Shaul Hurwitz
I am a research hydrologist with the USGS Volcano Science Center. My goals are to characterize and quantify the myriad processes occurring in volcano-hydrothermal systems that take place at spatial and temporal scales that span many orders of magnitude.
My research is focused on quantifying processes in continental hydrothermal systems by integrating hydrologic, geochemical, and geophysical data with models of groundwater flow, heat transport, thermodynamics, and statistics. An improved understanding of hydrothermal systems is important because: 1) pressure, temperature and chemical changes within these systems can provide early warnings of volcanic unrest, 2) many of the geochemical, geodetic, and seismic signals measured at the volcano’s surface have their origins, or are modulated by hydrothermal processes, 3) hydrothermal fluids constitute a major source of hazard as a propellant in steam-driven explosions, lubricant in mudflows, and transport agent for toxins, 4) fluids in these systems are a source of geothermal energy and an agent in the formation of mineral deposits, and 5) hot springs and their deposits provide insights on the origin and environmental limits of life on Earth and elsewhere in the solar system. Insights gleaned from these studies have implications for many science disciplines and are mostly summarized in co-authored review papers. This research supports of the USGS Volcano Hazards Program mission to “enhance public safety and minimize social and economic disruption from eruptions” and the Geothermal Research Investigation Project’s (GRIP) goals of assessing geothermal energy resources and the environmental impacts of energy production.
Research topics:
- Water-gas-rock interaction in volcano-hydrothermal systems using field observations, chemical and isotopic data, controlled laboratory experiments. and thermodynamic models
- Numerical simulations of volcano-hydrothermal systems
- Modulation of volcanic and geyser activity by cyclic hydrological and climatic forcers and by large earthquakes
- Post-glacial hydrothermal activity at Yellowstone
- Heat transport in volcanic systems
- Dynamics and chemistry of volcanic lakes
- Geyser dynamics
- The impact of geothermal energy production on groundwater quality
Education and Certifications
PhD (1999), The Hebrew University of Jerusalem
Science and Products
Dynamics of the Yellowstone hydrothermal system
Triggering and modulation of geyser eruptions in Yellowstone National Park by earthquakes, earth tides, and weather
Ca, Sr, O and D isotope approach to defining the chemical evolution of hydrothermal fluids: example from Long Valley, CA, USA
Constraints on the upper crustal magma reservoir beneath Yellowstone Caldera inferred from lake-seiche induced strain observations
Eruptions at Lone Star Geyser, Yellowstone National Park, USA, part 1: energetics and eruption dynamics
Temporal variations of geyser water chemistry in the Upper Geyser Basin, Yellowstone National Park, USA
Mechanics of Old Faithful Geyser, Calistoga, CA
Heat flow in vapor dominated areas of the Yellowstone Plateau volcanic field: implications for the thermal budget of the Yellowstone Caldera
Temperature data from wells in Long Valley Caldera, California
Note from the Hubbert Quorum
Climate-induced variations of geyser periodicity in Yellowstone National Park, USA
Boiling water at Hot Creek— The dangerous and dynamic thermal springs in California’s Long Valley Caldera
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Dynamics of the Yellowstone hydrothermal system
The Yellowstone Plateau Volcanic Field is characterized by extensive seismicity, episodes of uplift and subsidence, and a hydrothermal system that comprises more than 10,000 thermal features, including geysers, fumaroles, mud pots, thermal springs, and hydrothermal explosion craters. The diverse chemical and isotopic compositions of waters and gases derive from mantle, crustal, and meteoric sourceAuthorsShaul Hurwitz, Jacob B. LowensternTriggering and modulation of geyser eruptions in Yellowstone National Park by earthquakes, earth tides, and weather
We analyze intervals between eruptions (IBEs) data acquired between 2001 and 2011 at Daisy and Old Faithful geysers in Yellowstone National Park. We focus our statistical analysis on the response of these geysers to stress perturbations from within the solid earth (earthquakes and earth tides) and from weather (air pressure and temperature, precipitation, and wind). We conclude that (1) the IBEs oAuthorsShaul Hurwitz, Robert A. Sohn, Karen M. Luttrell, Michael MangaCa, Sr, O and D isotope approach to defining the chemical evolution of hydrothermal fluids: example from Long Valley, CA, USA
