• 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

1/31

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;

31 Cards in this Set

  • Front
  • Back

Eon

All time

Era

Before life

Period

Life evolution

Epoch

Since last extinction

Uniformitarianism

Assumes that the same physical processes active in the environment today have been operating throughout geologic time.

Catastrophism

Theory that the Earth has been affected in the past by sudden, short-lived, violent events, possibly worldwide in scope.

Half life geologic dating

Radioactive decay and half life

Crust

Oceanic and continental, earth's outermost shell of crystalline surface rock.

Mantle

Lower and upper (80% of earth's mass), denser and tightly packed at depth, grading to lesser densities toward and the surface.

Core

Inner and outer. Inner core is solid iron and nickel, and outer core is molten, metallic iron

Lithosphere

Includes the crust, the upper mantle (rigid part), and moho

Aesthenosphere

Upper viscous mantle on which the lithosphere floats. Plastic layer

Mohorovičić discontinuity

The boundary between the crust and the high velocity portion of the lithosphere upper mantle.

Continental crust

Granite, lower density, lighter color

Oceanic crust

Basalt, higher density, and darker color

Isostacy

Explains certain vertical movements of Earth's crust.

Subduction

An area where two plates of crust collide and the denser oceanic crust goes beneath the less dense continental plate, forming deep oceanic trenches.

Tectonic cycle

Rising magma, sea floor spreading, subduction, continental crust formation

Rock cylce

Igneous, metamorphic, and sedimentary

Igneous rock

Form from magma and it solidifies and crystallizes.

Sedimentary rock

Are derived from existing rocks or from organic materials such as bone and shell.

Metamorphic rock

Any rock can be transformed into this by going through profound physical and or chemical changes under pressure and increased temperature.

Magma

Composed of molten rock and is stored in the Earth's crust.

Lava

Is magma that reaches the surface of our planet through a volcano vent.

Plate tectonics

Is the theory that Earth's outer shell is divided into several plates that glide over the mantle, the rocky inner layer above the core.

Pangea

A supercontinent that existed during the late Paleozoic and Mesozoic era.

Gondwana

Part of Pangaea made up the Southern Hemisphere countries.

Laurasia

Northern part of Pangaea make up most of the northern hemisphere.

Divergent

Sea floor spreading

Convergent

Subduction

Transform

Lateral sliding