Test your knowledge of Earth's structure and geological processes in this Geology Practice Exam. It covers topics from the distribution of natural resources to the layers of the Earth, offering insights into both historical and physical aspects of geology.
All the above
why continents and oceans are different
Why a landscape looks the way it does
How life in the past was different than today
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Oceanic crust
Upper mantle
Lower mantle
Outer core
Inner core
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Whether it is part of the lithosphere
Elevation
Density of the crust
Thickness of the crust
Composition of the crust
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Heat trapped when the Earth was formed
Solar radiation trapped in the rock on the Earth's surface
Heat produced by air as it moves across the oceans
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Relative age
Absolute age
Numerical age
Radiometric age
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A rock can contain more than one mineral
A mineral is composed of chemical elements
A single rock can include more than one mineral
All the above
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Minerals
Crystals
Sand
Glass
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There are no planes along which the mineral can break
Cubes are the most common way two tetrahedron can join
Of the arrangement of atoms in crystal lattice
Halite is soluble in water
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The mineral will fracture in an irregular pattern
The mineral will not break
The mineral will fracture evenly along predictable planes
The mineral will still cleave but it will only occur along one plane
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The rock cooled slowly and then quickly
There was water in magma
The rock broke as it flowed
The rock cooled slowly
The ash and pumice became compacted
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Porphyritic
Pegmatite
Aphanitic
Glassy
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A shield volcano
Composite volcano
A caldera
A scoria cone
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Calderas
Fissures
Cones
Domes
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The more explosive an eruption it is likely to produce
The more likely a volcanic dome is to form
The longer the lava flows on an eruption will produce
The less explosive an eruption is likely to produce
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Rhyolite lava flows
Basalt lava flows
Andestite lave flows
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The low viscosity of basaltic magma allow it to flow downhill for long distances
They never erupt from the same plate twice
Their abundant ash layers spread out large distances
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Large amounts of rain and snowmelt mix with loose ash on steep slopes
Hot mud commonly erupts from their central craters
Such volcanoes form preferentailly in rainy tropical locations
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All of these are used to monitor volcano
Measuring tilting on he flanks of a volcano
Measuring changes in heat flow from satellites
Measuring seismic activity with seismic instruments
Measuring sulfur dioxide gas emissions
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All of the above
Deep rocks are exposed at the surface and yield young isotopic ages
Uplift can be measured with a gps
The top of Mount Everest contains a limestone with marine fossils
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The thickness of continental crust
The temperature of the crust
Whether the area is over a hot sport
Whether the crust is old or was formed more recently
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Isostasy
Superposition
Elastic rebound
Equanimity
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All of the above
Mantle upwellings
Continental collisions
Subduction zones
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Part of the continent have been added by the accretion of tectonic terranes
Large parts of the continent are subducted deep within the mantle
Older rocks have been uplifted and eroded away
Older rocks are commonly remelted over huge regions
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Continental collision
Continental rifting
Seafloor spreading
Transform faulting
Hot spot activity
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Continental rifting following by seafloor spreading
A continental collision
Subduction of Africa beneath Arabia
Subduction of Arabia beneath Africa
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All of these
The distribution of glacial deposits and directions of glacial scratch marks
The distribution of fossils
The shape of the continents
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Diverge
Collide
Subduct
Slide past one another
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Subduction
Transformation
Convergence
Divergence
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Centimeters per year
Meters per year
Kilometers per year
Hundreds of kilometers per year
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Movement of iron and electrical currents within Earth's outer core
Convection currents in the asthenosphere
Salty water moving through the deep parts of the crust
Aligned magnetic minerals within Earth's inner core
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Use the different in time it takes for seismic waves to reach three or more stations
All of the above
Use gps measurements of how the land move
Measure the amplitude of surface waves in a single station
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The magnitide
The richer scale
The depth of the focus
The amount of shaking
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All of the above
Trigger landslides
Generate a tsunami
Cause rigid buildings to collapse
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High population densities
Substandard construction practices or poor regulation
Building on solid rock
Building on loose sediment
Building on a water front
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These are all reasons the US has varying risks of seismic activity
Volcanic activity can cause seismic risk in some areas
Some regions in the continetal interior have active fault systems
Some areas are near plate boundaries, while others are not
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Brittle deformation
Ductile behavior
Growth of new minerals
Metamorphism
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Compression, Tension and Shear
Confining stress, deformation and folding
Convergence, divergence and transform faulting
Positive, negative and neutral
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Compression
Tension
Confining pressure
Fluid pressure
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Right before an earthquake
Right after an earthquake
Several weeks or months after a earthquake
None
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Sediment and sedimentary rocks
Sediment and igneous rocks
Sediment and metamorphic rocks
Mainly igneous rocks with some soil
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Physical and chemical weathering
Subduction and melting
Transportation and deposition
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Loose sediment hardens into sedimentary rock
Loose sediment breaks off of sedimentary rocks
Sediment settles from the water column
None
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The processes and sediment of stream and rivers
The movement of fluids underground
The hydrological cycle
None
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Closely spaced fractures
A soluble chemical composition
A quartz-rich rock
A rock composed of abundant loose pieces
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Some parts that are reddish a wide range in the size of clasts
Some angular and some rounded clasts
Mostly sand
A great variety of rock types as clasts
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All of these
Agents of transport
Strength of current
Sediment supply
Steepness of slope
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Weathering of rocks releases chemical elements that make the oceans salty
Salt deposits that formed early in earth history become dissolved by modern oceans
The early oceans were salty from dirt and debris on incoming comets
Blowing salt crystals become incorporated into clouds and falls with the rainfall
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Soil and other weathering products tend to accumulate more on gentle slopes than on steep slopes
Weather a slope faces toward or away from the sun is not important factor influencing weathering.
Time is not a critical factor in weathering because physical and chemical processes have not changed much through time.
Chemical weathering occurs fastest in cold or dry climates
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