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Relevant bibliographies by topics / Volcanism – California – Long Valley Caldera

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Academic literature on the topic 'Volcanism – California – Long Valley Caldera'

Author: Grafiati

Published: 24 July 2021

Last updated: 13 February 2022

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Journal articles on the topic "Volcanism – California – Long Valley Caldera"

1

Evans, John R., and Andrew M. Pitt. "Reliable automatic detection of long-period volcanic earthquakes at Long Valley caldera, California." Bulletin of the Seismological Society of America 85, no. 5 (October 1, 1995): 1518–22. http://dx.doi.org/10.1785/bssa0850051518.

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Abstract Capturing the rare long-period (LP) volcanic earthquakes occurring in and near Long Valley caldera, California, is important to ongoing volcanic-hazards monitoring. It is difficult, however, because LP events are weak, emergent, and almost devoid of energy above a few hertz. Automatic systems designed for tectonic earthquakes routinely fail to capture LP events. We applied a PC-based teleseism-specific event-detection computer program to capturing these events. Retuning the software for LP events involved only changing parameters originally designed for change in this algorithm. Our retuned algorithm has captured every known LP event at Long Valley from October 1992 through the end of 1994. We monitored up to 16 stations known to produce good records of LP events, saving those events that triggered enough of these stations (typically 10 of 16) within a specified time window. The principal difficulty has been the algorithm's sensitivity to regional earthquakes, which have waveforms similar to LP events. During our test, the 1992 Landers, 1994 Northridge, and 1994 Double Springs Flat (Nevada) earthquakes each have swamped the detector, requiring careful, active management of PC disk resources. The efficacy of this retuned algorithm and the poor performance of tectonic-earthquake detectors during some volcanic emergencies make this algorithm an attractive candidate for volcano monitoring.

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Li, Bing Q., Jonathan D. Smith, and Zachary E. Ross. "Basal nucleation and the prevalence of ascending swarms in Long Valley caldera." Science Advances 7, no. 35 (August 2021): eabi8368. http://dx.doi.org/10.1126/sciadv.abi8368.

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Earthquake swarms are ubiquitous in volcanic systems, being manifestations of underlying nontectonic processes such as magma intrusions or volatile fluid transport. The Long Valley caldera, California, is one such setting where episodic earthquake swarms and persistent uplift suggest the presence of active magmatism. We quantify the long-term spatial and temporal characteristics of seismicity in the region using cluster analysis on a 25-year high-resolution earthquake catalog derived using leading-edge deep-learning algorithms. Our results show that earthquake swarms beneath the caldera exhibit enlarged families with statistically significant tendency for upward migration patterns. The ascending swarms tend to nucleate at the base of the seismogenic zone with a spatial footprint that is laterally constrained by the southern rim of the caldera. We suggest that these swarms are driven by the transport of volatile-rich fluids released from deep volcanic processes. The observations highlight the potential for extreme spatial segmentation of earthquake triggering processes in magmatic systems.

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Mayeda, Kevin, Stuart Koyanagi, and Keiiti Aki. "Site amplification from S-wave coda in the Long Valley caldera region, California." Bulletin of the Seismological Society of America 81, no. 6 (December 1, 1991): 2194–213. http://dx.doi.org/10.1785/bssa0810062194.

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Abstract Following the work of Phillips (1985), we have computed site amplification factors for coda waves at many sites in the Long Valley region in the eastern Sierra Nevada. We computed ratios of coda amplitudes measured at 15 stations in and around Long Valley caldera relative to a granitic site, MMPM, for six frequency bands centered at 1.5, 3.0, 6.0, 9.0, 12.0, and 15.0 Hz. All station sites located within the caldera experienced large ground motion amplification at 1.5 and 3.0 Hz, ranging between five and 17 times that of the reference site. However, at higher frequencies, these same sites exhibited significantly less amplification than the reference granite site. This is attributed to the competing effects of an impedance contrast between the basement rock and caldera fill and very high absorption in the caldera fill at high frequencies. Station MMLM, located on top of a volcanic plug, displayed the largest amplitudes of all the sites studied for frequencies between 9.0 and 15.0 Hz. A dike structure attached to the plug couples the basement rock to the surface. At high frequencies, the resulting large amplitudes at MMLM are not due to amplification resulting from a strong impedance contrast; rather, the absorption under this site is very low, perhaps lower than at the reference site, MMPM. Outside the caldera, another hard-rock site located at Devil's Postpile, MDPM, generally behaved like the reference site for all frequencies. The lowest amplifications observed came from a site outside the caldera, MDCM, located on thin pyroclastic ash deposits overlying granitic basement. This can be attributed to a dominance of absorption over the amplification caused by lower impedance of this layer. Variations among sites on similar surface geology may be due to small local variations in impedance and absorption under and adjacent to the site. The range in the spectral decay parameter, κ, between caldera and rock sites are comparable to results of Anderson and Hough (1984) for sites on alluvium and rock in the San Fernando region. These surprisingly different amplifications support the need for additional site-specific studies. Amplifications determined in this study for the frequency range 1.5 and 3.0 Hz correlate remarkably well with Eaton's (1990) residuals for duration magnitude, FMAG, and amplitude magnitude, XMAG, for the USGS northern California seismic array, further supporting the use of coda waves in determining site-specific amplification.

