|
Kundalila Falls
Kundalila Falls is a waterfall on the Kaombe River in Zambia. It falls over the lip of the Muchinga escarpment and makes a waterfall near the small town of Kanona in the Serenje District. It is set in the wilderness on the edge of the Muchinga escarpment. It is the only waterfall of such grandeur that is set so high on the escarpment. The name 'Kundalila Falls' means "crying dove" in the local Bemba language. From top of the falls there are views over the Luangwa Valley which is part of the Albertine Rift, the western branch of the East African Rift The East African Rift (EAR) or East African Rift System (EARS) is an active continental rift zone in East Africa. The EAR began developing around the onset of the Miocene, 22–25 million years ago. In the past it was considered to be part of a .... In multiple stages the Kaombe River drops approximately 80m from the escarpment. At the foot of the fall is a natural deep pool surrounded by wild flowers. Visitors are allowed to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kundalila Falls
Kundalila Falls is a waterfall on the Kaombe River in Zambia. It falls over the lip of the Muchinga escarpment and makes a waterfall near the small town of Kanona in the Serenje District. It is set in the wilderness on the edge of the Muchinga escarpment. It is the only waterfall of such grandeur that is set so high on the escarpment. The name 'Kundalila Falls' means "crying dove" in the local Bemba language. From top of the falls there are views over the Luangwa Valley which is part of the Albertine Rift, the western branch of the East African Rift The East African Rift (EAR) or East African Rift System (EARS) is an active continental rift zone in East Africa. The EAR began developing around the onset of the Miocene, 22–25 million years ago. In the past it was considered to be part of a .... In multiple stages the Kaombe River drops approximately 80m from the escarpment. At the foot of the fall is a natural deep pool surrounded by wild flowers. Visitors are allowed to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zambia
Zambia (), officially the Republic of Zambia, is a landlocked country at the crossroads of Central Africa, Central, Southern Africa, Southern and East Africa, although it is typically referred to as being in Southern Africa at its most central point. Its neighbours are the Democratic Republic of the Congo to the north, Tanzania to the northeast, Malawi to the east, Mozambique to the southeast, Zimbabwe and Botswana to the south, Namibia to the southwest, and Angola to the west. The capital city of Zambia is Lusaka, located in the south-central part of Zambia. The nation's population of around 19.5 million is concentrated mainly around Lusaka in the south and the Copperbelt Province to the north, the core economic hubs of the country. Originally inhabited by Khoisan peoples, the region was affected by the Bantu expansion of the thirteenth century. Following the arrival of European exploration of Africa, European explorers in the eighteenth century, the British colonised the r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Serenje District
Serenje is a town of Serenje District, Zambia, lying just off the Great North Road and TAZARA Railway. Serenje has a railway station on the TAZARA railway. Serenje is approximately 191 km from Kapiri Mposhi on the Great North Road. Mkushi is the district west of Serenje. The Mulembo Falls lie near the town. Economy The inhabitants of Serenje district engage in subsistence agriculture. Though the area is blessed with rich soils and thick forests, economic development appears to have eluded this Zambian rural outpost. Society Serenje is home to the Lala people whose primary language is ciLala. The Lala language, like most languages spoken on the Copperbelt and Central provinces of Zambia, is classified as belonging to the Bemba language group. The Lala people, like most ethnic groups in central and northern and northwestern parts of Zambia, are said to have descended from the Luba-Lunda Kingdom in present-day Congo DRC. Serenje district is constituted by a number of Chie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bemba Language
The Bemba language, ''ChiBemba'' (also ''Cibemba, Ichibemba, Icibemba'' and ''Chiwemba''), is a Bantu language spoken primarily in north-eastern Zambia by the Bemba people and as a lingua franca by about 18 related ethnic groups. History Bemba is one of the spoken languages in Zambia, spoken by many people who live in urban areas, and is one of Zambia's seven recognized regional languages. Zambia's first president, Kenneth Kaunda, though Malawian by descent, was raised in a Bemba-speaking community, and two of the four Zambian presidents since have been Bemba-speakers. The third president, Levy Mwanawasa, was a Lenje, from the Copperbelt Province who belong to the Bantu Botatwe (“three people”) ethnic grouping that comprises the Tonga-Lenje-Ila peoples. The Fourth President, Rupiah Bwezani Banda was a Chewa from the Eastern Province. In the years after the MMD took power in 1991, it was accused numerous times of promoting Bemba over other regional languages in the country ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Luangwa Valley
The Luangwa River is one of the major tributaries of the Zambezi River, and one of the four biggest rivers of Zambia. The river generally floods in the rainy season (December to March) and then falls considerably in the dry season. It is one of the biggest unaltered rivers in Southern Africa and the that make up the surrounding valley are home to abundant wildlife. Source and Upper-Middle Luangwa Valley ''Note: distances stated are approximate straight-line distances from source''. The Luangwa rises in the Lilonda and Mafinga Hills in north-east Zambia at an elevation of around 1500 m, near the border with Tanzania and Malawi, and flows in a southwesterly direction through a broad valley. About 150 km from its source it has dropped to an elevation of about 690 m and becomes a meandering river with a flood-plain several kilometres wide. Over the next 300 km the meanders increase, with many oxbow lakes and abandoned meanders. Near Mfuwe, the river's elevat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Albertine Rift
