Hydrogeologic Investigation of the Southern Taos Valley, Taos County, New Mexico

Total Page:16

File Type:pdf, Size:1020Kb

Hydrogeologic Investigation of the Southern Taos Valley, Taos County, New Mexico NEW MEXICO BUREAU OF GEOLOGY AND MINERAL RESOURCES Hydrogeologic Investigation of the Southern Taos Valley, Taos County, New Mexico Peggy S. Johnson Paul W. Bauer Brigitte Felix Final Technical Report August 2016 (updated November 2016) Open-File Report 581 New Mexico Bureau of Geology and Mineral Resources A division of New Mexico Institute of Mining and Technology Socorro, NM 87801 (575) 835 5490 Fax (575) 835 6333 geoinfo.nmt.edu Hydrogeologic Investigation of the Southern Taos Valley, Taos County, New Mexico Peggy S. Johnson Paul W. Bauer Brigitte Felix Final Technical Report August 2016 (updated November 2016) Open-File Report 581 New Mexico Bureau of Geology and Mineral Resources PROJECT FUNDING Taos County New Mexico Bureau of Geology and Mineral Resources, Aquifer Mapping Program Healy Foundation The views and conclusions are those of the authors, and should not be interpreted as necessarily representing the official policies, either expressed or implied, of the State of New Mexico. Cover photograph: View north down the Picuris piedmont in an area where Quaternary sand and gravel depos- its cover a complex system of buried Embudo faults and Picuris-Pecos faults. Proterozoic rocks of the Sangre de Cristo Mountains are on the right horizon, and isolated volcanoes of the Taos Plateau volcanic field in the Rio Grande rift are on the left horizon. The water well being drilled in the fall of 2015 penetrated 1200 feet of Santa Fe Group and Picuris Formation sedimentary rocks. Photograph by Paul Bauer NEW MEXICO BUREAU OF GEOLOGY AND MINERAL RESOURCES SOUTH TAOS VALLEY, TAOS COUNTY CONTENTS Proterozoic rocks ....................................................31 Executive Summary ............................................................. 1 Faults of the Southern Taos Valley ..........................31 I. Introduction ....................................................................... 3 Picuris-Pecos fault system ..................................31 Background ............................................................................. 3 Embudo fault zone .................................................32 Previous work ....................................................................... 4 Sangre de Cristo fault zone ...............................32 Purpose and scope .............................................................. 5 Los Cordovas fault zone .....................................33 Description of the study area ....................................... 6 Structural and Subsurface Geology ........................34 Geography ..................................................................... 6 Taos graben ................................................................34 Geomorphology and surface hydrology ...... 6 Miranda graben .......................................................34 Land status and accessibility .............................. 8 Geometry of buried faults ..................................35 Conceptual structural model of the .............................................................................. 9 II. Methods study area ...............................................................35 Geologic mapping and cross sections ...................... 9 3D patterns of basin-fill units ..........................35 Aerial photogrammetry and Southern extent of basalt ...................................38 field mapping .......................................................10 The Picuris embayment .......................................38 Boreholes .....................................................................10 Hydrogeologic cross sections .....................................39 Geophysics ..................................................................10 Summary of geologic investigations .......................42 Development of cross sections ........................10 Depiction of faults in the cross sections ....12 IV. Hydrogeologic Systems of the Water-level measurements, water-table map, ............................................... and groundwater hydrographs ............................12 Southern Taos Valley 45 ............................................... Measurement and inventory methods ........12 Hydrostratigraphic units 45 Water-table map ............................................... 12 Santa Fe Group basin fill ....................................45 ............ Groundwater-level fluctuations ......................18 Pennsylvanian–Proterozoic bedrock 47 Geochemical Methods ....................................................18 Basin-bedrock hydrologic boundary and hydrogeologic windows .......................48 Data collection and analysis .............................19 Picuris piedmont aquifer ...............................................49 Data compilation and data quality ...............20 Perched groundwater ............................................49 III. Geology of the Southern Taos Valley ....21 Deep confined basin-fill aquifer ......................54 Regional Geology ..............................................................21 Miranda Canyon bedrock aquifers .........................54 Rio Grande rift .........................................................21 Groundwater fluctuations ............................................54 Taos Plateau volcanic field .................................21 Seasonal water-level fluctuations ...................56 Rio Grande gorge ...................................................23 Annual and short-term water-level Picuris Mountains and fluctuations ............................................................57 