Wanne tectonic tsarin sadaukar Rasha a fili? Tectonics da topography na Rasha Bayyana

A babbar yanki na gandun daji daga Pechora da Karelian taiga, itacen oak bazuwa zuwa tsakiyar band, wanda ya hada da daji hatsi barns kuma makiyaya tundra - dukan wannan yankin - ba cewa wasu, a matsayin Rasha a fili. Taswirar kasar mu tabbatar da cewa waɗannan ƙasashe ne babban yawan birane da garuruwa, sabili da haka suna da mafi densely lugar.

Rasha ko Gabas Turai Bayyana gani a fiye da dubu-shekara tarihi na Rasha. Ta yi aiki a matsayin mai filin domin kwata 'yanci fadace-fadace, shi kuwa suka bi ta Tatar-mangolawa, dakarun na Napoleon da kuma Hitler. Shi ne a kan wannan a fili fãta shimfiɗaɗɗa grandiose neman sauyi events. Yana kuma shige da asali yi na gurguzu al'umma. Kuma har yanzu wannan yanki ne mai muhimmanci da tattalin arziki na Rasha.

labarin kasa

Gabas Turai Bayyana aka located a cikin sararin ƙasa. A ta yanki, shi ne na biyu kawai ga Amazon. Its ƙasar farawa daga tekun na Baltic Sea da kuma mika zuwa dutsen jeri na Urals, daga White Sea da Barents Sea zuwa Caspian da kuma Azov.

A ɓangaren da na Rasha Bayyana ne irin wannan cewa yana da damar yin amfani da biyu tekuna.

A arewa maso yammacin ɓangare na wannan yanki yana da iyaka ga Scandinavian duwãtsu. A kudu maso yammacin da yamma ya kai gare shi da kunya na tsakiya da Turai da kuma Carpathians. Me kuma suna cikin duwatsu a kan iyakar da yankin shagaltar da ta Rasha a fili? Map nuna wuri a kudu maso gabashin Caucasus, da Urals da Mogodzhary - a gabas. Bugu da kari, da yankin da Rasha da bayyana ƙare a arewacin kafa na Crimean Mountains in Crimean sashin. Wannan dukan yanki na hudu da miliyan murabba'in mita. Wannan shi ne fiye da biyu da rabin kilomita dubu daga arewa zuwa kudu, da kuma dubu - daga gabas zuwa yamma.

A ɓangaren da na Rasha Bayyana ne irin wannan cewa, ta manyan yankunan su ne a cikin Rasha Federation. Haka kuma, a nan suna located kasashe irin su Latvia da kuma Belarus, Estonia, Lithuania, Ukraine da kuma Moldova, Poland da kuma Finland, Bulgaria da Romania, da kuma Kazakhstan.

taimako

A cikin ƙasa na gabashin Turai Bayyana located tudu, da matsakaicin tsawo - daga 200 zuwa 300 mita saman teku matakin. Akwai kuma filayen kwari da yayyo su manyan koguna. Matsakaicin tsawo na bayyana ne lura a cikin Urals, kazalika a Bugulma-Veremeevskoy tudu. Ga shi kai matakin na 479 m. A talakawan tsawo daga cikin matakin da dukan ƙasar kwari ne a kusa da 170 mita.

Description da rarrabuwa na waje ãyõyin taimako tsunduma orography. Wannan shi ne daya daga cikin batutuwa, wanda ya hada da labarin kasa. Rasha Bayyana a kan filaye, wanda aka bayyana orography, ne zuwa kashi uku makada - tsakiya, arewa da kudancin. A farko daga gare su a cikin Rasha a fili, za ka iya ganin irin wannan wani tudu: Volga, Central Rasha, Bugulma-Belebey da Janar Sirt. Sun rabu da juna Low Volga da Oka-Don filayen kwari.

A tsakiyar band

Relief na Rasha Bayyana a arewacin tsiri na mafi yawa low-maƙaryaciya. Kawai a wasu wuraren a yankin singly ko a kananan tutocin furanni a warwatse kananan tudu. A cikin shugabanci daga yamma zuwa gabas da kuma arewa-maso-gabas suna m Smolensk da Moscow, kazalika da Valdai Hills da ridges na Arewa Zone. Ta hanyar da yankuna ne watershed tsakanin Arctic, Arewa, Atlantic, kazalika da draining ciki Aral-Caspian tasa. Abin lura shi ne cewa daga Arewa ridges ga Barents kuma White tekuna, akwai wasu raguwa a cikin ƙasa na filayen.

A cikin uku, kudancin tsiri akwai yawa filayen kwari. Daga gare su, The Black Sea, Caspian da sauransu. Sun rabu da low elevations (Stavropolskaya Ergeni da t. D.).

