Volcanoes Notes
Volcanism
- Volcanism is the process where molten magma from the mantle moves to the Earth's crust.
Volcano Anatomy
- Eruption cloud
- Ash (tephra) fall
- Eruption
- Prevailing wind
- Bombs
- Pyroclastic debris
- Landslide
- Magma
- Pyroclastic flow
- Fumaroles and hot springs
- Ground
Plate Convergence and Volcanism
- Ocean-Ocean Convergence
- Mid-ocean ridge
- Ocean plate
- Asthenosphere
- Hot spot volcanism
- Active volcano over hot spot
- Extinct volcano
- Mantle plume
- Ocean-Continent Convergence
- Progressively older
- Wave erosion
- Mantle plume
- Subsiding seafloor
Types of Volcanism
Intrusive Volcanism
- Occurs when magma forms igneous intrusions into the rocks of the Earth's crust.
- Ancient Volcanic Features:
- Ash plume
- Cinder cone
- Recent lava flows
- Stock with radiating dikes
- Palisade
- Stock
- Volcano conduit
- Laccolith
- Sill
- Dike
- Magma chamber
- Pluton
- Batholith
- Batholith:
- The largest type of igneous intrusion.
- Forms deep in the crust.
- Large round shape.
Granite Dome
- A batholith exposed on the surface.
Laccolith
- Mushroom-shaped structure where magma forces the overlying strata upwards.
- Size: 100s of meters.
Lopolith
- Similar to a laccolith.
- The weight of the overlying strata causes the lopolith to sink into a saucer-shaped structure.
Sill
- Forms where magma intrudes horizontally between layers of rock.
Dyke
- Forms when magma intrudes vertically between layers of rock.
Extrusive Volcanism
- When magma reaches the surface it is called lava.
- The volcano also ejects rocks, ash, and steam.
- Gases emitted include sulfur dioxide, carbon dioxide, and nitrogen.
Volcanic Eruptions
- Steam raises the humidity of the air, causing heavy rain.
- Rain combines with ash and dust to form mud.
- The central pipe is widened, and a crater is formed.
Composite Volcano
- Consists of alternating layers of ash and cinders and lava.
- Cone-shaped.
- Side vents or fissures allow trapped magma to reach the surface.
- Conelets are built up on the sides of the volcano.
- Other types: shield cone, cinder cone.
Volcano Diagram
- Lava
- Older Layers
- Gases, Ashes, & Cinders
- Crater
- Dike
- Sill
- Magma Under Pressure
Types of Volcano
- Fissure volcano:
- Gentle basaltic slope of lava
- Shield volcano:
- Gentle slope of basaltic lava
- Dome volcano:
- Steep convex slope from thick, fast-cooling lava
- Ash-cinder volcano
- Composite volcano
- Caldera volcano:
- New cone
- Branch pipe
- Old cone
Calderas
- Form when a volcano has not erupted for a long period of time.
- Lava builds up and solidifies in the crater.
- A huge explosion blows off the top of the mountain.
Lake in a Caldera
- Sometimes the caldera will fill with water to form a lake.
Lava Plateaus
- Fissure eruptions occur when lava flows from a number of cracks.
- The lava is very fluid and flows for thousands of kilometers.
- The lava cools and solidifies into volcanic rock (basalt).
- Example: The highest parts of the Drakensburg (1300 m thick).
Active and Dormant Volcanoes
- Active: volcanoes which still erupt.
- Dormant: volcanoes which are resting (recorded activity in the past).
- Extinct: volcanoes that have not erupted in recorded history.
Active Volcanoes, Plate Tectonics, and the "Ring of Fire"
- Eurasian Plate
- North American Plate
- Pacific Plate
- Antarctic Plate
Examples of Volcanoes
- Vesuvius
- Vulcano
- Stromboli
- Mt. Etna
Effect of Volcanoes on People
- Lava flows burn and bury vegetation and buildings.
- Ash can cover buildings and smother vegetation.
- Respiratory problems due to breathing in ash and poisonous gases.
- People can be killed by lava bombs.
- Volcanoes set off mud slides.
Positive Effects of Volcanic Activity
- Volcanic ash can act as a fertilizer for soil.
- Lava weathers into fertile soil.
- Hot springs and geysers are associated with volcanoes and they become tourist attractions.
- Underground heated water and steam is used for electricity and heating systems.
Geothermal Power
- Production Well
- Injection Well