Monday, 16 June 2014

TURKANA LAKE

Coordinates: 3°35′N 36°7′E
Lake type            Saline, monomictic, alkaline, endorheic
Primary inflows Omo River, Turkwel River, Kerio River
Primary outflows             Evaporation
Catchment area                130,860 km²
Basin countries Ethiopia, Kenya
Max. length        290 km
Max. width         32 km 20 mi
Surface area       6,405 km2 2,473 sq mi
Average depth  30.2 m
Max. depth        109 m
Water volume   203.6 km³
Surface elevation             360.4 m
Islands  North Island, Central Island, South Island volcanic
Settlements       El Molo, Loyangalani, Kalokol, Eliye Springs, Ileret, Fort Banya.
The lake was named Lake Rudolf in honour of Crown Prince Rudolf of Austria by Count Sámuel Teleki de Szék and his second-in-command Lieutenant Ludwig Ritter Von Höhnel, a Hungarian and an Austrian,on 6 March 1888. They were the first Europeans to have recorded visiting the lake after a long safari across East Africa. Natives who live around Lake Turkana include the Turkana, Rendille, Gabbra, Daasanach, Hamar Koke, Karo, Nyagatom, Mursi, Surma and Molo peoples. For the location of many of these peoples, refer to the dialect map in the article.
J. W. Gregory reported in The Geographical Journal of 1894 that it had been called 'Basso Narok'. This means "Black Lake" in the Samburu language. Likewise, Lake Stefanie is "Basso Naibor" in Samburu, meaning "White Lake". The Samburu are among the dominant tribes in the lake Turkana region when the explorers came." What the native form of this phrase was, what it might mean, and in which language is not clear. The lake kept its European name during the colonial period of British East Africa. After the independence of Kenya, the president, Mzee Jomo Kenyatta, renamed it in 1975 after the Turkana, the predominant tribe there.
At some unknown time, the lake acquired an alternate name as the Jade Sea from its turquoise colour seen approaching from a distance. The colour comes from algae that rise to the surface in calm weather. This is likely also a European name. The Turkana refer to the lake as Anam Ka'alakol, meaning "the sea of many fish". It is from the name Ka'alakol that Kalokol, a town on the western shore of Lake Turkana, east of Lodwar, derives its name. The previous indigenous Turkana name for Lake Turkana was Anam a Cheper. The area still sees few visitors, being a two-day drive from Nairobi. The lake is also an imaginary boundary of the Rendille and Borana and Oromo to the Turkana land. The area is primarily clay-based and is more alkaline than seawater.


MALAWI LAKE

Lake Malawi is between 560 kilometres 350 mi and 580 kilometres 360 mi long, and about 75 kilometres 47 mi wide at its widest point. The total surface area of the lake is about 29,600 square kilometres 11,400 sq mi. The lake has shorelines on western Mozambique, eastern Malawi, and southern Tanzania. The largest river flowing into it is the Ruhuhu River, and there is an outlet at its southern end, the Shire River, a tributary that flows into the very large Zambezi River in Mozambique.
The lake lies in a valley formed by the opening of the East African Rift, where the African tectonic plate is being split into two pieces. This is called a divergent plate tectonics boundary. It is variously estimated at about 40,000 years old or about one to two million years. The lake is about 350 kilometres 220 mi southeast of Lake Tanganyika, another of the great lakes of the East African Rift.
There is a rocky island about 3 kilometres from the western shore of the lake, across from Nkopola. named Boadzulu Island. The exact coordinates are 14°15'2.2"14.2506° south and 35°8'33.1" 35.1425° east. The island is uninhabited and is remarkable for the large number of cichlids which live in the surrounding waters.
European discovery and colonization
The Portuguese trader Candido José da Costa Cardoso was the first European to visit the lake in 1846.[8] David Livingstone reached the lake in 1859, and named it "Lake Nyasa".Much of the African region surrounding this lake was soon claimed by the British Empire and formed into the colony of Nyasaland. Although the Portuguese took control of the eastern shore of this lake, the island of Likoma was used as a mission station by the Universities' Mission to Central Africa, and as a result, Likoma and the nearby islet of Chizumulu were incorporated into Nyasaland rather than to Mozambique. Today, these islets form lacustrine exclaves: Malawian land surrounded by Mozambiquian waters.citation needed
On August 16, 1914, Lake Malawi was the scene of a brief naval battle when the British gunboat SS Gwendolen, commanded by a Captain Rhoades, heard that World War I had broken out, and he received orders from the British Empire's high command to "sink, burn, or destroy" the German Empire's only gunboat on the lake, the Hermann von Wissmann, commanded by a Captain Berndt. Rhoades's crew found the Hermann von Wissmann in a bay near "Sphinxhaven", in German East African territorial waters. Gwendolen disabled the German boat with a single cannon shot from a range of about 1,800 metres 2,000 yd. This very brief gunboat conflict was hailed by The Times in England as the British Empire's first naval victory of World War I. until that time, the lakeshore that is now in Tanzania had been a part of German East Africa.citation needed
Borders

The largest portion of the area of the lake is in Malawi. However, about a quarter of the area belongs to Mozambique. This area includes the waters surrounding the Malawian islets of Likoma and Chizumulu, which are this lake's only two inhabited islets. The islet of Likoma is dominated by a large stone and brick Anglican cathedral that was built by missionaries in the early 20th century. A notable feature of both islets is their significant number of baobab trees. The islets support a population of several thousand people, who in addition to being fishermen, grow plants such as cassavas, bananas, and mangoes for food.