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Mankinen, Edward A., C. Sherman Grommé, G. Brent Dalrymple, Marvin A. Lanphere, and Roy A. Bailey. "Paleomagnetism and K-Ar ages of volcanic rocks from Long Valley Caldera, California." Journal of Geophysical Research 91, B1 (1986): 633. http://dx.doi.org/10.1029/jb091ib01p00633.

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Prudencio, Janire, and Michael Manga. "3-D seismic attenuation structure of Long Valley caldera: looking for melt bodies in the shallow crust." Geophysical Journal International 220, no. 3 (December 2, 2019): 1677–86. http://dx.doi.org/10.1093/gji/ggz543.

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SUMMARY Unrest at Long Valley caldera (California) during the past few decades has been attributed to the ascent of hydrothermal fluids or magma recharge. The difference is critical for assessing volcanic hazard. To better constrain subsurface structures in the upper crust and to help distinguish between these two competing hypotheses for the origin of unrest, we model the 3-D seismic attenuation structure because attenuation is particularly sensitive to the presence of melt. We analyse more than 47 000 vertical component waveforms recorded from January 2000 through November 2016 obtained from the Northern California Earthquake Data Center. We then inverted the S-to-coda energy ratios using the coda normalization method and obtained an average Q of 250. Low attenuation anomalies are imaged in the fluid-rich western and eastern areas of the caldera, one of which corresponds to the location of an earthquake swarm that occurred in 2014. From a comparison with other geophysical images (magnetotellurics, seismic tomography) we attribute the high attenuation anomalies to hydrothermal systems. Average to high attenuation values are also observed at Mammoth Mountain (southwest of the caldera), and may also have a hydrothermal origin. A large high attenuation anomaly within the caldera extends from the surface to the depths we can resolve at 9 km. Shallow rocks here are cold and this is where earthquakes occur. Together, these observations imply that the high attenuation region is not imaging a large magma body at shallow depths nor do we image any isolated high attenuation bodies in the upper ≈8 km that would be clear-cut evidence for partially molten bodies such as sills or other magma bodies.

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Murphy, Benjamin S., Robert R. Gaines, and Jade Star Lackey. "Co-Evolution of Volcanic and Lacustrine Systems In Pleistocene Long Valley Caldera, California, U.S.A." Journal of Sedimentary Research 86, no. 10 (October 2016): 1129–46. http://dx.doi.org/10.2110/jsr.2016.70.

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Lowenstern, Jacob B., Robert B. Smith, and David P. Hill. "Monitoring super-volcanoes: geophysical and geochemical signals at Yellowstone and other large caldera systems." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 364, no. 1845 (June 27, 2006): 2055–72. http://dx.doi.org/10.1098/rsta.2006.1813.

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Earth's largest calderas form as the ground collapses during immense volcanic eruptions, when hundreds to thousands of cubic kilometres of magma are explosively withdrawn from the Earth's crust over a period of days to weeks. Continuing long after such great eruptions, the resulting calderas often exhibit pronounced unrest, with frequent earthquakes, alternating uplift and subsidence of the ground, and considerable heat and mass flux. Because many active and extinct calderas show evidence for repetition of large eruptions, such systems demand detailed scientific study and monitoring. Two calderas in North America, Yellowstone (Wyoming) and Long Valley (California), are in areas of youthful tectonic complexity. Scientists strive to understand the signals generated when tectonic, volcanic and hydrothermal (hot ground water) processes intersect. One obstacle to accurate forecasting of large volcanic events is humanity's lack of familiarity with the signals leading up to the largest class of volcanic eruptions. Accordingly, it may be difficult to recognize the difference between smaller and larger eruptions. To prepare ourselves and society, scientists must scrutinize a spectrum of volcanic signals and assess the many factors contributing to unrest and toward diverse modes of eruption.

