Continental Drift
Earth Layers
Plate Boundaries
Convergent Zones
Proof & Power
100

Wegener's continental drift was rejected because this energy is too weak to move continents

Tidal energy

100

The asthenosphere is composed of rock akin to this

Play Doh

100

Scarring due to movement along a transform plate boundary

Fracture zone

100

Oceanic-oceanic convergence creates these volcanic features

Volcanic island arc

100

Chain of volcanic structures formed as plates move over a hot spot

Hot spot track

200

This fossil reptile (and geological records) match across separated continents

Mesosaurus

200

Unlike continental drift, plate tectonics include movement of these plates

Oceanic plates

200

Divergent plate boundaries are known as these systems in the ocean

Oceanic ridge system

200

Addition of hot water from wet, subducted material generates this melting, creating volcanoes

Partial melting

200

Subduction force moving the plate

Slab pull

300

These two continents seem to fit well together like puzzle pieces

Africa and South America

300

These are irregular segments of the lithosphere in motion

Lithospheric plates

300

Type of plate boundary where two plates move past one another

Transform

300

Continental-continental convergence pushes plates up to form these

Tall mountains

300

Deep ocean drilling verified this at divergent boundaries

Seafloor spreading

400

The continents once existed as a single landmass, a supercontinent named this, which drifted apart

Pangaea

400

Located beneath the lithosphere and composed of malleable rock

Asthenosphere

400

Type of plate boundary where two plates move towards each other

Convergent

400

Oceanic-continental convergence creates these on continents

Continental volcanic arc

400

What sort of stripes radiate from a spreading center?

Magnetic reversal stripes

500

This German scientist (1880-1930) was first to propose the theory of continental drift

Alfred Wegener

500

The crust and upper mantle constitute this rigid layer

Lithosphere

500

Type of plate boundary where two plates move apart

Divergent
500

Depressions formed where one plate subducts another at convergent boundaries

Deep-ocean trench

500

Plates move over these stationary surface expressions of mantle plumes

Hot spot