A mountain or a hill with an opening that connects the earth's interior to its surface and from which a variety of materials from inside of the earth is ejected onto the surface
Volcanic landforms
Intrusive volcanic landforms
Extrusive volcanic landforms
Intrusive volcanic landforms
Formed when magma cools inside the earth's crust
Extrusive volcanic landforms
Formed on the surface by the cooling of lava as well as by the accumulation of solid volcanic material
Sill
A mass of magma which has solidified along the bedding plane
Laccolith
A mass of magma which has intruded between rock layers so that when it solidifies it causes the layer of rock above it to arch upwards
Dike
A mass of magma which cools across the bedding plane in a vertical or lateral direction
Batholith
A large dome-shaped mass of magma which is formed deep inside of the earth's crust and often acts as a magma chamber
Volcanic plug
A volcanic feature formed when magma hardens within the vent of an active volcano
Magma
Molten material inside of the earth
Lava
Molten material on the surface
Types of lava
Basic lava
Acidic lava
Basic lava
Hotter than acidic lava, has a low silica content, fluid in nature, able to flow faster and over longer distances
Acidic lava
Has a higher silica content, viscous in nature, flows more slowly and solidifies closer to the vent
Basic lava
Associated with calm or effusive eruptions
Acidic lava
Associated with explosive eruptions
Solid materials ejected from a volcano
Ash
Cinder
Bomb
Block
Ash
The finest solid material ejected from the volcano, can be very dangerous and hazardous
Cinders or lapilli
Pebble-shaped volcanic materials
Bombs
Larger materials with aerodynamic shapes
Blocks
The largest solid volcanic materials, may even be materials that have broken off the cone
Lava plateau
Formed from basic lava, where lava is ejected from a vent or a long crack and flows over a long distance, creating a generally flat area
Shield volcano
Formed where basic lava is ejected from a central vent and flows over long distances to create a cone that is low and has a gentle side
Acid lava dome
High dome-shaped volcanic cone with a narrow base and steep convex slopes, formed by the eruption of acidic lava
Composite cone (Strata volcano)
Large and steep cone with alternating layers of lava and ash
Ash and cinder cone
Volcanic cone with concave slopes formed from the accumulation of pyroclastic materials including cinder and ash
Caldera
Large basin-shaped depression formed when the top of an existing cone has collapsed after the summit or the top of the volcano has been removed by an explosive eruption
Volcanic eruptions
May result in volcanic structures increasing in size or the top of a volcano being blown off, creating calderas
Dormant volcano
A volcano which has not erupted for a long time but still has the ability to erupt
Extinct volcano
A volcano which has erupted in the past but has completely stopped erupting
Extinct volcanoes
May become subjected to processes of denudation such as erosion, weathering, or mass wasting, exposing intrusive landforms
Hot magma coming into contact with ground water can cause the ground water to be heated up and ejected as hot springs