Colorado State-Wide Forest Legacy Assessment of Need
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Richard Dallin Westwood: Sheriff and Ferryman of Early Grand County
Richard Dallin Westwood: Sheriff and Ferryman of Early Grand County BY JEAN M. WESTWOOD ON FEBRUARY I7, I889, RICHARD DALLIN WESTWOOD, twenty-six years old, left Mount Pleasant, Utah, bound for Moab, a settlement in the far eastern edge of what was then Emery County. He was looking for a piece of farm land on which he could build a home for himself, his young wife, Martha, and their baby daughter, Mary Ellen. It was just ten years since the first permanent settlers had moved into "Spanish Valley" by the Grand (Colorado) River in the southeast part of the territory. The valley had long been part of western history. Mrs. Westwood lives in Scottsdale, Arizona. Above: Richard Dallin Westwood, ca. 1888. All photographs accompanying this article are courtesy of the author. Richard Dallin Westwood 67 Indian "writings" are still found on the rocks. Manos, metates, arrow heads, stone weapons, and ancient bean, maize, and squash seeds have all been frequent finds throughout the area, attesting to early Indian cultures. The Spanish Trail through here was used first by the early Span iards as a route from New Mexico to California.^ Later it was used in part by Mexican traders, trappers, prospectors, and various Indian tribes. The first party traveling the entire trail apparently was led by WiUiam WolfskiU and George C. Young in the winter of 1830-31.2 In 1854 Brigham Young sent a small expedition under William D. Huntington to trade with the Navajos and explore the southern part of Utah territory. They used this route. The next year Young called forty- one men under Alfred N. -
Understanding and Mapping Variability of the Niobrara Formation
UNDERSTANDING AND MAPPING VARIABILITY OF THE NIOBRARA FORMATION ACROSS WATTENBERG FIELD, DENVER BASIN by Nicholas Matthies A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Master of Science (Geology). Golden, Colorado Date________________ Signed:____________________________________ Nicholas Matthies Signed:____________________________________ Dr. Stephen A. Sonnenberg Thesis Advisor Golden, Colorado Date:_______________ Signed:____________________________________ Dr. Paul Santi Professor and Head Department of Geology and Geological Engineering ii ABSTRACT Wattenberg Field has been a prolific producer of oil and gas since the 1970s, and a resurgence of activity in recent years in the Niobrara Formation has created the need for a detailed study of this area. This study focuses on mapping regional trends in stratigraphy, structure, and well log properties using digital well logs, 3D seismic data, and core X-ray diffraction data. Across Wattenberg, the Niobrara is divided into the Smoky Hill Member (made up of A Chalk, A Marl, B Chalk, B Marl, C Chalk, C Marl, and Basal Chalk/Marl) and the Fort Hays Limestone Member. Directly beneath the Niobrara, the Codell Sandstone is the uppermost part of the Carlile Formation. Stratigraphic trends in these units are primarily due to differential compaction and compensational sedimentation. The largest structural trend is a paleo-high that runs east-west to northeast-southwest across the middle of the field. It has a relief of about 100 ft, and is 20 mi wide. The A Chalk and A Marl show evidence of submarine erosion over this area. Faults mapped from 3D seismic data are consistent with previously published data on a proposed polygonal fault system in the Denver Basin. -
High-Resolution Correlation of the Upper Cretaceous Stratigraphy Between the Book Cliffs and the Western Henry Mountains Syncline, Utah, U.S.A
