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थ्व पौ देवनागरीं बोट छ्यला थःमंतुं नेपाललिपिइ हिलातःगु ख। थ्व पौयात च्वसु पतिइ यंकेन्ह्यः छकः ब्वनाः पाय्छि जू/मजूगू स्वयादिसँ। [[𑐎𑐶𑐥𑐵:Greatrift.jpg|thumb|250px|𑐄𑐟𑑂𑐟𑐬𑐷 𑐏𑐞𑑂𑐜। 𑐳𑐶𑐣𑐵𑐃 𑐥𑑂𑐬𑐵𑐫𑐡𑑂𑐰𑐶𑐥 𑐡𑐠𑐸𑐂 𑐡𑐸 𑐢𑐵𑑅𑐳𑐵 𑐩𑐺𑐟 𑐳𑐵𑐐𑐬 𑐰 𑐖𑑀𑐬𑑂𑐜𑐣 𑐏𑐸𑐳𑐶 𑐄𑐟𑑂𑐟𑐬𑐫𑑂 𑐮𑐵]] 𑐟𑐢𑑄𑐐𑐸 𑐬𑐶𑐦𑑂𑐚 𑐳𑑂𑐰𑐣𑐶𑐐 𑐕𑐐𑐸 𑐟𑐢𑑄𑐐𑐸 𑐨𑑁𑐐𑑀𑐮𑐶𑐎 𑐧𑐣𑐵𑐰𑐚 𑐏𑑅। 𑐠𑐸𑐎𑐶𑐐𑐸 𑐴𑐵𑐎 𑐎𑐬𑐶𑐧 𑑖𑑐𑑐𑑐 𑐎𑐶 𑐩𑐶 𑐡𑐸। 𑐠𑑂𑐰 𑐡𑐎𑑂𑐲𑐶𑐞 𑐥𑐱𑑂𑐔𑐶𑐩 𑐊𑐳𑐶𑐫𑐵𑐫𑐵𑐐𑐸 𑐄𑐟𑑂𑐟𑐬𑐷 𑐳𑐷𑐬𑐶𑐫𑐵 𑐣𑐶𑐳𑐾𑑄 𑐥𑐹𑐬𑑂𑐰𑐷 𑐀𑐦𑑂𑐬𑐶𑐎𑐵𑐫𑐵𑐐𑐸 𑐩𑐢𑑂𑐫 𑐩𑑀𑐖𑐵𑐩𑑂𑐧𑐶𑐎 𑐟𑐎𑑂𑐎 𑐠𑑂𑐫𑑄। 𑐠𑑂𑐰 𑐳𑑂𑐰𑐣𑐶𑐐𑐫𑐵𑐐𑐸 𑐧𑑂𑐫𑐵 𑑓𑑐 𑐣𑐶𑐳𑐾𑑄 𑑑𑑐𑑐 𑐎𑐶𑐩𑐶 𑐟𑐎𑑂𑐎 𑐡𑐸 𑐰 𑐠𑐸𑐎𑐶𑐐𑐸 𑐖𑐵 𑐕𑐸𑑄 𑐳𑐕𑐶 𑐣𑐶𑐳𑐾𑑄 𑐡𑑂𑐰𑐮𑑄𑐡𑑂𑐰 𑐩𑐶𑐚𑐬 𑐟𑐎𑑂𑐎 𑐡𑐸। 𑐠𑐸𑐎𑐶𑐐𑐸 𑐣𑐵𑑄 𑐀𑐣𑐰𑐾𑐲𑐎 𑐖𑑀𑐴𑑂𑐣 𑐰𑐵𑐮𑑂𑐚𑐬 𑐐𑑂𑐬𑐾𑐐𑑀𑐬𑐷𑐣𑑄 𑐟𑐫𑐵𑐡𑐶𑐐𑐸 𑐏𑑅।
𑐨𑐹𑐐𑑀𑐮
[सम्पादन]𑐠𑐸𑐎𑐶𑐐𑐸 𑐡𑐎𑑂𑐮𑐾 𑐄𑐟𑑂𑐟𑐬𑐫𑐵𑐐𑐸 𑐨𑐵𑐐 𑐮𑐾𑐧𑐵𑐣𑐣𑐫𑐵𑐐𑐸 𑐧𑐾𑐎𑑂𑐎𑐵 𑐳𑑂𑐰𑐣𑐶𑐐𑐮𑑄 𑐰𑐿। 𑐠𑑂𑐰 𑐨𑐵𑐐𑑄 𑐮𑐾𑐧𑐵𑐣𑐣 𑐐𑐸𑑄 𑐰 𑐊𑐣𑑂𑐚𑐶-𑐮𑐾𑐧𑐵𑐣𑐣 𑐐𑐸𑑄𑐫𑐵𑐟 𑐧𑐵𑐃। 𑐡𑐎𑑂𑐲𑐶𑐞𑐾 𑐠𑐸𑐎𑐶𑐫𑐵𑐟 𑐴𑐸𑐮𑐵 𑐳𑑂𑐰𑐣𑐶𑐐 𑐢𑐵𑐂 𑐰 𑐠𑐶𑐎𑐶𑐮𑐶𑑄 𑐖𑑂𑐘𑐵𑐮𑐶𑐮𑐷 𑐐𑐸𑑄 𑐰 𑐐𑑀𑐮𑐵𑐣 𑐴𑐵𑐂𑐚𑐫𑐵𑐟 𑐧𑐵𑐃। 𑐀𑐗 𑐡𑐎𑑂𑐲𑐶𑐞𑐾, 𑐠𑑂𑐰 𑐳𑑂𑐰𑐣𑐶𑐐𑐮𑐾 𑐖𑑀𑐬𑑂𑐜𑐣 𑐏𑐸𑐳𑐶 𑐮𑐵 𑐰𑐿। 𑐖𑑀𑐥𑑂𑐬𑑂𑐜𑐣 𑐏𑐸𑐳𑐶 𑐴𑐸𑐮𑐵 𑐥𑐸𑐏𑐸 𑐖𑐸𑐫𑐵 𑐂𑐖𑐬𑐵𑐫𑐮𑐫𑐵𑐐𑐸 𑐖𑑂𑐘𑐵𑐮𑐶𑐮𑐷 𑐳𑐵𑐐𑐬 𑐖𑐸𑐳𑐾𑑄 𑐡𑐎𑑂𑐲𑐶𑐞𑐾 𑐖𑑀𑐬𑑂𑐜𑐣 𑐳𑑂𑐰𑐣𑐶𑐐 𑐖𑐸𑐫𑐵 𑐂𑐖𑐬𑐵𑐫𑐮-𑐖𑑀𑐬𑑂𑐜𑐣 𑐳𑐶𑐩𑐵𑐣𑐵𑐫𑐵𑐐𑐸 𑐩𑐺𑐟 𑐳𑐵𑐐𑐬𑐫𑑂 𑐠𑑂𑐫𑐣𑐶। 