Composed of the crust and the upper mantle, constant but very slow in motion
Plates
Rigid sections of the lithosphere that move as a unit
Plate Tectonics Theory
The entire lithosphere of the earth is broken into numerous segments called plates
Crust
Average density is 2.8g/cm3 and 5-50km thick
Continental crust is thicker but less dense
Oceanic crust is thinner but more dense
Earthquake
Vibration of earth due to the rapid release of energy
Triangulation Method
Measures earthquakes with 3 Seismographs
Seismograph
Device used to record earthquake waves
Seismogram
Record made by a seismograph
Types of Plate Boundaries
Divergent Boundary - Constructive, creates rift valleys and mid-oceanic ridges
Convergent Boundary - Destructive, creates mountains, volcanos, or subduction zones that form large trenches
Transform Boundary - Conservative, creates deep trenches, and scarps and ridges
Types of Convergent Plate Boundaries
Continental-Oceanic - The latter subducts under the former and volcanic arc forms above it. The pieces that subduct melts and becomes magma that rises.
Oceanic-Oceanic - The older plate will subduct under the other. Trenches and volcanic island arcs form above the younger plate.
Continental-Continental - They will buckle up and form mountain ranges.
Subduction
Bending of the crust towards the mantle
Trench
Submarine valleys, lowest part of the ocean
Tsunami
The Japanese term for "harbor wave," a series of ocean waves with very long wavelengths
Continental Volcanic Arc
Mountains formed in part by igneous activity associated with subduction of oceanic lithosphere beneath a continent
Volcanic Island Arc
A chain of volcanoes that develop parallel to a trench
Hotspot
Concentration of heat in the mantle capable of creating magma
Magma
Mass of molten rock
Mid-Ocean Ridge
A continuous mass of land with long width and height on the ocean floor
Fracture
A break in a rock with no movement
Fault
A break in a rock along which a movement has occurred