The River Parrett flows through the counties of Dorset and Somerset in South West England, from its source in the Thorney Mills springs in the hills around Chedington in Dorset. Flowing northwest through Somerset and the Somerset Levels to its mouth at Burnham-on-Sea, into the Bridgwater Bay nature reserve on the Bristol Channel, the Parrett and its tributaries drain an area of 660 square miles (1,700 km2) – about 50 per cent of Somerset's land area, with a population of 300,000.
The River Huntspill is an artificial river, in the Somerset Levels, in the Sedgemoor district of Somerset, England. It was built in 1940 to supply process water to ROF Bridgwater, and has resulted in reduced flooding of the lower Brue Valley. Huntspill Sluice at the river's western end, also known as West Huntspill Sluice, separates it from the River Parrett.
The River Axe is a river in South West England. The river is formed by water entering swallets in the limestone and rises from the ground at Wookey Hole Caves in the Mendip Hills in Somerset, and runs through a V-shaped valley. The geology of the area is limestone and the water reaches Wookey Hole in a series of underground channels that have eroded through the soluble limestone. The river mouth is in Weston Bay on the Bristol Channel.
The River Cary is a river in Somerset, England. It is sourced from the Park Pond in Castle Cary and flows towards the southwest.
Somerset is a rural county in the southwest of England, covering 4,171 square kilometres (1,610 sq mi). It is bounded on the north-west by the Bristol Channel, on the north by Bristol and Gloucestershire, on the north-east by Wiltshire, on the south-east by Dorset, and on the south west and west by Devon. It has broad central plains with several ranges of low hills. The landscape divides into four main geological sections from the Silurian through the Devonian and Carboniferous to the Permian which influence the landscape, together with water-related features.
The Cass River is a 61.5-mile-long (99.0 km) river in the Thumb region of the U.S. state of Michigan. It drains large portions of Sanilac and Tuscola counties and smaller portions of Genesee, Huron, Lapeer, and Saginaw counties.
King's Sedgemoor Drain is an artificial drainage channel which diverts the River Cary in Somerset, England along the southern flank of the Polden Hills, to discharge into the River Parrett at Dunball near Bridgwater. As the name suggests, the channel is used to help drain the peat moors of King's Sedgemoor. There was opposition to drainage schemes from the local inhabitants, who feared that they would lose their common grazing rights. However, the main channel was constructed between 1791 and 1795, and despite some defects, brought some relief from flooding to the area.
Brush Creek is a 15.3-mile-long (24.6 km) tributary of Wills Creek in Pennsylvania in the United States.
Moxie Falls is a waterfall in Somerset County, Maine. At a vertical drop of over 90 feet (30 m) into a pool about 17 feet (5 m) deep, Moxie Falls is one of the highest falls in New England. The falls are part of Moxie Stream which flows from Moxie Pond into the Kennebec River approximately 1 kilometer (0.62 mi) downstream the falls. Moxie Stream drains Moxie Pond approximately 5 miles (8.0 km) upstream of the falls.
The Carrabassett River, a tributary of the Kennebec River, is located in Franklin County and Somerset County, Maine, in the United States. It rises near Sugarloaf Mountain, east of Rangeley Lake, and runs for 33.8 miles (54.4 km), flowing southeast past Kingfield and joining the Kennebec River in the town of Anson.
The Lees River or Lee's River, shown on federal maps as the Lee River, is a 2.9-mile-long (4.7 km) tidal river that forms part of the boundary between Swansea and Somerset, Massachusetts. It flows south to drain into Mount Hope Bay.
Moxie Mountain is a mountain located in Somerset County, Maine.
Bhargavi River flows across Odisha, India. It forms the Mahanadi–Kuakhai distributary system branching off from the Kuakhai River and draining into Chilka Lake.
The South Branch Penobscot River is a river in Somerset County, Maine. Its source, Penobscot lake, the north end of which at is about 1,000 feet (300 m) from the Canada–United States border in Sandy Bay. This section of the border runs along the height of land separating the watersheds of the Penobscot River and the Monument River, which feeds into the Saint Lawrence River.
The county of Somerset is in South West England, bordered by the Bristol Channel and the counties of Bristol and Gloucestershire to the north, and Wiltshire to the east, Dorset to the south, and Devon to the west. The climate, influenced by its proximity to the Atlantic Ocean and the prevailing westerly winds, tends to be mild, damp and windy.
The Sowy River is an artificial drainage channel in Somerset, England, designed to act as a flood relief channel for the River Parrett. Water from the Parrett can be diverted into it just below Langport, and is conveyed to the King's Sedgemoor Drain, which discharges back into the Parrett much nearer to its outfall into the Bristol Channel. Following extensive flooding of the surrounding land in 2014, new culverts to carry the river under the A372 road at Beer Wall were constructed, and a three-year project to raise the banks and widen the channel to increase its capacity was undertaken.
Rock Brook is a tributary of Beden Brook in Somerset County, New Jersey in the United States.
The Tarago River is a perennial river of the Western Port catchment, located in the West Gippsland region of the Australian state of Victoria.
The North Drain flows westerly from Hurn Sluice on the River Sheppey to the North Drain Pumping Station at the River Brue, in Somerset, England.
