Title: Volcanoes
1Volcanoes
2Concepts
- Location of active volcanoes
- Volcanism
- 3 categories
- Viscosity
- 5 types of extrusive volcanism
- Examples of each
- 3 types of lava flows
- Dangers of volcanic eruptions
3What do you notice about their locations?
4Volcanism
- Definition the origin and movement of magma
- Three categories
- Extrusive magma is expelled onto surface
- Intrusive magma solidifies in the shallow crust
near the surface. Can be exposed after
weathering. - Plutonic magma solidifies deep inside the crust.
- Viscosity The ability for lava to flow.
Reflective of the amount of silica present in the
magma. - LOW silica LOW viscosity nonexplosive
- HIGH silica HIGH viscosity explosive
5VolcanismExtrusive Examples
Mt. Shasta, CA
Mt. Fuji, Japan
6VolcanismIntrusive Examples
Right Stone Mountain, GA Below Devils Tower, WY
7VolcanismPlutonic Examples
85 Types of Extrusive Volcanism1. Shield Volcano
- Central vent allows magma from chamber to spill
out, slowly building the volcano in layers. - Produces wide, gently sloping mountains
- Best example Hawaiian volcanoes (right Mauna
Loa)
95 Types of Extrusive Volcanism2. Composite
Volcano
- Stratovolcano
- Central vent allows magma to come up from chamber
below - Produces symmetrical, steep-sloped mountains
- Most explosive type of volcano
- Examples Mt Fuji,Mt Shasta, Mt St Helens
105 Types of Extrusive Volcanism2. Composite
Volcano example Mt St Helens in 1980
115 Types of Extrusive Volcanism3. Caldera Volcano
- Formed when the upper part of a volcano collapses
- The magma chamber below is (partially or
completely) emptied after an eruption - The emptied magma chamber can no longer support
the weight of the overlying rock - The overlying rock collapses into itself, forming
a circular basin - Volcanic activity can continue if there is still
magma in the chamber below - Example Crater Lake, OR
125 Types of Extrusive Volcanism3. Caldera Volcano
example Crater Lake, OR
Crater Lake was formed after Mt Mazama (a
stratovolcano) erupted and collapsed back in on
itself.
135 Types of Extrusive Volcanism4. Cinder Cones
- Smallest mountain formation of all volcanic
landform types - Cone-shaped peaks build up from small, solid
particles, ejected into air by small volcanic
vent - Generally lt1,500 high
- Example Wizard Island
145 Types of Extrusive Volcanism4. Cinder Cone
example Wizard Island in Crater Lake, OR
155 Types of Extrusive Volcanism5. Lava Dome
- Plug Dome
- High-silica lava exits from a vent. Due to its
high viscosity (doesnt flow very fast or far),
it builds up into a dome. - Effectively plugs the main vent. Can still emit
ash, gases, and even lava. - Example Lava Dome in Mt St Helens crater.
163 Types of Lava Flows
- Aa
- Clinky
- Blocky, choppy lava flows that does not flow well
over land - Pahoehoe
- Smooth, unbroken lava
- Ropy surface
- Pillow Lava
- Lava emerges from underwater volcanic vents
- Lava cools crusts when it hits colder water
- When crust fractures, lava oozes out and creates
billowing pillows
17Aa
Pahoehoe
18Pillow Lava
19Dangers of Volcanic Eruptions
- Burning Hot Lava
- Earthquakes, Landslides and Tsunamis
- These are often related an earthquake might jar
some land loose, resulting in a landslide. The
earthquake may set off the tsunami. Also, if the
landslide falls into the ocean, can trigger a
tsunami. - Mudslides (Lahars)
- Ash Fallout
- Pyroclastic Flow (nuée ardente)
20Dangers of Volcanic EruptionsMudslide (Lahar)
examples
Mt. Pinatubo, Philippines 1991 eruption
Mt. St. Helens, WA 1980 eruption
21Dangers of Volcanic EruptionsAsh fallout
example Mt. Pinatubo, Philippines 1991 eruption
22Dangers of Volcanic EruptionsAsh fallout
example Mt. St. Helens 1980 eruption
23Dangers of Volcanic EruptionsPyroclastic flow
example Mt St Helens 1980 eruption
- Hot gases, ash, rock that become a fluid cloud
that move down the side of the volcano. Can
travel great distances. - nuée ardente French for glowing cloud