don't have a clue?!
Magma that cools quickly forms into igneous rock, when it cools quickly it becomes a lava rock. Lava cools very quickly at first and forms a thin crust that insulates the interior of the lava flow.
It cools.
A gas filled rock that cools quickly is likely a vesicular basalt. This type of rock forms from lava that is erupted from a volcano and cools rapidly, trapping gas bubbles inside. The rapid cooling prevents the bubbles from escaping, creating a porous texture.
yes
No. Small crystals form.
The thickness of insulation affects the rate at which hot water cools down by providing a barrier that prevents heat from escaping quickly. Thicker insulation reduces heat transfer, so hot water will cool down more slowly compared to thinner insulation. By controlling variables such as the initial temperature of the hot water and the ambient temperature of the surroundings, one can isolate the effect of insulation thickness on cooling rate.
Yes, the number of layers of insulation can affect how quickly water cools down. More layers of insulation typically provide better thermal resistance, slowing down heat transfer from the water to the surrounding environment, thus helping to retain heat for a longer period of time.
A fan.
Lava will cool quickly compared to underground magma.
When lave cools fairly quickly, but not instantaneously, the rock that is producing will have small or nearly invisible crystalsform.
it explodes
It cools quickly.
"Larger than if it cools quickly" is about all that's definitively possible to say.
Magma that cools quickly forms into igneous rock, when it cools quickly it becomes a lava rock. Lava cools very quickly at first and forms a thin crust that insulates the interior of the lava flow.
Keeping in mind that insulation does allow the limited flow of thermal energy through its material, imagine if you will, a wall of around 1m thickness. On one side of the wall, the temperature is 100oC, while on the other the temperature is 0oC. The 100C side of the wall will start absorbing heat from the environment and will transfer part of that heat inside the wall, lets say at 10cm depth. That part of the wall will start heating up and its temperature will rise. Since its temperature has now risen, it will start transferring heat to the 20cm depth inside the wall. Of course keep in mind that in reality the transfer of heat and temperature change is smooth like a ramped and not in steps like my example above. This will go on all the way through to the other side of the wall. This way, a temperature gradient will be formed inside the wall. The thickness of the wall dictates the form of the temperature gradient, thus it dictates the rate of heat transfer from the inside to the outside (higher to lower temperature). This is displayed by Fouriers' Law, ΔQ/Δt=-Ak ΔT/Δx Where ΔT is the difference in temperature between the inside and outside, Δx, the thickness of the "insulator", A the surface area, k the conductivity and ΔQ/Δt is the rate of heat transfer. The larger Δx is, the lower the heat transfer will be.
Small
It cools.