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all geography including DSDP/ODP Sites and Legs
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Utah County Utah
LOWER MISSISSIPPIAN CRINOID (ECHINODERMATA) FAUNA FROM UTAH COUNTY, UTAH
Application of gravity and magnetic methods to assess geological hazards and natural resource potential in the Mosida Hills, Utah County, Utah
Potential Geologic Hazards near the Thistle Landslide, Utah County, Utah
Mapping groundwater contamination using dc resistivity and VLF geophysical methods; a case study
A Geotechnical Database for Utah (GeoDU) enabling quantification of geotechnical properties of surficial geologic units for geohazard assessments
CONODONT BIOSTRATIGRAPHY OF THE ORDOVICIAN OPOHONGA LIMESTONE IN WEST-CENTRAL UTAH
Comment on: When Landslides Are Misinterpreted as Faults: Case Studies from the Western United States
Depositional History of Paleocene—Lower Eocene Flagstaff Limestone and Coeval Rocks, Central Utah
Shallow subsurface structure of the Wasatch fault, Provo segment, Utah, from integrated compressional and shear-wave seismic reflection profiles with implications for fault structure and development
Is the Wasatch fault footwall (Utah, United States) segmented over million-year time scales?
Basement complexes in the Wasatch fault, Utah, provide new limits on crustal accretion
Paleoseismic Results from the Alpine Site, Wasatch Fault Zone: Timing and Displacement Data for Six Holocene Earthquakes at the Salt Lake City–Provo Segment Boundary
A Geophysical Investigation of Shallow Deformation Along an Anomalous Section of the Wasatch Fault Zone, Utah, USA
THE CRYSTAL STRUCTURE OF BILLINGSLEYITE, Ag 7 (As,Sb)S 6 , A SULFOSALT CONTAINING As 5+
Debris Basin and Deflection Berm Design for Fire-Related Debris-Flow Mitigation
Watershed reconstruction of a Paleocene–Eocene lake basin using Sr isotopes in carbonate rocks
Origin and emplacement of igneous rocks in the central Wasatch Mountains, Utah
Volumetric faults in field-sized reservoir simulation models: A first case study
12. Geochemistry of cave pools connected to an alpine epikarst—Timpanogos Cave National Monument, Utah
Weekly water samples collected in the spring and summer of 2012 demonstrate the dynamic geochemistry within the epikarst of an alpine karst aquifer in Timpanogos Cave National Monument in the Wasatch Mountains near Salt Lake City, Utah, USA. The results of chemical analysis of water from four cave pools, supplemented with concurrent samples from the American Fork River, suggest three modes of recharge: (1) diffuse recharge through the permeable matrix of the carbonate rock, (2) rapid recharge through open fractures in the epikarst, and (3) rapid recharge via piston flow through fractures occluded with colluvium. Water levels in the cave pools recharged by diffuse flow were very stable during the study period. Elevated dissolved solids characterized the geochemistry, including solutes associated with hydrothermal activity in this region (e.g., SO 4 2− and F − ). Isotopes of sulfur and carbon, along with cation-anion ratios suggest that sulfide oxidation may play some role in modern dissolution of the carbonate bedrock. In situ geochemical reactions influence the concentration of some solutes (e.g., HCO 3 − , Ca 2+ , F − ) and may cause a shift in the isotopes of dissolved inorganic carbon. Water levels in the cave pools characterized by rapid recharge, in comparison, were highly variable. When the flow path was direct, the geochemistry of the pool was strongly influenced by the timing and rate of recharge. During times of limited recharge, the geochemistry of these pools evolved toward the values of pools dominated by diffuse flow. On the other hand, when the flow path was impeded by colluvium, recharge was stored, and the geochemical signal was homogenized. In both cases, the source of recharge may be from elevations substantially above the cave pool.