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Tiampo, K. F., J. B. Rundle, J. Fernandez, and J. O. Langbein. "Spherical and ellipsoidal volcanic sources at Long Valley caldera, California, using a genetic algorithm inversion technique." Journal of Volcanology and Geothermal Research 102, no. 3-4 (November 2000): 189–206. http://dx.doi.org/10.1016/s0377-0273(00)00185-2.

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Miller, C. Dan. "Holocene eruptions at the Inyo volcanic chain, California: Implications for possible eruptions in Long Valley caldera." Geology 13, no. 1 (1985): 14. http://dx.doi.org/10.1130/0091-7613(1985)13<14:heativ>2.0.co;2.

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Ji, Kang Hyeun, Thomas A. Herring, and Andrea L. Llenos. "Near real-time monitoring of volcanic surface deformation from GPS measurements at Long Valley Caldera, California." Geophysical Research Letters 40, no. 6 (March 26, 2013): 1054–58. http://dx.doi.org/10.1002/grl.50258.

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Dissertations / Theses on the topic "Volcanism – California – Long Valley Caldera"

1

Chaudet, Roy Edward. "The petrology and geochemistry of Precaldera Magmas, Long Valley Caldera, Eastern California." Thesis, Virginia Polytechnic Institute and State University, 1986. http://hdl.handle.net/10919/104307.

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Peers, Justin, Ashleigh Reeves, Christopher Gregg, Michael K. Lindell, and Andrew Joyner. "Improving volcano risk communication at the Long Valley Caldera and Mono-Inyo Craters volcanic system, eastern California, USA." Digital Commons @ East Tennessee State University, 2018. https://dc.etsu.edu/asrf/2018/schedule/4.

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Exposure to volcano hazards can lead to crises; with or without an eruptive event. Therefore, it is important to distinguish that volcanic events (unrest & eruptions) are physical phenomena while volcanic crises are social. Volcanic eruptions, unlike some other geologic hazards are often preceded by weeks or months of precursors, which offer the opportunity to reduce risk by early intervention. However, resistance to discussion of local hazards can hinder stakeholders’ (emergency managers, scientists, etc.) ability to mitigate volcano hazards and create well-informed protocols to respond when disaster strikes. The Long Valley Caldera (LVC) east of California’s Sierra Nevada Mountain Range, has experienced unrest since 1978, at which time a M5.6 earthquake ended 20 years of seismic quiet. Seismicity continued, followed by significant ground deformation and doming of the caldera floor, increased fumarolic activity, and CO2 degassing which has contributed to tree kills and human fatalities. Extensive research in volcano science provides an understanding of the physical phenomena behind the mechanics of volcanos, but limited resources have been dedicated to understanding human processes in response to volcano hazards and their corresponding disasters. Misconceptions and uncertainty surrounding organizational and physical communication of risk information can amplify economic consequences resulting from volcanic crises. This study will utilize two methods to obtain perceptions that local stakeholders and residents hold towards hazards in their region; and their confidence in the agencies that are responsible in responding to crises. A questionnaire sent to 1,200 households in February, 2018 asked head-of-households about their awareness of volcano hazards, preparedness for a volcano emergency, and perceptions of stakeholders responsible for decision making and warning systems. Mental model interviews conducted with stakeholders in summer, 2018 will provide insight on methods used by decision makers tasked with responding to disasters at LVC and the greater Long Valley Volcanic Region (LVVR). Mental models, i.e. schema, are a representation of how a person thinks about and mentally conceptualizes objects, events, and relationships in the real world. Robust to change, mental models are not easily altered; however, new information is either dismissed or made to fit within previous beliefs. Research suggests that the more discordant new information is with respect to existing beliefs, the more likely the information is to challenge those beliefs, providing opportunities for change. Together, these household and stakeholder studies will identify issues surrounding risk communication and risk management to improve tools that communicate the uncertainty of volcanic activity in the LVVR.

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Barton, David J. "Frequency-magnitude distribution and spatial fractal dimension of seismicity at The Geysers geothermal area and Long Valley Caldera, California." Thesis, Durham University, 1998. http://etheses.dur.ac.uk/5046/.

