Planet Earth
How scientists know
Earth's crust
fossils
What else changes the earth's surface
100

Outer most layer of Earth

Crust

100

Another name for deep valleys 

trenches

100

plates collide or rub alongside


How are earthquakes caused

100

entire (whole) animals have been found preserved-even the soft tissues.

Original Remains

100

the movement of rock and minerals from one place to another

erosion

200

Inner most layer of earth

Inner core

200

another name for mountain chains

ridges

200

Explain how volcanoes are formed.

subduction when plates push together or pulling apart

200

Ancient (very old) worm holes, burrows and footprints are sometimes found that have been preserved over time.

Trace Fossils

200

the wearing away and physical breakdown of rocks

mechanical weathering

300

Layer under the crust

Mantle

300

These are found along narrow strips of land

Earthquakes and volcanoes

300

Explain how mountains are formed

plates push together or rub alongside

300

Sometimes dead organisms become covered with layers of sediment

Carbon Fossils

300

when particles of rock that have been eroded away from one place begin to collect or build up in another place

sedimentation

400

Layer beside inner core

Outer core

400

large areas have few or none of these

volcanoes

400

describe theory of sea floor spreading

scientists believe that new surface rock is being formed at the ocean ridges.

400

Over time, water dissolves the calcium in the bones of dead bodies and leaves silica behind.

Petrified Fossils

400

when rock is changed by chemical reactions

chemical weathering

500

pressure and consistency of inner core

increased pressure and rock is solid and hard

500

This moves very slowly away from ridges and towards the trenches

ocean floor

500

Describe the theory of continental drift

Scientists believe that the continents used to be connected and have drifted apart over time and continue to drift slowly.

500

Describe the geologic time scale

A set of dates based on the finding of simple and complex fossils that allows Earth's history to be broken into time periods. A theory from this is that organisms began as simple creatures and evolved to become more complex organisms. 

500

when rock is changed and broken down by the plants and animals living in or on it.

Biological weathering