Thin, easy flowing lava is usually rich in iron and magnesium. Thick, slow moving lava is usually rich in silica.
Rhyolite is felsic and thus silica rich.
silca rich
No. Scoria is relatively silica poor.
no its the least silica rich of granitic and andesitic magma.
This is because silica-rich magma is thicker. The thicker the magma, the chance for the dissolved gas in there to escape is less likely. This causes an explosion. When the gases do escape, they cause an even bigger explosion
Thin, easy flowing lava is usually rich in iron and magnesium. Thick, slow moving lava is usually rich in silica.
Usually neither. A'a and pahoehoe lavas are both of mafic composition (rich in iron and magnesium, poor in silica) and form basalt when they cool. Composite volcanoes usually erupt material of intermediate to felsic composition (felsic is rich in alkalis, aluminum, and silica), with lavas cooling into rocks such as andesite, dacite, and rhyolite.
The SiO4 tetrahedra continuously form bonds with adjacent ions and atoms, essentially causing the liquid to strik to itself.
Rhyolite is felsic and thus silica rich.
silca rich
lava rich in silica
Silica is sand dust.
silica-rich magma
No. Scoria is relatively silica poor.
no its the least silica rich of granitic and andesitic magma.
Calcite does not contain any silica. It is a carbonate mineral.