Salt dome
Anticline
Fault trap
All of the above
North American Cordillera
Himalayas
Appalacians
Alps
5
1
10
32
13.7 billion
3.6 billion
542 million
4.6 billion
300km
700km
1,000km
500km
Atomic structure
Mass number
Atomic number
Atomic strata
Deposition
Erosion
Isostasy
Gravitational collapse
Terrane
Crust
Continent
Phaneritic
Porphyritic
Pyroclastic
Aphanitic
Opposite, normal
Reverse, regular
Normal, reverse
Normal, opposite
Rill
Mouth
Divide
Pothole
Ground shaking, total energy released
Total energy released, ground shaking
Intensity, ground shaking
Ground shaking, intensity
Abyssal plain
Continental margin
Deep-ocean basin
Mid-ocean ridges
The lithosphere glides on its weak zone
It is the graveyard of subducted lithosphere
Magma from the D layer rises to the surface
The “D” layer plays a major role in transform faults
Above the water table
Below the water table
Underwater
In outer space
The Himalayas
Basin and Ridge Province
Japan
San Andreas
Earthquakes occur
Rocks spring back into their original position
Faults rupture
Foreshocks occur
Minerology
Texture
Chemical composition
All of the above
Continental
Marine
Transitional
All of the above
Examine the materials composing the Earth
Understand the many processes that operate beneath and upon Earth’s surface
Understand the origin of Earth and its development through time
Study plate tectonics
Asthenosphere
Lithosphere
Transition zone
Mantle
It is not a solid
It lacks a well-defined chemical composition
It is organic
It lacks a repetitive atomic structure
Pahoehoe
Aa
Lava tubes
Pillow lava
Physical
Chemical
Mass wasting
Erosion
Sun spots
Surface warming
CO2 levels rising
Increased aerosols
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