650 likes | 844 Views
Classroom presentations to accompany Understanding Earth , 3rd edition. prepared by Peter Copeland and William Dupré University of Houston. Chapter 5 Volcanism. Volcanoes. Plumbing System of a Volcano. Fig. 5.1. May 1990 Eruption of Kilauea, Hawaii. James Cachero/Sygma.
E N D
Classroom presentations to accompany Understanding Earth, 3rd edition prepared by Peter Copeland and William Dupré University of Houston Chapter 5 Volcanism
Plumbing System of a Volcano Fig. 5.1
May 1990 Eruption of Kilauea, Hawaii James Cachero/Sygma
Major difference between plutonic and volcanic rocks is texture, a reflection of cooling rate. Volcanic rocks
Nonvolatile material Material ejected from volcanoes • Lava: magma that has flowed on the surface of the Earth. • Tephra: fragments that solidified in the air during eruption.
aa pahoehoe Types of Lava
Aa Lava Pahoehoe Lava Fig. 5.3 Kim Heacox/DRX
Columbia Plateau Flow Basalts Fig. 5.2 Martin G. Miller
Pyroclastic flow Air-fall Mudflow (lahar) Tephra
Mixture of hot gases, ash, and rocks forming a super-heated and dense current capable of moving 150 km/hr. Pyroclasticflow (nueé ardente)
Pyroclastic Flow from the 1998 Eruption on Montserrat R.S.J. Sparks
Escaping a Pyroclastic Flow at Mount Unzen, Japan, 1991 Fig. 5.9 AP/Wide World Photos
Volcanic Bomb Fig. 5.7 Science Source/Photo Researchers
Volcanic Breccia Fig. 5.8 Doug Sokell/Visuals Unlimited
Pillow basalt Phreatic explosions Submarine eruptions
Pillow Lava Fig. 5.4 Woods Hole Oceanographic Institute
Phreatic Explosion in the Pacific Fig. 5.18 Maritime Safety Agency, Japan
Vesicular Basalt Fig. 5.5 Glen Oliver/Visuals Unlimited
Pyroclasic Eruption at Arenal Volcano, Costa Rica Fig. 5.6 Gregory G. Dimijian/Photo Researchers
Shield volcanoes Stratovolcanoes (composite) Domes and cones Fissure eruptions (flood basalts) Submarine eruptions Eruptive styles and landforms
Low-viscosity lava flows Low-silica magma — mafic Basalt Pahoehoe Aa Gently sloping flanks — between 2 and 10 degrees Tend to be very large Spatter cone — minor feature Shield volcanoes
Shield Volcano Fig. 5.10
Olympus Mons Shield Volcano NASA, Viking Orbiter 1
Formed of pyroclastics only Steep sides — ~30 degrees Relatively small Short duration of activity Cinder cones
Cinder Cone Fig. 5.12
Cerro Negro Cinder Cone, near Managua, Nicaragua in 1968 Fig. 5.13 Mark Hurd Aerial Surveys
Forms above a volcanic vent Viscous lava — usually silica-rich (or cooler magma) Associated with violent eruptions Volcanic domes
Inyo Obsidian Domes-California P. L. Kresan
Lava Dome Fig. 5.11 Lyn Topinka/USGS
Alternating pyroclastic layers and lava flows Slopes intermediate in steepness Intermittent eruptions over long time span Mostly andesite Distribution Circum-Pacific Belt (“Ring of Fire”) Mediterranean Belt Composite volcano
Composite Volcano Fig. 5.14
Mt Fujiyama, Japan Fig. 5.15 Raga/The Stock Market
Before May, 1980 Emil Muench/Photo Researchers
After May, 1980 David Weintraub/Photo Researchers
Depression at top of volcano produced during an eruption May have younger domes within it Caldera
Crater Lake, Oregon Fig. 5.17 Greg Vaughn/Tom Stack
Shiprock, New Mexico an exposed volcanic pipe (diatreme) Fig. 5.19 Fred Padula
When low-viscosity lava is issued from cracks in the Earth tens of kilometers long. Fissure eruptions
Fissure Eruptions Form Lava Plateaus Fig. 5.20
Laki fissure (Iceland) erupted in 1783 extruding the largest lava flow in human history. Fig. 5.21 Tony Waltham
Mafic lava — solidifies to basalt Fissure flows Plateau basalts Columnar structure or jointing Lava floods
Columbia Plateau Flow Basalts Fig. 5.2 Martin G. Miller
Welded Tuff: California Fig. 5.23 1 foot Gerals and Buff Corsi/Visuals Unlimited
Ash-flow Sheets Draping Topography, Japan Fig. 5.24 S. Aramaki
Caution: Volcanologist at Work Fig. 5.25 Maurice Krafft/Photo Researchers