University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln Dissertations & Theses in Earth and Atmospheric Earth and Atmospheric Sciences, Department of Sciences 5-2012 HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A. Drew L. Seymour University of Nebraska, [email protected] Follow this and additional works at: http://digitalcommons.unl.edu/geoscidiss Part of the Geology Commons, Sedimentology Commons, and the Stratigraphy Commons Seymour, Drew L., "HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A." (2012). Dissertations & Theses in Earth and Atmospheric Sciences. 88. http://digitalcommons.unl.edu/geoscidiss/88 This Article is brought to you for free and open access by the Earth and Atmospheric Sciences, Department of at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in Dissertations & Theses in Earth and Atmospheric Sciences by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH, U.S.A. By Drew L. Seymour A THESIS Presented to the Faculty of The Graduate College at the University of Nebraska In Partial Fulfillment of Requirements For Degree of Master of Science Major: Earth and Atmospheric Sciences Under the Supervision of Professor Christopher R. Fielding Lincoln, NE May, 2012 HIGH-RESOLUTION CORRELATION OF THE UPPER CRETACEOUS STRATIGRAPHY BETWEEN THE BOOK CLIFFS AND THE WESTERN HENRY MOUNTAINS SYNCLINE, UTAH. U.S.A. Drew L. Seymour, M.S. -
Book Cliffs the Book Cliffs Rise As If Startled out of the Mancos Shale Desert
!People of the Book Cliffs The Book Cliffs rise as if startled out of the Mancos Shale desert. This bright edge stretches east-west, two hundred miles between Grand Junction, Colorado and Price, Utah, stair-stepping four thousand feet up from the desert to a summit that’s cloaked in aspen, fir, and spruce. Erosion has dissected the cliffs into isolated canyons, carved by intermittent streams that all flow south toward the Colorado River. Even so, the cliffs and canyons are considered part of the !Uinta Basin because their rock layers, like the Green River Formation, are tilted north. Pockets of true wilderness still exist within the Book Cliffs. Black bear, bighorn, mule deer, and cougars are at home in these canyons. People have lived in and moved through this country for thousands of years−the Utes most recently, the Fremont before them, and the enigmatic Barrier !Canyon people with their alien pictographs staring at us as if from outer space. Wolf Bennett and his daughters came here from Colorado to see the pictographs and to clamber around the rocks of Sego Canyon. Wolf’s spent his life as a guide and values what these canyons !offer his family−opportunities to discover, a diversion from cityscapes, a sense of wonder. A mile down canyon, Bob Holloway and his two adopted children were watering fruit trees at the ranch he’d recently bought. The roof needed work. Bob and his wife wanted to get out of the rat race in Green River. That town’s population of 900 might swell if a proposed oil refinery and nuclear power plant are built. -
GROUNDWATER LEVELS in the DENVER BASIN BEDROCK AQUIFERS 2017
GROUNDWATER LEVELS in the DENVER BASIN BEDROCK AQUIFERS 2017 by Andrew D. Flor John W. Hickenlooper Robert W. Randall Governor Executive Director, DNR Kevin G. Rein Matthew A. Sares State Engineer Manager, Hydrogeology Section GROUNDWATER LEVELS IN THE DENVER BASIN BEDROCK AQUIFERS 2017 This report updates basic data concerning the depth to and elevation of groundwater in the four main Denver Basin bedrock aquifers collected during the spring and summer of 2017. The report is organized first by aquifer, then by well name. Well completion information is provided, where available. Wells that may be completed in more than one aquifer are listed according to the uppermost aquifer. Approximately 95 water-level measurements in this year’s report were obtained by Division of Water Resources (Division) personnel. A total of six wells have been instrumented with data loggers to collect daily water-level data. These include the following: - four wells in the Castle Rock area that monitor all four Denver Basin aquifers; CO3_LTDW (DB-204), CO3_TKD (DB-205), CO6_KA (DB-206) and CO3_KLF (DB-203); and - two wells near Golden in the Pleasant View Metropolitan District are completed in the Arapahoe (DB-201) and Laramie-Fox Hills (DB-200) aquifers. Water-level data from 126 cooperator wells are also included in this report. Personnel from cooperating water districts and municipalities graciously provided these data upon request. The Division appreciates the cooperation of the many entities that provide water-level information. Recent Legislation has directed the Division of Water Resources, in consultation with the Colorado Water Conservation Board, to encourage qualified parties to submit water level data for inclusion in the statewide water level database. -
