igneous rock
Heat, pressure, or transfer of elements through high temperature solutions.
Heat and high pressure
they are normally formed inside or very near volcanoes. To form igneous rock magma must cool the it will turn into and igneous rock (intrusive or extrusive)
Bromine, as many other materials gets a higher melting point when pressure is low [less energy is needed to set molecules free] and lower melting point when pressure is high [more energy needed].
Minerals are formed by elements coming together, and then lots of pressure and heat is added over millions of years.
metamorphic rock
Heat, pressure, or transfer of elements through high temperature solutions.
Heat is only energy. In areas of low pressure, such as high altitudes, "heat" particles, which are charged electrons, escape more quickly. As more "heat" (electrons) escapes more quickly, things freeze more quickly. As far as I know melting and boiling points are higher, not lower in high altitudes.
The melting point is not changed by pressure. It is still over 32O
It keeps your processor from melting. Do not run a PC without a heat sink on your processor. Processors can get to extremley high temperatures. The heat sink absorbs this heat and removes it using a fan.
Heat and high pressure
regional: heat and pressure and shear stress (LOCAL)- contact: heat- high pressure- low deformational: high -pressure, low- heat
It passes heat out of the high pressure high temp vaporized refrigerant so the it becomes a high pressure lower temperature liquid.It passes heat out of the high pressure high temp vaporized refrigerant so the it becomes a high pressure lower temperature liquid.
Because melting occur at high temperature; at this temperature bonds between particles are weaker.
When the sedimentary rock is going under heat and pressure, turning it into a metamorphic rock.
they are normally formed inside or very near volcanoes. To form igneous rock magma must cool the it will turn into and igneous rock (intrusive or extrusive)
The melting point of a solid is the temperature at which it changes STATE from SOLID to LIQUID. At the melting point the solid and liquid phase exist in equilibrium. The melting point of a substance depends (usually slightly) on pressure and is usually specified at STANDARDatmospheric pressure.