Segen River

Last updated

Segen is a river that arises from Delo Mountain, central Amarro, Ethiopia. The river flows to the east, then to the north and to the west and last to the south to join the Weito River. On the western side of Amarro horst the valley through which the river flows is called Segen Valley.

Ethiopia country in East Africa

Ethiopia, Oromo: Itiyoophiyaa, Somali: Itoobiya, Hebrew: אתיופיה -officially the Federal Democratic Republic of Ethiopia, is a country in the northeastern part of Africa, popularly known as the Horn of Africa. It shares borders with Eritrea to the north, Djibouti to the northeast, and Somalia to the east, Sudan and South Sudan to the west, and Kenya to the south. With over 102 million inhabitants, Ethiopia is the most populous landlocked country in the world and the second-most populous nation on the African continent that covers a total area of 1,100,000 square kilometres (420,000 sq mi). Its capital and largest city is Addis Ababa, which lies a few miles west of the East African Rift that splits the country into the Nubian Plate and the Somali Plate.

The Weito River is a river in the Southern Nations, Nationalities, and Peoples' Region of Ethiopia. It rises in the Guge Mountains, flowing south into Lake Chew Bahir at latitude and longitude 4°49′58″N36°58′54″E.


Related Research Articles

Rhine river in Western Europe

The Rhine is a European river that begins in the Swiss canton of Graubünden in the southeastern Swiss Alps, forms part of the Swiss-Liechtenstein, Swiss-Austrian, Swiss-German and then the Franco-German border, then flows through the German Rhineland and the Netherlands and eventually empties into the North Sea.

Valley Low area between hills, often with a river running through it.

A valley is a low area between hills or mountains typically with a river running through it. In geology, a valley or dale is a depression that is longer than it is wide. The terms U-shaped and V-shaped are descriptive terms of geography to characterize the form of valleys. Most valleys belong to one of these two main types or a mixture of them, at least with respect to the cross section of the slopes or hillsides.

Assiniboine River river in Saskatchewan and Manitoba, Canada

The Assiniboine River is a 1,070-kilometre (660 mi) river that runs through the prairies of Western Canada in Saskatchewan and Manitoba. It is a tributary of the Red River. The Assiniboine is a typical meandering river with a single main channel embanked within a flat, shallow valley in some places and a steep valley in others. Its main tributaries are the Qu'Appelle, Souris and Whitesand Rivers. For early history and exploration see Assiniboine River fur trade.

The Tioughnioga River is a 34.2-mile-long (55.0 km) tributary of the Chenango River in central New York in the United States. It drains a dissected plateau area east of the Finger Lakes at the northernmost edge of the watershed of the Susquehanna River.

Feather River river in the United States of America

The Feather River is the principal tributary of the Sacramento River, in the Sacramento Valley of Northern California. The river's main stem is about 73 miles (117 km) long. Its length to its most distant headwater tributary is just over 210 miles (340 km). The main stem Feather River begins in Lake Oroville, where its four long tributary forks join together—the South Fork, Middle Fork, North Fork, and West Branch Feather Rivers. These and other tributaries drain part of the northern Sierra Nevada, and the extreme southern Cascades, as well as a small portion of the Sacramento Valley. The total drainage basin is about 6,200 square miles (16,000 km2), with approximately 3,604 square miles (9,330 km2) above Lake Oroville.

River Worth river in the United Kingdom

The River Worth is a river in West Yorkshire, England. It flows from minor tributaries on the moors above Watersheddles Reservoir down the Worth Valley to Haworth, where it is joined by Bridgehouse Beck which flows from Oxenhope. The River Worth is itself a tributary of the River Aire, which it joins at the end of the Worth Valley in Keighley.

River Culm river in the United Kingdom

The River Culm flows through the Devon Redlands in Devon, England and is the longest tributary of the River Exe. It rises in the Blackdown Hills at a spring near RAF Culmhead in Somerset, and flows west through Hemyock, then Culmstock to Uffculme. The river turns south, through Cullompton, skirting the northern boundary of Killerton Park to join the River Exe on the north-western outskirts of Exeter. The name of the river is thought to mean 'knot' or 'tie', in reference to the river's twists and loops.

