New Marlborough is a town in Berkshire County, Massachusetts, United States. It is part of the Pittsfield, Massachusetts Metropolitan Statistical Area. The population was 1,509 at the 2010 census. New Marlborough consists of five villages: Clayton, Hartsville, Mill River, New Marlborough Village and Southfield.
The Connecticut River is the longest river in the New England region of the United States, flowing roughly southward for 406 miles (653 km) through four states. It rises at the U.S. border with Quebec, Canada, and discharges at Long Island Sound. Its watershed encompasses 11,260 square miles (29,200 km2), covering parts of five U.S. states and one Canadian province, via 148 tributaries, 38 of which are major rivers. It produces 70% of Long Island Sound's fresh water, discharging at 18,400 cubic feet (520 m3) per second.
The Housatonic River is a river, approximately 149 miles (240 km) long, in western Massachusetts and western Connecticut in the United States. It flows south to southeast, and drains about 1,950 square miles (5,100 km2) of southwestern Connecticut into Long Island Sound. Its watershed is just to the west of the watershed of the lower Connecticut River.
The Lackawanna River is a 42-mile-long (68 km) tributary of the Susquehanna River in northeastern Pennsylvania in the United States. It flows through a region of the northern Pocono Mountains that was once a center of anthracite coal mining in the United States. It starts in north Wayne County, Pennsylvania and ends in east Luzerne County, Pennsylvania in Duryea, Pennsylvania. The lower reaches of the river flow through the urban areas of Scranton, which grew around its banks in the 19th century as an industrial center. Its name comes from a Lenni Lenape word meaning "stream that forks".
The Caney Fork River is a river that flows through central Tennessee in the United States, draining a substantial portion of the southwestern Cumberland Plateau and southeastern Highland Rim regions. It is a major tributary of the Cumberland River, and is part of the Cumberland, Ohio and Mississippi basins. The river is 143 miles (230 km) long, and its watershed covers 1,771 square miles (4,590 km2) in eleven counties. Monterey, Baxter, Sparta, Smithville, McMinnville, Altamont, Spencer and Gordonsville are among the towns that are at least partially drained by the river.
Campbell Falls State Park Reserve is an undeveloped, public recreation area and nature preserve located in the town of Norfolk, Connecticut. The 102-acre (41 ha) state park offers hiking, stream fishing, and views of the park's namesake waterfall which cascades nearly 100 feet (30 m) on the Whiting River just north of the Connecticut/Massachusetts state line. Legislation passed in 1923 and 1924 provided for the joint management of the park after the land was donated to the two states by the White Memorial Foundation. A stone monument within the park marks the border between the states.
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.
The Powwow River is a 22.8-mile-long (36.7 km) river located in New Hampshire and Massachusetts in the United States. It is a tributary of the Merrimack River, part of the Gulf of Maine watershed.
The Dowagiac River is a southwesterly flowing 30.9-mile-long (49.7 km) stream in the Lower Peninsula of the U.S. state of Michigan. It is tributary to the St. Joseph River which flows, in turn, into eastern Lake Michigan.
The Ware River is a 35.4-mile-long (57.0 km) river in central Massachusetts. It has two forks, the both of which begin in Hubbardston, Massachusetts. The Ware River flows southwest through the middle of the state, joins the Quaboag River at Three Rivers, Massachusetts, to form the Chicopee River on its way to the Connecticut River.
The Quaboag River is a 25.7-mile-long (41.4 km) river in Massachusetts that heads at Quaboag Pond in Brookfield at an elevation of 594 feet (181 m) above sea level. It flows west to the village of Three Rivers, Massachusetts, at an elevation of 290 feet (88 m).
The Millers River is a 52.1-mile-long (83.8 km) river in northern Massachusetts, originating in Ashburnham and joining the Connecticut River just downstream from Millers Falls, Massachusetts. The river was formerly known as Paquag or Baquag, a Nipmuc word meaning "clear water". Sections of the river are used for whitewater kayaking, and a section upriver is popular with flatwater racers.
The Quinebaug River is a river in south-central Massachusetts and eastern Connecticut, with watershed extending into western Rhode Island. The name "Quinebaug" comes from the southern New England Native American term, spelled variously Qunnubbâgge, Quinibauge, etc., meaning "long pond", from qunni-, "long", and -paug, "pond". The river is one of the namesake rivers in the Quinebaug and Shetucket Rivers Valley National Heritage Corridor.
The Elk River Chain of Lakes Watershed is a 75-mile-long (121 km) waterway consisting of 14 lakes and connecting rivers in the northwestern section of the Lower Peninsula of the U.S. state of Michigan, which empty into Lake Michigan.
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 Sebec River is a tributary of the Piscataquis River in Piscataquis County, Maine. From the outflow of Sebec Lake in Sebec, the river runs 10.0 miles (16.1 km) east and southeast to its confluence with the Piscataquis in Milo.
Roaring Brook is a tributary of Hunlock Creek in Luzerne County, Pennsylvania, in the United States. It is approximately 5.0 miles (8.0 km) long and flows through Ross Township and Hunlock Township. The watershed of the stream has an area of 6.17 square miles (16.0 km2). It has one named tributary, which is known as Lewis Run. Additionally, a dammed pond known as Harris Pond is located at the stream's headwaters. The Roaring Brook Swamp, which is listed as a Locally Significant Area on the Luzerne County Natural Areas Inventory, is also located in the watershed.
The Middle Branch Croton River is a tributary of the Croton River in Putnam and Westchester counties in the state of New York. It lies within the Croton River watershed and is part of the New York City water supply system's Croton Watershed.
The Blackberry River is a westward-flowing river located entirely in the far northwest corner of the U.S. state of Connecticut. The river runs for nine miles (14 km) through the towns of Norfolk and North Canaan, where it empties into the Housatonic River. The river provided waterpower for industrial purposes from the early 1700s through the first part of the 20th century.
The Bantam River is a two-part, southward-flowing stream located in northwest Connecticut in the United States. The full river comprises two streams that flow into and out of Bantam Lake and that are referred to as Bantam Lake Inlet and Bantam Lake Outlet. The two sections of the river enter and leave Bantam Lake at points approximately 2,800 feet (850 m) apart on the lake's north shore. The river drains an area of more than 25,000 acres (10,000 ha) in the towns of Goshen, Litchfield, Morris, and Washington. Its total course is approximately 18 miles (29 km) in length. The river rises in the marsh area north of the Litchfield Reservoir and empties into the Shepaug River. It forms the southern boundary of Mount Tom State Park.
