Here we are with "The Perfect Practice Test For Geology Exams Part- II." Geology is a significant part of our daily lives. This course is the study of the Earth and everything that makes up the planet. The questions in the quiz below cover everything you should have at the tip of your fingers concerning Geology.
Streak
Cleavage
Cracking luster
Habit
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Sulfides
Uranides
Native metals
Silicates
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Basalt
Peridotite
Iron-Nickel alloy
Granite
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By the weathering of pre-existing rocks
By changes in mineral composition
At great depth within Earth
By crystallization of molten rock
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Inner core, crust, mantle, hydrosphere
Core, crust, mantle, hydrosphere
Inner core, outer core, mantle, crust
Core, inner mantle, outer mantle, crust
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Materials that always contain fossils
Static in their nature, meaning once they become an igneous rock, they will always be an igneous rock
Native always lain down horizontally and with the oldest on the bottom
Aggregates of one or more minerals
Materials that always behave in a brittle manner
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The collection of scientific facts through observation and measurement
The assumption of conclusions without prior experimentation or observation
The development of one or more working hypotheses or models to explain facts
The development of observations and experiments to test the hypotheses
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Along the margins of continents
In the interior regions of continents
Scattered throughout continents
Along only the eastern margins of continents
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It has a specific and predictable chemical composition
It has a specific internal crystal structure
It can be liquid or solid
It can be identified by its characteristic physical properties
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The seafloor spreads and magma rises up to fill the gap, forming underwater features like oceanic ridges and submarine volcanoes
The seafloor rises up and heats up the surrounding water to cause tsunamis
A gap is created and sea water rushes in to cool the magma in the trench
There are huge mountains formed by the plates colliding
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Iron, silicon
Silicon, sodium
oxygen, carbon
silicon, oxygen
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Law of superposition
Theory of superstition
Theory of correlative deposition
Law of original correlation
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Physical geology is the study of fossils and sequences of rock strata; historical geology is the study of how rocks and minerals were used in the past.
Historical geology involves the study of rock strata, fossils, and geologic events, utilizing geologic time scale as a reference; physical geology includes the study of how rocks form and of how erosion shapes the land surface.
Physical geology involves the study of rock strata, fossils, and deposition in relation to plate movements in the geologic past; historical geology charts how and where the plates were moving in the past.
None of the above—physical geology and historical geology are essentially the same.
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Luster
Cleavage
Streak
Hardness
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Isotropy
Isobration
Isostasy
Isomonism
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Principle of fossil succession
Principle of cross correlation
Law of correlative indexing
Law of fossil regression
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Stratovolcanoes associated with subduction and a convergent plate boundary.
Shield volcanoes fed by a long-lived hot spot below the Pacific lithospheric plate
Shield volcanoes associated with a mid-Pacific ridge and spreading center.
Stratovolcanoes associated with a mid-Pacific transform fault
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Stratovolcanoes on the edge of a plate and shield volcanoes on the adjacent plate
Two, converging, oceanic plates meeting head-on and piling up into a mid-ocean ridge
A divergent boundary where the continental plate changes to an oceanic plate
a deep, vertical fault along which two plates slide past one another in opposite directions
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A strike-slip fault that forms the boundary between tectonic plates
A dip-slip fault connecting an anticline with a syncline
The rift bounding faults on a mid-ocean ridge
A reverse fault that steepens into a thrust fault
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The Sun
Heat from Earth’s interior
Both A and B
None of the above
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magma welt
Basalt spout
Melt well
Hot spot
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Subduction zones along convergent plate boundaries
transform fault zones along divergent plate boundaries
rift zones along mid-ocean ridges
Sites of long-lived, hot spot volcanism in the ocean basins
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A rock has an orderly, repetitive, geometrical, internal arrangement of minerals; a mineral is a lithified or consolidated aggregate of rocks.
A mineral consists of its constituent atoms arranged in a geometrically repetitive structure; in a rock the atoms are 03.01 Which of the following best defines a mineral and a rock? rock, randomly bonded without any geometric pattern.
In a mineral the constituent atoms are bonded in a regular, repetitive, internal structure; a rock is a lithified or consolidated aggregate of different mineral grains.
A rock consists of atoms bonded in a regular, geometrically predictable arrangement; a mineral is a consolidated aggregate of different rock particles.
