Pungwe River (Portuguese: Rio Púngoè or Rio Púnguè ) is a 400 km (250 mi) long river in Zimbabwe and Mozambique . It rises below Mount Nyangani in the Eastern Highlands of Zimbabwe and then flows southeastwards through the Manica and Sofala provinces of Mozambique. The Pungwe enters the Urema Valley , the southernmost portion of the Great Rift Valley , where it forms the southern boundary of Gorongosa National Park . The Urema River joins it, and the river follows the rift valley southward. Large seasonal wetlands form around the Pungwe and Urema rivers in the rift valley section. It empties into the Mozambique Channel at Beira , forming a large estuary. It is one of the major rivers of Mozambique and often causes floods.
7-758: The principal left tributaries are, from upstream to downstream, the Nhazonia, Txatola, Vinduzi, and Nhandugue-Urema. The right tributaries are the Honde and the Muda. Administratively, the Pungwe Basin covers parts of Sofala and Manica provinces in Mozambique, and a large part of Mutasa District in Zimbabwe. A small portion of the basin in Zimbabwe falls in Nyanga District . As of 2003,
14-673: Is a river in Eastern Highlands of Zimbabwe which runs through the Honde Valley . It flows from Mount Inyangani on the western edges of Honde Valley where it is joined by several of its major tributaries: the rivers Mupenga, Buu, Mtarazi and Ngarura. It deposits its waters into the Pungwe River , already in Mozambique, which in turn empties in the Indian Ocean. Mtarazi Falls , Zimbabwe's highest at 762 metres (2,500 ft) flows into
21-614: The Honde south of Pungwe Gorge at the Honde River valley just outside Nyanga National Park . Parts of the Honde in the southern Nyanga support lush vegetation, the closest Zimbabwe has to Jungle. Further south, the Honde provides water for communal irrigation in an otherwise dry area. The 500 square kilometres (190 sq mi) of the Honde Valley in Zimbabwe are extensively cultivated, often with gravity fed irrigation channels. Extensive use
28-768: The Pungwe River basin, with possibly severe consequences for agricultural production. While the between-year variability in flow is not predicted to change significantly, within-year variability is expected to increase . This will worsen both floods and droughts. Discharge of the Pungwe River at Jangada ( 19°26′56.7276″S 34°32′16.2204″E / 19.449091000°S 34.537839000°E / -19.449091000; 34.537839000 ). Period from 1998/01/01 to 2023/12/31 (Source: The Flood Observatory ): (m/s) (m/s) Honde River 18°29′05″S 32°51′08″E / 18.48470°S 32.85234°E / -18.48470; 32.85234 Honde River pronounced Horn-de
35-471: The Pungwe River through an inter-catchment transfer facility. The quantities transferred to are limited to a maximum of 0.7 cubic metres (25 cu ft)/second by the provisions of a water permit and system design. In addition, on 27 September 1995, it was agreed at a meeting of the Mozambican and Zimbabwean ministers responsible for water affairs that water could be abstracted from the Pungwe River to supply
42-514: The basin's population in Mozambique is estimated at 1,104,000 people and that for Zimbabwe at 96,000 people. Beira metropolitan area in Mozambique receives its water supply from the Pungwe River. The 2004 water demand from the Beira/Dondo water supply, which included the Mutua and Mafambisse areas, was estimated at 25,339 cubic metres (894,800 cu ft)/day. The city of Mutare is supplied from
49-555: The city of Mutare, with an upper limit of 1 cubic metre (35 cu ft)/second. Consequently, a fixed abstraction of 60,480 cubic metres (2,136,000 cu ft) per day by Mutare city has been adopted as water demand from the Pungwe River. The Mutasa Rural District is also expected to draw water from the Pungwe pipeline to supply villages along its route. Climate change is predicted to lead to about 10% reduction in annual rainfall. This implies decreased river flow and available water for
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