• 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

1/33

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;

33 Cards in this Set

  • Front
  • Back

Definition: Rock

-Aggregate of many minerals


-Naturally occurring


-Coherent (one section); grains are not interlocking



Igneous

-Cooling of lava or magma


-Includes both intrusive and extrusive rocks

Sedimentary

-Fragments of rocks, minerals, organic matter


-Formed by compaction, cementation, chemical precipitation

Metamorphic

-Alteration of existing rocks


-Heat and pressure without melting



Intrusive

Formed undergound and then pulled up

Extrusive

Mineral formed on surface after extreme heat

Divergent Plate Boundary

-Plates move apart
-New crust forms
-Occurs: sea floor + continents

-Plates move apart


-New crust forms


-Occurs: sea floor + continents



Early Stage of Divergent Plate Boundary

-Rifting is taking place




EX/ Red Sea

Mid Stage of Divergent Plate Boundary

-Ocean basin is widening


-Linear increase in age with increase in distance




EX/ Central Atlantic Ocean

Mid Ocean Ridges (M.O.R)

-Large canyons in the ocean


-Sea floor spreading in the ocean


-Rising asthenosphere melts, forming mafic magma


-Pooled magma solidifies into oceanic crustal rock




(See: Pillow Basalt, Dikes, Gabbro)

Pillow Basalt

Magma quenched at sea floor

Dikes

Hot, semi-liquid substance that spews from volcanoes cools and becomes solid

Black Smokers

-Found at M.O.R


-Water entering fractured rocks, heated by magma


-Hot water dissolves minerals & cycles out rock


-When water reaches surface, minerals crystalize

Convergent Plate Boundary

-Plates come together
-Density of the crust
  a) Subduction zone (creates volcanoes) 
  b) Collision zone (creates mountains)

-Plates come together


-Density of the crust


a) Subduction zone (creates volcanoes)
b) Collision zone (creates mountains)



Subduction Zone

-The downgoing plate slowly sinks down, into the asthenosphere


-Older oceanic plate goes under


-Subducting plate descends at 45 degree

Earthquake

-When rock breaks in down moving plates, that's an Earthquake


-Earthquakes happen on plate boundaries (particularly in the convergent zone)

Features of Subduction

1) Deep Ocean Trenches


2) Accretionary Prisms


3) Fore-Arc Basins


4) Volcanic Arcs

Deep Ocean Trenches

Deep, away from land

Accretionary Prisms

Pile of sediment on top of plate going down. Mud.

Fore-Arc Basin

The space between the subduction zone

Volcanic Arcs

-A chain of volcanoes on overriding plate


-As it warms, the water is driven off


-Descending plate causes partial melting


-Magma rises and melts through overriding plate

Back-Arc Basin

-A marginal sea behind an arc


-Forms behind an island and a continent

Transform Plate Boundary

-Plates slide past one another
-Different spreading rates, no new plates
-Lots O' little Earthquakes
EX/ San Andreas Fault Zone

-Plates slide past one another


-Different spreading rates, no new plates


-Lots O' little Earthquakes


EX/ San Andreas Fault Zone

Continental Transform

-Cut across continental crust




EX/ San Andres

Triple Junction

-3 plate boundaries intersect 


EX/ Juan de Fuca Plate

-3 plate boundaries intersect




EX/ Juan de Fuca Plate

Hot Spots

-Rising mantle material away from plates


-Originates from deep mantle plume


-Magma rises to surface


-Pierce the overriding plates


-Plate motion pulls volcano off of plume


a) This results in a chain of volcanoes


b) Reinforces sea floor spreading


EX/ Hawaii

Derivative Science

Based in physics, chemistry, biology, math

Integrative Science

Interweaves those fields from derivative science

Uniformitarianism

-Nature follows consistent laws


-Laws operated in the past as they do today


-Geologic processes act naturally and slowly over long periods of time

Name the Layers of Earth

-Magnetosphere


-Atmosphere


-Hydrosphere


-Biosphere


-Solid Earth (lithosphere)

How old is Earth?

4.6 billions years

Endogenic

From Earth's internal energy


-plate tectonics

Exogenic

Powered by solar radiation


-atmosphere/ hydrosphere/ biospheres