BISON HERD UNIT MANAGEMENT PLAN Book Cliffs, Bitter Creek and Little Creek Herd Unit #10A and #10C Wildlife Board Approval November 29, 2007
1 BISON HERD UNIT MANAGEMENT PLAN Book Cliffs, Bitter Creek And Little Creek Herd Unit #10A AND #10C Wildlife Board Approval November 29, 2007 BOUNDARY DESCRIPTION Uintah and Grand counties - Boundary begins at the Utah-Colorado state line and the White River, south along this state line to the summit and north-south drainage divide of the Book Cliffs; west along this summit and drainage divide to the Uintah-Ouray Indian Reservation boundary; north along this boundary to the Uintah-Grand County line; west along this county line to the Green River; north along this river to the White River; east along this river to the Utah-Colorado state line. NORTH BOOK CLIFFS LAND OWNERSHIP RANGE AREA AND APPROXIMATE OWNERSHIP Bitter Creek Little Creek Combined North Subunit Subunit Subunits Ownership Area % Area % Area (acres) % (acres) (acres) BLM 644,446 45.6 2,389 4.1 646,835 44 SITLA 165,599 11.7 48,912 84.4 214,911 15 DWR 15,138 1.1 6,551 11.3 21,689 1 PRIVATE 70,091 5.0 0 0 70,091 5 UTE TRIBE TRUST 517,506 36.6 82 0.2 517,588 35 LAND TOTAL 1,412,740 100 57,934 100 1,471,114 100 BOOK CLIFFS BISON HISTORY AND STATUS Bison were historically present in the general East Tavaputs Plateau and Uintah Basin. The Escalante expedition reported killing a bison near the present site of Jensen, Utah in September 1776. Bison are also commonly depicted in Native American rock art and pictographs found throughout the area. -
Park County, Colorado World War II 4Th Draft Registration "Old Man"
Park County, Colorado World War II 4th Draft Registration "Old Man" This Registration was the 4th of 6 draft registrations conducted by the Selective Service System which commenced on April 27, 1942 and was terminated on March 31, 1947 by an act of Congress. The purpose of the registration was to collect information on industrial capacity and skills of men aged 45 to 64 who were born on April 18, 1877 through and including February 16, 1897 and who were not already in the military that could be utilized for national service if needed. A description including race, height, weight, complexion and obvious physical characteristics are included on the back of the card. Papers/cards attached to a few cards may give more information about the individuals' military history, decorations, citations, change of address or death. Copies of both sides of the card may be obtained by writing the National Archives & Records Administration, National Archives - St Louis, PO Box 38757, St. Louis, MO 63138-0757. The cost is $7.00. The information needed to obtain a copy of the card is the person's full name, city and county of registration, and date of birth. This compilation is for Park County, Colorado. Men who lived in Park County at the time of registration and those who were listed as born in Park County are included in this collection. Please see our other 3 counties for their respective areas. Name of Registrant Age Date of Birth Place of Birth City and/or County Registered In Colorado Ackley, Harley J. 50 22 Sep 1891 Sand Priarie, Wisconsin Fairplay, Park Co. -
PALEONTOLOGICAL TECHNICAL REPORT: 6Th AVENUE and WADSWORTH BOULEVARD INTERCHANGE PHASE II ENVIRONMENTAL ASSESSMENT, CITY of LAKEWOOD, JEFFERSON COUNTY, COLORADO
