The type of stress that involves vertical movement is known as "compression" or "tension" stress. Compression occurs when materials are pushed together, leading to a decrease in volume, while tension occurs when materials are pulled apart, resulting in elongation. These types of stress are commonly associated with tectonic plate movements, where compression can lead to the formation of mountains, and tension can cause rift valleys.
vertical... i think
A fault with little or no vertical movement is called a strike-slip fault. In this type of fault, the rocks on either side of the fault move horizontally past each other, usually in a side-to-side motion. This movement can cause earthquakes when the stress along the fault overcomes friction and the rocks suddenly slip.
A fault that forms as a result of shear stress is called a strike-slip fault. In this type of fault, the rocks on either side of the fault move horizontally past one another, typically along a vertical or near-vertical fault plane. Strike-slip faults are often associated with tectonic plate boundaries, such as transform boundaries, where lateral movement occurs. An example of a well-known strike-slip fault is the San Andreas Fault in California.
Shearing stress is typically associated with strike-slip faults, where two blocks of the Earth's crust slide past one another horizontally. This type of faulting occurs due to lateral forces acting parallel to the fault line, resulting in deformation without significant vertical movement. An example of a strike-slip fault is the San Andreas Fault in California.
Yes, deep cracks in the Earth's crust where rocks move in opposite directions are known as faults. These geological features occur due to tectonic forces, causing stress to build up in the crust until it is released as an earthquake. The movement along faults can be horizontal or vertical, depending on the type of fault. Common types include strike-slip faults, where the movement is primarily horizontal, and normal or reverse faults, which involve vertical displacement.
vertical... i think
vertical... i think
Type I: Moderate movement of the urethra, with no hernia or cystocele
A fault with little or no vertical movement is called a strike-slip fault. In this type of fault, the rocks on either side of the fault move horizontally past each other, usually in a side-to-side motion. This movement can cause earthquakes when the stress along the fault overcomes friction and the rocks suddenly slip.
vertical movement of a body of water called
a creep meter measures vertical movement and a tilt meter measures horizontal movement. Hope my answer works for you thanks
Monocline
A fault is a fracture in the Earth's crust where movement has occurred. This movement can be horizontal, vertical, or a combination of both. Faults can generate earthquakes when the stress along the fault is released suddenly, resulting in movement along the fault surface.
The vertical movement of air is called convection. This process involves the transfer of heat through the movement of air or fluid particles.
Faults in earth science are fractures or discontinuities in the Earth's crust where there has been movement. This movement can be vertical, horizontal, or diagonal, and is caused by stress within the Earth's lithosphere. Faults are classified by the direction of movement as either normal (extensional), reverse (compressional), or strike-slip (lateral).
Shearing stress is typically associated with strike-slip faults, where two blocks of the Earth's crust slide past one another horizontally. This type of faulting occurs due to lateral forces acting parallel to the fault line, resulting in deformation without significant vertical movement. An example of a strike-slip fault is the San Andreas Fault in California.
jelly