pillow lava.... i think
Volcanoes with very viscous magmas tend to erupt explosively due to the high resistance to gas escape. When magma is thick and sticky, gas bubbles can become trapped, leading to increased pressure within the magma chamber. Once the pressure exceeds the strength of the surrounding rock, it results in a violent eruption as the gas escapes rapidly, fragmenting the magma into pyroclastic material and causing explosive outbursts. This is contrasted with low-viscosity magmas, which allow gases to escape more easily and typically result in effusive eruptions.
Because low silica magmas tend to be hotter and more fluid/runny than high silica magmas.
Cone volcanoes which are likely to erupt explosively are found at subduction zones. Spreading zones (constructive plate boundaries) and hot spots produce quieter volcanoes because their lava is thinner. The ones at hot spots are shield volcanoes.
Felsic magmas produce the most violent reputations. This is because felsic magmas are the most viscous and thus can hold the most gasses. These trapped gases can expand explosively when they reach lower pressure near the surface.
Composite volcanoes typically have andesitic magma, which is intermediate in composition between felsic and mafic magmas. This type of magma is more viscous than mafic magma, leading to explosive eruptions and the buildup of lava and ash layers that form the characteristic steep-sided cone shape of composite volcanoes.
pillow lava.... i think
Volcanoes with very viscous magmas tend to erupt explosively due to the high resistance to gas escape. When magma is thick and sticky, gas bubbles can become trapped, leading to increased pressure within the magma chamber. Once the pressure exceeds the strength of the surrounding rock, it results in a violent eruption as the gas escapes rapidly, fragmenting the magma into pyroclastic material and causing explosive outbursts. This is contrasted with low-viscosity magmas, which allow gases to escape more easily and typically result in effusive eruptions.
The temperature, the pressure, and the type of magma. High silicate magmas generally erupt explosively.
Heat from the mantle melts part of the lower crust
Because low silica magmas tend to be hotter and more fluid/runny than high silica magmas.
Andesite is an extrusive igneous rock found on or near volcanoes that contain intermediate magmas.
Cone volcanoes which are likely to erupt explosively are found at subduction zones. Spreading zones (constructive plate boundaries) and hot spots produce quieter volcanoes because their lava is thinner. The ones at hot spots are shield volcanoes.
Felsic magmas produce the most violent reputations. This is because felsic magmas are the most viscous and thus can hold the most gasses. These trapped gases can expand explosively when they reach lower pressure near the surface.
The source is not as important as the gas content and viscosity. For example, Kilauea in Hawaii doesn't erupt very explosively; it is just a fire fountain. The more explosive volcanoes are those with a blocked magma chamber that builds pressure under a solid surface. Hotspot volcanoes tend to be less explosive because most are on the seafloor.
Composite volcanoes typically have andesitic magma, which is intermediate in composition between felsic and mafic magmas. This type of magma is more viscous than mafic magma, leading to explosive eruptions and the buildup of lava and ash layers that form the characteristic steep-sided cone shape of composite volcanoes.
No, volcanoes can extrude a variety of magma types, which can vary in composition, temperature, and viscosity. Different types of volcanoes, like stratovolcanoes and shield volcanoes, often produce different types of magma due to variations in geological conditions and processes.
Silica-poor magmas, typically basaltic in composition, have lower viscosities compared to silica-rich magmas. This low viscosity allows the magma to flow easily and spread out over large distances, leading to the formation of broad, gently sloping volcanoes. Additionally, the lower gas content in silica-poor magmas results in less explosive eruptions, further contributing to the gentle profile of these volcanic structures. As a result, the accumulation of lava flows creates a wide, shield-like shape characteristic of shield volcanoes.