Fold (geology)
Rock often deforms in such a way that it bends instead of breaking. This is called a fold. The term fold is used in geology when one or a stack of originally flat, level surfaces, such as sedimentary strata, are bent or curved as a result of pressure and high temperature. The basic cause is likely to be some aspect of plate tectonics.
When two forces act towards each other from opposite sides, rock layers are bent into folds. How folds are formed due to compression is known as folding. Folding is one of the endogenetic processes; it takes place within the Earth's crust.
Folds in rocks vary in size from microscopic crinkles to mountain-sized folds. They occur singly as isolated folds and in extensive fold trains of different sizes, on a variety of scales. A set of folds distributed on a regional scale constitutes a fold belt, a common feature of orogenic zones.
There are large-scale and small-scale folds. Large-scale folds are found mainly along a collision boundary between two tectonic plates.
Structure of a fold
The upfold is called an anticline. The downfold is called a syncline.
The imaginary line joining the highest points along the upfold is called the crest line.
The flanks of a fold are known as the limbs.
The central line from which the rock strata dip away in opposing directions is called the axis of fold.
According to the degree of folding of the layers, folds can be classified into five main types.
- symmetrical fold: two limbs are of equal steepness
- Asymmetrical fold: one limb is steeper than the other
- Overfold: one limb is pushed over the other
- Recumbent fold: two limbs are nearly parallel
- Overthrust fold: compressional force is so great that the rock strata are broken and slide over the other.
Formation of a fold mountain
Large depressions called geosynclines form between plates. Seas filled the geosynclines and rivers flowing into them carried sediments (sand and silt) which build up on the sea bed. Over millions of years the sediments were compressed, by their own weight, into sedimentary rocks, e.g. sandstone, limestone etc.
Landforms formed by folding
Large-scale folding will develop parallel ranges of round-top mountains along destructive plate boundaries. These mountains are known as fold mountains.
Examples of fold mountain ranges:
Fold (geology) Media
Folds of alternate layers of limestone and chert occur in Greece. The limestone and chert were originally deposited as flat layers on the floor of a deep sea basin. These folds were produced by Alpine deformation.
Kink band folds in the Permian of New Mexico, USA
Rainbow Basin syncline in the Barstow Formation near Barstow, California
Fold description 3D model
Flank and hinge of geological fold
Folds observed during the Girls into Geoscience inaugural Irish Fieldtrip
Fold description based on interlimb angles
Ramsay classification of folds by convergence of dip isogons (red lines).
An anticline in New Jersey
A monocline at Colorado National Monument
