• 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

1/28

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;

28 Cards in this Set

  • Front
  • Back
  • 3rd side (hint)

Deposition

Sedimentation deposited in layers in lake or ocean.

Lake/Ocean

Compaction

Sediments squeezed together by pressure of overlaying sediments layers.

Squeeze

Cemntation

Dissolved minerals in water move through compacted sediments plus glued together.

Gravel

Conglomerate

Sand

Sandstone

Silt

Silt stone

Clay

Shale/Mudstone

Basalt

Dense,black,no mineral grains

Scoria

Black/Red Holes

Pumice

Grey, Small holes, not very dense

Granite/Diorite

Mineral grains, large & visible

Outer cooled magma

Extrusive igneous rock

Inner cooled magma

Intrusive igneous rock

Weathering

Breaking down rock into smaller pieces

Erosion

Movement of sediments one place to another

Sediment Process order

Weathering,Erosion,deposition,compation,cementation

Chemical Sediment

Formed when dissolved minerals precipitate out of a solution

Organic Sediment

Rock formed from remains of a once living organism.

Metamorphic Rock

Changed rocks,change in minerals composition, and in form.

Quartz + Sandstone

Quartzite

Granite

Gneiss

Limestone + CaCO3

Marble

Shale + Mudstone

Slate

Coal

Anthracite Coal

Mica

Mica schist

Garnet

Garnet schist

Subduction

A process that takes place at the convergent boundaries by which one tectonic plate moves under another tectonic plate and sinks into the mantle as the the plates converge.

Seafloor spreading name of man,date, and theory.

Man : Harry Hess



Time : Period



Theory : Hot and less dense material below the earth's crust rises toward the earth's surface at mid ocean ridges then flows sideways carrying the seafloor away from the ridge both ways.