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San Luis Valley Conservation Area EA and LPP EA Chapter 3
Chapter 3 — Affected Environment This chapter describes the biological, cultural, and on the eastern side of the valley floor, the Oligocene socioeconomic resources of the SLVCA that could be volcanic rocks of the San Juan Mountains dip gently affected by the no-action alternative (alternative A) eastward into the valley floor, where they are inter- and the proposed action (alternative B). The SLVCA bedded with valley-fill deposits. Valley-fill deposits consists of 5.2 million acres within the Southern Rock- consist of sedimentary rocks that inter-finger with ies and Arizona/New Mexico Plateau ecoregions (U.S. volcanic deposits. Quaternary deposits include pedi- Environmental Protection Agency 2011). The project ments along the mountain fronts, alluvium, and sand encompasses significant portions of seven counties in dunes (USFWS 2011). southern Colorado as well as small parts of two coun- ties in northern New Mexico. Just over 50 percent of MINERALS the total project area is publicly owned; however, the Sand and gravel are the major mineral commodities distribution of public/private ownership is uneven, with mined in the vicinity of the San Luis Valley. Rock, over 90 percent of Mineral County administered by sand, and gravel mines are scattered throughout the the USFS, but less than 1 percent of Costilla County valley, but are concentrated around the cities of Ala- in State or Federal ownership. The project boundary mosa and Monte Vista and the town of Del Norte, is defined by the headwaters hydrologic unit (HUC Colorado. No coal mining permits are active in the 6) of the Rio Grande. SLVCA (Colorado Division of Reclamation, Mining, Because of the nearly 7,000 feet in elevation change and Safety 2012). -
San Luis Valley Conservation Area Land Protection Plan, Colorado And
Land Protection Plan San Luis Valley Conservation Area Colorado and New Mexico December 2015 Prepared by San Luis Valley National Wildlife Refuge Complex 8249 Emperius Road Alamosa, CO 81101 719 / 589 4021 U.S. Fish and Wildlife Service Region 6, Mountain-Prairie Region Branch of Refuge Planning 134 Union Boulevard, Suite 300 Lakewood, CO 80228 303 / 236 8145 CITATION for this document: U.S. Fish and Wildlife Service. 2015. Land protection plan for the San Luis Valley Conservation Area. Lakewood, CO: U.S. Department of the Interior, U.S. Fish and Wildlife Service. 151 p. In accordance with the National Environmental Policy Act and U.S. Fish and Wildlife Service policy, an environmental assessment and land protection plan have been prepared to analyze the effects of establishing the San Luis Valley Conservation Area in southern Colorado and northern New Mexico. The environmental assessment (appendix A) analyzes the environmental effects of establishing the San Luis Valley Conservation Area. The San Luis Valley Conservation Area land protection plan describes the priorities for acquiring up to 250,000 acres through voluntary conservation easements and up to 30,000 acres in fee title. Note: Information contained in the maps is approximate and does not represent a legal survey. Ownership information may not be complete. Contents Abbreviations . vii Chapter 1—Introduction and Project Description . 1 Purpose of the San Luis Valley Conservation Area . 2 Vision for the San Luis Valley National Wildlife Refuge Complex . 4 Purpose of the Alamosa and Monte Vista National Wildlife Refuges . 4 Purpose of the Baca national wildlife refuge . 4 Purpose of the Sangre de Cristo Conservation Area . -
Minerals of the San Luis Valley and Adjacent Areas of Colorado Charles F
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/22 Minerals of the San Luis Valley and adjacent areas of Colorado Charles F. Bauer, 1971, pp. 231-234 in: San Luis Basin (Colorado), James, H. L.; [ed.], New Mexico Geological Society 22nd Annual Fall Field Conference Guidebook, 340 p. This is one of many related papers that were included in the 1971 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
A MODEL for BIOMASS ASSESSMENT E-023 SUBMITTED BY: Dr
• A MODEL FOR BIOMASS ASSESSMENT E-023 SUBMITTED BY: Dr. Stephen J. Walsh Associate Professor Dr. George p. Malanson Assistant Professor Dr. John D. Vitek Associate Professor Dr. David R. Butler Assistant Professor Department of Geography Oklahoma State University & in conjunction with USDA/Agricultural Research Service SUBMITTED TO: Dr. Norman N. Durham, Director Water Research Center Oklahoma State University March 14, 1983 Introduction The surface of the earth is a complex system responding to the input of energy, natural and human. Human use of the surface for maximum agricultural efficiency requires knowledge of the interactions of all variables involved in the system. Broad categories of phenomena, including the atmosphere (weather and climate), biosphere (vegetation, fauna, and human activity), hydrosphere (precipitation, runoff, infiltration, fluvial erosion, and evapotranspiration), and the lithosphere (soil, topography, and parent material), can be identified as the major variables in any assessment. Assessment of interactions requires data from various sources. The emergence of remote sensing as a source of data for assessments in the last decade permits the development of more accurate predictive models. Refinements in data acquisition, such as improved resolution, the use of radar, and the correlation of detailed surface observations with satellite overpasses, provide researchers with the capability to assess inter relationships and create accurate models. A conceptual model, Figure 1, illustrates the interaction of the Department of Geography/CARS and the USDA/Agricultural Research Service with components of the natural system for the purpose of creating a predictive model for biomass assessment~~CARS, the remote sensing center at Oklahoma State University, plus ARS of the USDA bring different skills to this joint research effort. -
Summits on the Air – ARM for USA - Colorado (WØC)
Summits on the Air – ARM for USA - Colorado (WØC) Summits on the Air USA - Colorado (WØC) Association Reference Manual Document Reference S46.1 Issue number 3.2 Date of issue 15-June-2021 Participation start date 01-May-2010 Authorised Date: 15-June-2021 obo SOTA Management Team Association Manager Matt Schnizer KØMOS Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Page 1 of 11 Document S46.1 V3.2 Summits on the Air – ARM for USA - Colorado (WØC) Change Control Date Version Details 01-May-10 1.0 First formal issue of this document 01-Aug-11 2.0 Updated Version including all qualified CO Peaks, North Dakota, and South Dakota Peaks 01-Dec-11 2.1 Corrections to document for consistency between sections. 31-Mar-14 2.2 Convert WØ to WØC for Colorado only Association. Remove South Dakota and North Dakota Regions. Minor grammatical changes. Clarification of SOTA Rule 3.7.3 “Final Access”. Matt Schnizer K0MOS becomes the new W0C Association Manager. 04/30/16 2.3 Updated Disclaimer Updated 2.0 Program Derivation: Changed prominence from 500 ft to 150m (492 ft) Updated 3.0 General information: Added valid FCC license Corrected conversion factor (ft to m) and recalculated all summits 1-Apr-2017 3.0 Acquired new Summit List from ListsofJohn.com: 64 new summits (37 for P500 ft to P150 m change and 27 new) and 3 deletes due to prom corrections. -
Sangre De Cristo Salida and San Carlos Wet Mountains San Carlos Spanish Peaks San Carlos
Wild Connections Conservation Plan for the Pike & San Isabel National Forests Chapter 5 – Complexes: Area-Specific Management Recommendations This section contains our detailed, area-specific proposal utilizing the theme based approach to land management. As an organizational tool, this proposal divides the Pike-San Isabel National Forest into eleven separate Complexes, based on geo-physical characteristics of the land such as mountain ranges, parklands, or canyon systems. Each complex narrative provides details and justifications for our management recommendations for specific areas. In order to emphasize the larger landscape and connectivity of these lands with the ecoregion, commentary on relationships to adjacent non-Forest lands are also included. Evaluations of ecological value across public and private lands are used throughout this chapter. The Colorado Natural Heritage Programs rates the biodiversity of Potential Conservation Areas (PCAs) as General Biodiversity, Moderate, High, Very High, and Outranking Significance. The Nature Conservancy assesses the conservation value of its Conservation Blueprint areas as Low, Moderately Low, Moderate, Moderately High and High. The Southern Rockies Ecosystem Project's Wildlands Network Vision recommends land use designations of Core Wilderness, Core Agency, Low and Moderate Compatible Use, and Wildlife Linkages. Detailed explanations are available from the respective organizations. Complexes – Summary List by Watershed Table 5.1: Summary of WCCP Complexes Watershed Complex Ranger District -
Preliminary Evaluation of Potential Acecs---Royal
Preliminary Evaluation of Potential ACECs—Royal Gorge Field Office Relevance and Importance Criteria Prepared by U.S. Department of the Interior Bureau of Land Management Royal Gorge Field Office Cañon City, CO February 2017 This page intentionally left blank Preliminary Evaluation of Potential iii ACECs—Royal Gorge Field Office Table of Contents Acronyms and Abbreviations ....................................................................................................... ix Executive Summary ...................................................................................................................... xi _1. Introduction .............................................................................................................................. 1 _1.1. Eastern Colorado Resource Management Plan ............................................................... 1 _1.2. Authorities ....................................................................................................................... 1 _1.3. Area of Consideration ..................................................................................................... 1 _1.4. The ACEC Designation Process ..................................................................................... 1 _2. Requirements for ACEC Designation .................................................................................... 3 _2.1. Identifying ACECs .......................................................................................................... 5 _2.2. Special Management -
