Recurrence Rates of Basaltic Volcanism in SP Cluster, San Francisco Volcanic Field, Arizona
Document Type
Article
Publication Date
7-1998
Digital Object Identifier (DOI)
https://doi.org/10.1130/0091-7613(1998)026<0655:RROBVI>2.3.CO;2
Abstract
A new compilation of 23 K-Ar and 40Ar-39Ar radiometric ages, stratigraphic and paleomagnetic correlations, and cone morphology from the SP cluster, San Francisco volcanic field, Arizona, is used to illustrate a quantitative approach to long-term volcanic hazards assessment for basaltic volcanic fields. SP cluster is a group of 67 basaltic cinder cones, tuff rings, spatter cones, and lava flows, all predominantly younger than 1700 ka. Relatively steady-state volcanic activity (1 volcano per 15 k.y.) has characterized the SP cluster since 780 ka. This activity has been concentrated in an ∼250 km2 area since about 300 ka. We estimate that the chance of an eruption in the SP cluster during the next 1000 yr has an upper bound (95% confidence level) of 13%. Spatial and temporal probability models further indicate with 90% confidence that an eruption will take place within this 250 km2 area of the SP cluster within the next 22–26 k.y., a rate of activity significantly greater than predicted by field-wide averages. Thus, spatial variations in recurrence rate of basaltic volcanism, such as those recognized in the SP cluster, should be considered in the formulation of hazard assessments.
Was this content written or created while at USF?
No
Citation / Publisher Attribution
Geology, v. 26, issue 7, p. 655-658
Scholar Commons Citation
Conway, F. M.; Connor, Charles B.; Hill, B. E.; Condit, C. D.; Mullaney, K.; and Hall, C. M., "Recurrence Rates of Basaltic Volcanism in SP Cluster, San Francisco Volcanic Field, Arizona" (1998). School of Geosciences Faculty and Staff Publications. 1669.
https://digitalcommons.usf.edu/geo_facpub/1669
