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  2. Horst and graben - Wikipedia

    en.wikipedia.org/wiki/Horst_and_graben

    A graben is a section of crust that has lowered relative to the blocks on either side, which is a result of its bounding faults dipping towards each other. [2] The plural of graben can be either graben or grabens. Graben form low-lying features such as basins and rift valleys. [1] [2] They can be very long relative to their width.

  3. Graben - Wikipedia

    en.wikipedia.org/wiki/Graben

    Graben often occur side by side with horsts. Horst and graben structures indicate tensional forces and crustal stretching. Graben are produced from parallel normal faults, where the displacement of the hanging wall is downward, while that of the footwall is upward. The faults typically dip toward the center of the graben from both sides.

  4. Horst (geology) - Wikipedia

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

    In physical geography and geology, a horst is a raised fault block bounded by normal faults. [1] Horsts are typically found together with grabens . While a horst is lifted or remains stationary, the grabens on either side subside . [ 2 ]

  5. Basin and range topography - Wikipedia

    en.wikipedia.org/wiki/Basin_and_range_topography

    With crustal extension, a series of normal faults which occur in groups, form in close proximity and dipping in opposite directions. [4] As the crust extends it fractures in series of fault planes, some blocks sink down due to gravity, creating long linear valleys or basins also known as grabens, while the blocks remaining up or uplifted produce mountains or ranges, also known as horsts.

  6. Fault (geology) - Wikipedia

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

    A downthrown block between two normal faults dipping towards each other is a graben. A block stranded between two grabens, and therefore two normal faults dipping away from each other, is a horst. A sequence of grabens and horsts on the surface of the Earth produces a characteristic basin and range topography.

  7. Fault block - Wikipedia

    en.wikipedia.org/wiki/Fault_block

    Lifted type block mountains have two steep sides exposing both sides scarps, leading to the horst and graben terrain seen in various parts of Europe including the Upper Rhine valley, a graben between two horsts – the Vosges mountains (in France) and the Black Forest (in Germany), and also the Rila – Rhodope Massif in Bulgaria, Southeast ...

  8. ESPN's Kirk Herbstreit: Indiana 'was not a team that should ...

    www.aol.com/sports/espns-kirk-herbstreit-indiana...

    Indiana may not have been one of the very best teams in college football, but a team that goes 11-1 in a power conference was always going to be a foregone conclusion to make the 12-team College ...

  9. File:Fault-Horst-Graben.svg - Wikipedia

    en.wikipedia.org/wiki/File:Fault-Horst-Graben.svg

    English: geological structure of Horst and graben. Français : Structure géologique des horst et graben . Svenska: Geologisk skiss över horstar och gravsänkor.