Sudden movement or vibration of the Earth'srockyouterlayer
Volcanic earthquake
Earthquake caused by the movement of magma beneath the surface of the Earth
The Earth continuously changes over time, and earthquake and volcanic activities modify the landscape in a random and remarkable way over a long period of time
Earthquakes happen when two large pieces of the Earth's crust suddenly slip
Crustal plates
The outer shell of the Earth
Fault line
The surface along which the crustal plates move
Seismometer
Instrument that responds to ground noises and shaking such as caused by earthquakes, volcanic eruptions, and explosions
Magnitude
The energy released by an earthquake at the focus, calculated from earthquakes recorded by a seismograph
Intensity
The strength of an earthquake perceived and felt by people in a certain locality, generally higher near the epicenter
Magnitude is a quantitative measure of an earthquake's strength in terms of energy released, while intensity is an indicator of the severity of shaking generated at a given location
Focus
The actual location where fault movement begins, below the Earth's surface
Epicenter
The point at the land surface directly above the focus
Types of natural earthquakes
Tectonic earthquakes
Volcanic earthquakes
Tectonic earthquakes
Produced by sudden movement along faults and plate boundaries
Volcanic earthquakes
Produced by the movement of magma beneath the volcanoes
The difference between tectonic and volcanic earthquakes is that tectonic earthquakes cause collapse of different structures, while volcanic earthquakes cause explosions
Cause of volcanic eruption
Movement of magma beneath the surface of the Earth, resulting in pressure changes and stress on the crust
Scientists cannot predict earthquakes, but they can point out where fault lines are to know where earthquakes are likely to occur
The largest earthquake ever recorded was in Chile in 1960, measuring 9.6 on the Richter scale, and the largest in the U.S. was a 9.2 magnitude in Alaska in 1964
Earthquakes can cause huge waves in the ocean called tsunamis, and the movement of tectonic plates can form large mountain ranges like the Himalayas and the Andes