ummmmmm i dont know you tell meee!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!!! :O)
The stress that occurs when two items collide is known as impact stress. This type of stress is caused by the sudden application of force when the objects come in contact with each other, leading to deformation or damage.
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.
When two tectonic plates collide, compressional stress occurs. This stress causes the rocks to fold and deform, leading to the formation of mountain ranges, such as the Himalayas. The intense pressure and friction between the plates can also result in earthquakes and volcanic activity.
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.
Compressive stress in the crust leads to the formation of folding mountains. This stress occurs when tectonic plates collide, causing the crust to buckle and fold, resulting in the uplift of mountain ranges. The compressive forces push rocks together, leading to the formation of anticlines and synclines, which are characteristic features of folding mountains.
The stress that occurs when two items collide is known as impact stress. This type of stress is caused by the sudden application of force when the objects come in contact with each other, leading to deformation or damage.
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.
When two tectonic plates collide, compressional stress occurs. This stress causes the rocks to fold and deform, leading to the formation of mountain ranges, such as the Himalayas. The intense pressure and friction between the plates can also result in earthquakes and volcanic activity.
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.
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.
Shear stress.
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.
Compressive stress in the crust leads to the formation of folding mountains. This stress occurs when tectonic plates collide, causing the crust to buckle and fold, resulting in the uplift of mountain ranges. The compressive forces push rocks together, leading to the formation of anticlines and synclines, which are characteristic features of folding mountains.
One major type of stress that occurs at convergent plate boundaries is compressional stress. This stress is caused by the collision of two tectonic plates, leading to the plates pushing against each other and causing rocks to compress and deform, leading to the formation of mountain ranges or subduction zones.
A hanging wall fault experiences compressional stress. This occurs when tectonic plates push against each other, causing the hanging wall block to move upward relative to the footwall block. This type of stress is typical in convergent plate boundaries where plates collide. The resulting geological features often include mountain ranges and uplifted terrains.
Usually occurs at plate boundary collision areas.