stored in carbonate rock.
Yes, this is a very good description of the cause of an earthquake.
If a rock undergoes horizontal stress, Anticlines and Synclines will form.
Geological stress is a force applied to a rock.
Tensile stress.
Stress that pushes rock in diffrent directions is called tension. Not shearing
The three main types of stress in a rock are shearing, tension, and compression.
Elastic potential energy stored in the rock is released in the form of vibrations and heat.
As a result of subduction, the continental crust becomes more compressed and warped by the huge pressures between these two plates. The stressed causes the rock to deform or change shape by bending. Energy was stored in the deformed areas in the form of elastic potential energy, much like when a spring is compressed. When the stress becomes greater then the breaking strength of the rock, a break occurs in the fault. The stored energy within the misshapen plate is suddenly released. When the stress is relieved,that is when when the tectonic plates begin to move under the earths crust.
Potential energy is the energy stored in a rock before its fall from a hill.
Stress, in geology, is pressure and can result in an earthquake should the stress in a rock layer suddenly slip when the rock fractures and there is a sudden movement between the two surfaces.
The stress force that causes a mass of rock to pull or twist in opposite directions is called tension. Shearing is the stress force that causes a mass of rock to pull or twist in opposite directions.