Before the Oil and Gas Conservation Commission of the State of Colorado
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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. -
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. -
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. -
7.0 References
I-70/32nd Avenue Interchange Environmental Assessment 7.0 REFERENCES Amuedo and Ivey. 1975. Coal mine subsidence and land-use in the Boulder-Weld coalfield, Boulder and Weld Counties, Colorado: Colorado Geological Survey, Environmental Geology Series EG-9. Anderson, D.G. and J. Stevens. 2000. City of Wheat Ridge Open Space Areas Biological Inventory. Colorado. American Society for Testing and Materials (ASTM). 2000. ASTM Standards on Environmental Site Assessments for Commercial Real Estate. E 1527-00. Beane, Ronald. 1998. Presence/absence surveys for Preble’s meadow jumping mouse, Coors Brewing Company – Eastern Parcel, Jefferson County, Colorado. October 14. Brown, R.W. 1943. Cretaceous-Tertiary boundary in the Denver Basin, Colorado: Geological Society of America Bulletin, v. 54. Brown, R.W. 1962. Paleocene flora of the Rocky Mountains and the Great Plains: U.S. Geological Survey Professional Paper 375. Bryant, B., McGrew, L., and Wobus, R.A. 1981. Geologic map of the Denver 1° X 2° Quadrangle, north-central Colorado: U.S. Geological Survey Investigations Map, I-1163, 2 sheets (Scale 1:250,000). CH2MHILL. 2000. I-70 Denver to Golden Major Investment Study, Final Major Investment Study Report. November. CH2M HILL. 2001a. Ute ladies’-tresses orchid presence/absence survey final report, I-70/SH 58 Interchange, Jefferson County, Colorado. CDOT Project No. NH 0703-246. October 31. CH2M HILL. 2001b. Threatened, endangered, and sensitive species, I-70/SH 58 Interchange, Jefferson County, Colorado. CDOT Project No. NH 0703-246. October. City of Lakewood. 2003. Comprehensive Plan. February. Retrieved March 2006 from http://www.ci.lakewood.co.us City of Wheat Ridge. -
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. -
Denver Basin
Regional Tectonics and Their Thermal Influence on Sedimentary Basins: Denver Basin BROKAW, CASEY P., Graduate Student (Geophysics), Southern Methodist University, Roy M. Huffington Department of Earth Sciences Purpose Observations & Analysis The purpose of this project is to analyze the heat flow regime within the sedimentary Denver Basin and assess its variability. Thermal conduc- Thermal Conductivity of Basin Sediments Bottom Hole Temperature Data tivity measurements were made on Cretaceous sedimentary core samples provided by Anadarko Petroleum Corp. and the United States Geo- Average thermal conductiv- logical Survey Core Research Center (USGS CRC). Measured thermal conductivity values were used to calibrate and constrain heat flow ity values by formation. Formations are scaled for within the basin. Two equilibrium logs along with the newly measured thermal conductivity were used to calculate site specific heat flow. thickness and grain size. These new data points help constrain the observed variation in heat flow along the basin’s western syncline. Methods for the analytics of Thermal conductivity meas- urements were made on causation of basin thermal variability will follow outlines similar to those of Blackwell & Steele, 1989 (see Table 1 for thermal effects). core samples utilizing the divided bar apparatus and Table 1. From Blackwell and Steele’s study Thermal Conductivity of Sedimentary Rocks: methods outlined by Black- Measurement and Significance. It Illustrates the variables and their scale of effect that can well & Spafford, 1987. Study Area effect the thermal regimes within sedimentary basins. Generally sediments showed a decrease in ther- Uncorrected BHTS were extracted utilizing a spatial extraction (10 km radius from Eq. log well site) based on the sedimentary formations * mal conductivity value with an increase in shale/clay they were measured within. -
DENVER BASIN PROVINCE (039) by Debra K
DENVER BASIN PROVINCE (039) by Debra K. Higley, Richard M. Pollastro, and Jerry L. Clayton INTRODUCTION The Denver Basin Province is an asymmetrical Laramide-age structural basin located in eastern Colorado, southeastern Wyoming, the southwestern corner of South Dakota, and the Nebraska Panhandle. Two basin deeps located along the axis of the basin, close to the Front Range, separate the steeply dipping western flank and gently dipping eastern flank. The basin is bounded on the west by the Front Range of the Rocky Mountains, on the northwest by the Hartville Uplift, on the northeast by the Chadron Arch, and on the southwest and southeast by the Apishapa Uplift and Las Animas Arch, respectively. The primary producing plays in this province are the Dakota Group (Combined D and J Sandstones) Play (3905), and the J Sandstone Deep Gas (Wattenberg) Play (3906). Approximately 90 percent of the 800 MMBO and 1.2 TCFG produced from the basin has been from the J sandstone (Land and Weimer, 1978, Tainter, 1984). These two plays include 180 oil accumulations containing 1 or more MMBO. Eighteen fields have produced 6 BCFG or more (Hemborg, 1993d). Half of the province's 1.2 TCFG has been produced from the Wattenberg field; this field was discovered in 1970 and has produced about 0.63 TCFG and 2.2 MMBO from the J sandstone, Codell Sandstone, and Sussex (Terry) Sandstone. The largest oil field in the Denver Basin is Adena with more than 62 MMBO produced from the J and D sandstones and estimated ultimate recoverable of 62.5 MMBO. -
Abdullin Colostate 0053N 11378.Pdf (3.002Mb)
THESIS GEOPHYSICAL CONSTRAINTS ON THE FLEXURAL SUBSIDENCE OF THE DENVER BASIN Submitted by Ayrat Abdullin Department of Geosciences In partial fulfillment of the requirements For the Degree of Master of Science Colorado State University Fort Collins, Colorado Fall 2012 Master’s Committee: Advisor: Dennis L. Harry Sven Egenhoff Michael Lefsky ABSTRACT GEOPHYSICAL CONSTRAINTS ON THE FLEXURAL SUBSIDENCE OF THE DENVER BASIN The Denver Basin is an asymmetric Laramide (Late Cretaceous through Eocene) foreland basin covering portions of eastern Colorado, northwestern Kansas, southwestern Nebraska, and southeastern Wyoming, USA. It is bordered on the west by the Rocky Mountain Front Range Uplift, a basement cored Laramide anticline bounded by thrust faults, and on the east by the Great Plains and stable North American craton. A ~400 mGal negative Bouguer gravity anomaly exists over the Denver Basin and Front Range Uplift, with its minimum located over the highest topography in the central part of the uplift, approximately 100 km west of the Denver Basin. This study examines three hypotheses concerning the isostatic state of the basin and adjacent Front Range Uplift. These hypotheses are that the modern shape of the basin is due to: 1) flexure of the lithosphere under the surface load of the current topography, or 2) flexure under a subsurface load beneath the Rocky Mountains, or 3) a combination of both surface and subsurface loads. To test these hypotheses, spectral analysis and forward gravity modeling was conducted along three profiles located in the northern, central, and southern parts of the basin. Bouguer gravity power spectra along the profiles reveal 5 major density interfaces interpreted to represent the base of the lithosphere (at depths of 132 to 153 km), base of the crust (45-55 km), a mid-crustal boundary (about 20 km), the top of Precambrian basement (1-2 km), and a boundary between the Pierre Shale and Niobrara Formations within the pre-Laramide sedimentary section (-1-0 km).