Practice for Geology Exam 3
Iron in Earth's core
Water stored in the oceans
Increasing pressures increase the density of mantle rocks at depth
The larger circumference of Earth at the equator relative to the poles means that the highest density occurs at zero degrees latitude
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Heat is transferred from Earth's interior towards the surface mainly by radiation.
Heat is transferred from Earth's interior towards the surface mainly by conduction.
Heat flow, as measured on Earth's surface, is higher along mid-ocean ridges and other volcanically active regions but lower within the interiors of stable continents.
Heat flow, as measured on Earth's surface, is the same everywhere.
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Site A
Site B
Site C
Site D
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Surface waves
P-waves
S-waves
Refracted waves
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Refraction
Reflection
Diffraction
Deflection
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Temperature
Type
Velocity
Magnitude
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Asthenosphere/mesosphere
Mesosphere/outer core
Outer core/inner core
Crust/upper mantle
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S-waves change into P-waves
S-waves slow down because of the presence of a few percent partial melt
S-waves cannot penetrate through the asthenosphere
S-waves speed up because of an increase in density of mantle rocks
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P- and S-waves are reflected back to the surface.
The two transition zones prevent P- and S-waves from reaching the lower mantle.
They slow down because mantle material is softened at these depths.
They speed up due to density increases in mantle rock resulting from phase changes in minerals.
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P-waves slow down while S-waves speed up when passing through the outer core.
Both P- and S-waves are prevented from passing through the outer core.
S-waves cannot pass through the outer core while P-waves slow down significantly when passing through this layer.
Both P- and S-waves increase in velocity when passing through the outer core.
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Peridotite
Andesite
Granite
Basalt
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Only P-waves are detected by seismometers.
Only P-waves are generated by earthquakes.
S-waves change into P-waves.
No P-waves are detected by seismometers.
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Heat flow
Magnetic field
Gravity
Rotation
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Minerals are mostly created through the activities of organisms.
Atoms within the crystal structure of a mineral are usually disorganized and randomly distributed.
The minerals quartz and halite are considered separate minerals because of differences in crystal sizes
A given mineral has a specific crystal structure and chemical composition.
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All silicate minerals have silicon and oxygen in their chemical formula.
Silicate tetrahedra can bond with cations but not with other tetrahedra.
The basic building block of all silicate minerals is the silicon-oxygen tetrahedron.
Silicate minerals are the most abundant minerals in Earth's crust.
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Mica
Pyroxene
Hematite
Plagioclase feldspar
Quartz
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Halides
Sulfates
Oxides
Silicates
Carbonates
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Native element minerals are all soft and easily scratched
Native element minerals only form ionic bonds
Native element minerals are bonded to sulfur
Native element minerals are comprised of only one element
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Mica and gold
Quartz and halite
Gypsum and anhydrite
Calcite and olivine
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Uplift and exposure
Lithification
Burial to greater depths
Increase the temperature
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Any rock type can be uplifted and exposed to weathering agents.
Sedimentary rocks can convert into metamorphic rocks if the temperature and pressure conditions are right.
Only igneous rocks can be uplifted and exposed to weathering.
Igneous rocks can bypass the weathering stage and convert directly into metamorphic rocks.
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An igneous pluton forms from lava that is extruded onto Earth's surface and cools quickly.
Lava erupted on Earth's surface cools very slowly when exposed to the atmosphere.
Magma crystallizing deep in the crust cools slowly and forms large crystals.
Fast cooling rates of magma produce large crystals.
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Batholith
Sill
Dike
Volcanic neck
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Only plutonic rocks with large crystals.
Explosive eruptions and volcanic ash.
Quiet eruptions and fluid lava.
Mild eruptions that crystallize into mafic igneous rocks only.
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Felsic
Intermediate
Ultramafic
Mafic
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Yields explosive eruptions
Has low silica content
Erupts volcanic ash
Is thick and sticky, thus retaining its gases
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Clay minerals
Rock fragments
Dissolved ions
Water
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Crystallize directly from water.
Are composed of particles of pre-existing rocks.
Include rock salt and limestone.
