Earthquakes can strike any location at any time, but history shows they occur in the same general patterns year after year, principally in three large zones of the earth: The world's greatest earthquake belt, the circum-Pacific seismic belt, is found along the rim of the Pacific Ocean, where about 81 percent of our planet's largest earthquakes occur. Some faults crack through the Earth because of the stress and strain of the moving plates. Most earthquakes occur along the edge of the oceanicand continental plates. Earthquakes and volcanoes also allow geoscientists to indirectly study the interior of the earth.

However, where transform Plate boundaries run through continents, they can cause major earthquakes. For example, the New Madrid area of Missouri (1811-1812), Charleston, South Carolina (1889), Boston (1755), and Hawaii (1975) are all places which have large earthquakes.

In fact because of the behavior of earthquakes and volcanoes the core of the theory of plate tectonics has been proved. Earthquakes occur along all types of plate boundaries: subduction zones, transform faults, and spreading centers.

Away from plate boundaries, almost all earthquakes are less powerful than magnitude 5.5, but occasional powerful earthquakes can still occur, such as the New Madrid earthquakes of 1811-1812 [3]. Plate tectonics, earthquakes and volcanoes are closely related. Sometimes the molten rock rises to the surface, through the continent, forming a line of volcanoes. Along Plate Edges.

The Ring of Fire is the most seismically and volcanically active zone in the world. Transform faults are found where plates slide past one another.


The earth's crust(the outer layer of the planet) is made up of several pieces, called plates. Earthquakes occur all the time all over the world, both along plate edges and along faults. There's a variety of things and, basically, anything which can apply large forces to the plates can cause earthquakes. About 80% of earthquakes occur where plates are pushed together, called convergent boundaries. That only occurs at convergent boundaries, where plates are sometimes pushed deep beneath the surface and into the mantle.

About 80% of earthquakes occur where plates are pushed together, called convergent boundaries.
Since neither plate is stronger than the other, they crumple and are pushed up.

Divergent faults and rift valleys within a continental mass also host shallow-focus earthquakes . Earthquakes are located along the normal faults that form the sides of the rift or beneath the floor of the rift. Another form of convergent boundary is a collision where two continental plates meet head-on.

There are three types of plate boundaries: spreading zones, transform faults, and subduction zones.


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