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  2. Topographic prominence - Wikipedia

    en.wikipedia.org/wiki/Topographic_prominence

    This can be calculated for a given peak in the following manner: for every path connecting the peak to higher terrain, find the lowest point on the path; the key col (or highest saddle, or linking col, or link) is defined as the highest of these points, along all connecting paths; the prominence is the difference between the elevation of the ...

  3. Mountain formation - Wikipedia

    en.wikipedia.org/wiki/Mountain_formation

    Mountain formation occurs due to a variety of geological processes associated with large-scale movements of the Earth's crust (tectonic plates). [1] Folding , faulting , volcanic activity , igneous intrusion and metamorphism can all be parts of the orogenic process of mountain building. [ 2 ]

  4. Geomorphometry - Wikipedia

    en.wikipedia.org/wiki/Geomorphometry

    In simple terms, geomorphometry aims at extracting (land) surface parameters (morphometric, hydrological, climatic, etc.) and objects (watersheds, stream networks, landforms, etc.) using input digital land surface model (also known as digital elevation model, DEM) and parameterization software. [3]

  5. Altitudinal zonation - Wikipedia

    en.wikipedia.org/wiki/Altitudinal_zonation

    Decreasing air temperature usually coincides with increasing elevation, which directly influences the length the growing season at different elevations of the mountain. [ 2 ] [ 7 ] For mountains located in deserts, extreme high temperatures also limit the ability of large deciduous or coniferous trees to grow near the base of mountains. [ 8 ]

  6. Isostasy - Wikipedia

    en.wikipedia.org/wiki/Isostasy

    The basis of the model is Pascal's law, and particularly its consequence that, within a fluid in static equilibrium, the hydrostatic pressure is the same on every point at the same elevation (surface of hydrostatic compensation): [3] [8] h 1 ⋅ρ 1 = h 2 ⋅ρ 2 = h 3 ⋅ρ 3 = ... h n ⋅ρ n

  7. Topographic isolation - Wikipedia

    en.wikipedia.org/wiki/Topographic_isolation

    The topographic isolation of a summit is the minimum distance to a point of equal elevation, representing a radius of dominance in which the peak is the highest point. It can be calculated for small hills and islands as well as for major mountain peaks and can even be calculated for submarine summits.

  8. Massenerhebung effect - Wikipedia

    en.wikipedia.org/wiki/Massenerhebung_effect

    The Massenerhebung effect (German for "mountain mass elevation") describes variation in the tree line based on mountain size and location. In general, mountains surrounded by large ranges will tend to have higher tree lines than more isolated mountains due to heat retention and wind shadowing. This effect is important for determining weather ...

  9. Elevation - Wikipedia

    en.wikipedia.org/wiki/Elevation

    In aviation, the term elevation or aerodrome elevation is defined by the ICAO as the highest point of the landing area. It is often measured in feet and can be found in approach charts of the aerodrome. It is not to be confused with terms such as the altitude or height. [1] Part of a topographic map of Haleakala , showing elevation.