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Fairplay, Leonard Summer Built the South Park Brewery* and Summer Saloon* of Native Sandstone
L When the fire of 1873 destroyed much of Fairplay, Leonard Summer built the South Park Brewery* and Summer Saloon* of native sandstone. They are among seven structures on their original sites in South Park City Museum (719-836-2387). L Named for a beloved teacher, Edith Teter School* is among the oldest in Colorado. The original 1880s section is constructed of native sandstone in the Italianate style. Listed on the State Alma Town Hall Linda Balough ALMA Register of Historic Properties, the building still serves as an ele- he settlement of Alma sprang up in 1873 when the Boston and mentary school in Fairplay (719-836-4279). TColorado Smelting Company built a smelting operation there. At L At 100 4th Street, South Park City Museum is a collection of 10,578 feet, Alma currently is the highest incorporated town in the United 40 period buildings containing 60,000 artifacts depicting a mining States. Listed on the State Register of Historic Properties, the 1925 Alma town from the late 1800s. Seven buildings are on their original sites, two of which are listed on the National Register of Historic Places. To School is a rare local example of Mission-style buildings. It now serves McGraw Park Gary E. Nichols Como Roundhouse Debra Queen-Stremke BAILEY arrange group tours call (719) 836-2387. as Alma’s Town Hall and is open to the public during regular business n 1864 William L. Bailey settled here and built the Entriken Cabin with from 1883 to 1948. A smaller building was moved to the school site in L Originally a 1931 hostelry the Hand Hotel Bed & Breakfast hours. -
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. -
Regional Analysis of Flood Hazards Along the Colorado Front Range.” Speaker--John Pitlick, Professor of Geography, University of Colorado, Boulder
Newsletter of the Society March 2014 ColoradoColorado ScientificScientific SocietySociety The objective of the Society is to promote the knowledge and understanding of Earth science, and its application to human needs Thursday, March 20th: R EGIONAL A NALYSIS OF F LOOD H AZARDS ALONG THE C OLORADO F RONT R ANGE by John Pitlick Professor of Geography University of Colorado, Boulder Location—Shepherd of the Hills Church, 11500 W. 20th. Ave. (at Simms St.), Lakewood, Colorado Social time— 6:30 p.m. Lecture—7:00 p.m. 1 Abstract The hazards associated with rare but intense rainfall are well known in Colorado, and many communi- ties along the Front Range have taken action over the years to mitigate potential damage and loss of life from rare floods. In September 2013, we had the opportunity to observe firsthand what it is like to get half a years-worth of precipitation in one or two days, and we can begin to appreciate how the actions taken to reduce flood risks in the city of Boulder benefited the community as a whole. Nonetheless many questions have arisen in the aftermath of the 2013 flood. For example, media reports have sug- gested that this was a 100-yr flood. What is the basis for that estimate? How do published maps of in- undation for floods with different return periods compare with the extent of flooding in 2013? Did burned areas contribute disproportionately to the floods? We don't have complete answers to all these questions just yet, thus my goal in this talk is to share results from past work (my own, plus others) that will help put the September 2013 floods in perspective Biography John Pitlick's research focuses on linkages between surface-water hydrology and geomorphology in high-gradient river systems. -
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 -
Integrated Management of Target Shooting Scoping Proposed Action 1
INTEGREATED MANAGEMENT OF TARGET SHOOTING ON THE PIKE NATIONAL FOREST Proposed Action for Public Scoping, January 2021 Background The Pike National Forest (the Forest), part of the Pike and San Isabel National Forests Cimarron and Comanche National Grasslands, is located in central Colorado, stretching north from Pikes Peak to Mount Evans, and west to the Continental Divide past the town of Fairplay (Figure 1). Given the Forest includes part of the Colorado Front Range adjacent to the two most populous centers in the state (the Denver metro area and Colorado Springs), much of this "urban" forest experiences heavy recreational use. In recent years, overall recreation use levels have increased in line with the population growth of the Colorado Front Range urban corridor. The US Census Bureau estimates the populations of Colorado, the Denver metro area, and the city of Colorado Springs grew by eight to ten percent in the five years between 2011 and 2016 (US Census Bureau, 2019). The combined population of the Denver metro area and Colorado Springs, both areas within a one-hour drive of the Pike National Forest, are estimated to have grown from over 3,263,400 in 2011 to over 3,570,500 in 2016 (ibid). The USDA Forest Service National Visitor Use Monitoring program estimates that annual visitation to the Pike and San Isabel National Forests (the smallest unit of measure available) increased five percent in the same period, from 4,281,000 site visits per year in 2011 to 4,502,000 site visits per year in 2016 (the last year data is available) (USDA Forest Service 2011, 2016). -
September 2015 Newsletter
