Augusta.
Millinocket Lake is 9 miles (14 km) northwest of Millinocket, Maine, and is drained by Millinocket Stream, which flows through the town of Millinocket into the West Branch Penobscot River 2 miles (3.2 km) south of town. The lake is fed by Sandy Stream, which drains the southeastern slopes of Mount Katahdin by tributaries including Roaring Brook, Avalanche Brook, Spring Brook, Beaver Brook, and Rum Brook. Sandy Stream is a good spawning habitat for rainbow smelt, which are a primary prey for lake trout and land-locked Atlantic salmon living in the lake.
Spencer Lake extends southward from Fish Pond in Hobbstown township into Maine township 3, range 5. The north end of the lake receives drainage from Whipple Bog, Whipple Pond, Hall Pond, Toby Pond, and Chub Pond through Fish Pond. The south end of the lake overflows through Little Spencer Stream and thence Spencer Stream 6 miles (9.7 km) to the Dead River 14 miles (23 km) upstream of the confluence with the Kennebec River at The Forks. The lake supports a native population of lake trout and brook trout, and has been stocked with land-locked Atlantic salmon. There is a boat launch area at the north end of the lake accessible from a 2-mile (3.2 km) gravel road 11 miles (18 km) west off U.S. Route 201 at Parlin Pond.
A chain of three Jo-Mary Lakes along the border of Penobscot County and Piscataquis County drain into the Pemadumcook Chain of Lakes in the North Maine Woods. The flow sequence is from Upper Jo-Mary Lake into Middle Jo-Mary Lake and then through Lower Jo-Mary Lake into Pemadumcook Lake.
Nahmakanta Lake is the source of Nahmakanta Stream in the North Maine Woods. Nahmakanta Stream flows 4 miles (6.4 km) from the southeast end of the lake in Maine township 1, range 11, to the Pemadumcook Chain of Lakes in township 1, range 10. The Appalachian Trail follows Nahmakanta Stream and the southwest shore of Nahmakanta Lake. The northwest end of the lake in township 2, range 11, receives drainage from Rainbow Lake via Rainbow Stream, from Gould Pond via Gould Brook, from the Bean Ponds via Bean Brook, and from Female Pond, Wadleigh Pond, the Musquash Ponds, and Pollywog Pond via Pollywog Brook. These streams provide spawning habitat for brook trout and land-locked Atlantic salmon, while lake trout spawn in the shoals of the lake.
Hancock Brook is an east-bank tributary to the Saco River at Hiram, Maine. The brook originates in eastern Denmark and flows through a chain of ponds along the border between Hiram and Sebago. The narrow-gauge Bridgton and Saco River Railroad was built along the brook in 1882, and operated until 1941.
Musquacook Stream is a tributary to the Allagash River in the North Maine Woods. The stream originates in a chain of lakes in Maine range 11 townships 10, 11 and 12. The flow sequence is from Clear Lake through Fifth Musquacook Lake into Fourth Musquacook Lake in Piscataquis County; and from Fourth Musquacook Lake through Third Musquacook Lake, Second Musquacook Lake, and First Musquacook Lake into the Allagash River Musquacook Deadwater in Aroostook County.
Parmachenee Lake is on the Magalloway River near the Canadian border on the western edge of Maine. The lake was named for the daughter of Native American chief Metalluk, and is best known for the Gilded Age Parmachenee Club. The Magalloway River headwaters enter the north end of the lake in Parmachenee township, and the lake extends south into Lynchtown township where it overflows 2 miles (3.2 km) upstream of Aziscohos Reservoir.
