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horst    音标拼音: [h'ɔrst]

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  • Horst (geology) - Wikipedia
    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
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  • Horst and graben | Faulting, Tectonics Geomorphology | Britannica
    horst and graben, elongate fault blocks of the Earth’s crust that have been raised and lowered, respectively, relative to their surrounding areas as a direct effect of faulting Horsts and grabens may range in size from blocks a few centimetres wide to tens of kilometres wide; the vertical movement may be up to several thousand feet
  • Horst Welding | Family of Companies
    Farm equipment manufacturing has always been, and will continue to be the main focus of Horst Welding The product lineup consists of snow blades, snow pushers, snow wings, loader attachments, header wagons, and running gear
  • HORST Definition Meaning - Merriam-Webster
    The meaning of HORST is a block of the earth's crust separated by faults from adjacent relatively depressed blocks
  • Horst - definition of horst by The Free Dictionary
    Define horst horst synonyms, horst pronunciation, horst translation, English dictionary definition of horst horst n A mass of the earth's crust that lies between two faults and is higher than the surrounding land
  • What does Horst mean? - Definitions. net
    A horst is a raised geological formation, such as a mountain range, that has been created by the movement of tectonic plates in the earth's crust It is typically formed between two parallel faults or fractures in the earth's surface and is elevated relative to the surrounding landscape
  • Horst Structures: Definition Geology | Vaia
    Horst structures are elevated blocks of the Earth's crust, formed between two parallel fault lines, rising above the surrounding terrain (grabens) Characteristics include parallel fault lines, uplifted central block, and patterns of ridges and valleys
  • horst - Encyclopedia of World Geography
    A horst is left standing either by sinking of the crust on either side of a pair of normal faults or by physical lifting of a crustal block between the faults Geomorphologists often use the German word graben (which means “trench” or “grave”) for the low-lying block between two horsts
  • Horst and graben - Wikipedia
    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]





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