LAKE KIVU

The lake covers a total surface area of some 2,700 km2 and stands at a height of 1,460 metres 4,790 ft above sea level. Some 1 370 km2 or 58% of the lake's waters lie within DRC borders. The lake bed sits upon a rift valley that is slowly being pulled apart, causing volcanic activity in the area, and making it particularly deep: its maximum depth of 480 m (1,575 ft) is ranked eighteenth in the world.
The world's tenth-largest inland island, Idjwi, lies in Lake Kivu, as does the tiny island of Tshegera, which also lies within the boundaries of Virunga National Park; while settlements on its shore include Bukavu, Kabare, Kalehe, Sake and Goma in Congo and Gisenyi, Kibuye and Cyangugu in Rwanda.
Native fish include species of Barbus, Clarias, and Haplochromis, as well as Nile Tilapia. Limnothrissa miodon, one of two species known as the Tanganyika sardine, was introduced in 1959 and formed the basis of a new pelagic zone fishery. In the early 1990s, the number of fishers on the lake was 6,563, of which 3,027 were associated with the pelagic fishery and 3,536 with the traditional fishery. Widespread armed conflict in the surrounding region from the mid-1990s resulted in a decline in the fisheries harvest.
Chemistry
Lake Kivu is a fresh water lake and, along with Cameroonian Lake Nyos and Lake Monoun, is one of three that experience limnic eruptions. Analysis of Lake Kivu's geological history indicates sporadic massive biological extinction on millennial timescales. The trigger for lake overturns in Lake Kivu's case is unknown but volcanic activity is suspected. The gaseous chemical composition of exploding lakes is unique to each lake; in Lake Kivu's case, methane and carbon dioxide due to lake water interaction with a volcano. The amount of methane is estimated to be 65 cubic kilometers (if burnt over one year, it would give an average power of about 100 gigawatts for the whole period). There is also an estimated 256 cubic kilometers of carbon dioxide. The methane is reported to be produced by microbial reduction of the volcanic CO2. The risk from a possible Lake Kivu overturn is catastrophic, dwarfing other documented lake overturns at Lakes Nyos and Monoun, because of the approximately two million people living in the lake basin.
Cores from the Bukavu Bay area of the lake reveal that the bottom has layered deposits of the rare mineral monohydrocalcite interlain with diatoms, on top of sapropelic sediments with high pyrite content. These are found at three different intervals. The sapropelic layers are believed to be related to hydrothermal discharge and the diatoms to a bloom which reduced the carbon dioxide levels low enough to precipitiate monohydrocalcite.
Scientists hypothesize that sufficient volcanic interaction with the lake's bottom water that has high gas concentrations would heat water, force the methane out of the water, spark a methane explosion, and trigger a nearly simultaneous release of carbon dioxide. The carbon dioxide would then suffocate large numbers of people in the lake basin as the gases roll off the lake surface. It is also possible that the lake could spawn lake tsunamis as gas explodes out of it.
The risk posed by Lake Kivu began to be understood during the analysis of more recent events at Lake Nyos. Lake Kivu's methane was originally thought to be merely a cheap natural resource for export, and for the generation of cheap power. Once the mechanisms that caused lake overturns began to be understood, so did awareness of the risk the lake posed to the local population.

An experimental vent pipe was installed at Lake Nyos in 2001 to remove gas from the deep water, but such a solution for the much larger Lake Kivu would be considerably more expensive. No plan has been initiated to reduce the risk posed by Lake Kivu.[dubious – discuss] the approximately 500 million tonnes of carbon dioxide in the lake is a little under 2 percent of the amount released annually by human fossil fuel burning. Therefore the process of releasing it could potentially have costs beyond building and operating the system.

LAKE VICTORIA

Lake Victoria during its geological history, went through changes ranging from its present shallow depression, through to what may have been a series of much smaller lakes. Geological cores taken from its bottom show Lake Victoria has dried up completely at least three times since it formed. These drying cycles are probably related to past ice ages, which were times when precipitation declined globally. Lake Victoria last dried out 17,300 years ago, and it refilled beginning about 14,700 years ago. Geologically, Lake Victoria is relatively young – about 400,000 years old – and it formed when westward-flowing rivers were dammed by an upthrown crustal block.
This geological history probably contributed to the dramatic cichlid speciation that characterises its ecology, as well as that of other African Great Lakes, although some researchers dispute this, arguing while Lake Victoria was at its lowest between 18,000 and 14,000 years ago, and it dried out at least once during that time, there is no evidence of remnant ponds or marshes persisting within the desiccated basin. If such features existed, then they would have been small, shallow, turbid, and/or saline, and therefore markedly different from the lake to which today's species are adapted.
The shallowness of Lake Victoria, its limited river inflow, and its large surface area compared to its volume make it vulnerable to the effects of climate changes.
Hydrology and limnology
Lake Victoria receives 80% of its water from direct precipitation. Average evaporation on the lake is between 2.0 and 2.2 metres 6.6 and 7.2 ft per year, almost double the precipitation of riparian areas. In the Kenya Sector, the main influent rivers are the Sio, Nzoia, Yala, Nyando, Sondu Miriu, Mogusi and the Migori. Combined, these rivers contribute far more water to the lake than does the largest single inflowing river, the Kagera River, which enters the lake from the west.


Lake Victoria and the Great Rift Valley
The only outflow from Lake Victoria is the Nile River which exits the lake near Jinja, Uganda. In terms of contributed water, this makes Lake Victoria the principal source of the longest branch of the Nile, however, the most distal source of the Nile Basin, and therefore the ultimate source of the Nile, is more often considered to be one of the tributary rivers of the Kagera River the exact tributary remains undetermined, and which originates in either Rwanda or Burundi. The uppermost section of the Nile is generally known as the Victoria Nile until it reaches Lake Albert. Although it is a part of the same river system known as the White Nile and is occasionally referred to as such, strictly speaking this name does not apply until after the river crosses the Uganda border into South Sudan to the north.
The lake exhibits eutrophic conditions. In 1990–1991, oxygen concentrations in the mixed layer were higher than in 1960–1961, with nearly continuous oxygen supersaturation in surface waters. Oxygen concentrations in hypolimnetic waters i.e. the layer of water that lies below the thermocline, is noncirculating, and remains perpetually cold were lower in 1990–1991 for a longer period than in 1960–1961, with values of less than 1 mg per litre < 0.4 gr/cu ft occurring in water as shallow as 40 metres compared with a shallowest occurrence of greater than 50 metres in 1961. The changes in oxygenation are considered consistent with measurements of higher algal biomass and productivity. These changes have arisen for multiple reasons: successive burning within its basin, soot and ash from which has been deposited over the lake's wide area; from increased nutrient inflows via rivers, and from increased pollution associated with settlement along its shores.

The extinction of cichlids in the genus Haplochromis has also been blamed on the lake's eutrophication. The fertility of tropical waters depends on the rate at which nutrients can be brought into solution. The influent rivers of Lake Victoria provide few nutrients to the lake in relation to its size. Because of this, most of Lake Victoria's nutrients are thought to be locked up in lake-bottom deposits. By itself, this vegetative matter decays slowly. Animal flesh decays considerably faster, however, so the fertility of the lake is dependent on the rate at which these nutrients can be taken up by fish and other organisms. There is little doubt that Haplochromis played an important role in returning detritus and plankton back into solution. With some 80% of Haplochromis species feeding off detritus, and equally capable of feeding off one another, they represented a tight, internal recycling system, moving nutrients and biomass both vertically and horizontally through the water column, and even out of the lake via predation by humans and terrestrial animals. The removal of Haplochromis, however, may have contributed to the increasing frequency of algal blooms, which may in turn be responsible for mass fish kills.

