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Shield Volcanoes

• Low angle constructed principally Basaltic Volcanoes of • Examples: and Kilauea, • Thin flows References: • Summit Encyclopedia of Volcanoes, pp. 283-289 • May have lateral zones • May have lava in the crater

Skaldbreidur

Mount Etna, Stratovolcanoes

• A volcano constructed of alternating layers of lava and pyroclastic materials • Steep slope angles (~35°) • Examples: Fuji, and Kliuchevskaya, Kamchatka • May exhibit persistent activity (Etna, ) • Volumes of erupted lava proportional to repose time structure Popocatepetl

Mount Augustine Cones in Arc Settings

• Tholeiitic or calc-alkaline compositions • Merge to • Continuous feeding from depth into a shallow chamber • May be associated with fissures and monogenetic cones • Cones may be truncated by edifice collapse – Example: Augustine,

Facies at a stratovolcano Monogenetic Volcano Fields

• Composed of volcanoes that erupt only once • Common edifice is a scoria cone • rings and small shields are also common • Example: Pinacate, Mexico • Vent systems are dikes or pipes (diatremes) Scoria Cones Scoria Cones

• Simplest and commonest volcanic form

• Characterized by three parameters Tuff Rings – Height, width, crater width

• Standard initial slope of 30o Pillow Lavas • Conical shape • Occur in several environments

Sunset Crater, Scoria Cone Section

Diatremes Tuff Cones

pipes • Massive deposits • Diatreme • Thickly bedded • Contains • Palagonitized • Ultramafic • Bedding up to 30o • Mixture of rocks , Italy •Wet surges • Driven by deep CO2 Tuff Rings

• Thinly-bedded Cerro Colorado, Mexico

• Poorly-indurated

• Beds less than 12o

• Sandwave beds

• Dry surges

Basaltic Scoria Cone Fields SanSan Francisco Francisco Volcanic Field • 10s to 1000s of cones • General elliptical shape • Aspect ratio of 2:1 to 5:1 • 10 to 70 km in length • Areas of extensional σ • Elongate perpendicular to 3 • Widespread in western USA • Pinacate example

Small Fields Fields

• North rim of Grand • Extensive sheets of lava flows Canyon • Flood the • Scoria cones aligned • Associate with crustal dilation along fault planes • May coincide with mass bioextinctions • Examples: Deccan, and Columbia River , USA Flow Units

• Compound lava flows • Overlapping pahoehoe flows • Interconnected lava shields • Lava ponds in depressions • Inward directed dips of large fields • Cut by numerous swarms+

Columnar Join

Shasta Central Volcanoes

• A volcano that erupts magmas of various compositions – to silicic • Many have a central composed of silicic rocks and domes • A shallow chamber is part of the eruptive system Volcano Interior

• The eroded core of these volcanoes may expose a pluton • Feeding system may be a ring complex • These may be a host for economic deposits

Alteration Zones

Silicic Silica Potassic Adularia Sericitic Argillic Clays, no mica

Chloritic Chlorite Propylitic , , Chlorite