Cone Morphology, Volcanic Deposits, and Eruption and Deposition Mechanisms at Red Mountain, Northern Arizona
dc.contributor.author | Holm, Richard F. | |
dc.contributor.author | Wade, William J. | |
dc.date.accessioned | 2024-03-05T20:41:16Z | |
dc.date.available | 2024-03-05T20:41:16Z | |
dc.date.issued | 2024-02-29 | |
dc.identifier.citation | Holm, R.F. and Wade, W.J., 2024, Cone Morphology, Volcanic Deposits, and Eruption and Deposition Mechanisms at Red Mountain, Northern Arizona. Arizona Geological Survey Contributed Report, CR-24-A, 19 p. | en_US |
dc.identifier.uri | http://hdl.handle.net/10150/671107 | |
dc.description | Red Mountain is a composite tuff cone in the San Francisco volcanic field in northern Arizona; its morphology is unique. A large amphitheater-like valley cuts deep into the northeast side, exposing over 900 feet of firmly cemented tuffs. A large breach penetrates the west side. The slopes of the cone are concave, reflecting bedding dips that flatten from the summit to the base. The cone height to basal width ratio is 28 % smaller than the ratios of young, fresh cinder cones. The tuffs are grouped into two lithologic types: (1) palagonitic lapilli tuffs and thin fine-ash tuffs, and (2) scoriaceous lapilli tuffs. Groups 1. and 2. are interlayered in beds centimeters to decimeters to meters thick. Outcrop textures, structures, sorting, bedding characteristics, and colors indicate that group 1 tuffs originated by hydromagmatic steam explosions, and deposition by wet base surges and fallout from ash clouds. Group 2 tuffs originated by Strombolian blasts and ballistic-fall deposition. The eruption occurred during the middle Pleistocene (0.740+/-110 Ma), concurrent with a cold period when the water table could have been high, perhaps in the cavernous Kaibab Formation. Here, Strombolian blasts could have been followed quickly by resupply of ground water for steam explosions. The amphitheater’s origin is ambiguous. Erosion is the simplest explanation. | en_US |
dc.language.iso | en | en_US |
dc.publisher | Arizona Geological Survey (Tucson, AZ) | en_US |
dc.relation.ispartofseries | Arizona Geological Survey Contributed Report | en_US |
dc.relation.url | https://library.azgs.arizona.edu/ | en_US |
dc.rights | Arizona Geological Survey. All rights reserved. | en_US |
dc.rights.uri | http://rightsstatements.org/vocab/InC/1.0/ | en_US |
dc.subject | Red Mountain | en_US |
dc.subject | volcanology | en_US |
dc.subject | volcanic eruptions | en_US |
dc.subject | geomorphology | en_US |
dc.subject | northern Arizona | en_US |
dc.subject | geochemistry | en_US |
dc.subject | composite volcano | en_US |
dc.subject | Volcanic ash, tuff, etc. -- Arizona -- Coconino County. | en_US |
dc.subject | San Francisco Volcanic Field | en_US |
dc.title | Cone Morphology, Volcanic Deposits, and Eruption and Deposition Mechanisms at Red Mountain, Northern Arizona | en_US |
dc.contributor.department | Northern Arizona University | en_US |
csdgm.bounding.west | 35.24768366235605, -112.50186675924878 | en_US |
csdgm.bounding.east | 35.19274822447731, -110.9481473510868 | en_US |
csdgm.bounding.north | 35.79881565052138, -111.77160683969382 | en_US |
csdgm.bounding.south | 34.92815425496206, -111.68548571866557 | en_US |
dc.description.collectioninformation | Documents in the AZGS Documents Repository collection are made available by the Arizona Geological Survey (AZGS) and the University Libraries at the University of Arizona. For more information about items in this collection, please contact azgs-info@email.arizona.edu. | en_US |
refterms.dateFOA | 2024-03-05T20:41:17Z |