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  2. Window (geology) - Wikipedia

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

    A tectonic window, or fenster (lit. "window" in German), is a geologic structure formed by erosion or normal faulting on a thrust system. In such a system the rock mass ( hanging wall block ) that has been transported by movement along the thrust is called a nappe .

  3. The Window (1949 film) - Wikipedia

    en.wikipedia.org/wiki/The_Window_(1949_film)

    The Window presents a frightening vision of helplessness, vividly conveying childish frustration at being dismissed or ignored by one's parents. Director and onetime cameraman Tetzlaff adroitly injects a maximum of suspense into the film, enabling the audience to identify with Driscoll's predicament and to view his parents as evil, almost as ...

  4. Nappe - Wikipedia

    en.wikipedia.org/wiki/Nappe

    The shaded material is the nappe. The erosional hole is called a window or fenster. The klippe is the isolated block of the nappe overlying autochthonous material. In geology, a nappe or thrust sheet is a large sheetlike body of rock that has been moved more than 2 km (1.2 mi) [1] or 5 km (3.1 mi) [2] [3] above a thrust fault from

  5. Hohe Tauern window - Wikipedia

    en.wikipedia.org/wiki/Hohe_Tauern_window

    The Tauern Window is a geological structure in the Austrian Central Eastern Alps. It is a window (in German fenster) in the Austroalpine nappes where high-grade metamorphic rocks of the underlying Penninic nappes crop out. The structure is caused by a large dome-like antiform in the nappe stacks of the Alps.

  6. Klippe - Wikipedia

    en.wikipedia.org/wiki/Klippe

    The erosional hole is called a window or fenster. The klippe is the isolated block of the nappe overlying autochthonous material. A klippe (German for cliff or crag) is a geological feature of thrust fault terrains. The klippe is the remnant portion of a nappe after erosion has removed connecting portions of the nappe.

  7. Monument Valley - Wikipedia

    en.wikipedia.org/wiki/Monument_Valley

    View of Monument Valley in Utah, looking south on U.S. Route 163 from 13 miles (21 km) north of the Utah–Arizona state line Mitchell Mesa from the View Hotel.. Monument Valley (Navajo: Tsé Biiʼ Ndzisgaii, pronounced [tsʰépìːʔ ǹtsɪ̀skɑ̀ìː], meaning "valley of the rocks") is a region of the Colorado Plateau characterized by a cluster of sandstone buttes, with the largest reaching ...

  8. Olympus Geological History Museum - Wikipedia

    en.wikipedia.org/wiki/Olympus_Geological_History...

    The Olymp is a so-called tectonic window. [2] This means that erosion and warping have released old rock layers that would normally be hidden. This fact ensures that geologists from all over the world travel to Olympus for research purposes. Further panels explain that Mount Olympus got its present form after the Würm ice age. As the ice ...

  9. Karst window - Wikipedia

    en.wikipedia.org/wiki/Karst_window

    A karst window, also known as a karst fenster, is a geomorphic feature found in karst landscapes where an underground river is visible from the surface within a sinkhole. [ 1 ] [ 2 ] In this feature, a spring emerges, then the discharge abruptly disappears into a sinkhole .