caledonian orogeny sentence in Hindi
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- The resulting Caledonian Orogeny produced an Alpine-style mountain range.
- The Caledonian orogeny is named for Caledonia, the Latin name for Scotland.
- The final stages of the Caledonian orogeny involved sinistral strike-slip faulting.
- The Caledonian orogeny did not affect this area.
- Both were created during the creation of the Caledonian orogeny 500 million years ago.
- During the Caledonian orogeny the crater was buried under a several kilometre thick mountain chain.
- The Caledonian orogeny united the northern and southern portions of present-day Great Britain.
- The system was active during the Caledonian Orogeny and was reactivated during the later Variscan Orogeny.
- In western Norway, these gneisses were again deformed during the Caledonian orogeny ca . 400 Ma.
- These rocks were folded when the ancient continents of Laurentia and Avalonia collided during the Caledonian orogeny.
- During the Devonian Period the thickened welt of crust formed by the Caledonian orogeny began to collapse.
- From the late Neoproterozoic Era to Carboniferous Period, Europe underwent the Caledonian Orogeny and Variscan Orogeny.
- The resulting Caledonian Orogeny produced an Alpine-style mountain range in much of north and west Britain.
- The Caledonian ( Iapetus ) plate cycle saw the formation of the Iapetus suture during the Caledonian orogeny.
- The fault occurred in the Caledonian orogeny, during a late stage of this period of mountain building.
- The Caledonian orogeny was one of several orogenies that would eventually form the supercontinent Pangaea in the Late Paleozoic era.
- This part of Scotland largely comprises ancient rocks from the Cambrian and Precambrian, which were uplifted during the later Caledonian Orogeny.
- The Rhenohercynian basin, a back-arc basin, formed at the southern margin of Euramerica just after the Caledonian orogeny.
- They collided in the Caledonian orogeny and formed the Caledonide mountains of North America, Greenland, the British Isles and Norway.
- They were formed during the Caledonian orogeny of the Silurian period and then rejuvenated in the Hercynian orogeny of the Upper Carboniferous period.
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