• Shuffle
    Toggle On
    Toggle Off
  • Alphabetize
    Toggle On
    Toggle Off
  • Front First
    Toggle On
    Toggle Off
  • Both Sides
    Toggle On
    Toggle Off
  • Read
    Toggle On
    Toggle Off
Reading...
Front

Card Range To Study

through

image

Play button

image

Play button

image

Progress

1/37

Click to flip

Use LEFT and RIGHT arrow keys to navigate between flashcards;

Use UP and DOWN arrow keys to flip the card;

H to show hint;

A reads text to speech;

37 Cards in this Set

  • Front
  • Back

seismic waves

reveal its concentric layers

seismographs

record earthquake wave motion, primary, scondary, and surface waves

kinds of crusts

continental and oceanic

continental crust

made of andesitic rocks

oceanic crust

basaltic composotion

wegener

theory of continental drift

paleomagnetism

magnetism frozen in rocks at the time of their formation, evidence of continental displacements and records

seismic waves

messages from the interior

primary waves

speediest, first to arrive at seismograph

secondary waves

secondary to arrive, rock segments vibrate at right angles to travel direction

body waves

p and s waves, penetrate deep in the interior

surface waves

large motion waves that travel through the outer crust

discontinuities

boundaries wehre seismic waves experience an abrupt change in velocity or direction

mantle

upper mantle permit waves to travel faster

moho discontinuity

30 km beneath surface of continents and less deep beneath ocean floors, between crust and mantle

Gutenberg discontinuity

outer boundary of the core

shadow zone

waves do not appear

isostasy

condition of vertical balance, float at different heights in water

oceanic crust

more dense

laurasia

northern part of pangea

gondwana

southern portion of pangea

pahthalassa

universal ocean



spreading center

plate moving away

trailning edge

new oceanic crus is added to the trailing edge of each separating plate

guyots

sea floor volcanoes with flat tops

transform plate boundary

plates move sideways

subduction zone

one slab plunges down when they collide

suture zone

faulting, folding, metamorphism and intrusive activity

accretionary prism

contorted and metamorphosed body of rock, continental oceanic convergence

melange

complexly folded jumble of deformed and transported rocks, continental oceanic convergance

ophiolite suite

distinctive assemblage of rocks composed of deep-sea sediment, continental oceanic convergence

blueschists

metamorphic rock containing blue materials showing convergence of continental and oceanic plates

wilson cycle

opening of new ocean basin along divergent zones and expansion on basin as seafloor spreading

inclination

angel of the magnetic field with respect to he horizontal

inclination

used to determine latitude

thermal plumes

concentrated areas of heat

width of magnetic strips

wide=long time, narrow=short