Chemical
Detrital
Organic
Above
Below
On
Condensation
Erosion
Weathering
Compaction
Rock cycle
Melting process
Formation of crystals
Compaction
Weathering and erosion
Cementation
Heat and pressure
Magma
Lava
Both magma and lava
Magma
Lava
Neither magma or lava
Both magma and lava
Layers
Lack of layers
Large mineral grains
Air holes
Chemical or organic
Intrusive or extrusive
Foliated or nonfoliated
Basaltic or granitic
Formed when loose material become pressed or cemented together or when minerals form from solutions
Formed from magma
A type of foliated igneous rock
Formed because of changes in temperature and pressure, or the presence of hot watery fluids
Made of molten material
A mixture of minerals, organic matter, volcanic glass, or other materials
Formed by heat and pressure
Either igneous or sedimentary
Tiny
Invisible
Fine-grined
Large
Rocks
Crystals
Matter
Minerals
It is denser than the surrounding solid rock
It is less dense than the surrounding solid rock
Heat and pressure
It has the same density as the surrounding solid rock
Extrusive
Intrusive
Detrital
Coarse-grained
Extrusive
Fine-grained
Detrital
Intrusive
Silica rich
Lower in density than granitic rocks
Rich in iron and magnesium
Basaltic
Andesitic
Granitic
All of the possibilities listed with this question
Sediments becoming pressed or cemented together
Crystals solidifying from magma
Sediments forming from solution
Water evaporating leaving crystals behind
Held together with natural cements
Formed when atoms of melted minerals rearrange themselves
Formed when lava erupts from a volcano
Formed by magma trapped below Earth's surface
Metamorphic
Detrital
Organic
Chemical
Chemical
Detrital
Organic
Basaltic
Foliated metamorphic
Nonfoliated metamorphic
Basaltic
Organic
Compaction
Cementation
Weathering
Erosion
Compaction
Cementation
Weathering
Erosion
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