RAINY LAKE

Earliest documentation of the lake's name is "Tekamamiwen" shown as "Lac de Tecamamiouen" on the Ochagach map c. 1728, as "Lac Tacamamioüer" on the 1739 de l'Isle map, as "Lake Tecamaniouen" on the 1757 Mitchell Map and as "Lake Tekamamigovouen" on the Thomas Jefferys' 1762 Map of Canada. Pierre Gaultier de Varennes, sieur de La Vérendrye cites that the name was a corruption from the Cree "taki-kimiwen", meaning "It always is raining", referring to the Rainy River, though the language does not quite support that claim. He also cites that the lake was also known as "Ouichichick" Ojibwe word Gojijiing or Cree Kocicīhk, both meaning "at the place of inlets". Early documents lists the portion of Rainy Lake east of the Brule Narrows as "Cristinaux Cree Lake"or as "Little Lake."
Recreation on Rainy Lake
Voyageurs National Park
On Rainy Lake, Voyageurs National Park maintains an extensive network of over boat-in camping sites, hiking trails, and designated snowmobile trails for winter use.
Fishing
The lake is popular for sport and recreational fishing for species such as Walleye, Northern pike, Muskellunge, Largemouth and Smallmouth bass, which are all considered excellent freshwater sportfish. Rainy Lake is home to the annual Canadian Bass Championship, which has occurred every summer since 1996. The lake is dotted with many small islands on both the Canadian and American sides; they are the sites of numerous fishing cabins, small fishing resorts, and vacation homes. Tourism is an important part of the local economy.
Governance
The level of Rainy Lake is controlled at the hydro-electric power houses of the international dam that spans the Rainy River between International Falls and Fort Frances, at two water-control dams located at Kettle Falls where the outflow from Namakan Lake enters Rainy Lake, and at the Sturgeon Falls Generating Station located on the Seine River. The companies that own and operate the powerhouses Boise Inc. on the U.S. side and H2O Power Limited Partnership on the Canadian side are responsible for maintaining lake level and flow changes from the dams within normal ranges, subject to regulatory oversight by the International Rainy Lake Board of Control IRLBC. The IRLBC is a board of the International Joint Commission IJC, which is a bi-national organization created out of the International Boundary Waters Treaty of 1909 for the purposes of handling boundary water issues between the United States and Canada.

LAKE ONTARIO

Geography
Lake Ontario Basin
View from Fort Ontario, Oswego, New York
Historic cannon at Fort Niagara; Toronto across the lake
Lake Ontario is the easternmost of the Great Lakes and the smallest in surface area (7,340 sq mi, 18,960 km2), although it exceeds Lake Erie in volume (393 cu mi, 1,639 km3). It is the 14th largest lake in the world. When its islands are included, the lake has a shoreline that is 712 miles (1,146 km) long. As the last lake in the Great Lakes' hydrologic chain, Lake Ontario has the lowest mean surface elevation of the lakes at 243 feet (74 m) above sea level; 326 feet (99 m) lower than its neighbor upstream. Its maximum length is 193 statute miles (311 kilometres; 168 nautical miles) and its maximum width is 53 statute miles (85 km; 46 nmi). The lake's average depth is 47 fathoms 1 foot (283 ft; 86 m), with a maximum depth of 133 fathoms 4 feet (802 ft; 244 m). The lake's primary source is the Niagara River, draining Lake Erie, with the St. Lawrence River serving as the outlet. The drainage basin covers 24,720 square miles (64,030 km2). with all the Great Lakes, water levels change both within the year (owing to seasonal changes in water input) and among years (owing to longer term trends in precipitation). These water level fluctuations are an integral part of lake ecology, and produce and maintain extensive wetlands.TheA lake also has an important freshwater fishery, although it has been negatively affected by factors including over-fishing, water pollution and invasive species.
Baymouth bars built by prevailing winds and currents have created a significant number of lagoons and sheltered harbors, mostly (but not limited to) Prince Edward County, Ontario and the easternmost shores. Perhaps the best-known example is Toronto Bay, chosen as the site of the Upper Canada (Ontario) capital for its strategic harbour. Other prominent examples include Hamilton Harbour, Irondequoit Bay, Presqu'ile Bay, and Sodus Bay. The bars themselves are the sites of long beaches, such as Sandbanks Provincial Park and Sandy Island Beach State Park. These sand bars are often associated with large wetlands, which support large numbers of plant and animal species, as well as providing important rest areas for migratory birds. Presqu'ile, on the north shore of Lake Ontario, is particularly significant in this regard. One unique feature of the lake is the Z-shaped Bay of Quinte which separates Prince Edward County from the Ontario mainland, save for a 2-mile (3.2 km) isthmus near Trenton; this feature also supports many wetlands and aquatic plants, as well as associated fisheries.
Major rivers draining into Lake Ontario include the Niagara River; Don River; Humber River; Trent River; the Cataraqui River; the Genesee River; the Oswego River; the Black River; and the Salmon River.
Geology
The lake basin was carved out of soft, weak Silurian-age rocks by the Wisconsin ice sheet during the last ice age. The action of the ice occurred along the pre-glacial Ontarian River valley which had approximately the same orientation as today's basin. Material that was pushed southward by the ice sheet left landforms such as drumlins, kames, and moraines, both on the modern land surface and the lake bottom, reorganizing the region's entire drainage system. As the ice sheet retreated toward the north, it still dammed the St. Lawrence valley outlet, so that the lake surface was at a higher level. This stage is known as Lake Iroquois. During that time the lake drained through present-day Syracuse, New York into the Mohawk River, thence to the Hudson River and the Atlantic. The shoreline created during this stage can be easily recognized by the (now dry) beaches and wave-cut hills 10 to 25 miles (15 to 40 km) from the present shoreline.

