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Orogeny is the formation of mountains through structural disturbance, especially by folding and faulting.
In agricultural societies, for example, myths have been collected that ascribe the unevenness of land or the formation of mountains to an ancient mishap or evil force.
For example, he raised questions about the formation of mountains and explained the existence there of fossils by positing that Earth was once underwater.
Despite Wegener's inability to explain the physical processes that may have caused the drift of these large land masses, the author proposed that the formation of mountains, via compressive forces, the occurrence of earthquakes, and volcanism are consequences of continental drift [ 59].
According to the "tree-like" synade-model of macroevolution proposed here, all extant and extinct organisms have, through the eons of geological time, benefited from the dynamic Earth due to the creation of early terrestrial land masses within giant marine habitats, and the subsequent formation of mountains, deserts, freshwater ecosystems, and deep oceans [ 64, 75].
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Of particular relevance to the story of primate evolution are the vegetational changes resulting from the formation of mountain ranges.
Occasionally, petroleum deposits elevated during the formation of mountain ranges have been exposed by erosion to form tar deposits.
Forces such as continental drift, the submerging of ocean floors, and the formation of mountain ranges have acted within the time frame of evolutionary history to create natural barriers between species where at previous times there were none.
Many have naturally perished due to necessity of constitution, in the time interval passed from the formation of large mountains to that of small reliefs, as others have perished in the epoch when actual continents made their appearance up to the one we live in; and like others, still will finally perish in the future and what we know will be sought in vain by our descendants.
The formation of high mountains separated by deep valleys will have reduced gene flow between Cupressus populations that were diverging into different species in different valleys and hastened the fixation of locally specific haplotypes.
Another important consequence of continued plate movement has been the formation of large mountain ranges at the sites of plate collision.
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