Sangre de Cristo Mountains .......................23 Water-level changes and hydrographs .........58 Geologic Units .....................................................................23 Drought versus depletion ...................................63 Surficial deposits ......................................................23 Summary of hydrogeologic systems .......................63 Servilleta Basalt ........................................................25 Santa Fe Group basin fill ....................................25 V. Thermal, and Chemical Characteristics Picuris Formation ...................................................28 of Groundwater ............................................................67 Older Tertiary volcanic rocks ..........................30 Thermal conditions ..........................................................67 Paleozoic rocks .........................................................30 Chemical characteristics ................................................73 NEW MEXICO BUREAU OF GEOLOGY AND MINERAL RESOURCES SOUTH TAOS VALLEY, TAOS COUNTY Major ions and water type ................................73 Figures Minor ions, trace elements 1. Location map, land status, and regional setting . 4 and mineral saturation ............................... 81 2. Neighborhood associations ........................................... 6 Groundwater residence time .......................................82 3. Physiographic features of the Taos area Mineral solution, precipitation with acequias and sites of interest ............................. 7 and disequilibrium ............................................85 4. Watersheds of the Taos Valley with surface Summary of water chemistry and water sites and precipitation stations ...................... 8 age investigations .........................................................88 5. Map of wells, springs and surface-water sites ...13 6. Regional geologic map ...................................................22 ..................................... VI. Summary and Conclusions 91 7. Generalized geologic map ............................................24 ................................................................... Geologic model 91 8. Stratigraphy of the southern Taos Valley ............25 ............................................... Picuris piedmont aquifer 91 9. Photos of Servilleta Basalt ............................................27 ..................................................... Deep confined aquifer 92 10. Photos of the Lama formation ..................................27 Bedrock aquifers ................................................................92 11. Photograph of lake-clay deposit in Miranda Canyon hydrogeology ...............................92 basin-fill sediments ...........................................................28 Aquifer interconnection and compartments ......93 12. Photograph of the Chama-El Rito member Groundwater trends ........................................................93 of the Tesuque Formation ............................................29 Groundwater chemistry and age ..............................93 13. Photograph of Ojo Caliente Sandstone ................29 14. Photograph of the Chamita Formation ................29 15. Photograph of the Picuris Formation ....................30 VII. Recommendations .........................................................95 16. Photos of the Embudo fault zone ............................33 17. Photos of the Los Cordovas fault zone ................34 Project Staff & Acknowledgments ........................97 18. Structural model of three regional fault systems ................................................................ 36–37 References ..........................................................................98 19. Hydrogeologic cross sections .............................. 39–41 20. Map of groundwater domains in the Picuris piedmont aquifer ...............................................46
Recommended publications
  • Fire History in the Taos Valley Watersheds, New Mexico, USA
    fire Article Surface Fire to Crown Fire: Fire History in the Taos Valley Watersheds, New Mexico, USA Lane B. Johnson 1 and Ellis Q. Margolis 2,* 1 University of Minnesota, Cloquet Forestry Center, 175 University Drive, Cloquet, MN 55720, USA; [email protected] 2 U. S. Geological Survey, Fort Collins Science Center, New Mexico Landscapes Field Station, 301 Dinosaur Trail, Santa Fe, NM 87508, USA * Correspondence: [email protected]; Tel.: +1-505-954-2251 Received: 9 February 2019; Accepted: 8 March 2019; Published: 14 March 2019 Abstract: Tree-ring fire scars, tree ages, historical photographs, and historical surveys indicate that, for centuries, fire played different ecological roles across gradients of elevation, forest, and fire regimes in the Taos Valley Watersheds. Historical fire regimes collapsed across the three watersheds by 1899, leaving all sites without fire for at least 119 years. Historical photographs and quaking aspen (Populus tremuloides Michx.) ages indicate that a high-severity fire historically burned at multiple high-elevation subalpine plots in today’s Village of Taos Ski Valley, with large high-severity patches (>640 ha). Low-severity, frequent (9–29-year median interval) surface fires burned on the south aspects in nearby lower elevation dry conifer forests in all watersheds. Fires were associated with drought during the fire year. Widespread fires commonly burned synchronously in multiple watersheds during more severe drought years, preceded by wet years, including fire in all three watersheds in 1664, 1715, and 1842. In contrast, recent local “large” wildfires have only burned within single watersheds and may not be considered large in a historical context.
