anything being pulled apart is under a tensile load. springs, cables, and ropes often experience tension forces
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.
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.
Gravitational force Electromagnetic force Strong nuclear force Weak nuclear force Frictional force Tension force Spring force Magnetic force Electric force Buoyant force
There is no way to answer because you have not given any examples where a force would be represented.
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.
Tensional force is created when there is an applied force that pulls or stretches an object. This force is typically generated by the interaction between two objects or components, such as when a rope is pulled from both ends or when a spring is stretched. Tensional force is responsible for maintaining the structural integrity of the object and counteracting the forces trying to compress or break it.
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.
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.
Gravitational force Electromagnetic force Strong nuclear force Weak nuclear force Frictional force Tension force Spring force Magnetic force Electric force Buoyant force
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.
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
Tensional forces typically cause objects to stretch or elongate.
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.
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