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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2015
High-resolution statewide modeling of groundwater recharge in New Mexico
David G. Ketchum1, Talon Newton2 and Fred Phillips1 1New Mexico Tech, 801 Leroy Pl., Socorro, NM, 87801, dgketchum@gmail.com 2New Mexico Bureau of Geology and Mineral Resources The rate and distribution of groundwater recharge to New
Rollalong resistivity surveys reveal karstic paleotopography developed on near-surface gypsum bedrock: Lakewood, New Mexico
Lewis Land1 and Lasha Asanidze2 1NMBGMR, 400-1 Cascades Ave., Carlsbad, NM, 88220, lland@nckri.org 2Ivane Javakhishvili Tbilisi State University Following flooding in September 2013, several areas in northern Eddy County, New Mexico were damaged by multiple
Application of HydroGeoSphere to model three-dimensional hydrological processes in the Valles Caldera watershed, New Mexico: Preliminary results
Michael Louis Wine1 and Daniel Cadol1 1New Mexico Institute of Mining and Technology, 801 Leroy Place, Socorro, NM, NM, 87801, USA, mlw63@cornell.edu Application of HydroGeoSphere to model three-dimensional hydrological processes in the Valles Caldera watershed,
Miocene and Modern climate in the California Sierra Nevada and Implications for Stable Isotope-Based Paleoaltimetry
Lauren Wheeler1, Joseph Galewsky1, Matthew Huber2 and Nicholas Herold3 1Earth and Planetary Sciences Department, University of New Mexico, laurenwheeler@unm.edu 2Department of Earth Sciences, University of New Hampshire 3Earth, Atmospheric, and Planetary Science, Purdue University The
Preliminary Description of an Ianthasaurus-like Edaphosaurid From the Lower Permian Bursum Formation, Otero County, New Mexico
Thomas Lee Suazo1, Amanda Kaye Cantrell1 and Spencer G. Lucas1 1New Mexico Museum of Natural History, 1801 Mountain Road NW, Albuquerque, NM, 87104, tom.suazo@state.nm.us An incomplete, articulated skeleton of a medium-sized edaphosaurid from the Early
N-S extension and bimodal magmatism during early Rio Grande rifting: Insights from E-W striking dikes at Faulkner Canyon, south central New Mexico
Cory Christian Paliewicz New Mexico State University, 1123 2nd Street, Apt. 2, Las Cruces, NM, 88005, palie1cc@nmsu.edu North-northeast extension and bimodal magmatism during early Rio Grande rifting is recorded by the emplacement histories of two
New Mexico’s Paleoclimate and its Affect on Plesiadapiform Biogeographic Dispersal – A study of fossil geographic range compared with estimated body mass for these stem primates
Clayton Dean Pilbro New Mexico State University, 1780 E University Ave, Las Cruces, NM, 88003, Cpilbro@gmail.com Plesiadapiformes (possible stem-primates) proliferatedaround the world during the Paleocene-Eocene with a large sample found in the San Juan Basin
Changes in Rio Grande Rift Tectonism as Inferred from Subsidence Curves
Evan Gragg1, Dan Koning2, Jolante van Wijk1, Gary Axen1, Brad Sion1, Rediet Abera1, Kyle Murray1, Jeff Dobbins1, Mark Murray1 and Richard Chamberlin2 1Department of Earth and Environmental Science, New Mexico Institute of Mining and Technology,
Sediment Analysis From Cerro Medio Drainage, Jemez Mountains, Nm: Assessing Causes of Color Changes in the Vertical Profile
Angelica K. Gallegos1 and Jennifer Lindline1 1New Mexico Highlands University, PO box 9000, Las Vegas, NM, 87701, teeni_tiny41@yahoo.com The Cerro del Medio drainage in the Jemez Mountains contains more than 10 laterally continuous alternating light-dark
Geochemistry of White Rock Canyon Springs, Northern New Mexico
Tanner K. Grulke1, Laura J. Crossey1, Karl E. Karlstrom1 and Valerie Blomgren1 1University of New Mexico, Albuquerque, NM, 87106, tgrulke@unm.edu The Rio Grande runs through White Rock Canyon in North-Central New Mexico. White Rock Canyon
Timing, geochemistry, and distribution of magmatism in the Rio Grande rift
Rediet Abera1, Brad Sion, Jolante van Wijk, Gary Axen, Dan Koning, Richard Chamberlin, Evan Gragg, Kyle Murray and Jeff Dobbins 1New Mexico Institute of Mining and Technology, 801 Leroy Place, Office #196, Socorro, NM, 87801,
The active Rio Grande rift: summarizing our current understanding of present-day deformation from geodetic and stress measurements
Kyle Dennis Murray1, Jeff Dobbins1, Mark Murray1, Jolante van Wijk1 and Gary Axen1 1New Mexico Institute of Mining and Technology, 801 Leroy, Socorro, NM, 87801, United States, kmurray@nmt.edu Geodetic and stress-field studies of the Rio
Geochemistry of Aquifer Recharge Projects in New Mexico