When the ice finally receded from the St. Lawrence valley, the outlet was below sea level, and for a short time the lake became a bay of the Atlantic Ocean, in association with the Champlain Sea. Gradually the land rebounded from the release of the weight of about 6,500 feet (2,000 m) of ice that had been stacked on it. It is still rebounding about 12 inches (30 cm) per century in the St. Lawrence area. Since the ice receded from the area last, the most rapid rebound still occurs there. This means that the lake bed is gradually tilting southward, inundating the south shore and turning river valleys into bays. Both north and south shores experience shoreline erosion, but the tilting amplifies this effect on the south shore, causing loss to property owners.A

LAKE ERIE

Geographic features;
See also: Lake Erie Basin
(Lake Erie 42.2° N, 81.2) has a mean elevation of 571 feet above sea level. It has a surface area of 9,910 square miles 25,667 km with a length of 241 statute miles 388 km; 209 nmi and breadth of 57 statute miles  92 km; 50 nmi at its widest points.
It is the shallowest of the Great Lakes with an average depth of 10 fathoms 3 feet 62 ft; 19 m and a maximum depth of 35 fathoms 210 ft; 64 m For comparison, Lake Superior has an average depth of 80 fathoms 3 feet 483 ft; 147 m, a volume of 2,900 cubic miles 12,100 km3 and shoreline of 2,726 statute miles 4,385 km. Because it is the shallowest, it is also the warmest of the Great Lakes, and in 1999 this almost became a problem for two nuclear power plants which require cool lake water to keep their reactors cool. The warm summer of 1999 caused lake temperatures to come close to the 85 °F (29 °C) limit necessary to keep the plants cool. Also because of its shallowness, and in spite of being the warmest lake in the summer, it is also the first to freeze in the winter. The shallowest section of Lake Erie is the western basin where depths average only 25 to 30 feet 7.6 to 9.1 m; as a result, "the slightest breeze can kick up lively waves," according to a New York Times reporter in 2004. The "waves build very quickly", according to other accounts. Sometimes fierce waves springing up unexpectedly have led to dramatic rescues; in one instance, a Cleveland resident trying to measure the dock near his house became trapped but was rescued by a fire department diver from Avon Lake, Ohio:
In a tug of war against the waves, the two were finally hauled out by rope. After being trapped for an hour-and-a-half, Baker was back on dry land, exhausted and battered but alive.
—Tatiana Morales, CBS News, 2004
The Niagara River empties Lake Erie into Lake Ontario. This water has just passed over Niagara Falls.
This area is also known as the "thunderstorm capital of Canada" with "breathtaking" lightning displays. Lake Erie is primarily fed by the Detroit River from Lake Huron and Lake St. Clair and drains via the Niagara River and Niagara Falls into Lake Ontario. Navigation downstream is provided by the Welland Canal, part of the Saint Lawrence Seaway. Other major contributors to Lake Erie include the Grand River, the Huron River, the Maumee River, the Sandusky River, the Buffalo River, and the Cuyahoga River. The drainage basin covers 30,140 square miles 78,000 km2.
Point Pelee National Park, the southernmost point of the Canadian mainland, is located on a peninsula extending into the lake. Several islands are found in the western end of the lake; these belong to Ohio except for Pelee Island and eight neighboring islands, which are part of Ontario.
Major cities along the Lake Erie include Buffalo, New York; Erie, Pennsylvania; Toledo, Ohio; Port Stanley, Ontario; Monroe, Michigan; Sandusky, Ohio; and Cleveland, Ohio.
Partial map of the Lake Erie Islands
Islands
See also: Lake Erie Islands
Islands tend to be located in the western side of the lake and total 31 in number (13 in Canada, 18 in the U.S.). The island-village of Put-in-Bay on South Bass Island attracts young crowds who sometimes wear "red bucket hats" and are prone to "break off cartwheels in the park" and general merriment. Kelleys Island was depicted by the Chicago Tribune as having charms that were "more subtle" than Put-in-Bay, and offers amenities such as beach lounging, hiking, biking, and "marveling at deep glacial grooves left in limestone." Pelee Island is the largest of Erie's islands, accessible by ferry from Leamington, Ontario and Sandusky, Ohio. The island has a "fragile and unique ecosystem" with plants rarely found in Canada, such as wild hyacinth, yellow horse gentian (Triosteum angustifolium), and prickly pear cactus, as well as two endangered snakes, the blue racer and the Lake Erie water snake. Songbirds migrate to Pelee in spring, and monarch butterflies stop over during the fall.
Water levels
Lake Erie has a lake retention time of 2.6 years,the shortest of all the Great Lakes. This means that the lake water is renewed from upstream sources every three years. The lake's surface area is 9,910 square miles (25,667 km2). Lake Erie's water level fluctuates with the seasons as in the other Great Lakes. Generally, the lowest levels are in January and February, and the highest in June or July, although there have been exceptions. The average yearly level varies depending on long-term precipitation. Short-term level changes are often caused by seiches that are particularly high when southwesterly winds blow across the length of the lake during storms. These cause water to pile up at the eastern end of the lake. Storm-driven seiches can cause damage onshore. During one storm in November 2003, the water level at Buffalo rose by 7 feet (2.1 m) with waves of 10–15 feet (3–4.5 m) for a rise of 22 feet (6.7 m). Meanwhile, at the western end of the lake, Toledo experienced a similar drop in water level. Lake water is used for drinking purposes.
Historic High Water. The lake fluctuates from month to month with the highest lake levels in October and November. The normal high-water mark is 2.00 feet (0.61 m) above datum (569.2 ft or 173.5 m). In the summer of 1986, Lake Erie reached its highest level at 5.08 feet (1.55 m) above datum.[27] The high water records were set from 1986 (April) through January 1987. Levels ranged from 4.33 to 5.08 feet (1.32–1.55 m) above Chart Datum.

Historic Low Water. Lake Erie experiences its lowest levels in the winter. The normal low-water mark is 1.50 feet (0.46 m) below datum (569.2 ft or 173.5 m). In the winter of 1934, Lake Erie reached its lowest level at 1.50 feet (0.46 m) below datum. Monthly low water records were set from July 1934 through June 1935. During this twelve-month period water levels ranged from 1.50 feet (0.46 m) to the Chart Datum.

