Department of Geosciences
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- High-Resolution Electronic Supplement for "The San Andreas Fault paleoseismic record at Elizabeth Lake: Why are there fewer surface-rupturing earthquakes on the Mojave section?"Bemis, Sean P.; Scharer, Kate; Dolan, James (2021-03-05)This dataset consists of the electronic supplement for Bemis et al. (2021) published in the Bulletin of the Seismological Society of America. The files shared through the BSSA website have been saved at a reduced resolution to meet their file size limitation. This is a duplicate of that archive, but these files are saved at a higher resolution to ensure this data is universally accessible and permanently archived.
- James Cave Epikarst Monitoring Drip DataSchreiber, Madeline E.; Eagle, Sarah; Schwartz, Benjamin; Orndorff, William D.; Gerst, Jonathan (2013-05-07)James Cave is located in Pulaski County, Virginia and formed within the Cambro-Ordovician Conococheague formation. Continuous (10 minute interval) monitoring of cave drip rate and precipitation was conducted from late summer 2007 to winter 2013 using HOBO® tipping bucket rain gauges and multi-station data loggers. At the subsurface sites, drips were collected using tarps with areas of 2.43m2, 3.07m2, and 3.51m2 for MS1, MS2, and MS3, respectively. Precipitation was measured at the surface near the cave entrance.
- James Cave Epikarst Monitoring Temperature and Specific Conductance Data as of 120701Schreiber, Madeline E.; Eagle, Sarah; Schwartz, Benjamin; Orndorff, William D.; Gerst, Jonathan (2013-05-08)James Cave is located in Pulaski County, Virginia and formed within the Cambro-Ordovician Conococheague formation. Continuous (10 minute interval) monitoring of specific conductance and water temperature of cave drips and cave stream from January 2011 to winter 2013 using HOBO® conductivity loggers. At the subsurface sites, drips were consolidated using tarps with areas of 2.43m2, 3.07m2, and 3.51m2 for MS1, MS2, and MS3, respectively and funneled into a reservoir for measurement and logging of conductivity and temperature. These data are presented as the temperature compensated specific conductance. Additionally, this submission includes air temperature taken via HOBO® temperature sensors and loggers. The air temperature data are subject to considerable artifacts such as an increase in temperature during sampling events.