Kioga: see Kyoga Kyoga or Kioga, lake, c.100 mi (160 km) long, formed by the Victoria Nile, S central Uganda, E Africa. The Victoria Nile flows through the lake on its way from Lake Victoria to Lake Albert.The main inflow from Lake Victoria is regulated by the Nalubaale Power Station in Jinja.Another source of water is the Mount Elgon region on the border between Uganda . with swampy arms whose areas are relatively limited (Hurst and Phillips 1938). The water balance of Lake Kyoga, Uganda 343 Fig. The districts include Nakasongola, Apac, Amolator, Soroti, Lira, Kayunga . The 130 km stretch of the Nile from Lake Vic-toria to Lake Kyoga is termed the Victoria Nile. In contrast to lakes formed by rifting in the GLRA (Lakes Albert, Tanganyika and Malawi), lakes Victoria and Kyoga are the products of these downwarping processes and are linked hydraulically via the Victoria Nile River. The type, length and number of prey ingested by Nile perch changes with the Lake Kyoga is also known as a rift valley lake which is an extension of the Victoria Nile that flows through the lake and also its way from Lake Victoria to lake Albert, the major inlet from Lake Victoria is controlled by the Nalubaale power station in . Lakes are formed in different ways a. Discuss the formation of Kyoga basin and examine the economic viability of the lake to the region where it is located. Fold mountains iv. with swampy arms whose areas are relatively limited (Hurst and Phillips 1938). In 2004, ten districts and 192 beach management units bordering Lake Kyoga waters formed LAKIMO with support from UK Department for International Development (DFID). Lakes Albert, Edward and George lie on or close to the DRC border, while the marshy and ill-defined lake Kyoga lie in the center of Uganda. Sudan, they first settled at in Northern Uganda betore moving to their present homelands ? Its average depth reaches 3 m, its maximum depth is 5.7 m. The Victoria Nile flows through Lake Kyoga on its way from Lake Victoria to Lake Albert. The downwarping of the middle course of the Mara - Kagera River created the Lake Victoria basin. Chemchane Sebkha in Mauritania. The extensions of lake kyoga include lake kwania, lake Bisina and lake Opeta. The many-armed lake is shallow, with swampy, papyrus-reeded shores; masses of papyrus are broken loose by strong winds and at times have completely blocked the river. Uganda is a renown hub for both natural and man made lakes, as a country well watered with unceasing rains that make it a home to many fresh water lakes, including Lake Victoria which is arguably the largest fresh water lake in Africa. Navigation for shallow-draft vessels is possible between Namasagali and Masindi Port. thin lake (Lake Obweruka) was formed as combining the current Lake Edward and Lake Albert, and then Ruwenzori Mountains were uplifted, rivers which couldn't flow to west, formed Lake Victoria and Lake Kyoga. lake in the world 7], with an area of 69,000 km[2. formed in similar manner is inselbergs. c) (i) Lakes that have formed due to crustal warping in East Africa - Lake Victoria(- Lake Kyoga(- Lake Wamala(- Lake Kachira(1 x 2 = 2mks (ii) How crustal warping leads to the formation of lakes - Earth movements cause crustal downwarping (- This leads to the formation of a basin like depression This site has a direct connection with Lake Kyoga, but has been semi-isolated from Lake Victoria since the completion of . Block mountain ii. The basin lies along the north edge of the Tanzanian craton (continental core) and has been the site of deposition since precambrian time. It receives the outflow from the Victoria Nile and is drained northward and then westward over the low northern end of the Rift escarpment (the Murchison Falls) to Lake Albert. This may end up changing the direction of the rivers in the area. This cluster also includes the Victoria Nile sample population. Downwarping and upwarping are a result of such crustal movements that affect the river path and the profile of its bed. Kyoga or Kioga (kyō´gä), lake, c.100 mi (160 km) long, formed by the Victoria Nile, S central Uganda, E Africa. 