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Volcanoes. Chapter 18 Page 498. 18.1 Zones of Volcanism. Volcanism = describes all the processes associated with the discharge of magma, hot fluids and gases. Ring of Fire. Active volcanoes that create a “ring” pattern in the pacific ocean
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Volcanoes Chapter 18 Page 498
18.1 Zones of Volcanism • Volcanism = describes all the processes associated with the discharge of magma, hot fluids and gases.
Ring of Fire • Active volcanoes that create a “ring” pattern in the pacific ocean • Typically volcanoes from convergent and divergent boundaries.
Convergent Volcanoes • Volcanoes that form from plates colliding or subducting. • Land volcanoes tend to be explosive
Divergent Volcanism • 2/3rds of volcanism underwater • The ocean ridges that form tend to release giant pillow lava. • Tend to be non-Explosive and large
Hot Spots • Volcano that forms NOT at a plate boundary. • Magma rises from HOT WEAK areas of the mantle • We can also measure the rate and direction the plates are moving by these
Anatomy of a Volcano • Conduit = tube • Vent = opening • Crater = depression around the vent Side vent = smaller opening Ash cloud = small cloud of ash
Calderas • Large crater that may have formed from a large explosion. • Sometimes forms into a lake
18.2 Explosive Eruptions • Tephra = is the erupted material from the volcano. • Can be solidified lava OR pieces of crust • Classified by size: • Less than 2 mm is called ASH • Largest is called BLOCKS
Explosion effects Ash can rise into atmosphere hurting: • Airplanes • Change in weather (Block sun’s rays therefore lower temps) • Death/disease • Food chain instability
Proclastic Flows • Clouds of ash and other tephra • Travels at speeds of 125 mph • Mixed with hot gases • up to temps of 700*C • Can kill thousands AFTER the explosion
Volcanic Gases • The more dissolved gases in the magma, the more explosive the magma is! • CO2, SO2, HSO4, H2O vapor • This will mix in the air to form ACID RAIN which changes the acidity or PH of the surround water supplies. • They may also increase in temperature due to bubbling magma underneath
Types of Volcanoes • 1. Shield Volcanoes • 2. Cinder Cones • 3. Composite Volcanoes • All three depend on 2 factors: 1.Type of material that forms it 2.Type of eruption
Shield Volcano • Broad, gently sloping, circular base • Largest type • Nonexplosive eruption which leaves layers of lava.
Cinder Cone • Formed from eruptions that eject small pieces of magma from the air. • The small pieces pile back around the vent causing the cinder cone shape. • Small and steep
Composite Volcanoes • Violent eruptions • Formed by layers of hardened chunks of lava from the eruptions alternating between explosions and oozing of lava • Cone shaped with concave slopes (larger than cinder)