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You can compare the density of two different minerals by measuring their mass and volume. The formula to calculate density is density = mass/volume. Once you have these measurements, you can compare the densities of the two minerals to determine which one is denser.
some other way the scientist can compare minerals is crashing each other or take some elements and them revise it.
fluoride chlorine
You can use the Mohs hardness scale to compare the hardness of minerals. The scale ranges from 1 (softest - talc) to 10 (hardest - diamond), with each mineral being able to scratch minerals with lower hardness numbers but not those with higher numbers. This allows for a quick way to determine the relative hardness of different minerals.
What is special is that bare minerals don't give you that "cakey" look, it feels like you're not wearing anything either. They usually compare bare minerals to everyday minerals. Everyday minerals are said to be cheaper and come in different shades.
because it is lame
In Bowen's reaction series, feldspar minerals go through a continuous change of composition, while iron-magnesium groups have an abrupt change of mineral types. When magma cools, the feldspars that form are calcium-rich. As cooling continues, the feldspars react with magma and the feldspar composition changes. The result is a zoned crystal with sodium-rich outer layers and calcium-rich core. For iron-magnesium minerals, when magma starts cooling, a mineral begins to crystallize. However, when the magma temperature drops, a whole new mineral begins to form. The previously formed minerals reacts with the magma and is converted into the new mineral.
Mohs created the Mineral Hardness scale in 1822. It is a comparison table showing 10 common minerals and their relative hardness values. Scientists can use it to compare to other unknown minerals and for classification of minerals. In science you always want to be able to compare something to something else. So instead of saying something is soft or hard, the Mohs Scale gives a relative value to the description.
They appear to be igneous in nature with earth common minerals. Because the earth is geologically active and has flowing water, we see all rock types on the surface.
The table of minerals is significant because it provides a systematic way to categorize and compare different minerals based on their composition and properties. By using the table, scientists can easily identify and study the characteristics of various minerals, helping to understand their unique properties and how they form in nature. This information is crucial for fields such as geology, mineralogy, and materials science.
because it has some precious value s compare to the oters metals
People (geologists) have organized rocks and minerals into categories to better study them and compare their properties. The rocks themselves do not care about organization.