Ages of Selected Intrusive Rocks Ana Associated Ore Deposits in the Colorado Mineral Belt
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MOUNT SOPRIS 12,965 Feet
Aspen Ranger District 806 West Hallam Aspen, CO 81611 (970) 925-3445 (970) 925-5277- Fax United States Department of Agriculture MOUNT SOPRIS 12,965 feet LENGTH: 6 miles from Dinkle Lake ELEVATION GAIN: 4,253 feet AVERAGE HIKING/CLIMBING TIME: USGS MAP(S): Sopris 10 hours RECOMMENDED SEASON(S): SKILL FACTOR: More difficult Late spring and summer ATTRACTIONS/CONSIDERATIONS: If you plan to climb Sopris, allow two days. The first day, hike to the lakes, set up camp in a designated site and explore, fish or just enjoy the scenery. On the second day, get up early and begin climbing to finish the hike before the aftenoon thunderstorms. ACCESS: Procees south on Hwy 133 for 1.4 miles to Prince Creek Road and take a left. The trailhead is approximately 8 miles up the road and just before the Dinkle Lake at the Thomas Lake Trailhead. The first three miles to Thomas Lakes is easy. NARRATIVE: The easiest route is up the east ridge. From the upper lake, walk to the base of the steep slope to the southeast of the lake. Ascend this slope on the new hiking trail to the ridge, and continue across the high, sparsely timbered slope to the southern ridge. Follow this ridge up the mountain. You will come upon one stretch of fairy steep, loose rock but should have no problem if you use care. Soon you will be on the main ridge to the summit. Enjoy your view! You may want to cross one half mile saddle to West Sopris, which is the same elevation as East Sopris, and offers a superb view of the Crystal River Valley and Avalanche Creek. -
Crystal River and Wast Sopris Creek Report Section 7
7. References Bredehoeft, J.D. 2006. On Modeling Philosophies. Ground Water, Vol. 44 (4), pp. 496-499. Bryant, B. and P.L. Martin. 1988. The Geologic Story of the Aspen Region -Mines, Glaciers and Rocks. Bulletin 1603. U.S. Geological Survey. CDNR. 2008. Guide to Colorado Water Rights, Well Permits, and Administration. Colorado Dept. of Natural Resources, Office of State Engineer. (http://www.water.state.co.us/pubs/wellpermitguide.pdf ). Daly, C. and G.L. Johnson. 1999. PRISM Spatial Climate Layers; PRISM Guide Book. PRISM Group, Oregon State University. Devlin, J.F., and M. Sophocleous. 2005. The Persistence of the Water Budget Myth and its Relationship to Sustainability. Hydrogeology Journal, Vol. 13(4), pp. 549-554. ESRI. 2002. Getting Started with ArcGISTM . ESRI, Redlands, California. Freethey, G.W., and G.E. Gordy. 1991. Geohydrology of Mesozoic Rocks in the Upper Colorado River Basin in Arizona, Colorado, New Mexico, Utah, and Wyoming, Excluding the San Juan Basin. Professional Paper 1411-C. U.S. Geological Survey. Geldon, A.L. 2003a. Geology of Paleozoic Rocks in the Upper Colorado River Basin in Arizona, Colorado, New Mexico, Utah, and Wyoming, Excluding the San Juan Basin. Professional Paper 1411-A. U.S. Geological Survey. Geldon, A.L. 2003b. Hydrologic Properties and Ground-Water Flow Systems of the Paleozoic Rocks in the Upper Colorado River Basin in Arizona, Colorado, New Mexico, Utah, and Wyoming, Excluding the San Juan Basin. Professional Paper 1411-B. U.S. Geological Survey. Harlan, R., K.E. Kolm, and E.D. Gutentag. 1989. Water Well Design and Construction. Elsevier Science Publishers, Amsterdam, The Netherlands. -
Personal Recollections of Early Denver
Personal Recollections of Early Denver .J OSEPII EMERSOX S11nTn* Recollections, like everything else, must have a beginning, and my first memory of early Denver has to do with a Fourth of .July Christmas. It has remained vivid, unforgettable, undoubtedly because of th<:' successive shocks to the sensitive ear drums of a small child. Tt was prior to the Chinese riot of 1880 and the large Chinatown of the city, extending from Sixteenth along vVazee and Vlynkoop streets and directly in the rear of the American House for seYeral blocks, was a busy mart, a growth of the steady immi gration of the "Celestials" to Colorado, where thousands had been, and still were, employed in placer mining around Central City, at Fairplay, Tarryall, California Gulch, and other gold camps. Chinatmn1 was their suppl~' source. Here \Yere silk and clothing shops, stores of exotic atmosphere with shelves crowded with im ports, fine tea, spices, drugs, and foods from China, tapestries, fans, laces, and there were many laundries. Underground floors were tunnels leading to burrows and the larger rooms where Nepen- 1heized sleepers lay in bunks, the air sticky and sweet with the fumes of opium. 