Frozen Ground
Frozen Ground Th e News Bulletin of the International Permafrost Association Number 32, December 2008 INTERNATIONAL PERMAFROST ASSOCIATION Th e International Permafrost Association, founded in 1983, has as its objectives to foster the dissemination of knowledge concerning permafrost and to promote cooperation among persons and national or international organisations engaged in scientifi c investigation and engineering work on permafrost. Membership is through national Adhering Bodies and Associate Members. Th e IPA is governed by its offi cers and a Council consisting of representatives from 26 Adhering Bodies having interests in some aspect of theoretical, basic and applied frozen ground research, including permafrost, seasonal frost, artifi cial freezing and periglacial phenomena. Committees, Working Groups, and Task Forces organise and coordinate research activities and special projects. Th e IPA became an Affi liated Organisation of the International Union of Geological Sciences (IUGS) in July 1989. Beginning in 1995 the IPA and the International Geographical Union (IGU) developed an Agreement of Cooperation, thus making IPA an affi liate of the IGU. Th e Association’s primary responsibilities are convening International Permafrost Conferences, undertaking special projects such as preparing databases, maps, bibliographies, and glossaries, and coordinating international fi eld programmes and networks. Conferences were held in West Lafayette, Indiana, U.S.A., 1963; in Yakutsk, Siberia, 1973; in Edmonton, Canada, 1978; in Fairbanks, Alaska, 1983; in Trondheim, Norway, 1988; in Beijing, China, 1993; in Yellowknife, Canada, 1998, in Zurich, Switzerland, 2003, and in Fairbanks, Alaska, in 2008. Th e Tenth conference will be in Tyumen, Russia, in 2012.Field excursions are an integral part of each Conference, and are organised by the host Executive Committee 2008-2012 Council Members Professor Hans-W. -
Late Mesozoic to Cenozoic Cooling Histories of the Flanks of the Northern and Central Rio Grande Rift, Colorado and New Mexico
New Mexico Bureau of Mines & Mineral Resources A DIVISION OF NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY Late Mesozoic to Cenozoic cooling histories of the flanks of the northern and central Rio Grande rift, Colorado and New Mexico Shari A. Kelley1, Charles E. Chapin2, and Jeff Corrigan3 1Department of Geological Sciences, Southern Methodist University, Dallas, Texas 75275; 2New Mexico Bureau of Mines & Mineral Resources, Socorro, New Mexico 87801; 3ARCO Oil and Gas Company, Plano, Texas 75075 SOCORRO 1992 11 NEW MEXICO INSTITUTE OF MINING & TECHNOLOGY Laurence H. Lattman, President NEW MEXICO BUREAU OF MINES & MINERAL RESOURCES Charles E. Chapin, Director and State Geologist BOARD OF REGENTS Ex Officio Bruce King, Governor of New Mexico Alan Morgan, Superintendent of Public Instruction Appointed Lt. Gen. Leo Marquez, President, 1989-1995, Albuquerque Charles Zimmerly, Secretary/Treasurer, 1991-1997, Socorro Diane D. Denish, 1992-1997, Albuquerque J. Michael Kelly, 1992-1997, Roswell Steve Torres, 1991-1997, Albuquerque BUREAU STAFF ORIN J. ANDERSON, Senior Geologist DEBBIE GOERING, Staff Secretary VIRGINIA McLesion, Economic Geologist RUBEN ARCHULETA, Metallurgical Lab. Tech. Lois GOLLMER, Geotechnical Records Clerk NORMA J. MEEKS, Director of Publications Office Augustus K. ARMSTRONG, USGS Geologist IBRAHIM GUNDILER, Senior Metallurgist BARBARA R. Popp, Chemical lab. Tech. II GEORGE S. AusTIN, Senior Industrial Minerals Geologist STEVE HAASE, Ground-Water Geologist MARSHALL A. REITER, Senior Geophysicist AL BACA, Maintenance Carpenter II WILLIAM C. HANEBERG, Engineering Geologist JACQUES R. RENAULT, Senior Geologist JAMES M. BARKER, Senior Industrial Minerals Geologist JOHN W. HAWLEY, Senior Env. Geologist JAMES M. ROBERTSON, Senior Economic Geologist PAUL W. BAUER, Field Economic Geologist LYNNE HEMENWAY, Computer Pub./Graphics Spec. -
2017 Colorado Sheep & Goat
