What are the three types of volcanoes and what type of eruptions does each volcano have?
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Transcript of What are the three types of volcanoes and what type of eruptions does each volcano have?
What are the three types of volcanoes and what type of
eruptions does each volcano have?
What do you know about volcanoes?
And…Do you know of
any famous volcanoes?
Volcanoes
The cause of it all…• What do you think causes volcanoes to
erupt?
• The shift in the Earth’s plates are what causes volcanoes to form and erupt.
• As the plates join or separate some of the molten rock is exposed.
Where do volcanoes erupt?There are three places…
• Convergent plate boundaries – where two of Earth’s plates join together
• Divergent plate boundaries – where two of Earth’s plates move apart RING OF FIRE!!
• Hot spots – active areas below the earths crust
Volcanoes of the World
Structure of a Volcano
• Magma – the molten, or liquid-like, rock within the Earth
• Lava – magma that reaches Earth’s surface and is exposed to O2 (two types of lava are Pahoehoe and Aa)
• Viscosity~ Low viscosity = water high viscosity = maple syrup
• Vent – an opening through which molten (liquid-like) rock flows onto Earth’s surface
• Crater- the central opening at the top or summit of volcano.
• Volcanoes always have one central vent, but can also have several smaller side vents.
•(thickness), resistance of a liquid to flow.
Structure of a Volcano
magma
central vent
side vent
lava
old layers of lava
ash cloud
Earth’s crust
Stages of a Volcano• Magma chamber- the chamber below the volcano
that stores the magma.
• Without a magma chamber attached to the volcano it will be come extinct. With it, it is still considered active.
• If the volcano is still attached to its magma chamber but hasn’t erupted recently (100 years) it is considered to be dormant. It can still erupt at anytime!!
Types of VolcanoesThere are three major types of
volcanoes:
Shield volcanoesComposite volcanoesCinder cone volcanoes But there is also a fourth major
volcanoeLava domes
Shield Volcanoes• The flowing lava gives the volcano
gently sloping sides.• They have mild Eruptions that can
occur several times. • The lava tends to flow great
distances. • The magma rich in iron and
magnesium and is very fluid (low viscosity).
Shield Volcanoes• They have mild Eruptions that can
occur several times.• Mauna Loa and Kilaeua in Hawaii are
examples of a shield volcanoes.
Mauna Loa (Shield Volcano)
Kilauea Caldera
Kilauea Crater
Composite Volcanoes
• They have much steeper slopes than shield volcanoes.
• They have alternating layers of lava and cinders.
• Eruptions can be flowing lava or explosions. Explosive eruptions come from the trapped gases and produce cinders and ash.
Composite Volcanoes
• The magma is rich in silica and much thicker than magma from a shield volcano.
• Gases get trapped inside this thicker magma.
• Mount Fuji in Japan and Mount St. Helens in Washington State in the US are examples of composite volcanoes.
Mt. Fuji (Composite Volcano)
• Stands over 13,000 ft. tall
• Surrounded by 5 lakes• Last erupted in 1707-
08.
Mount St. Helen’s Composite Volcano
Mount St. Helen’s Thermal Imaging
Mount St. Helen’s before and after
eruption
1979 1980
Cinder Cone Volcanoes
• Cinder Cones have very steep sides!• Usually only active for a short time and then
become dormant (inactive).
• The magma inside a cinder cone volcano has large amounts of silica (63%) and gas trapped in it.
• The large amounts of hot ash and lava thrown out of the vent fall to the ground forming the cone shape that these volcanoes have.
Cinder Cone Volcanoes
• Violent and explosive eruptions because of all the gas trapped in the magma.
• Paricutin in Mexico and Mount Vesuvius in Italy are examples of a cinder cone volcanoes.
Paricutin Volcano (Cinder Cone)
• Grew over 5 stories in the first week• Continued to erupt for 8 years
reaching a height of over 1,300 ft.
Mount Vesuvius
What do you notice in this picture?
Mount Vesuvius Thermal Imaging
Volcanic Dangers• Pyroclastic flows• Lahars• Lava• Volcanic ash• Volcanic gas
Which volcanic danger kills most people?Volcanic
Ash
Pyroclastic flows• Pyroclastic flows
mixtures of hot gases, ash and rocks that travel about 450mi/hr down the sides of volcanoes.
• Dangerous because… • The poisonous gases
can be as hot as 1,000 degrees.
• They destroy anything in its path!
• They are rare and don’t happen in every eruption!
Pyroclastic Flows can even travel across
water!
Ash and Pumice distribution
People of Pompeii
Animals of Pompeii
Lahars• Lahars are
mudflows formed by the mixing of volcanic particles and water.
• Dangerous because…
• Carry large boulders and logs down the side of a volcanoes.
• Can easily crush or shear off anything in its path!
Damage caused from Lahars
Lava• Lava is molten rock expelled by a
volcano during an eruption. • Lava is a liquid at temperatures
ranging from 1,300 °F to 2,200 °F. • Although lava is about 100,000 times
the viscosity of water, it can flow great distances before cooling and solidifying.
• Dangerous because…• Lava can kill people, animals, and
destroy property and even bury entire towns!
Types of Lava• Pahoehoe
lava is runny and fast moving (up to 50 km/h).
• Has high iron content.
Pahoehoe Lava
Types of Lava
• Aa flows are chunky and slow moving lava flows
• Has a high silica content
Aa Lava
Kona Lava Fields
Lava Tubes
Thurston’s Lava Tube