What Is Meant By Elastic Rebound Quizlet. The palte or rock layer keeps on deforming till it r. Web elastic rebound noun geology a theory of earthquakes that envisages gradual deformation of the fault zone without fault slippage until friction is overcome, when the fault suddenly.
Earthquake and plates tectonics Elastic rebound
Web elastic rebound refers to how the slippage along a fault (i.e., earthquake) allows the deformed rock to regain its original shape in a new location. Web elastic rebound noun geology a theory of earthquakes that envisages gradual deformation of the fault zone without fault slippage until friction is overcome, when the fault suddenly. Rebound is governed by various properti…. The idea is that a fault is stuck until the strain accumulated in. The palte or rock layer keeps on deforming till it r. Energy is released more stress than the rock can hold returns elastically deformed rock to its shape. Which of the following best describes. As the earth’s crust deforms, the rocks which span the. Web elastic rebound is what happens to the crustal material on either side of a fault during an earthquake. Web 100% (3 ratings) the elastic rebound defines how the energy is transferred during the earthquakes.
The palte or rock layer keeps on deforming till it r. Web elastic rebound refers to how the slippage along a fault (i.e., earthquake) allows the deformed rock to regain its original shape in a new location. Which of the following best describes. It describes the build up and release of stress during an earthquake. The palte or rock layer keeps on deforming till it r. Web elastic rebound is what happens to the crustal material on either side of a fault during an earthquake. Web elastic rebound theory. Rebound is governed by various properti…. Web elastic rebound is caused by the accumulated pressure on the rocks lining each side of a fault. The idea is that a fault is stuck until the strain accumulated in. Web elastic rebound noun geology a theory of earthquakes that envisages gradual deformation of the fault zone without fault slippage until friction is overcome, when the fault suddenly.
