The theory of plate tectonics
The hypothesis that explains the release of energy during an earthquake is called the elastic rebound theory. This theory states that rocks on either side of a fault are deformed by tectonic stresses until they reach a breaking point. Once this breaking point is exceeded, energy is released in the form of seismic waves, causing an earthquake.
The hypothesis that explains the release of energy during an earthquake is the elastic rebound theory. This theory posits that tectonic plates are subjected to stress as they move and become deformed, storing elastic energy. When the stress exceeds the strength of the rocks, they break and quickly return to their original shape, releasing the stored energy in the form of seismic waves, which we experience as an earthquake. This process occurs along faults where the rocks are most likely to fracture.
The scientific theory is called plate tectonics, which describes the movement and interaction of Earth's lithosphere plates. This theory explains phenomena such as earthquakes, volcanoes, and mountain formation.
The elastic rebound theory for the origin of earthquakes was first proposed by American geologist Harry Fielding Reid in 1910. This theory states that tectonic stress builds up along faults until it exceeds the strength of the rocks, causing them to suddenly break and release energy in the form of an earthquake.
According to the kinetic theory of gases, gas particles are in constant random motion due to their kinetic energy. This theory also explains how gas pressure and temperature are related to the average kinetic energy of the gas particles.
elastic rebound theory
Due to the disturbances in tectonic plates
elastic rebound theory
the theory explains how Earth's plates form and move. it also explains how plates interact ,producing volcanoes,mountain range ,earthquakes,and featurs of the ocean floor
The hypothesis that explains the release of energy during an earthquake is called the elastic rebound theory. According to this theory, stress builds up along a fault line until it exceeds the strength of the rocks, causing them to suddenly break and release accumulated energy in the form of seismic waves.
The hypothesis that explains the release of energy during an earthquake is called the elastic rebound theory. This theory states that rocks on either side of a fault are deformed by tectonic stresses until they reach a breaking point. Once this breaking point is exceeded, energy is released in the form of seismic waves, causing an earthquake.
The Elastic-Rebound theory explains how earthquakes occur. Rocks on opposite sides of a fault are subjected to force, causing them to shift. They absorb strength which causes them to deform and exceed their internal strength. A sudden movement occurs along the fault and this causes the energy and rocks to go back to their pre-deformed state.
If by "why" you mean "what," a well tested framework that explains a wide range of observations in science is called a theory.
The theory of plate tectonics helps to explain how earthquakes and volcanic eruptions occur.
The hypothesis that explains the release of energy during an earthquake is the elastic rebound theory. This theory posits that tectonic plates are subjected to stress as they move and become deformed, storing elastic energy. When the stress exceeds the strength of the rocks, they break and quickly return to their original shape, releasing the stored energy in the form of seismic waves, which we experience as an earthquake. This process occurs along faults where the rocks are most likely to fracture.
Plate tectonics is the theory that explains the movement of Earth's surface. It states that the Earth's lithosphere is divided into large plates that float on the semi-fluid asthenosphere below, causing them to move and interact with one another. This movement is responsible for various geological processes such as earthquakes, volcanic eruptions, and the formation of mountain ranges.
The theory that explains how continents moved apart is called plate tectonics. It proposes that the Earth's lithosphere is divided into several large plates that move and interact with each other, causing phenomena like continental drift, earthquakes, and volcanic activity.