NEW MEXICO GEOLOGICAL SOCIETY · SPRING MEETING
Spring Meeting Abstracts
Explore research presented at the NMGS Annual Spring Meeting. Browse abstracts from 1983 onward, choose a meeting year, or open an abstract to read the full text.
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2022
Measuring Microplastics in the Middle Rio Grande Through Albuquerque, New Mexico
Raven Longwolf Alcott1, Alexandra Hurst, Sofia Jenkins-Nieto, Sarah Ann Polsin and Gary Weissmann 1 ravenlal@unm.edu The vast production of plastics has resulted in an increase of microplastics (MPs) in the environment. MPs are found in
New Mexico Underground: Spectacular Subsurface Systems for Interdisciplinary Science and Exploration
Penelope J. Boston NASA Ames Research Center, Moffett Field, CA, 94035, penelope.j.boston@nasa.gov In New Mexico, we enjoy many magnificent landscapes and varieties of geology and wildlife. But beneath our feet, there is a wondrous hidden
Gypsum Sediments in Lehman Caves, Great Basin National Park, NV, USA.
Zoe E. Havlena1, Daniel S. Jones1, Louise D. Hose2, Harvey R. DuChene3, Amanda L. Labrado4 and Benjamin Brunner4 1New Mexico Institute of Mining and Technology, 801 Leroy Pl., Socorro, NM, 87801, zoe.havlena@student.nmt.edu 2Department of Geological
Geochemistry of the Tajo granite, Socorro County, New Mexico
Haley Dietz1 and Virginia T. McLemore2 1New Mexico Institute of Mining and Technology, 911 Bursum Place, Socorro, NM, 87801, haley.dietz@student.nmt.edu 2New Mexico Bureau of Geology and Mineral Resources, 801 Leroy Place, Socorro, NM, 87801 The
Elucidating the Structural Geometry and Major Faults of the San Marcial Basin, Socorro County, Using Total Bouguer Gravity Anomaly Data.
Kyle K. Gallant1, Alex J. Rinehart1, Daniel J. Koning2 and Andrew P. Jochems2 1New Mexico Institute of Mining and Technology, 801 Leroy Pl, Socorro, NM, 87801, kyle.gallant@student.nmt.edu 2New Mexico Bureau of Geology and Mineral Resources,
The double-edged sword of ultra-high precision 40Ar/39Ar geochronology: Investigating previously unresolved complexities in sanidine age distributions
Tyler B. Cantrell1, Matthew T. Heizler1 and Jake Ross1 1New Mexico Tech, 801 Leroy Place, Socorro, NM, 87801 Improvement in the precision of 40Ar/39Ar sanidine geochronology has demonstrated that single crystal sanidine dates from ignimbrites
Hydrogeology of Snowy River Passage, Fort Stanton Cave, New Mexico
Brad Talon Newton NM Bureau of Geology, 801 Leroy Place, Socorro, NM, 87801, talon.newton@nmt.edu Fort Stanton Cave is located in the upper Rio Hondo Basin in the northern Sacramento Mountains in south central New Mexico.
Source Tracking Analysis of Aluminum, Arsenic, and Lead Entering the San Juan River in the Four Corners Region, USA.
Rachel L. Mixon1, Johanna M. Blake1, Jeb E. Brown1, Shaleene Chavarria1, Christina L. Ferguson1 and Douglass B. Yager1 1U.S. Geological Survey, 6700 Edith Blvd NE, Albuquerque, NM, 87113, rlmixon@usgs.gov The San Juan River is a
Continuous Measurement of Evaporation in High-humidity Caves: A Case Study in Fort Stanton Cave, New Mexico
Jake Collison1, Talon Newton2 and Scott Christenson2 1UNM: Civil, Construction & Environmental Engineering Department, jakec@unm.edu 2NM Bureau of Geology and Mineral Resources Monitoring evaporation rates in humid caves in arid areas may provide information about
Characterization and Origin of the REE-bearing Magmatic-hydrothermal breccia pipes in the Gallinas Mountains, Lincoln County, New Mexico
Stellah Cherotich1 and Virginia McLemore2 1New Mexico Tech, 801 Leroy Place, Socorro, NM, 87801, stellah.cherotich@student.nmt.edu 2New Mexico Bureau of Geology and Mineral Resources, 801 Leroy Pl., Socorro, NM, 87801 Breccia pipes are a common host
Geochemical niches of extremophile communities in an ephemeral acid rock drainage
Mackenzie B. Best1 and Daniel S. Jones1 1New Mexico Institute of Mining and Technology, Earth and Environmental Science, 801 Leroy Pl., Socorro, NM, 87801, mackenzie.best@student.nmt.edu Acid rock drainage (ARD) occurs when metal sulfide minerals are
Mineral Resource Potential of Land Parcels in Southwest New Mexico
