Explore key concepts of Earth's structure and history with this quiz. Topics include the scientific method, plate tectonics, geologic time, and the principles of radiometric dating. Understand the age of Earth and the fundamentals of fossil formation through observation-based questions.
Absolute age
Plate tectonics
Divergent boundaries
Radioactivity
Natural selection
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Relative age dating
Absolute age dating
Deformation of the asthenosphere
Formation of the lithosphere
Organic evolution
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Divergent
Lithospheric
Convergent
Organic
Transform
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4,600,000 years
5.5 million years
150,000 to 300,000 years
4.6 billion years
704 million years
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Particles that are expelled
Daughter atoms
Rock outcrops in Canada
Divergent boundaries
Natural selection
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Have formed only days ago
Be at the age corresponding to the second half-life
Have passed the age of the second half-life
Be at the age corresponding to the first half-life
Be worthless for age dating
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Uniformitarianism
Actualism
Catastrophism
Principle of original lateral continuity
Natural Selection
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Principle of Unconformity
Principle of Superposition
Principle of Original Horizontality
Principle of Original Lateral Continuity
Principle of Intrusive Relationships
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A layered sandstone
A fossiliferous limestone
A fossiliferous shale
A gneiss rock that extremely altered through contact metamorphism
A basaltic rock cooled from a volcano
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Seconds, minutes, hours and days
Days, hours, minutes and seconds
Seconds, hours, minutes and days
Months, days, years and hours
Hours, minutes, days and months
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On the platform of the craton.
On the shield of the craton.
In an orogenic belt.
On the ocean shelf.
On the abyssal plain.
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Less than 1.
More than 3.
Between 1 and 2.
Between 2 and 3.
Can't be determined.
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Pleistocene Epoch
Silurian System
Cambrian Period
Cenozoic Era
Phanerozoic Eon
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Depositional environment
Orogenic belt
Continental shelf
Craton
Continental platform
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Glacial lake
River channel
Continental shelf
Wind-blown dune
Alluvial fan
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Lake
Delta
Alluvial fan
Deep marine
Wind-blown dune
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Chronostratigraphic units
Fining upward successions
Onlap and offlap sequences
Transgressions and regressions
Biofacies and lithofacies
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Shale over sandstone
Limestone over conglomerate
Sandstone over conglomerate
Sandstone over shale
Shale over conglomerate
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Facies
Member
Group
Formation
Time-rock unit
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Reworked fossils
Haploid
Index fossils
Trace fossils
Unaltered fossils
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Extinction rate
Geologic time
Geologic range
Rate of evolution
Relative geologic age
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Paleomagnetism
Tillites
Evaporites
Coal seams
Annual rings
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Strike-slip
Normal
Thrust
Transform
Oblique
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Lateral faults
Subduction zone
Hot spots
Midoceanic ridge
Continental rifting
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Continental-continental crustal convergence
Oceanic-oceanic crustal convergence
Transform boundaries
Divergent boundaries in oceans
Divergent boundaries under continents
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Basin
Monocline
Syncline
Dome
Anticline
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Reverse
Normal
Right lateral
Left lateral
Transform
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Fossilized imprints of soft-bodied animals or plants
Segmented worms that existed during the late Precambrian
Fossilized tracks, trails, burrows and nests made by ancient animals
Small bits or remnants of the hard body parts of ancient marine animals
The thin layer of carbon left behind from plant material
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Rapid burial by sediments or extrusive materials
Hard parts such as bones, teeth and shells
Presence of oxygen-tolerant bacteria
Burial in a low-oxygen environment
Having a metamorphic rock nearby
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When depositional environments migrate laterally, sediments of one environment come to lie on top of sediments of an adjacent environment
When depositional environments migrate laterally, sediments of one environment do not come in contact with sediments of an adjacent environment
The present is the key to the past
Sediments from one depositional environment are not similar to sediments of another adjacent environment
Small streams meet to form larger streams, which in turn flow into still larger rivers
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Replacement
Carbonization
Permineralization
Mold making
Cast making
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Range zone
Assemblage zone
Concurrent range zone
Stage
Series
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Replacement
Molds and casts
Permineralization
Petrifaction
Carbonization
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The relative scale of geologic time is based on superposition and fossil succession, whereas radiometric dating provides an absolute scale in which events are measured in years.
The relative scale of geologic time is based on absolute scale in which events are measured in years, whereas absolute dating provides superposition and fossil succession.
The relative scale of geologic time is based on sedimentary archives, whereas absolute dating provides a final comparison between two geological entities.
The relative scale of geologic time is based on event stratigraphy and marker beds, whereas absolute dating provides a numeric scale in which events are measured by isotopes and fossils.
There is no difference between the relative scale and the absolute scale of geologic time.
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