This is probably the hardest geology test! The earth is an exciting place in our solar system, and through geology, we understand some of the rocks, minerals, volcanoes, and even shifts with the earth’s rocks. Do you think you can pass what has come to be known as the most challenging geology quiz? Take it up and get to share See morethe score you get to see if you do understand the geology.
Hydrocarbons
Carbohydrates
Pure forms of carbon
Carbonate minerals
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Gas, because it is more stable at high temperatures
Oil, because it is more stable at low pressures
Oil, because it is more stable at high temperatures
Gas, because it is more stable at low pressures
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Either a source or reservoir rock
A seal rock
A reservoir rock
A source rock
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200 to 350 °C
100 to 250 °C
90 to 160 °C
30 to 60 °C
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Shields
domes
Basins
Active margins
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The most common of the naturally occurring isotopes of that element
Rare even in uranium oxide deposits, and thus usable reactor fuel must be enriched with respect to this isotope
Heavier than the other well-known isotope of uranium
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Bronze
Copper
Gold
Iron
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Thick basinal sandstones and shales
Blueschists
Evaporite sequences
Igneous rocks
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Residual mineral deposits
Hydrothermal deposits
Placer deposits
Sedimentary deposits
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Aluminum oxides
iron oxides
Copper sulfides
Copper oxides
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Nonmetallic minerals only
Iron and aluminum ores
Base metals only
No mineral resources are renewable
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True
False
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True
False
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Thrust
Reverse
Normal
Abnormal
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20 km beneath New Madrid
20 km south of New Madrid
200 km beneath New Madrid
In New Madrid ("hypocenter" and "epicenter" mean precisely the same thing)
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Surface waves
Interior waves
R-waves
Body waves
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Produce most of the damage to buildings during earthquakes
Travel more rapidly than body waves
Are the first waves initially produced in an earthquake
Are the first waves to arrive at a seismograph station after an earthquake
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Seismic gap
Wadati-Benioff zone
Trench
Wegener belt
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Is based on past earthquake activity
Works on the principle that zones of past seismicity will be active in the future
Includes the notion of seismic gaps—places where an earthquake is “overdue”
All of the above
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New Madrid
Los Angeles
Tokyo
Mexico City
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The influence of abrupt changes in density associated with major contrasts in rock type at depth
The arcuate nature of trenches at subduction zones, where most earthquakes are generated
The spheroidal nature of the Earth itself
Gradual changes in density with depth beneath the surface
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a high-velocity zone for seismic waves traveling in the outer core
A P-wave "shadow" zone for seismometers situated between 104° and 140° from earthquake hypocenters
A low-velocity zone (LVZ) at a depth of 200 km where about 2% of the rock may be melted
A S-wave "shadow" zone for seismometers situated on the far side of the Earth from earthquake hypocenters
Both D and B
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A concept in existential philosophy.
Change in the chemical composition of a rock.
Moving toward the middle.
Change.
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The original minerals are recrystallized in the solid state, and they are sometimes replaced by a new set of minerals.
They always develop a strong foliation.
They always melt and then recrystallize upon cooling.
They always turn green, which is why they are called greenschists.
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Is made up primarily of quartz.
Most commonly forms in contact metamorphic environments.
Has platty mineral grains (like micas) aligned parallel to each other, causing the rock to break into flat slabs.
Is most likely to form in response to falling temperature and pressure.
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Amphibolite : greenschist : blueschist
Marble : greenschist : quartzite
Granite : gabbro : phyllite
Greenschist : amphibolite
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Blueschist : greenschist : amphibolite cooler → hotter
Slate : phyllite : schist : gneiss cooler → hotter
Gneiss : schist : phyllite : slate cooler → hotter
Lapilli : lahar :tuff : ignimbrite cooler → hotter
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Limestone
Ignimbrite
Basalt
Shale
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Sediments on a subducting slab are heated and deformed.
Basalt is erupted under seawater.
Magma is emplaced adjacent to relatively cool sedimentary rocks.
Magma is emplaced into very deeply buried and already-hot igneous rocks.
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Hot spots.
Himalayan-type orogens.
Subduction zones.
Mid-ocean ridges.
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Gneisses have more feldspar and less mica than schists.
Gneisses form from sedimentary rocks and schists form from igneous rocks.
Gneisses are generally older than schists.
Gneisses form in subduction zones and schists form in batholiths.
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Occurs when seawater reacts with hot seafloor rocks.
Generates metamorphic rocks that usually lack foliation.
occurs mainly at or near mid-ocean ridges and transform faults.
All of the above.
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Deposition
Erosion
Weathering
Sedimentation
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Deposition
Physical weathering
Chemical weathering
Erosion
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Chemical weathering
Physical weathering
Erosion
Deposition
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Physical weathering breaks boulders directly into spherical cobbles and pebbles
Chemical weathering attacks corners and edges of rock more rapidly than its interior
Physical weathering predominates and there is little chemical weathering
Chemical weathering works at a uniform rate throughout the rock
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Temperate forests
Deserts
Grasslands
Tropical rain forests
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Deserts
Grasslands
Temperate forests
Tropical rain forests
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Be well sorted
Have angular grains
Include coarse grains, such as cobbles
Include fine grains, such as clay
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Water
Wind
ice
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Velocity of the water at the moment the sediment settled to the bottom
Geographic extent of the weathering source rock at outcrop
average velocity of the water from the time of erosion until deposition
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Possesses more angular grains than breccia
Is finer grained than breccia
Possesses more rounded grains than breccia
Is coarser grained than breccia
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Volcanoclastic debris
Lava flows
Volcanoes
Pele's hair
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Pyroclastic blocks that acquire aerodynamic shapes during flight out of the volcanic vent
Explosive bodies of lava with high volatile content
Cinders that explode upon impact with the ground
Used in highly hazardous volcanoes to mitigate volcanic hazards via small controlled eruptions
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Normal mid-ocean ridge activity
A submarine hot-spot located along a mid-ocean ridge
A submarine hot-spot located within the interior of a plate
Subduction of an oceanic plate underneath the continental Eurasian Plate
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Great Smoky Mountains
Carlsbad Caverns
Acadia
Yellowstone
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Mars / shield
Io (a moon of Jupiter) / shield
Mars / cinder cone
Venus / stratovolcano
Earth / shield
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The viscosity of the lava
The composition of the lava
The proportion of volatiles within the lava
All of the above
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