The Central Pangean Mountains were an extensive northeast–southwest trending mountain range in the central portion of the supercontinent Pangaea during the Carboniferous, Permian and Triassic periods. They were formed as a result of collision between the large landmasses of Euramerica (also known as Laurussia) and Gondwana during the formation of Pangaea. At its greatest elevation during the early part of the Permian period, it was comparable to the present Himalayas. Remnants of this massive mountain range include the Appalachian Mountains and Ouachita Mountains of North America as well as the Bohemian Massif and Massif Central in Europe.
A number of mountain building periods were involved in the formation of the Central Pangean Mountains, including the Acadian, Caledonian, Alleghenian, Mauritanide and Variscan orogenies.
The eastern portions of the range are also called the Variscan Mountains.[1]
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and 28 Related for: Central Pangean Mountains information
The CentralPangeanMountains were an extensive northeast–southwest trending mountain range in the central portion of the supercontinent Pangaea during...
pressure varies by 36 millibars on average throughout the year. The CentralPangeanMountains potentially played a similar role in the megamonsoon as the Tibetan...
formed part of the same mountain chain as the Little Atlas in Morocco. This mountain range, known as the CentralPangeanMountains, extended into Scotland...
factors with increased weathering of the growing CentralPangeanMountains and the influence of the mountains on precipitation and surface water flow. Closure...
part of the larger CentralPangeanMountains along with the Scottish Highlands, the Ouachita Mountains, and the Anti-Atlas Mountains. The modern ranges...
suggests that the CentralPangeanMountains contributed to the deposition of vast quantities of coal in the late Carboniferous. The mountains created an area...
Germany and Poland. The Zechstein Sea lay in the rain shadow of the CentralPangeanMountains to the south. At times the Zechstein Sea may have connected with...
Pangaea. The resulting Alleghanian orogeny created the CentralPangeanMountains. The mountains were located close to the equator and produced a year-round...
Europe; these are now believed to have formed a single chain, the CentralPangeanMountains. Fossil evidence for Pangaea includes the presence of similar...
Panthalassa subducted under the southeastern South China. The CentralPangeanMountains, which began forming due to the collision of Laurasia and Gondwana...
the Anti-Atlas range in North Africa are parts of the ancient CentralPangeanMountains, made when minor supercontinents collided to form the supercontinent...
the sedimentary basin of the Congo River. The Congo Basin is located in Central Africa, in a region known as west equatorial Africa. The Congo Basin region...
faults Fold mountains – Mountains formed by compressive crumpling of the layers of rock Guyot – Isolated, flat-topped underwater volcano mountain List of...
Triassic, it diverged into two vicariant lineages separated by the CentralPangeanMountains: A. atlantis in the east, and A. dorotheae & the Cumnock species...
sedimentary basin, separated by divides formed by fault blocks, plateaus and mountain ranges, where rock waste eroded from higher surfaces has been deposited...
During the Triassic the Mauritanide Belt was split from the Appalachian Mountains (with which it was previously a single orogen) as the Atlantic Ocean opened...
WSW-ENE faults trends are found in the northeast of the basin near the Aïr Mountains. The sediments from Cambrian to Pleistocene times are 1,500 to 2,000 metres...
Nile rift, Melut Basin and Muglad Basin all terminate on the line of the Central African Shear Zone, a major strike-slip shear zone. It is now known that...
during the breakup of the Pangean supercontinent. The province has been described as extending within Pangaea from present-day central Brazil northeastward...
deposited in the central Transantarctic Mountains, whereas the carbonate rock in the same periods was deposited in the Pensacola Mountains. Due to destructive...
discontinuous series of mountain ranges with distinct geological origins. The rocks making up the mountains were formed before the mountains were raised. The...