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What is the most common mineral group is broken into subgroups of ferromagnesium and nonferromagnesium?
Silicate
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What is the most common mineral group broken into the subgroups of ferromagnesium and nonferromagnesium?
Silicate
What is the most common mineral group broken into?
The most common mineral group is the silicates, which are composed of silicon and oxygen, the two most abundant elements in the Earth's crust. Silicates are further divided into various subgroups based on their structural arrangements, such as nesosilicates, inosilicates, phyllosilicates, and tectosilicates. This diversity contributes to the formation of a wide range of rock types and geological formations. Other significant mineral groups include carbonates, oxides, and sulfates, but silicates dominate in terms of abundance and variety.
Why do minerals get processed?
It is all part of life minerals come and go so to start a new mineral you need an old broken down mineral
How do minerals dissolve?
Minerals dissolve when they come into contact with a solvent such as water and the chemical bonds holding the mineral's atoms together are broken. This process involves the mineral's ions entering into the solution, leading to the mineral dissolving and dispersing into the solution. The ability of a mineral to dissolve depends on its chemical composition and the properties of the solvent.
Is the word coal a noun?
Yes, the word 'coal' is a noun, a word for a form of the mineral carbon that is broken into pieces suitable for use as fuel; a word for a thing.
What is the most common mineral group broken into the subgroups of ferromagnesium and nonferromagnesium?
Silicate
The most common mineral group is broken into the subgroups of ferromagnesium and nonferromagnesium?
its silicate
What most common mineral group is broken into the subgroups of ferromagnesian and non ferromagnesian?
The most common mineral group that is broken into the subgroups of ferromagnesian and non-ferromagnesian is the silicate mineral group. Ferromagnesian silicates contain iron and/or magnesium, while non-ferromagnesian silicates do not contain these elements. Examples of ferromagnesian silicates include olivine and pyroxene, while examples of non-ferromagnesian silicates include feldspar and quartz.
During recystallization the bonds between atoms in a mineral are broken and can join to form a?
new mineral with a different crystalline structure.
What are two type s of cholesterol?
there is HDL=cholesterol LDL=bad cholesterol, there are triglycerides and these can all be broken down into subgroups as well vldd and vhdl
How is the color of a mineral when it is broken up and powdered?
A streak test.
What is the color of a mineral when it is broken up and powered?
a dusty white
Is the color of the mineral when it is broken up and powdered?
A streak test.
At what size is a rock to small to technically be a rock?
When it is broken down into an individual mineral grain or crystal, in which case it is a mineral.
How is the color of a mineral when it is broken up and powdered revealed?
A streak test.
What property uses the color a mineral when it is broken up to identify it?
streak.
Why do minerals get processed?
It is all part of life minerals come and go so to start a new mineral you need an old broken down mineral
