fracture
folding
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.
I found that folding happens
I found that folding happens
Compressive stress makes rocks thicker by pushing the rock layers together, causing them to compact and increase in thickness. This type of stress typically occurs when tectonic plates collide, leading to the formation of mountain ranges and thicker rock layers.
Compressive stress causes folding mountains to form. This stress occurs when tectonic plates collide or converge, leading to the deformation and folding of rock layers, ultimately creating mountain ranges.
This stress is called tensional stress, which causes rock layers to stretch and move apart. It can result in the formation of faults or fractures in the rocks, as well as the creation of features like rift valleys or grabens. Tensional stress typically occurs in divergent plate boundaries where tectonic plates are moving away from each other.
A fault called a normal fault occurs when tectonic plates pull apart and tensional stress causes the rock layers to break and move along the fault line. In a normal fault, the hanging wall moves down relative to the footwall due to the extensional forces acting on the rocks.
Frost wedging is a type of physical weathering that occurs in places with large changes in daily temperatures. This process happens when water seeps into cracks in rocks, freezes, expands, and causes stress on the outer layers of the rocks, eventually leading to their breakdown.
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When rock layers bend due to stress, they undergo deformation through a process known as folding. This can result in the formation of structures like anticlines (upward-arching folds) and synclines (downward-arching folds). The degree of bending can vary from gentle folds to tight, complex structures depending on the type and amount of stress applied.
Onion-skin weathering is a geological process that mainly occurs in the deserts. The rock experiences stress on the outer layers because of the heating and expansion during the day and the cooling and contracting at night. this process is achieved through changes in temperature.