Rocks and Minerals Warmups

Rocks and Minerals Warmups

KG - University

38 Qs

quiz-placeholder

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Rocks and Minerals Warmups

Rocks and Minerals Warmups

Assessment

Quiz

Other Sciences

KG - University

Medium

Created by

Rebecca Lefkoff

Used 51+ times

FREE Resource

38 questions

Show all answers

1.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Ricardo has an igneous rock in his rock collection. Where did this rock most likely form?
in a volcano
on a forest floor
on a coral reef
at the bottom of a river

2.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Cleavage of a mineral is related to a mineral's
chemical composition
streak color
luster
crystalline structure

3.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Which kind of rock is formed when volcanic lava cools?
sedimentary
metamorphic
igneous
magma

4.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

A student wants to study how igneous rock changes to sedimentary rock. Is this a good project if the student needs to complete the study within a month. 
Yes because the changes will happen quickly and be significant.
Yes because the changes will be easily observed since they are very obvious.
No because the difference between igneous rock and sedimentary rock is not noticeable.
No because the changes will take much longer than a month to occur.

5.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Sedimentary rocks are not found on the Moon because
there is no silicon on the Moon.
lava flows are missing from the surface.
the Moon's gravity is too weak.
there is no weathering on the Moon.

6.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

Rocks found on Earth are generally classified as sedimentary, metamorphic, or igneous. On which basis are these classifications made?
where the rocks are found
how the rocks were formed
the color and shape of the rocks
the chemical composition of the rocks

7.

MULTIPLE CHOICE QUESTION

30 sec • 1 pt

The formation of metamorphic rocks depends on all of the following except
the composition of the parent rocks
Earth's magnetic field
 temperature.
pressure.

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