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What mineral determines magma viscosity?
A magma's viscosity is directly related to its degree of silica content.
What two main factors affect magmas viscosity?
The main factors that affect magma's viscosity are temperature and silica content. Higher temperatures generally result in lower viscosity, as the magma becomes more fluid. Lower silica content also leads to lower viscosity, as silica molecules tend to create more resistance to flow.
What is Mt Fuji's magmas viscosity?
Mount Fuji's magma is known to have relatively low viscosity compared to other volcanoes, which contributes to its more gentle eruptions. This low viscosity magma allows for gases to escape more easily, reducing the likelihood of explosive eruptions.
What is the difference between viscosity and volcanic erutions?
Viscosity refers to a fluid's resistance to flow; fluids with high viscosity are thicker and flow more slowly. Volcanic eruptions, on the other hand, involve the expulsion of magma, gases, and ash from a volcano. Viscosity can affect the explosiveness or effusiveness of a volcanic eruption, as more viscous magmas typically lead to more explosive eruptions.
Does mafic magma explode?
Mafic magmas generally have lower viscosity and gas content compared to felsic magmas, so they tend to flow more easily rather than explode. However, in certain conditions where gas build-up is high and pressure is released rapidly, mafic magma may still explode, but it is less common than with felsic magmas.
A magmas viscosity is directly related to its?
A magma's viscosity is directly related to its temperature and silica content. Higher temperatures and lower silica content result in lower viscosity, making the magma more fluid and able to flow more easily.
What is a magmas viscosity related to?
The silica content. A higher silica content results in a more viscous magma.
Magma viscosity is directly related to what?
silica content
What kind of magmas produce violent volcanic eruptions?
Magmas with high viscosity and gas content tend to produce violent volcanic eruptions. High viscosity magmas are thicker and have more difficulty releasing gas, leading to pressure build-up and explosive eruptions. This often occurs with felsic or rhyolitic magmas.
Why do volcanic eruptions differ?
The main cause of differences in volcanic eruption characteristics is due to the viscosity of the magma. High viscosity magmas are high in sticky silica which traps gas and produces explosive eruptions. Low viscosity magmas are low in silica and produce eruptions with far less energetic characteristics.
What mineral determines magma viscosity?
A magma's viscosity is directly related to its degree of silica content.
How are the eruptive styles different depending on the magmas viscosity?
depending on the space before and temp at the time
Why are granitic magmas thicker than basaltic magmas?
Granitic magmas are thicker than basaltic magmas because they have higher silica content, which increases viscosity. The higher silica content leads to stronger bonding between the silica tetrahedra, making it more difficult for the magma to flow. Basaltic magmas, on the other hand, have lower silica content and are less viscous, allowing them to flow more easily.
How hot does magma have to be to explode?
The explosive potential of magma depends more on viscosity gas content than on temperature. Most magmas are at temperature of at least 700 degrees Celcius. Interestingly, the most explosive magmas are the high-silica magmas, which have lower melting temperatures.
What kind of magmas are generated in places where volcanoes erupt both explosively and nonexplosively?
Volcanoes that erupt both explosively and nonexplosively typically generate magmas with a range of compositions. This can include basaltic magmas for nonexplosive eruptions due to their low viscosity, and intermediate to silicic magmas for explosive eruptions due to their high gas content and higher viscosity. The mixture of magma types leads to varying eruption styles within the same volcanic system.
Why do silica poor magmas produe broad volcanoes with gentle slopes?
Silica-poor magmas, typically basaltic in composition, have lower viscosity compared to silica-rich magmas. This lower viscosity allows them to flow easily and spread over large distances, resulting in the formation of broad, gently sloped volcanoes. The fluid nature of these eruptions generally leads to less explosive activity, contributing to the broad shape of the volcano. Consequently, the accumulation of layers of low-viscosity lava contributes to the characteristic gentle slopes.
What is directly related to the concentration of solutions?
I suppose that you think to the density, viscosity, refractive index, radiation absorption etc.