'l'he steam laundry hadn't come, and the Chinese had a monop oly on laundering. 'l'o homes all over the city trotted the tireless, affable, pig-tailed little yellow men in their blue-black tunics, flap ping trousers and felt white-soled slippers, delivering newspaper wrapped bundles. We " ·ere living at Coffield 's ''family boarding house,'' a spacious two-story verandahed frame residence where the Colorado National Bank now stands at Seventeenth and Champa streets. -
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. -
2015 SSSA Program
Latinos and the Change of a Nation: Implications for the Social Sciences 95th Annual Meeting of the Southwestern Social Science Association April 8 – 11, 2015 Grand Hyatt, Denver Denver, Colorado 1 SSSA Events Time Location Wednesday April 8 Registration & Exhibits 2:00 - 5:00 p.m. Imperial Ballroom SSSA Executive Committee 3:00 - 5:00 p.m. Mount Harvard Nominations Committee Meeting 1 4:00 – 5:30 pm Mount Yale Thursday April 9 Registration & Exhibits 8:00 a.m. – 5:00 p.m. Imperial Ballroom Nominations Committee 8:30 - 9:45 a.m. Mount Harvard Membership Committee 8:30 - 9:45 a.m. Mount Yale Budget and Financial Policies Committee 8:30 - 9:45 a.m. Mount Oxford Resolutions Committee 10:00 - 11:15 a.m. Mount Harvard Editorial Policies Committee 10:00 - 11:15 a.m. Mount Oxford Site Policy Committee 10:00 - 11:15 a.m. Mount Yale SSSA Council 1:00 - 3:45 p.m. Mount Oxford SSSA Presidential Address 4:00 - 5:15 p.m. Mount Sopris B SSSA Presidential Reception 5:30 - 7:30 p.m. Mount Evans Friday April 10 Registration & Exhibits 8:00 a.m. – 5:00 p.m. Imperial Ballroom SSSA Student Social & Welcome Continental 7:15 – 8:45 a.m. Grand Ballroom Breakfast (FOR REGISTERED STUDENTS ONLY, No Guests or Faculty/Professional Members) SSSA General Business Meeting 1:00 - 2:15 p.m. Grand Ballroom Saturday April 11 Registration 8:00 – 11:00 am Imperial Ballroom 2016 Program Committee 7:15 - 8:30 a.m. Pike’s Peak Getting to Know SSSA 8:30 – 9:15 a.m. -
Geochronology Database for Central Colorado
Geochronology Database for Central Colorado Data Series 489 U.S. Department of the Interior U.S. Geological Survey Geochronology Database for Central Colorado By T.L. Klein, K.V. Evans, and E.H. DeWitt Data Series 489 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior KEN SALAZAR, Secretary U.S. Geological Survey Marcia K. McNutt, Director U.S. Geological Survey, Reston, Virginia: 2010 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment, visit http://www.usgs.gov or call 1-888-ASK-USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: T.L. Klein, K.V. Evans, and E.H. DeWitt, 2009, Geochronology database for central Colorado: U.S. Geological Survey Data Series 489, 13 p. iii Contents Abstract ...........................................................................................................................................................1 Introduction.....................................................................................................................................................1 -
Profiles of Colorado Roadless Areas
PROFILES OF COLORADO ROADLESS AREAS Prepared by the USDA Forest Service, Rocky Mountain Region July 23, 2008 INTENTIONALLY LEFT BLANK 2 3 TABLE OF CONTENTS ARAPAHO-ROOSEVELT NATIONAL FOREST ......................................................................................................10 Bard Creek (23,000 acres) .......................................................................................................................................10 Byers Peak (10,200 acres)........................................................................................................................................12 Cache la Poudre Adjacent Area (3,200 acres)..........................................................................................................13 