September 2015 The Clotting Connection Volume 5, Issue 5 A Newsletter for Families with Bleeding and Clotting Disorders Affiliated with Children’s Hospital Colorado and University of Colorado Hospital Take in the Colors Photo: South of Fairplay by Merilee Ashton INSIDE THIS ISSUE Fall Colors NHF Annual Meeting Update Factor Packing Slips Outreach Clinics Photo: Maroon Bells by Ali Schomerus Events Autumn is upon us and it’s a great time to plan a hike, walk, or drive to see the fall News colors. Hiking and walking can be low impact and the movement is good for joints and muscles. Our NHF Chapter in Colorado regularly hosts hikes to inspire and challenge through their Backpacks and Bleeders program. We’re lucky to live in a region where there are many opportunities to see this colorful change of season in all its glory. Whether it’s a walk in your neighborhood or a road trip to take in the views, grab your shoes and sunscreen and enjoy the colors before they fade. We asked around at the HTC and came up with a list of our favorite family-friendly hikes to enjoy at this lovely time of year. Be sure to check in advance for trail conditions, weather, and prepare for emergencies. Find us on Facebook, Twitter, Rocky Mountain National Park The park has been celebrating its 100th anniversary and the opportunity to see fall and our website for frequent colors and wildlife in the area are abundant. Take advantage of the 355 miles of updates on news and events. hiking trails in the park, the amazing views along Trail Ridge Road, or plan a Go to facebook.com/ picnic. -
Bibliography and Resource Guide – Park County's Cultural History
PARK COUNTY’S CULTURAL HISTORY: A BIBLIOGRAPHY AND RESOURCE GUIDE COMPILED BY THE PARK COUNTY HISTORIC PRESERVATION ADVISORY COMMISSION P.O. Box 1373; Fairplay, CO 80440. This document will list resources that can supply or lead to significant information on Park County and/or Park County people, even though some resources may have a much broader scope. Newspaper items will generally be cited only when they concern newsworthy events, or information that helps to interpret the times. Abbreviations and omission of publishers will be employed in order to save space (Abbreviated 1850-1900 dates [such as 1/1/87], will refer to the 19th Century; if there is doubt, later years will contain all 4 digits. The Denver Post, Denver Republican, Denver Times, Fairplay Flume, & Rocky Mtn. News newspapers will usually appear as DP, DR, DT, FF, & RMN. Pages & columns will appear as numbers within parentheses.). When a resource entry does not indicate its subject, a short description may be included in parentheses at the end of the entry. Users should not assume that information in the listed resources is always accurate. Indeed, Park County history has been infected with errors and myths that have become "gospel" just because they appeared in print. A thorough, careful user of the resources included here will be able to replace most error and fantasy with the facts. Also included will be a separate list of general resources with no or few direct Park County references. Still, they may help with analysis or interpretation of such things as artifacts, buildings, or historic activities and context. -
PIKE and SAN ISABEL NATIONAL FORESTS Antelope Creek (6,900 Acres)
PIKE AND SAN ISABEL NATIONAL FORESTS Antelope Creek (6,900 acres) ......................................................................................................... 3 Aspen Ridge (14,200 acres) ............................................................................................................ 4 Babcock Hole (8,900 acres) ............................................................................................................ 5 Badger Creek (12,400 acres)........................................................................................................... 7 Boreas (10,200 acres)...................................................................................................................... 8 Buffalo Peaks East (5,700 acres) .................................................................................................... 9 Buffalo Peaks South (15,300 acres) .............................................................................................. 10 Buffalo Peaks West (8,300 acres) ................................................................................................. 12 Burning Bear (19,300 acres) ......................................................................................................... 13 Chicago Ridge (5,900 acres) ......................................................................................................... 14 Chipeta (28,700 acres) .................................................................................................................. 15 Cuchara North -
Ozone in Remote Areas of the Southern Rocky Mountains
Atmospheric Environment 82 (2014) 383e390 Contents lists available at ScienceDirect Atmospheric Environment journal homepage: www.elsevier.com/locate/atmosenv Ozone in remote areas of the Southern Rocky Mountains Robert C. Musselman*, John L. Korfmacher US Forest Service, Rocky Mountain Research Station, 240 West Prospect Road, Fort Collins, CO 80526, USA highlights O3 concentrations would contribute to NAAQS exceedances at most sites. Mid-level O3 concentrations contributed to the high values of the W126 metric. There were significant year-to-year O3 differences. O3 was persistent at night, particularly at higher elevations. O3 levels at high elevation sites suggested evidence of stratospheric intrusion. article info abstract Article history: Ozone (O3) data are sparse for remote, non-urban mountain areas of the western U.S. Ozone was Received 17 June 2013 monitored 2007e2011 at high elevation sites in national forests in Colorado and northeastern Utah using Received in revised form a portable battery-powered O3 monitor. The data suggest that many of these remote locations already 21 October 2013 have O concentrations that would contribute to exceedance of the current National Ambient Air Quality Accepted 24 October 2013 3 Standard (NAAQS) for O3 and most could exceed a proposed more stringent secondary standard. There were significant year-to-year differences in O3 concentration. Ozone was primarily in the mid- Keywords: concentration range, rarely exceeding 100 ppb or dropping below 30 ppb. The small diel changes in Air pollution Forests concentration indicate mixing ratios of NOx, VOCs, and O3 that favor stable O3 concentrations. The large High elevation number of mid-level O3 concentrations contributed to high W126 O3 values, the metric proposed as a NAAQS possible new secondary standard. -