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Although there is no obvious reason why seismic 6-value and the spatial fractal dimension of earthquakes, D, should be related, there are several reports of observed empirical correlations between these two quantities. In order to investigate this phenomenon, and attempt to relate it to different types of earthquakes, industrially induced seismicity in The Geysers geothermal area, California and earthquake swarms in Long Valley caldera, California were analysed. Raw seismograms from the Unocal-NEC-Thermal network in The Geysers were processed automatically, calculating magnitudes from coda lengths and locating them using a three-dimensional velocity model. Seismicity correlated with the locations of commercial wells and surface fault locations. The entire Geysers dataset was too complex for clear correlations between b, D, seismicity and injection to be observed. In several cases, short pulses of injection induced bursts of seismicity of either small-magnitude, clustered events or large-magnitude diffuse seismicity, resulting always in a transient anomaly of negative b/D. However, sometimes pulses of injection were not accompanied by b/D transients and sometimes b/D transients were not accompanied by known injection. The latter cases may or may not indicate undisclosed injection activity. A seismic crisis in Long Valley caldera was associated with major b/D anomalies that accompanied migration of the activity from a hydrothermal zone on the south edge of the resurgent dome to the right-lateral, blind, near-vertical South Moat fault to the immediate south. The results indicated that the hydrothermal zone is an inhomogeneous structure whereas the South Moat has a mature, coherent fault plane, capable of generating magnitude M = 6 earthquakes and posing a threat to the town of Mammoth Lakes.

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Mhana, Najwa. "Geothermal Methods : application of time-dependent tomography to detect changes in structure at Long Valley caldera and the Coso geothermal area, California." Thesis, Durham University, 2016. http://etheses.dur.ac.uk/12078/.

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Structural changes in active volcanic and producing geothermal systems are expected because of changes in the distribution of fluids, gases and cracks in the host rocks. Such changes have traditionally been studied using seismic tomography where two independent inversion results are differenced. A new tomography program tomo4d, inverts two epochs simultaneously, imposing constraints to minimize the structural differences calculated between different epochs. This method suppresses spurious changes not required by the data. Both methods were applied to data from Long Valley caldera and the Coso geothermal area, and the results compared. Long Valley caldera, California, has been seismically active since 1978. In particular, a region to the south of the resurgent dome (the “south moat”) and Mammoth Mountain have experienced multiple swarms involving hundreds of thousands of earthquakes. Inverting data from 1997 and 2009/10 using tomo4d detected changes with weaker anomaly strengths compared to those of simul2000A. Some changes imaged using simul2000A are thus not required by the data. Variable changes in Vp, Vs and Vp/Vs were detected and are interpreted as pore pressure decrease and/or drying of minerals, CO2 depletion and flooding during the tectonically active period. The Coso geothermal area, California, is highly seismogenic, with thousands of earthquakes occurring each year. Time-dependent seismic tomography was performed for the years 1996, 2006, 2007, 2008, 2010 and 2012 using both simul2000A and tomo4d. The epochs 1996-2006 and 2007-2012 were studied in detail. During the first epoch, Vp, Vs and Vp/Vs mostly increased in the geothermal field whereas during the second epoch changes were more varied and less extreme. It is concluded that different parts of this tripartite field have different reservoir characteristics, and that operational activities changed with time. These likely involved increasing water saturation in some areas as a result of increased water injection in recent years.

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Boone, William J. "Microseismicity near Long Valley caldera, California, June 29 to August 12, 1982." 1985. http://catalog.hathitrust.org/api/volumes/oclc/13339421.html.

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Thesis (M.S.)--University of Wisconsin--Madison, 1985.
Typescript. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 52-55).

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Books on the topic "Volcanism – California – Long Valley Caldera"

1

Bailey, Roy A. Quaternary volcanism of Long Valley caldera and Mono-Inyo craters, eastern California: Long Valley caldera, California July 20-27, 1989. Washington, D.C: American Geophysical Union, 1989.

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Hill, David P. Development of alert criteria for future volcanic unrest in Long Valley Caldera, California. [Denver, Colo.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1990.

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3

Mankinen, Edward A. Preliminary geomagnetic paleointensities from Long Valley Caldera, California. Menlo Park, CA: U.S. Geological Survey, 1994.

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4

Howle, James F. Hydrologic data for Long Valley Caldera, Mono County, California, 1994-96. Sacramento, Calif: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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5

Roberts, Carter W. High-precision stations for monitoring gravity changes in Long Valley caldera, California. [Denver, Colo.?]: Dept. of the Interior, U.S. Geological Survey, 1988.

