WELL a pahoehoe and aa are created by a non explosive eruption
when some people think of volcanic eruptions, they often imagine rivers of red-hot lava, called lava flows. lava flows come from nonexplosive eruptions. it still spurts lava but non-explosivley!
Magma that is low in silica and produces nonexplosive eruptions is called basaltic magma. As basaltic magma has a low viscosity due to its low silica content, it tends to flow more easily, resulting in nonexplosive eruptions with lava flows.
During a nonexplosive eruption, you can expect to see a steady flow of lava mainly from fissures or vents on the volcano. This type of eruption typically causes slow-moving lava flows, rather than dramatic explosions. Ash and gas emissions may still occur but are usually not as intense as in explosive eruptions.
Basaltic magma produces nonexplosive eruptions, such as those seen at shield volcanoes like Mauna Loa in Hawaii. These eruptions typically involve the gentle flow of lava, creating broad, gently sloping landforms. The low viscosity of basaltic magma allows gas to escape easily, reducing the likelihood of explosive activity. As a result, these eruptions can be sustained over long periods, contributing to the growth of the volcano.
A type of eruption that produces a gentle flow of lava is called an effusive eruption. In these eruptions, lava flows steadily and slowly, typically without explosive activity. The lava tends to have low viscosity, allowing it to flow easily across the surface of the volcano.
when some people think of volcanic eruptions, they often imagine rivers of red-hot lava, called lava flows. lava flows come from nonexplosive eruptions. it still spurts lava but non-explosivley!
Magma that is low in silica and produces nonexplosive eruptions is called basaltic magma. As basaltic magma has a low viscosity due to its low silica content, it tends to flow more easily, resulting in nonexplosive eruptions with lava flows.
During a nonexplosive eruption, you can expect to see a steady flow of lava mainly from fissures or vents on the volcano. This type of eruption typically causes slow-moving lava flows, rather than dramatic explosions. Ash and gas emissions may still occur but are usually not as intense as in explosive eruptions.
Basaltic magma produces nonexplosive eruptions, such as those seen at shield volcanoes like Mauna Loa in Hawaii. These eruptions typically involve the gentle flow of lava, creating broad, gently sloping landforms. The low viscosity of basaltic magma allows gas to escape easily, reducing the likelihood of explosive activity. As a result, these eruptions can be sustained over long periods, contributing to the growth of the volcano.
A type of eruption that produces a gentle flow of lava is called an effusive eruption. In these eruptions, lava flows steadily and slowly, typically without explosive activity. The lava tends to have low viscosity, allowing it to flow easily across the surface of the volcano.
Pahoehoe and AA lava are produced by quiet eruptions. This means that instead of a blast or explosion, the lava just flows out of the volcano. Pahoehoe lava is hot and flows quickly. AA lava is cooler in temperature and doesn't flow as quickly.
An explosive volcanic eruption. Pyroclastic flow is a mixture of fast flowing hot gases that travel down and away from the eruption.
shield volcanoes are only explosive if water somehow gets into the vent
Pyroclastic flow typically occurs during a violent eruption.
The type of eruption that a composite volcano has is lava flow with cinders and bombs in an explosive eruption
Lava flow.
Lava flow.