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30 Cards in this Set

  • Front
  • Back

Lithosphere

outer solid region of the earth that includes the crust and very upper mantle

Asthenosphere

upper mantle region of the earth, below the lithosphere

Continental Crust

-40% of the earths surface


-thickness 35-40 km


-density 2.7 g/cm

Oceanic Crust

-60% of the earths surface


-thickness 5-10 km


-density 30g/cm

Mantle

-thick layer of rocky materials


-67% of the earths mass


-depth 1800 miles

Outer Core

-made of iron and nickel


-all molten liquid


-magnetic

Inner Core

-high pressure=solid iron


-hot !

Mohorovicic Discontinuity

the moho is the boundary between the crust and the mantle



Iron

the element Fe

Convection Current

a current in a fluid that results from convection

Density

mass per unit volume

Paleomagnetism

the study of the record of the Earth's magnetic field in rocks

Magnetic Poles

the regions of a magnet that attracts or repels other magnetic objects

Dynamo Process

the earths magnetism thats generated by electrical currents in the outer iron core

Convergent Boundary

the region where two tectonic plates collide

Divergent Boundary

the region where two tectonic plates move away from each other

Transform Boundary

the region where two plate tectonics slide past each other in seperate directions

Earthquake

the movement of plate tectonics causing the earth to shake and/or form or destroy land

Volcano

when hot gases or liquids erupt from the earths crust because of convection

Mountain Range

a line of mountains connected by high ground

Trench

a long, narrow ditch

Rift Valley

a long narrow valley that lies in between two faults

Mid-Ocean Ridge

an underwater mountain range

Abraham Ortelius

though that all the continents were once connected

Eduard Suess

discovered an ancient continent called Gondwanaland

Alfred Wegener

created the Continental Drift theory

Theory of Continental Drift

the theory that all of the continents were joined together as one subcontinent called Pangea

Harry Hess

presented the theory of seafloor spreading

Seafloor Spreading

new crust being formed at mid-ocean ridges and old crust being destroyed at oceanic trenches

Laws of Thermodynamics

the laws define the fundamentals like temp and energy