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Javascript must be enabled to view our earthquake maps. To access USGS earthquake information without using javascript, use our Magnitude 2.5+ Earthquakes, Past Day ATOM Feed or our other earthquake feeds.

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Javascript must be enabled to view our earthquake maps. To access USGS earthquake information without using javascript, use our Magnitude 2.5+ Earthquakes, Past Day ATOM Feed or our other earthquake feeds.

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Earthquakes are formed by two tectonics plates sliding

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1. Strike slip fault line- Some Strike-Slip faults move in a left lateral motion.  They are also known as sinistral faults. The others that move in  a right lateral motion are known as dextral faults.  A class of strike slip faults are Transform fault lines where it causes a plate boundary.

2. Normal fault line- A geologic fault in which the hanging wall has moved downward relative to the footwall. Normal faults occur where two blocks of rock are pulled apart, as by tension

3. Reverse fault line- a fault in which the rock above the fault plane is displaced upward relative to the rock below the fault plane

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1. Divergent - linear feature that exists between two tectonic plates that are moving away from each other.

2. Convergent- is an actively deforming region where two (or more) tectonic plates or fragments of the lithosphere move toward one another and collide.

3. Transform-  is where two of the floats - two tectonic plates - side alongside each other. When this happens, the scraping of the two plates causes earthquakes.

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is where two of the floats - two tectonic plates - side alongside each other. When this happens, the scraping of the two plates causes earthquakes.

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a numerical scale for expressing the magnitude of an earthquake on the basis of seismograph oscillations

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are a type of body wave that is the first wave to arrive at the seismograph, called seismic waves in seismology, that can travel through a continuum.

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1. is one of the two main types of elastic body waves, so named because they move through the body of an object, unlike surface waves.

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The location where theearthquake begins. The ground ruptures at this spot, then seismic waves radiate outward in all directions.

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a spot above the point where earthquakes orginates.

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Fault-  is a crack in a rock along which slippage has occurred