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Roberts, Carter W. High-precision stations for monitoring gravity changes in Long Valley caldera, California. [Denver, Colo.?]: Dept. of the Interior, U.S. Geological Survey, 1988.

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Roberts, Carter W. Principal facts for 548 gravity stations in the Long Valley caldera and vicinity, California. [Reston, Va.?]: U.S. Dept. of the Interior, Geological Survey, 1987.

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8

Sorey, M. L. Hydrologic and chemical data from the Long Valley Hydrologic Advisory Committee Monitoring Program in Long Valley Caldera, Mono County, California, 1988-1997. Menlo Park, Calif: U.S. Dept. of the Interior, U.S. Geological Survey, 1998.

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9

Bailey, Roy A. Eruptive history and chemical evolution of the precaldera and postcaldera basalt-dacite sequences, Long Valley, California: Implications for magma sources, current seismic unrest, and future volcanism. Reston, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2004.

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Bailey, Roy A. Eruptive history and chemical evolution of the precaldera and postcaldera basalt-dacite sequences, Long Valley, California: Implications for magma sources, current seismic unrest, and future volcanism. Reston, Va: U.S. Dept. of the Interior, U.S. Geological Survey, 2004.

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Book chapters on the topic "Volcanism – California – Long Valley Caldera"

1

Hofton, M. A., J. B. Minster, J. R. Ridgway, N. P. Williams, J. B. Blair, D. L. Rabine, and J. L. Bufton. "Using airborne laser altimetry to detect topographic change at Long Valley Caldera, California." In Remote Sensing of Active Volcanism, 249–64. Washington, D. C.: American Geophysical Union, 2000. http://dx.doi.org/10.1029/gm116p0249.

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Charco, M., J. Fernández, K. Tiampo, M. Battaglia, L. Kellogg, J. McClain, and J. B. Rundle. "Study of Volcanic Sources at Long Valley Caldera, California, Using Gravity Data and a Genetic Algorithm Inversion Technique." In Geodetic and Geophysical Effects Associated with Seismic and Volcanic Hazards, 1399–413. Basel: Birkhäuser Basel, 2004. http://dx.doi.org/10.1007/978-3-0348-7897-5_7.

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Mortensen, Carl E., and Douglas G. Hopkins. "Tiltmeter Measurements in Long Valley Caldera, California." In Collected Reprint Series, 13767–76. Washington, DC: American Geophysical Union, 2014. http://dx.doi.org/10.1002/9781118782064.ch8.

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Reches, Ze'ev, and Jonathan Fink. "The Mechanism of Intrusion of the Inyo Dike, Long Valley Caldera, California." In Collected Reprint Series, 4321–34. Washington, DC: American Geophysical Union, 2014. http://dx.doi.org/10.1002/9781118782064.ch15.

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Denlinger, ROGER P., and Francis Riley. "Deformation of Long Valley Caldera, Mono County, California, from 1975 to 1982." In Collected Reprint Series, 8303–14. Washington, DC: American Geophysical Union., 2014. http://dx.doi.org/10.1002/9781118782095.ch8.

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Savageand, J. C., and R. S. Cockerham. "Earthquake Swarm in Long Valley Caldera, California, January 1983: Evidence for Dike Inflation." In Collected Reprint Series, 8315–24. Washington, DC: American Geophysical Union., 2014. http://dx.doi.org/10.1002/9781118782095.ch9.

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Dixon, Timothy H., Marcus Bursik, Susan Kornreich Wolf, Michael Heflin, Frank Webb, Frederic Farina, and Stefano Robaudo. "Constraints on deformation of the resurgent dome, Long Valley Caldera, California from space geodesy." In Contributions of Space Geodesy to Geodynamics: Crustal Dynamics, 193–214. Washington, D. C.: American Geophysical Union, 1993. http://dx.doi.org/10.1029/gd023p0193.

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Hill, David P. "Temperatures at the Base of the Seismogenic Crust Beneath Long Valley Caldera, California, and the Phlegrean Fields Caldera, Italy." In IAVCEI Proceedings in Volcanology, 432–61. Berlin, Heidelberg: Springer Berlin Heidelberg, 1992. http://dx.doi.org/10.1007/978-3-642-77008-1_27.

