What do you know about the earth’s history? Would you be able to pass this quiz? This quiz will inquire about which layer of the planet is the coolest, when the Precambrian Eon began and ended, the group of fossils found together in only one layer of rock, and how old the earth is. Historically speaking, you should unearth a See morelot of information with this quiz. Good Luck.
Billion
Mega-Million
Trillion
Million
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Minerals in the ground replace the dead thing as it breaks down
Organisms are trapped in amber or asphalt, preserving their body.
Traces of living organisms are found, such as burrows or footprints.
All of the above
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Sediments are deposited as essentially horizontal layers
Inclusions are older than the rocks they are contained in
Sediments spread out in all directions when they are deposited
Undisturbed sedimentary layers get younger from bottom to top
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A gap in the geologic record
A sequence of deformed rocks
A sedimentary layer of variable thickness
A period of deposition
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Precambrian
Mesozoic
Paleozoic
Cenozoic
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4.6 bya-570mya
570 mya-250 mya
250 mya-65mya
65 mya-present day
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Level
Index
Main
Frequent
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4.6 bya - 570 mya
570 mya-250 mya
250 mya-65 mya
65 may-present day
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Epochs
Periods
Ages
Eons
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250 mya-65 mya
65 mya-present day
4.6 bya-570mya
570-mya-250mya
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Dinosaurs
Trilobites
Humans
Bacteria
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4,000 years old
4.6 mya
4.6 bya
4,600 bya
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70
80
90
60
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Eons
Eras
Ages
Epochs
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Ages, epochs, periods, eras, eon
Epochs, periods, ages, eras, eon
Eon, eras, periods, epochs, ages
Eras, eons, periods, epochs, ages
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125
225
325
425
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Cooled down
Warmed up
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Paleozoic
Precambrian
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Precambrian
Mesozoic
Cenozoic
Paleozoic
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Precambrian
Paleozoic
Mesozoic
Cenozoic
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Precambrian
Paleooic
Mesozoic
Cenozoic
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4.6 bya-570 mya
570 -250 mya
250-65 mya
65 mya-today
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Precambrian
Paleozoic
Mesozoic
Cenozoic
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Precambrian
Paleozoic
Mesozoic
Cenozoic
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4.6 bya-570 mya
570-250 mya
250-65 mya
65mya-today
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Precambrian
Paleozoic
Mesozoic
Cenozoic
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Precambrian
Paleozoic
Mesozoic
Cenozoic
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Precambrian
Paleozoic
Mesozoic
Cenozoic
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Precambrian
Paleozoic
Mesozoic
Cenozoic
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Alien attack
Appearance of earliest trilobites
Advance and retreat of the last continental ice sheet
Formation of Pangaea
Extinction of the dinosaurs
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The evolution of oxygen-producing organisms
The formation of the tectonic plates
The emergence of trilobites
The deposition of soil during sedimentary rock formation
Gravity
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Paleozoic
Cenozoic
Jurassic
Precambrian
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Layer A
Layer B
Layer C
Layer D
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Crust
Mantle
Inner Core
Outer Core
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