sisselülitumise
Sisselülitumise is a concept in geology that refers to the rise of magma or gas-rich fluids to the Earth's surface through a fissure or volcanic eruption. This process involves the rapid movement of magma from depth to the surface, often resulting in the displacement of overlying rock or the creation of new volcanic landforms.
Sisselülitumise is often considered the opposite of volcanic cone formation, in which magma is more slowly
There are two main types of sisselülitumis: inflationary and effusive. Inflationary sisselülitumise occurs when magma accumulates
Sisselülitumise is an important process in shaping the Earth's surface, particularly in areas of plate tectonic