Christopher Wolf1, Bob Marley1 and Amy Ewing1 1Daniel B. Stephens & Associates, Inc., 6020 academy NE, Albuquerque, NM, 87109, cwolf@dbstephens.com Managed aquifer recharge is being implemented at sites across New Mexico as an important water
Defining the response of Southwestern North American climate to abrupt Northern Hemisphere climate change events during the last glacial period
Justin Grant Peinado1, Yemane Asmerom1, Victor Polyak1 and Matt Lachniet1 1University of New Mexico, Earth and Planetary Sciences, MSC03 2040, 1 University of New Mexico, Albuquerque, NM, 87131, peinadoj@unm.edu There are well-established reoccurring climate change
Birth and Evolution of the Rio Grande Fluvial System: New Insights From River Gravel Provenance Studies and 40Ar/39Ar Dated Paleoprofiles
Marisa Nicole Repasch1, Karl Karlstrom1 and Matt Heizler2 1University of New Mexico, Department of Earth and Planetary Sciences, 1 University of New Mexico, Albuquerque, NM, 87131, United States, mrepasch@unm.edu 2New Mexico Bureau of Geology and
Age of Carving of the Westernmost Grand Canyon: Conflicts and Potential Resolutions That Reconcile Geologic and Thermochronologic Data
Carmen Winn1, Karl Karlstrom1, Shari Kelley2, David Shuster3 and Matt Fox3 1Department of Earth and Planetary Sciences, University of New Mexico, MSC03 2040, Albuquerque, NM, 87131, cwinn264@unm.edu 2Earth and Environmental Sciences Department, New Mexico Tech,
The transition to wetter Late Holocene climate in Southwestern North America from speleothem data
Chrissy Allen1, Yemane Asmerom1, Victor Polyak1 and Matthew Lachniet2 1University of New Mexico, chrissyallen@unm.edu 2University of Nevada, Las Vegas Semi-arid, moisture-limited regions such as southwestern North America are particularly susceptible to drought effects due to
Exploring Soda Dam Travertine Mineralogy Through X-Ray Diffraction For A Better Insight Into Paleohydrology, Paleoclimatolgy And Geothermal History
Graham King Thomas1, Eric Peterson1, Laura J. Crossey1, Karl Karlstrom1 and April Jean2 1UNM, Department of Earth & Planetary Sciences, University of New Mexico, Albuquerque, NM, 87131, gthoma21@unm.edu 2Glorieta Geoscience, Glorieta Geoscience, 1723 2nd St,
Arthropod Biodiversity Higher Than Formerly Thought at the Late Pennsylvanian (middle Missourian: Kasimovian) Kinney Brick Quarry Lagerstatte, Central NM, USA
Amanda Kaye Cantrell1, Thomas Lee Suazo1, Spencer G. Lucas1 and Joerg Schneider2 1New Mexico Museum of Natural History, 1801 Mountain Road NW, Albuquerque, NM, 87104, amanda.cantrell@state.nm.us 2TU Bergakademie Freiberg, Bernhard-von-Cotta Str. 2, Freiberg, D-09599, Germany
depositional Setting and Sequence Stratigraphic Framework of the Lower Permian (wolfcampian) Hueco Formation (upper-Middle and Gastropod Members). Robledo Shelf, Western Orogrande Basin, New Mexico
Matthew Harder1, Katherine Giles1 and Gregory Mack2 1University of Texas at El Paso, mharder42@gmail.com 2New Mexico State University In recent years, the Lower Permian Wolfcamp Shale of Texas and New Mexico has become one of
Hydrogeologic Windows: Detection of Blind and Traditional Geothermal Play Fairways in Southwestern New Mexico
James Witcher1, Mark Person2, Shari Kelley3, Richard Kelley4, Jeffrey Bielicki5, Glenn Sutula5 and Richard Middleton4 1Witcher and Associates, Las Cruces, NM, 88001, jimwitcher@zianet.com 2Hydrology Department, New Mexico Institute of Mining and Technology, Socorro, NM, 87801
Paleomonsoonal Precipitation and Hydroclimate Variability From Glacial to Interglacial Climates in the Southwest: The Stoneman Lake, Arizona Record
Dylan J. Garcia1, Peter J. Fawcett1 and R. Scott Anderson2 1University of New Mexico, Earth and Planetary Sciences, MSC03 2040, 1 University of New Mexico, Albuquerque, NM, 87131, dylangarcia@unm.edu 2Northern Arizona University, Flagstaff, AZ Two
Quantifying the Effect of Thinning Vegetation on Evapotranspiration in a Mountainous Watershed through Remote Sensing
Peter M. ReVelle1, Jan M. H. Hendrickx1 and B. Talon Newton2 1New Mexico Tech, 801 Leroy Place, Socorro, NM, 87801, prevelle@nmt.edu 2New Mexico Bureau of Geology & Mineral Resources, New Mexico Tech, Socorro, NM, 87801
Late Holocene Alluviation in the Palomas Basin, South-Central New Mexico
Andy Jochems1, Daniel Koning1, Curtis Monger2 and Dave Love1 1New Mexico Bureau of Geology & Mineral Resources, New Mexico Institute of Mining & Technology, 801 Leroy Place, Socorro, NM, 87801, ajochems@nmbg.nmt.edu 2Plant & Environmental Sciences,