It is denser.
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 mixture of calcium and magnesium carbonates. The ratio of Ca:Mg can vary. If the Ca percentage is very high (above 90%), it is generally considered as calcite and if Mg is very high, it is considered as magnesite (not magnetite). Theoretically, dolomite should have 50:50 Ca:Mg ratio. Usually, dolomite is slightly resistive against weathering and diluted acids compared to calcite.
Marble is a metamorphic rock that is composed mainly of calcite and dolomite. These minerals are typically formed from the metamorphism of limestone or dolostone. Marble is known for its distinctive veining and high polish.
Chemically, the distinction between limestone and dolostone is that the first one is chiefly composed of calcite, CaCO3, whereas the second is rich in MgCO3-Dolomite-. Therefore, the difference is limestone has Ca and Dolostone has Mg.Mg is replacing Ca in the dolostone, in other words.It is very difficult to make the distinction in a macro-scale samples. You will need optical or chemical procedures to differentiate each one.
Marble is a metamorphic rock that forms from the recrystallization of limestone or dolostone under high pressure and temperature conditions. When limestone or dolostone undergoes metamorphism, the calcite or dolomite minerals recrystallize to form marble. Therefore, the primary rocks that change into marble are limestone and dolostone.
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 mixture of calcium and magnesium carbonates. The ratio of Ca:Mg can vary. If the Ca percentage is very high (above 90%), it is generally considered as calcite and if Mg is very high, it is considered as magnesite (not magnetite). Theoretically, dolomite should have 50:50 Ca:Mg ratio. Usually, dolomite is slightly resistive against weathering and diluted acids compared to calcite.
Marble, the rock, is metamorphic. From limestone.
Limestone can be metamorphosed into marble through the process of recrystallization under high pressure and temperature conditions. The calcite crystals in limestone are transformed into interlocking crystals of calcite or dolomite in marble, resulting in increased hardness and a distinctive pattern and coloration.
Marble is a metamorphic rock that is composed mainly of calcite and dolomite. These minerals are typically formed from the metamorphism of limestone or dolostone. Marble is known for its distinctive veining and high polish.
Chemically, the distinction between limestone and dolostone is that the first one is chiefly composed of calcite, CaCO3, whereas the second is rich in MgCO3-Dolomite-. Therefore, the difference is limestone has Ca and Dolostone has Mg.Mg is replacing Ca in the dolostone, in other words.It is very difficult to make the distinction in a macro-scale samples. You will need optical or chemical procedures to differentiate each one.
Dolomite isa sedimentary carbonate rock composed of calcium magnesium carbonate CaMg(CO3)2 . It is similar to limestone. It was originally identified in the Dolomite mountains, a part of the Alps in Italy.
Diabetics can have fluctuating specific gravity levels. In uncontrolled diabetes, specific gravity may be high due to dehydration caused by excessive urination. In controlled diabetes, specific gravity may be normal. It is important to consult a healthcare provider for accurate interpretation of specific gravity levels in diabetics.
It is usually high with dehydration.
There is no such thing as a specific gravity for any element.
It must be thickerer. Therefore, it must take more tomatoes to make the "high specific gravity" type.
8.5