    [Show full text]
  • Stratigraphic Nomenclature of Proterozoic Rocks, Northern New
    Stratigraphicnomenclature ol proterozoic rocks, northern NewMexico-revisions, redefinitions, andformalization byPaul W' Bauer, New MexicoBureau ol Minesancl Mineral Resources, Socono, NM 87801 , and Michaet L. Wiltiams,Department of Geology and Geography, Universityof Massachusetts, Amherst, MA 01003 Abstract lithotectonic nomenclature for the supra- Much of the exposed Proterozoic rock in crustal Precambrianrocks exposed in north- This paper proposes formal northern New Mexico can be assignedto one revisions of ern New Mexico. the lithostratigraphicnomenclature for some of four major lithologic assemblages:1) se- Early Proterozoic rocks in northern New quencesdominated by metamorphosedmafic volcanicrocks, ca 1,755-I,720 Ma in age;2) sequencesdominated by metamorphosed felsic volcanic rocks and immature clastic sedimentaryrocks, ca 1,700Ma and ca 1,500- tains, the Truchas Peaksarea, the Rio Mora- 1,650Ma in age;3)massive clean quartzite(s) and sequencesof interlayered pelitic schist and quartzite, 1,700-1,650Ma; and 4) intru- sive rocks that range widely in age and com- position (Robertsonet al., in press).Each of these is discussed separately.Table L sum- marizes both existing and proposed new no- Kiowa Mountain in the Tusas Mountains. menclature for stratified units. Several distinctive units are designated as of northern and central New Mexico, and formations: Big Rock Formation, Burned perhaps in parts of Arizona and southern Mafic metavolcanic sequences Mountain Formation, Marquenas Forma- Colorado (Burns and Wobus, 1.983;Wobus, tion, Clenwoody Formation. Extensive terrains dominated by amphi- The metase- 1985;Bauer and Williams, 1985;Grambling dimentary sequencepreviously bolite and mafic schist of igneous parenfage called the and Williams, 1985;Williams, Ortega Group is,renamedthe Hondo 1987).
    [Show full text]
  • Do Proterozoic Metamorphic Rocks in Northern New Mexico Record One
    Bucknell University Bucknell Digital Commons Honors Theses Student Theses 2016 Do Proterozoic Metamorphic Rocks in Northern New Mexico Record One Metamorphic Event At 1.4 Ga, or Two Overprinting Events At 1.65 GA and 1.4 GA Sara Vivienne Stotter Bucknell University, [email protected] Follow this and additional works at: https://digitalcommons.bucknell.edu/honors_theses Recommended Citation Stotter, Sara Vivienne, "Do Proterozoic Metamorphic Rocks in Northern New Mexico Record One Metamorphic Event At 1.4 Ga, or Two Overprinting Events At 1.65 GA and 1.4 GA" (2016). Honors Theses. 355. https://digitalcommons.bucknell.edu/honors_theses/355 This Honors Thesis is brought to you for free and open access by the Student Theses at Bucknell Digital Commons. It has been accepted for inclusion in Honors Theses by an authorized administrator of Bucknell Digital Commons. For more information, please contact [email protected]. iv ACKNOWLEDGEMENTS I would first like to thank my thesis advisor, Dr. Chris Daniel, for his unwavering guidance, encouragement, patience, and support throughout the course of my research project. Sophomore year, when I first started doing work with Dr. Daniel, I never imagined that I would accomplish and learn so much, and I am truly grateful for his insight and mentoring. He always pushed me to do my best, and continually challenged me to think critically which allowed me to reach my goals and excel beyond them. I would also like to thank Dr. Mary Beth Gray for her kind words and endless motivation that kept me going even in the most stressful of times.
