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
A simple numerical model of the Rio Grande Rift extension: implications on surface hydrology
Kyungdoe Han1 and John Wilson1 1Department of Earth and Environmental Science, New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM, 87801, kyungdoe.han@student.nmt.edu Tectonic extension of the Earth’s crust significantly alters the surface
Geoscience Outreach in the International Year of Caves and Karst
George Veni National Cave and Karst Research Institute, 400-1 Cascades Avenue, Carlsbad, NM, 88220, United States, gveni@nckri.org The International Year of Caves and Karst is a global effort to teach the world about the benefits
Geochemical fingerprinting of source water to the Snowy River deposit
Johanna M. Blake1, Christina Ferguson1 and Keely Miltenberger1 1U.S. Geological Survey, 6700 Edith Blvd. NE, Albuquerque, NM, 87113, jmtblake@usgs.gov The Snowy River deposit, located in the Fort Stanton-Snowy River Cave System near Capitan, New Mexico,
Sulfuric Acid Speleogenesis in the Frasassi Cave System, Italy, and Possible Implications for Guadalupe Mountain Caves
Daniel S. Jones Earth and Environmental Science Department, New Mexico Institute of Mining and Technology, and National Cave and Karst Research Institute, Socorro, NM, 87801, daniel.s.jones@nmt.edu Cave formation by sulfuric acid, known as “sulfuric acid
Spelunking into the Virosphere: Characterizing Viral Communties from Carlsbad Caverns National Park
Joseph Ulbrich1, Daniel S. Jones2 and Thomas L. Kieft1 1Biology Department, New Mexico Institute of Mining and Technology, joseph.ulbrich@student.nmt.edu 2Earth and Environmental Science Department, New Mexico Institute of Mining and Technology Viruses are the most
Caves in the Upper Pecos Watershed
Dennis McQuillan High Desert Science, 3 S Hijo de Dios, Santa Fe, NM, NM, 87508-9133, United States, geologist@highdesertscience.net Caves formed by dissolution along permeability structures in Paleozoic limestone in the Upper Pecos Watershed are of
Contrasting Microbial Communities in Cave Ferromanganese Deposits With Overlying Surface Soils
Diana E. Northup1, Jason C. Kimble1, Ara S. Winter1 and Robert L. Sinsabaugh1 1University of New Mexico, Department of Biology, MSC03 2020, Albuquerque, NM, 87131-0001, dnorthup@unm.edu Arid-land carbonate caves, such as Fort Stanton Cave, receive
The First Decade in Snowy River: Stalking the Mammoth Cave of the West
Donald G. Davis Fort Stanton Cave Study Project, 441 S Kearney St, Denver, CO, 80224-1237, dgdavis@nyx.net I first visited Fort Stanton Cave as a young caver in 1960, and as I wandered along its level,
Using electrical resistivity methods to map cave passages and conduits in the San Solomon Springs karstic aquifer system, West Texas, USA
Lewis Land1 and George Veni1 1National Cave & Karst Research Institute, 1015 Tijeras Ave. NW, suite 200, Albuquerque, NM, 87102, United States, lland@nckri.org Personnel with the National Cave and Karst Research Institute have conducted a
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
Photogrammetric Analysis of the Clayton Lake Dinosaur Tracksite, Early Cretaceous of Northeastern New Mexico
Michael A. Kvasnak1, John B. Rogers2 and Spencer G. Lucas3 1Central New Mexico Community College, 900 University Blvd. SE, Albuquerque, NM, 87106, mkvasnak@cnm.edu 2 900 University Blvd. SE 3New Mexico Museum of Natural History, 1801
Applying sandstone modal composition and ImageJ analysis to constrain feldspar alteration in Early Permian (Wolfcampian) nonmarine strata in New Mexico
Justin Matthew Friend1, Brian A. Hampton1 and Alicia L. Bonar2 1Department of Geological Sciences, New Mexico State University, Las Cruces, NM, 88003, United States, jmfriend@nmsu.edu 2ConocoPhillips School of Geology and Geophysics, University of Oklahoma, Norman,
Seismic Monitoring of Flash Floods—Sediment Transport, Flood Detection, and Flow Characteristics Inferred from Seismic Signals in an Ephemeral Watershed
John Mitchell McLaughlin1, Susan Bilek1 and Daniel Cadol1 1New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM, 87801, United States of America, John.mclaughlin@student.nmt.edu Ephemeral channels that characterize a large part of New
Navigating the Blm Proposal Submission Process to Gain Scientific Entries to Fort Stanton Cave
Knutt Peterson BLM Roswell Field Office, 2909W 2nd St, Roswell, NM, 88201, knuttpet@blm.gov Fort Stanton Cave is a unique environment which offers scientists and researchers the opportunity to discover, study, and explore the unknown. The
Fort Stanton Cave Formation Repair and Restoration Project
Michael C. Mansur Chair of the Southwestern Region of the National Speleologocal Society, P.O. Box 1117, Tajique, NM, 87016, mcmansur@zoho.com The goal of the Fort Stanton Cave Formation Repair and Restoration Project is to repair
Monitoring Sediment Erosion and Deposition in the Arroyo de los Pinos Through Structure from Motion (SfM) Photogrammetry
Rebecca Moskal1 and Daniel Cadol1 1New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM, 87801, rebecca.moskal@student.nmt.edu The Arroyo de los Pinos is a tributary of the Rio Grande that transports tons of
A new specimen of the eubaenine turtle Goleremys mckennai from the Paleocene Nacimiento Formation of northwestern New Mexico
Asher Jacob Lichtig1 and Spencer G. Lucas1 1New Mexico Museum of Natural History, 1801 Mountain Rd. NW, Albuquerque, NM, 87124, ajlichtig@gmail.com A skull and associated postcrania found in the Paleocene Nacimiento Formation are the first
Key speleothem paleoclimate results from Fort Stanton Cave
Victor J. Polyak1, Yemane Asmerom1 and Matthew S. Lachniet2 1Department of Earth and Planetary Geosciences, University of New Mexico, 221 Yale Blvd, Northrop Hall, Albuquerque,, NM, 87131, polyak@unm.edu 2Department of Geoscience, University of Nevada, 4505
Late Cretaceous (Cenomanian-Campanian) ammonite zones in the Chama Basin, Rio Arriba County, New Mexico
Paul L. Sealey1 and Spencer G. Lucas1 1New Mexico Museum of Natural History, 1801 Mountain Road, NW, Albuquerque, NM, 87104, ammonoidea@comcast.net Upper Cretaceous strata exposed in the Chama Basin in Rio Arriba County in northern
New Evidence Confirms the ~250 K.y. Duration for Deposition of the Paleocene Ojo Alamo Sandstone in the Southern San Juan Basin, New Mexico
James E. Fassett USGS Retired, Independent Research Geologist, 552 Los Nidos Dr, Santa Fe, 87501, jimgeology@aol.com The dinosaur-bearing Ojo Alamo Sandstone (OAS) of the San Juan Basin (SJB), NM and CO, is earliest Paleocene based