Summit accordance

Today we are going to delve into the world of Summit accordance, a topic that has been the subject of interest and debate in different areas over time. Summit accordance has aroused the curiosity and fascination of many people due to its importance in today's society. Throughout history, Summit accordance has played a fundamental role in different contexts, from politics and culture to science and technology. Throughout this article, we will explore the importance of Summit accordance, as well as its impact on society at large. Additionally, we will look at how Summit accordance has evolved over time and how it has influenced our lives in ways we may not have considered before. Get ready to enter the fascinating world of Summit accordance!

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 (sometimes also known by the German loan word gipfelflur) exists when hills and mountaintops, and eventually also plateaux, have such a 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. Other proposed explanations include:

  • 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 also

References

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