तधंगु रिफ्ट स्वनिग: Difference between revisions

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[[केन्या]]य् नैरोबीयागु उत्तरय् थ्व स्वनिग दकले गा वं। As the lakes in the Eastern Rift have no outlet to the sea, these lakes tend to be shallow and have a high [[mineral]] content as the evaporation of water leaves the salts behind. For example, [[Lake Magadi]] has high concentrations of soda ([[sodium carbonate]]) and [[Lake Elmenteita]], [[Lake Baringo]], [[Lake Bogoria]], and [[Lake Nakuru]] are all strongly alkaline, while [[Lake Naivasha]] needs to be supplied by freshwater springs to support its biological variety.
 
 
[[Image:EAfrica.jpg|thumb|right|300px|Map of East Africa showing some of the historically active volcanoes (red triangles) and the [[Afar Triangle]] (shaded, center) — a [[triple junction]] where three plates are pulling away from one another: the Arabian Plate, and the two parts of the African Plate (the Nubian and the Somalian) splitting along the East African Rift Zone (USGS).]]
[[Image:Africa6 006.jpg|right|300px|thumb|right|रिफ्ट स्वनिग एल्डोरेट, केन्या नापं]]