A message from Philipp Ruprecht (Assistant Professor, Geological Sciences, UNR):
Let me inform you that we have two more seminars this semester:
April 30—Roice Nelson, Jr. – Dynamic Measurement, LLC
Title: Lightning Analysis: Creating Geoframeworks
May 7—Daniela Pantosi (INGV, Italy) Slemmons Lecture
Title: The 2016 Earthquake Sequence in Central Italy: The Complexity of Normal Faults in Italy
Location: DMS 102 at University of Nevada, Reno (4 PM)
“In Nevada, one in four homes tested has elevated radon concentrations.”
You can test your home or business by obtaining a radon test kit from the Nevada Radon Education Program (University of Nevada Cooperative Extension):
“Select an area on the map or click on a link below to get radon test results by zip code.”
“You can also view an interactive map of “Radon in Nevada” from Nevada Bureau of Mines and Geology’s MyHazards website. Once there, click on the “Radon” symbol and then you can view geologic units representing possible radon risk combined with radon potential and average maps for Nevada.”
April 24 through April 30
The following earthquake and geologic hazard maps are free to walk-in customers (April 24 through April 30) and one penny with an online order (while supplies last). All of these maps listed below are also free as digital versions online.
A pair of earthquakes strongly shook Reno in 1914 and caused light damage to the city. The first earthquake was about magnitude 6 and occurred on February 18th at 10:17 a.m. PST. Shaking in Reno, Sparks, and Virginia City was so strong that people rushed to the streets fearing buildings were going to collapse (dePolo and Garside, 2006). The earthquake lasted for about 10 seconds and broke windows, cracked walls, and sent some parts of a brick firewall crashing to the ground in Reno (REG 2/18/1914). The shaking cracked plaster and tossed contents on floors. The earthquake also cracked windows and caused bricks to fall as far away as Virginia City (DTE 2/19/1914). A second, larger (-M 6.4) earthquake struck Reno on April 24th at 12:34 a.m. PST. This earthquake was stronger than the February event in nearly every aspect, and again people ran out of buildings in Reno. People were awakened from their sleep as far away as the Sacramento Valley in California from the shaking. In Reno, bricks fell from buildings, plaster was cracked, windows were cracked, and dishes were broken (REG 4/24/1914). Four chimneys were damaged up on University Hill (REG 4/24/1914). In Virginia City, people who were awake dashed to the streets, as pictures were jarred from walls and dishes fell from shelves (DTE 4/24/1914). (from NBMG Special Publication 37, Damaging Earthquakes in Nevada: 1840s to 2008, by Craig dePolo)
Search for your address with this interactive map:
The Staff Employees’ Council Classified Employee Recognition Committee announced that Bret Pecoraro has been selected as the 2018 Distinguished Classified Employee of the Year runner-up for his exceptional contributions to the University of Nevada, Reno and Nevada Bureau of Mines and Geology. This is a University-wide award recognizing outstanding classified staff “who exemplify the University’s standards for excellence and innovation.” It recognizes employees “with equal consideration of all eligible staff, regardless of the locus or level of responsibility within the College.” Bret was nominated by his supervisor, Dr. Bill Hammond and NBMG Acting Director, Dr. John Muntean.
Congratulations to Bret for this well-deserved and great honor!
Bret will be recognized at the “Silver and Blue Salute” on Wednesday, June 13, 2018 from 1–3 PM in the Joe Crowley Student Union Ballroom.
AEG Great Basin Chapter Student Night 2018
Thursday, April 19th, 2018
Emma McConville, Geology M.S.
Title: Geothermal Potential in Crescent Valley, Eureka County, Nevada
ABSTRACT: Crescent Valley received one of the highest favorability scores in phase I of the DOE-sponsored Nevada play fairway analysis project and was therefore selected for detailed study in phase II. As part of the detailed study, geological, geochemical and geophysical data were collected, synthesized, and analyzed to identify favorable structural settings for geothermal fluids in the basin. A total of nine favorable structural settings were identified. Two host known geothermal systems, and seven could potentially host blind geothermal systems. In phase II a predictive geothermal potential model was conducted for each favorable structural setting. The highest-ranking areas in Crescent Valley are in the Dann Hot Springs step-over (relay ramp), followed by the two northern step-overs along the Cortez Mountains front, as well as a fault intersection at Hot Springs Point.
Dustin Naphan, Geophysics M.S.
Title: Effect of Energy Directionality on ReMi Analysis
ABSTRACT: Seismic surveying methods used to determine shear wave velocities fall primarily into the category of either active or passive, in terms of their source. The purpose of such a survey is often to evaluate building site classification for earthquake shaking hazards, which requires Vs30 estimates at a minimum. For this reason, practitioners often choose passive methods, due to the locations of survey sites within noisy urban areas. There is debate over the reliability of passive methods compared to those that depend on an active source. The concern is that the overall directional origin of the source energy relative to array configuration is unknown, and may have the effect of overestimating velocity values in the raw analysis. In the case of a linear array, some proportion of an omni-directional ambient energy field will allow correct analysis. Refraction Microtremor (ReMi™) is a passive method that utilizes a linear array. To explore this issue, we conducted 3D synthetic studies as well as field recordings using an “L” shaped array configuration, consisting of two ReMi™ lines connected at a 90° angle. Such a geometry allows for analysis of effects from directionality. The synthetic modeling, which included added noise, demonstrates reliable shear-velocity estimates from cases with as little as 15% omni-directional energy. Several real-world examples collected from “L” arrays in the Reno-Sparks area demonstrate consistent results regardless of line orientation. We compiled a large volume of statistical data from the 10,000 ReMi™ surveys collected by Optim SDS for the Las Vegas Earthquake Parcel Map, at various array orientations. A regional analysis resulted in similar hazard-classification statistical distributions among Vs30 estimates, regardless of predominant array orientation.
