The Earth's crust consists of several large plates that are constantly moving.
A volcano is an opening on the earth’s surface where molten rock (magma) can escape from below the earth’s surface.
Volcanic eruptions occur when magma rises to the surface through fissures or vents, often accompanied by explosive activity such as ash clouds and lava flows.
Plate tectonics is the theory that explains how these plates move, interact with one another, and create geological features on our planet.
Volcanic eruptions occur when magma rises to the surface through fissures or vents in the earth’s crust.
Shield Volcanoes - These volcanoes have gentle slopes and are formed by repeated lava flows over long periods of time.
Cinder Cone Volcano - A small cone-shaped volcano composed mainly of cinders and ash ejected during eruption.
There are three main types of volcanoes: shield volcanoes, composite volcanoes, and cinder cone volcanoes.
Shield Volcano - A type of volcano characterized by gentle slopes and broad bases, formed primarily by fluid basaltic lava flows.
A volcano is an opening in the Earth’s crust where lava, ash, rock fragments, hot gases, and steam can escape from below the surface.
Volcanic eruptions occur when magma rises to the surface through fissures or vents, which may be located along plate boundaries.
There are three main types of volcanoes based on their shape: