it is compression
Folding is usually the result of compressional stress, where rocks are squeezed together and deform due to tectonic forces. This can lead to the bending or curving of rock layers.
Sand squeezed together, and aged, can make a pearl.
The main types of stress acting on rocks in Death Valley are compressional stress, where rocks are being squeezed together, and shear stress, where rocks are being pushed in opposite directions horizontally. These stresses can lead to the formation of faults and fractures in the rocks.
Fold mountains.
The dominant type of stress associated with folded mountains is compressional stress caused by tectonic plate collision. As plates converge, the rocks are squeezed and folded, leading to the formation of folded mountain ranges such as the Himalayas and the Appalachians.
Compression stress pushes rock in the opposite direction, causing it to be squeezed and compacted. This type of stress often leads to the folding and faulting of rocks as they respond to the pressure by deforming and moving.
a type of rock formed by layers of sediments that were squeezed and stuck together over a long time
Tensile stress occurs when members are pulled apart, causing tension within the material. This type of stress occurs when forces act to stretch or elongate the material, potentially leading to deformation or fracture.
The type of rocks formed when rock fragments are squeezed together is called sedimentary rocks. These rocks are created through a process known as compaction, where accumulated sediments, such as sand, silt, and clay, are pressed together under pressure over time. Examples of sedimentary rocks include sandstone, shale, and conglomerate.
its the circulation of the rock and when it pushes together
Folded mountains are formed when the Earth's crust is squeezed together. This process causes the rock layers to fold and buckle, creating prominent ridges and peaks. The Appalachian Mountains in the eastern United States are an example of folded mountains.
It depends on the type of plates coming together but two continental plates will form a mountain chain. An example would be the Indian sub-continent colliding with Asia to form the Himalayas.