Near the continents
At the mid-ocean ridges
Far from the mid-ocean ridges
Near Asia
Lithosphere
Asthenosphere
Core
Continents
Century
Decade
Day
Year
Crust
Asthenosphere
Core
Atmosphere
Alps
Rockies
Himalaya
Appalachian
Fossils
Rock structures
Fossils and rock structures
Convergent
Stable
Divergent
Transform
Glomar
Glossopteris
Pangaea
Wegener
Subduction zones
Transform Boundaries
Convection Currents
Divergent Boundaries
Divergent Boundary
Convergent Boundary
Transform Boundary
Lithosphere
New material is being added to the asthenosphere
Earthquakes break apart the ocean floor
Sediments accumulate at the area of spreading
Molten material beneath Earth's crust rises to the surface
Very Little
Slowly
Quickly
200 Million
300 Million
400 Million
500 Million
Mesosaurus
Glossopteris
Reversed itself in the past
Weakened
Become stronger
Retained the same
Seismometer
Magnetometer
Geologist's Compass
Vertical
Convection
Horizontal
None of the answers are correct
Density
Magnetism
Stop inside the
Cool the
Sink Back Into
Warm
Transform Boundary
Divergent Boundary
Convergent Boundary
Convergent Boundary
Divergent Boundary
Hot Spot
Transforming Boundary
Transform Boundaries
Convergent continental-continental boundaries
The center of continents
Convergent oceanic-continental boundaries
Volcanoes
Strike-Slip faults
Mountain Ranges
Rift Valleys
Appalachian Mountains
Himalaya
Mid-ocean Ridge
San Andreas Fault
Rift Valley
Subduction Zone
Transform Boundary
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