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Carbon
Chlorine
Oxygen
Sodium
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Granopteris
Monastarious
Glossopteris
Mesosaurus
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Isotopes
Ions
Isochrons
Periodic elements
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Drill holes
Examination of deep mine shafts
Seismic waves
Volcanic eruptions
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He failed to provide a mechanism
He didn’t know about earthquake distribution at the time
He used ferns and fossil plants as part of his evidence
He used the shelves instead of the continent margin themselves
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Horizontally directed; compressive stresses
Horizontally directed; extensional stresses
Vertically directed; extensional or stretching stresses
Vertically directed; compressional stresses
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A rocky layer composed mainly of crustal rocks
A rocky layer having a relatively uniform chemical composition
A rigid layer of crustal and mantle material
A plastic layer composed mainly of mantle material
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Within the crust
Between the mantle and outer core
Within the outer core
In the upper mantle
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Strata with fossils are generally deposited on strata with no fossils.
Older strata generally are deposited on younger strata without intervening, intermediate age strata.
Older fossils in younger strata indicate a locally inverted geologic time scale.
Any sedimentary deposit accumulates on older rock or sediment layers.
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James Ussher
Alfred Wegener
Charles Lyell
James Hutton
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Divergent boundaries by submarine eruptions and intrusions of rhyolitic magma
Convergent boundaries by submarine eruptions and intrusions of rhyolitic magma
Divergent boundaries by submarine eruptions and intrusions of basaltic magma
Convergent boundaries by submarine eruptions and intrusions of basaltic magma
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Generalization
Hypothesis
Theory
Law
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Rising material in the seafloor and ocean basin causes the seafloor to spread laterally away from continents.
Sinking material in the mantle causes seafloor to diverge at the edges of continents
Rising material in the mantle spreads laterally carrying the seafloor away from seafloor ridges in the center of the ocean basin.
Sinking material in the mantle spreads laterally, forcing seafloor into continents at the edges of ocean basins.
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A basaltic shield volcano
An explosive stratovolcano
A small, welded tuff cone
A basaltic cinder cone
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Dike
Sill
Laccolith
Pluton
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Electrons in the valence bond level
Neutrons in the outer nuclear shell
Electrons in the nucleus
Proton in the nucleus
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Accretionary-wedge complex
Continental shelf, terrain complex
Mass movement complex
Subterranean-accumulation complex
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Lithified loess (wind-blown) deposits in the deserts of Chile, Australia, and Africa
Tillites (rocks formed by glaciers) in South Africa and South America
thick sediments in the Amazon and Congo deltas of South America and Africa
Cold water fossils in the deep-water sediments of the South Atlantic abyssal plain
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Stick slip
Oblique slip
Dip slip
Strike slip
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Northern movement of Baja California and a sliver of western California toward the Hawaiian Islands.
Northward movement of India into Eurasia
Westward movement of the South American plate over the Nazca plate.
Arabian peninsula slamming into North Africa under the Red Sea
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The atoms have different numbers of electrons but the same number of neutrons
The atoms have different numbers of neutrons and the same number of protons.
The atoms have the same number of electrons and different numbers of protons
The atoms have different numbers of protons and the same number of neutrons
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Layers in sandstone found at the top of a mountain that are similar to layers at a sandy beach illustrate that the sandstone used to be sand at sea level some time ago
Sand rolling along a stream bottom shows that sediment is moving downstream
Along a coastline, wave-cut erosional features now well above sea level indicate that the land was uplifted
Layers in sand that compose a modern beach today that are similar to layers in sandstone formed millions of years ago illustrate that there have been similar beaches in Earth’s past
An erupting volcano proves that burning subterranean coal beds provide the heat
India
South America
Australia
Antarctica
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Zone in the upper mantle that deforms by plastic flowage
Cool, rigid layer of crust and upper mantle that forms the tectonic plates
Deforms mainly by brittle fracturing and faulting
Partial melting of rising granitic plumes produces huge volumes of basaltic magma
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Convergent boundary on a volcanic arc above a northward-subducting Pacific plate
Transform boundary where North America has moved towards Alaska
Divergent boundary where shield volcanoes are forming
Convergent, continental margin with uplifted fault blocks, much like those of the Basin and Range Province
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