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clay minerals and quartz
Rocks are made of grains that fit together.
Olivine, Pyroxene, Amphibole, Biotite, Muscovite, Potassium Feldspar, Quartz, Plagioclase are the minerals that make up the Igneous Rocks!:)another one is mica
Biotite and muscovite micas, quartz, magnetite, olivine, amphiboles, and feldspars.
Clay minerals and quartz are the chief constituents of most sedimentary rocks in this category. To answer why, clay minerals are the most abundant product of the chemical weathering of silicate minerals, especially the feldspars. Clays are fine-grained minerals with sheetlike crystalline structures similar to the micas. Quartz is abundant because it is extremely durable and very resistant to chemical weathering. Thus, when igneous rocks such as granite are attacked by weathering processes, individual quartz grains are freed.
clay minerals and quartz
Breccia is an inorganic land-derived sedimentary rock. It is clastic (fragmental), but not foliated. Breccia is composed of mostly quartz, feldspar, and clay minerals; it may contain fragments of other rocks and minerals.
mafic rocks can be made up of orthoclase feldspar and quartz
rock salt
rock salt
Rocks are made of grains that fit together.
Clastic sedimentary rocks are made of broken pieces of preexisting rock that are compacted together. The mineral quartz makes up sixty percent of the clastic sedimentary rocks.
rock salt and conglomerate
rock salt and conglomerate
Olivine, Pyroxene, Amphibole, Biotite, Muscovite, Potassium Feldspar, Quartz, Plagioclase are the minerals that make up the Igneous Rocks!:)another one is mica
Biotite and muscovite micas, quartz, magnetite, olivine, amphiboles, and feldspars.
Quartz Feldspar Mica Heavy minerals e.g Garnet/Zircons Bioclasts