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Get the Hwange, Matabeleland North local weather forecast by the hour and the next 10 days.
Hwange is also a tourism centre due to the presence of the nearby Hwange National Park, the largest National Park in Zimbabwe. The national park is home to a vast number of elephant, giraffe, lion and other wildlife. Royal Bank Zimbabwe, a commercial bank, maintains a branch in the town. [5] Zimbabwe's biggest power plant, Hwange Thermal Power ...
Hwange National Park (formerly Wankie Game Reserve) is the largest natural reserve in Zimbabwe. It is around 14,600 sq km in area. It is around 14,600 sq km in area. It lies in the northwest of the country, just off the main road between Bulawayo and Victoria Falls .
Kazuma Pan National Park covers 31,300 hectares (77,000 acres) and is located in the northwest corner of Zimbabwe, between Kazungula and Hwange national parks, and south-west of Victoria Falls. Basically, it was developed as a safe haven for the animals during the hunting season, as it formed an extension of the Matetsi Safari Area.
Vic Falls is a major centre for outdoor pursuits in Zimbabwe, with people from all over the country and many parts of the world travelling to view the falls and the nearby Hwange National Park. Additionally, 110-year-old coal fired rail steamer offers meals to the Victoria Falls bridge and Zambian border.
Kazuma Pan National Park is situated in Zimbabwe's extreme north-western corner, lying on the Botswana border a short distance north-west of Hwange National Park.Some 77,345 acres (313 km 2) in area, it provides one of Zimbabwe's few areas of plains scenery, with good visibility and sparse but important mammal populations.
As seen in Hwange National Park, Zimbabwe's largest game reserve, the area is also known for its substantial wildlife population. However, the most famous geographic feature of Matebeleland North is Victoria Falls , the world's largest waterfalls that are located on the Zambezi river on the northern border of the province.
Tsholotsho is located in an area which once used to be a waterlogged basin over 250 million years ago. This basin can be traced as far north as Hwange and is responsible for the formation of the coal deposits in Hwange. Tsholotsho has two principal rivers which are Manzamnyama and Gwayi.