compression and tension are opposite. compression pushes the crust together but tension pulls it apart
the 3 kinds of stress are compression,tension, and shearing
yes tension pulls the rocks apart which produces expanding faultscompression pushes the rocks together which produces crushing faultsshear slides the rocks past each other which produces slipping faults
The Earth's crust can fold and crack due to tectonic forces, such as compression and tension along plate boundaries. Compression causes rocks to fold, creating mountain ranges, while tension leads to the formation of faults and fractures, resulting in earthquakes. Other factors such as volcanic activity, erosion, and gravitational forces can also contribute to the folding and cracking of the Earth's crust.
A fault-block mountain is typically formed by tensional forces where blocks of the Earth's crust move vertically due to normal faults. These mountains result from the crust being pulled apart, leading to the uplift of fault blocks.
The major cause of deformation of the Earth's crust is tectonic plate movement. Plates can collide, pull apart, or slide past each other, leading to compression, tension, or shear forces that deform the crust. These interactions result in features such as mountains, rift valleys, and earthquakes.
Compression and tension can indeed affect the thickness of the Earth's crust. Compression can thicken the crust by folding and faulting, while tension can cause stretching and thinning of the crust through processes like rifting and faulting. These tectonic forces play a significant role in shaping the Earth's crust over geological time scales.
Tension, Compresion, and Shear :)
the 3 kinds of stress are compression,tension, and shearing
I think its thickness that's wat i put on my hw
Compression Stress Tension Stress Shearing Stress
yes tension pulls the rocks apart which produces expanding faultscompression pushes the rocks together which produces crushing faultsshear slides the rocks past each other which produces slipping faults
The primary forces that act on rocks in Earth's crust are compression and tension. Compression occurs when rocks are squeezed together, often leading to folding and faulting. Tension is when rocks are pulled apart, creating fractures and rifts. These forces are generated by tectonic plate movements and can result in various geological features.
Shearing, tension, and compression work over millions of years to change the shape and volume of rock. Those are types of stress.
Shearing, tension, and compression work over millions of years to change the shape and volume of rock. Those are types of stress.
The Earth's crust can fold and crack due to tectonic forces, such as compression and tension along plate boundaries. Compression causes rocks to fold, creating mountain ranges, while tension leads to the formation of faults and fractures, resulting in earthquakes. Other factors such as volcanic activity, erosion, and gravitational forces can also contribute to the folding and cracking of the Earth's crust.
Compression occurs when rocks are pushed together, causing them to fold or fault. Tension is when rocks are pulled apart, leading to rift valleys or normal faults. Shearing is when rocks slide past each other horizontally, resulting in strike-slip faults.
faulting