PALEONTOLOGICAL TECHNICAL REPORT: 6th AVENUE AND WADSWORTH BOULEVARD INTERCHANGE PHASE II ENVIRONMENTAL ASSESSMENT, CITY OF LAKEWOOD, JEFFERSON COUNTY, COLORADO Prepared for: TEC Inc. 1746 Cole Boulevard, Suite 265 Golden, CO 80401 Prepared by: Paul C. Murphey, Ph.D. and David Daitch M.S. Rocky Mountain Paleontology 4614 Lonespur Court Oceanside, CA 92056 303-514-1095; 760-758-4019 www.rockymountainpaleontology.com Prepared under State of Colorado Paleontological Permit 2007-33 January, 2007 TABLE OF CONTENTS 1.0 SUMMARY............................................................................................................................. 3 2.0 INTRODUCTION ................................................................................................................... 4 2.1 DEFINITION AND SIGNIFICANCE OF PALEONTOLOGICAL RESOURCES........... 4 3.0 METHODS .............................................................................................................................. 6 4.0. LAWS, ORDINANCES, REGULATIONS AND STANDARDS......................................... 7 4.1. Federal................................................................................................................................. 7 4.2. State..................................................................................................................................... 8 4.3. County................................................................................................................................. 8 4.4. City..................................................................................................................................... -
Denudation History and Internal Structure of the Front Range and Wet Mountains, Colorado, Based on Apatite-Fission-Track Thermoc
NEW MEXICO BUREAU OF GEOLOGY & MINERAL RESOURCES, BULLETIN 160, 2004 41 Denudation history and internal structure of the Front Range and Wet Mountains, Colorado, based on apatitefissiontrack thermochronology 1 2 1Department of Earth and Environmental Science, New Mexico Institute of Mining and Technology, Socorro, NM 87801Shari A. Kelley and Charles E. Chapin 2New Mexico Bureau of Geology and Mineral Resources, New Mexico Institute of Mining and Technology, Socorro, NM 87801 Abstract An apatite fissiontrack (AFT) partial annealing zone (PAZ) that developed during Late Cretaceous time provides a structural datum for addressing questions concerning the timing and magnitude of denudation, as well as the structural style of Laramide deformation, in the Front Range and Wet Mountains of Colorado. AFT cooling ages are also used to estimate the magnitude and sense of dis placement across faults and to differentiate between exhumation and faultgenerated topography. AFT ages at low elevationX along the eastern margin of the southern Front Range between Golden and Colorado Springs are from 100 to 270 Ma, and the mean track lengths are short (10–12.5 µm). Old AFT ages (> 100 Ma) are also found along the western margin of the Front Range along the Elkhorn thrust fault. In contrast AFT ages of 45–75 Ma and relatively long mean track lengths (12.5–14 µm) are common in the interior of the range. The AFT ages generally decrease across northwesttrending faults toward the center of the range. The base of a fossil PAZ, which separates AFT cooling ages of 45– 70 Ma at low elevations from AFT ages > 100 Ma at higher elevations, is exposed on the south side of Pikes Peak, on Mt. -
Colorado Agriculture
A Look at Colorado Agriculture Climate & Soil Capital: Denver • Colorado’s climate is generally dry and sunny. It is a semi-arid state averaging 15” of precipitation. • Colorado has dry winters, wetter springs and summer, highly changeable weather, often windy Population: 5,607,154 and the occasional monstrous thunderstorms with damaging hail. Founded: August 1, 1876 (38th) • Because of the difference in altitude found in the state there is a large range of temperatures. • The soils in the eastern plains regions and the valley of the western mountains are the most fertile State Bird: Lark bunting in the nation. State Tree: Blue Spruce • Colorado’s State soil is “Seitz soil” that consists of very deep, well drained, slowly permeable soils that were formed from igneous, sedimentary and volcanic rocks. Seitz soils are found on State Flower: Rocky Mountain mountains, mainly in southwestern and central Colorado. • Colorado’s warm days and cool nights help lock in sweetness in fruits such as peaches and Columbine melons. Number of Counties: 64 Crops & Livestock Largest City: Denver - 693,060 • Colorado ranks first nationally in production of proso millet. This annual grass is grown as a grain crop and is used for bird and livestock feed. Nickname: The Centennial State • Colorado’s production of sunflowers ranks fourth in the nation. Number of Farms: 33,800 • The San Luis Valley is the largest and highest alpine valley in the world capable of producing crops. Elevation in the valley ranges from 7,400 to 8,000 feet. Average Farm Size: 938 acres • Colorado produces more than 100 million points of pinto beach each year, ranking ninth nationally Total Farmland: 31.7 million acres in dry bean production. -
