Andesitic magma is more viscous and generally has more gas trapped in it. It is this the expansion of this gas under reduced pressure that drives the explosive force of an eruption. More gas means a more violent explosion.
The more silica content in the magma, the more viscous (thicker) the magma is. Thick magma rich in silica flows less easily than more thinner mafic (Basaltic-rich in Iron and magnesium) magmas
Dissolved gases in thick felsic lava will build up more pressure causing larger, more explosive eruptions
Because they just are. so dont underestimate the power of nature
Mauna Loa exhibits non-explosive eruptions (like many in the Hawaiian islands) in the form of low viscosity (more fluid) lava due to poor silica content.
Basaltic magmas are associated with fissure eruptions creating lava flows spilling out from cracks in the crust. This is because basaltic magmas are more viscous and contain a lower concentration of gases than rhyolitic magma and therefore are unable to build up sufficient pressure to produce explosive eruptions.
Lava domes are large geological features created by rhyolitic magma. Rhyolitic magma promotes plinian eruptions. Plinian eruptions can happen very quickly and shoot lave several miles into the air.
Basaltic lava, Andesitic lava, and Rhyolitic Lava :] (glad to help)
Silica(te) rich magma is usually an explosive eruption. The explosiveness of an eruption depends on - a) Gases trapped within the magma at eruption b) The Silica content c) The fragility of the crater walls and/or the volcanic plug.
Not necessarily. Pumice can be andesitic, but it may be rhyolitic or dacitic.
Mauna Loa exhibits non-explosive eruptions (like many in the Hawaiian islands) in the form of low viscosity (more fluid) lava due to poor silica content.
Rhyolitic magma. Boom! Basaltic magma is its exact opposite, while andesitic magma is in between the two.
Basaltic, andesitic and rhyolitic
Not necessarily. It is often andesitic or rhyolitic.
Pumice is produced in the lava from certain volcanic eruptions. It forms from gas-rich andesitic or rhyolitic lava and has so many gas bubbles that some pumice can float on water.
Basaltic magmas are associated with fissure eruptions creating lava flows spilling out from cracks in the crust. This is because basaltic magmas are more viscous and contain a lower concentration of gases than rhyolitic magma and therefore are unable to build up sufficient pressure to produce explosive eruptions.
Lava domes are large geological features created by rhyolitic magma. Rhyolitic magma promotes plinian eruptions. Plinian eruptions can happen very quickly and shoot lave several miles into the air.
Basaltic lava, Andesitic lava, and Rhyolitic Lava :] (glad to help)
False there classified as basaltic, andesitic and rhyolitic based on amount of silica.
basaltic,andesitic,rhyolitic
The difference between basalt lava and andesite lava is the chemical composition. Basalt lava comes from deep in the mantle of the Earth. Andesite's come from shallow sources near the continental plate margin.