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Magma with high silica content
The lower the viscosity is the hotter the magma is and faster it flows.Higher the viscosity is the cooler it is and slower it flows down.
The thickness of magma may be indicated by its measured temperature, its color, and the speed of its flow.
No. Shield volcanoes are fed by low-viscosity basaltic magma.
A magma's viscosity is directly related to its degree of silica content.
High temperature=low viscosityLow temperature=high viscosity
High temperature=low viscosityLow temperature=high viscosity
High temperature=low viscosityLow temperature=high viscosity
The three elements that determine viscosity in magma are:TemperatureSilicaOxides (gases)Viscosity changes the way in which magma will flow. Magma with low viscosity will flow much more easily than high viscosity magma.
The two main factors that affect viscosity are temperature and silica content. Higher temperatures lower viscosity while higher silica content increases viscosity.
Viscosity is the measure of a liquids resistance to flow. In the case of magma, the hotter it is, the lower the viscosity.
The viscosity decrease increasing the temperature.
Although other factors such as temperature and water content also affect the viscosity of magma, silica-rich magmas tend to be more viscous than silica-poor magmas in similar situations.
The temperature of the magma will affect its viscosity depending on its chemistry. Some minerals crystallize at higher temperatures than others, meaning that portions of the magma may have already solidified. At lower temperatures, the majority of the constituent minerals will have crystallized and solidified, leaving the magma highly viscous.
Viscosity is how thick the magma is and this can impact on how much a volcano erupts and how it flows.
Factors that determine the force of an eruption are magma viscosity and gas content.
Yes. Viscosity is the resistance of a fluid to flowing. A high viscosity means low flowing (I specifically mention this because this is a huge pitfall) When silica content increases, and when temperature decreases, the viscosity of a magma increases along with it.