Nau'in tectonic Tsarin

A cikin duniya ta ɓawon burodi yana da manyan yankunan wanda iyakoki ne m laifinsu. Wannan ne tectonic Tsarin. Sun yi karatu a raba ma'aunan kasa kimiyya. Its sunan - tectonics. Wannan horo mayar da hankali a kan biyu manyan Tsarin cewa suna located a cikin duniya a ɓawon burodi. Wannan dandali, kazalika da dabba ba a kanta bel. A farko daga cikin wadannan yankunan su ne barga, da ciwon wani lebur surface. Dandamali ne riga a ƙasa halakar folded Tsarin. A daidai wannan lokaci suna da wani biyu-Layer tsari. Saboda haka, a cikin ƙananan ɓangare na dandali ne crystalline tushe wanda aka hada da tsohon sawmills. Sama da wannan Layer ne mai sedimentary murfin. Shiga a cikin samuwar dauki daga baya adibas. Tectonics allocates slabs da katakai da dandamali. A farko su ne wadanda wuraren da kafuwar ta'allaka ne gaba ɗaya a kan zurfin, ta rufe sedimentary murfin. M crystalline rabo ne guda tushe, dagagge sama da ƙasa surface. Akwai kuma wani sedimentary murfin. Duk da haka, shi ne, ba m da kuma low-iko.

Game da m bel, shi ne wani elongated rabo a cikin ɓawon burodi, a cikin abin da wuri har zuwa yanzu lokaci ci gaba da ilimi tafiyar matakai.

Bisa ga wannan rarrabuwa, to a tectonic tsarin sadaukar Rasha a fili? Hakika, da farko kungiyar, cewa shi ne, zuwa dandamali.

A tarihin abin da ya faru

Dalili na Rasha Bayyana ne daɗaɗɗe dandali. Wannan shi ne dalilin da ya sa taimako na yankin kunshi yafi na Shefela. Da samuwar irin wannan sararin ƙasa da tasirin da take da, da yawa na halitta dalilai. Wannan iska, ruwa da kuma glaciers.

Kafuwar Gabas Turai dandali located a daban-daban zurfin. Kawai tsakanin Karelia da Kola Larabawa ta shiga cikin ƙasa ta surface. Wannan sashi an kira Baltic garkuwa. An hade tare da asalin Hibin zubar a kan Kola Larabawa. A cikin sauran kafuwar maida hankali ne akan sedimentary cover, wanda yana da wani daban-daban iko.
All elevations da suke a kan Gabas Turai Bayyana, kafa wani dandali kududdufai, ko a ƙarƙashin rinjayar da wani gleiser, ko tsince a kafuwar.

Effect na tectonic faranti na wuri mai faɗi

Rasha da bayyana yana da wani hali dandali taimako. Tare da duk da filayen kwarinta, kuma uplands ne na tectonic asalin. Mene ne siffofin wannan dandali? Wanne tectonic tsarin sadaukar Rasha a fili?

Da dukan da ƙasa mamaye lebur ƙasa. Kuma shi ke da godiya ga tectonic tsarin, wanda yana mai bayyana dandali. All tushe tafka magudi ya kai ga samuwar mafi girma a filayen kwari da kuma wasu tuddai. Alal misali, kiwon kafuwar Voronezh ne dalilin da Jamhuriyar Rasha Upland. Ragewan da dandamali ya kai ga zargin da kogwanni da kuma cikin Caspian ciki.

Tectonic tsarin da Rasha Bayyana a kan mafi ƙasa nuna Precambrian crystalline farantin da kafuwar. Kudancin zone located a kan arewa gefen Scythian farantin kwance a kan Paleozoic folded ginshiki. Wannan tsarin ya ba da wani karin daidai amsar tambayar a matsayin abin da na tectonic tsarin da kwazo Rasha a fili. A iyakar tsakanin biyu faranti ba zai tasiri a ƙasa.

A tsarin da tectonic strata

Duk da cewa da janar hali na ƙasa ne, bayyananne, a cikin sauƙi akwai biyu filayen kwari da kuma upland. A bayani ga wannan za a iya samu a cikin tectonic fasali na Rasha Bayyana. Gaskiyar cewa da tsarin shi ne iri-irin da kuma zalunci hali na zamani da ilimi da ƙungiyoyi. A kusa da jarrabawa ta bayyana cewa dandali a baya da Rasha da bayyana, ya kunshi karami abubuwa. Su ne:
- allon.
- anteklizy wakiltar yankunan m tushe.
- syncline ne yankunan glei Precambrian ginshiki ne dake a babban zurfin.

anteclise

The most of wadannan abubuwa suna located a cikin tsakiyar ɓangare na Rasha farantin. Wannan ne Volga-Urals da Voronezh anticline. Kamar yadda wani ɓangare na farko daga gare su ne manyan karfafa (vaults) da kuma ciki. A wannan yanayin, kauri da sediments ne game da 800 mita.

