The viscosity of lava during an effusive eruption is generally low, allowing it to flow easily and spread over large areas. This low viscosity is typically associated with basaltic lava, which has a high temperature and low silica content. As a result, effusive eruptions tend to produce gentle lava flows rather than explosive activity. The fluid nature of the lava contributes to the formation of broad, shield volcanoes.
Shield volcanoes have effusive eruptions. Effusive eruptions are a volcanic phenomenon; in some ways the opposite of explosive eruptions. An effusive eruption is characterized by an outpouring of low viscosity lava which has a fairly low volatile content. Usually, shield volcanoes have effusive eruptions.
Viscosity of magma affects the explosivity of a volcanic eruption. High-viscosity magma tends to trap gas bubbles, leading to pressure build-up and explosive eruptions, while low-viscosity magma allows gas to escape more easily, resulting in effusive eruptions. Ultimately, the viscosity of magma influences the type and intensity of volcanic activity.
Factors that determine the force of an eruption are magma viscosity and gas content.
Mount Santa Maria in Guatemala has experienced both effusive and explosive eruptions in its history. The 1902 eruption was explosive, causing catastrophic destruction, while subsequent eruptions have been effusive with lava flows.
A summit eruption can involve explosive activity, but not always. Summit eruptions can also involve effusive lava flows or steady emissions of ash and gas. The specific type of eruption depends on factors such as the magma's composition, gas content, and the volcano's plumbing system.
Shield volcanoes have effusive eruptions. Effusive eruptions are a volcanic phenomenon; in some ways the opposite of explosive eruptions. An effusive eruption is characterized by an outpouring of low viscosity lava which has a fairly low volatile content. Usually, shield volcanoes have effusive eruptions.
Viscosity of magma affects the explosivity of a volcanic eruption. High-viscosity magma tends to trap gas bubbles, leading to pressure build-up and explosive eruptions, while low-viscosity magma allows gas to escape more easily, resulting in effusive eruptions. Ultimately, the viscosity of magma influences the type and intensity of volcanic activity.
There are effusive eruptions and explosive eruptions.
Factors that determine the force of an eruption are magma viscosity and gas content.
A'a is associated with effusive (quiet) eruptions.
Effusive eruptions >:3 WPCMSAdv. Gif. Science
Effusive eruptions >:3 WPCMSAdv. Gif. Science
usually when it erupts its pretty much effusive or explosive
quiet eruption flows easeir cause it has a low viscosity and lava flows easier but explosive eruption has a high viscosity and lava flows slower
They indicate that an eruption is effusive rather than explosive.
They indicate that an eruption is effusive rather than explosive.
Mount Santa Maria in Guatemala has experienced both effusive and explosive eruptions in its history. The 1902 eruption was explosive, causing catastrophic destruction, while subsequent eruptions have been effusive with lava flows.