Rocks receive their densities by their mass divided by their volume. For example, if a rock has a mass of 9 grams, and a volume of 18 cubed cm, then the density would be 9/18 or .5 g/cm3.
Igneous rocks vary greatly in composition and method of formation, resulting in diverse densities.
The best way to find the densities between two rocks is by conducting a displacement test. You will need to measure the volume of water displaced when the rocks are submerged, and then calculate the density using the mass of the rocks and the displaced water.
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Basaltic Magmas are dark colored, heavy and are ferromagnesian in composition, so they most times do not form light colored rocks, rather, the Felsic Granitic Magma forms the light colored rocks with lower densities.
They tend to aggregate at high densities under rocks.
because the great amount of pressure creates higher density
False. Light colored rocks with lower densities typically form from felsic magma, which has a higher silica content compared to basaltic magma. Felsic rocks include granite and rhyolite, which are commonly light in color and less dense.
Felsic refers to igneous rocks that are rich in elements that form feldspar and quartz. Their densities vary, depending on the rock, but they generally have low density.
rocks and mineral deposits play a role in the various densities across the earth's surface :)
They look at the wave speeds as they travel thought the earth and find the densities of the rock. Then they compare the densities to the rocks they know. The use information for different seismographs to figure out the speed of the wave.
Olivine and pyroxene are commonly found in igneous rocks that are mafic in composition. These minerals indicate that the rock formed from magma with a higher iron and magnesium content. Mafic igneous rocks tend to be dark in color and have higher densities compared to felsic rocks.
Igneous rocks are denser than sedimentary rocks because the particles and materials making up the igneous rock are more closely packed and compacted making more matter able to fit into a tiny area of its structures.