This process describes the creation of volcanoes. The eruption of the hot spot begins the generation of the magma within the volcano.
It is colder than the lower mantle.
The surface feature above the mantle plume is known as the "hotspot".
It is colder than the lower mantle.
The asthenosphere lies in, and is the upper ductile part of, the mantle. It is the layer directly underneath the lithosphere; the layer composed of the crust and uppermost rigid mantle.
The feature that marks the location where one tectonic plate is pushed underneath another plate is called a subduction zone. In these zones, the denser oceanic plate is typically forced down into the mantle beneath a lighter continental plate or another oceanic plate. This process can lead to the formation of deep ocean trenches and is often associated with volcanic activity and earthquakes.
It is colder than the lower mantle.
It is colder than the lower mantle.
The surface feature above the mantle plume is known as the "hotspot".
Kimberlite pipes are a common geologic feature where diamonds are found. These cylindrical volcanic rock formations bring diamonds to the Earth's surface from deep within the mantle. Diamonds are typically formed under high pressure and temperature conditions, and kimberlite pipes are one of the few mechanisms for bringing them to the surface.
It is colder than the lower mantle.
The layer underneath the crust is called the mantle. It is made up of solid rock that is capable of flowing slowly over long periods of time.
The mantle. Earth's layers are core, outer core, mantle, lithosphere, and crust.
The asthenosphere lies in, and is the upper ductile part of, the mantle. It is the layer directly underneath the lithosphere; the layer composed of the crust and uppermost rigid mantle.
the mantle
The outer mantle is part of the Earth's mantle that is closer to the surface, while the inner mantle is deeper within the Earth. The outer mantle is composed of solid rock that can flow slowly over geologic time, while the inner mantle is under higher pressure and temperature, making it more solid and rigid.
The mantle, followed by the outer core then the inner core
Convection Currents created by the mantle underneath! :)