Kyle T. Stafford1 and Virginia T. McLemore2 1New Mexico Institute of Mining and Technology, kyle.stafford@student.nmt.edu 2New Mexico Bureau of Geology and Mineral Resources The Organ Mountains – Desert Peaks National Monument is a recently established
Reevaluating the emplacement history of the Cornudas Mountains
Mason N. Woodard1, Nels A. Iverson2, Virginia T. McLemore2 and Laura E. Waters3 1New Mexico Institute of Mining and Technology, New Mexico Bureau of Geology and Mineral Resources, 801 Leroy Place, Socorro, NM, 87801, mason.woodard@student.nmt.edu
Quantifying groundwater to surface water exchanges in the Belen reach of the MRGCD
Ethan Williams1, Daniel Cadol1, Lin Ma2 and Alex Rinehart1 1New Mexico Tech, 810 Leroy Place, Socorro, NM, 87801, ethan.williams@student.nmt.edu 2University of Texas at El Paso, 500 West University Avenue, El Paso, TX, 79968 Periodic synoptic
The Snowy River Calcite Formation Records a Complex History in Fort Stanton Cave
Michael N. Spilde1, Keely E. Miltenberger2, Christina L. Ferguson3 and Johanna M. Blake3 1University of New Mexico, Institute of Meteoritics, MSC03 2050, Albuquerque, NM, 87131, US, mspilde@unm.edu 2University of New Mexico, Earth and Planetary Sciences
Lithogeochemical Vectors and Mineral Paragenesis of Hydrothermal REE-Bearing Fluorite Veins and Breccias in the Gallinas Mountains, New Mexico
Evan J. Owen1, Alexander P. Gysi2, Virginia T. McLemore2 and Nicole Hurtig1 1New Mexico Tech, E&ES Department, 801 Leroy Place, Socorro, NM, 87801, evan.owen@student.nmt.edu 2New Mexico Bureau of Geology and Mineral Resources, 801 Leroy Place,
Multiple Modes Of Deformation In Fault Zone Juxtaposing Dissimilar Rock Types, Southern Chupadera Mountains, Socorro County, New Mexico
Kevin M. Hobbs NMBGMR, 801 Leroy Place, Socorro, NM, 87801, kevin.hobbs@nmt.edu In the southernmost outcrop of pre-Quaternary rock in the Chupadera Mountains, Socorro County, New Mexico, a down-to-the-south normal fault is exposed in a bedrock
40Ar/39Ar Geochronology Near Rio Grande-Red River Confluence Reveal a Latir Volcanic Field Source for 4.5 to 1.2 Ma Fluvial Deposits and a <1.2 Ma Carving of the Taos Gorge
Jacob R. Gehrz1, Matthew T. Heizler1, Karl E. Karlstrom2, Matthew J. Zimmerer1 and Kevin M. Hobbs1 1New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro,
Stoneman Lake, Az, Sediments Archive Southwestern North America Surface Processes Over the Last Two Glacial Cycles (and Beyond)
Spencer E. Staley1, Peter J. Fawcett1, R. Scott Anderson2, Gonzalo Jimenez-Moreno3, Vera Markgraf2 and Erik Brown4 1University of New Mexico, Albuquerque, NM, 87131, US, sestaley@unm.edu 2Northern Arizona University 3Universidad de Granada 4University of Minnesota, Duluth
Early Pleistocene (late Blancan) vertebrates from Simon Canyon, Socorro County, central New Mexico
Gary S. Morgan1, Daniel J. Koning2, M. Steven Shackley3, David W. Love2, Kevin M. Hobbs2 and Andrew P. Jochems2 1New Mexico Museum of Natural History, 1801 Mountain Road, NW, Albuquerque, NM, 87104, gary.morgan1@state.nm.us 2New Mexico
REE in Coalbeds in the San Juan River – Raton Coal Basins
Megan N. Badonie1 and Virginia T. McLemore2 1New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM, 87801, Megan.Badonie@student.nmt.edu 2New Mexico Bureau of Geology and Mineral Resources, 801 Leroy Place, Socorro, NM, 87801
Regional Geology of the Northeastern Sacramento Mountains, Lincoln and Otero Counties, New Mexico
Geoffrey Rawling New Mexico Bureau of Geology and Mineral Resources, 1015 Tijeras Avenue NW, Suite 200, Albuquerque, NM, 87102-2909, US, geoffrey.rawling@nmt.edu Permian through Eocene sedimentary rocks, and intrusive and extrusive rocks of the Eocene-Oligocene Sierra
Controls on flow conveyance losses in the San Acacia reach of the Middle Rio Grande
Katie McLain New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM, 87801, United States, katie.mclain@student.nmt.edu The San Acacia reach of the Middle Rio Grande experiences high conveyance losses throughout the year that
Geology of the Cambrian-Ordovician Lemitar Carbonatites, Socorro County, New Mexico: Revisited
Ethan B. Haft1, Virginia T. McLemore2, O. Tapani Rämö3 and Jonas Kaare-Rasmussen4 1New Mexico Institute of Mining and Technology, 801 Leroy Pl, Socorro, NM, 87801, ethan.haft@student.nmt.edu 2New Mexico Bureau of Geology and Mineral Resources, 801