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Younker, L. W., J. C. Eichelberger, P. W. Kasameyer, R. L. Newmark, and T. A. Vogel. "Results from Shallow Research Drilling at Inyo Domes, Long Valley Caldera, California and the Salton Sea Geothermal Field, Salton Trough, California." In Deep Drilling in Crystalline Bedrock, 172–88. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-73455-7_15.

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Hill, David P., Robert E. Wallace, and Robert S. Cockerham. "Review of Evidence on the Potential for Major Earthquakes and Volcanism in the Long Valley-Mono Craters-White Mountains Regions of Eastern California." In Practical Approaches to Earthquake Prediction and Warning, 571–94. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-017-2738-9_21.

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Conference papers on the topic "Volcanism – California – Long Valley Caldera"

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Hofton, Michelle A., J. B. Minster, J. R. Ridgway, J. B. Blair, D. L. Rabine, Jack L. Bufton, and N. P. Williams. "Using laser altimetry to detect topographic change at Long Valley caldera, California." In Aerospace Remote Sensing '97, edited by Giovanna Cecchi, Edwin T. Engman, and Eugenio Zilioli. SPIE, 1997. http://dx.doi.org/10.1117/12.298155.

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Peek, Sara, James F. Howle, William C. Evans, Deborah Bergfeld, Jennifer L. Lewicki, and Shaul Hurwitz. "GEOCHEMICAL AND HYDROLOGIC MONITORING OF THE HYDROTHERMAL SYSTEM IN LONG VALLEY CALDERA, EASTERN CALIFORNIA." In Cordilleran Section-117th Annual Meeting-2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021cd-363182.

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Andrews, Graham D. M., Abigail E. Martens, William Krugh, and Sarah R. Brown. "NEW AIRBORNE LIDAR IMAGERY OF THE INYO DOMES AND INYO CRATERS, LONG VALLEY CALDERA, CALIFORNIA." In 113th Annual GSA Cordilleran Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017cd-292710.

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Joseph, William. "CHARACTERIZING CRYSTAL ASSEMBLAGES FOR THE PETROGENESIS OF POST-COLLAPSE RHYOLITES IN THE LONG VALLEY CALDERA, CALIFORNIA." In 112th Annual GSA Cordilleran Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016cd-274615.

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Reports on the topic "Volcanism – California – Long Valley Caldera"

1

Goff, S. Field procedures manual: INYO-4, Long Valley Caldera, California. Office of Scientific and Technical Information (OSTI), January 1989. http://dx.doi.org/10.2172/6629384.

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Vogel, T. A. Drilling investigation of a young magmatic intrusion beneath Inyo Dome, Long Valley Caldera, California. Progress report. Office of Scientific and Technical Information (OSTI), January 1985. http://dx.doi.org/10.2172/5215425.

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Blackett, Robert. Regulatory, Land Ownership, and Water Availability Factors for a Magma Well: Long Valley Caldera and Coso Hot Springs, California. Office of Scientific and Technical Information (OSTI), September 1985. http://dx.doi.org/10.2172/893178.

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Zucca, J., G. Zandt, L. Steck, and W. Prothero. Recording of anomalous shear energy in the teleseismic P-wave coda at Long Valley Caldera, California, on a small aperture array. Office of Scientific and Technical Information (OSTI), March 1990. http://dx.doi.org/10.2172/7024307.

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Papike, J. J., M. S. Servilla, and K. H. Wohletz. Simulating silicic eruptions at Long Valley, California as a method to understand processes that influence eruption phenomena associated with caldera formation. IGPP progress report, October 1, 1993--August 31, 1994. Office of Scientific and Technical Information (OSTI), December 1994. http://dx.doi.org/10.2172/10118358.

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Geologic map of the Long Valley caldera, Mono-Inyo Craters volcanic chain, and vicinity, eastern California. US Geological Survey, 1989. http://dx.doi.org/10.3133/i1933.

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Hydrologic and geochemical monitoring in Long Valley caldera, Mono County, California, 1986. US Geological Survey, 1989. http://dx.doi.org/10.3133/wri894033.

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Hydrologic and geochemical monitoring in Long Valley Caldera, Mono County, California, 1985. US Geological Survey, 1987. http://dx.doi.org/10.3133/wri874090.

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Hydrologic and geochemical monitoring in Long Valley Caldera, Mono County, California, 1982-1984. US Geological Survey, 1985. http://dx.doi.org/10.3133/wri854183.

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Response plan for volcano hazards in the Long Valley Caldera and Mono Craters region, California. US Geological Survey, 2002. http://dx.doi.org/10.3133/b2185.

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