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Lake Turkana is a unique feature of the East African landscape. Besides being a permanent desert lake, it is the only lake that retains the waters originating from two separate catchment areas of the Nile. The Lake Turkana drainage basin draws its waters mainly from Kenya Highlands and Ethiopian Highlands. A map of lake turkana
The Daasanach share a traditional border with the Turkana. However, the border is moving toward south because of receding water. According to the Christian Science Monitor, the Daasanach have begun cultivating the land and fishing using the waters of the River Omo-Lake Turkana Delta in competition with the Kenyan Turkana people for both land and water resources.
Flamingo Lake on Central Island in Lake Turkana. The oldest sedimentary records go back to the Cretaceous, including units previously informally referred to as the Turkana grits like the Lapurr Sandstone and are dominated by eastward flowing fluvial sequences draining into the Indian Ocean; [3] later formations from the Oligocene and Miocene are characterised by similar fluvial regimes that ...
A map of the Ilemi Triangle showing 1938 "red line" or "Wakefield Line", 1947 "blue line" and Sudan's 1950 patrol line (green). To the southeast of the Ilemi triangle, Ethiopian emperor Menelik laid claim to Lake Turkana and proposed a boundary with the British to run from the southern end of the lake eastward to the Indian Ocean, which was shifted northward when the British and Ethiopian ...
An 1877 map of Mars by Giovanni Schiaparelli. North is at the top of this map. In most maps of Mars drawn before space exploration the convention among astronomers was to put south at the top because the telescopic image of a planet is inverted.
The Chalbi Desert is located in between Mount Marsabit and Lake Turkana. [1] [2] The area is 110 km long and 10 to 20 km wide and it extends over 100,000 km 2. [3] The area is composed of an ancient lake-bed, rocky surface and lava regions. [4] The ancient lake-bed of Chalbi used to be a shallow lake around 10,000 to 11,000 years ago. [5]
Scientists have said they know more about the surface of Mars than they do about the bottom of the largest fresh surface water system on earth. Here are some that have been discovered so far.
The source of this outflow has been suggested as overflow from the Argyre crater, formerly filled to the brim as a lake by channels (Surius, Dzigai, and Palacopus Valles) draining down from the south pole. If real, the full length of this drainage system would be over 8000 km, the longest known drainage path in the solar system.