Explore key geologic concepts with the 'Leaven Plate Tectonics Geologic Time And Fossils' quiz. This assessment covers observations, half-life, plate tectonics, Earth's age, and radioactive decay processes, enhancing understanding of Earth's structure and geological timeline.
Glacial lake
River channel
Continental shelf
Wind-blown dune
Alluvial fan
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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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Reworked fossils
Haploid
Index fossils
Trace fossils
Unaltered fossils
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Particles that are expelled
Daughter atoms
Rock outcrops in Canada
Divergent boundaries
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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Lateral faults
Subduction zone
Hot spots
Midoceanic ridge
Continental rifting
Replacement
Carbonization
Permineralization
Mold making
Cast making
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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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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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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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Continental-continental crustal convergence
Oceanic-oceanic crustal convergence
Transform boundaries
Divergent boundaries in oceans
Divergent boundaries under continents
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Unproven beliefs
A hypothesis
A question
Scientific laws
Observations
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