The Albertine Rift is the western branch of the East African Rift, covering parts of Uganda, the Democratic Republic of the Congo (DRC), Rwanda, Burundi and Tanzania. It extends from the northern end of Lake Albert to the southern end of Lake Tanganyika. The geographical term includes the valley and the surrounding mountains. Geology The Albertine Rift and the mountains are the result of tectonic movements that are gradually splitting the Somali Plate away from the rest of the African continent. The mountains surrounding the rift are composed of uplifted Pre-Cambrian basement rocks, overlaid in parts by recent volcanic rocks. Lakes and rivers The northern part of the rift is crossed by two large mountain ranges, the Rwenzori Mountains between Lake Albert and Lake Rutanzige (formerly Lake Edward) and the Virunga Mountains between Lake Rutanzige and Lake Kivu. The Virungas form a barrier between the Nile Basin to the north and east and the Congo Basin to the west and south. Lak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East African Rift
The East African Rift (EAR) or East African Rift System (EARS) is an active continental rift zone in East Africa. The EAR began developing around the onset of the Miocene, 22–25 million years ago. In the past it was considered to be part of a larger Great Rift Valley that extended north to Asia Minor. A narrow zone, the rift is a developing divergent tectonic plate boundary where the African Plate is in the process of splitting into two tectonic plates, called the Somali Plate and the Nubian Plate, at a rate of 6-7 mm per year. The rift system consists of three microplates, the Victoria Microplate to the north, and the Rovuma and Lwandle microplates to the south. The Victoria Microplate is rotating anti-clockwise with respect to the African plate. Its rotation is caused by the configuration of mechanically weaker and stronger lithospheric regions in the EARS. Extent A series of distinct rift basins, the East African Rift System extends over thousands of kilometers. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monuments And Historic Sites Of Zambia
This article gives lists of the National Monuments and other historic sites of Zambia, with a one- or two-line description providing links to details given on other pages. National Heritage Conservation Commission The Institution mandated by Cap 173 of the Laws of Zambia to manage and Conserve Zambia's outstanding Cultural and Natural Heritage resources is the National Heritage Conservation Commission (NHCC) which has its headquarters in usaka According to ICOMOS (see references), the NHCC's profile report, it lists over 4000 heritage sites in Zambia, including: * historic/architectural/buildings (over 384 sites) * historic sites (over 180 sites) * anthropological sites (over 189 sites) * engineering industrial structures (over 62 sites) * archaeological sites (over 2000 sites) * geomorphological sites, geophysical sites, palaeontological, ecology and other sites. However, only about 35% of the country's land area has been adequately surveyed for cultural heritage and, due to a s ... [...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] |
TAZARA
The Tazara Railway, also called the Uhuru Railway or the Tanzam Railway, is a railway in East Africa linking the port of Dar es Salaam in east Tanzania with the town of Kapiri Mposhi in Zambia's Central Province. The single-track railway is long and is operated by the Tanzania-Zambia Railway Authority (TAZARA). The governments of Tanzania, Zambia, and the People's Republic of China built the railway to eliminate landlocked Zambia's economic dependence on Rhodesia and South Africa, both of which were ruled by white-minority governments.Thomas W. Robinson and David L. Shambaugh. ''Chinese Foreign Policy: theory and practice'', 1994. Page 287. The railway provided the only route for bulk trade from Zambia's Copperbelt to reach the sea without having to transit white-ruled territories. The spirit of Pan-African socialism among the leaders of Tanzania and Zambia and the symbolism of China's support for newly independent African countries gave rise to Tazara's designation as t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waterfalls Of Zambia
A waterfall is a point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several ways, but the most common method of formation is that a river courses over a top layer of resistant bedrock before falling on to softer rock, which erodes faster, leading to an increasingly high fall. Waterfalls have been studied for their impact on species living in and around them. Humans have had a distinct relationship with waterfalls for years, travelling to see them, exploring and naming them. They can present formidable barriers to navigation along rivers. Waterfalls are religious sites in many cultures. Since the 18th century they have received increased attention as tourist destinations, sources of hydropower, andparticularly since the mid-20th centuryas subjects of research. Definition and terminology A waterfall is general ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geography Of Central Province, Zambia
Geography (from Greek: , ''geographia''. Combination of Greek words ‘Geo’ (The Earth) and ‘Graphien’ (to describe), literally "earth description") is a field of science devoted to the study of the lands, features, inhabitants, and phenomena of Earth. The first recorded use of the word γεωγραφία was as a title of a book by Greek scholar Eratosthenes (276–194 BC). Geography is an all-encompassing discipline that seeks an understanding of Earth and its human and natural complexities—not merely where objects are, but also how they have changed and come to be. While geography is specific to Earth, many concepts can be applied more broadly to other celestial bodies in the field of planetary science. One such concept, the first law of geography, proposed by Waldo Tobler, is "everything is related to everything else, but near things are more related than distant things." Geography has been called "the world discipline" and "the bridge between the human and th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Albertine Rift")
