rock
cottan balls The previous answer was surely a joke. The answer is rocks.
Mafic rocks, such as those found in the oceanic crust, are more dense than the felsic rocks found in the continental crust.
About that of water. This is true of most living things.
Yes, rocks on the Moon are generally denser than rocks on Earth. This is because the Moon lacks the same geological processes that can alter rock compositions and densities over time, resulting in more uniform-density rocks.
the density increases
As igneous rocks become more felsic, their density generally decreases. Felsic rocks, which are rich in silica and contain lighter minerals such as quartz and feldspar, tend to have lower specific gravities compared to mafic rocks that are richer in heavier minerals like olivine and pyroxene. Consequently, the overall density of the rock diminishes as the composition shifts towards more felsic minerals.
Sedimentary rocks typically have a lower density compared to igneous and metamorphic rocks due to their composition, which includes minerals and organic materials that are less dense.
May has 15 more grapes than apples.
As igneous rocks become more felsic, their density generally decreases. Felsic rocks, which are rich in silica and contain lighter minerals such as quartz and feldspar, tend to have lower overall densities compared to mafic rocks that are richer in iron and magnesium. This is due to the higher proportion of lighter elements in felsic compositions, leading to a less dense rock structure. Consequently, the trend shows that as the mineral composition shifts toward more felsic characteristics, the density diminishes.
the density
Rocks that undergo metamorphism can become either more or less dense, depending on the specific changes that occur. For example, the recrystallization of minerals during metamorphism can often lead to an increase in density, while the introduction of new minerals or pore spaces can result in a decrease in density.
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.