    [Show full text]
  • Museum of New Mexico a Plan for Data Recovery at Two Archaeologmal Sites Taos County, New Mexico Along Nm 522 Near Jan Cristobal
    MUSEUM OF NEW MEXICO A PLAN FOR DATA RECOVERY AT TWO ARCHAEOLOGMAL SITES ALONG NM 522 NEAR JAN CRISTOBAL, TAOS COUNTY, NEW MEXICO JEFFREY I,BOYER OFFICE OF ARCHAEOLOGICAL STUDIES ARCHAEOLOGY NOTES 230 MUSEUM OF NEW MEXICO ". .. OFFICE OF ARCHAEOLOGICAL STUDIES A PLAN FOR DATA RECOVERY AT TWO ARCHAEOLOGICAL SITES ALONG NM 522 NEAR SAN CRISTOBAL, TAOS COUNTY, NEW MEXICO Jeffrey L. Boyer with contributionsby James L. Moore Submitted by Timothy D. Maxwell Principal Investigator ARCHAEOLOGY NOTES 230 SANTA FE 1997 NEW MEXICO ADMINISTRATIVE SUMMARY During an archaeological survey conducted by the New Mexico State Highway and Transportation Department (NMSHTD) along NM 522 in Taos County, New Mexico, sixteen archaeological sites and sixtecn isolated occurrences were recorded.Of the sixteen sites, fifteen are scatters of chipped stone artifacts, including threc basalt quarry sites. The sixteenth site is a historic Hispanic acequia. The NMSHTD proposes to reconstruct this portion of NM 522, including building shoulders and extending culverts. Portions of two sites (LA 115550 [AR-03-02-07-5281 and LA 115544 [AR-03-02-07-523]) extend into proposed project limits and carmot be avoided during construction activities. LA 115550 (AR-03-02-07-528) is a basalt chipped stone artifact scatter, while LA 1 15544 (AK-03-02- 07-523) is a basalt quarry site. TheNMSHTD has requested that the Muscum of New Mexico's Oftice of Archacological Studies prepare a plan for data recovery investigations at these two sites, which are on the Questa Ranger District of the Carson National Forest. The primary focus of data recovery investigations at LA 115550 (AR-03-02-07-528) is to establish "base-line data'' for the site.
    [Show full text]
  • Proterozoic Assembly of North America: Insight from the Interactions of Deformation, Metamorphism and Magmatism in the Southwestern United States
    PROTEROZOIC ASSEMBLY OF NORTH AMERICA: INSIGHT FROM THE INTERACTIONS OF DEFORMATION, METAMORPHISM AND MAGMATISM IN THE SOUTHWESTERN UNITED STATES A Dissertation Presented to the Faculty of the Graduate School of Cornell University In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy by Robert Alexander Hunter August 2013 © 2013 Robert Alexander Hunter PROTEROZOIC ASSEMBLY OF NORTH AMERICA: INSIGHT FROM THE INTERACTIONS OF DEFORMATION, METAMORPHISM AND MAGMATISM IN THE SOUTHWESTERN UNITED STATES Robert Alexander Hunter, Ph. D. Cornell University One of the major goals of the geoscience community is to develop an accurate tectonic history of North America. Understanding how our continent evolved through time has numerous implications for our ability to develop accurate models of the tectonic evolution of continents – how they form, deform, and break. The interactions of deformation, metamorphism, and plutonism, three fundamental geological processes at work throughout the evolution of continents, record information that can be used to better understand the mechanisms and events that have shaped our continent. This dissertation employs metamorphic petrology, structural geology, geochemistry and geothermobarometry to interrogate the interactions of deformation, metamorphism and plutonism on multiple scales across the southwest United States. On a microscope scale, this dissertation shows that deformation and metamorphism can work in a positive feedback loop, facilitated by solution mass transfer, to localize both
