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.
the density increases
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.
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.
the density
The density of felsic rocks typically ranges from 2.6 to 2.8 g/cm3.
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.
Rocks have color, grain, specific density, and relative hardness.
Mafic rocks are generally denser than felsic rocks due to their higher content of iron and magnesium minerals. This higher density is attributed to the presence of heavier elements in mafic compositions.