Silica in natural form can be both particles or thick on fusion as in felsic magma origin
Silica is sand dust.
When lava flows through a patch of silica it become thick. When the thick lava hits water, it boils the water and traps the gasses. These gasses make a violent Explosion.
An acid magma or a granitic magma.
silica content
The three things that determine how thick or thin magma is temperature, silica content, and gas content.
Silica-rich thick magma is typically classified as either dacitic or rhyolitic magma. These magmas have higher silica content, making them more viscous and able to trap gas bubbles. They often erupt explosively due to the high pressure build-up caused by the thick magma.
Silica-rich magma is much more thick and viscous.
Thick due to high silica content.
Silica-rich thick magma is called rhyolite. It contains high levels of silica, making it very viscous and typically light in color. Rhyolite is associated with explosive volcanic activity due to the build-up of pressure caused by the slow movement of its thick lava.
Lava high in silica (granitic lava) tends to be thick and viscous, so the volcano is likely to be composite rather than shield.
it is normally intermediate flow because of the silica content.
The awnser is this, each tile consits of the outside coating which is borosilicate and the white center which is 90% air and 10% silica.