Rock Layers
Fossil Clues
Changing Landscapes
What Caused It?
Plate Tectonics
100

In undisturbed rock layers, this layer is the oldest.

bottom layer

100

Preserved remains or traces of ancient living things found in rock.

fossil 

100

The breaking of rock into smaller pieces by water, ice, wind, or acid.

weathering

100

Underground caves with marine fossils inside limestone were most likely formed by this process.

erosion by water

100

The slow movement of continents by moving tectonic plates.

continental drift

200

This rule says that lower undisturbed rock layers are older than layers above them.

Law of Superposition

200

Fossils of fish and marine crustaceans show that an area was once this environment.

underwater or an ocean environment

200

The movement of broken rock or soil to a new place.

erosion

200

An ocean basin may grow larger or smaller because of this slow movement of Earth’s crust.

plate movement or continental drift

200

The tool scientists use to measure extremely slow plate movement.

GPS

300

A crack or intrusion that cuts through other rock layers is this compared with those layers.

younger

300

When all members of a species die out, it is called this.

extinction

300

The dropping of eroded sediment in a new location.

deposition

300

A rock layer contains fossils below it but none above it, along with a thin ash layer. This most likely occurred.

volcanic eruption

300

When oceanic crust sinks beneath continental crust, this process occurs.

subduction

400

This type of dating compares whether rocks are older or younger without giving an exact age.

relative dating

400

A layer high in this element can be evidence of an asteroid impact.

iridium

400

A gradual sequence from shallow ocean to tidal zone to coastal plain shows this type of environmental change.

gradual change

400

Two continents collide, and neither crust sinks underneath the other. This creates this landform.

large mountain range

400

This collision forms the largest mountain ranges, such as the Himalayas.

continent-continent collision

500

This timeline organizes Earth’s past into eons, eras, periods, and epochs.

geologic time scale

500

Dinosaur fossils below an iridium-rich layer but not above it support this event.

an asteroid impact that caused extinction

500

An ash layer followed by missing fossils is evidence of this sudden event.

volcanic eruption

500

A mountain range that becomes shorter, rounder, and less steep over millions of years has been changed by these two processes.

weathering and erosion

500

Over millions of years, weathering and erosion make jagged mountains become this.

shorter, rounder, and less steep mountains

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