The density of rock B is greater because its volume is less.
Since rock A is bigger but has the same mass as rock B, it will have a lower density compared to rock B. Density is calculated by dividing mass by volume, so the larger volume of rock A will result in a lower density.
Rocks can be compared based on their mineral composition, texture, color, and density. By examining these characteristics, geologists can determine the type of rock and its origins. Additionally, rocks can be compared based on their hardness, cleavage, and overall physical properties.
The crustal rocks have less density than the mantle rocks. The continental crust is less dense than the oceanic crust, which is in turn less dense than the mantle beneath.
The density of felsic rocks typically ranges from 2.6 to 2.8 g/cm3.
No, not all rocks sink. The density and composition of a rock will determine whether it sinks or floats in water. Rocks with lower density or containing air pockets may float.
Rocks have a much higher density compared to gases. This is because rocks are made up of tightly packed molecules, whereas gases have molecules that are spread further apart. As a result, rocks have a higher mass per unit volume, leading to higher density.
rock
You smash a rock with a bigger rock
Rocks can be compared based on their mineral composition, texture, color, and density. By examining these characteristics, geologists can determine the type of rock and its origins. Additionally, rocks can be compared based on their hardness, cleavage, and overall physical properties.
It depends on the type of rock and the conditions. Generally, ice has a lower density than most rocks, which is why ice floats on water. Rocks vary in density based on their composition and can be denser than ice.
Normally, light colored igneous rocks are less dense compared to dark colored igneous rocks. This is because the light colored rocks have a less iron in them.
Igneous rocks are formed in and around volcanos, metamorphic rocks are formed by the partial melting of rocks deep underground.
wind could possibly move the rocks or smaller ones a. the rocks will compact to form another and a bigger and bigger one ect. also if the blew hard enough on old rock the rock might etc into smaller rocks on the process begins again
The crustal rocks have less density than the mantle rocks. The continental crust is less dense than the oceanic crust, which is in turn less dense than the mantle beneath.
The density of felsic rocks typically ranges from 2.6 to 2.8 g/cm3.
Density is just one property of rock that can be utilized in the discovery of ore deposits.
Less than. The moon rock density is greater in ferromagnesion and nickel content, with greater density, whereas silicate rocks contain largely quartz and feldspar minerals.
cottan balls The previous answer was surely a joke. The answer is rocks.