Co-Authored by: John Louie, Satish Pullammanappallil, Travis West, Aasha Pancha
Jason Craig, Geology M.S.
Title: Discovery and Analysis of a Potential Blind Geothermal System in Southern Gabbs Valley, Western Nevada
ABSTRACT: The southern Gabbs Valley geothermal prospect is a blind thermal anomaly located 5 km north of the Gabbs Valley Range and ~15 km southeast of the Don A. Campbell geothermal power plant in west-central Nevada. The discovery of this blind thermal anomaly was initiated from the development of a detailed geothermal potential map covering 96,000 km² of the Great Basin region. This map synthesized about 9 geologic and geophysical parameters and showed high geothermal potential in southern Gabbs Valley. Subsequent geologic reconnaissance identified areas of favorable structure for hosting a blind geothermal system. Areas displaying complex fault relationships were then targeted for further exploration utilizing a shallow 2-meter thermal survey. The first 2-meter survey incorporated 60 data points in the basin, with one anomalously high-temperature point located in the southern portion of the basin. Water samples were taken from the Diamond A ranch 6 km northwest of the thermal anomaly. These samples yielded a geothermometer of 130-140°C. Additional shallow temperature survey work has been completed constraining the extent of the thermal anomaly and establishing a 7 km² area with elevated 2-meter temperatures. Subsurface data generated from a new gravity survey show that the 2-meter thermal anomaly corresponds to a significant gravity gradient that probably reflects a subsurface fault and possible fault intersection. Exploration of the system is ongoing, and further detailed mapping of bedrock and Quaternary exposures in the area will aid in understanding the structural controls of this potential geothermal system. The integration of geochemical, geophysical, and geologic datasets in this area will elucidate the probability of a commercial-grade geothermal system and produce a conceptual model to be used in the selection of drill targets.
James Ingraffia, Geology M.S. with a Graduate Minor in Business
Title: Lithium and the Lithium Clays of McDermitt Caldera, Nevada
ABSTRACT: The renewable energy revolution has taken off with the advent of lightweight, rechargeable lithium-ion batteries. The demand for lithium used in these batteries has increased exponentially over the last decade and is expected to continue as electric automotives become mainstream and nations such as Germany transition entirely to renewable energy. To supply future lithium demand, mineral exploration has turned to lithium clay deposits like that of McDermitt Caldera, Nevada. Lithium is hosted in the caldera lake sediments, specifically in smectite and illite clays. Estimates of the resource are 2*10^9 million tons of lithium. Current research efforts are aimed at answering the question of origin for the clays: are they hydrothermal or diagenetic, or a combination of the two? Answering this question will have us taking ages of the deposit stratigraphy, examining the deposit mineral assemblages for information of lake conditions, and understanding the dynamics of the McDermitt Caldera lake such that lithium clays could form. These answers will help guide exploration for more caldera-hosted lithium lake sediments.
SURE STAY PLUS HOTEL BY BEST WESTERN
1981 TERMINAL WAY
RENO, NEVADA 89502
SOCIAL HOUR: 5:30PM
RSVP NO LATER THAN 5PM, TUESDAY, APRIL 17TH TO AEG CHAIRPERSON, MERRILY GRAHAM:
Please give us a 48-hour cancellation notice if you are not able to attend.
Wood Rodgers & Resource Concepts Inc.
We are providing complementary dinners to the first three students who submit RSVP’s. Any additional students will be charged $20.
Currently seeking a sponsor for student dinners! AEG can provide an itemized receipt for student dinner sponsorship. Email an AEG officer if you or your company is interested.
Selected wine and beer will be served in the meeting room following the Social Hour, compliments of Merrily Graham. The lounge is available for early arrivals at reduced Happy Hour prices.
This is the last meeting of the season, and the Fall/Winter speaker roster will be complete by the end of summer.
Ballots will be sent to members. Gary Luce is relocating to Arizona, and the following positions need to be filled: Vice-Chairperson, Treasurer, and Secretary. I will gladly serve another year to insure an easy transition.
Thank you to all who assisted Gary and myself, those who attended the meetings, the speakers, as well as the sponsors who generously contributed. A special thank you to Vivi-Anne Brock for her assistance with the meeting announcements.
I also wish to acknowledge Dr. John Louie’s many contributions, including student sponsorships. His guidance as the UNR AEG Campus Advisor has been invaluable in planning “Student Night.”
AEG Great Basin Chairperson
Tour nine interactive museums at ‘Day at the Museum’ May 5
Community welcome to attend family-fun event at the University of Nevada, Reno
Read the details in this story by Lauren Bain, Nevada Today, 3/29/2018:
“Day at the Museum will feature nine museums on the University of Nevada, Reno campus. Walking tours will take place from 10 a.m. to 4 p.m., Saturday, May 5, at any of the participating attractions.”
Day at the Museum Locations:
University Arboretum on Hilliard Plaza
Special Collections in the Mathewson-IGT Knowledge Center
Wilbur D. May Museum
Church of Fine Arts Galleries
Nevada Historical Society
Biggest Little Pollinator Garden
Museum of Natural History
W.M. Keck Museum