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.
Magma is not likely to form on the Earth's surface
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on the surface
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.
Pyroclasts can be formed of any type of magma. However, they are more likely to form with andesitic than basaltic magma. Rhyolitic magma will also readily form pyroclasts.
Pyroclastic material can form with magma of any composition, but it is more likely to form with high-viscosity magma.
Pyroclastic material is more likely to form with high viscosity magma.
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.
Rhyolitic magma, high in quartz and feldspar. Forms granite underground, rhyolite above ground.
basalt
magma
by magma
As magma cools, elements combine to form minerals.
The magma has to crystalize...
Large crystals form when a rock cools from magma slowly whereas smaller crystale form when there is a slow rate of cooling