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The Motlawa goes through Rokickie Lake to Martwa Wisła, a branch of the Vistula. [2] The total length of the river is estimated at 68 km, and its drainage basin is 1511.3 km 2. [3] The city of Gdańsk is situated at its mouth in the Martwa Wisła. In Gdańsk, the Motława ferry crosses the river, a service that has run since the year 1687. [4]
Nowa Motława (German: Neue Mottlau) is a branch of the Motława river in the district Śródmieście of the city of Gdańsk in Poland. It was artificially created in 1576. Nowa Motława and Motława are forming Granary Island (Polish: Wyspa Spichrzów, German: Speicherinsel).
Cuando River (Chobe River) (Linyanti River) Makwegana River (Selinda Spillway) (receives outflow from the Okavango during floods) Limpopo River. Shashe River.
The island Ołowianka on the river Motława is now connected by two bridges to the river banks. It is believed that since 1687 there has been a ferry between the island and the city. It is believed that since 1687 there has been a ferry between the island and the city.
The Motloutse River is a river in Botswana, a tributary of the Limpopo River.The catchment area is 19,053 square kilometres (7,356 sq mi). The Letsibogo Dam on the Motloutse has been built to serve the industrial town of Selebi-Phikwe and surrounding local areas, with potential for use in irrigation.
The Molopo River (Afrikaans: Moloporivier) is one of the main rivers in Southern Africa. It has a length of approximately 960 kilometres and a catchment area of 367,201 km 2 with Botswana , Namibia and South Africa sharing roughly about a third of the basin each.
The Ottawa River drains into the Lake of Two Mountains and the St. Lawrence River at Montreal. The river is 1,271 km (790 mi) long; it drains an area of 146,300 km 2 (56,500 sq mi), 65 per cent in Quebec and the rest in Ontario, with a mean discharge of 1,950 m 3 /s (69,000 cu ft/s). [1]
The Morava is a lowland river with a basin that consists of 51% plains; mountains make up only seven percent of the basin while thirty five percent are considered highland. The average slope of the river is 1.8‰ and at the confluence 4‰. The bedrock of the river basin is mostly crystalline bedrock and flysch. [2]