This is known as tensile 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.
Stress at a divergent plate boundary is called tensional stress. This stress creates pulling forces that lead to the plates moving away from each other, resulting in the formation of new oceanic crust.
A divergent boundary causes tensional stress, where tectonic plates are moving away from each other. This stress results in the stretching and thinning of the Earth's crust, leading to the formation of new crust through volcanic activity and seafloor spreading.
divergent plate boundaries are associated with normal faulting. Thus there is a horizontal least compressive stress, vertical most compressive stress and a intermediate horizontal stress. All stresses are orthoganal to each other.
This is known as tensile 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 stress
Tensional stress
Stress at a divergent plate boundary is called tensional stress. This stress creates pulling forces that lead to the plates moving away from each other, resulting in the formation of new oceanic crust.
A divergent boundary causes tensional stress, where tectonic plates are moving away from each other. This stress results in the stretching and thinning of the Earth's crust, leading to the formation of new crust through volcanic activity and seafloor spreading.
The type of stress that causes rocks to pull apart is a tension stress. It is the major type of stress found in divergent plate boundaries.
divergent plate boundaries are associated with normal faulting. Thus there is a horizontal least compressive stress, vertical most compressive stress and a intermediate horizontal stress. All stresses are orthoganal to each other.
We lack the knowledge which it would take to answer that question correctly.
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.
Tension stress pulls rocks apart, causing them to stretch and potentially break along fractures or faults. This type of stress is common in divergent plate boundaries and areas experiencing extensional tectonic forces.
Tensional stress pulls crust apart and stretches rock, causing it to deform and eventually break along fault lines. This type of stress commonly occurs at divergent plate boundaries where tectonic plates are moving away from each other.