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  2. Horst and graben - Wikipedia

    en.wikipedia.org/wiki/Horst_and_graben

    Diagram of horsts and grabens In geology , horst and graben (or range and valley ) refers to topography consisting of alternating raised and lowered fault blocks known as horsts and grabens . The features are created by normal faulting and rifting caused by crustal extension . [ 1 ]

  3. Strike and dip - Wikipedia

    en.wikipedia.org/wiki/Strike_and_dip

    Strike and dip are generally written as 'strike/dip' or 'dip direction,dip', with the degree symbol typically omitted. The general alphabetical dip direction (N, SE, etc) can be added to reduce ambiguity. For a feature with a dip of 45° and a dip direction of 75°, the strike and dip can be written as 345/45 NE, 165/45 NE, or 075,45.

  4. Transverse Valleys - Wikipedia

    en.wikipedia.org/wiki/Transverse_Valleys

    The Transverse Valleys (Spanish: Valles transversales) are a group of transverse valleys in the semi-arid northern Chile. They run from east to west (traversing Chile), being among the most prominent geographical features in the regions they cross. [1] They are located in the Chilean regions of Valparaíso, Coquimbo, and Atacama.

  5. Franciscan Complex - Wikipedia

    en.wikipedia.org/wiki/Franciscan_Complex

    Diagram (modified from Fig 3.11 in Irwin, 1990) showing the depositional setting of the Franciscan Assemblage and the contemporaneous Great Valley Sequence,. [ 5 ] The Franciscan Complex is an assemblage of metamorphosed and deformed rocks, associated with east-dipping subduction zone at the western coast of North America. [ 6 ]

  6. Drainage system (geomorphology) - Wikipedia

    en.wikipedia.org/wiki/Drainage_system...

    Dendritic drainage: the Yarlung Tsangpo River, Tibet, seen from space: snow cover has melted in the valley system. In geomorphology, drainage systems, also known as river systems, are the patterns formed by the streams, rivers, and lakes in a particular drainage basin. They are governed by the topography of land, whether a particular region is ...

  7. Pull-apart basin - Wikipedia

    en.wikipedia.org/wiki/Pull-apart_basin

    In geology, a basin is a region where subsidence generates accommodation space for the deposition of sediments. A pull-apart basin is a structural basin where two overlapping (en echelon) strike-slip faults or a fault bend create an area of crustal extension undergoing tension, which causes the basin to sink down.

  8. “The Year Without a Santa Claus” Turns 50: How Heat ... - AOL

    www.aol.com/without-santa-claus-turns-50...

    The Year Without a Santa Claus, a Christmas special from Jules Bass and Arthur Rankin, Jr., turns 50 this December. The beloved special was adapted from the book of the same name by Phyllis ...

  9. Graben - Wikipedia

    en.wikipedia.org/wiki/Graben

    Diagram illustrating the structural relationship between grabens and horsts Infrared-enhanced satellite image of a graben in the Afar Depression. In geology, a graben (/ ˈ ɡ r ɑː b ən /) is a depressed block of the crust of a planet or moon, bordered by parallel normal faults.