2. Lake Kyoga is fed by the Victoria Nile. papyrus islands plug much of the angle formed by Lakes Kyoga and Lake Kwania as they merge int.o the Kyoga Nile (see Fig.!). Formed when rock masses are reduced in size after many years of erosion Examples are namuli - mozambique, homboli - mali Other smaller features which may be formed in smaller manner are inselbergs Formation of lakes A lake is hollow or depression on the surface of the earth which is filled with water. Once such depression occur it results into formation of Lakes when water collects on them. Downwarping lakes Are also called depression lakes They are usually shallow Formed when pats of the earth warped downwards and the sorrounding areas warped upwards They include Vi - victoria Ba -bangweull www.arena.co.ke 0713779527 ____ ____ seven countries. The submersion of macrophyte cover by the El Niño opened up the lake and exposed these . Lakes formed through down-warping are called depressional lakes. Located in central Uganda, Lake Kyoga is a shallow, 129km long lake which is part of the African Great Lakes system. The Kyoga catchment extends over 60 000 km2 which is ~25% of Uganda's surface area of 240 000 km2. A shallow lake - 10-12 feet deep - with dense floating papyrus fringes, it is an important fish ground for the local people. The lake's maximum depth ranges between 80 to 84 meters (262 to 276 feet) and has a 40-meter (130-foot) average depth. Location of Study Area Lake Kyoga (Figure 2) lies on the central African plateau (altitude of 1100 m), Answer (1 of 3): Lake Victoria formed in a down drop basin between two faults of the East African Rift System. River Nile was formed about 30,000 years ago. QN. The lake is around 3000 km2 and drains large parts of Uganda. Residual mountains Fold mountains Formed after sedimentary rock fold amt the edges Examples of fold mountains includes:atlas in north africa Cape ranges in . Water flows in from Lake Victoria then flows out to Lake Albert. Chemchane Sebkha in Mauritania. Na i The Food ofhaplochromine species surviving inthenearshore stations of Lake Lake Kyoga Integrated Management Organisation-LAKIMO has slipped into limbo because of lack of funds. It is a large shallow lake in Uganda about 1720km (660sq.mi). Kyoga provides transportation for a large cotton-growing region. The Victoria Nile has fingerlike extensions with a surface of Nile that flows its water in the lake on its way from Lake Victoria to lake Albert. Downwarping . Lake Kyoga, Uganda. Lake Kyoga was itself formed by back tilting of the Kafu River, which made a lake with the distinctive dendritic pattern of a drowned valley. Overview on Lake Victoria There are many lakes in Africa, but this article is about Lake Victoria. papyrus islands plug much of the angle formed by Lakes Kyoga and Lake Kwania as they merge int.o the Kyoga Nile (see Fig.!). Kisumu is a city that has developed and is continuing to grow than other cities like Nakuru, Nairobi and Mombasa.Kisumu city is located in Kisumu county .There are three nice places visit while in Kisumu. Roughly circular doming or downwarping is actually fairly common, but it's more rare for water to highlight it so clearly. 1 Map of the East African lake region (after Sutcliffe and Parks 1999). 3. This happens when there is pressure from either side of the rocks during compression. Kisumu city is nearby lake victoria which makes this place very unique.Lake victoria is the largest lake in kenya and it was formed by downwarping process.When you visit this place is . With a capacity of 2,424 cubic kilometers (1.965109 acres. It has been subject to repeated up and down . Lake Victoria flows through lake kyoga to lake albert and makes the albert Nile. The evolution of the Onega Trough is divided into three stages: pre-sill, or preparatory, subsynchronous, and post-sill. Playas/sebkha is a lake contained in an inland drainage basin in a desert formed when rain or flood water flows into a basin formed by crustal warping e.g. It formed when westward-flowing rivers were dammed by an upthrown crustal block. Lake Kyoga has many arms, and its surface area is around 1,720km². catfishes and lungfish (Worthington 1929). The 1,720km squared by area is a shallow lake that opens its elevation to 1,033 metres. The many-armed lake is shallow, with swampy, papyrus-reeded shores; masses of papyrus are broken loose by strong winds and at times have completely