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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. Transfer zone - Wikipedia

    en.wikipedia.org/wiki/Transfer_zone

    A few kilometers south of Cairo there are en echelon minor faults between two major faults that produce a relay ramp style transfer zone. In the northern part of the Suez rift system the Gharandal transfer zone accommodates deformation in a broad anticlinal structure between two listric faults in a collateral horst and graben.

  7. Half-graben - Wikipedia

    en.wikipedia.org/wiki/Half-graben

    Lake-filled half-graben showing sedimentation dominantly from the 'hinge' margin. Four zones of sedimentation can be defined in a half-graben. The first is "escarpment margin" sedimentation, found along the major border faults bounding the half graben, where the deepest part of the basin meets the highest rift-shoulder mountains. [6]

  8. Play Hearts Online for Free - AOL.com

    www.aol.com/games/play/masque-publishing/hearts

    Enjoy a classic game of Hearts and watch out for the Queen of Spades!

  9. Anatomy of the human heart - Wikipedia

    en.wikipedia.org/wiki/Anatomy_of_the_human_heart

    The heart is a muscular organ situated in the mediastinum.It consists of four chambers, four valves, two main arteries (the coronary arteries), and the conduction system. The left and right sides of the heart have different functions: the right side receives de-oxygenated blood through the superior and inferior venae cavae and pumps blood to the lungs through the pulmonary artery, and the left ...