How is stress stored between tectonic plates? This animation shows the buildup of stress along the margin of two stuck plates that are trying to slide past one another. They eventually rupture along the fault. The rock is deformed as it builds up strain in the plates; stress increases along the contact. Rock is deformed as it builds up strain in the plates at locked plate boundaries. Stress and strain increase along the contact until the friction is overcome and rock breaks. Actual video footage
0:05
How is stress stored between tectonic plates? This animation shows the buildup of stress along the margin of two stuck plates that are trying to slide past one another. They eventually rupture along the fault. The rock is deformed as it builds up strain in the plates; stress increases along the contact. Rock is deformed as it builds up strain in the plates at locked plate boundaries. Stress and strain increase along the contact until the friction is overcome and rock breaks. Actual video footage
655 viewsJul 16, 2019
FacebookEarthScope Consortium
This animation describes stress in Earth's outer layer and how it leads to faults and plate boundaries. https://www.iris.edu/hq/inclass/animation/earthquake_faults_plate_boundaries__stress | EarthScope Consortium
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This animation describes stress in Earth's outer layer and how it leads to faults and plate boundaries. https://www.iris.edu/hq/inclass/animation/earthquake_faults_plate_boundaries__stress | EarthScope Consortium
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FacebookEarthScope Consortium
Earth’s thin, brittle outer shell of rock is under a constant state of stress. Stress impacts the formation of small local faults, and broader tectonic plate boundaries. How the rock responds, depends on the type of stress and the conditions the rock is being subjected to when it encounters stress. It is this change in Earth’s crust that generates different types of faults and plate boundaries. https://www.iris.edu/hq/inclass/animation/earthquake_faults_plate_boundaries__stress | EarthScope Cons
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Earth’s thin, brittle outer shell of rock is under a constant state of stress. Stress impacts the formation of small local faults, and broader tectonic plate boundaries. How the rock responds, depends on the type of stress and the conditions the rock is being subjected to when it encounters stress. It is this change in Earth’s crust that generates different types of faults and plate boundaries. https://www.iris.edu/hq/inclass/animation/earthquake_faults_plate_boundaries__stress | EarthScope Cons
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FacebookEarthScope Consortium
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