Trail Listing
Trail Listing Trail Listing South Park Ranger District 320 US Highway 285, PO Box 219, Fairplay, CO 80440 719-836-2031 Website: www.fs.fed.us/r2/psicc/sopa Trail Name and Number Distance Difficulty Use USGS Maps Elevation Access Observ. Rock Moderate- Hiking 1. 1. Hwy 285 near Shawnee Ben Tyler #606 11.4 Mi. Mt. Logan 9,500-13,000 Difficult Horse Riding 2. 2. Lost Park Rd (CR 56) at Rock Creek TH Shawnee McCurdy Mtn 1. Twin Eagles TH off Tarryall Rd Moderate- Hiking Farnum Peak 2. Lost Park CG off Lost Park Rd (CR 56) Brookside-McCurdy #607 32.6 Mi. 8,500-11,880 Difficult Horse Riding Topaz Mtn via Wigwam Trail Shawnee 3. CR 64 W of Bailey 1. CR 56 to FSR 817 to Long Gulch TH Colorado Trail #1776 Hiking Topaz Mtn 7.8 Mi. Moderate 10,000-11,000 2. CR 56 to FSR 134 to North Fork TH Segment 4 Horse Riding Windy Peak 3. CR 56 to Brookside-McCurdy TH Topaz Mtn 1. At the top of Kenosha Pass Colorado Trail #1776 Hiking Observ. Rock 14 Mi. Moderate 9,000-11,000 2. CR 56 to FSR 133 to Rock Creek TH Segment 5 Horse Riding Mt. Logan 3. CR 56 to FSR 817 to Long Gulch TH Jefferson Hiking 1. At the top of Kenosha Pass Colorado Trail #1776 Jefferson 11 Mi. Moderate Horse Riding 9,900-11,600 2. Jefferson Lake Recreation Area at Beaver Segment 6 Boreas Pass Mtn Biking Ponds Picnic Ground 5.9 Mi.- Trail-Easy Mt. -
Colorado Are Being Studied to Determine If They Should Be Recommended for Addition to the the STUDY AREA National Wild and Scenic Rivers System (National System)
Chapter 1 Purpose Of and Need for Action CHAPTER 1 Purpose of and Need for Action 1.1 INTRODUCTION If any portions of the study rivers were found eligible and suitable, a recommendation for SELECTION designation would be forwarded to Congress, along with this document. Congress then The eligibility and suitability of 99.5 miles of the would determine if the recommended river(s) or North Fork of the South Platte River and river segment(s) should be added to the segments of the South Platte River mainstem in National System. Colorado are being studied to determine if they should be recommended for addition to the THE STUDY AREA National Wild and Scenic Rivers System (National System). All of the South Platte River The river segments identified for study total study corridor and most of the North Fork 99.5 miles and are located in Douglas, Jefferson, study corridor lie within the boundaries of the Park, and Teller Counties, in Colorado. The Pike National Forest (National Forest). Both study river corridors are mostly National Forest areas, however, include many private and local System lands administered by the Pike and government inholdings, and a 6.6-mile stretch San Isabel National Forests, Comanche and along the North Fork lies just outside the Cimarron National Grasslands, but also include National Forest boundary. This section is private inholdings and lands managed by mostly in private ownership but includes some Denver Water and Jefferson County. public lands managed by the Denver Board of Water Commissioners (Denver Water) and Jefferson -
Southern Rockies Lynx Linkage Areas
Southern Rockies Lynx Amendment Appendix D - Southern Rockies Lynx Linkage Areas The goal of linkage areas is to ensure population viability through population connectivity. Linkage areas are areas of movement opportunities. They exist on the landscape and can be maintained or lost by management activities or developments. They are not “corridors” which imply only travel routes, they are broad areas of habitat where animals can find food, shelter and security. The LCAS defines Linkage areas as: “Habitat that provides landscape connectivity between blocks of habitat. Linkage areas occur both within and between geographic areas, where blocks of lynx habitat are separated by intervening areas of non-habitat such as basins, valleys, agricultural lands, or where lynx habitat naturally narrows between blocks. Connectivity provided by linkage areas can be degraded or severed by human infrastructure such as high-use highways, subdivisions or other developments. (LCAS Revised definition, Oct. 2001). Alpine tundra, open valleys, shrubland communities and dry southern and western exposures naturally fragment lynx habitat within the subalpine and montane forests of the Southern Rocky Mountains. Because of the southerly latitude, spruce-fir, lodgepole pine, and mixed aspen-conifer forests constituting lynx habitat are typically found in elevational bands along the flanks of mountain ranges, or on the summits of broad, high plateaus. In those circumstances where large landforms are more isolated, they still typically occur within 40 km (24 miles) of other suitable habitat (Ruggerio et al. 2000). This distribution maintains the potential for lynx movement from one patch to another through non-forest environments. Because of the fragmented nature of the landscape, there are inherently important natural topographic features and vegetation communities that link these fragmented forested landscapes of primary habitat together, providing for dispersal movements and interchange among individuals and subpopulations of lynx occupying these forested landscapes.