Earthquake: The perceptible shaking of the surface of the earth, caused by the sudden release of energy in earth's crust that releases seismic waves (USGS)
The earth: is dynamic
The outermost layer of the earth is broken into pieces that are called plates that are moving away or toward each other
Crust: outermost layer. Surface of the earth
Mantle: Highly viscous layer of the earth
outer core: hot and liquid; mostly nickel and iron
inner core: solid iron and little nickel
Pangea was the supercontinent that existed 250 Million years ago
Pangea was divided into two; Laurasia and Gondwanaland
3 boundaries of the plate: divergent, convergent, and transform
Divergent: causes volcanos to occur. Spreading centers where plates are moving apart and new crust is created by magma pushing up the mantle
convergent: one plate is subducted underneath another plate.
Transform: two plates sliding past each other
Plates move because of the intense heat in its core that causes molten rocks in the mantle to move.
Plates move in a pattern called convection cell
Types of natural earthquakes: Tectonic and Volcanic
Tectonic: produced by sudden movement of plates and fault boundaries
Volcanic: magma beneath volcanoes move
Ways of describing strength of an earthquake: intensity and magnitude
Intensity: perceived strength based on the relative effect to people, generally higher near the epicenter
magnitude: based on instrumentality derived infos and correlated strentgh