We present chemical and isotopic data for fluids, minerals and rocks from the Long Valley meteoric-hydrothermal system. The samples encompass the presumed hydrothermal upwelling zone in the west moat of the caldera, the Casa Diablo geothermal field, and a series of wells defining a nearly linear, ∼16 km long, west-to-east trend along the likely fluid flow path. Fluid samples were analyzed for theAuthorsShaun T. Brown, B. Mack Kennedy, Donald J. DePaolo, Shaul Hurwitz, William C. EvansConstraints on the upper crustal magma reservoir beneath Yellowstone Caldera inferred from lake-seiche induced strain observations
Seiche waves in Yellowstone Lake with a ~78-minute period and heightsAuthorsKaren Luttrell, David Mencin, Oliver Francis, Shaul HurwitzEruptions at Lone Star Geyser, Yellowstone National Park, USA, part 1: energetics and eruption dynamics
Geysers provide a natural laboratory to study multiphase eruptive processes. We present results from a four–day experiment at Lone Star Geyser in Yellowstone National Park, USA. We simultaneously measured water discharge, acoustic emissions, infraredintensity, and visible and infrared video to quantify the energetics and dynamics of eruptions, occurring approximately every three hours. We define fAuthorsLeif Karlstrom, Shaul Hurwitz, Robert Sohn, Jean Vandemeulebrouck, Fred Murphy, Maxwell L. Rudolph, Malcolm J.S. Johnston, Michael Manga, R. Blaine McCleskeyTemporal variations of geyser water chemistry in the Upper Geyser Basin, Yellowstone National Park, USA
Geysers are rare features that reflect a delicate balance between an abundant supply of water and heat and a unique geometry of fractures and porous rocks. Between April 2007 and September 2008, we sampled Old Faithful, Daisy, Grand, Oblong, and Aurum geysers in Yellowstone National Park's Upper Geyser Basin and characterized temporal variations in major element chemistry and water isotopes (δ18O,AuthorsShaul Hurwitz, Andrew G. Hunt, William C. EvansMechanics of Old Faithful Geyser, Calistoga, CA
In order to probe the subsurface dynamics associated with geyser eruptions, we measured ground deformation at Old Faithful Geyser of Calistoga, CA. We present a physical model in which recharge during the period preceding an eruption is driven by pressure differences relative to the aquifer supplying the geyser. The model predicts that pressure and ground deformation are characterized by an exponeAuthorsM.L. Rudolph, M. Manga, Shaul Hurwitz, Malcolm J. S. Johnston, L. Karlstrom, Chun-Yong WangHeat flow in vapor dominated areas of the Yellowstone Plateau volcanic field: implications for the thermal budget of the Yellowstone Caldera
Characterizing the vigor of magmatic activity in Yellowstone requires knowledge of the mechanisms and rates of heat transport between magma and the ground surface. We present results from a heat flow study in two vapor dominated, acid-sulfate thermal areas in the Yellowstone Caldera, the 0.11 km2 Obsidian Pool Thermal Area (OPTA) and the 0.25 km2 Solfatara Plateau Thermal Area (SPTA). Conductive hAuthorsShaul Hurwitz, Robert Harris, Cynthia Anne Werner, Fred MurphyTemperature data from wells in Long Valley Caldera, California
The 30-by-20-km Long Valley Caldera (LVC) in eastern California (fig.1) formed at 0.76 Ma in a cataclysmic eruption that resulted in the deposition of 600 km? of Bishop Tuff outside the caldera rim (Bailey, 1989). By approximately 0.6 Ma, uplift of the central part of the caldera floor and eruption of rhyolitic lava formed the resurgent dome. The most recent eruptive activity in the area occurredAuthorsChristopher Farrar, Jacob DeAngelo, Colin Williams, Frederick Grubb, Shaul HurwitzNote from the Hubbert Quorum
No abstract available.AuthorsSteven E. Ingebritsen, Shaul Hurwitz, E. E. BrodskyClimate-induced variations of geyser periodicity in Yellowstone National Park, USA
The geysers of Yellowstone National Park, United States, attract millions of visitors each year, and their eruption dynamics have been the subject of extensive research for more than a century. Although many of the fundamental aspects associated with the dynamics of geyser eruptions have been elucidated, the relationship between external forcing (Earth tides, barometric pressure, and precipitationAuthorsShaul Hurwitz, Ashish Kumar, Ralph Taylor, Henry HeaslerBoiling water at Hot Creek— The dangerous and dynamic thermal springs in California’s Long Valley Caldera
The beautiful blue pools and impressive boiling fountains along Hot Creek in east-central California have provided enjoyment to generations of visitors, but they have also been the cause of injury or death to some who disregarded warnings and fences. The springs and geysers in the stream bed and along its banks change location, temperature, and flow rates frequently and unpredictably. The hot spriAuthorsChristopher D. Farrar, William C. Evans, Dina Y. Venezky, Shaul Hurwitz, Lynn K. Oliver - Science
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