Palermo is a town in Waldo County, Maine, United States. The population was 1,535 at the 2010 census. Palermo is included in the Augusta, Maine micropolitan New England City and Town Area.
The brook trout is a species of freshwater fish in the char genus Salvelinus of the salmon family Salmonidae. It is native to Eastern North America in the United States and Canada, but has been introduced elsewhere in North America, as well as to Iceland, Europe, and Asia. In parts of its range, it is also known as the eastern brook trout, speckled trout, brook charr, squaretail, or mud trout, among others. A potamodromous population in Lake Superior, as well as an anadromous population in Maine, is known as coaster trout or, simply, as coasters. The brook trout is the state fish of nine U.S. states: Michigan, New Hampshire, New Jersey, New York, North Carolina, Pennsylvania, Vermont, Virginia, and West Virginia, and the Provincial Fish of Nova Scotia in Canada.
Akers Pond is a 276-acre (1.1 km2) water body located in Coos County in northern New Hampshire, United States, in the town of Errol. Water from Akers Pond flows via Clear Stream to the Androscoggin River and thence into Maine.
Dan Hole Pond is a 443-acre (1.8 km2) water body located in Carroll County in eastern New Hampshire, United States, in the towns of Ossipee and Tuftonboro. The pond is situated on the south side of the Ossipee Mountains. Water exits Dan Hole Pond via the Dan Hole River, part of the Ossipee Lake watershed and ultimately that of the Saco River in Maine.
Great East Lake is an 1,825-acre (7.4 km2) water body located in Carroll County, New Hampshire, and York County, Maine, in the United States. The lake is shared by the towns of Wakefield, New Hampshire, and Acton, Maine, with 45% of its surface area in Acton and 55% in Wakefield. The lake is the farthest upstream of the five headwater lakes of the Salmon Falls River, a tributary of the Piscataqua River. Water from Great East Lake flows out its dam and through the 800-foot (240 m) Newichawannock Canal into Horn Pond, then into the Salmon Falls River below Horn Pond.
The Medomak River, historically known as the Muscongus River, is a 40-mile-long (64 km) river in Maine. From its source in Liberty, the river winds 32 miles (51 km) south to the head of its tidal river estuary in Waldoboro, then about 8 miles (13 km) south to Bremen. The river flows through Hockomock Channel into the head of Muscongus Bay. Medomak is Abenaki for "place (river) of many alewives".
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 Sheepscot River is a 66-mile-long (106 km) river in the U.S. state of Maine. Its lower portion is a complex island estuary with connections to the Kennebec River downstream of Merrymeeting Bay.
The West Branch Sheepscot River is a 24.9-mile-long (40.1 km) river in Maine. The branch originates in the northwest corner of Palermo and flows southwesterly through Branch Pond and the village of Weeks Mills in the town of China. The branch then flows southerly through the town of Windsor to a confluence with the Sheepscot River between Coopers Mills and North Whitefield. The branch is bridged by Maine State Route 3 between Branch Pond and Weeks Mills, by Maine State Route 105 at Windsor and by concurrent Maine State Routes 17 and 32 near Coopers Mills.
Horn Pond is a 227-acre (92 ha) water body located on the border of Acton, Maine, and Wakefield, New Hampshire, in the United States. The lake is both spring-fed and fed by the outflows of Great East Lake to the north and Wilson Lake to the east. Horn Pond's outlet is the Salmon Falls River which forms a natural border between Maine and New Hampshire and empties into the Piscataqua River east of Dover, New Hampshire, and ultimately the Gulf of Maine.
Unity Pond is the largest lake in Waldo County, Maine. It is within the towns of Unity, Burnham, and Troy. The main tributaries are Meadow Brook, Bithers Brook, and Carlton Stream. The sole outflow is Twenty-Five Mile Stream, via a wetlands to the southwest of the lake, which in turn feeds into the Sebasticook River. The lake is surrounded by almost 300 residences, of which slightly more than half are seasonal. It is also used for boating, fishing, camping, and swimming. Kanokolus Beach on the southwest shore and Burnham Town Beach are both open to the public.
St. George Lake is the fourth largest lake in Waldo County, Maine. It is in the township of Liberty, on the western side of Waldo County. Lake St. George State Park is on the northwest shore of the lake.
Beech Hill Pond is a lake in Otis, Hancock County, Maine, in the United States. It is 4.5 miles long, half a mile wide, and up to 104 feet deep. Trout, salmon, and other species of fish have been observed in the lake. Bald eagles and loons also live on the shoreline.
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.
Toddy Pond is a long, narrow Maine lake with three basins. The southern basin extends from Blue Hill northward to the middle basin forming the boundary between Penobscot and Surry. The northern basin is in Orland, where US route 1 follows the shoreline of the northern tip of the pond. The north end of the pond overflows through Alamoosook Lake into the Orland River. The northern basin cold-water habitat has a self-sustaining population of lake trout, and is stocked with splake, brown trout, and land-locked Atlantic salmon. Smallmouth bass and white perch thrive in the warmer water of the middle and southern basins. The pond is used by a spring spawning fun of alewife. There is a public boat launching site off highway 1 at the north end of the pond.
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.
China Lake is a pond in Kennebec County, Maine. Located northeast of the state capital of Augusta, China Lake is situated in the towns of China and Vassalboro. China Lake has two large basins connected by a narrow neck. The elongated eastern basin with an average depth of less than 30 feet (9.1 m) is entirely within the town of China, and has an irregular shoreline heavily developed with residences and seasonal cottages. The more nearly circular western basin extending into East Vassalboro is as deep as 85 feet (26 m), and shoreline development around the western basin has been discouraged to allow use as a water supply for Waterville and Winslow. The western basin overflows into Outlet Stream in the town of Vassalboro. Outlet Stream flows 7 miles (11 km) north to discharge into the Sebasticook River in Winslow 1 mile (1.6 km) upstream of the Kennebec River.