BALATON LAKE

Location               Hungary
Coordinates       46°50′N 17°44′ECoordinates: 46°50′N 17°44′E
Type      Rift lake
Primary inflows Zala River
Primary outflows             Sió
Catchment area                5,174 km2 1,998 sq mi
Basin countries Hungary
Max. length        77 km 48 mi
Max. width         14 km 8.7 mi
Surface area       592 km2 229 sq mi
Average depth  3.2 m 10 ft
Max. depth        12.2 m 40 ft
Water volume   1.9 km3 0.46 cu mi
Residence time 2 years
Shore length1    236 km 147 mi
Surface elevation             104.8 m 344 ft
In Hungarian, the lake is known simply as Balaton, or "the Balaton". This name derives from the Slavic blato meaning 'mud' or 'swamp' from earlier Proto-Slavic boltьno, Slovene: Blatno jezero, Slovak: Blatenské jazeroSlavic prince Pribina began to build in January 846 a fortress as his seat of power and several churches in the region of Lake Balaton, in a territory of modern Zalavár surrounded by forests and swamps along the river Zala. His well fortified castle and capital of Balaton Principality that became known as Blatnohrad or Moosburg "Swamp Fortress" served as a bulwark both against the Bulgarians and the Moravians.
The Romans called the lake Lacus Pelso "Lake Pelso".Pelso derives from a local name for the lake, perhaps from the Illyrian language, as the Illyrians once populated the region. Paleolinguists who? surmise that "Pelso" meant "shallow" in Illyrian; this deduction is based on a surmised Proto-Indo-European root *pels-.citation needed
The German name for the lake is Plattensee. It is unlikely that the Germans named the lake so for being shallow since the adjective platt is a Greek loanword that was borrowed via French and entered the general German vocabulary in the 17th century. It is also noteworthy that the average depth of Balaton 3.2m is not extraordinary for the area cf. the average depth of the neighbouring Neusiedler See, which is roughly 1m.
Climate
Map of Balaton in ancient times
Lake Balaton affects the local area precipitation every year. The area receives approximately two to three inches 5–7 cm more precipitation than most of Hungary, resulting in more cloudy days and less extreme temperatures. The lake's surface freezes during winters. The microclimate around Lake Balaton has also made the region ideal for viniculture. The lake, acting as a mirror, greatly increases the amount of sunlight that the grapevines of the region receive.citation needed The Mediterranean-like climate, combined with the soil containing volcanic rock, has made the region notable for its production of wines since the Roman period two thousand years ago.
While a few settlements on Lake Balaton, including Balatonfüred and Hévíz, have long been resort centres for the Hungarian aristocracy, it was only in the late 19th century that the Hungarian middle class began to visit the lake. The construction of railways in 1861 and 1909 increased tourism substantially, but the post-war boom of the 1950s was much larger.
The last major German offensive of World War II, Operation Frühlingserwachen, was conducted in the region of Lake Balaton in March 1945, being referred to as "the Lake Balaton Offensive" in many British histories of the war. The battle was a German attack by Sepp Dietrich's Sixth Panzer Army and the Hungarian Third Army between 6 March and 16 March 1945, and in the end, resulted in a Red Army victory. Several Ilyushin Il-2 wrecks have been pulled out of the lake after having been shot down during the latter months of the war.
During the 1960s and 1970s, Balaton became a major tourist destination for ordinary working Hungarians and especially for subsidised holiday excursions for union members. It also attracted many East Germans and other residents of the Eastern Bloc. West Germans could also visit, making Balaton a common meeting place for families and friends separated by the Berlin Wall until 1989.
The collapse of Communism after 1991 and the dismantling of the unions saw the gradual but steady reduction in numbers of lower-paid Hungarians

KAGERA LAKE

Primary inflows Kagera River
Primary outflows             White Nile (river) (known as the "Victoria Nile" as it flows out of the lake)
Catchment area                184,000 km2 (71,000 sq mi)
238,900 km2 (92,200 sq mi) basin
Basin countries Tanzania
Uganda
Kenya
Max. length        337 km (209 mi)
Max. width         250 km (160 mi)
Surface area       68,800 km2 (26,600 sq mi)
Average depth  40 m (130 ft)
Max. depth        83 m (272 ft)
Water volume   2,750 km3 (660 cu mi)
Shore length1    3,440 km (2,140 mi)
Surface elevation             1,133 m (3,717 ft)
Islands  84 (Ssese Islands, Uganda)

Location               African Great Lakes
Coordinates       1°S 33°ECoordinates: 1°S 33°E
Primary inflows Kagera River
Primary outflows             White Nile river known as the "Victoria Nile" as it flows out of the lake
Catchment area                184,000 km2 71,000 sq mi
238,900 km2 92,200 sq mi basin
Basin countries Tanzania
Uganda
Kenya
Max. length        337 km 209 mi
Max. width         250 km 160 mi
Surface area       68,800 km2 26,600 sq mi
Average depth  40 m 130 ft
Max. depth        83 m 272 ft
Water volume   2,750 km3 660 cu mi
Shore length1    3,440 km 2,140 mi
Surface elevation             1,133 m 3,717 ft

                                      Lake Victoria during its geological history, went through changes ranging from its present shallow depression, through to what may have been a series of much smaller lakes. Geological cores taken from its bottom show Lake Victoria has dried up completely at least three times since it formed. These drying cycles are probably related to past ice ages, which were times when precipitation declined globally. Lake Victoria last dried out 17,300 years ago, and it refilled beginning about 14,700 years ago. Geologically, Lake Victoria is relatively young – about 400,000 years old – and it formed when westward-flowing rivers were dammed by an upthrown crustal block.
This geological history probably contributed to the dramatic cichlid speciation that characterises its ecology, as well as that of other African Great Lakes, although some researchers dispute this, arguing while Lake Victoria was at its lowest between 18,000 and 14,000 years ago, and it dried out at least once during that time, there is no evidence of remnant ponds or marshes persisting within the desiccated basin. If such features existed, then they would have been small, shallow, turbid, and/or saline, and therefore markedly different from the lake to which today's species are adapted.

The shallowness of Lake Victoria, its limited river inflow, and its large surface area compared to its volume make it vulnerable to the effects of climate changes.

Thursday, 12 June 2014

KARIBA LAKE

Primary inflows Kagera River
Primary outflows             White Nile (river) (known as the "Victoria Nile" as it flows out of the lake)
Catchment area                184,000 km2 (71,000 sq mi)
238,900 km2 (92,200 sq mi) basin
Basin countries Tanzania
Uganda
Kenya
Max. length        337 km (209 mi)
Max. width         250 km (160 mi)
Surface area       68,800 km2 (26,600 sq mi)
Average depth  40 m (130 ft)
Max. depth        83 m (272 ft)
Water volume   2,750 km3 (660 cu mi)
Shore length1    3,440 km (2,140 mi)
Surface elevation             1,133 m (3,717 ft)
Islands  84 (Ssese Islands, Uganda)

Location               African Great Lakes
Coordinates       1°S 33°ECoordinates: 1°S 33°E
Primary inflows Kagera River
Primary outflows             White Nile river known as the "Victoria Nile" as it flows out of the lake
Catchment area                184,000 km2 71,000 sq mi
238,900 km2 92,200 sq mi basin
Basin countries Tanzania
Uganda
Kenya
Max. length        337 km 209 mi
Max. width         250 km 160 mi
Surface area       68,800 km2 26,600 sq mi
Average depth  40 m 130 ft
Max. depth        83 m 272 ft
Water volume   2,750 km3 660 cu mi
Shore length1    3,440 km 2,140 mi
Surface elevation             1,133 m 3,717 ft

