Earths Layers and Plate Tectonics
Continental Drift & Wegener's Evidence
Fossils & Fossilization
Dating Methods & Rock Layers
Erosion & Landforms
100

This is the outermost layer of Earth that is broken into pieces called tectonic plates.

The crust

100

This supercontinent, whose name means "all Earth" in Greek, existed when all continents were connected together.

Pangea

100

These scientists study fossils to understand Earth's history and learn about ancient life.

Paleontologists

100

This law states that in undisturbed rock layers, older rocks are on the bottom and younger rocks are on top.

The Law of Superposition

100

This is the process that breaks down and wears away landforms over time.

Erosion

200

This process, like water boiling or a hot air balloon rising, causes hot material to rise and cool material to sink in Earth's mantle.

 Convection

200

The theory that continents have moved across Earth's surface slowly over millions of years.

Continental drift

200

Footprints, burrows, and coprolites are examples of this type of fossil that shows evidence of ancient animal activity.

 Trace fossils

200

This term describes the method of determining which fossils are older or younger compared to each other

Relative dating

200

This force of erosion carved the Grand Canyon over millions of years.

Water Erosion

300

 At this type of plate boundary, two plates move apart and new crust forms.

a divergent boundary

300

This freshwater reptile fossil was found in both South America and Africa, but couldn't have swum across the Atlantic Ocean.

Mesosaurus

300

During fossilization, the organism must be covered quickly by this material to protect it from decay.

Sediment

300

The collection of rock layers arranged in chronological order is called this.

The fossil record

300

This type of erosion creates sand dunes in Death Valley and shapes desert formations in Monument Valley.

Wind erosion

400

This happens when an ocean plate slides under a continental plate at a convergent boundary

Subduction

400

Lystrosaurus was a land reptile found in Africa, India, and this frozen continent, proving it wasn't always covered in ice.

Antarctica

400

Body fossils preserved in amber or ice are called this type of fossil

True Form Fossils

400

This dating method gives the exact age of a rock or fossil in years. 

Absolute dating

400

Ocean waves cutting coastal cliffs and creating sea stacks along the Big Sur coastline is an example of this type of erosion.

Water erosion

500

This type of plate boundary is where plates slide past each other, causing earthquakes.

Transform boundary

500

Scientists found ancient glacial scratches in tropical places like Africa and India, which only make sense if these continents were once positioned near this pole.

South Pole

500

 A mold fossil is an impression left in rock, while this type of fossil is created when the impression fills in with minerals.

Cast Fossil

500

 According to the Law of Superposition, in undisturbed rock layers, the oldest layers are found here while the youngest are on top.

Bottom Layer 

500

Landslides and rockfalls are caused by this force of erosion that reshapes mountain slopes and creates new hills.

Gravity

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