Fold mountain

mountains formed by compressive crumpling of the layers of rock

Fold mountains are mountains formed mainly by the effects of folding on layers in the upper part of the Earth's crust. The term is rather out of date, though still fairly common in physical geography literature.

Convergence of two continental plates.
Even when mountains are worn down, the evidence is there in the remaining rocks. Millook, Cornwall
Zagros mountain range, seen from space.

In the time before plate tectonics became well understood, the term was used for mountain belts, such as the Himalayas. These mountain ranges are not caused by the folding of the earth's crust. The main mechanism causing a thickening of the crust at these sites of continent-continent collision along boundary is thrust faulting.

Fold mountains are formed when two tectonic plates move together (a convergent plate boundary). Fold mountains are usually formed from sedimentary rocks which accumulated along the margins of continents. When plates and the continents riding on them collide, the accumulated layers of rock may crumple and fold like a tablecloth that is pushed across a table, particularly if there is a mechanically weak basal layer such as salt.[1]


  • The Jura mountains – a series of sub-parallel mountainous ridges formed by folding over a Triassic salt bed due to thrust movements as the Alps pushed into Europe.
  • The 'Simply Folded Belt' of the Zagros mountains in Iran – here both thrusts and folds are occurring. This mountain range, about 1,500 kilometres long, formed only in the past five million years. Oil reserves and huge salt deposits are rising up from the subsurface. They emerge as salt "glaciers". This, and their regular folding, makes these mountains unique in the world.[1]
  • The Akwapim-Togo ranges in Ghana
  • part of the Appalachians in the Eastern United States, known as the "Ridge-and-Valley Appalachians".

Related pagesEdit


  1. 1.0 1.1 Ulmer, S. (11 August 2011). "Fold mountains slip on soft areas". ETH Life. ETH Zürich. Retrieved 21 February 2012.