The Allagash River is a tributary of the Saint John River, approximately 65 miles (105 km) long, in northern Maine in the United States. It drains in a remote and scenic area of wilderness in the Maine North Woods north of Mount Katahdin. The name "Allagash" comes from the Abenaki language, a dialect of the Algonquin languages, spoken by the Penobscot Tribe The word, /walakéskʸihtəkʸ/, means "bark stream".
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 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.
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 downstream from Moosehead Lake.
The Eagle Lake Tramway is a historic timber-transport mechanism in the remote North Maine Woods in northeastern USA. The tramway, built in 1902 and operated until 1907, transported timber across a neck of land between Eagle Lake and Chamberlain Lake, with one end eventually becoming the eastern terminus of the Eagle Lake and West Branch Railroad in 1927. The remnants of the tramway and rail station were listed on the National Register of Historic Places as the Tramway Historic District in 1979. The tramway is part of the Allagash Wilderness Waterway, a Maine state park.
Chamberlain Lake is one of the largest and deepest lakes in the North Maine Woods. The lake originally drained north through Eagle Lake and Churchill Lake into the Allagash River tributary to the Saint John River. Nineteenth-century logging operations diverted the lake into the Penobscot River before designation of the Allagash Wilderness Waterway in 1966.
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.
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.
Allagash Lake is in the North Maine Woods on the boundary of Maine range 14 townships 7 and 8. Allagash Stream flows into the northwest corner of the lake from Allagash Pond, Crescent Pond, and Mud Pond in township 9 range 15. Allagash Stream overflows the northeast corner of the lake and flows 5 miles (8.0 km) through Little Round Pond into Chamberlain Lake. Chamberlain Lake originally overflowed through Eagle Lake and Churchill Lake to the Allagash River; but was diverted through Telos Cut to the Penobscot River in the 1850s. Allagash Lake provides good habitat for togue and squaretail.
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.
Chemquasabamticook Lake is the source of Chemquasabamticook Stream in the North Maine Woods. The lake is in Maine townships 9 and 10 of range 15, and township 9 of range 14. Tributaries include Sweeney Brook, Boucher Brook, Gannet Brook, Fool Brook, and Ross Inlet. Chemquasabamticook Stream flows 22 miles (35 km) from a disused dam at the north end of the lake to reach Long Lake on the Allagash River. Chemquasabamticook Lake has a self-sustaining native squaretail population, and rainbow smelt have been introduced to encourage more rapid growth of the native togue.
Millinocket Lake is the source of Millinocket Stream in the North Maine Woods north of Baxter State Park. Millinocket Stream flows 5.5 miles (8.9 km) to Maine township 8, range 8, where it joins Munsungan Stream to form the Aroostook River. The lake extending along the border of Maine range 9 townships 7 and 8 is impounded behind a wooden dam. The dam enlarged the lake to include Little Millinocket Lake and Moose Pond by flooding adjoining bogs to store water for hydropower. The large areas of shallow flooded bog are a good habitat for fallfish, yellow perch and white suckers; but with summer water temperatures ranging from 70° near the surface to 55° in the deeper areas, dissolved oxygen concentrations become unfavorable for trout. Tributaries to the lake drain a number of small ponds to the west of the lake including Atkins Pond, Blackmore Pond, Buckley Pond, Big Caribou Pond, Little Caribou Pond, Chandler Pond, Elsie Pond, Ervin Pond, Jack Pond, Kyle Pond, Line Pond, Mathews Pond, May Pond, Little Moose Pond, Upper Moose Pond, Pretty Pond, Snowshoe Pond, and Spring Pond.
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.
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.
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) eastward 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.
