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Geological Formation

Hill chain

Structural and Tectonic Formations

A hill chain, sometimes called a hill ridge, is an elongated line of hills made up of a succession of more or less prominent hilltops, domed summits, hill ridges and saddles, together with associated lateral ridges and branches that can form a complex topographic structure. It can occur within a larger hill range, within an area of low rolling hill country, or on a plain, and it can link two or more otherwise separate hill ranges. The line between a hill chain and a mountain chain is not sharp and depends on how a given region defines a hill or a mountain.

Connections

Caused By

Glaciation, Processes
Source Hill chain (Wikipedia)
Orogeny, Processes
Source Hill chain (Wikipedia)

In Discipline

Source Hill chain (Wikipedia)
Sources
Hill chain (Wikipedia)
  • In Discipline: Geomorphology, Lead paragraph
    A hill chain, sometimes also hill ridge, is an elongated line of hills that usually includes a succession of more or less prominent hilltops, domed summits or kuppen, hill ridges and saddles and which, together with its associated lateral ridges and branches, may form a complex topographic structure
  • Caused By: Orogeny, Lead sentence
    The chain-like arrangement of hills in a chain is a consequence of their collective formation by mountain building forces or ice age earth movements.
  • Caused By: Glaciation, Lead sentence
    The chain-like arrangement of hills in a chain is a consequence of their collective formation by mountain building forces or ice age earth movements.
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