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  2. Tilted block faulting - Wikipedia

    en.wikipedia.org/wiki/Tilted_block_faulting

    Tilted block faulting, also called rotational block faulting, is a mode of structural evolution in extensional tectonic events, a result of tectonic plates stretching apart. [ 1 ] [ 2 ] When the upper lithospheric crust experiences extensional pressures, the brittle crust fractures, creating detachment faults . [ 3 ]

  3. Horst and graben - Wikipedia

    en.wikipedia.org/wiki/Horst_and_graben

    The Basin and Range Province in the western United States is an extensive region of alternating valleys and ridges caused by horst and graben as well as tilted block faulting. [ 1 ] The Condroz and Ardennes regions of Wallonia are good examples of a succession of horst and graben.

  4. Basin and range topography - Wikipedia

    en.wikipedia.org/wiki/Basin_and_range_topography

    Tilted block faulting, also known as half-graben or rotational block faulting, can also occur during extension. Large gently dipping normal faults, also known as detachment faults, act as platforms in which normal faulted blocks tilt or slide along. However, instead of the whole block subsiding only one side, the block may slip along the ...

  5. Tilted Towers - Wikipedia

    en.wikipedia.org/wiki/Tilted_Towers

    Tilted Towers was a small city location in Fortnite: Battle Royale, [1] [2] and a current location in Fortnite Reload. [3] Located near the center of the map, the city is composed of several large skyscrapers with cramped interiors, each consisting of several stories, [1] [2] the tallest of which is a large clock tower. [4]

  6. Extensional tectonics - Wikipedia

    en.wikipedia.org/wiki/Extensional_tectonics

    They range in width from somewhat less than 100 km up to several hundred km, consisting of one or more normal faults and related fault blocks. [2] In individual rift segments, one polarity (i.e. dip direction) normally dominates, giving a half-graben geometry. [6] Other common geometries include metamorphic core complexes and tilted blocks.

  7. Fault block - Wikipedia

    en.wikipedia.org/wiki/Fault_block

    Lifted fault-block geology Tilted fault-block formation in the Teton Range. Fault-block mountains often result from rifting, an indicator of extensional tectonics. These can be small or form extensive rift valley systems, such as the East African Rift zone. Death Valley in California is a smaller example.

  8. List of fault zones - Wikipedia

    en.wikipedia.org/wiki/List_of_fault_zones

    This list covers all faults and fault-systems that are either geologically important [clarification needed] or connected to prominent seismic activity. [clarification needed] It is not intended to list every notable fault, but only major fault zones. [clarification needed

  9. Mountain formation - Wikipedia

    en.wikipedia.org/wiki/Mountain_formation

    When a fault block is raised or tilted, a block mountain can result. [17] Higher blocks are called horsts, and troughs are called grabens. A spreading apart of the surface causes tensional forces. When the tensional forces are strong enough to cause a plate to split apart, it does so such that a center block drops down relative to its flanking ...