Dry magma refers to magma that has a low water content, typically less than 1%. This type of magma is primarily composed of silicate minerals and is associated with more explosive volcanic eruptions due to its higher viscosity, which can trap gases and increase pressure. Dry magma is often found in tectonically active regions, where the conditions for its formation are prevalent. In contrast, wet magma contains more volatiles, which can lead to different eruptive behaviors.
How much dry ice? Regardless, a signifigant amount to all of the dry ice will sublime (solid CO2 will not melt under any atmospheric circumstances) and some to all of the magna will solidify into igneous rock. The results are dependent on the quantity of dry ice.
This is called the magma chamber.
Before lava reaches the surface it is called magma.
Molten rock under the surface is called "magma". When magma reaches the surface it is called "lava".
Magma is molten rock beneath the Earth's surface, while a magma chamber is a reservoir where magma is stored before it rises to the surface as lava. Essentially, magma is the molten rock itself, while a magma chamber is the space within the Earth where magma is stored.
combine dry ice and water
Basaltic magma is considered "dry" because it has relatively low water content compared to other types of magma. This is why basaltic eruptions tend to be less explosive compared to more water-rich magmas like andesitic or rhyolitic magmas.
How much dry ice? Regardless, a signifigant amount to all of the dry ice will sublime (solid CO2 will not melt under any atmospheric circumstances) and some to all of the magna will solidify into igneous rock. The results are dependent on the quantity of dry ice.
An acid magma or a granitic magma.
magma
This is called the magma chamber.
Before lava reaches the surface it is called magma.
basaltic,andesitic,rhyolitic
Molten rock under the surface is called "magma". When magma reaches the surface it is called "lava".
Magma is molten rock beneath the Earth's surface, while a magma chamber is a reservoir where magma is stored before it rises to the surface as lava. Essentially, magma is the molten rock itself, while a magma chamber is the space within the Earth where magma is stored.
Baslatic magma is hotter.
No. Magma is not alive.