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Kafue Ferry
Kafue is a town in the Lusaka Province of Zambia and it lies on the north bank of the Kafue River, after which it is named. It is the southern gateway to the central Zambian plateau on which Lusaka and the mining towns of Kabwe and the Copperbelt are located.Camerapix: "Spectrum Guide to Zambia." Camerapix International Publishing, Nairobi, 1996. It is located on the T2 Road ( Great North Road). Site Kafue is at the south-eastern foot of a range of granite hills rising 200 m and extending over an area of about 250 km², and occupies a shelf of land between the hills and the river, just high enough to avoid its annual flood. The town extends along some shallow valleys between the hills. A 400 m wide strip of small farms and gardens separates the town from a bend of the river which is about 300 m wide in the dry season and 1.3 km wide in the rainy season, sometimes inundating a floodplain 10 km wide on the opposite bank, which consequently is uninhabited save for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flag Of Zambia
The flag of Zambia is the national flag of Zambia. It was adopted upon independence on 24 October 1964, by the first Republican President Dr. Kenneth David Kaunda. Before that, Zambia was the British protectorate of Northern Rhodesia and used a defaced Blue Ensign as its flag. The current flag is used as both national flag and ensign. It is green with an orange-coloured African fish eagle in flight over a rectangular block of three vertical stripes, coloured, from left to right: red, black and orange. The placement of the eagle and block of stripes at the flag's Fly (flag), fly is notable as most emblems and devices on flags are placed at centre or at the hoist. Green stands for the nation's lush flora, red for the nation's struggle for Freedom (political), freedom, black for the Zambian people, and orange for the land's natural resources and mineral wealth. Additionally, the Eagle (heraldry), eagle flying above the coloured stripes is intended to represent the people's ability ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chirundu Bridge
The Chirundu Bridge now consists of two road bridges side by side across the Zambezi River between the small town of Chirundu, Zambia and the village of Chirundu, Zimbabwe. At this location around 65 km downstream from the Kariba Dam the river is about 400 m wide. The bridges carry the Harare to Lusaka section of the Great North Road, which extends between South Africa and East Africa, and was once seen as part of a Cape to Cairo Road. Chirundu is the only town on the Zambezi where two bridges cross the river. The Otto Beit Bridge (1939) The first Chirundu Bridge is the Otto Beit Bridge built in 1938-9 by Dorman Long and financed by the Beit Trust, which funded most of central and southern Africa's colonial era bridges including the Beit Bridge across the Limpopo River, the Kafue Bridge, and the Luangwa Bridge. The Otto Beit Bridge was the first modern suspension bridge outside the United States built with parallel wire cables. It has a span of 382 m (main span 320 m). ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zimbabwe
Zimbabwe (), officially the Republic of Zimbabwe, is a landlocked country located in Southeast Africa, between the Zambezi and Limpopo Rivers, bordered by South Africa to the south, Botswana to the south-west, Zambia to the north, and Mozambique to the east. The capital and largest city is Harare. The second largest city is Bulawayo. A country of roughly 15 million people, Zimbabwe has 16 official languages, with English, Shona language, Shona, and Northern Ndebele language, Ndebele the most common. Beginning in the 9th century, during its late Iron Age, the Bantu peoples, Bantu people (who would become the ethnic Shona people, Shona) built the city-state of Great Zimbabwe which became one of the major African trade centres by the 11th century, controlling the gold, ivory and copper trades with the Swahili coast, which were connected to Arab and Indian states. By the mid 15th century, the city-state had been abandoned. From there, the Kingdom of Zimbabwe was established, fol ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Great North Road (Zambia)
The Great North Road is a major route in Zambia, running north from Lusaka through Kabwe, Kapiri Mposhi (the road continues by way of a right turn just north of Kapiri Mposhi), Serenje, Mpika (where it makes a left turn), Kasama, Mbala and Mpulungu. 82km North of Mpika is a signposted right turn onto a well maintained gravel road leading to Shiwa Ng'andu (12km) and Kapishya Hot Springs (32km). The road from Zambia's border with Zimbabwe at Chirundu to Lusaka is now regarded as being part of the Great North Road; but this is only since the opening of the Chirundu Bridge in 1939 - before that, the Great North Road ran from Livingstone to Lusaka, as part of the original Cape to Cairo Red Line by Cecil John Rhodes. The portion from Mbala to Mpulungu could be regarded as a spur linking to the Lake Tanganyika steamer service which was popular with travellers up to the 1950s. When the Mpika-Tanzania highway (the Tanzam Highway) via Tunduma was upgraded in the 1960s and provided a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kafue Bridge
Kafue is a town in the Lusaka Province of Zambia and it lies on the north bank of the Kafue River, after which it is named. It is the southern gateway to the central Zambian plateau on which Lusaka and the mining towns of Kabwe and the Copperbelt are located.Camerapix: "Spectrum Guide to Zambia." Camerapix International Publishing, Nairobi, 1996. It is located on the T2 Road ( Great North Road). Site Kafue is at the south-eastern foot of a range of granite hills rising 200 m and extending over an area of about 250 km², and occupies a shelf of land between the hills and the river, just high enough to avoid its annual flood. The town extends along some shallow valleys between the hills. A 400 m wide strip of small farms and gardens separates the town from a bend of the river which is about 300 m wide in the dry season and 1.3 km wide in the rainy season, sometimes inundating a floodplain 10 km wide on the opposite bank, which consequently is uninhabited save fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zambia Railways
