science grade 8

Froggy Jumps

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geologic time

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Heba Mongy

Egypt

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science grade 8


Froggy Jumps science grade 8Version en ligne geologic time par Heba Mongy 1 who proposed the principle of uniformitarianism? a charles darwin b albert einstein c james hutton 2 fossils of simple organisms are usually found in : a the youngest rock layers b the oldest rock layers c only volcanic rocks 3 which of the following events marks a mass extinction ? a a single species disappears slowly b many species die out in a short period of time c all fossils become complex at once 4 which process does not cause gaps in the rock record ? a weathering b erosion c deposition 5 which of the following is not a type of unconformity? a angular unconformity b disconformity c lithoconformity 6 which principle states that the oldest rock layers are at the bottom and youngest at the top a lateral continuity b superposition c cross-cutting 7 geologists fill in missing parts of the rock record mainly by a digging deeper holes b looking only at rock colors c correlating rock layers and fossils from different places 8 weathering and erosion can cause gaps in the rock record a true b false c 9 a complete rock record can always be found in one place a true b false c 10 fossils are not useful in matching rock layers between distant locations a true b false c

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science grade 8

Froggy Jumps

À propos de cette activité

Créé par

Téléchargez la version pour jouer sur papier

Top Jeux

Froggy Jumps

pizza

Froggy Jumps

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Froggy Jumps

science grade 8Version en ligne

par Heba Mongy

who proposed the principle of uniformitarianism?

fossils of simple organisms are usually found in :

which of the following events marks a mass extinction ?

which process does not cause gaps in the rock record ?

which of the following is not a type of unconformity?

which principle states that the oldest rock layers are at the bottom and youngest at the top

geologists fill in missing parts of the rock record mainly by

weathering and erosion can cause gaps in the rock record

a complete rock record can always be found in one place

fossils are not useful in matching rock layers between distant locations