River Roding river in the United Kingdom

The River Roding is a river in England that rises at Molehill Green near Dunmow in Essex. It then flows south through Essex and London and forms Barking Creek as it reaches the River Thames.

Sutlej river in India

The Sutlej River (Punjabi: ਸਤਲੁਜ, Sanskrit: शतद्रुम, , is the longest of the five rivers that flow through the historic crossroads region of Punjab in northern India and Pakistan. The Sutlej River is also known as Satadree It is addressed as Shatarudra by the Gorkhalis. It is the easternmost tributary of the Indus River.

Drainage divide Line that separates neighbouring drainage basins

A drainage divide, water divide, divide, ridgeline, watershed, or water parting is the line that separates neighbouring drainage basins. On rugged land, the divide lies along topographical ridges, and may be in the form of a single range of hills or mountains, known as a dividing range. On flat terrain, especially where the ground is marshy, the divide may be harder to discern.

Meander A sinuous bend in a series in the channel of a river

A meander is one of a series of regular sinuous curves, bends, loops, turns, or windings in the channel of a river, stream, or other watercourse. It is produced by a stream or river swinging from side to side as it flows across its floodplain or shifts its channel within a valley. A meander is produced by a stream or river as it erodes the sediments comprising an outer, concave bank and deposits this and other sediment downstream on an inner, convex bank which is typically a point bar. The result of sediments being eroded from the outside concave bank and their deposition on an inside convex bank is the formation of a sinuous course as a channel migrates back and forth across the down-valley axis of a floodplain. The zone within which a meandering stream shifts its channel across either its floodplain or valley floor from time to time is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering problems for local municipalities attempting to maintain stable roads and bridges.

Mahoning Valley (geographic)

The Mahoning Valley is a geographic valley encompassing the area of northeast Ohio and northwest Pennsylvania that drains into the Mahoning River. The Mahoning and Shenango rivers empty into the Beaver River, which empties into the Ohio River. The Mahoning River flows through Lawrence County and the Shenango River flows through Mercer County in Pennsylvania, and then the Mahoning River flows from Stark, Mahoning, Trumbull, and Portage counties in Ohio. The three main tributaries of the Mahoning River are Mosquito Creek, West Branch, and Eagle Creek, all in Ohio. It is often referred to by locals as the "Ho".

Freital Place in Saxony, Germany

Freital is a town in the district of Sächsische Schweiz-Osterzgebirge in the Free State of Saxony, Germany. The town is situated on a small river, the Weißeritz, and is 8 kilometres southwest of Dresden.

Shyok River river in India

The Shyok River flows through northern Ladakh in India and the Ghangche District of Gilgit–Baltistan of Pakistan spanning some 550 km (340 mi).

Brahmaputra Valley

The Brahmaputra Valley is a region situated between hill ranges of the eastern and northeastern Himalayan range in Eastern India.

The Great Valley is a west-to-east valley through the center of Chester County, Pennsylvania, United States. It is also sometimes referred to as Chester Valley, and both names are in use throughout the region. The valley stretches from the Schuylkill River in Montgomery County in the east, southwesterly through Chester and Lancaster counties. The valley is most distinct in central Chester County, although traces of it can be followed almost the entire distance between the Delaware and Susquehanna rivers.

Passumpsic River river in the United States of America

The Passumpsic River is a 22.7-mile-long (36.5 km) tributary of the Connecticut River, in Vermont. Though primarily a Caledonia County river, it is the only river to flow through all three counties of the Northeast Kingdom.

River Natural flowing watercourse

A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as stream, creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague.

Surkhi Parsa District District in Parwan Province, Afghanistan

Surkh-o- Parsa sometimes spelt as Surkhi Parsa is a district in Parwan Province, Afghanistan. The center of the district is called Lulinj and is a green valley around a river.

Mezitli River river in Turkey

Mezitli River is a rivulet in Mersin Province, Turkey