Zambia Railways (ZR) is the national railway company of Zambia, one of the two major railway organisations in Zambia. The other system is the binational TAZARA Railway (TAZARA) that interconnects with the ZR at Kapiri Mposhi and provides a link to the Tanzanian port of Dar es Salaam. History The gauge Cape gauge ZR network was built during British colonial rule as part of the vision of the Cape-Cairo railway but the economic spur was to access the mines of Central Africa. The railway started as part of Rhodesia Railways, the company which ran the railways of Northern Rhodesia and Southern Rhodesia as an integrated operation, which was one of the largest employers and enterprises in both countries. The railway arrived in the future Zambia early in 1905 when the 150 km Livingstone-Kalomo line was built in advance of completion in September of that year of the Victoria Falls Bridge from the then Southern Rhodesia to Livingstone. The first wagons on the line were hauled by ox ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kafue Railway Bridge
The Kafue Railway Bridge was built to carry the Livingstone to Lusaka railway line in what is now Zambia over the Kafue River in 1906. It is a steel girder truss bridge of 13 spans each of supported on concrete piers. It was built for Mashonaland Railways, later merged into Rhodesian Railways which operated the line from 1927 until succeeded in Zambia by Zambia Railways in 1966. With a length of the Kafue Railway Bridge was the longest bridge on the Rhodesian Railways network. It includes nearly of embankments raised about where the line crosses the river's wider rainy season channel, and a lower embankment about long where it crosses the river's the shallower floodplain to the south-west of the bridge. The bridge is visible at decimal latitude/longitude -15.7876, 28.1766. The town of Kafue is at the bridge's northern end and the Kafue Bridge on the Great North Road is downstream. See also History of Zambia The history of Zambia experienced many stages from colonization t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rift Valley
A rift valley is a linear shaped lowland between several highlands or mountain ranges created by the action of a geologic rift. Rifts are formed as a result of the pulling apart of the lithosphere due to extensional tectonics. The linear depression may subsequently be further deepened by the forces of erosion. More generally the valley is likely to be filled with sedimentary deposits derived from the rift flanks and the surrounding areas. In many cases rift lakes are formed. One of the best known examples of this process is the East African Rift. On Earth, rifts can occur at all elevations, from the sea floor to plateaus and mountain ranges in continental crust or in oceanic crust. They are often associated with a number of adjoining subsidiary or co-extensive valleys, which are typically considered part of the principal rift valley geologically. Earth's rift valleys The most extensive rift valley is located along the crest of the mid-ocean ridge system and is the result of s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zambezi
The Zambezi River (also spelled Zambeze and Zambesi) is the fourth-longest river in Africa, the longest east-flowing river in Africa and the largest flowing into the Indian Ocean from Africa. Its drainage basin covers , slightly less than half of the Nile's. The river rises in Zambia and flows through eastern Angola, along the north-eastern border of Namibia and the northern border of Botswana, then along the border between Zambia and Zimbabwe to Mozambique, where it crosses the country to empty into the Indian Ocean. The Zambezi's most noted feature is Victoria Falls. Its other falls include the Chavuma Falls at the border between Zambia and Angola, and Ngonye Falls near Sioma in western Zambia. The two main sources of hydroelectric power on the river are the Kariba Dam, which provides power to Zambia and Zimbabwe, and the Cahora Bassa Dam in Mozambique, which provides power to Mozambique and South Africa. Additionally, two smaller power stations are along the Zambezi Riv ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zambezi Escarpment
Zambezi Escarpment is a name used for the escarpments forming both sides of the rift valley or graben in which lie the middle Zambezi river and Lake Kariba. They are fault scarps, rising 500 to 600 m higher than the lake or river, running from the Batoka Gorge roughly 800 km to the lower Zambezi, and facing each other about 50 to 100 km apart, closer in the west and opening up in the east. The northern Zambezi Escarpment in Zambia is steeper. It is somewhat broken north of Lake Kariba, but is particularly steep and well-formed from a point north of Siavonga going east through the Lower Zambezi National Park to the Luangwa River. Along this section the bottom of the valley is relatively flat and provides a sharp contrast to the scarps. The southern Zambezi Escarpment in Zimbabwe is quite marked in the west at the Chizarira Hills and the Chizarira National Park, but the slope becomes more broken and gentler further east around Matusadona National Park. It becomes steep ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kafue Gorge
Kafue is a town in the Lusaka Province of Zambia and it lies on the north bank of the Kafue River, after which it is named. It is the southern gateway to the central Zambian plateau on which Lusaka and the mining towns of Kabwe and the Copperbelt are located.Camerapix: "Spectrum Guide to Zambia." Camerapix International Publishing, Nairobi, 1996. It is located on the T2 Road ( Great North Road). Site Kafue is at the south-eastern foot of a range of granite hills rising 200 m and extending over an area of about 250 km², and occupies a shelf of land between the hills and the river, just high enough to avoid its annual flood. The town extends along some shallow valleys between the hills. A 400 m wide strip of small farms and gardens separates the town from a bend of the river which is about 300 m wide in the dry season and 1.3 km wide in the rainy season, sometimes inundating a floodplain 10 km wide on the opposite bank, which consequently is uninhabited save fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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