𑐩𑐺𑐟 𑐳𑐵𑐐𑐬𑑄 𑐡𑐎𑑂𑐲𑐶𑐞𑐾, 𑐬𑐶𑐦𑑂𑐚𑐫𑑂 𑐰𑐵𑐡𑐷 𑐀𑐬𑐧𑐵 𑐰 𑐀𑐎𑐧𑐵𑐫𑐵𑐐𑐸 𑐏𑐵𑐜𑐷 𑐰 𑐮𑐶𑐥𑐵 𑐴𑑂𑐫𑐵𑑄𑐐𑐸 𑐳𑐵𑐐𑐬 𑐮𑐵 𑐰𑐿।
thumb|left|𑐖𑑀𑐬𑑂𑐜𑐣 𑐬𑐶𑐦𑑂𑐚 𑐳𑑂𑐰𑐣𑐶𑐐 𑐳𑐬𑑂𑐐𑐟𑑄 𑐴𑑂𑐫𑐵𑑄𑐐𑐸 𑐳𑐵𑐐𑐬𑐫𑐵𑐐𑐸 𑐡𑐎𑑂𑐲𑐶𑐞𑐷 𑐨𑐵𑐐 marks a fork in the rift। 𑐂𑐠𑐶𑐫𑑀𑐥𑐶𑐫𑐵 𑐰 𑐊𑐬𑐶𑐟𑐺𑐫𑐵𑐫𑐵𑐐𑐸 𑐀𑐦𑐵𑐬 𑐟𑑂𑐬𑐶𑐨𑐹𑐖 𑐰𑐵 𑐡𑐵𑐣𑐵𑐎𑐶𑐮 𑐜𑐶𑐥𑑂𑐬𑐾𑐳𑐣 𑐚𑑂𑐬𑐶𑐥𑐮 𑐖𑑄𑐎𑑂𑐳𑐣𑐫𑐵𑐐𑐸 𑐠𑐵𑐫𑑂 𑐖𑐸𑐂𑐦𑐸। 𑐊𑐜𑐾𑐣𑐫𑐵𑐐𑐸 𑐏𑐵𑐜𑐷 𑐬𑐶𑐦𑑂𑐚𑐫𑐵𑐐𑐸 𑐥𑐹𑐬𑑂𑐰𑐷 𑐣𑐶𑐬𑐣𑑂𑐟𑐬𑐟𑐵 𑐏𑑅 - 𑐬𑐶𑐦𑑂𑐚 𑐡𑐾 𑐳𑑂𑐰𑐫𑐵 𑐣𑑂𑐴𑑂𑐫 𑐀𑐬𑐧𑐷 𑐥𑑂𑐬𑐵𑐫𑐡𑑂𑐰𑐶𑐥 𑐀𑐦𑑂𑐬𑐶𑐎𑐵𑐫𑐵𑐐𑐸 𑐣𑑂𑐫𑐾𑐎𑐸 𑐣𑐵𑐥 𑐳𑑂𑐰𑐵𑐣𑐵𑐔𑑂𑐰𑑄𑐐𑐸 𑐖𑐸𑐮 𑐰 𑐠𑑂𑐰 𑐠𑐵𑐳𑑄 𑐩𑐢𑑂𑐫 𑐩𑐴𑐵𑐳𑐵𑐐𑐬𑐷𑐫 𑐬𑐶𑐖𑐫𑐵𑐐𑐸 𑐬𑐸𑐥𑐾 𑐴𑐶𑐣𑑂𑐡 𑐩𑐴𑐵𑐳𑐵𑐐𑐬𑐫𑑂 𑐣𑐶𑐬𑐣𑑂𑐟𑐬𑐟𑐵 𑐧𑐷। 𑐡𑐎𑑂𑐲𑐶𑐞𑐥𑐱𑑂𑐔𑐶𑐩 𑐡𑐶𑐱𑐵𑐫𑑂 𑐠𑑂𑐰 𑐟𑐢𑑄𑐐𑐸 𑐬𑐶𑐦𑑂𑐚 𑐳𑑂𑐰𑐣𑐶𑐐𑐫𑐵𑐐𑐸 𑐬𑐸𑐥𑐾 𑐣𑐶𑐬𑐣𑑂𑐟𑐬 𑐖𑐸𑐂 𑐰 𑐊𑐠𑐶𑐫𑑀𑐥𑐶𑐫𑐵𑐮𑐷 𑐴𑐵𑐂𑐮𑑂𑐫𑐵𑐣𑑂𑐜𑐫𑐵𑐟 𑐣𑐶𑐐𑐸 𑐨𑐵𑐐𑐫𑑂 𑐧𑐵𑐃।
𑐥𑐹𑐬𑑂𑐰𑐷 𑐀𑐦𑑂𑐬𑐶𑐎𑐵𑐫𑑂 𑐠𑑂𑐰 𑐳𑑂𑐰𑐣𑐶𑐐 𑐣𑐶𑐐𑐸 𑐨𑐵𑐐𑐫𑑂 𑐧𑐵𑐃, 𑐥𑐹𑐬𑑂𑐰𑐷 𑐬𑐶𑐦𑑂𑐚 𑐰 𑐥𑐱𑑂𑐔𑐶𑐩𑐷 𑐬𑐶𑐦𑑂𑐚।
𑐥𑐱𑑂𑐔𑐶𑐩𑐷 𑐬𑐶𑐦𑑂𑐚 (𑐀𑐮𑑂𑐧𑐬𑑂𑐚𑐵𑐂𑐣 𑐬𑐶𑐦𑑂𑐚) 𑐀𑐦𑑂𑐬𑐶𑐎𑐵𑐫𑐵𑐐𑐸 𑐕𑐸𑑄 𑐟𑐢𑑄𑐐𑐸 𑐐𑐸𑑄𑐟𑐾𑐐𑐸 (𑐡𑐳𑐸-𑐨𑐶𑐬𑐸𑑄𑐐𑐵 𑐐𑐸𑑄, 𑐩𑐶𑐟𑐸𑐩𑑂𑐧𑐵 𑐐𑐸 𑐰 𑐬𑐸𑐰𑐾𑐣𑑂𑐖𑑀𑐬𑐷 𑐱𑑂𑐬𑐺𑑄𑐏𑐮𑐵𑐫𑐵𑐐𑐸 𑐳𑐶𑐠𑐾 𑐮𑐵 𑐢𑐵𑑅𑐳𑐵। 𑐠𑐸𑐎𑐶𑐮𑐶 𑐬𑐶𑐦𑑂𑐚 𑐳𑑂𑐰𑐣𑐶𑐐 𑐥𑐸𑐏𑐸𑐟 𑐡𑐸 𑐰 𑐠𑑂𑐰 𑐥𑐸𑐏𑐸𑐮𑐶 𑐴𑐮𑐶𑐩𑐫𑐵𑐐𑐸 𑐡𑐎𑑂𑐮𑐾 𑐐𑐵𑐰𑑄𑐐𑐸 𑐥𑐸𑐏𑐸 𑐡𑐳𑐸-𑐟𑐵𑑄𑐐𑐵𑐣𑑂𑐫𑐶𑐎𑐵 (𑑑𑑔𑑗𑑐 𑐩𑐶𑐚𑐬), 𑐨𑐶𑐎𑑂𑐚𑑀𑐬𑐶𑐫𑐵 𑐁𑐡𑐶।
