Basaltic magma has the lowest melting temperature among the common types of magma, typically ranging from about 1000 to 1200 degrees Celsius. This type of magma is rich in iron and magnesium and has a lower silica content compared to other magmas like andesitic or rhyolitic magma. Its relatively low viscosity allows it to flow easily, often resulting in non-explosive volcanic eruptions.
Intermediate magma is formed through a combination of processes, primarily the partial melting of the Earth's crust and the mixing of different magma types. This type of magma typically has a composition between that of basaltic and granitic magmas, often resulting from the melting of sedimentary rocks or the contamination of basaltic magma with crustal materials. Additionally, subduction zone dynamics can contribute to the generation of intermediate magma, where water from subducting plates lowers the melting temperature of the surrounding mantle materials.
When the temperature reaches the lowest melting point of the mineral or minerals of which the rock is made.That depends entirely on what type of rock you have, and what it's made up of. Different substances have different melting points. Igneous rock has the highest, which means they don't melt easily. You'd have to know what types of materials are in the rock and look up their respective melting points in a chemistry book, or online. There is no one single answer to your question.
Temperature, among other factors, effects the viscosity(thickness) of magma. However, for the most part, the temperature of magma is relatively consistent because magma is the type of molten rock that has not yet exited the volcano, so there are fewer factors to effect the temperature.
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More iron and magnesium in magma can make it more dense and viscous. This can result in a thicker magma that is less likely to flow easily. It may also affect the melting temperature and can influence the type of volcanic eruptions that occur.
Basaltic magma is produced at the coolest temperatures because it has a lower silica content and therefore has a lower melting point compared to other types of magma. This type of magma typically erupts quietly and forms basaltic rock, such as the kind found at mid-ocean ridges.
Intermediate magma is formed through a combination of processes, primarily the partial melting of the Earth's crust and the mixing of different magma types. This type of magma typically has a composition between that of basaltic and granitic magmas, often resulting from the melting of sedimentary rocks or the contamination of basaltic magma with crustal materials. Additionally, subduction zone dynamics can contribute to the generation of intermediate magma, where water from subducting plates lowers the melting temperature of the surrounding mantle materials.
Temperatures of most magmas are in the range 700 °C to 1300 °C (or 1292 °F to 2372 °F), but very rare carbonatite melts may be as cool as 600 °C, and komatiite melts may have been as hot at 1600 °C
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Mount Shasta typically has andesitic magma, which is a type of intermediate magma that is common in subduction zone environments. This type of magma is rich in silica and forms from the partial melting of both oceanic and continental crust.
When the temperature reaches the lowest melting point of the mineral or minerals of which the rock is made.That depends entirely on what type of rock you have, and what it's made up of. Different substances have different melting points. Igneous rock has the highest, which means they don't melt easily. You'd have to know what types of materials are in the rock and look up their respective melting points in a chemistry book, or online. There is no one single answer to your question.
These are solids with covalent bonds.
Temperature, among other factors, effects the viscosity(thickness) of magma. However, for the most part, the temperature of magma is relatively consistent because magma is the type of molten rock that has not yet exited the volcano, so there are fewer factors to effect the temperature.
Type your answer here... Nonpolar molecules
Mineral composition of the magma, Rate of cooling of the magma, Temperature of the magma, Presence of volatiles and Amount of water present in the magma.
More iron and magnesium in magma can make it more dense and viscous. This can result in a thicker magma that is less likely to flow easily. It may also affect the melting temperature and can influence the type of volcanic eruptions that occur.
Igneous rock is not necassarily made of fire, it is made of magma melting to form it.