Magma is a term for rock in liquid form. It differs from lava only in 1 respect, its location. Whilst lava is the name for liquid rock released from a volcano in an eruption, magma is the name for liquid rock found beneath the surface of a planet. The temperature for magma is around 700-1300 degrees Celcius.
Magma can rise and lower at different levels magma can determine how the eruption happend by its rising level
High water content in the magma. This will flash vaporize when pressure is removed and the magma becomes lava, causing steam explosions in that lava.
The properties of the three types of magma depend with viscosity, density and temperature. This is usually determine by heat and how far the molten rock are far from the surface of the earth.
the two types of volcanic eruptions are magma and lava
Magma is a hot fluid from deep within the Earth's crust. The set of magma conditions that produce the most explosive eruptions are high viscosity and the presence of dissolved gases.
True. Many eruptions produce massive clouds of ash, gas, and pumice rather than lava. Phreatic eruptions, as another example, are essentially steam explosions.
The crystal and gas content and temperature of a magma help determine a volcano's eruption style. • Crystals in magma make it more viscous, so magma with a high crystal content is more likely to explode than flow. • Gases create explosions if they cannot easily escape from viscous magma, but they can also be released without explosions (or with only minor ones) from fluid magma. • High-temperature magmas usually erupt effusively, while low-temperature magmas cannot flow easily and are more likely to erupt explosively.
Its magma composition.different types of volcanic eruptions form different types of volcanoes
The properties of the three types of magma depend with viscosity, density and temperature. This is usually determine by heat and how far the molten rock are far from the surface of the earth.
the two types of volcanic eruptions are magma and lava
poopy blows it up
Magma is a hot fluid from deep within the Earth's crust. The set of magma conditions that produce the most explosive eruptions are high viscosity and the presence of dissolved gases.
True. Many eruptions produce massive clouds of ash, gas, and pumice rather than lava. Phreatic eruptions, as another example, are essentially steam explosions.
There are a few different types of volcanic eruptions, with all being potentially dangerous. Scientist have experimented with different ways to relieve the internal pressure causing the eruptions, including drilling into the magma pool and detonating underground bombs. However, there is to date no way to prevent volcanic eruptions.
There are effusive eruptions and explosive eruptions.
The crystal and gas content and temperature of a magma help determine a volcano's eruption style. • Crystals in magma make it more viscous, so magma with a high crystal content is more likely to explode than flow. • Gases create explosions if they cannot easily escape from viscous magma, but they can also be released without explosions (or with only minor ones) from fluid magma. • High-temperature magmas usually erupt effusively, while low-temperature magmas cannot flow easily and are more likely to erupt explosively.
The two main types of magma are mafic and felsic.
Caldera-forming eruptions do not involce lava flows but massive plumes of ash and pumice. The material produced is usually rhyolite. After a caldera-forming eruption, however, the composition can shift, especially since eruptions can be triggered by the mixing of different types of magma.
A Stratovolcano Composite Volcano.