Baikal Musulunci: tsarin, topography, dutsen tsarin, musamman

Baikal nadawa fãra daga lokacin orogeny, kuma shi ne located in Siberia. Wannan sunan da aka gabatar a fanning binciken kasa Shatsky a cikin thirties na karshe karni girmama na eponymous lake, domin shi ne a wancan lokacin, wannan bangare na yankin da aka kafa.

A cikin abun da ke ciki da kuma halaye na nadawa ce wannan labarin. Bayani zai taimaka domin ya koyi game da wannan yanki na duniya.

A tsarin da nadawa

Wannan ninka tsarin kafa ta ci daga yankuna biyu - da Baikal da kuma Yenisei. Shi yana da wani m da wani ciki na, da kuma iyakar da ke tsakanin su protrudes zone, gudanar daga tafkin zuwa Mame kogin. Baikal yankin na nadawa kasu kashi na waje da kuma ciki. A karshen hada da abubuwa masu arziki a zamanin d kankara.

Features

Babban siffa daga cikin Baikal Ninka System ne cewa shi aka kafa na dogon lokaci (da dukan karshe mataki Proterozoic), da kuma sãsanninta, suna located in yawa sassa na Urals, Taimyr, Kazakhstan, da Caucasus, Iran, Tien Shan da sauransu. Bugu da kari, baykality kowa a cikin wasu sassa na Duniya. Alal misali, a kasar Faransa, India, North America da kuma Australia. Duk da haka, a cikin wadannan bangarori ne, a maimakon haka, su analogs (Kadoma, minaaskaya, musgravidy). Baikal ninka "inuwõyi" da kuma wani ɓangare na Brazil, located a kan Red Sea Coast.

A wani zamanin mahara dandamali baicalensis tectogenetic sa'an nan a kafa a sakamakon da tectonic furrows, wanda baya ta fara cika da wani jam'i na sedimentary kankara. A sakamakon hakowa da kuma ayyukan bincike a fagen geophysics, wadannan GROOVES aka samu a wasu dandamali - da Gabas Turai da kuma Siberian. Ko da a cikin kudu na duniya (a cikin sassa na Antarctic), wannan kafa nadawa dandali, dandana metamorphic da Magnetic tafiyar matakai.

A tsarin

Mountain jeri, wanda yana da Baikal nadawa, ya hada da kudancin Siberia. Wadannan sun hada da Trans-Baikal da Baikal yankin, wanda shi ne wani tudu Olekma tare Game plateaus (Vitim, Baikal) da kuma uplands (Charskaya, Patom da Severobaikalsk). Wadannan sassa ne batun glaciation. A nan ana ayi da low duwãtsu da kwaruruka, wanda su ne a kan laifi Lines.

A manyan yawan arzikin albarkatun kasa na Baikal ninka. Relief yadda na musamman da daban-daban adibas ne a cikin wannan tsarin (msl, jan, Mercury, da zinariya, tin, tutiya da sauransu). Kuma, kamar yadda sunan ya nuna, mafi muhimmanci janye a nan shi ne tafkin Baikal, wanda yana da jinjirin wata siffar. An located a cikin Baikal dutsen iyaka, kewaye a kan dukkan bangarorin da dutsen jeri. Shimfidar wurare na wadannan wurare da kuma jawo hankalin masu yawon shakatawa.

lake Baikal

Baikal folded - biyunsa wuri. Cewa babu daya ne kawai lake, game da wanda aka ce dan kadan mafi girma. Its tsawon shi ne fiye da mutum ɗari shida da kilomita, da jimlar yanki maida hankali ne akan wani yanki a kan dubu uku murabba'in mita. km. Kamar yadda aka sani a da yawa, shi ne mafi zurfi a duniya. A wasu wurare da zurfin kai fiye da mil bãya, kuma idan muka dauki ma'anar darajar, game da ɗari bakwai. Yana da na kowa sanin cewa gudana a cikin tafkin mai yawa na gudãna (fiye da ɗari uku), kuma ya bi daya kawai - da Angara. fiye da rabin zo daga mai shigowa ruwa a kan kogin. Selenga. A Baikal yana da dama tsibiran, da most of wanda shi ne Olkhon. An gano cewa lake aka kafa game da miliyan 25 da suka wuce. Saboda haka, a manyan jiki na ruwa an dauke su ba kawai mafi zurfi amma kuma mafi tsoho. Kuma godiya ga bambance bambancen ƙasa a kan Baikal arziki duniyar Flora da fauna.

Baikal

A arewa maso yammacin lake jeri ne Yammacin Pribaikalye wanda shi ne kunkuntar tsiri, kuma ya kai wani tsawo na 450 mita. Wadannan dutsen tsarin waje duba wuce yarda da kyau da kuma daidai fayyace bakin tafkin. Musamman alama spiky dutse kololuwa. Baikal nadawa (taimako nau'i ne wadanda ba misali) janyo hankalin masana kimiyya da dama a duniya.

Baikal

Zabaikalye zubar tsakanin Pribaykalye da kogin Argun. Its tsawon ne game da daya da rabi kilomita dubu da yake kudu maso yammacin yankin arewa-maso-gabas. A wasu wurare, da duwãtsu located a kan ruwa matakin. Dangane da tsarin da kuma shekaru na taimako, Baikal za a iya raba da dama da alaka yankunan. A mafi kunya ne wani encoder, wanda ya kai wani tsawo na uku kilomita. Saboda ta sau da yawa, kuma da yawa masu hawa ziyarci wannan halitta abu, kamar Baikal Musulunci. A tsari na taimako na yankin ne mai ban mamaki. Kuma kawai a kan wannan dutse mai tsayi glaciers sun samu a lõkacin da Quaternary glaciations. Wannan kunya ne kunshe a Stanovoy tsarin, wanda aka kafa daga kwari da duwãtsu tsakanin sarƙoƙi. A abun da ke ciki na kowane sarkar hada da gangaren char da lebur ridges. A kudancin Trans-Baikal yanki baza Shefela. Saboda a wadannan wurare a lokacin da shekara low matakan da ruwan sama, da yashewa matakai ne m. A cikin gabashin ɓangare na Trans-Baikal saboda ruwa sosai kafa proluvial-gishiri madaukai. The taimako a nan ya dubi asali. An yafi bayyana a lebur sassan, wanda tsaya daga sharply da babban ridges. Wannan irin taimako kira Gobi.

Duk da dutsen jeri na Baikal nadawa da kuma musamman topography, fiye da su ne ban sha'awa ga masana kimiyya.