Want this question answered?
Metamorphic rocks that consist of only one mineral and have large interlocking crystals often have a coarse-grained texture. This means that the individual mineral grains are easily visible to the naked eye. Examples of such rocks include quartzite (formed from quartz) and marble (formed from calcite).
Interlocking
hi everyone nice to meet you i am katie!
When water combines with mineral grains, the grains become larger. The increase in size of mineral grains strains the rock material and weakens it.
Not very, over geologic time. Limestone is vulnerable to chemical attack from naturally acidic rainfall and runoff.
Igneous rock has interlocking grains with no specific pattern.
interlocking grains fit tightly together to make hard rocks
Interlocking
Granite does not have rounded grains but contains interlocking grains. An example of a rock with rounded grains is a sandstone.
Metamorphic rocks that consist of only one mineral and have large interlocking crystals often have a coarse-grained texture. This means that the individual mineral grains are easily visible to the naked eye. Examples of such rocks include quartzite (formed from quartz) and marble (formed from calcite).
not sure but i know it's an example of interlocking grains.. Interlocking visible crystals would be good descriptive words for granite.
Interlocking
hi everyone nice to meet you i am katie!
Crystalline rock is composed of interlocking crystalline grains, as in granite. Clastic rock is composed of rock or mineral grains which have become cemented together by the processes of lithification. Examples of clastic rock are sandstone and conglomerate.
foliated
When water combines with mineral grains, the grains become larger. The increase in size of mineral grains strains the rock material and weakens it.
No. Granite does not have gaps between the grains. The crystals in an intrusive igneous rock are interlocking.