Tensional force is created when a string is stretched beyond its original length
At divergent boundaries, the force present is tensional stress caused by the pulling apart or separation of tectonic plates. This tensional stress leads to the formation of rift valleys and mid-ocean ridges as magma rises to fill the gap created by the diverging plates.
Tensional force is a pulling force that occurs when an object is being stretched or pulled in opposite directions. It is commonly seen in objects like ropes, cables, and springs, where the force is applied in a way that creates tension along the length of the object.
tensional forces
This could cause an earthquake.
anything being pulled apart is under a tensile load. springs, cables, and ropes often experience tension forces
Tensional forces are created when a structure is pulled or stretched in opposite directions. These forces play a crucial role in the mechanics of structures by helping to distribute loads and maintain stability. In essence, tensional forces help to counteract compressive forces and prevent the structure from collapsing under pressure.
Tensional stress from divergent plate boundaries causes a normal fault to form. This stress pulls rocks apart along a fault line, causing the hanging wall to drop relative to the footwall.
Gravitational force Electromagnetic force Strong nuclear force Weak nuclear force Frictional force Tension force Spring force Magnetic force Electric force Buoyant force
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 boundary is the meeting zone of two tectonic plates at a normal fault; the plates move apart
A normal fault results from tensional forces pulling rocks apart, causing the hanging wall to move downward relative to the footwall. A reverse fault is caused by compressional forces pushing rocks together, resulting in the hanging wall moving up relative to the footwall. A strike-slip fault is produced by horizontal shearing forces causing rocks to move horizontally past each other.
Tensional forces typically cause objects to stretch or elongate.