                                      Lake Victoria during its geological history, went through changes ranging from its present shallow depression, through to what may have been a series of much smaller lakes. Geological cores taken from its bottom show Lake Victoria has dried up completely at least three times since it formed. These drying cycles are probably related to past ice ages, which were times when precipitation declined globally. Lake Victoria last dried out 17,300 years ago, and it refilled beginning about 14,700 years ago. Geologically, Lake Victoria is relatively young – about 400,000 years old – and it formed when westward-flowing rivers were dammed by an upthrown crustal block.
This geological history probably contributed to the dramatic cichlid speciation that characterises its ecology, as well as that of other African Great Lakes, although some researchers dispute this, arguing while Lake Victoria was at its lowest between 18,000 and 14,000 years ago, and it dried out at least once during that time, there is no evidence of remnant ponds or marshes persisting within the desiccated basin. If such features existed, then they would have been small, shallow, turbid, and/or saline, and therefore markedly different from the lake to which today's species are adapted.

The shallowness of Lake Victoria, its limited river inflow, and its large surface area compared to its volume make it vulnerable to the effects of climate changes.

MWERU LAKE

Physical geography.
Mweru is mainly fed by the Luapula River, which comes in through swamps from the south, and the Kalungwishi River from the east. At its north end the lake is drained by the Luvua River, which flows in a northwesterly direction to join the Lualaba River and thence to the Congo. It is the second-largest lake in the Congo's drainage basin and is located 150 km west of the southern end of the largest, Lake Tanganyika.
The Luapula forms a swampy delta almost as wide as the southern end of the lake. In a number of respects the lower river and lake can be treated as one entity. For a lake in a region with pronounced wet and dry seasons, Mweru does not change much in level and area. The annual fluctuation in level is 1.7m, with seasonal highs in May and lows in January. This is partly because the Luapula drains out of the Bangweulu Swamps and floodplain which tend to regulate the water flow, absorbing the annual flood and releasing it slowly, and partly because Mweru's outlet, the Luvua, drops quickly and flows swiftly, without vegetation to block it. A rise in Mweru is quickly offset by a faster flow down the Luvua.
Mweru's average length is 118 km and its average width is 45 km, with its long axis oriented northeast-southwest. Its elevation is 917 m, quite a bit higher than Tanganyika 763 m. It is a rift valley lake lying in the Lake Mweru-Luapula graben, which is a branch of the East African Rift. The western shore of the lake in DR Congo exhibits the steep escarpment typical of a rift valley lake, rising to the Kundelungu Mountains beyond, but the rift valley escarpment is less pronounced on the eastern shore.
Mweru is shallow in the south and deeper in the north, with two depressions in the north-eastern section with maximum depths of 20 m and 27 m.
A smaller very marshy lake called Mweru Wantipa also known as the Mweru Marshes  lies about 50 km to its east, and north of the Kalungwishi. It is mostly endorheic and actually takes water from the Kalungwishi through a dambo most of the time, but in times of high flood it may overflow into the Kalungwishi and Lake Mweru.
Human geography.
Exploration
The lake was known to Arab and Swahili traders  of ivory, copper and slaves  who used Kilwa Island on the lake as a base at one time. They used trade routes from Zanzibar on the Indian Ocean to Ujiji on Lake Tanganyika to Mweru and then to the Lunda, Luba, Yeke or Kazembe kingdoms, the last being on the southern shores of Mweru. Western trade routes went from those kingdoms to the Atlantic, so Mweru lay on a transcontinental trade route.
Between 1796 and 1831 Portuguese traders/explorers Pereira, Francisco de Lacerda and others visited Kazembe from Mozambique to get treaties to use the trade route between their territories of Mozambique and Angola. The Portuguese must have known of the lake, and the visitors only had to walk to higher ground about 5 km north of Kazembe's Kanyembo capital to see the lake 10 km distant. However they were more interested in trade routes than discovery, they had approached from the south and their movements were restricted by Mwata Kazembe, and they did not provide an account of it.  Explorer and missionary David Livingstone, who referred to it as 'Moero', is credited with its discovery during his travels of 1867-'8.
Livingstone witnessed the devastation and suffering caused by the slave trade in the area to the north and east of Mweru, and his accounts did help rally opposition to it. The last of the slave trading in the area was as late as the 1890s, however. Meanwhile between 1870 and 1891, skirmishes and wars between the Yeke king Msiri and neighbouring chiefs and traders unsettled the area. Few Europeans had visited Mweru since Livingstone, until Alfred Sharpe in 1890–1 and the Stairs Expedition in 1892 both passed by on their way to seek treaties with Msiri. The Stairs Expedition killed Msiri and took Katanga for the King Leopold II of Belgium. Sharpe left one of his officers to set up the first colonial outpost in the Luapula-Mweru valley, the British boma at Chiengi in 1891.
Historical development.
Lake Mweru and its main inlets, the lower Luapula River and its swamps, and the Kalungwishi. Also shown is Mweru's outlet, the Luvua River going on north to the Lualaba and Congo rivers. Water shows up as black in this false-colour NASA satellite image. The extent of the swamps is shown by the solid blue line, and the extent of floodplain is shown as a dotted line. The towns are, in Zambia: 1 Chiengi, 2 Kashikishi, 3 Nchelenge, 4 Mwansabombwe, 5 Mwense; in DR Congo: 6 Pweto, 7 Kilwa, 8 Kasenga. Other features: 9: Chisenga Island, 10 the largest swamp island in DR Congo, 11 the main floodplain. Image credit: Jacques Descloitres, MODIS Rapid Response Team, NASA/GSFC.
The western shore of Luapula-Mweru became part of the Belgian Congo and the eastern shore part of Northern Rhodesia, a British protectorate. Although Kilwa Island is closer to the western shore, it was allocated to Northern Rhodesia, and consequently Zambia has 58% of the lake waters, and DR Congo 42%.
The first Belgian outposts on the lake were set up at Lukonzolwa and Pweto which were at various times the headquarters of their administration of Katanga. They stamped out the slave trade going north-east around the lake. The first mission station on the lake was established in 1892 by Scottish missionary Dan Crawford of the Plymouth Brethren at Luanza on the Belgian side of the lake.
The British moved their boma from Chiengi to the Kalungwishi, with one or two British officers such as Blair Watson, and a force of African police. In conjunction with operations around Abercorn further down the trade route, this was enough to end the slave trade going east from Mweru, but not enough to bring Mwata Kazembe under British rule, and a military expedition had to be sent in 1899 from British Central Africa Nyasaland to do that job see the article on Alfred Sharpe for more details.
The move of the boma from Chiengi to Kalungwishi had the effect of leaving the Belgian boma at Pweto a free rein at the northern end of the lake, leading a hundred years later to about 33 km² of Zambian territory next to Pweto being ceded to the DR Congo then Zaire. See the Luapula Province border dispute for further details and references.
After 1900, the Belgian Congo province of Katanga on the western shores of the lake developed faster than the Northern Rhodesian side, the Luapula Province and the town of Kasenga a few hours by boat up the Luapula River became the most developed in the Luapula-Mweru valley, and until the 1960s was the main commercial centre with better services and infrastructure than elsewhere. The Elizabethville mines started up more quickly than those of the Copperbelt, and Kasenga supplied its workforce with fish. Since 1960, political crises, government neglect and wars on the Congolese side have produced a deterioration in infrastructure, while peace on the Zambian side has produced an increase in population and services, causing the balance to change .
Centres of population on the lake.
Many fishing villages dot Mweru's shores. A number are seasonal camps. The main towns on the Zambian side are Nchelenge, Kashikishi and Chiengi, and on the DR Congo side, Kilwa the town opposite the island, Lukonzolwa and Pweto.
Besides Kilwa Island, there are two other inhabited islands in the lake: Zambia's Isokwe Island of 3 km², and a 2 km² Congolese island next to the mouth of the Luapula. Two other islands in the Luapula swamps have shores on the lake.

