Our Globe
Make It Move
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Rock On
100

Is the International Date Line is this kind of line on the globe.

Longitudinal

100
These two plates meet along the Western coastline of the United States and Canada.

The Pacific Plate and the North American Plate

100

This happens to the tension on rocks after an earthquake.

It is decreased

100

Magma when it reaches the surface of the earth.

Lava

100

Crystalline structures that are found in nature

Minerals

200

This part of the Earth does NOT have four seasons.

Near the Equator

200

This is happening in the Mid-Atlantic Ridge... (subduction or seafloor spreading)

Seafloor spreading

200

These play a big role in whether buildings stand in an earthquake.

engineering design and materials used to build

200

The measurement scale used to detect earth tremors.

The Richter Scale

200

These have flat faces and a definite shape that rocks do not.

Crystals

300

This is the layer of the Earth found directly beneath the crust.

Mantle

300

This happens often along the San Andreas Fault.

Earthquakes

300

This is where earthquakes are most prone to occur.

Along fault lines.

300

The year the Island of Surtsey first appeared.

1963

300

These are the minerals found in granite (defined as a rock)

Quartz, Mica, and Feldspar

400

The earth's crust is the thicker here than in the ocean.

Under Land

400

The Himalayan Mountains are thought to have formed when two crustal plates did what?

Collided into one another.

400

Along this famous connected line of faults there are many volcanoes and earthquakes.

Ring of Fire

400

Rocks that cool and harden from hot magma BELOW the surface of the earth.

Intrusive Rocks

400

The two conditions generally necessary in order to form metamorphic rocks.

Heat and Pressure

500

These may cause the earths' crust to slowly move and play a role in producing the earth's magnetic field.

Convection - type currents

500

This may have been the original land mass.

Pangaea

500

According to this, rocks break loose from a position of tension and surge forward.

The Elastic Rebound Theory

500

Dikes and sills are both examples of these kinds of rocks.

Intrusive Rocks

500

These are the three main groups of rocks - igneous, sedimentary, and _____

metamorphic