First Debsconeag Lake | |
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Coordinates | 45°47′N68°59′W / 45.783°N 68.983°W [1] |
Max. length | 2 mi (3.2 km) [2] |
Surface area | 361 acres (146 ha) [3] |
Max. depth | 140 feet (43 m) [4] |
Water volume | 19,744 acre⋅ft (24,354,000 m3) [3] |
Surface elevation | 502 ft (153 m) [1] |
Second Debsconeag Lake | |
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Coordinates | 45°47′N69°02′W / 45.783°N 69.033°W [5] |
Max. length | 1.7 mi (2.7 km) [2] |
Surface area | 172 acres (70 ha) [3] |
Max. depth | 28 feet (8.5 m) [6] |
Water volume | 2,733 acre⋅ft (3,371,000 m3) [3] |
Surface elevation | 531 ft (162 m) [5] |
Third Debsconeag Lake | |
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Coordinates | 45°46′N69°03′W / 45.767°N 69.050°W [7] |
Max. length | 2.5 mi (4.0 km) [2] |
Max. width | 1 mi (1.6 km) [2] |
Surface area | 970 acres (390 ha) [3] |
Max. depth | 162 feet (49 m) [8] |
Water volume | 57,736 acre⋅ft (71,216,000 m3) [3] |
Surface elevation | 568 ft (173 m) [7] |
Fourth Debsconeag Lake | |
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Coordinates | 45°45′N69°05′W / 45.750°N 69.083°W [9] |
Max. length | 1.2 mi (1.9 km) [2] |
Surface area | 223 acres (90 ha) [3] |
Max. depth | 150 feet (46 m) [10] |
Water volume | 12,793 acre⋅ft (15,780,000 m3) [3] |
Surface elevation | 630 ft (190 m) [9] |
Fifth Debsconeag Lake | |
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Coordinates | 45°46′N69°06′W / 45.767°N 69.100°W [11] |
Max. length | 0.7 mi (1.1 km) [2] |
Surface area | 87 acres (35 ha) [3] |
Max. depth | 42 feet (13 m) [12] |
Water volume | 988 acre⋅ft (1,219,000 m3) [3] |
Surface elevation | 810 ft (250 m) [11] |
Sixth Debsconeag Lake | |
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Coordinates | 45°46′N69°07′W / 45.767°N 69.117°W [13] |
Max. length | 0.3 mi (0.48 km) [2] |
Surface area | 30 acres (12 ha) [3] |
Max. depth | 26 feet (7.9 m) [14] |
Water volume | 316 acre⋅ft (390,000 m3) [3] |
Surface elevation | 971 ft (296 m) [13] |
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.
The first lake is the second-largest of the chain, and holds more water than the combined total of the four smaller lakes. [3] The west end of the first lake receives discharge from the upstream lakes of the Debsconeag chain, while the eastern end overflows into the Debsconeag Deadwater on the West Branch at about the same level as the first lake. [2] The first lake supports a population of lake trout and land-locked Atlantic salmon. [4]
The second lake is the fourth-largest of the chain, but twice as large as the fifth lake. [3] In addition to discharge from the upstream lakes of the Debsconeag chain, the west end of the second lake receives drainage from Big and Little Beaver Ponds, Big and Little Minister Ponds, and Moose Pond. The east end of the second lake overflows into the first lake 900 yards (820 m) to the east. [2] The population of native brook trout fare poorly in competition with pumpkinseed and yellow perch. [6]
The third lake is larger than the combined total of all the other lakes in the chain. [3] Drainage from the fourth lake enters the end of the western arm of the lake, while the northwestern arm of the lake overflows into the second lake 400 yards (370 m) to the north. [2] This unusually clear lake supports a native population of brook trout and lake trout. [8]
The fourth lake is the third-largest of the chain, and holds more water than the combined total of the three smaller lakes. [3] Drainage from the fifth lake enters the north side of the lake, while the east end of the lake overflows into the third lake 600 yards (550 m) to the east. [2] This unusually clear lake supports a few brook trout, but is a more favorable habitat for lake trout. [10]
The fifth lake is the second-smallest of the chain. It is three times as large as the smallest sixth lake. [3] Drainage from the upstream ponds enters the west end of the lake, while the east end of the lake overflows into the fourth lake 900 yards (820 m) to the southeast. [2] The lake supports a population of native brook trout in competition with introduced yellow perch. Falls below the lake prevent upstream migration into the lake. [12]
The sixth lake (sometimes called the sixth pond) is the smallest of the chain. [3] The lake supports a population of native brook trout. [14] The east end of the lake overflows into the fifth lake. [2]
The Eighth Debsconeag Pond at 45°47′N69°08′W / 45.783°N 69.133°W [15] drains through the Seventh Debsconeag Pond at 45°46′N69°07′W / 45.767°N 69.117°W [16] into the chain of lakes downstream of the sixth lake and upstream of the fifth lake. [2] These ponds are much smaller than any of the six lakes. [3]
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 Baker Branch Saint John River is a 48.0-mile-long (77.2 km) river. This river is a tributary of the Saint John River, flowing in the Maine North Woods, in Maine, in the Northeastern United States.
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.
The Seboeis River is a river in Penobscot County, Maine. The river is the outflow of Snowshoe Lake in Maine Township 7, Range 7, WELS; Snowshoe Lake is fed via a short stream from Grand Lake Seboeis. The river runs 28.1 miles (45.2 km) south — through White Horse Lake, Seboeis Deadwater, Upper Seboeis River Gorge, and Gagnon Flat — to its confluence with the East Branch of the Penobscot River in T.3 R.7 WELS.
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.
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.
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.
Schoodic Lake is a deep Maine lake with a small drainage basin. The lake covers much of the western half of Lake View Plantation. Tributaries drain Orson Bog, Norton Pond, and Jaquith Pond in eastern Brownville. The south end of the lake overflows through Schoodic Stream 5 miles (8.0 km) to the Piscataquis River 13 miles (21 km) upstream of the Piscataquis confluence with the Penobscot River at Howland. The lake provides good habitat for togue, squaretail, and land-locked Atlantic salmon. Fishermen also find smallmouth bass, white sucker and round whitefish.
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.
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.
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.
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.
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.