𑐎𑐾𑐣𑑂𑐫𑐵𑐫𑑂 𑐣𑐿𑐬𑑀𑐧𑐷𑐫𑐵𑐐𑐸 𑐄𑐟𑑂𑐟𑐬𑐫𑑂 𑐠𑑂𑐰 𑐳𑑂𑐰𑐣𑐶𑐐 𑐡𑐎𑐮𑐾 𑐐𑐵 𑐰𑑄। 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.
𑐖𑐶𑐫𑑀𑐠𑐬𑑂𑐩𑐮 𑐖𑑂𑐫𑐵𑐏𑑃
[सम्पादन]The formation of the Rift Valley continues, probably driven by mantle plumes and ultimately a result of the African superswell. The associated geothermal activity and spreading at the rift has caused the lithosphere to thin from a typical 100 km thickness for continents to a mere 20 km. Though it is common for one arm of a triple junction to fail, if spreading continues the lithosphere may rupture several million years hence, splitting eastern Africa off to form a new landmass. In short, this will lead to the formation of a new mid-ocean ridge.
The volcanic activity at this site and unusual concentration of hotspots has produced the volcanic mountains Mount Kilimanjaro, Mount Kenya, Mount Karisimbi, Mount Nyiragongo, Mount Meru and Mount Elgon as well as