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Assuming you meant 'Feldspar' - it's a group of rock-forming silicate based minerals.
They don't. The Earth's crust is composed mostly of silicate minerals. The core is believed to be metal based on the behavior of seismic waves passing through it. The density of the core is consistent with iron and nickel.
It is composed of minerals which are largely not based on carbon.
A rock is an agglomeration of different minerals. Minerals are classified into categories based on their chemistry: oxides, sulphides, silicates, carbonates etc. Rocks are classified primarily by the process that formed them: igneous, sedimentary, or metamorphic.
Bio-inorganic substance is Biological chemicals which are not carbon based; e.g Minerals etc.
The grouping of silicate and non-silicate minerals is based on whether they contain silicon and oxygen. Silicate minerals are divided into smaller groups based on their structure. Non-silicate minerals are didvided into smaller groups based on their composition.
Minerals can be classified into 13 groups according to their constituents. The major groups are: (1) native elements; (2) sulfides; (3) sulfosalts; (4) oxides and hydroxides; (5) halides and borates; (6) carbonates; (7) nitrates and iodates; (8) phosphates, vanadates, and arsenates; (9) sulfates; (10) tungstates and molybdates; and (11) silicates.
Minerals of a nonsilicate crystal have very high densities because their crystal structures are based on the packing of atoms that are as close together as possible. This structure is called this closest packing.
They are classified based on the structure of their silicate group. Silicate minerals all contain silicon and oxygen.
Assuming you meant 'Feldspar' - it's a group of rock-forming silicate based minerals.
There are more than 2 groups of minerals. The following groupings exist based on their chemical composition:SilicatesOxidesSulfatesSulfidesCarbonatesNative elementsHalides
The minerals that contain silica. This would include quartz, as well as the silicates. The siliceous ooze is the biogenic sediment, containing the remains of organisms whose skeleton is based on silicates.
Stone is a generic term. It usually means a rock, and chemically it refers to an aggregate of minerals, many of which are complex substances, often based on silicate minerals.
The chemical compound silicon dioxide, also known as silica or silox (from the Latin "silex"), is the oxide of silicon, chemical formula SiO2, and has been known for its hardness since the 9th century. Silica is most commonly found in nature as sand or quartz. It is a principal component of most types of glass and substances such as concrete.
The native elements have very high desities because their crystal structures are based on the packing of atoms as close together as possible
A rich assemblage of silicate-based minerals forming the igneous rocks that are solidified from magma. The faster the cooling the finer the crystals but the minerals are the same for a specific eruption or intrusion irrespective of cooling rate.
leucite