Geospatial Model of the Universal Soil Loss Equation for Fremont County, Colorado and the Universal Soil Loss Equation Applied to Fuels Reduction Treatments
Geospatial Model of the Universal Soil Loss Equation for Fremont County, Colorado and the Universal Soil Loss Equation Applied to Fuels Reduction Treatments A Master’s Thesis Presented to the Faculty of The College of Science and Mathematics Colorado State University-Pueblo Pueblo, Colorado In Partial Fulfillment Of the Requirements for the Master of Science in Applied Natural Science By Annie Thayer Merriam Colorado State University-Pueblo May 2005 Certificate of Acceptance This thesis presented in partial fulfillment of the requirements for the degree of Master of Science in Applied Natural Science by Annie Thayer Merriam Has been accepted by the Graduate Faculty of the College of Science and Mathematics Colorado State University-Pueblo. Approval of Thesis Committee: Graduate Advisor (Dr. Brian Vanden Heuvel) Date Committee Member (Dr. Neal Osborn) Date Committee Member (Dr. Moussa Diawara) Date Graduate Director (Dr. Mel Druelinger) Date Dedication For Butch, my nightlight in a strange house, For without you I would be sitting in the dark with a stubbed toe. Acknowledgements Foremost I would like to thank my supervisor at the Bureau of Land Management, John Smeins. John is responsible for giving me the opportunity to complete this research and he also helped refine my focus of this research to what it is today. John has also taught the true definition of fuels reduction: “eliminating small, weak, trees, so that, few, large, strong, ones may grow.” I would also like to thank everyone else who supported me at BLM. To my committee, the deepest thank you. To Dr. Neal Osborn who was the first to show me the wonderful world of botany and is the reason I have the profession that I do. -
Colorado Municipalities Vol
Colorado Municipalities Vol. 97, No. 1, January 2021 CML'S POLICY DEVELOPMENT PROCESS AND 2021 LEGISLATIVE PRIORITIES Going into each legislative session, CML begins its policy development process, which guides our legislative priorities. A DAY IN THE LIFE OF CML'S ADVOCACY TEAM CML's Advocacy Team represents municipal interests to the Colorado General Assembly. Check out what a typical day in the life looks like. LEGISLATIVE EDITION Building Communities. It’s what we do. James Mann Melissa Buck Sherry Villafane Ryan Miles Stephen Broden Senior Municipal Municipal Advisor Municipal Advisor Senior Investment Managing Director, Advisor/Principal Advisor Arbitrage Metropolitan District Advisory • Financial Management Planning Debt Issuance & Management • Investments & Arbitrage Consulting [email protected] ehlers-inc.com (800) 552-1171 The information provided in these materials does not create or imply a fiduciary relationship. It is solely for the purposes of marketing our services to you. Ehlers is the jointmarketing name for all its affliated businesses. Please visit www.ehlers-inc.com/disclosures for more information. CEBT | Partnering with CML CEBT CEBTPartnering has been providing with employee CML benefits through a nonprofit trust to public entities for CEBT has been providingover 30 employeeyears benefits through a nonprofit trust to public entities for 40 years Employee Benefit Solutions Medical - Dental - Vision - Life Jim Hermann | Willis Towers Watson (303) 803-9105 | (800) 332-1168 [email protected] www.cebt.org Comprehensive HR solutions for advanced organizational performance. HR ON DEMAND We offer On-Demand HR Services Human Resources support for your organization doesn’t need to break the budget. We offer scalable solutions so that you can pay for what you need.