The force responsible for making two tectonic plates jerk into a new position is typically the release of built-up stress along a fault line, resulting in an earthquake. This sudden movement is known as fault slippage and can occur from the accumulation of strain over time due to the slow motion of the plates against each other. This sudden release of energy causes the plates to move and can result in seismic activity.
The San Andreas Fault experiences primarily strike-slip forces, where two tectonic plates slide past each other horizontally. This type of motion causes earthquakes along the fault line as stored energy is released.
Convergent boundaries produce earthquakes as two tectonic plates collide or converge, leading to intense pressure build-up and eventual release in the form of seismic waves. This can result in deep-focus earthquakes or shallow-focus earthquakes, depending on the location within the boundary where the movement occurs.
A sudden jerk of land is called a fault. It occurs when there is a sudden release of energy along a fracture in the Earth's crust, resulting in seismic activity such as earthquakes.
Earthquakes are caused by the sudden release of energy in the Earth's crust, typically along fault lines where tectonic plates meet. This release of energy in the form of seismic waves propagates through the Earth, causing the ground to shake. The magnitude of an earthquake is measured on the Richter scale, which quantifies the energy released by the earthquake.
Earthquakes are tremors or vibrations in the Earth's crust that are caused by the build up or accumulation of pressure (more correctly termed stress).More:The Earth's crust, or lithosphere (hard outer surface) is made up of "tectonic plates", or large plates. There are about 7 major plates and many smaller plates, around 100 km thick, which sit upon a lower soft layer (the asthenosphere). The tectonic plates are always slowly moving, but they get stuck at their edges due to friction. When the stress on the edge overcomes the friction, there is an earthquake that releases energy in waves that travel through the earth's crust and cause the shaking that we feel.This accumulation of stress causes the rocks that make up the crust to deform elastically. This is very similar to what happens when you squash or stretch a spring and causes a form of energy to be stored in the rocks of the crust - technically described as elastic potential energy.When this stress gets too large, it exceeds the strength of the rocks in the crust and causes a brittle failure. Brittle failures are failures where fractures form through the material. As these have been happening for a long time, the earth's lithosphere is already fractured. These fractures are known as faults and as these represent zones of weakness within the lithosphere, it is along faults where the majority of earthquake occur when they slip suddenly.This sudden brittle failure causes all of the elastic potential energy to be released at one time in the form of seismic waves, just as if a spring or elastic band that was being stretched suddenly snapped.These seismic waves cause the tremors that people feel on the surface and which can cause damage to buildings and other structures.Please see the related links for more information.The Earth's crust, or lithosphere (hard outer surface) is made up of "tectonic plates", or large plates. There are about 7 major plates and many smaller plates, around 100 km thick, which sit upon a lower soft layer (the asthenosphere).When these plates move against each other along plate boundaries (where two plates meet) or along faults (a rift), an earthquake occurs. This may be through a variety of movements: sideways, up and down or apart. This causes anything upon the upper surface, above the earthquake, to also shift, whether they be buildings, roads, bridges, railways, etc.What you actually feel when you feel the shaking of an earthquake are the seismic waves.There are three types of seismic waves and they are determined by the properties of the rock through which they travel:P-waves (compressional waves) or primary waves are the first waves: they travel the fastest and can travel through everything.Then the S-waves (shear waves) or secondary waves come: they move slower and cannot travel through liquids.At last the Surface-waves come. They are the slowest and they cause the biggest damage. Often it is when the surface-waves come that the buildings collapse.An earthquake describes when the earth moves the ground under your feet. It can slide it from side to side or move it a few feet in one direction. It can lift it up in one place and make it sink in another. The results of this are quite visible in and near Anchorage, Alaska. One street in that town shows where an earthquake make the ground fell. Driving south, dead trees stick up out of a lake where the ground fell below sea level. Earthquakes are caused when faults or cracks in the earth's shell suddenly slip past each other. When they jerk, they move a lot of land with them. That makes the earth tremble. Sometimes it damages buildings.The official definition for the word earthquake is "a sudden and violent shaking of the ground, sometimes causing great destruction, as a result of movements within the earth's crust or volcanic action." knowing these earthquakes happen almost everywhere they do most take place in the U.Sin the state of California just a (FYI)tectonic plates- move in 3 ways1. collide w/ eachother2.seperate from eachother3. slide against eachotherwhen plates are moved to the breaking point it causes an eartquakean earthquake is a seismic wave
They can actually feel the earthquake.
the earths gravitiy causes it to push down
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earthquakes
When two plates jerk into a new position, it can result in an earthquake. The sudden movement along a fault line caused by the plates shifting can release a significant amount of energy, leading to seismic waves being generated and felt as vibrations on the Earth's surface.
During an earthquake, people can feel the force of the plates shifting against each other, causing shaking of the ground. This can result in a variety of sensations, including swaying, rocking, or jolting motions depending on the earthquake's magnitude and distance from the epicenter.
Tectonic plates are always trying to slowly move, but they more often than not find another tectonic plate in there path of motion. After enough pressure is built up between these plates trying to move past each other, a sudden "jerk" between them happens, and the restoring force from this "jerk" causes the waves we call "seismic waves" to happen.
ur senses
Yank or jerk.
jerk yank
There is no specific formula. The "jerk" refers to the third derivative of a function, specifically a position versus time function in physics. The jerk function describes how the acceleration changes over time.
throttle position sensor