blocked the river. For example, Lake Victoria occupies 18800square kilometers that could have been used for other activities. Why is lake kyoga swampy - Lake Kyoga is a touristic lake situated in the centre of Uganda. Shared by three Eastern African counties, namely Uganda, Tanzania, and Kenya, Lake Victoria is a large freshwater lake in Eastern Africa. The Columbia Electronic Encyclopedia . Lake Kyoga has many arms, and its surface area is around 1,720km². The open waters of the lakes cover 2 600 km2. This study considers the role of sill genesis in the tectonic evolution of the Onega Trough during the Middle to Late Paleoproterozoic (Jatulian-Vepsian). km. miles) in area with mean depth of 3.6 m and maximum depth of 6 m [1] [2] . Figure 4. Down-warping is the downward movement of the land. Downwarping lakes Are also called depression lakes They are usually shallow Formed when pats of the earth warped downwards and the sorrounding areas warped upwards They include Vi - victoria Ba -bangweull www.arena.co.ke 0713779527 Cha -chad kyo -kyoga volcanic processes a. Which community below did not not settle settle in in Tanzania after migration from the Congo Basin? Lake Kyoga (also spelled Kioga) is a large shallow lake in Uganda, about 1,720 km 2 (660 sq mi) in area and at an elevation of 1,033 metres. Uganda, Northwest Uganda, Lake Kyoga is formed by the Victoria Nile in its middle course, and has many arms or tentacles. Mbabazi~. Lake Victoria is located in Africa occupying a shallow depression. When did the Rift Valley form? 27. Kyoga or Kioga (kyō`gä), lake, c.100 mi (160 km) long, formed by the Victoria Nile, S central Uganda, E Africa. The local basin draining directly into Lake Kyoga is 57,000 km2. The many-armed lake is shallow, with swampy, papyrus-reeded shores; masses of papyrus are broken loose by strong winds and at times have completely blocked the river. The lake has fingerlike extensions with a surface of 1,720 sq. it is found in central Uganda region in northwest of Lake Victoria. Lake Victoria, the second largest lake in the world, is shared by Uganda with Tanzania and Kenya. During its geological history, Lake Victoria went through changes ranging from its present shallow depression, through to what may have been a series of much smaller lakes. Block K1: Lake Kyoga (1967 and 1968) - after the Nile perch were well established and haplochromines had been depleted. The shallow lake has large areas of papyrus swamp. Lakes and other water bodies are also affec. Lake Kyoga is a large shallow lake in Uganda of about 1720 km 2 (660 sq. The Lake Tahoe Basin was formed by vertical motion (normal) faulting. A lake is hollow or depression on the surface of the earth which is filled with water. Lakes that have formed due to crustal warping in East Africa . Lake Victoria overflowed at the lowest point on its watershed at Jinja to form the stretch of the Nile between Lakes Victoria and Kyoga and then further on to Lake Albert. The victoria Nile plungs via the lake making its way from the Uganda's largest lake Victoria, waving to Lake Albert.Kyoga prominently forms part of the Great Lakes System. 35 million years ago. Lake Kyoga was formed by similar backtilting of the Kafu River. by . Lake Kyoga basin Uganda. Down-warping leads to the formation of a basin or a depression. River Nile was formed about 30,000 years ago. Formation of Lakes. Downwarping lakes Are also called depression lakes They are usually shallow Formed when pats of the earth warped downwards and the sorrounding areas warped upwards They include Vi - victoria Ba -bangweull www.arena.co.ke 0713779527 Cha -chad kyo -kyoga volcanic processes a. '""\Cl..~ Population characteristics of Oreochromis esculentus inthe Victoria and Kyoga lake basins inrelation toconservation and restoration ofthe s ecies. Figure 2-21 shows the geological map of Lake Kyoga Basin. Lake Kyoga. Other smaller features which may be formed in smaller manner are inselbergs. Fault lakes -Lake Edward ,Kivu ,Naivasha ,Malawi ,Tanganyika ,Turkana ,Eyasi ,Albert ,Abaya and Natron . Introduction. Answer (1 of 2): What you are probably alluding to is tectonic/isostatic movements of the earths crust - and how it affects rivers. 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