Lava with high viscosity is called slica-rich lava
No, low viscosity lava flows faster than high viscosity lava. Low viscosity lava is more fluid and can move more easily, while high viscosity lava is more sticky and tends to move more slowly.
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Viscosity is a measure of a fluid's resistance to flow. Higher viscosity lava flows more slowly because it is more resistant to deformation and requires more force to move. Lower viscosity lava flows more quickly as it can deform and flow more easily.
The resistance to flow of lava depends on its viscosity, which is influenced by factors such as temperature, composition, and gas content. Lava with low viscosity (more fluid) flows more easily, while lava with high viscosity (more sticky) flows less easily. The resistance to flow can also be affected by topography and the presence of obstacles in the lava's path.
Lava with high viscosity is called slica-rich lava
No, low viscosity lava flows faster than high viscosity lava. Low viscosity lava is more fluid and can move more easily, while high viscosity lava is more sticky and tends to move more slowly.
Silica content is directly proportional to viscosity, so the higher the silica content of a lava, the higher its viscosity. high viscosity means a lava will be thick and slow moving, hence probably meaning an explosive eruption. lava's with a high viscosity include rhyolite and andesite whereas lava's with a low viscosity (runny ones) include basalt.
low viscosity lava due to the violent eruption of the volcano
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No. Pillow lava is basaltic, low-viscosity lava. Krakatoa is a stratovolcano with a style of ereuption more characteristic of high-viscosity andesitic lava.
Eyjafjallajokull Volcano has medium viscosity. The term "magma" is used to describe molten rock below the Earth's surface, while "lava" is used for molten rock that has reached the surface. Eyjafjallajokull's eruption in 2010 produced lava flows of medium viscosity.
Viscosity is a measure of a fluid's resistance to flow. Higher viscosity lava flows more slowly because it is more resistant to deformation and requires more force to move. Lower viscosity lava flows more quickly as it can deform and flow more easily.
The resistance to flow of lava depends on its viscosity, which is influenced by factors such as temperature, composition, and gas content. Lava with low viscosity (more fluid) flows more easily, while lava with high viscosity (more sticky) flows less easily. The resistance to flow can also be affected by topography and the presence of obstacles in the lava's path.
Mount Tambora typically produces highly viscous lava due to its high silica content. This results in the lava being thick and slow-moving, leading to more explosive eruptions.
The viscosity of lava flow from a cinder cone volcano is typically high, leading to slower-moving lava flows. This is due to the higher silica content of the lava, which increases its viscosity. As a result, cinder cone volcanoes often produce short, thick flows that can cool and solidify quickly.
The measure of a lava's mobility is called viscosity, which refers to the resistance of a substance to flow. Lava with low viscosity is more fluid and flows more easily, while lava with high viscosity is thicker and flows more slowly.