By TOO fast I assume you are asking why the glass breaks?
Cooling causes the molecules in the glass to loose energy. When hot the atoms are forced farther apart. As they cool they come closer together. This causes mechanical stress. If the difference in stress of adjacent areas becomes too great a fracture between the two areas occur.
Heat causes glass to expand. If one section of glass is heated while another is not. The expansion of the glass can create enough pressure inside to break the glass.
If you cool glasses then they will become really cold and frozen
It will be smaller than when a crystal slowly cools, because if it cools rapidly, the crystals have less time to cool
Not enough information. Some crystals will break if they cool rapidly, some crystals will not form correctly if the solution cools too quickly.
cools slowly.
The water vapor will condense and with sufficient particle matter it will form clouds and possibly precipitation.
they depend on how fast it cools down
As a general rule extrusive igneous rock crystals are very small, often microscopic, as the rock cools very rapidly. Conversely intrusive magma often cools so slowly that sizeable crystals can develop.
small
Not enough information. Some crystals will break if they cool rapidly, some crystals will not form correctly if the solution cools too quickly.
cools slowly.
When a magma cools/solidifies, crystals are formed. The quicker the magma cools, the tinier the crystals. A granite for example, which is formed through slow cooling in the Earth's crust, consists out of big crystals. Contrary, magma erupting at the surface (which is then called lava) cools rapidly and consists out of tiny crystals. In extreme cases, the lava cools so rapidly that the resulting rock appears glassy. Hope this helps!
Due to lack of humidity and cloud cover, the desert cools rapidly after sunset.
The water vapor will condense and with sufficient particle matter it will form clouds and possibly precipitation.
crystal
Fine crystal grain.
they depend on how fast it cools down
As a general rule extrusive igneous rock crystals are very small, often microscopic, as the rock cools very rapidly. Conversely intrusive magma often cools so slowly that sizeable crystals can develop.
both the water and soil heats up but the soil heats up rapidly and the water heats up slowly. If it cools down the soil cools down faster and the water cools down slower.
if lava cools slowly, it will have a lot of crystals. When it cools fast, there will be little to no crystals what s ever.