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WorksheetsUnit 8: Rocks and Minerals
Total questions: 29
Worksheet time: 15mins
A common Earth material that are the building blocks of rocks.
Minerals
Atoms
Inorganic
Composition
Which of the following is a characteristic of a mineral? (check all that apply)
Solid
Man made
Inorganic
Naturally occurring
Definite chemical composition
A solid composted of one or more types of minerals.
Rock
Mineral
Monomineralic
Polymineralic
The color of a minerals powder.
Color
Streak
Luster
Cleavage
The way a mineral reflects light. It can be metallic or non-metallic.
Fracture
Color
Hardness
Luster
This is not a very reliable source to identify a mineral.
Color
Streak
Hardness
Breakage
Tendency for a mineral to split along a smooth, flat surface.
Cleavage
Fracture
Tendency for a mineral to break into pieces with uneven surfaces.
Cleavage
Fracture
A mineral's ability to scratch or be scratched. We test this by scratching the mineral on glass.
Streak
Hardness
Luster
Cleavage
The "gluing" together of rock fragments.
Cementation
Compaction
Solidification
Lava
The dropping off of sediments by wind, water and/or ice
Solidification
Compaction
Deposition
Weathering
The hardening of liquid rock as it cools.
Solidification
Erosion
Weathering
Magma
The breakdown of rock material at Earth's surface
Weathering
Erosion
Deposition
Compaction
Molten (melted) rock beneath Earth's surface
Magma
Lava
Melted rock on Earth's surface
Magma
Lava
Igneous rocks that form quickly on Earth's surface
Extrusive
Intrusive
Igneous rocks that form slowly beneath Earth's surface
Extrusive
Intrusive
Rocks that form when sediments are compacted and cemented together
Igneous
Sedimentary
Metamorphic
Rocks that are formed when molten (melted rock) cools and solidifies.
Igneous
Sedimentary
Metaphoric
Sedimentary rocks made from sediments joined together after deposition, burial, compaction and cementation.
Clastic
Crystalline
Chemical
Bioclastic
Sedimentary rocks that form when water containing dissolved mineral evaporates and leaves behind solid minerals.
Clastic
Crystalline
Bioclastic
Sedimentary rocks that form from the remains of living things.
Clastic
Crystalline
Bioclastic
Rocks formed directly from any type of rock under extreme heat and pressure.
Igneous
Sedimentary
Metamorphic
Occurs when large areas of rock are under intense heat and pressure; associated with mountain buliding.
Regional metamorphism
Contact metamorphism
Occurs when molten rock comes into contact with surrounding rock in a small area
Regional metamorphism
Contact Metamorphism
The light-colored and dark-colored bands of minerals that form parallel to the foliated in metamorphic rocks
Banding
Compaction
Deposition
Solidification
Igneous rocks that are rich in silicon and aluminum and are lighter in color and have a lower density
Felsic
Mafic
Igneous rocks that are rich in iron and magnesium and have a higher density and darker color.
Mafic
Felsic
Gas pockets found in Igneous rocks
Vesicular
Interlocking crystals
Glassy texture
