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Аппалачський кам'яновугільний басейн — оди … Аппалачський кам'яновугільний басейн — один з найбільших у світі вугільних басейнів. Розташований на сх. США, на території шт. Алабама, Кентуккі, Вірджинія, Західна Вірджинія, Огайо, Меріленд, Пенсільванія, простягаючись більш ніж на 1200 км вздовж півд. схилів Аппалачів. на 1200 км вздовж півд. схилів Аппалачів.
, The geology of the Appalachians dates back … The geology of the Appalachians dates back to more than 480 million years ago. A look at rocks exposed in today's Appalachian Mountains reveals elongate belts of folded and thrust faulted marine sedimentary rocks, volcanic rocks and slivers of ancient ocean floor – strong evidence that these rocks were deformed during plate collision. The birth of the Appalachian ranges marks the first of several mountain building plate collisions that culminated in the construction of the supercontinent Pangaea with the Appalachians and neighboring Anti-Atlas mountains (now in Morocco) near the center. These mountain ranges likely once reached elevations similar to those of the Alps and the Rocky Mountains before they were eroded.e Rocky Mountains before they were eroded.
, Appalachernas geologi går tillbaka till fö … Appalachernas geologi går tillbaka till för mer än 480 miljoner år sedan. Berg som exponerats i dagens Appalacherna, där långsträckta bälten av veckade eller "brutna" sedimentära bergarter, vulkaniska bergarter och strimlor av ofiolit från den forntida havsbottnen, ger vid handen att dessa bergarter deformerades av kontinentalplattor som kolliderade. Appalachernas födelse markerar den första av flera förskjutningar som kulminerade i uppbyggandet av superkontinenten Pangea med Appalacherna och angränsande Anti-Atlas (nu i Marocko) nära centrum. Dessa bergskedjor nådde troligen en höjd som liknar de motsvarande i Alperna och Klippiga bergen innan de eroderades.a och Klippiga bergen innan de eroderades.
, Il bacino degli Appalachi è un bacino stru … Il bacino degli Appalachi è un bacino strutturale di avampaese che contiene rocce sedimentarie paleozoiche che coprono l'intero periodo che va dall'inizio del Cambriano fino al Permiano. Il suo nome fa riferimento ai monti Appalachi, una catena montuosa situata nella parte orientale del nord America. Da nord a sud la provincia del bacino degli Appalachi attraversa gli stati americani di New York, Pennsylvania, Ohio, Virginia Occidentale, Maryland, Kentucky, Virginia, Tennessee, Georgia e Alabama. Il margine settentrionale del bacino degli Appalachi si estende al di fuori della costa dei laghi Erie e Ontario fino al confine tra Stati Uniti e Canada. La provincia del bacino degli Appalachi copre un'area di circa 185 500 miglia quadre (480 000 km²) e ha una lunghezza di 1 075 miglia (1 730 km) da nordest a sudovest e una larghezza da 20 fino a 310 miglia (30 fino a 500 km) da nordovest a sudest. Il fianco nordovest del bacino è un largo che digrada dolcemente a sudovest del . Un terrane complesso dovuto alle spinte della fagliazione (Appalachian Fold e Thrust Belt o Eastern Overthrust Belt), formatosi alla fine del Paleozoico in seguito all'orogenesi alleganiana, caratterizza il fianco orientale del bacino. Le rocce metamorfiche e ignee della Blue Ridge Thrust Belt che delimitano la parte orientale della provincia del bacino degli Appalachi furono spinte verso ovest per più di 150 miglia (240 km) al di sopra delle rocce sedimentarie del Paleozoico.a delle rocce sedimentarie del Paleozoico.
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Appalachernas geologi går tillbaka till fö … Appalachernas geologi går tillbaka till för mer än 480 miljoner år sedan. Berg som exponerats i dagens Appalacherna, där långsträckta bälten av veckade eller "brutna" sedimentära bergarter, vulkaniska bergarter och strimlor av ofiolit från den forntida havsbottnen, ger vid handen att dessa bergarter deformerades av kontinentalplattor som kolliderade. Appalachernas födelse markerar den första av flera förskjutningar som kulminerade i uppbyggandet av superkontinenten Pangea med Appalacherna och angränsande Anti-Atlas (nu i Marocko) nära centrum. Dessa bergskedjor nådde troligen en höjd som liknar de motsvarande i Alperna och Klippiga bergen innan de eroderades.a och Klippiga bergen innan de eroderades.
, The geology of the Appalachians dates back … The geology of the Appalachians dates back to more than 480 million years ago. A look at rocks exposed in today's Appalachian Mountains reveals elongate belts of folded and thrust faulted marine sedimentary rocks, volcanic rocks and slivers of ancient ocean floor – strong evidence that these rocks were deformed during plate collision. The birth of the Appalachian ranges marks the first of several mountain building plate collisions that culminated in the construction of the supercontinent Pangaea with the Appalachians and neighboring Anti-Atlas mountains (now in Morocco) near the center. These mountain ranges likely once reached elevations similar to those of the Alps and the Rocky Mountains before they were eroded.e Rocky Mountains before they were eroded.
, Il bacino degli Appalachi è un bacino stru … Il bacino degli Appalachi è un bacino strutturale di avampaese che contiene rocce sedimentarie paleozoiche che coprono l'intero periodo che va dall'inizio del Cambriano fino al Permiano. Il suo nome fa riferimento ai monti Appalachi, una catena montuosa situata nella parte orientale del nord America.ta nella parte orientale del nord America.
, Аппалачський кам'яновугільний басейн — оди … Аппалачський кам'яновугільний басейн — один з найбільших у світі вугільних басейнів. Розташований на сх. США, на території шт. Алабама, Кентуккі, Вірджинія, Західна Вірджинія, Огайо, Меріленд, Пенсільванія, простягаючись більш ніж на 1200 км вздовж півд. схилів Аппалачів. на 1200 км вздовж півд. схилів Аппалачів.
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Bacino degli Appalachi
, Appalachernas geologi
, Geology of the Appalachians
, Аппалачський кам'яновугільний басейн
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