A magma containing not much silica (= SiO2). For example: a basaltic magma.
These magma's have a low viscosity since the lower the SiO2-content, the lower the viscosity; and hence flow easily (↔ a felsic magma).
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A low-silica magma has a lower concentration of silica oxide compared to high-silica magmas. This type of magma is typically associated with basaltic or mafic compositions, which have higher temperatures and lower viscosity, allowing for easier flow and the formation of shield volcanoes.
Silicic magma is term used to describe magma with a high silica content. The higher silica content makes the magma more viscous and traps gases. Volcanoes with silicic magma tend to have much more violent eruptions. Think Mt. St. Helens (silicic) vs. Mt. Kilauea (Basaltic).
Silicate magma is magma with high levels of silica in it. Silica is found in the Earth's crust and often mixes with magma.
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.
Baslatic magma is hotter.