The more silica in lava, the more viscous the lava is. Silica (SiO2) content varies from 50 percent to 70 percent. Basaltic lava, which is 50 percent silica, is runny and contains relatively little gas. Granitic lava, typically around 70 percent silica, is 70 percent silica. It is much thicker and contains much more gas. As a result when granitic lava flows, it tends to release gasses (water and carbon dioxide) explosively.
The lava on the Hawaiian Islands in basaltic, and flows easily. The lava in Mount St Helens is very thick, so when it finally reaches the surface it causes a much more violent and dangerous eruption.
the atoms start to lose heat and come closer together, then turing into a compound which forms a mineral. Hope this helps!
There isn't a item called Magama Stone.
=yes the magama hide out=
volcanoes
Magama from a volcano that cools
The R-value of mineral wool insulation typically ranges from 3.0 to 3.7 per inch of thickness.
The mineral quartz affects the thickness of magma by increasing its viscosity. When quartz-rich magma cools and solidifies, it forms a dense and viscous rock, like granite. This high viscosity can result in explosive volcanic eruptions.
By mid-ocean ridges.
The mineral that affects magma thickness is silica. Magma with high silica content tends to be more viscous, resulting in thicker magma. Conversely, magma with low silica content is less viscous and flows more easily.
The ocean floors are largely made of magma.
No, it is not considered bad to boil mineral water. All boiling does is sterilize water, it has not shown to be harmful or to decrease the mineral effects.
Magama.