The Catawba River originates in Western North Carolina and flows into South Carolina, where it later becomes known as the Wateree River. The river is approximately 220 miles (350 km) long. It rises in the Appalachian Mountains and drains into the Piedmont, where it has been impounded through a series of reservoirs for flood control and generation of hydroelectricity. The river is named after the Catawba tribe of Native Americans, which lives on its banks. In their language, they call themselves "yeh is-WAH h’reh", meaning "people of the river."
Lake Sharpe is a large reservoir impounded by Big Bend Dam on the Missouri River in central South Dakota, United States. The lake has an area of 56,884 acres (230.20 km2) and a maximum depth of 78 ft (24 m). Lake Sharpe is approximately 80 mi (130 km) long, with a shoreline of 200 mi (320 km). Lake Sharpe is the 54th largest reservoir in the United States. The lake starts near Ft. Thompson and stretches upstream to Oahe Dam, near Pierre. The lake is located within the following counties: Buffalo, Lyman, Hyde, Hughes, and Stanley. The Big Bend of the Missouri is about 7 miles (11 km) north of the dam.
Goose Pond is a 625-acre (2.5 km2) water body located in Grafton County in western New Hampshire, United States, in the towns of Canaan and Hanover. It is considered a great pond by the state of New Hampshire. The lake has 6.3 miles (10.1 km) of shoreline, and is approximately 3 miles (5 km) long by 0.5 miles (0.8 km) wide. All but the northernmost end of the pond is in the town of Canaan. The average depth of the pond is approximately 10 feet (3.0 m), with the deepest part approximately 35 feet (11 m). The lake is part of the Mascoma River watershed, flowing to the Connecticut River.
Grafton Pond is a 319-acre (1.3 km2) water body located in Grafton County in western New Hampshire, United States, in the town of Grafton. The pond is part of the Mascoma River watershed, flowing to the Connecticut River. Outflow from the pond travels through Bicknell Brook to Crystal Lake in Enfield, then north to the Mascoma River in West Canaan.
Pawtuckaway Lake is a 784-acre (3.17 km2) reservoir in Rockingham County in southeastern New Hampshire, United States, in the town of Nottingham. The lake is located in the Piscataqua River drainage basin.
Savoy, Mountain State Forest is a Massachusetts state forest located primarily in the towns of Savoy and Florida, with portions extending into neighboring Adams and North Adams. Situated along the Hoosac Mountain Range, it features four ponds, and seven hill and mountain summits, including Lewis Hill (2177 ft), Flat Rock Hill (2195 ft), Spruce Hill (2566 ft), and Borden Mountain (2505 ft). Also within the forest are at least two notable waterfalls, Parker Brook Falls and Tannery Falls, the latter of which is a 100-foot (30 m) drop. The forest is managed by the Department of Conservation and Recreation.
Lake Lashaway is a 293-acre (1.19 km2) pond located near the East Brookfield and North Brookfield, Massachusetts town line. The Lake Lashaway Community Association’s website is www.LakeLashaway.org. The town line cuts the lake approximately in half. The lake lies just to the north of state Route 9 as it passes through East Brookfield.
The Seven Mile River or Sevenmile River is a 9.6-mile-long (15.4 km) stream in central Massachusetts. It heads at Browning Pond, at the Oakham and Spencer border, and travels south through Spencer, following a short distance from State Route 31. It crosses under Route 31 the highway becomes Pleasant Street, then continues south along Old Meadow Road and under State Route 9 near the junction of State Route 49. It then parallels Route 9 to its south until it joins the East Brookfield River between Lake Lashaway and Quaboag Pond.
The Sugden Reservoir is a Massachusetts reservoir located in Spencer, Massachusetts. It forms the headwaters of Shaw Brook, which is a tributary to Turkey Hill Creek, a major tributary to the Seven Mile River. This water body is part of the Chicopee River Watershed.
Browning Pond is located in Oakham and Spencer, Massachusetts. This 89-acre (360,000 m2) great pond forms the headwaters of the Seven Mile River. It is part of the Chicopee River Watershed.
Split Rock Dam is a minor ungated concrete faced rock fill embankment dam with concrete chute spillway across the Manilla River upstream of Manilla in the north-western slopes region of New South Wales, Australia. The dam's purpose includes flood mitigation, irrigation, water supply and conservation. The impounded reservoir is called Split Rock Reservoir.
Tispaquin Pond is a 194-acre (0.79 km2) warm water pond in Middleborough, Massachusetts. The pond is in the Taunton River Watershed. The average depth of the pond is seven feet, and the maximum depth is eight feet. Transparency of the water is six feet. Shorts Brook and Woods Brook provide the inflow for the pond. The outflow is Fall Brook, a tributary of the Nemasket River. Camp Avoda and Camp Yomechas are located on the pond. Access to the southern shore of the pond is via Eldon Street off Rocky Gutter Street. An unpaved launch area is suitable for car top boats and canoes. It is a popular spot for recreational fishing, particularly for yellow perch and largemouth bass.
The Coolmunda Dam is an earth–fill embankment dam with a gated spillway across the Macintrye Brook, a tributary of the Dumaresq River, that is located on Darling Downs in Coolmunda, Goondiwindi Region, Queensland, Australia. The main purposes of the dam are for irrigation and potable water supply. The impounded reservoir is called the Lake Coolmunda.
Spencer State Forest is a Massachusetts state forest and recreation reserve located in the town of Spencer, managed by the Massachusetts Department of Conservation and Recreation. The 92 mile (148 km) Midstate Trail passes through the state forest. The Commonwealth of Massachusetts also conducts logging in some parts of the property.
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.
Carcoar Dam is a minor ungated concrete double parabolic arch dam with an uncontrolled overflow spillway across the Belubula River upstream of Carcoar in the central west region of New South Wales, Australia. The dam's purpose includes irrigation, water supply, and water conservation.
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.
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 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.