Cherokee Park (7,600 acres) ....................................................................................................................................14 Comanche Peak Adjacent Areas A - H (45,200 acres).............................................................................................15 Copper Mountain (13,500 acres) .............................................................................................................................19 Crosier Mountain (7,200 acres) ...............................................................................................................................20 Gold Run (6,600 acres) ............................................................................................................................................21 -
Robotic Asteroid Prospector
Robotic Asteroid Prospector Marc M. Cohen1 Marc M. Cohen Architect P.C. – Astrotecture™, Palo Alto, CA, USA 94306-3864 Warren W. James2 V Infinity Research LLC. – Altadena, CA, USA Kris Zacny,3 Philip Chu, Jack Craft Honeybee Robotics Spacecraft Mechanisms Corporation – Pasadena, CA, USA This paper presents the results from the nine-month, Phase 1 investigation for the Robotic Asteroid Prospector (RAP). This project investigated several aspects of developing an asteroid mining mission. It conceived a Space Infrastructure Framework that would create a demand for in space-produced resources. The resources identified as potentially feasible in the near-term were water and platinum group metals. The project’s mission design stages spacecraft from an Earth Moon Lagrange (EML) point and returns them to an EML. The spacecraft’s distinguishing design feature is its solar thermal propulsion system (STP) that provides two functions: propulsive thrust and process heat for mining and mineral processing. The preferred propellant is water since this would allow the spacecraft to refuel at an asteroid for its return voyage to Cis- Lunar space thus reducing the mass that must be launched from the EML point. The spacecraft will rendezvous with an asteroid at its pole, match rotation rate, and attach to begin mining operations. The team conducted an experiment in extracting and distilling water from frozen regolith simulant. Nomenclature C-Type = Carbonaceous Asteroid EML = Earth-Moon Lagrange Point ESL = Earth-Sun Lagrange Point IPV = Interplanetary Vehicle M-Type = Metallic Asteroid NEA = Near Earth Asteroid NEO = Near Earth Object PGM = Platinum Group Metal STP = Solar Thermal Propulsion S-Type = Stony Asteroid I. -
Carbondale Creative District (PDF)
5TH EDITION Guidebook WIFI LOGIN • Network: Orchard Free Public Wifi • No password WELCOME TO THE SUMMIT A two-day professional development conference for creative entrepreneurs, emerging creatives, municipal and non-profit cultural workers, and creative district leaders. May 5, 2016 Greetings: On behalf of the State of Colorado, it is my distinct pleasure to welcome you to the 5th annual Colorado Creative Industries Summit here in Carbondale. As embodied by this year’s theme, the State of Colorado is embracing a culture of possibility. We are recognized as a leader in building sustainable communities and economies by cultivating creative talent, leveraging local resources, and fostering a sense of place through the arts and innovation. It is our independent spirit at the heart of these movements and what continues to drive us forward, paving the way for others to follow. Colorado’s creative industries have a significant impact on the strength of our economy and continue to play an integral role in our overall vitality. Whether it is a community on the Front Range or in a small rural or mountain town, the creative sector touches all four corners of our state, contributing to the inner workings of what makes us unique. During your time in Carbondale, we hope you will take a moment to celebrate the exceptional variety, skill, and determination inherent within the Colorado creative community. As Coloradans, we all have the good fortune of benefitting from the diverse projects and goods generated by our creative industries. Thank you to everyone who is participating in this year’s summit. -
Forest Wide Hazardous Tree Removal and Fuels Reduction Project
