Publications
Below are publications related to the Groundwater and Streamflow Information Program.
Filter Total Items: 1026
A semi-structured MODFLOW-USG model to evaluate local water sources to wells for decision support A semi-structured MODFLOW-USG model to evaluate local water sources to wells for decision support
In order to better represent the configuration of the stream network and simulate local groundwater-surface water interactions, a version of MODFLOW with refined spacing in the topmost layer was applied to a Lake Michigan Basin (LMB) regional groundwater-flow model developed by the U.S. Geological. Regional MODFLOW models commonly use coarse grids over large areas; this coarse spacing...
Authors
Daniel T. Feinstein, Michael N. Fienen, Howard W. Reeves, Christian D. Langevin
Identifying long term empirical relationships between storm characteristics and episodic groundwater recharge Identifying long term empirical relationships between storm characteristics and episodic groundwater recharge
Shallow aquifers are an important source of water resources and provide base flow to streams; yet actual rates of groundwater recharge are difficult to estimate. While climate change is predicted to increase the frequency and magnitude of extreme precipitation events, the resulting impact on groundwater recharge remains poorly understood. We quantify empirical relations between...
Authors
Arik Tashie, Benjamin B. Mirus, Tamlin Pavelsky
Paleomagnetic record determined in cores from deep research wells in the Quaternary Santa Clara basin, California Paleomagnetic record determined in cores from deep research wells in the Quaternary Santa Clara basin, California
Paleomagnetic study of cores from six deep wells provides an independent temporal framework for much of the alluvial stratigraphy of the Quaternary basin beneath the Santa Clara Valley. This stratigraphy consists of 8 upward-fining cycles in the upper 300 m of section and an underlying 150 m or more of largely fine-grained sediment. The eight cycles have been correlated with the marine...
Authors
Edward A. Mankinen, Carl M. Wentworth
Copper speciation in variably toxic sediments at the Ely Copper Mine, Vermont, United States Copper speciation in variably toxic sediments at the Ely Copper Mine, Vermont, United States
At the Ely Copper Mine Superfund site, Cu concentrations exceed background values in both streamwater (160–1200 times) and sediments (15–79 times). Previously, these sediment samples were incubated with laboratory test organisms, and they exhibited variable toxicity for different stream sites. In this study we combined bulk- and microscale techniques to determine Cu speciation and...
Authors
Bryn E. Kimball, Andrea L. Foster, Robert R. Seal, Nadine M. Piatak, Samuel M. Webb, Jane M. Hammarstrom
Testing and use of radar water level sensors by the U.S. Geological Survey Testing and use of radar water level sensors by the U.S. Geological Survey
The United States Geological Survey uses water-level (or stage) measurements to compute streamflow at over 8000 stream gaging stations located throughout the United States (waterwatch.usgs.gov, 2016). Streamflow (or discharge) is computed at five minute to hourly intervals from a relationship between water level and discharge that is uniquely determined for each station. The discharges...
Authors
Janice M. Fulford
Volcanogenic massive sulphide and orogenic gold deposits of northern southeast Alaska Volcanogenic massive sulphide and orogenic gold deposits of northern southeast Alaska
This five-day field trip visits the most significant mineral deposits in northern southeast Alaska. The trip begins and ends with regional transects in the interior Intermontane terranes around Whitehorse, Yukon, and the Insular terranes along the northern Chatham Strait region of southeast Alaska (Fig. A-1 and Fig. A-2; Plate-1). To put the deposits in a regional tectonic framework, the...
Authors
Patrick J Sack, Susan M. Karl, Nathan Steeves, J Bruce Gemmell
Late quaternary changes in lakes, vegetation, and climate in the Bonneville Basin reconstructed from sediment cores from Great Salt Lake: Chapter 11 Late quaternary changes in lakes, vegetation, and climate in the Bonneville Basin reconstructed from sediment cores from Great Salt Lake: Chapter 11
Sediment cores from Great Salt Lake (GSL) provide the basis for reconstructing changes in lakes, vegetation, and climate for the last ~ 40 cal ka. Initially, the coring site was covered by a shallow saline lake and surrounded by Artemisia steppe or steppe-tundra under a cold and dry climate. As Lake Bonneville began to rise (from ~ 30 to 28 cal ka), Pinus and subalpine conifer pollen...
Authors
Robert S. Thompson, Charles G. Oviatt, Jeffrey S. Honke, John McGeehin
Fire in the Earth System: Bridging data and modeling research Fire in the Earth System: Bridging data and modeling research
Significant changes in wildfire occurrence, extent, and severity in areas such as western North America and Indonesia in 2015 have made the issue of fire increasingly salient in both the public and scientific spheres. Biomass combustion rapidly transforms land cover, smoke pours into the atmosphere, radiative heat from fires initiates dramatic pyrocumulus clouds, and the repeated...
Authors
Srijn Hantson, Silvia Kloster, Michael Coughlan, Anne-Laure Daniau, Boris Vanniere, Tim Bruecher, Natalie M. Kehrwald, Brian I. Magi
Water isotope systematics: Improving our palaeoclimate interpretations Water isotope systematics: Improving our palaeoclimate interpretations
The stable isotopes of oxygen and hydrogen, measured in a variety of archives, are widely used proxies in Quaternary Science. Understanding the processes that control δ18O change have long been a focus of research (e.g. Shackleton and Opdyke, 1973; Talbot, 1990 ; Leng, 2006). Both the dynamics of water isotope cycling and the appropriate interpretation of geological water-isotope proxy...
Authors
M. D. Jones, S. Dee, L. Anderson, A. Baker, G. Bowen, D. Noone
Geomorphic evolution of the San Luis Basin and Rio Grande in southern Colorado and northern New Mexico Geomorphic evolution of the San Luis Basin and Rio Grande in southern Colorado and northern New Mexico
The San Luis Basin encompasses the largest structural and hydrologic basin of the Rio Grande rift. On this field trip, we will examine the timing of transition of the San Luis Basin from hydrologically closed, aggrading subbasins to a continuous fluvial system that eroded the basin, formed the Rio Grande gorge, and ultimately, integrated the Rio Grande from Colorado to the Gulf of Mexico...
Authors
Chester A. Ruleman, Michael Machette, Ren A. Thompson, Dan M Miggins, Brent M Goehring, James B. Paces
Regional and local correlations of feldspar geochemistry of the Peach Spring Tuff, Alvord Mountain, California Regional and local correlations of feldspar geochemistry of the Peach Spring Tuff, Alvord Mountain, California
The chemical composition of feldspar grains in an ignimbrite from the Spanish Canyon Formation in the Alvord Mountain area, California, have been used to confirm similarities in three measured sections locally, and they are similar to exposures of the Peach Spring Tuff (PST) regionally. Feldspar grains were identified on the basis of texture (zoning, as mantled feldspars, or in crystal...
Authors
David C. Buesch
South Park, Colorado: The interplay of tectonics and sedimentation creates one of Colorado’s crown jewels South Park, Colorado: The interplay of tectonics and sedimentation creates one of Colorado’s crown jewels
Recent mapping efforts and hydrocarbon exploration in the South Park Basin have brought to light the magnitude in complexity of a structural basin already recognized for its unique sedimentary and tectonic setting. This fi eld trip to one of Colorado’s scenic gems will examine how Paleozoic, Mesozoic, and Cenozoic strata record the tectonic signatures of at least three orogenic episodes...
Authors
Peter E Barkmann, Edward J Sterne, Marieke Dechesne, Karen J. Houck