    [Show full text]
  • The History and Preservation of the Acequia Madre Del Río Pueblo
    The history and preservation of the Acequia del Madre del Río Pueblo, Taos, New Mexico A publication of The Paseo Project in support of the Friends of the Acequia Madre P | 1 The Paseo Project is excited to present Acequia Aquí: The history and preservation of the Acequia Madre del Río Pueblo. The essay and series of maps illuminate the deteriorating acequia network at the heart of the town of Taos. Through community collaborations, The Paseo Project seeks to educate, illuminate and support this historic and culturally important public infrastructure. Through this exploration, the Paseo Project seeks to transform our community by celebrating the downtown acequia network through creative and artistic events and installations. With the help of this booklet, we hope that you will better understand the history and value the acequia system has provided to our community and imagine with us new ways that we can celebrate the gift of their presence. – The Paseo Project Team table of contents: This project was made possible by the LOR Foundation essay: The Acequia Madre del Río Pueblo in the support of the Acquia Madre del Pueblo. by Sylvia Rodríguez. .1-6 faces of the acequia: Eloy Jeantete . 2 map of the Acequia Madre del Río Pueblo. 3 We’d like to give special thanks to the following people: Charles Chacon J.R. Logan Charles Chacon faces of the acequia: George Trujillo . .4 Jim Schlarbaum Gina Azzari Barbara Scott Sylvia Rodriguez Eloy Jeantete LOR Foundation map A | Acequia Madre del Juanita Lavadie George Trujillo Friends of the Acequia Madre Río Pueblo Headgate .
    [Show full text]
  • An Environmental History of the Middle Rio Grande Basin
    CHAPTER 3 HUMAN SETTLEMENT PATTERNS, POPULATIONS, AND RESOURCE USE This chapter presents an overview, in three main sec- reasoning, judgment, and his ideas of enjoyment, tions, of the ways in which each of the three major eco- as well as his education and government (Hughes cultures of the area has adapted to the various ecosys- 1983: 9). tems of the Middle Rio Grande Basin. These groups consist of the American Indians, Hispanos, and Anglo-Americans. This philosophy permeated all aspects of traditional Within the American Indian grouping, four specific Pueblo life; ecology was not a separate attitude toward groups—the Pueblo, Navajo, Apache, and Ute—are dis- life but was interrelated with everything else in life. cussed in the context of their interactions with the environ- Another perspective on Native Americans was given by ment (Fig. 15). The Hispanic population is discussed as a Vecsey and Venables (1980: 23): single group, although the population was actually com- posed of several groups, notably the Hispanos from Spain To say that Indians existed in harmony with na- or Mexico, the genizaros (Hispanicized Indians from Plains ture is a half-truth. Indians were both a part of and other regional groups), mestizos (Hispano-Indio nature and apart from nature in their own “mix”), and mulatos (Hispano-Black “mix”). Their views world view. They utilized the environment ex- and uses of the land and water were all very similar. Anglo- tensively, realized the differences between hu- Americans could also be broken into groups, such as Mor- man and nonhuman persons, and felt guilt for mon, but no such distinction is made here.
