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Volcanic Eruptions. Mafic Lava  Dark colored  Rich in magnesium and iron  Formed from oceanic crust  Cools rapidly.

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Presentation on theme: "Volcanic Eruptions. Mafic Lava  Dark colored  Rich in magnesium and iron  Formed from oceanic crust  Cools rapidly."— Presentation transcript:

1 Volcanic Eruptions

2 Mafic Lava  Dark colored  Rich in magnesium and iron  Formed from oceanic crust  Cools rapidly

3 Felsic Lava  Light colored  Rich in silica  Formed from continental crust

4 Eruptions  Composition of lava determines the force of the eruption

5 Oceanic Eruptions  Erupt on the ocean floor and oceanic islands  Mafic lava  Very hot  Very thin (watery)  Flows easily

6 Continental Eruptions  Erupt on the land  Felsic lava  Cooler  Thicker  Contains large amounts of gases  Carbon dioxide and water vapor  Explosive

7 Mafic Lava  Pyroclastic material (tephra)-rock fragments ejected from volcanoes  Volcanic ash- less than 2 mm  Volcanic dust- less than.25 mm  Both can travel around the Earth in the atmosphere

8 Volcanic Cones  Piles of volcanic material around the vent

9 Volcanic cones  Shield cones  Cover wide areas  Broad at the base  Gentle slope  Quiet eruptions  Example Hawaiian Islands

10 Shield cones

11 Volcanic cones  Cinder cones  Explosive eruptions  Very steep slopes  Rarely more than a few hundred meters high

12 Cinder cones

13 Volcanic cones  Composite cones  Develop into high volcanic mountains  Alternating types of eruptions  Examples: Mount Fuji, Mount Hood, Mount St. Helens

14 Composite cones

15 Crater  Funnel shaped pit at the top of a volcanic vent

16 Caldera  Large basin shaped depression caused by an explosive eruption  Magma chamber below a vent, causing the volcanic cone to collapse

17 Predicting Volcanoes  Earthquakes  Temperature changes in rock around vent  Bulging of the surface of the volcano  Change in gases given off


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