Volcanoes only occur on the boundaries between tectonic plates, and this is the same for earthquakes. this is why there are many volcanoes and earthquakes in Indonesia and the south East Asia region, but very few any where in Europe or Antarctica. So volcanoes don't occur within a tectonic plate.
Several minerals form in slow cooling magma. Some of those minerals are quartz, plagioclase feldspar, and potassium feldspar. These are the same minerals that are found in granite.
There are two known processes by which magma ceases to exist: by volcanic eruption, or by crystallization within the crust or mantle to form a pluton. In both cases the bulk of the magma eventually cools and forms igneous rocks.
Well there are minerals every where so then the minerals could end up in the magma and then go threw the rock cycle.
Booze is a liquid liquor, Ozone is a toxic (elemental) gas O3
magma is a mixture of several different types of rock.
Pyroclastic material is more likely to form with high viscosity magma.
Mafic magma is more likely to form volcanic rock. Mafic magma is rich in magnesium and iron, and tends to have lower viscosity and higher temperatures, allowing it to flow more easily to the surface and form volcanic rocks such as basalt.
igneous rocks usally form by cooled magma.
The metamorphosed limestone will most likely be a skarn or marble, both formed from contact with an intruding granitic magma.
basalt
magma
Pyroclasts can be formed by both basaltic and andesitic magma. Basaltic magma typically forms pyroclastic materials like scoria and ash, while andesitic magma can produce a variety of pyroclasts including volcanic bombs and pumice. The type of pyroclasts produced depends on factors such as the composition of the magma and the eruption style.
by magma
As magma cools, elements combine to form minerals.
You didnt even put nothing if you not gone answer the question dont put nun period
The magma has to crystalize...
The rock which will form will be marble because the limestone undergoes metamorphosis (partial recrystallisation).