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  2. Fold mountains - Wikipedia

    en.wikipedia.org/wiki/Fold_mountains

    Fold mountains form in areas of thrust tectonics, such as where two tectonic plates move towards each other at convergent plate boundary.When plates and the continents riding on them collide or undergo subduction (that is – ride one over another), the accumulated layers of rock may crumple and fold like a tablecloth that is pushed across a table, particularly if there is a mechanically weak ...

  3. Mountain formation - Wikipedia

    en.wikipedia.org/wiki/Mountain_formation

    Mountain formation refers to the geological processes that underlie the formation of mountains. These processes are associated with large-scale movements of the Earth's crust (tectonic plates). [1] Folding, faulting, volcanic activity, igneous intrusion and metamorphism can all be parts of the orogenic process of mountain building. [2]

  4. Fold (geology) - Wikipedia

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

    These folds were produced by Alpine deformation. In structural geology, a fold is a stack of originally planar surfaces, such as sedimentary strata, that are bent or curved ("folded") during permanent deformation. Folds in rocks vary in size from microscopic crinkles to mountain-sized folds. They occur as single isolated folds or in periodic ...

  5. Fold and thrust belt - Wikipedia

    en.wikipedia.org/wiki/Fold_and_thrust_belt

    A fold and thrust belt (FTB) is a series of mountainous foothills adjacent to an orogenic belt, which forms due to contractional tectonics. Fold and thrust belts commonly form in the forelands adjacent to major orogens as deformation propagates outwards. Fold and thrust belts usually comprise both folds and thrust faults, commonly interrelated.

  6. Geology of the Western Carpathians - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Western...

    The Western Carpathians are an arc -shaped mountain range, the northern branch of the Alpine - Himalayan fold and thrust system called the Alpide belt, which evolved during the Alpine orogeny. In particular, their pre- Cenozoic evolution is very similar to that of the Eastern Alps, and they constitute a transition between the Eastern Alps and ...

  7. Mountain - Wikipedia

    en.wikipedia.org/wiki/Mountain

    Mont Blanc in Aosta Valley, Italy, the highest point in the European Union. There is no universally accepted definition of a mountain. Elevation, volume, relief, steepness, spacing and continuity have been used as criteria for defining a mountain. [5] In the Oxford English Dictionary a mountain is defined as "a natural elevation of the earth ...

  8. Glossary of geology - Wikipedia

    en.wikipedia.org/wiki/Glossary_of_geology

    Also called Indianite. A mineral from the lime-rich end of the plagioclase group of minerals. Anorthites are usually silicates of calcium and aluminium occurring in some basic igneous rocks, typically those produced by the contact metamorphism of impure calcareous sediments. anticline An arched fold in which the layers usually dip away from the fold axis. Contrast syncline. aphanic Having the ...

  9. Alpine orogeny - Wikipedia

    en.wikipedia.org/wiki/Alpine_orogeny

    Alpine orogeny. Tectonic map of southern Europe and the Middle East, showing tectonic structures of the western Alpide mountain belt. The Alpine orogeny or Alpide orogeny[dubious – discuss] is an orogenic phase in the Late Mesozoic [1] (Eoalpine) and the current Cenozoic that has formed the mountain ranges of the Alpide belt.