Only in Leaf Green, on One Island (I think Kindle Road)
Eyjafjallajökull primarily produces basaltic to andesitic magma. The composition of its magma is influenced by the subduction of the North American Plate beneath the Eurasian Plate, which can lead to more evolved magma types. This volcanic system is known for its explosive eruptions due to the interaction of magma with ice and water, as seen in its 2010 eruption.
These are called vesicles, which are voids left by gas bubbles escaping from magma as it solidifies. They are commonly seen in aphanitic rocks like basalt and andesite.
The center of the earth is the core. It is full of molten hot magma. It is generally pictured as red when seen in drawings.
Slow cooling of magma far beneath earth's surface has a phaneritic texture (this means that the individual crystals are large enough to be seen with the naked eye).
An acid magma or a granitic magma.
Volcanoes with magma rich in basalt typically occur at divergent boundaries and hotspot locations. At divergent boundaries, such as mid-ocean ridges, tectonic plates pull apart, allowing magma to rise and create basaltic lava. Additionally, hotspots, which are areas where plumes of hot mantle material rise, can produce basaltic magma as seen in places like the Hawaiian Islands.
Basaltic magma is the most abundant type erupted at oceanic spreading centers. It is low in silica content and flows easily due to its low viscosity, allowing it to create the characteristic volcanic features seen at mid-ocean ridges.
Yes, Mount Popocatepetl is high in silica because it is a stratovolcano, which typically contains high amounts of silica in its magma composition. Silica-rich magma tends to be more viscous, leading to explosive eruptions as seen with the eruptions of Popocatepetl.
magma
This is called the magma chamber.
Before lava reaches the surface it is called magma.
basaltic,andesitic,rhyolitic