Are more likely than chemical sedimentary rocks to contain fossils of marine organisms.
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Mountain valley
Desert
Uplifted bedrock undergoing weathering and erosion
Continental shelf
Beach
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Particle sizes in breccia are smaller than those found in conglomerate.
Particles in breccia are angular, while particles in conglomerate are rounded.
Breccia is a detrital sedimentary rock whereas conglomerate is a chemical sedimentary rock.
Breccia contains fossils whereas conglomerate does not.
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Rock salt
Chert
Limestone
Rock gypsum
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Contact
Burial
Dynamic
Regional
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Deep within mountain ranges
Along fault planes
Within high pressure areas where fluids are absent
Near mid-ocean ridges
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Sandstone
Schist
Gneiss
Slate
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Reactions between rocks and hot magmatic fluids result in the formation of green, blocky minerals containing water in their crystal structures.
Minerals are platy and randomly oriented in different directions due to high temperature, low pressure metamorphism.
Alignment of platy minerals like micas in a common direction due to direct pressure during metamorphism.
Recrystallization of original minerals into large, equal-sized crystals that appear as granules in a metamorphic rock.
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Dynamic
Contact
Regional
Hydrothermal
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Quartzite
Marble
Mylonite
Schist
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Eurasia
Pangea
Gondwanaland
Euroamerica
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Assume randomness in the way glaciers move.
Assume that all ice flows originated in Australia.
Assemble these continents into a giant supercontinent.
Take into account changes in Earth's magnetic field over the last three hundred million years.
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Similar fossils of ancient plants and animals found on the five southern continents now separated by oceans.
Coal deposits in Antarctica.
Polar wander curves.
A cooling, shrinking Earth.
Reef-building corals in frozen Greenland.
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Sites of hydrothermal discharges on the seafloor known as black smokers.
Plate boundary where new oceanic lithosphere is created.
Lithospheric plates converge along mid-ocean ridges.
Sites of undersea volcanic activity
Long, undersea mountain ranges found in all the major ocean basins of the world.
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Even though Earth's magnetic polarity occasionally reverses, the direction of magnetic lines of force have always pointed towards the magnetic north pole.
Magnetic stripes in oceanic crust only reflect periods of normal magnetic polarity.
Magnetic stripes on the seafloor only exhibit normal polarity to the left of a mid-ocean ridge, and reverse polarity to the right of the ridge.
The Geomagnetic Time Scale indicates numerous reversals in Earth's magnetic field over the last 5 million years.
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Magnetic inclination and declination can be measured in some igneous rocks.
Magnetic declination today is a compass needle pointing to the magnetic north pole.
Polarity reversals in Earth's magnetic field only affect the magnetic inclination, but not the declination, of ancient rocks.
The magnetic inclination of a compass needle is zero degrees at the equator.
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Magnetization of ancient rocks point to various pole positions in the past that are artifacts of continental drift and not because poles actually migrated.
Earth's magnetic field was in the process of reversing over the past 500 million years.
Earth had two north magnetic poles in the past that eventually merged into one pole.
The magnetic north and south poles were at one time joined in the northern hemisphere, but have since drifted apart to their present locations.
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Oceanic crust becomes progressively older as we approach a mid-ocean ridge.
The ages of oceanic crust are truncated at convergent plate boundaries.
The youngest oceanic crust occurs along mid-ocean ridges.
The oldest oceanic crust within an ocean basin occurs along the margins of the basin and furthest from the mid-ocean ridge.
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Oceanic hot spot
Transform plate boundary
Mid-ocean ridge
Convergent plate boundary
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Crust only
Crust and solid upper portion of the mantle directly above the asthenosphere
Crust and asthenosphere
Oceanic lithosphere only
Continental lithosphere only
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Oceanic hot spot
Mid-ocean ridge
Transform fault
Subduction zone
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Boundary where oceanic crust is destroyed
Sites of plate collision and subduction
Only occurs where a continental plate meets an oceanic plate
Associated with volcanic arcs and mountain ranges
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Mantle plumes
Magnetic reversals
Mantle convection
Volcanoes and earthquakes
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