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 Little Androscoggin River is a 51.4-mile-long (82.7 km) river in Maine. It flows from Bryant Pond in Woodstock to its confluence with the Androscoggin River in Auburn. The Androscoggin flows into Merrymeeting Bay in the Kennebec River estuary.
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 Pleasant River is a 13.1-mile-long (21.1 km) tributary of the Presumpscot River in the U.S. state of Maine.
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.
Harris Station Dam is a hydroelectric dam in Northeast Somerset, Somerset County, Maine. Also known as the Indian Pond Project, the dam was built from 1952 to 1954 as the largest hydroelectric dam in the state of Maine. It impounds the Kennebec River at the southern end of the natural Indian Pond, about 12 miles (19 km) downstream from Moosehead Lake.
Caucomgomoc Lake is in the North Maine Woods at the corner of townships 6 and 7 in ranges 14 and 15. Loon Stream flows into the southern end of the lake from Loon Lake, Bear Pond, Big Hurd Pond, Little Hurd Pond, Bear Brook Pond, McDougal Pond, and tributaries from the southwest. Overflow from Little Shallow Lake through Shallow Lake, Daggett Pond, and Round Pond enters the east side of Caucomgomoc Lake through Ciss Stream. Smaller tributaries Avery Brook, Middle Brook, and Ramsell Brook flow into the north end of the lake. There is a dam at the lake outlet on the eastern shore a short distance south of Ciss Stream. Discharge through the dam flows down Caucomgomoc Stream through Black Pond and Chesuncook Lake to the West Branch Penobscot River at Ripogenus Gorge. White perch and yellow perch have largely replaced historic trout populations in the lake.
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 Fish River chain of lakes is a series of five lakes in the North Maine Woods region of northern Maine, in a tributary stream to the Fish River. The lakes are an important northern Maine recreation area providing habitat for wildlife including rainbow smelt, brook trout, lake trout, and land-locked Atlantic salmon.
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.
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.
The chain of Debsconeag Lakes in the North Maine Woods is a tributary to the West Branch Penobscot River. The flow sequence is from the Sixth Debsconeag Lake through the Fifth, Fourth, Third, Second, and First into the Debsconeag Deadwater on the West Branch.
Highland Lake is a lake in the U.S. state of Maine. Formerly known as Duck Pond, the lake extends from the northern tip of Westbrook through the western edge of Falmouth into east Windham, Maine. The south end of the lake overflows via Mill Brook 4 miles (6.4 km) through Westbrook to the Presumpscot River at Riverton. The shoreline of the lake is heavily developed with residences, seasonal cabins, and a state-owned parking area off Mast Road in Falmouth for the launch of canoes and car-top boats. The deeper northern basin of the lake in Windham has been stocked with brown trout, splake, alewife, and occasionally brook trout and land-locked Atlantic salmon. Highland Lake's shallow southern basin is favorable habitat for white perch and chain pickerel, and has been stocked with largemouth bass.
Peabody Pond extends from the southern tip of Bridgton into northern Sebago forming the western boundary of Naples, Maine. The eastern tip of the lake receives drainage from Cold Rain Pond in Naples. The southern tip of the lake overflows as the Northwest River through 5 miles (8.0 km) of boggy land to the western shore of Sebago Lake at East Sebago. The pond has a native population of rainbow smelt, and has been stocked with smallmouth bass, lake trout, and land-locked Atlantic salmon. A boat-launching area near the outlet of the lake is accessible from Tiger Hill Road off Maine State Route 107.
Crescent Lake receives drainage from Coffee Pond and Dumpling Pond in northern Casco, Maine, and extends south into Raymond. The south end of the lake overflows through Tenny River to Panther Pond 1 mile (1.6 km) south. The town of Raymond maintains a boat ramp on Maine State Route 85 at the south end of Crescent Lake. Smallmouth bass, largemouth bass, chain pickerel, and white perch thrive in the lake. Dissolved oxygen deficiency below the 11-metre (36 ft) summer thermocline limits suitability for cold-water fish; but the lake supports populations of cusk and rainbow smelt.
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.
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. Flow from one pond to the next is sometimes called Baker Stream rather than the Baker Branch Saint John River. Great Northern Paper Company dug a canal from Fifth Saint John Pond 2 miles (3.2 km) westward to the North Branch Penobscot River in 1939, and built a dam at the north end of Fifth Saint John Pond so pulpwood logs harvested in the upper Saint John River watershed could be floated down the Penobscot River to Millinocket, Maine. The canal and dam have fallen into disrepair so most drainage from the ponds again flows down the Saint John River. All upstream ponds with the exception of the first had dams to regulate discharge flow for log driving, but those dams have similarly fallen into disrepair. Moose use the ponds as summer refuge from heat and biting insects.
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.
