volcanoes
DESCRIPTION
Volcanoes. What is a Volcano?. A volcano is a vent in the earth’s crust through which hot gas, ash and molten rock flows. How do Volcanoes Form?. Subduction Zones. Hot Spots. Magma/Lava. Magma : molten rock located underground Lava: Molten rock that has reached the surface. Viscosity. - PowerPoint PPT PresentationTRANSCRIPT
VOLCANOES
What is a Volcano?A volcano is a vent in the earth’s crust
through which hot gas, ash and molten rock flows.
How do Volcanoes Form?Subduction Zones
Hot Spots
Magma/Lava
Magma: molten rock located undergroundLava: Molten rock that has reached the
surface
Viscosity
Viscosity is the resistance to flow of a fluid.The viscosity of magma is determined by the
amount of silica present.
High Viscosity Magma High amounts of silica results in thick slow
moving magma with high gas content
Low viscosity Magma Low amounts of silica results in thin, runny
magma with low gas content
Types and Characteristics of Magma
Basaltic Andesitic RhyoliticSilica Content Least (50%) Intermediate
(60%)(73%)
Gas Content Least Intermediate HighestViscosity Lowest Intermediate HighestType of
eruptionRarely
explosiveSometimes explosive
Explosive
Melting Temp. Highest Intermediate LowestType of volcano
Shield Composite Cinder Cone
Location Rifts and oceanic hot
spots
Subduction Zones
Contential Hot Spots
Types of Volcanoes
Shield VolcanoShield volcanoes are commonly found at
divergent plate boundaries and oceanic hot spots. Shield volcanoes are large with
gently sloped sides. The magma is mainly composed of basaltic magma which has a
low viscosity.
Shield Volcano
Cinder Cone
Small steep sided volcano which erupts gas-rich basaltic lava. It is formed when highly
viscos magma is thrown into the air from the vent, cooling and breaking into fragments
upon hitting the ground.
Cinder Cone
Composite Volcano
Composite volcanoes, sometimes called stratovolcanoes are characterized bylarge steep sides which are a result of
repetitive explosive eruptions of andesitic and rhyolitic lava and ash. This type of
volcano is mainly located along subduction zones.
Composite Volcano
Pyroclastic Flow
Explosive volcanoes can produce avalanches of hot gasses, ash, and rock. Pyroclastic flows can reach speed in excess of 100
km/h with temperatures greater than 10000 C.
Classification of Pyroclastic Material
AshDiameter less than 2 mm
LapilliDiameter from 2 mm to 64 mm
Lava Block or BombDiameter greater than 64 mm
Pyroclastic Flow
Lahars
Melted snow or ice creates a mudflow that rushes down the volcano at speeds in excess
of 100 km/h
Lahar
Caldera
Following an eruption, the walls of a volcano are weakened and collapse into the vent and
form a large crater shaped basin called a caldera.
Caldera
Crater Lake