The Congolese side of the lake was affected by the Second Congo War of 1999-2003, from which it is still recovering. Many refugees entered Zambia at Pweto and were accommodated in camps in Mporokoso and Kawambwa districtsa

LAKE CHAD

Lake Chad is located mainly in the far west of Chad, bordering on northeastern Nigeria. The Chari River, fed by its tributary the Logone, provides over 90% of Lake Chad's water, with a small amount coming from the Yobe River in Nigeria/Niger. Despite high levels of evaporation, the lake is fresh water. Over half of the lake's area is taken up by its many small islands including Bogomerom archipelago, reedbeds and mud banks, and a belt of swampland across the middle divides the northern and southern halves while the shorelines are largely composed of marshes.
Because Lake Chad is very shallow—only 10.5 metres 34 ft at its deepest—its area is particularly sensitive to small changes in average depth, and consequently it also shows seasonal fluctuations in size of about 1 m every year. Lake Chad has no apparent outlet, but its waters percolate into the Soroand Bodélé depressions. The climate is dry most of the year, with occasional rains from June to December.
Lake Chad French: lac Tchad  is a historically large, shallow, endorheic lake in Africa, the size of which has varied over the centuries. According to theGlobal Resource Information Database of the United Nations Environment Programme, it shrank as much as 95% from about 1963 to 1998, but "the 2007 satellite image shows significant improvement over previous years." Lake Chad is economically important, providing water to more than 30 million people living in the four countries surrounding it Chad, Cameroon, Niger, and Nigeria on the edge of the Sahara Desert. It is the largest lake in the Chad Basin.
Lake Chad gave its name to the country of Chad. The name Chad is a local word specify meaning "large expanse of water", in other words, a "lake".
Lake Chad is the remnant of a former inland sea, paleolake Mega-Chad. At its largest, sometime before 5000 BC, Lake Mega-Chad was the largest of four Saharan paleolakes, and is estimated to have covered an area of 400,000 km2 150,000 sq mi, larger than the Caspian Sea is today, and may have extended as far northeast as within 100 km 62 mi of Faya-Largea.
Lake Chad was first surveyed from shore by Europeans in 1823, and it was considered to be one of the largest lakes in the world then In 1851, a party including the German explorer Heinrich Barth carried a boat overland from Tripoli across the Sahara Desert by camel and made the first European waterborne survey. British expedition leader James Richardson died just days before reaching the lake
Lake Chad has shrunk considerably since the 1960s, when its shoreline had an elevation of about 286 metres 938 ft above sea level and it had an area of more than 26,000 square kilometres 10,000 sq mi, making its surface the fourth largest in Africa. An increased demand on the lake's water from the local population has likely accelerated its shrinkage over the past 40 years
The size of Lake Chad greatly varies seasonally with the flooding of the wetlands areas. In 1983, Lake Chad was reported to have covered 10,000 to 25,000 km2 3,900 to 9,700 sq mihad a maximum depth of 11 metres 36 ft and a volume of 72 km3 17 cu m
Volcanism
The region shows much evidence of volcanic activity in the last 5000 years. The Katwe-Kikorongo and Bunyaruguru Volcanic Fields, with extensive cones and craters, lie either side of the Kazinga Channel on the north-west shore of the lake. It is thought that Lakes George and Edward have been joined as one larger lake in the past, but lava from these fields flowed in and divided it, leaving only the Kazinga Channel as the remnant of the past union. To the south, the May-ya-Moto thermally active volcano lies 30 km away, and the Nyamuragira volcano in the western Virunga Mountains lies 80 km south, but its lava flo
ws have reached the lake in the past.
The Katwe-Kikorongo field features dozens of large craters and cones covering an area of 30 km by 15 km between lakes Edward and George, and includes seven crater lakes. The largest of these, the 2.5-kilometre-long Lake Katwe, occupies a crater 4 km across and is separated from Lake Edward by just 300 m of land. The crater is about 100 m deep, and Lake Katwe's surface is about 40 m lower than Lake Edward's. It is remarkable that the volcanic origin of this area south-east of the Ruwenzoris was not known until reported by G. F. Scott Elliot in 1894. Stanley visited Lake Katwe in 1889 and noted the deep depression, the salinity of the lake, and a spring of sulphurous water nearby, but failed to connect this to volcanism.
The similarly-sized Bunyaruguru field on the other side of the Kazinga Channel contains about 30 crater lakes, some larger than Katwe.
Settlements
Lake Edward lies completely within the Virunga National Park Congo and the Queen Elizabeth National Park (Uganda) and does not have extensive human habitation on its shores, except atIshango (DRC) in the north, home to a park ranger training facility. About two-thirds of its waters are in the DR Congo and one third in Uganda. Apart from Ishango  the main Congolese settlement in the south is Vitshumbi while the Ugandan settlements are Mweya and Katwe in the north-east, near the crater lake of that name which is the chief producer of salt for Uganda. The Mweya Safari Lodge is the main tourist facility serving both Lake Edward and Lake Katwe. The nearest cities are Kasese in Uganda to the north-east and Butembo in DR Congo, to the north-west, which are respectively about 50 km and 150 km distant by road.


