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Ventura County California
High-resolution seismic reflection to improve accuracy of hydrogeologic models in Ventura County, California, USA
The Influence of Irrigation on Slope Movements, Ventura County, California, USA
Paleoseismologic Evidence for a Very Large ( M w >7), Post-A.D. 1660 Surface Rupture on the Eastern San Cayetano Fault, Ventura County, California: Was This the Elusive Source of the Damaging 21 December 1812 Earthquake?
Mapping Liquefaction Hazards in Simi Valley, Ventura County, California
New late Paleocene molluscs from the Simi Hills, Ventura County, California
Structural Analysis of Fractures in Cores from Saticoy Field, Ventura County, California
Stratigraphic Relations of Phosphate- and Gypsum-Bearing Upper Miocene Strata, Upper Sespe Creek, Ventura County, California: GEOLOGICAL NOTES
Late Cretaceous Paleogeography Near Wheeler Gorge, Ventura County, California
Relationship of Big Pine, San Guillermo, and Ozena Faults, Northwestern Ventura County, California: ABSTRACT
Foraminiferal Section Along Adams Canyon, Ventura County, California
Calcium Chloride Waters from Certain Oil Fields in Ventura County, California
Notes on the geology of Ventura County, California
The South Mountain oil field [Ventura County, California]
The Ventura (Avenue) [oil] field [Ventura County], California
The Oil Fields of Ventura County, California
Abstract Following the January 17, 1994, Northridge, California, earthquake (M = 6.7), Ventura County, California, experienced a major outbreak of coccidioidomycosis (valley fever), a respiratory disease contracted by inhaling airborne fungal spores. In the eight weeks following the earthquake (January 24 through March 15), 203 outbreak-associated cases were reported, which is about an order of magnitude more than the expected number of cases, and 3 of these cases were fatal. Simi Valley, in easternmost Ventura County, had the highest attack rate in the county, and the attack rate decreased westward across the county. The temporal and spatial distribution of coccidioidomycosis cases indicates that the outbreak resulted from inhalation of spore-contaminated dust generated by earthquake-triggered landslides. Canyons northeast of Simi Valley produced many highly disrupted, dust-generating landslides during the earthquake and its aftershocks. Prevailing winds after the earthquake were from the northeast, which transported dust into Simi Valley and beyond to communities to the west. The 3 fatalities from the coccidioidomycosis epidemic accounted for 4% of the total earthquake-related fatalities.