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29 Cards in this Set

  • Front
  • Back

The modern scientific theory which describes the movement of Earth's outer layer

Plate Tectonics

lithosphere

the uppermost mantle along with the overlying curst, behave as a strong, rigid layer

Lithospheric plates or plates

moves as a unit over the material of the asthenosphere

divergent plate boundaries

two plates move apart

convergent plate boundaries (Subduction zone)

two plates move towards one another

transform fault boundaries

two plates grind past each other

straitions

scratches or groves created by glacial debris as it moves.

magma

a body of molten rock found at depth include any dissolve gases and crystals

seafloor spreading

new oceanic crust is produced at the crests of mid-ocean ridges

continental rifting

the landmass may split into two or more smaller continents

rift valley

the crust fractures to form a long trough

melt

the liquid portion of magma excluding the solid crystals

basaltic

fine-grained igneous rock of mafic composition

earthquake

the vibration of earth, produced by the rapid release of energy

focus

energy radiates in all direction from its source

faults

a break in rock mass along which movement has occured

elastic rebound

the sudden release of stored strain in rocks that result in movement along the fault

seismology

the study of earthquake waves

Seismographs

instruments that record seismic waves

surface waves

waves traveling along the outer part of earth

body waves

waves travel through the earths interior

primary Waves

alternating compression and expansion of material through which it passes. Push and Pull

secondary waves

oscillation perpendicular to the direction of propagation shake

epicenter

the point on earth's surface directly above the focus

deep-focus earthquakes

focus greater than 300 kilometers

inner core

a solid, iron-rich, sphere having a diameter of 2432 kilometers

outer core

a fluid metallic layer some 2270 kilometers thick

mantle

a solid, rocky layer having a thickness of about 2885 kilometers

crust

a very thin outer skin that ranges from about 7 to more than 70 kolometers thick