Have erupted at least oncewithin the last 10,000 years
Inactive/Dormant Volcanoes
Have not erupted in the past 10,000 years but still have a possibility to erupt
Effusive Eruptions
Characterized by outpourings of lava on to the ground
Shield Cone Volcanoes
Wide and somewhat flat
Form from a quiet eruption
Lava flows out quietly and for great distances
Low silica level
Low viscosity lava
High or low levels of gas
Composite Volcanoes (Strato Volcanoes)
Magma is rich in silica and much thicker than magma from a shield volcano
Gases get trapped inside this thicker magma
Form from explosive eruptions
Produce a lot of lava and ash
Small, with steep sides
High in silica
High viscosity magma
High levels of gas
Cinder Cone Volcanoes (Scoria Cones)
Magma has large amounts of gas trapped in it
Violent and explosive type of eruptions (single type of eruption)
Has tall, very steep sides
Low silica lava
High levels of gas
Simplest type of volcanoes
Volcanic Eruptions
Magmatic
Phreatic
Phreatomagmatic
Magmatic Eruptions
Produce juvenile clasts during explosive decompression of gas within magma that propels it forward
Strombolian
Hawaiian
Vulcanian
Pelean
Plinian
Strombolian Eruptions
Calmest of the eruption type
Lava is very hot, thin, and runny which allows for fast flowing lava flows
Fluid basaltic lava is thrown into the air in jets from a vent or line of vent
Vulcanian Eruptions
An eruption resulting from the release of large quantities of accumulated magmatic gas which lifts fine ash with great force high into the air
More violent and explosive than Strombolian eruptions, short, violent, relatively small explosion of viscous magma
Plinian Eruptions
The largest and most violent of all the types of volcanic eruptions
The eruption columns are usually shaped like a mushroom (similar to a nuclear explosion) or an Italian pine tree
Characterized by a very high ash cloud that rise upwards to 50,000 feet (almost 10 miles) high
Plinian Eruption
Mount Vesuvius, which erupted in 79 A.D. in Italy
Pelean Eruptions
Eruptions that occur when gas rich pasty lava accumulates to form a dome on volcano
"Glowing clouds" of gas and ash flew down the mountain at over 70 miles per hour
Occurs when a large quantity of gas, dust, ash and lava fragments are blown out of volcanoes crater
Phreatomagmatic Eruption
Characterized by an explosive water magma interaction through which large amount of steams and magmatic gases are released
Phreatic Eruptions
Also called steam blast eruptions
Driven by explosive expanding of steam resulting from cold ground or surface water coming into contact with hot rock or magma
Surtseyan Eruption
Kind of hydromagmatic eruption where magma interact explosively with shallow groundwater or surface water
Occur when undersea volcano matured enough to break the surface of the water
Submarine Eruption
Type of volcanic eruption that takes place beneath the surface of water
They generate at subduction zone and within the tectonic plate where hotspots can be located
Pillow lava are ejected
Subglacial Eruption
Interaction between lava and ice often under glacier
Occurs at areas of high latitude and high altitude
Vulcanian Volcanoes
Characterized by violent and explosive eruptions. Lava flows are fast-moving, intense, and short-lived. Typically produce lava with high silica content and higher viscosity. Also known as Strombolian Volcanoes or Fire Fountaining.
Shield Cone Volcanoes
Characterized by a gently sloping, flat-topped shape, resembling a shield. Formed from quiet eruptions with little to no explosive activity. Lava flows are calm, slow-moving, and can travel long distances. Typically produce lava with low silica content and low viscosity.
Phreatic Eruption
A steam-powered eruption, occurring when water interacts with hot rocks, without direct magma involvement.
Lava Flow
The flow of molten rock (lava) onto the surface, often from a vent or fissure.
Phreatomagmatic Eruption
Interaction between magma and water, producing explosive eruptions with a mix of pyroclastic flows and rock.
Magmatic Eruption
The eruption of magma (molten rock) from the Earth's interior, producing various types of eruptions.
Vulcanian Eruptions
Eruptions resulting from the release of large quantities of accumulated magmatic gas which lifts fine ash with great force high into the air. More violent and explosive than Strombolian eruptions, with viscous magma.
What's the difference?
Vulcanian Eruptions: more violent, explosive, and involve viscous magma, while Strombolian Eruptions are less violent, involve less viscous magma.