Often referred to as Acapulco Gold, but more commonly known these days as Mexican sativa, it is often used in breeding projects which have led to numerous world-class strains such as Skunk #1, multiple Haze varieties and even the fabled Blueberry line (check out #11, #10 and #2).
Melting Points of Rocks. Igneous rocks form through the crystallization of magma. There is a considerable range of melting temperatures for different compositions of magma. All the silicates are molten at about 1200Â°C and all are solid when cooled to about 600Â°C.Often the silicates are grouped as high, medium and low-melting point solids.he pattern shown above where different kinds of minerals crystallize at different temperatures is further developed in the Bowen reaction series. The crystallization temperatures play a large role in the development of the different kinds of igneous rocks upon the cooling of magma.
Most magma that reaches the surface in volcanic eruptions comes from a part of Earth's mantle called the asthenosphere. The asthenosphere is a layer of solid rock that is near its melting point. Turning this solid rock into liquid magma means changing its temperature, pressure, and water content.Try your hand at melting rock to create magma. The first thing to try changing is the temperature.Your rock is a toasty 1,500 degrees Celsius, but it's still solid. Click on the words lower or raise to change the temperature your rock is subjected to inside Earth.ry your hand at melting rock to create magma. The first thing to try changing is the temperature. Your rock is a toasty 1,500 degrees Celsius, but it's still solid. Click on the words lower or raise to change the temperature your rock is subjected to inside Earth.