normal fault occurs...odyssey
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.
The stress at a divergent boundary is called tensional stress. This stress occurs when tectonic plates move away from each other, causing the crust to stretch and thin out.
The three types of stress that can change a rock as tectonic plates move horizontally are shear stress, compressional stress, and tensional stress. Shear stress occurs when rocks are pushed past one another, leading to deformation along faults. Compressional stress can cause rocks to fold or break as they are squeezed together, while tensional stress results in pulling apart, leading to stretching or fracturing of the rock. These stresses contribute to various geological features and processes associated with plate tectonics.
Rock folding occurs when tectonic forces cause the Earth's crust to bend and deform, usually in response to compression or collision of tectonic plates. This deformation can result in curved or wrinkled layers of rock, known as folds, forming within the Earth's crust.
The process you are referring to is called tectonic deformation or tectonic overturning. It occurs when internal tectonic forces cause rock layers to rotate or flip over. This can happen during intense geological events like folding, faulting, or mountain building.
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.
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.
Tensional stress force pulls on the crust and stretches rock. This type of stress occurs where tectonic plates are moving away from each other.
Tensional stress
Tensional stress
The stress at a divergent boundary is called tensional stress. This stress occurs when tectonic plates move away from each other, causing the crust to stretch and thin out.
Tensional forces can lead to features such as faulting, folding, and stretching or extension of the Earth's crust. Faulting occurs when rocks break and move along a fault plane, while folding involves bending and warping of rock layers. Stretching or extension results in the thinning and spreading apart of the crust.
The force that pulls apart the crust is called tensional or extensional tectonic stress, which occurs at divergent plate boundaries where tectonic plates move away from each other. This pulling force can lead to the formation of rift valleys and mid-ocean ridges.
The three types of stress that can change a rock as tectonic plates move horizontally are shear stress, compressional stress, and tensional stress. Shear stress occurs when rocks are pushed past one another, leading to deformation along faults. Compressional stress can cause rocks to fold or break as they are squeezed together, while tensional stress results in pulling apart, leading to stretching or fracturing of the rock. These stresses contribute to various geological features and processes associated with plate tectonics.
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The geological formation that often occurs at subduction zones where one tectonic plate subducts under another is called a trench.
Earthquakes are primarily caused by tectonic stress, which occurs when the Earth's tectonic plates interact. This stress can result from three main types of tension: compressional stress, where plates push together; tensional stress, where plates pull apart; and shear stress, where plates slide past one another. When the accumulated stress exceeds the strength of the rocks, it releases energy in the form of seismic waves, causing an earthquake.