Crazy
The more silaceous the lava, (higher silica content), the more explosive the eruption.
The type of volcanic eruption is primarily determined by the composition of the magma beneath the volcano. Magma high in silica tends to be more viscous and leads to explosive eruptions, while lower silica magma tends to flow more easily, resulting in effusive eruptions. Other factors such as the presence of gas, the amount of pressure, and the shape of the volcano can also influence the type of eruption.
Silica content in strombolian eruptions is typically low (around 50-52%), as they are characterized by the eruption of basaltic magma. This type of magma has a lower silica content compared to other types such as andesitic or rhyolitic magmas, which are associated with different types of volcanic eruptions like explosive ones.
Mt. Hood has lava with high silica content, resulting in a more viscous and explosive eruption compared to lavas with lower silica content. High silica lava tends to form more explosive eruptions due to its increased resistance to flow.
felsic magma, which has high viscosity due to its high silica content. This high viscosity can lead to the build-up of pressure and gas bubbles, resulting in explosive eruptions.
The more silaceous the lava, (higher silica content), the more explosive the eruption.
It was a quiet eruption and it was low in silica
The properties of magma that help to determine the type of eruption are the magma's viscosity and its silica content. Those volcanoes that exhibit massive eruptions have a high viscosity and high silica content.
The type of volcanic eruption is primarily determined by the composition of the magma beneath the volcano. Magma high in silica tends to be more viscous and leads to explosive eruptions, while lower silica magma tends to flow more easily, resulting in effusive eruptions. Other factors such as the presence of gas, the amount of pressure, and the shape of the volcano can also influence the type of eruption.
Pelean
Silica content in strombolian eruptions is typically low (around 50-52%), as they are characterized by the eruption of basaltic magma. This type of magma has a lower silica content compared to other types such as andesitic or rhyolitic magmas, which are associated with different types of volcanic eruptions like explosive ones.
Mt. Hood has lava with high silica content, resulting in a more viscous and explosive eruption compared to lavas with lower silica content. High silica lava tends to form more explosive eruptions due to its increased resistance to flow.
Scientists measure the silica content in magma to classify it into different types based on its composition. The silica content determines the magma's viscosity, which impacts how easily gases can escape and influences the type of volcanic eruption that may occur.
magma or lava dried after a volcanic eruption.
felsic magma, which has high viscosity due to its high silica content. This high viscosity can lead to the build-up of pressure and gas bubbles, resulting in explosive eruptions.
Pelean
Igneous rocks with high amounts of silica are classified as felsic rocks. Common examples include granite and rhyolite. These rocks typically have a lighter color and are less dense than mafic rocks, which have lower silica content. The high silica content contributes to their viscosity during magma formation and eruption.