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Rivers of Ghana (2 C, 34 P) Pages in category "Bodies of water of Ghana" This category contains only the following page. This list may not reflect recent changes. G.
In 1961, the Government of Ghana assumed ownership of the lagoon. It dredged the water body and raised the level of some nearby land, to reduce the risk of flooding, then established industries on surrounding drained and reclaimed land—initially brewing and food processing, later car repairs and then electronic scrap processing at Agbogbloshie.
This is a list of rivers in Ghana. This list is arranged by drainage basin, with respective tributaries indented under each larger stream's name. Ghana The Pra River ...
Bodies of water of Ghana (4 C, 1 P) D. Dams in Ghana (1 C, 7 P) F. Fishing in Ghana (1 C, 2 P) Floods in Ghana (11 P) H. Hydroelectricity in Ghana (2 C) S.
South Ghana contains evergreen and semi-deciduous forests consisting of trees such as mahogany, odum, ebony and it also contains much of Ghana's oil palms and mangroves with shea trees, baobabs and acacias found in the northern part of Ghana. Its southernmost coast at Cape Three Points is 4° 30' north of the equator. [1]
The water supply and sanitation sector in Ghana is a sector that is in charge of the supply of healthy water and also improves the sanitation of water bodies in the country. In Ghana, the drinking water supply and sanitation sectors face a number of issues, including relatively limited sanitation access, intermittent supply , significant water ...
Keta Lagoon, also called Anlo-Keta lagoon, is the largest of the over 90 lagoons [2] that cover the 550 km [3] stretch of the coastline of Ghana. This lagoon is 126.13 km in length. It is located in the eastern coast of Ghana and separated from the Gulf of Guinea [4] by a narrow strip of sandbar. This open salty water is surrounded by flood ...
The Birim River basin lies in the Man Shield area of the West African craton, which has been overlaid by Early Proterozoic metasedimentary Birimian rocks. These rocks appear to have originated in mid-oceanic arcs of volcanoes, which formed a crust that collided with and rode over the Man shield portion of the West African Craton and was compressed to form a series of folds generally trending ...