Yes, Kilauea's magma is typically gassy, containing significant amounts of dissolved gases such as water vapor, carbon dioxide, and sulfur dioxide. As the magma rises toward the surface, pressure decreases, allowing these gases to exsolve and form bubbles, which can lead to explosive eruptions or effusive lava flows. The gas content can vary depending on the specific conditions within the magma chamber and the composition of the magma.
Kilauea is a shield volcano fed by gas-poor basaltic magma. It is the gas in the magma that makes eruptions explosive. Kilauea has occasionally produced explosive eruptions when magma cam in contact with water.
pahoehoe
Kilauea volcano typically produces tholeiitic basalt magma, which is low in silica content and flows easily. This type of magma is associated with shield volcanoes like Kilauea, known for their gentle eruptions and copious lava flows.
Similarities: Both types of eruptions can result in explosive events like pyroclastic flows and ash clouds. Both eruptions can be triggered by a buildup of pressure within the volcano. Differences: Eruptions of less gassy magma tend to produce slower-moving lava flows compared to the more gassy magma eruptions which produce fast-moving and explosive pyroclastic flows. More gassy magma eruptions often result in larger ash plumes and have a greater potential for creating volcanic ash clouds that can impact air travel.
No, the eruption of Kilauea in Hawaii is not associated with subduction boundary. Kilauea is a shield volcano located on a hotspot, where magma rises from the mantle, creating volcanic eruptions.
gassy magma has more silicon than not so gassy that's why there's loud and quiet explosions by: Rielly Krumbholz
Kilauea is a shield volcano fed by gas-poor basaltic magma. It is the gas in the magma that makes eruptions explosive. Kilauea has occasionally produced explosive eruptions when magma cam in contact with water.
pillow lava
pahoehoe
Kilauea volcano typically produces tholeiitic basalt magma, which is low in silica content and flows easily. This type of magma is associated with shield volcanoes like Kilauea, known for their gentle eruptions and copious lava flows.
Similarities: Both types of eruptions can result in explosive events like pyroclastic flows and ash clouds. Both eruptions can be triggered by a buildup of pressure within the volcano. Differences: Eruptions of less gassy magma tend to produce slower-moving lava flows compared to the more gassy magma eruptions which produce fast-moving and explosive pyroclastic flows. More gassy magma eruptions often result in larger ash plumes and have a greater potential for creating volcanic ash clouds that can impact air travel.
Three Million gallons of magma
That depends on the forc of the eruption and the viscosity of the magma.
heat and pressure pushed magma out of the side vents making it ooze out and also magma shoots out of the crater.
No, the eruption of Kilauea in Hawaii is not associated with subduction boundary. Kilauea is a shield volcano located on a hotspot, where magma rises from the mantle, creating volcanic eruptions.
No. Kilauea was formed when the Pacific Plate moved over a hot spot in the Earth's mantle. Magma formed a plume upward into the Earth's crust and formed a volcano: Kilauea. 9 +10 = 21
it deposits great soil and has a magma chamber that can create geothermal energy.