No. Magma is molten rock with some gasses mixed in.
The ease with which it flows or how thin or thick it is. the more solid it is the higher the viscosity. As in Oil the thicker it is the higher the viscosity machine oil low viscosity, gearbox oil high viscosity.
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.
The ease with which it flows or how thin or thick it is. the more solid it is the higher the viscosity. As in Oil the thicker it is the higher the viscosity machine oil low viscosity, gearbox oil high viscosity.
this answer has to do with density if magma becomes less dense than rock it will rise to the top ,for example vegetable oil in water.
An acid magma or a granitic magma.
yes because the molten rock is heavy so the water floats on top of it like the oil and water experiment but even so, the heat of the magma would turn the water to steam faster than you can say two.
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.
Less dense materials rise to the top of magma due to buoyancy, similar to how oil floats on water. As magma cools and crystallizes, lighter minerals form and become less dense, causing them to ascend. This process leads to the formation of a stratified structure in the magma chamber, with denser materials settling at the bottom and lighter ones accumulating at the top. This separation is essential for the differentiation of igneous rocks.