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  2. Alleghanian orogeny - Wikipedia

    en.wikipedia.org/wiki/Alleghanian_orogeny

    The Alleghanian orogeny, a result of three separate continental collisions. USGS. The immense region involved in the continental collision, the vast temporal length of the orogeny, and the thickness of the pile of sediments and igneous rocks known to have been involved are evidence that at the peak of the mountain-building process, the Appalachians likely once reached elevations similar to ...

  3. Central Pangean Mountains - Wikipedia

    en.wikipedia.org/wiki/Central_Pangean_Mountains

    Map of Earth during the Early Permian, around 285 million years ago, showing Central Pangean mountain range at equator. The Central Pangean Mountains were formed during the collision of Euramerica and northern Gondwana as part of the Variscan and Alleghanian orogenies, which began during the Carboniferous approximately 340 million years ago, and complete by the beginning of the Permian around ...

  4. List of orogenies - Wikipedia

    en.wikipedia.org/wiki/List_of_orogenies

    Laramide orogeny – Period of mountain building in North America – Rocky Mountains, western North America, (40–70 Ma) ... early Carboniferous Period, ...

  5. Carboniferous - Wikipedia

    en.wikipedia.org/wiki/Carboniferous

    Carboniferous is the period during which both terrestrial animal and land plant life was well established. [10] Stegocephalia (four-limbed vertebrates including true tetrapods), whose forerunners (tetrapodomorphs) had evolved from lobe-finned fish during the preceding Devonian period, became pentadactylous during the Carboniferous. [11]

  6. Variscan orogeny - Wikipedia

    en.wikipedia.org/wiki/Variscan_orogeny

    Location of the Hercynian-Alleghenian mountain belts in the middle of the Carboniferous period.Present day coastlines are indicated in grey for reference. [1]The Variscan orogeny, or Hercynian orogeny, was a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea.

  7. Category:Carboniferous North America - Wikipedia

    en.wikipedia.org/wiki/Category:Carboniferous...

    Carboniferous life of North America (1 C, 2 P) M. Carboniferous Mexico (7 P) Mississippian North America (2 C) P. Pennsylvanian North America (1 C, 7 P) S.

  8. Pennsylvanian (geology) - Wikipedia

    en.wikipedia.org/wiki/Pennsylvanian_(geology)

    In North America, where the early Carboniferous beds are primarily marine limestones, the Pennsylvanian was in the past treated as a full-fledged geologic period between the Mississippian and the Permian. In parts of Europe, the Mississippian and Pennsylvanian are one more-or-less continuous sequence of lowland continental deposits and are ...

  9. Category:Carboniferous United States - Wikipedia

    en.wikipedia.org/wiki/Category:Carboniferous...

    Carboniferous United States: geologic formations of the Carboniferous Period, in Paleozoic Era United States, North America. Subcategories. This category has the ...