BANYOLES LAKE

Location               Banyoles, Catalonia
Coordinates       42°07′31″N 2°45′19″ECoordinates: 42°07′31″N 2°45′19″E
Primary inflows Rec d'en Morgat, Riera del Vilar, Rec Majo, Rec de la Font Pudusa, Rec de les Ustunes
Primary outflows             none
Catchment area                11.42 km²
Basin countries Spain
Max. length        2,100 m
Max. width         750 m
Surface area       1.12 km²
Average depth  14.8 m
Max. depth        62.4 m
Water volume   12,000,000 m³
Shore length1    9.13 km
Surface elevation             172 m
Lake of Banyoles or Estany de Banyoles is a natural lake located in the comarca "Pla de l'Estany", Province of Girona, in northeastern Catalonia, Spain. It is named after the nearby town of Banyoles, to which it belongs entirely. On the western shore it borders with the town of Porqueres. The lake is approximately 2,100 m by 750 m with an average depth of 15 m that in several points gets down to 46.4 metres. It is located in a natural tectonic depression.
Presently Lake Banyoles is the largest natural lake in Catalonia. Lake Sils, located 33 kn further south, was formerly the largest lake in the area until it was drained in 1851.
Flora and fauna[edit]

There are both native and introduced fish species in the lake, like carp, gardí, bavosa de riu, sunfish, tench, black bass and eel. It is known that other fishes like the pike, the peix gat and the goldfish were introduced in the 19th century, but no specimens of those species have been found in recent surveys in the lake

VOLTA LAKE

Location               west east
Coordinates       6°30′N 0°0′ECoordinates: 6°30′N 0°0′E
Lake type            Reservoir
Primary inflows White Volta River
Black Volta River
Primary outflows             Volta River
Catchment area                385,180 km2 148,720 sq mi
Basin countries Ghana
Surface area       8,502 km2 3,283 sq mi
Average depth  18.8 m 62 ft
Max. depth        75 m 246 ft
Water volume   148 km3 32.6 × 1012 gallons
Shore length1    4,800 kilometres 2,980 mi
Surface elevation
85 m 279 ft
                                                       
Lake Volta lies along the Greenwich Meridian, and just six degrees of latitude north of the Equator. The lake's northmost point is close to the town of Yapei, and its southmost extreme is at the Akosombo Dam, 520 kilometers  320 mi downstream from Yapei. Akosombo Dam holds back both the White Volta River and the Black Volta River, which formerly converged, where the middle of the reservoir now lies, to form the single Volta River. The present Volta River flows from the outlets of the dam's powerhouse and spillways to the Atlantic Ocean in southmost Ghana.
The main islands within the lake are Dodi, Dwarf and Kporve. Digya National Park lies on part of the lake's west shore.
The lake is formed by the Akosombo Dam, which was originally conceived by the geologist Albert Ernest Kitson in 1915, but whose construction only began in 1961 with completion in 1965. Because of the formation of Lake Volta, about 78,000 people were relocated to new towns and villages, along with 200,000 animals belonging to them. About 120 buildings were destroyed, not including small residences, as over 3,000 square miles 7,800 km2 of territory was flooded.

The Akosombo Dam provides electricity for much of the country, as well as for export to Togo, Benin, and nearby countries, to earn foreign exchange value. Lake Volta is also important for transportation providing a waterway for both ferries and cargo watercraft. Since the huge lake lies in a tropical area, the water remains warm year-round naturally. Given good management, Lake Volta is the location of a vast population of fish and large fisheries.
The lake also attracts tourism, and tourist cruises visit the island of Dodi.

Recent developments include a large-scale enterprise to harvest submerged timber from the flooded forests under Lake Volta. This project harvests high-value tropical hardwood without requiring additional logging or destruction of existing forest and, according to Wayne Dunn, "could generate the largest source of environmentally sustainable natural tropical hardwood in the world." The Ghanaian-owned company Underwater Forest Resources has committed itself to making said lumber available in the global market, while Flooring Solutions Ghana have become the suppliers of hardwood floors, using the rare wood from the Lake.citation needed In addition to generating foreign currency for the region and reducing the dependence of locals on fishing as a primary economic activity, the removal of submerged trees is improving navigation on the lake and increasing safety.

Albert Lake

Lake Albert is located in the center of the continent, on the border between Uganda and the Democratic Republic of the Congo formerly Zaire. Lake Albert is the northernmost of the chain of lakes in the Albertine Rift, the western branch of the East African Rift. It is about 160 km 100 mi long and 30 km 19 mi wide, with a maximum depth of 51 m 168 ft, and a surface elevation of 619 m 2,030 ft above sea level.

Lake Albert is part of the complicated system of the upper Nile. Its main sources are the Victoria Nile, ultimately coming from Lake Victoria to the southeast, and the Semliki River, which issues from Lake Edward to the southwest. The water of the Victoria Nile is much less saline than that of Lake Albert. Its outlet, at the northernmost tip of the lake, is the Albert Nile which becomes known as the Mountain Nile when it enters South Sudan.


At the southern end of the lake, where the Semliki comes in, there are swamps. Farther south loom the mighty Ruwenzori Range, while a range of hills called the Blue Mountains tower over the northwestern shore. The few settlements along the shore include Butiaba and Pikachu.

In 1864 the explorer Samuel Baker & Sass Flóra found the lake and named it after the recently deceased Prince Albert, consort of Queen Victoria. In the 20th century Congolese president Mobutu Sese Seko temporarily named the lake after himself.

European colonialists operated shipping on the lake. The British planned shipping on Lake Albert as part of a network of railway, river steamer and lake steamer services linking British interests in Egypt, East Africa and southern Africa. The Thornycroft shipyard at Woolston, Hampshire built the cargo and passenger ship SS Robert Coryndon for this purpose in 1930.She was named after the British Army officer Robert Thorne Coryndon, who was Governor of Uganda 1918-22. Sir Winston Churchill described the ship as "the best library afloat" and Ernest Hemingway called her "magnificence on water". She either was scuttled in 1962 or sank in 1964. She remains unsalvaged and partly submerged in the lake.

Heritage Oil and Tullow Oil have announced major oil finds in the Lake Albert basin, with estimates that the multi-billion barrel field will prove to be the largest onshore field found in sub-saharan Africa for more than twenty years.
In March 2014, a boat carrying Congolese refugees capsized in Lake Albert, killing more than 250 people.