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Volcanism Volcanic Features Location and Types of Volcanic Activity Effusive Eruptions Explosive Eruptions Volcano Forecasting and Planning

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Page 1: Volcanism Volcanic Features Location and Types of Volcanic Activity Effusive Eruptions Explosive Eruptions Volcano Forecasting and Planning

VolcanismVolcanic Features  Location and Types of Volcanic Activity  Effusive Eruptions  Explosive Eruptions  Volcano Forecasting and Planning

Page 2: Volcanism Volcanic Features Location and Types of Volcanic Activity Effusive Eruptions Explosive Eruptions Volcano Forecasting and Planning

Volcanic Settings

Figure 12.24

Page 3: Volcanism Volcanic Features Location and Types of Volcanic Activity Effusive Eruptions Explosive Eruptions Volcano Forecasting and Planning

Shield and Composite Volcanoes

Figure 12.32

Page 4: Volcanism Volcanic Features Location and Types of Volcanic Activity Effusive Eruptions Explosive Eruptions Volcano Forecasting and Planning

EFFUSIVE ERUPTIONSGenerally at hots spots, spreading centers

Mantly comes directly to surface

Hot lava; low viscosity, very mafic, flows easily, gases escape easily

Forms shields, flood basalts

Page 5: Volcanism Volcanic Features Location and Types of Volcanic Activity Effusive Eruptions Explosive Eruptions Volcano Forecasting and Planning
Page 6: Volcanism Volcanic Features Location and Types of Volcanic Activity Effusive Eruptions Explosive Eruptions Volcano Forecasting and Planning

FLOOD BASALTS

Page 7: Volcanism Volcanic Features Location and Types of Volcanic Activity Effusive Eruptions Explosive Eruptions Volcano Forecasting and Planning

Columbia River basalt flow

Composite Volcano

Page 8: Volcanism Volcanic Features Location and Types of Volcanic Activity Effusive Eruptions Explosive Eruptions Volcano Forecasting and Planning

EXPLOSIVE ERUPTIONSFound at subduction zones

Magma low temp (800 degrees C), high viscosity, does not flow easilty, more felsic mineralogy, gases trapped, hard to predict explosions

Forms composite volcanoes, cinder cones, calderas, aerial bombs, nuee ardente gas flows, very destructive

Page 9: Volcanism Volcanic Features Location and Types of Volcanic Activity Effusive Eruptions Explosive Eruptions Volcano Forecasting and Planning

Composite Volcanoes

Figure 12.34

Page 10: Volcanism Volcanic Features Location and Types of Volcanic Activity Effusive Eruptions Explosive Eruptions Volcano Forecasting and Planning
Page 11: Volcanism Volcanic Features Location and Types of Volcanic Activity Effusive Eruptions Explosive Eruptions Volcano Forecasting and Planning

Nuee ardente: pyroclastic flow, of searing superheated gas and incandescent volcanic ash and dust

Mount Pelee, on the Carribean island of Martinique, 1902 eruption. All but 2 of the more than20,000 people in the town of St. Pierre were killed.

Page 12: Volcanism Volcanic Features Location and Types of Volcanic Activity Effusive Eruptions Explosive Eruptions Volcano Forecasting and Planning

Over a century ago, on August 26,1883, the island volcano of Krakatau ("Krakatoa") in Indonesia, a virtually unknown volcanic island with a history of violent volcanic activity, exploded with devastating fury. The eruption was one of the most catastrophic natural disasters in recorded history. The effects were experienced on a global scale. Fine ashes from the eruption were carried by upper level winds as far away as New York City. The explosion was heard more than 3000 miles away. Volcanic dust blew into the upper atmosphere affecting incoming solar radiation and the earth's weather for several years. A series of large tsunami waves generated by the main explosion, some reaching a height of nearly 40 meters (more than 120 feet) above sea level, killed more than 36,000 people in the coastal towns and villages along the Sunda Strait on Java and Sumatra islands. Tsunami waves were recorded or observed throughout the Indian Ocean, the Pacific Ocean, the American West Coast, South America, and even as far away as the English Channel. 

KRAKATAU: World’s largest explosion?