1. Mt. Unzen, Japan, 1991 Dormant for 200 years Woke up in 1990; erupted into 1992 Lots of pyroclastics Killed the Krafts and Harry Glicken, a survivor of Mt. St. Helens Site of volcano warning system 1991 - 43 scientists and journalists were killed by a three-mile-long pyroclastic flow, a fast-moving river of hot gas and rock that can speed along at speeds up to 450 miles per hour.

2. Introduction to Volcanic Hazards 50 ‑ 60 erupt each year50 ‑ 60 –3 ‑ 4 in the US (mostly in Alaska) –Many potentially active in northwestern US and Alaska Often at remote locations Sometimes near population centers –Japan –Philippines, –Mexico –Indonesia

3. Introduction to Volcanic Hazards

5. Locations of Volcanism 1: Plate Boundaries Mostly along plate boundaries; 80% in the "ring of fire“. Molten rock, including small components of dissolved gases, produced where lithospheric plates interact with other earth materials is called MAGMA Lava- magma from a volcano Typically produce composite volcanoes, whose magma is high in silica content.

6. Locations of Volcanism 2: Hot spots Typically produce shield volcanoes, whose magma is low in silica content. Example: Hawaiian Islands

7. Volcano Types Shield volcanoes –Largest type Hawaii Iceland Indian Ocean Islands –Gentle slopes (about 10° ) –Among the tallest mountains –Generally non ‑ explosive eruptions: low silica basaltic flows –Some occurrences Pyroclastic materials (tephra) Lava tubes Calderas Rift zones (normal faults)

8. Volcano Types Cinder cones – Much smaller (few km 2 ) –Steeper (>30 ‑ 35°) –Mostly pyroclastic materials –Easily eroded-poorly preserved –Often initial phase

9. Volcano Types Composite/Stratovolcanoes –Many in NWUS (Rainier, St. Helens, Hood) – Andesitic (intermediate) –Layers of andesite/ pyroclastics –Slopes ± 30 ‑ 35° –May erupt explosively – considered to be “most destructive”, due to eruptive style

10. Three Types of Volcanoes Q: What sets the shape of these volcanoes? A: Magma viscosity, for the most part, which is determined by silica content and termperature

11. Mt. St.Helens – a typical composite volcano Before After Composite Volcanoes commonly produce Andesites – a silica-rich igneous rock http://www.youtube.com/watch?v=gewmUaR5sQo

12. Volcano Types Volcanic Domes – Siliceous, viscous magmas (rhyolite) –Mt. Lassen, CA –Mt. St. Helens

13. Volcanic Origins Occurrences –Mid ‑ oceanic ridges (basalts) Shield volcanoes in Iceland –Shield volcanoes over hot spots (Hawaii) –Composite volcanoes (subduction zones) Andesitic Common around Pacific Rim –Fissure Flows Columbia River Deccan Basalts, India South Africa

14. Volcanic Origins –Caldera eruptions Extremely explosive and violent Rhyolitic magmas Volcanic domes Craters, Calderas, and Vents –Craters Depressions around the tops of volcanoes Form by explosion or collapse May be flat bottomed or funnel shaped Much smaller than calderas Long Valley, Ca

15. Volcanic Features –Hot Springs and Geysers Old Faithful

16. Crater Lake, Oregon a good example of a caldera

17. Volcanic Features –Calderas Large diameter (20 + km) circular depressions Explosive ejection-large scale collapse May contain multiple vents None in Recent times –10 in the last 1My –3 in North America (Yellowstone, WY. and Long Valley, CA.) »Classified as resurgent Produce large amounts of pyroclastic debris (1,000 km 3 )

18. Caldera-Forming Eruptuion @ Yellowstones ~600 ka October 7, 2003

19. Caldera Migration

20. Volcanic Hazards Effects –Primary effects Flows Pyroclastics Release of gases –Secondary effects Debris flows Mudflows Floods Fires

21. Lava Flows Pahoehoe –Fast moving (m/hr) –Low viscosity, smooth textured Aa –Slow moving (m/day) –Blocky, sintered appearance Control methods –Bombing (most successful in Italy) –Chilling (most successful in Iceland –Deflection walls (being tried in Iceland) –Results have been mixed

22. Pyroclastic Hazards Blowing of tephra into the atmosphere Pyroclastic activity Volcanic ash eruptions or ash falls –Rock fragments –Volcanic glass –Gases Lateral blasts (Mt. St. Helens) Pyroclastic flows or ash flows –Cloud of rock fragments, glass, and hot gases flowing rapidly down slope –Hot avalanche, ignimbrite, nuee ardentes

23. Volcanic Hazards

24. A nueé ardente: Mt. St. Helens Pyroclastic Hazard

25. Pyroclastic Hazards Ash Fall –Cover large areas Thousands of square kilometers –Vegetation –Surface water –Structural damage –Health hazards –Transportation problems

26. Pyroclastic Hazards Ash Flows –Travel at high speeds –Contain very hot materials –Examples Martinique (Pelee, and St. Pierre) Mt. Unzen Montserrat (Plymouth)

27. Volcanic Gases Gases emitted –H 2 O most abundant gas emitted –CO 2 next –About 90% of emitted gases Hazardous gases seldom reach population centers –CO 2 (hazardous) Lake Nyos, Cameroon, West Africa Killed 1,700 people and 3,000 cattle Other gases –Most in small quantities SO 2, NO x, HF, H 2 S –May be injected high in the atmosphere

28. Lake Nyos

29. Debris Flows and Mud Flows Debris Flows –50% + of the particles are 2 mm or greater –Snow and ice melted by eruption –Mt. Redoubt, Alaska flow equals the Mississippi at flood stage Mudflows –50% of more of particles are smaller than 2 mm Examples –Mt. Rainier's old flows threaten large cities in Washington State (Tacoma and Seattle) –Armero, Nevada del Ruiz, Colombia (22,000 dead) –Potential large "landslides" along the north coast of the Island of Hawaii may generate large tsunamis

30. Debris-Mudflow Hazard Map

31. Case Histories Mount Pinatubo, Philippines Mount St. Helens, Washington Pompeii ‑ Herculaneum, Italy

32. Modern Vesuvius 3 around Bay of Naples Population density about 15,000/km 2 Herculaneum (79 A.D); 10m ash 5,000 residents, mostly escaped

33. Prediction of Volcanic Activity Seismic activity Geophysical monitoring Topographic monitoring Emitted gas monitoring Geologic history Volcanic Alert or Warning

34. Adjustment/ Perception of Volcanic Hazard