I think it is the continental magma.
Continental crust.
The largest volumes of magma extruded on the continents are typically found along divergent plate boundaries, such as mid-ocean ridges. Here, magma rises from the mantle to create new crust as tectonic plates move apart. Examples include the East African Rift and the Mid-Atlantic Ridge.
Dark-colored magma is typically basaltic magma, which is rich in iron and magnesium. This type of magma is known for its low viscosity and ability to flow easily, commonly found in volcanic areas such as shield volcanoes.
magma is very hot so as it boils it moves the plates of the earth causing the continents to slowly move apart
it is a magma type
Igneous, the world magma really gives away the answer. Magma = Ignite Ignite is to do with fire, heat and flame etc.
Basaltic magma is produced at the coolest temperatures because it has a lower silica content and therefore has a lower melting point compared to other types of magma. This type of magma typically erupts quietly and forms basaltic rock, such as the kind found at mid-ocean ridges.
Gondwana rock type has been found across many southern continents, including South America, Africa, Antarctica, Australia, and the Indian subcontinent. These rocks formed when these continents were part of the supercontinent Gondwana, which existed over 500 million years ago.
well first go to google and the type temperate forest and then u will get your answer
Rhyolitic magma. This type of magma is found where the gases can't escape like in volcanic eruptions. Because the gas can not escape, the magma becomes viscous, resulting in the explosions being violent and unpredictable. The other type of magma is Basaltic magma. This can be found where continent plates are pulling away from each other and the magma is nearer the surface. This allows the gas to escape and therefore the magma is less viscous and doesn't result in explosive volcanoes, here eruptions are gentle and 'rifts' are more likely, where lava is persistent. I hope this helps! :)
Examples of magma include basaltic magma, andesitic magma, and rhyolitic magma. Basaltic magma is the most common type and is associated with oceanic volcanic activity. Andesitic magma has intermediate silica content and is found at convergent plate boundaries. Rhyolitic magma is highly viscous and contains high amounts of silica, commonly found in continental volcanic regions.
The average composition of magma in a composite volcano is andesitic. Composite volcanoes are highly variable though. They can erupt anything from basalt to rhyolite.