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  2. The Elder Scrolls II: Daggerfall - Wikipedia

    en.wikipedia.org/wiki/The_Elder_Scrolls_II:...

    The Elder Scrolls II: Daggerfall is an open-world, action role-playing game published by Bethesda Softworks.The second video game in the Elder Scrolls series, it was released on September 20, 1996 for MS-DOS, following the success of 1994's The Elder Scrolls: Arena.

  3. List of The Elder Scrolls video games - Wikipedia

    en.wikipedia.org/wiki/List_of_The_Elder_Scrolls...

    The Elder Scrolls games take place in the fictional world of Nirn, on the continent of Tamriel. The first game, The Elder Scrolls: Arena , was released in 1994. It was intended for players to assume the role of an arena combatant, but development shifted the game into a role-playing game (RPG), beginning a tradition that persists throughout the ...

  4. 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 ...

  5. Mountain formation - Wikipedia

    en.wikipedia.org/wiki/Mountain_formation

    Zard-Kuh, a fold mountain in the central Zagros range of Iran. When plates collide or undergo subduction (that is, ride one over another), the plates tend to buckle and fold, forming mountains. While volcanic arcs form at oceanic-continental plate boundaries, folding occurs at continental-continental plate boundaries.

  6. Mountain - Wikipedia

    en.wikipedia.org/wiki/Mountain

    Mount Everest, Earth's highest mountain. A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock.Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (980 ft) above the surrounding land.

  7. Geology of the Appalachians - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_Appalachians

    As Pangea rifted apart a new passive tectonic margin was born, and the forces that created the Appalachian, Ouachita, and Marathon Mountains were stilled. Weathering and erosion prevailed, and the mountains began to wear away. [10] By the end of the Mesozoic, the Appalachian Mountains had been eroded to an almost-flat plain. [10]

  8. See photos of the real 1972 Andes plane crash that inspired ...

    www.aol.com/news/see-photos-real-1972-andes...

    "Society of the Snow" is earning raves for its a ccurate depiction of the terrifying 1972 plane crash in the Andes mountains that involved a Uruguayan rugby team.. The new Netflix drama, directed ...

  9. Lewis Overthrust - Wikipedia

    en.wikipedia.org/wiki/Lewis_Overthrust

    The Canadian Rocky Mountain foreland thrust and fold belt is a northeastward tapering deformational belt consisting of Mesoproterozoic, Paleozoic, and Mesozoic strata. The Lewis thrust sheet is one of the major structures of the foreland thrust and fold belt extending over 280 mi (450 km) from Mount Kidd near Calgary, AB in the Southeast Canadian Cordillera to Steamboat Mountain, located west ...