The three types of magma, named for the rock they form are basaltic, rhyolitic and andesitic. Rhyolitic magma is rich in silica and water vapor.
Highly viscous felsic magma.
An acid magma or a granitic magma.
lava
Yes.
yes
Igneous rocks that are dense and dark-colored are called basaltic rocks. They are formed from magma that is rich in iron and magnesium and poor in silica content.
If there is a high silica content in the magma, the eruption is usually more violent and explosive. Magma with a high silica content flows slower so pressure can build up and eventually erupt.
Low silica defines BASALTIC rocks. Iron rich is defined by FERROUS. Not sure about Mg though. Mineral rich is a good one...
I think like granite, amethysts are formed from magma deep underground. This helps them to cool slowly forming the large crystals they have.
rich
Silica is sand dust.
An acid magma or a granitic magma.
Silica-rich magma is much more thick and viscous.
Viscose lava e.g. andesitic or rhyolitic. This might not be the definition your looking for though.
no its the least silica rich of granitic and andesitic magma.
silica-rich magma
Acidic lava is very viscous, and thus will harden and block the vent. The magma will force its way out through the vent and create a violent explosion.
silica rich magma associated with explosive eruptions because it tends to trap water and gas bubbles :)
High silica magma is light in color, thick, sticky and less dense than basalt magma. The magma that forma volcanoes is rich in silica. High silica magma have low temperatures because magma that is high in silica have the lowest temperatures. Silica rich magma builds a tall cone shaped volcano, a Stratovolcano. Magma that is high in silica resists flowing, so expanding gases are trapped in it. Pressure builds up until the gases blast out in a violent, dangerous explosion.
red or scarlet
Yes
The silica-rich magma, also called felsic magma, is more viscous than iron-rich or mafic magma. This means resists flow more (just as syrup is more viscous than water). The high viscosity means that the felsic magma can trap more gasses, leading to explosive eruptions, rather than effusive ones.