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Discover the wonders of volcanic activity, from types of volcanoes to the materials expelled, and their impact on the environment and climate. Learn about volcanic landforms and the distribution of volcanoes worldwide.
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I. Introduction From: Roman god of fire, Vulcan
I. Introduction From: Roman god of fire, Vulcan • What is a volcano? A conical mountain formed around a vent where lava, pyroclastic materials, and gases are erupted.
I. Introduction B. Volcanic activity: • Active • Dormant • Extinct
B. Volcanic Activity 1. Active volcanoes • activity in the last few centuries Ex: Vesuvius, 79 A.D. (50 times in 2000 yr) Ex: Mt. St. Helens (1980)
B. Volcanic Activity 2. Dormant volcanoes • “quiet” for the last hundred to thousands of years, but still have potential to erupt. Mt. Rainier
B. Volcanic Activity 3. Extinct volcanoes • No eruption in historical times • No signs of erupting again
Introduction C. Volcano Distribution • Most volcanoes occur in one of three areas: • Circum-Pacific (i.e. The Ring of Fire) • 60% • Mediterranean • 20% • Spreading centers • 10 – 15%
II. Volcanic materials • Three types of material expelled from volcanoes
Volcanic materials A. Lava (“the liquid”) • Molten rock
Volcanic materials A. Lava • Molten rock • Si affects viscosity
II. Volcanic materials A. Lava 1) Pahoehoe lava • Basaltic lava • Low viscosity
II. Volcanic materials A. Lava 1) Pahoehoe lava • Basaltic lava • Low viscosity • Cools moderately slowly • Ropelike appearance
II. Volcanic materials A. Lava 2) Aa lava (pronounced aa-aa) • Basaltic lava • Higher viscosity • Solidifies while flowing • Angular pieces
II. Volcanic materials A. Lava 3) Pillow lavas • Lava extruded underwater • Cools and contracts • Spherical masses • Ocean floor
II. Volcanic materials A. Lava (“the liquid”) B. Ash and pyroclastic material (“the solid”) • Airborne material ejected by a volcano • Classified based on size:
B. Ash and pyroclastic material (“the solid”) * Volcanic ash • Fine ash - <0.06mm • Coarse ash – 0.06mm to 2mm • Composition = rock, mineral, and volcanic glass
B. Ash and pyroclastic material (“the solid”) * Cinders • 2 mm and 64 mm • Composition - same as ash • Hazardous when falling
B. Ash and pyroclastic material (“the solid”) C) Bombs • Larger than 64mm • Molten rock solidifies in the air • Shapes vary
II. Volcanic materials C. Volcanic gases (“the gases”) • Volatiles • H2S – Hydrogen sulfide • H2O – Water vapor • SO2 – Sulfides • CO2 – Carbon dioxide • N2 – Nitrogen • HCl – Hydrochloric Acid • Significance?
II. Volcanic materials A) Determines violence of an eruption • High gas = violent eruptions • Violent eruptions = felsic magmas • High viscosity magma traps gas • Expansion is prevented, pressure builds
II. Volcanic materials B) Effects on global climate • CO2 – Greenhouse gas • SO2 – Blocks sunlight
II. Volcanic materials • Hazards to humans • Clouds of CO2 get released • Travels across the ground
III. Volcanic Landforms • An erupting volcano will produce a number of distinct landforms including: A. Volcanic cones B. Flood basalts C. Calderas
A. Volcanic cones Three types of volcanic cones:
A. Volcanic cones 1) Shield volcanoes • Multiple layers of basaltic lava • Shallow sides due to magma’s low viscosity • Gentle eruptions
A. Volcanic cones 1) Shield volcanoes • Tall volcanoes –3 or 4 miles tall • Wide base – Diameter of ten of miles
A. Volcanic cones • Mauna Loa volcano, Hawaii
1996 1997
A. Volcanic cones 2) Cinder cones – • Smallest volcanic cone • Layered ash and cinders Ex: El Paricutin
A. Volcanic cones 2) Cinder cones • Short, narrow cone, • Steep sides • Violent eruptions