Geosciences 470R/570R Volcanology: Physical Processes and Petrologic Applications Study Sheet for Final Examination on 13 May 2015 Emphasis on lectures, on major concepts; supported by required reading (papers); textbook provides context. Final will emphasize material since midterm. You should know the following: Types of volcanic landforms, e.g. Lava dome, Stratocone/stratovolcano/composite volcano, Caldera, Crater, Cinder cone, Shield volcano, Maar, Diatreme, Tuff ring, Tuff cone, Pillow lava, Littoral cone Time, length, volume scales Key terms necessary to understand magmas and to map volcanic rocks Phenocryst abundance, identity of and relative proportions of various phenocrysts and microphenocrysts, nature of groundmass (glassy, microcrystalline, vesicularity) Magma, melt; phyric, aphyric; obsidian, vitrophyre Flow foliation; basal, carapace, and foreset breccias Unwelded, partially welded, and welded; fiamme, compaction foliation, cooling unit Welded ignimbrites versus welded fall deposits; rheomorphism Lahar, mudflow, giant pumice horizon, jöhkulhlaup, hyaloclastite, pillow Lava dome versus resurgent dome Central vent eruption vs. ring-fracture eruption Maar, diatreme, tuff ring, tuff cone Basic physical properties of magmas Relative temperature ranges of terrestrial and extraterrestrial volcanic eruptions, e.g., komatiite > basalt > andesite > dacite > rhyolite > carbonatites > sulfur > cryovolcanic Principal controls on viscosity Differences in composition: Metaluminous, peraluminous, peralkaline Volatiles Geologic fluids present in or an essential ingredient necessary to form various types of volcanic products (e.g., surface water in lahars; glacial ice in jöhkulhlaups; silicate liquids in pahoehoe) Relative abundances in various compositions of rocks, especially water and sulfur Controls on solubility for major volatiles Plinian eruptive plumes and underlying vent (be able to sketch) Components (regions/phases); controls Primary versus secondary plumes Pyroclastic eruptive products, characteristics, transport mechanisms, and depositional controls 1 Fall deposits (both unwelded and, uncommonly, welded) Flow deposits (both block-and-ash flow and ignimbite/ash-flow tuff) Surge deposits Transport processes: Which are transported by: Mass-flow and resulting from gravitational collapse or explosive collapse of a lava dome? Suspension and favored by low particle concentration and subvertical particle trajectory? Mass-flow and resulting from eruptive column collapse or eruptive fountaining of pumice? Traction and favored by low particle concentration and subhorizontal particle trajectory? Suspension and favored by low magma viscosities and proximity to eruptive vent? Silicic lavas (be able to sketch the zoning diagrams) Eruptive sequence and processes; flow-dome complex; lava domes versus lava flows Primary features—zoning and controls Features developed during cooling—zoning and controls Zoning in ash-flow tuffs/ignimbrites (be able to sketch the zoning diagrams) Features developed during emplacement (standard ignimbrite flow unit)—layers, controls Features developed during post-emplacement welding and compaction—zoning, controls Features developed during cooling—zoning, controls Zoning in pyroclastic surge deposits (be able to sketch) Depositional facies (sandwave, massive, planar) Caldera cycle Three-fold stages [A. Precollapse volcanism; B. Ash-flow eruption and concurrent collapse; C. Resurgence and post-caldera deposition] and components of each Concept of repose times Ties to key examples (e.g., Long Valley, Valles; Creede; Yellowstone, Pantelleria) will help your understanding Eruptive styles: Eruptive behavior/characteristics and typical volcanic products Plinian Vulcanian Peléan Strombolian Hawaiian Surtseyan Intermediate, mafic, and ultramafic (including carbonatitic) lava flows Characteristics, including relative viscosities Controls Tube versus channel delivery of lava to the lava flow front Stratovolcanoes Characteristic behaviors (e.g. Hildreth and Lanphere, 1994) 2 Debris-avalanche deposits Hummocky topography Amphitheater/sector collapse Hydromagmatism Impact of water/mass ratio Controls by depth of aquifer, depth of water Volcanic hazards Lessons from Mount St. Helens, USA Lessons from Pinatubo, Philippines Lessons from Unzen, Japan Lessons from Nevado del Ruiz/Armero, Colombia (e.g., Voight, 1990) Threats at other sites Mineral deposits Major types of deposits relevant to volcanology Surficial landforms of porphyry deposits Extraterrestrial volcanism Key characteristics distinguishing Moon, Mercury, Venus, Mars, Jupiter, Io, Neptune Processes: Hot spots, plate tectonics, gravitational deformation, bombardment, surface heating Implications for presence or absence of plate tectonics; dead vs. dynamic planet Controls on sizes and types of volcanoes, including surface temperature, atmospheric pressure Cryovolcanism Volcanism and climate Weather vs. climate Layering of atmosphere: Troposphere, stratosphere, mesosphere Importance of injection of material into stratosphere Importance of magmatic composition (S content and explosivity) and hydromagmatism Importance of tropical vs. temperate vs. polar latitudes Spatial and time scales of climatic influences of volcanic eruptions 3