तधंगु रिफ्ट स्वनिग: Difference between revisions

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[[Image:Greatrift.jpg|thumb|250px|उत्तरी खण्ड। सिनाई प्रायद्विप दथुइ दु धासा [[मृत सागर]] व [[जोर्डन खुसि]] उत्तरय् ला]]
[[Image:Greatrift.jpg|thumb|250px|Northern section of the Great Rift Valley. The [[Sinai Peninsula]] is in center and the [[Dead Sea]] and [[Jordan River]] valley above]]
'''तधंगु रिफ्ट स्वनिग''' छगु तधंगु भौगोलिक बनावट खः। थुकिगु हाक करिब ६००० कि मि दु। थ्व दक्षिण पश्चिम एसियायागु उत्तरी [[सीरिया]] निसें पूर्वी अफ्रिकायागु मध्य मोजाम्बिक तक्क थ्यं। थ्व स्वनिगयागु ब्या ३० निसें १०० किमि तक्क दु व थुकिगु जा छुं सछि निसें द्वलंद्व मिटर तक्क दु। थुकिगु नां अनवेषक [[जोह्न वाल्टर ग्रेगोरी]]नं तयादिगु खः।
 
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पूर्वी अफ्रिकाय् थ्व स्वनिग निगु भागय् बाई, '''पूर्वी रिफ्ट''' व '''पश्चिमी रिफ्ट'''।
 
पश्चिमी रिफ्ट (अल्बर्टाइन रिफ्ट) अफ्रिकायागु छुं तधंगु गुंतेगु (दसु-भिरुंगा गुं, मितुम्बा गु व रुवेन्जोरी श्रृंखलायागु सिथे ला धासा। थुकिलि रिफ्ट स्वनिग पुखुत दु व थ्व पुखुलि हलिमयागु दक्ले गावंगु पुखु दसु-तांगान्यिका (१४७० मिटर), भिक्टोरिया आदि।
The Western Rift, also called the Albertine Rift, is edged by some of the highest mountains in Africa, including the [[Virunga Mountains]], [[Mitumba Mountains]], and [[Ruwenzori Range]]. It contains the [[Rift Valley lakes]], which include some of the deepest [[lake]]s in the world (up to 1,470 meters deep at [[Lake Tanganyika]]). [[Lake Victoria]], the second largest area freshwater lake in the world, is considered part of the Rift Valley system although it actually lies between the two branches. All of the [[Great Lakes (Africa)|African Great Lakes]] were formed as the result of the rift, and most lie within its rift valley.
 
In [[Kenyaकेन्या]]य् theनैरोबीयागु valleyउत्तरय् isथ्व deepestस्वनिग toदकले theगा north of [[Nairobi]].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|Theरिफ्ट Riftस्वनिग Valleyएल्डोरेट, near Eldoret,केन्या Kenyaनापं]]
 
==Geothermal activity==
==जियोथर्मल ज्याखँ==
 
The formation of the Rift Valley continues, probably driven by [[mantle plume]]s 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]].
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The volcanic activity at this site and unusual concentration of [[hotspot (geology)|hotspot]]s has produced the volcanic mountains [[Mount Kilimanjaro]], [[Mount Kenya]], [[Mount Karisimbi]], [[Mount Nyiragongo]], [[Mount Meru, Tanzania|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 [[carbonatite|natrocarbonatite]] volcano in the world.
 
==मानव विकासक्रमय् लुयावगु उत्खननतः==
==Discoveries in human evolution==
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 [[Hominidae|hominid]] ancestors of modern humans have been found there, including those of "[[Australopithecus afarensis|Lucy]]", a nearly complete [[australopithecine]] skeleton, which was discovered by anthropologist [[Donald Johanson]]. [[Richard Leakey|Richard]] and [[Mary Leakey]] have also done significant work in this region.
 
==स्वया दिसँ==
==See also==
*[[ग्राबेन]]
*[[Graben]]
*[[होर्स्ट (खनिजशास्त्र)]]
*[[Horst (geology)]]
*[[रिफ्ट स्वनिग]]
*[[Rift valley]]
 
== पिनेयागु स्वापूत ==
== External links ==
*[http://anthro.palomar.edu/hominid/images/map_of_great_rift_valley.gif Smallचीधंगु simpleसाधरण-colouredरङ्गयागु mapनक्सा किपा]
*[http://www.albertinerift.org/arift-protectedareas Mapsअल्बर्टाइन fromरिफ्ट theज्याझ्वयागु Albertine Rift Programmeनक्सा]
 
[[Category:Great Rift Valley|*अफ्रिका]]
[[Category:Seismic faults]]
 
[[an:Bal d'o Gran Rift]]