A ƙasa na Voronezh anticline hankali sauka zuwa arewa. A surface harsashinsa ne na bakin ciki a ta kauri shaida na carbon, da kuma Devonian ordovika. A kan wani m kudancin kafaɗar overlying kankara na Paleogene kuma Cretaceous. Shi ne a nan, kuma carbon.

syneclise

A mafi tsoho da hadaddun a cikin abun da ke ciki kashi ne Moscow yankin. A nan, crystalline ginshiki na faruwa a cikin duniya ta ɓawon burodi a babban zurfin. Dalili Moscow syneclise ne aulacogens, wanda suna cike m strata na Reef. Sama da wadannan yadudduka da sedimentary cover aka wakilta daban-daban kankara daga Cambrian ga Cretaceous.

A Neogene-Quaternary Moscow syneclise halartar m karfafa. Wannan ya nuna a cikin ƙasa, inda akwai irin wannan wani tudu a matsayin Valdai Hills da Smolensk-Moscow, kazalika da filayen kwari - Northern Dvina da Upper Volga.

A kan Gabas Turai Bayyana ne wani babbar syneclise - Pechora. Yana bautarka da ƙasa na sandan a arewa-maso-gabashin ɓangare na Rasha Plate. Its a block tushe ne m at daban-daban zurfin, kai gabashin yankin daga 5000 zuwa 6000 mita. Cika da syncline ne m strata Paleozoic kankara wanda zoba Meso-Cenozoic adibas.

ma'adanai

Saboda haka, da muka yanke shawarar yin oda zuwa wani tectonic tsarin sadaukar Rasha a fili, abin da yake ta geologic tarihi. Saboda da dogon lokaci na da samuwar, wannan mafi tsufa dandali ne mai iko geostruturu. Ya ƙunshi inexhaustible reserves na ma'adanai. Saboda haka, a cikin kafuwar dandali samu adibas tama. Suna located a sashi na Kursk Magnetic anomaly. A sedimentary cover dandali gano kwal reserves. Da suka ci gaba a cikin gabashin ɓangare na Donets Basin da kuma Moscow tasa. A Mezozoic da Paleozoic ne reserves na man fetur da kuma iskar gas. Wannan ne Ural-Volga tasa. Ba da nisa daga Syzran gano shale. A cikin zurfin na Rasha Bayyana yawa daban-daban kayan gini - .. farar ƙasa da tsakuwa, da yumɓun, da dai sauransu ruwan kasa farar ƙasa, haƙar gishiri da phosphates samu a cikin sedimentary murfin.

A bambancin da halitta yankunan

Kamar yadda muka riga sani, da Rasha Bayyana aka located a cikin sararin ƙasa. Wannan shi ne dalilin da ya sa shi ne halin da mai pronounced bambancin da sauyin yanayi. Halitta zones na Rasha da bayyana gabatar a duk da bambancin. A Far Arewa - tundra tare da low ikon da matalauta da ciyayi girma a kan peat humus kasa. Summer kwantar da wadannan sassa, tare da high zafi, da kara saboda da kusanci na Arctic Ocean.

Just kudu na yankin ne gandun daji tundra zone. Next shi ne tsakiyar yankin na Rasha Bayyana. An rufe gandun daji. A ta arewacin aka mamaye duhu coniferous taiga, wanda ke tsiro a kan boggy podzolic kasa. Wajen kudu akwai gauraye iri-iri, alternating tare da deciduous gandun daji na itacen oak, Maple da Linden.

Halitta zones na Rasha fili a kudancin gandun daji da kuma steppe aka gabatar. Wannan ƙasa tare da m, kamar yadda mai mulkin, black gona da herbaceous ciyayi.

wanda bai isa ƙasar

Matsananci kudu-maso-gabas da Gabas Turai Bayyana aka located a cikin Caspian ciki. Ƙarƙashin rinjayar da bushe sauyin yanayi a nan kafa Semi-hamada yanki, located a kan chestnut kasa. A wasu wuraren akwai kuma Hamada. Wannan sashi na launin toka kasa, gishiri licks da gishiri Marshes.

ƙarshe

Ta yaya mafi cikakken da kuma Rasha a fili za a iya karatu a daki-daki? A tebur a cikin abin da daban-daban Manuniya gabatar (tectonic tsarin, halitta yankunan, sauyin yanayi da kuma t. D.) Ya kamata a hankali dauke. Wannan shi ne mai ban mamaki na gani taimakon da za su iya samar da invaluable taimako a fahimtar da koyo da ake buƙata abu.