Dolomite is a type of limestone containing magnesium carbonate as well as the calcium carbonate of ordinary limestone. As with ordinary limestone, dolomite is a deposit of microscopic skeletons of dead plankton. When the plankton die their skeletons settle to the bottom of the ocean, forming a ooze that eventually solidifies. When mountain building activities raise this on the land we get limestone or dolomite.
Triumph Dolomite was created in 1972.
The metamorphosed form of dolomite is called marble. Dolomite is a sedimentary rock primarily composed of the mineral dolomite, while marble is a metamorphic rock that forms from the recrystallization of limestone or dolomite under high heat and pressure.
Yes, both calcite and dolomite are carbonates.
The chemical classification group that dolomite belongs to is a carbonate. Dolomite is an element of calcium magnesium carbonate and has the chemical formula CaMg(CO3)2.
China is the world's leading producer of dolomite.
Dolomite is a metal, a dolomite mountain is a mountain made of dolomite
Dolomite is a type of carbonate material that is made up of calcium magnesium carbonate. The weight of dolomite depends on how big the chunk is that you're looking at.
Dolomite is generally ground into coarse or finelygrained powder and made into calcium/magnesium capsules or antacids for human consumption.
"Dolomite: Simply Better."
the color of the streak for dolomite is white
The outside of a dolomite rock can be many colors it just depends on the rock itself. (this was made by a freshman in high school so if this is wrong that take it out on yourself for believing it)
Yes. Dolomite is a carbonate, not a silicate.
Triumph Dolomite was created in 1972.
The metamorphosed form of dolomite is called marble. Dolomite is a sedimentary rock primarily composed of the mineral dolomite, while marble is a metamorphic rock that forms from the recrystallization of limestone or dolomite under high heat and pressure.
Dolomite is a carbonate. The formula is CaMg(CO3)2
Yes, both calcite and dolomite are carbonates.
Dolomite typically exhibits three cleavage planes that intersect at approximately 90 degrees, resulting in rhombohedral cleavage.