Usually occurs at plate boundary collision areas.
The type of stress that will squeeze and shorten a rock body is known as compressional stress. This stress occurs when forces are applied towards each other, resulting in the rock's volume decreasing and causing it to deform. Compressional stress is commonly associated with tectonic plate convergence, leading to the formation of mountain ranges and various geological structures.
Tensional stress.
Tensional stress.
The type of stress developed at a convergent boundary is Compressional Stress.
Tensional stress pulls crust apart and stretches rock, causing it to deform and eventually break along fault lines. This type of stress commonly occurs at divergent plate boundaries where tectonic plates are moving away from each other.
Pacific plate is a oceanic plate. Mostly basaltic rock with a sedimentary rock layer on top.
Tensional stress causes rocks to pull apart. This type of stress occurs when rocks are being pulled in opposite directions, leading to the stretching and extension of the rock mass. Over time, this can lead to the formation of faults and fractures in the rocks.
The type of stress that causes rocks to pull apart is a tension stress. It is the major type of stress found in divergent plate boundaries.
diamonds
The major type of stress that occurs at convergent plate boundaries is compressional stress. This stress arises as tectonic plates move toward each other, leading to the subduction of one plate beneath another or the collision of two continental plates. The result can be the formation of mountain ranges, earthquakes, and volcanic activity.
shearing work
Tensional stress occurs when layers of rock are pulled apart. This type of stress results in the stretching and thinning of rock layers, leading to the formation of features like rift valleys or normal faults.