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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. 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.

  4. Lexington Limestone - Wikipedia

    en.wikipedia.org/wiki/Lexington_Limestone

    These sandbars are today preserved as the Tanglewood Member - a complex formation of well-sorted limestone that makes up the bulk of the Lexington Limestone in the inner Bluegrass region. Most of the debris that makes up the Tanglewood member represents the broken and abraded fragments of locally abundant calcified animals, mainly crinoids ...

  5. 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.

  6. 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] This is often caused by extensional forces pulling apart the crust.

  7. National Register of Historic Places listings in Kentucky

    en.wikipedia.org/wiki/National_Register_of...

    This is a list of properties and historic districts in Kentucky that are listed on the National Register of Historic Places. There are listings in all of Kentucky's 120 counties . The locations of National Register properties and districts (at least for all showing latitude and longitude coordinates below), may be seen in an online map by ...

  8. Volunteers and city workers try to reconnect the water supply to a nursing home in Elkhorn City, Ky., on Friday, July 29, 2022. The pipe, along with some of KY-197, washed away yesterday when the ...

  9. Geology of Kentucky - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Kentucky

    The geology of Kentucky formed beginning more than one billion years ago, in the Proterozoic eon of the Precambrian. The oldest igneous and metamorphic crystalline basement rock is part of the Grenville Province, a small continent that collided with the early North American continent.