    [Show full text]
  • Rio Grande Del Norte National‘ Monument
    Rio Grande del Norte National‘ Monument New Mexico – Taos Field Office Science Plan 2019 U.S. Department of the Interior Bureau of Land Management TABLE OF CONTENTS SECTION 1: INTRODUCTION AND SCIENTIFIC MISSION 3 1.1 Purpose of National Conservation Lands Science Plans 3 1.2. Unit and geographic area description 4 1.3. Scientific Mission 7 SECTION 2: SCIENTIFIC BACKGROUND OF THE NATIONAL CONSERVATION LANDS UNIT 8 2.1. Monument Objects and Scientific Understanding 8 Cultural Resources 8 Río Grande Gorge Cultural Resources Project 10 Nomadic Indian Presence in the Upper Rio Grande 10 Ecological Diversity 11 Soil Maps and Ecological Site Descriptions 11 Range Program and NRCS 11 Assessment, Inventory and Monitoring (AIM) Terrestrial Program 11 Riparian and Aquatic Habitat Assessment and Monitoring 12 ● AIM National Aquatic Monitoring Framework 12 ● Proper Functioning Condition (PFC) 12 Vegetation Treatment Monitoring as a part of the AIM Program (report last updated 2018; additional updates forthcoming). 12 Rare Plant Monitoring 13 Weeds Mapping 13 Tree-ring fire history of the Rio Grande del Norte Monument 13 Geology 14 Geologic Quadrangle Mapping of Southern Taos County 14 Geologic Investigations of the Southern San Luis Basin 14 Geophysical Investigations of the San Luis Basin 15 Wildlife and Fisheries Resources 15 Bee Surveys 15 Anasazi' Yuma Skipper (Ochlodes yuma anasazi) and Monarch Butterfly (Danaus plexippus) Studies at Wild Rivers 17 Big Game Migration/Movement Corridors/Winter Range 17 Surveys for Nesting Pinyon Jays at Rio Grande del Norte National Monument 18 Rio Grande del Norte National Monument Science Plan 1 Bird Surveys at Rio Grande del Norte National Monument 19 Mule Deer Studies 19 Orilla Verde Riparian Recovery Study 20 Aquatic macroinvertebrate assemblages of the RGDN National Monument: Environmental and Anthropogenic Effects 21 Fisheries and Aquatic Resources 21 3.1.
    [Show full text]
  • NPDES Authorization to Discharge to Waters of the United States, Permit No
    NPDES authorization to discharge to waters of the United States, Permit No. NM0024066 The applicant's mailing address is: Town of Taos Wastewater Treatment Facility P.O. Box 250 Ranchos de Taos, NM 87557 The wastewater treatment plant is located at 1030 Dea Ln in Taos, Taos County, New Mexico. Under the SIC Code 4952, the applicant operates a publicly owned treatment works (POTW) with a design capacity of 2.0 MGD serving a total population of 6602 that includes Town of Taos, Taos Pueblo, El Valle de Los Ranchos and El Prado. The facility discharges into an unnamed arroyo thence to the Rio Pueblo de Taos in Waterbody Segment No. 20.6.4.122 of the Rio Grande Basin. Designated uses of the receiving water are stated in the Fact Sheet. This is a renewal of a permit previously issued on issued July 17, 2012, with an effective date of September 1, 2012, and an expiration date of August 31, 2017. Changes from the previous permit are: Sufficiently Sensitive Methods requirements have been added; Limits for BOD5 have been changed to 17/21 mg/L from 30/45 mg/L along with the mass loadings; and, Mercury monitoring requirements have been revised. A fact sheet is available. State Certification This Notice also serves as Public Notice of the intent of the New Mexico Environment Department, Surface Water Quality Bureau to consider issuing Clean Water Act (CWA) Section 401 Certification. The purpose of such certification is to reasonably ensure that the permitted activities will be conducted in a manner that will comply with applicable New Mexico water quality standards, including the anti-degradation policy, and the statewide water quality management plan.
    [Show full text]
  • Taos in Summer
    National Geographic Traveler VOLUME I, NUMBER 2 DEPARTMENTS, _ FEATURE ARTICLES, _ 1 Correspondents 6 A Town to Restorethe Spirit- Letters from our readers Taos in Summer 18 SummerHighlighls 9 by Tony Hillerman, photographs by Steve Northup 1 Events of interest in your region and elsewhere around the Like generations of painters, writers, and free spirits, you United States, Canada, and Mexico can glory in Taos's spectacular surroundings, casual life- 11 Northeast 9, Southeast 174, North Central 186, Mountains and Plains 198, style, and invigorating mix of cultures. Travel- Wise 27 Southwest 206, Far West 210, Canada 216, Mexico 220 Cometo the Fair-Des Moines, Iowa 32 TravelingEasy 161 l by Michael Gartner, photographs by Scott Rutherford tt Pat Robbins, MANAGING EDITOR, NATIONAL GEOGRAPHIC WORLD Traveling With Children A wry guide to the Iowa State Fair. Sample the foods, meet old-timers and first-time prizewinners, judge a pie- Bulletin 162 baking contest, and see a really big pig. Travel- Wise 43 Homestays in foreign countries and the United States, vaca- tioning on federal lands, books on cassettes Homageto Buffalo Bill 46 by Dee Brown, photographs by Melinda Berge Museums devoted to the Plains Indians, Western art, and firearms complement the Buffalo Bill Historical Center's Illustration Credits original collection of memorabilia. Travel- Wise 51 Cover: David Cole Coates. Above, clockwise from upper left: Taos-David R Bridge, NATIONAL GEOGRAPHIC TRAVElER; San Juan lslands--© Pat O'Hara; Iowa State FaIr-Scott Rutherford; Amish country-Todd Buchanan; Monti- Gaspe-Quebec'S Wild Peninsula 52 cello-Robert Llewellyn; De'lali~Art Wolfe/Aperture Photobank; Jambo- by Kenneth Brower, photographs by Sandy Felsenthal ree~Joe Viesti.