107°0'0"W VAIL k GYPSUM B e 6 u 6 N 1 k 2 k 1 h 2 e . e 6 . .1 I- 1 o 8 70 e c f 7 . r 0 e 2 2 §¨¦ e l 1 0 f 2 u 1 0 3 2 N 4 r r 0 1 e VailVail . 3 W . 8 . 1 85 3 Edwards 70 1 C 1 a C 1 .1 C 8 2 h N 1 G 7 . 7 0 m y 1 k r 8 §¨¦ l 2 m 1 e c . .E 9 . 6 z W A T m k 1 5 u C 0 .1 u 5 z i 6. e s 0 C i 1 B a -7 k s 3 2 .3 e e r I ee o C r a 1 F G Carterville h r e 9. 1 6 r g 1 N 9 g 8 r e 8 r y P e G o e u l Avon n C 9 N C r e n 5 ch w i r 8 .k2 0 N n D k 1 n 70 a tt e 9 6 6 8 G . c 7 o h 18 1 §¨¦ r I-7 o ra West Vail .1 1 y 4 u h 0 1 0. n lc 7 l D .W N T 7 39 . 71 . 1 a u 1 ch W C k 0 C d . 2 e . r e 1 e 1 C st G e e . r 7 A Red Hill R 3 9 k n s e 5 6 7 a t 2 . -
Isotopic Age Determinations, Unaltered and Hydrothermally Altered Igneous Rocks, North-Central Colorado Mineral Belt A.A
Isotopic age determinations, unaltered and hydrothermally altered igneous rocks, north-central Colorado mineral belt A.A. Bookstrom, C.W. Naeser, and J.R. Shannon Isochron/West, Bulletin of Isotopic Geochronology, v. 49, pp. 13-20 Downloaded from: https://geoinfo.nmt.edu/publications/periodicals/isochronwest/home.cfml?Issue=49 Isochron/West was published at irregular intervals from 1971 to 1996. The journal was patterned after the journal Radiocarbon and covered isotopic age-dating (except carbon-14) on rocks and minerals from the Western Hemisphere. Initially, the geographic scope of papers was restricted to the western half of the United States, but was later expanded. The journal was sponsored and staffed by the New Mexico Bureau of Mines (now Geology) & Mineral Resources and the Nevada Bureau of Mines & Geology. All back-issue papers are available for free: https://geoinfo.nmt.edu/publications/periodicals/isochronwest This page is intentionally left blank to maintain order of facing pages. 13 ISOTOPIC AGE DETERMINATIONS, UNALTERED AND HYDROTHERMALLY ALTERED IGNEOUS ROCKS, NORTH-CENTRAL COLORADO MINERAL BELT ARTHUR A. BOOKSTROM 1805 Glen Ayr Dr., Lakewood, CO 80215 CHARLES W. NAESER U.S. Geological Survey, Denver, CO 80225 JAMES R. SHANNON Department of Geology, Colorado School of Mines, Golden, CO 80401 Monzonite and granodiorite intrusions of the Empire Fission-track age determinations were done in the fission- district are early Tertiary (65 Ma) in age, as dated by track laboratory of the U.S. Geological Survey in Denver, Simmons and Hedge (1978). Monzonite and granodiorite and at the University of Utah Research Institute. People intrusions of the Alma district have yielded isotopic ages who cooperated in this study include Mark Coolbaugh, ranging from 71 to 41 Ma (Bookstrom, in press). -
Old Spanish National Historic Trail Final Comprehensive Administrative Strategy
Old Spanish National Historic Trail Final Comprehensive Administrative Strategy Chama Crossing at Red Rock, New Mexico U.S. Department of the Interior National Park Service - National Trails Intermountain Region Bureau of Land Management - Utah This page is intentionally blank. Table of Contents Old Spanish National Historic Trail - Final Comprehensive Administrative Stratagy Table of Contents i Table of Contents v Executive Summary 1 Chapter 1 - Introduction 3 The National Trails System 4 Old Spanish National Historic Trail Feasibility Study 4 Legislative History of the Old Spanish National Historic Trail 5 Nature and Purpose of the Old Spanish National Historic Trail 5 Trail Period of Significance 5 Trail Significance Statement 7 Brief Description of the Trail Routes 9 Goal of the Comprehensive Administrative Strategy 10 Next Steps and Strategy Implementation 11 Chapter 2 - Approaches to Administration 13 Introduction 14 Administration and Management 17 Partners and Trail Resource Stewards 17 Resource Identification, Protection, and Monitoring 19 National Historic Trail Rights-of-Way 44 Mapping and Resource Inventory 44 Partnership Certification Program 45 Trail Use Experience 47 Interpretation/Education 47 Primary Interpretive Themes 48 Secondary Interpretive Themes 48 Recreational Opportunities 49 Local Tour Routes 49 Health and Safety 49 User Capacity 50 Costs 50 Operations i Table of Contents Old Spanish National Historic Trail - Final Comprehensive Administrative Stratagy Table of Contents 51 Funding 51 Gaps in Information and