the Crater Highlands in Tanzania. The Ol Doinyo Lengai volcano remains active, and is currently the only natrocarbonatite volcano in the world.
𑐩𑐵𑐣𑐰 𑐰𑐶𑐎𑐵𑐳𑐎𑑂𑐬𑐩𑐫𑑂 𑐮𑐸𑐫𑐵𑐰𑐐𑐸 𑐄𑐟𑑂𑐏𑐣𑐣𑐟𑑅
[सम्पादन]The Rift Valley has been a rich source of fossils that allow study of human evolution, especially in an area known as Piedmont. Because the rapidly eroding highlands have filled the valley with sediments, a favourable environment for the preservation of remains has been created. The bones of several hominid ancestors of modern humans have been found there, including those of "Lucy", a nearly complete australopithecine skeleton, which was discovered by anthropologist Donald Johanson. Richard and Mary Leakey have also done significant work in this region.
𑐳𑑂𑐰𑐫𑐵 𑐡𑐶𑐳𑑃
[सम्पादन]𑐥𑐶𑐣𑐾𑐫𑐵𑐐𑐸 𑐳𑑂𑐰𑐵𑐥𑐹𑐟
[सम्पादन]
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विकिमिडिया मंका य् थ्व विषय नाप स्वापु दुगु मिडिया दु: Great Rift Valley |