    [Show full text]
  • Revised Regional Correlations and Tectonic Implications Of
    Revised regional correlations and tectonic implications of Paleoproterozoic and Mesoproterozoic metasedimentary rocks in northern New Mexico, USA: New fi ndings from detrital zircon studies of the Hondo Group, Vadito Group, and Marqueñas Formation James V. Jones III1,*, Christopher G. Daniel2, Dirk Frei3, and Kristine Thrane3 1Department of Earth Sciences, University of Arkansas at Little Rock, Little Rock, Arkansas 72204, USA 2Department of Geology, Bucknell University, Lewisburg, Pennsylvania 17837, USA 3Geological Survey of Denmark and Greenland (GEUS), Øster Voldgade 10, DK-1350, Copenhagen K, Denmark ABSTRACT sources to the south and Mesoproterozoic zir- Jones et al., 2009). In the southwestern United con with age probability peaks at 1479 and States (Fig. 1), quartzite and related rhyolite suc- Detrital zircon ages from quartzite and 1457 Ma. Weighted averages of 1477 ± 13 Ma cessions are key marker units for distinguish- metaconglomerate in the Tusas and Picuris and 1453 ± 10 Ma for the youngest detrital ing the age and tectonic setting of events that Mountains in northern New Mexico reveal zircon in the middle and upper Marqueñas resulted in growth of southern Laurentia during new information about age and provenance Formation provide new maximum deposi- the Paleoproterozoic (Karlstrom and Bowring, trends within a >1000 km2 Proterozoic sedi- tional age constraints, indicating that it is 1988; Hoffman, 1988; Williams, 1991; Jessup mentary basin and provide a critical test not part of the Vadito Group. The minimum et al., 2006; Whitmeyer and Karlstrom, 2007; of regional correlations. Samples from the age is not well constrained but is interpreted Amato et al., 2008; Jones et al., 2009).
    [Show full text]
  • The Case of the Taos Valley Acequias
    Common Pool Resources and Disturbances in Social Capital: The Case of the Taos Valley Acequias November, 2012 Steven M. Smith, University of Colorado, Boulder ([email protected]) Abstract: Social capital is an important element in the successful management of a common pool resource. User groups which share high levels of trust with one another reduce the costs of monitoring and enforcing rules. While theory and games highlight the importance of repeated interactions, empirical work is limited to cross-sectional analysis in which socioeconomic attributes proxy for social capital. I focus on the role of repeated interaction and estimate the impact of introducing new users (not additional) to well-established common property institutions in Taos County, New Mexico. I build a panel data set of 25 communal irrigation systems, known as acequias, from 1984 to 2008. Using satellite imagery to assess the output of each acequia in each year, fixed effects regressions are ran to measure the impact of new users being present. Other user group characteristics are included, specifically, the number of users, the economic heterogeneity of the users, as well as the cultural homogeneity of the group. The panel data and fixed effects analysis allows me to focus on the impact of the disturbance within a system. The structure of the data also permits me to correct for the omitted variable bias which likely plagues cross-sectional analysis. Fixed effects control all variables which vary across systems but not within a system, in addition to those which vary uniformly over time. I find that the introduction of new users, lowering the social capital, does negatively impact the system, though smaller shocks have less impact and the systems are resilient overtime, returning to normal levels of output after 4 years.
    [Show full text]