C OLORADO PARKS & WILDLIFE 2017 Colorado Sheep & Goat APPLICATION DEADLINE: APRIL 4 online brochure cpw.state.co.us 2017 Colorado Sheep & Goat Hunting Online Features Watch more Colorado Parks and Wildlife videos on our VIMEO & YOUTUBE VIDEO CHANNELS VIDEOS: WHAT’S NEW: 2017 BIG GAME GET UPDATED on the new, general regulatory changes to the 2017 Sheep & Goat and Big Game brochures. See this brochure for species- and unit- specific changes. THE FUTURE OF CONSERVATION LEARN HOW your license dollars contribute directly to the conservation of wildlife species and outdoor recreation in Colorado. HUNTER PINK GET INFORMED about the new hunter pink cloth- ing alternative to fluorescent orange. There’s a link MORE ONLINE to the fact sheet in the video too! QUIZ AND RESOURCES: MOUNTAIN GOAT IDENTIFICATION HUNTING COLORADO’S If you are hunting mountain goats, it is difficult — but extremely impor- tant — that you identify female goats properly. Read the CPW online PUBLIC LANDS guide and take the quiz to ensure you know your target and avoid fines once you are hunting in the field. CLICK TO TAKE THE QUIZ HEAR THE DETAILS about big game, small game Rocky Mountain Bighorn Sheep and waterfowl hunting on Colorado’s public lands, © Wayne Lewis, CPW 2 including State Wildlife Areas, State Trust Lands and State Parks. 2017 Colorado Sheep & Goat Hunting 2017 Colorado Sheep & Goat Hunting TABLE OF CONTENTS 2017 What’s New ...................................................1 CPW OFFICE LOCATIONS cpw.state.co.us License Fees & Information ................................. 1 ADMINISTRATION Watch more Colorado Parks and Wildlife videos on our VIMEO & YOUTUBE VIDEO CHANNELS • Fees and surcharges 1313 Sherman St., #618 • Hunter education requirements Denver, 80203 303-297-1192 In the Field & Special License Information ......... -
The Impact of Temperature, Elevation, and Aspect on The
THE IMPACT OF TEMPERATURE, ELEVATION, AND ASPECT ON THE POTENTIAL DISTRIBUTION OF PERMAFROST IN SAN JUAN MOUNTAINS, COLORADO A Dissertation by MUHAMMAD IRHAM Submitted to the Office of Graduate and Professional Studies of Texas A&M University in partial fulfillment of the requirements for the degree of DOCTOR OF PHILOSOPHY Chair of Committee, John R. Giardino Committee Members, John D. Vitek Hongbin Zhan Chris Houser Head of Department, Michael Pope May 2016 Major Subject: Geology Copyright 2016 Muhammad Irham ABSTRACT A portions of San Juan Mountains are located in the alpine critical zone, which extends from the boundary layer between the atmosphere and the surface of Earth. In this zone, atmospheric and geomorphic processes drive all interactions. The focus of this research is on changes associated with the location of potential permafrost in the San Juan Mountains of Colorado. Study of potential permafrost can provide important information regarding the distribution and stability of permafrost under warming climatic conditions. Understanding patterns of temperature and aspect are vital steps in understanding the distribution of potential permafrost in alpine environments, its current stability, and such changes that might occur in the future. To study this question, three objectives were assessed. First, historical climate records, standard adiabatic rate, and ArcGIS methods were applied to analyze the impact of temperature on the climate change. Second, aerial photographs and field investigations were applied to classify the spatial extent of permafrost in a selected region of the San Juan Mountains. Digital Elevation Models (DEM) in ArcGIS were created to evaluate elevation, slope, and aspect relative to the elevations of permafrost. -
A Validation of Ground Penetrating Radar For
A VALIDATION OF GROUND PENETRATING RADAR FOR RECONSTRUCTING THE INTERNAL STRUCTURE OF A ROCK GLACIER: MOUNT MESTAS, COLORADO, USA A Thesis by WILLIAM REVIS JORGENSEN Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE May 2007 Major Subject: Geology A VALIDATION OF GROUND PENETRATING RADAR FOR RECONSTRUCTING THE INTERNAL STRUCTURE OF A ROCK GLACIER: MOUNT MESTAS, COLORADO, USA A Thesis by WILLIAM REVIS JORGENSEN Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE Approved by: Co-Chairs of Committee, John R. Giardino Mark Everett Committee Member, Vatche P. Tchakerian Head of Department, John H. Spang May 2007 Major Subject: Geology iii ABSTRACT A Validation of Ground Penetrating Radar for Reconstructing the Internal Structure of a Rock Glacier: Mount Mestas, Colorado, USA. (May 2007) William Revis Jorgensen, B.S.; B.S., Texas A&M University Co-Chairs of Advisory Committee: Dr. John R. Giardino Dr. Mark Everett Rock glaciers are dynamic landforms and, as such, exhibit interesting and well- developed structural features, which translate to surface morphology in the form of ridges and furrows. These distinguishing features have led researchers to study the physics behind the movement and internal deformation of rock glaciers. For years researchers had no access to the internal makeup of rock glaciers. Thus, proposed models and discussion have been based on theoretical concepts of electromagnetic (EM) wave propogation. With the application of ground penetrating radar (GPR) to provide a view of the interior structure of a rock glacier, researchers had “real” data to verify their models.