Density is a measure of how much mass is contained in a give unit volume (density=mass/volume). It is usually expressed in kg/m^3. Put simply, if mass is a measure of how much 'stuff' there is in an object, density is a measure of how tightly that 'stuff' is packed together.
One of the ways we can see density illustrated in everyday life is by looking at whether things float or sink in a liquid (water, for example). If an object is less dense than the liquid it is placed in, it will float. If it is more dense, it will sink. This is why an anchor, which is very dense (lots of mass in a relatively small volume) sinks very quickly, while an inner tube (not much mass in a relatively large volume) floats and is very difficult to push underwater.
Some elements are naturally found in very dense forms,and one of the most surprising cases of a less dense object floating on a denser liquid occurs when objects are put in a container of liquid mercury (Hg). This element is a metal that is liquid at room temperature, and it is VERY dense. In fact, it is denser than lead, and metal objects like forks, coins, or even a cannonball will float on top of it!
Cooler material is more dense and hotter material is less. This means that plates become more dense as they cool.
Yes, that is correct. Magma is less dense than the solid rock around it, causing it to rise towards the surface through cracks and fractures in the Earth's crust. This movement occurs due to the buoyancy of the less dense magma compared to the denser surrounding rock.
Because it is less dense than the material that makes up the earth's crust, but more dense than the material that makes up the air.
This process is known as convection, where cooler, denser material sinks while warmer, less dense material rises. This movement of material within the Earth's mantle helps drive the motion of tectonic plates.
The specific heat of a material is influenced by its atomic or molecular structure and how tightly packed its particles are. In denser materials, particles are more closely packed, which allows them to transfer energy more efficiently but requires less energy input to raise their temperature compared to less dense materials, where particles are more spread out and have more degrees of freedom. Consequently, denser materials tend to have lower specific heats.
Cooler material is more dense and hotter material is less. This means that plates become more dense as they cool.
bends towards the normal.
less dense than the material of the Earth's mantle
Actually, heated materials are less dense. When heat is applied to a substance such as liquid, it becomes less dense. It is this less dense and heated material that rises because it weighs less. The part of the mantle that is more dense would be any substance that is cooling and is sinking down.
density is mass per unit volume so the less mass per cubic(what ever measure) the less buoyant.
Actually, hot, less dense material rises, and cold, denser material sinks. Denser material will be heavier (per unit volume) and gravity therefore pulls it down. Less dense material has buoyancy and rises. It's very logical.
Magma?
There are a number of things that may happen to substances that are less dense than the surrounding material. In most cases, this is what will cause them to float on the surrounding material.
it is less dense.
In science, "less dense" means that a substance has a lower mass per unit of volume compared to another substance. This is commonly observed when an object or material floats in a more dense substance, such as when ice (less dense) floats on water (more dense).
Convection.
Rarefaction