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The highest of hills in this picture show fairly similar heights making up a summit accordance. Aerial photograph from the Altai region of Russia.

A summit accordance exists when hill and mountaintops tops, and eventually also plateaux, have such disposition that they form a geometric plane that may be either horizontal or tilted. Summit accordances can be the vestiges of former continuous erosion surfaces that were uplifted and eroded.[1] Other proposed explanations include:[2]

  • the possibility that erosion becomes more effective at height, tearing down mountains that stand out
  • that isostasy regulates the height of individual mountain masses meaning that small mountains might be uplifted and large mountains dragged down
  • that landscape dissection by uniformly spaced streams eventually reach a state in which summits attain similar heights
  • that summit accordance is derivative of structural planes exposed by erosion

See alsoEdit

ReferencesEdit

  1. ^ Lidmar-Bergström, Karna. "Toppkonstans". Nationalencyklopedin (in Swedish). Cydonia Development. Retrieved June 22, 2015.
  2. ^ Beckinsale, Robert P.; Chorley, Richard J. (2003) [1991]. "Chapter Seven: American Polycyclic Geomorphology". The History of the Study of Landforms. Volume Three. Taylor & Francis e-Library. pp. 235–236.