Rhyolitic magma is a gas. The rhyolitic magma usually has to largest gas contents.
The most common dissolved gas in magma is water vapor, or H2O. Other important gases that may be present in magma and released during volcanic eruptions are carbon dioxide, sulfur dioxide, and hydrogen sulfide.
Various gasses escape from magma. Water vapor is the most abundant, but other common gasses include carbon dioxide and sulfur dioxide.
Magma in a shield volcano usually has a low gas content.
Volcanoes vary a lot in how they erupt. The most important factor is the gas content of the magma. All magmas have gases dissolved in them, in the same way that soft drinks have carbon dioxide dissolved in to make them fizzy. As the magma gets close to the surface, the pressure on the magma decreases. That causes some of the gas to bubble out of the magma. Magma with low gas content comes out of the volcano without violent explosions and then flows peacefully down the sides of the volcano.
Magma contains a variety of gasses, the most common of which are water vapor, carbon dioxide, and sulfur dioxide.
Rhyolitic magma is a gas. The rhyolitic magma usually has to largest gas contents.
The most common dissolved gas in magma is water vapor, or H2O. Other important gases that may be present in magma and released during volcanic eruptions are carbon dioxide, sulfur dioxide, and hydrogen sulfide.
Gas is stored in the Magma chamber at the bottom of the volcano, along with the magma.
Various gasses escape from magma. Water vapor is the most abundant, but other common gasses include carbon dioxide and sulfur dioxide.
It could be, but magma differs depending on its gas percentage. The lower gas percentage it has, the smoother the magma flows. if it has a high gas percentage, it is usually explosive.
The gas was trapped in the magma.
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Magma in a shield volcano usually has a low gas content.
Volcanoes vary a lot in how they erupt. The most important factor is the gas content of the magma. All magmas have gases dissolved in them, in the same way that soft drinks have carbon dioxide dissolved in to make them fizzy. As the magma gets close to the surface, the pressure on the magma decreases. That causes some of the gas to bubble out of the magma. Magma with low gas content comes out of the volcano without violent explosions and then flows peacefully down the sides of the volcano.
Typically, high viscosity, high gas magma results in a Plinian (explosive) eruption. The gas pulverizes the magma into ash and may form lateral pyroclastic flows.
At most depths, gas is dissolved in the magma under pressure. When the magma gets close to the surface the gas comes out of solution, forming bubbles which expand rapidly. If enough gas is present in the magma, this expansion results in eruptions that take the form of violent explosions and generate large clouds of ash.