The Bowen's Reaction Series lists the order of crystallization of minerals from high temperature to low temperature environments, starting with olivine and ending with quartz. See the link below.
Gold and Copper.
Minerals with higher melting points will crystallize.
The process is cooling. When magma cools slowly, large well-define crystals form.
Olivine is the first mineral to crystallize as the mineral first to crystallize is the last to melt.
As a magma crystallizes it undergoes fractional crystallization in which mafic minerals crystallize first and felsic minerals crystallize last. Therefore, as fractional crystallization occurs the magma becomes increasingly less mafic and increasingly more felsic. The viscosity also increases as a magma becomes more felsic.
A geyser may form from ground water heated by magma.
Magma rises when it is being pushed or heated from below.
Here are more than two- Galena, Gold, Copper, Sulfur, Pyrite.
i can give you more than two Galena, Gold, Copper, Sulfur, Pyrite
Yes, minerals can crystalize when magma melts.
Magma is molten rock, as the magma cools the minerals crystallize out of it, the slower it cools, the larger the crystals.
No. Magma is already at least partially molten. Mineral crystallize when magma solidifies.
Minerals with higher melting points will crystallize.
The process is cooling. When magma cools slowly, large well-define crystals form.
Olivine is the first mineral to crystallize as the mineral first to crystallize is the last to melt.
As a magma crystallizes it undergoes fractional crystallization in which mafic minerals crystallize first and felsic minerals crystallize last. Therefore, as fractional crystallization occurs the magma becomes increasingly less mafic and increasingly more felsic. The viscosity also increases as a magma becomes more felsic.
A geyser may form from ground water heated by magma.
The temperature of the magma will affect its viscosity depending on its chemistry. Some minerals crystallize at higher temperatures than others, meaning that portions of the magma may have already solidified. At lower temperatures, the majority of the constituent minerals will have crystallized and solidified, leaving the magma highly viscous.