Strategic Master Plan Update and Much Has Changed
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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. -
South Summit ACP FINAL Report.Pdf
CO 9 SOUTH SUMMIT ACCESS STUDY SUMMIT COUNTY LINE (MP 77.49) TO BOREAS PASS RD (MP 86.26) DEC 2020 South Summit Colorado State Highway 9 Access and Conceptual Trail Design Study SOUTH SUMMIT COLORADO STATE HIGHWAY 9 ACCESS AND CONCEPTUAL TRAIL DESIGN STUDY CO-9: M.P. 77.49 (Carroll Lane) to M.P. 86.26 (Broken Lance Drive/Boreas Pass Road) CDOT Project Code 22621 December 2020 Prepared for: Summit County 208 Lincoln Avenue Breckenridge, CO 80424 Bentley Henderson, Assistant Manager Town of Blue River 0110 Whispering Pines Circle Blue River, CO 80424 Michelle Eddy, Town Manager Town of Breckenridge 150 Ski Hill Road Breckenridge, CO 80424 Rick Holman, Town Manager Colorado Department of Transportation Region 3 – Traffic and Safety 222 South 6th Street, Room 100 Grand Junction, Colorado 81501 Brian Killian, Permit Unit Manager Prepared by: Stolfus & Associates, Inc. 5690 DTC Boulevard, Suite 330W Greenwood Village, Colorado 80111 Michelle Hansen, P.E., Project Manager SAI Reference No. 1000.005.10, 4000.031, 4000.035, 4000.036 Stolfus & Associates, Inc. South Summit Colorado State Highway 9 Access and Conceptual Trail Design Study TABLE OF CONTENTS Executive Summary ....................................................................................................... i 1.0 Introduction ......................................................................................................... 1 1.1 Study Background ............................................................................................. 1 1.2 Study Coordination .......................................................................................... -
Central Front Range Colorado What's Important to YOU?
CentralSan Luis Valley Front Colorado Range Colorado What’sWhat’s ImportantImportant to to YOU? YOU? PleasePlease select select your your county: county: Alamosa □Custer Chaffee □El Paso Conejoe □Fremont Costilla □Park Mineral□Teller Rio Grande Saguache TheThe Colorado Colorado Department Department of of Transportation Transportation wantswants to to know know what’swhat’s important important to to you. you. Please completePlease this complete survey beforethis survey December before 15, December 2013, fold, 15, and2013, mail fold, it backand mailto the it backaddress to the printed address at the printed at the bottom of bottomthe survey of theor yousurvey can ortake you the can survey take theat www.coloradotransportationmatters.com.survey at www.coloradotransportationmatters.com . Watch for resultsWatch on for that results website on that website. YourYour input input is is important important – it will— helpit will shape help the shape Statewide the Transportation Statewide Transportation Plan Plan. Fold oneFold one 3. What do you feel makes the Central Front Range 1. Why is transportation important to you? 1. Why is transportation important to you? 3. regionWhat do unique? you feel makes the San Luis Valley unique? ? PlacePlace an anX in X the in thebox boxbeside beside your topyour two top two: Place an X in the box beside your top three Select your top three: Moves Moves people peopleand goods and safely goods safely Urban amenities Urban amenities Supports Supports existing existing businesses businesses Rural living with nearby city amenities Helps economic development Innovation Rural and living creativity with nearby city amenities Helps economic development Gets me to work and/or vital services Agriculture Innovation and creativity Gets me to work and/or vital services Helps me live my life the way I want Freight/shipping Agriculture industry Helps me live my life the way I want Sense of community PLEASE Freight/shipping industry 2. -
Generalized Surficial Geologic Map of the Denver 1° × 2° Quadrangle, Colorado
U.S. DEPARTMENT OF THE INTERIOR MISCELLANEOUS FIELD STUDIES MAP MF–2347 U.S. GEOLOGICAL SURVEY Version 1.0 PAMPHLET GENERALIZED SURFICIAL GEOLOGIC MAP OF THE DENVER 1° × 2° QUADRANGLE, COLORADO Compiled by David W. Moore, Arthur W. Straub, Margaret E. Berry, Michael L. Baker, and Theodore R. Brandt 2001 CONTENT AND PURPOSE rock landslide deposit” and “stabilized dune sand.” Large areas (generally >1 km2; >0.4 mi2) of exposed This map locates surficial geologic deposits of bedrock, mostly devoid of surficial materials, are Quaternary age in the greater Denver area and mapped with a symbol “R.” surrounding region. Physical properties of the deposits are described. The physical properties PARTICLE SIZE AND COLOR include dominant grain size, composition, potential to expand upon sorption of water, and others. Origins TERMINOLOGY and ages of the deposits, and their inherent geologic hazards are identified. The properties of deposits and We used geological and soil textural terms to materials on and near the land surface affect its describe the size of particles in the surficial deposits. suitability for societal uses. Examples of such use Particle sizes ranged from microns to meters in include large-scale landfill sites, gravel pits and rock diameter. The combined use of geologic and soil quarries, large-scale residential developments, terminology resulted from a necessity to consult greenbelts, utility lines, and roads. Planners, zoning various data sources to characterize the materials. officials, builders, and interested citizens should have Clasts are particles larger than 2 mm in diameter. We a clear grasp of how the properties of surficial used geologic terms to describe clasts. -
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. -
Eleven-Mile Canyon Demonstration Project
Case Study 4 The Eleven-mile Canyon Demonstration Project Project Overview The Eleven-mile Canyon Demonstration Project is located on the South Platte River in Park County, Colorado (figure 1). This project area is located in a semiarid (less than 15 inches of precipitation per year) portion of the foothills zone of the Rocky Mountains (Pennak 1977). The bedrock underlying this canyon area is comprised primarily of biotite granite that produces highly erodible, unproductive soils. This condition also results in sparse ground cover, contributing to the area’s erosive nature. The landscape is bisected by relatively steep, narrow drainages with abundant erosional stream channels. Figure 1: Vicinity map of Eleven-mile Canyon. Study reaches are identified by reach numbers. (The inset map identifies the location of the canyon within the Pike National Forest.) In the late 1800s a railroad was built in the Eleven-mile Canyon, further narrowing the Eleven-mile Canyon floor. Large native trees were removed Eleven-mile Canyon Demonstration Project from the valley floor for use in the nearby metropolitan areas. In the early 1900s the city of Denver began building reservoirs and associated conduits for water storage in the South Platte River corridor, for use by the increasing population. The releases from these reservoirs have created a hydrograph considerably different than what would be expected under historic conditions (figure 2). The removal of trees, location and maintenance of the road corridor, and modified flow releases from upstream reservoirs has created a stream system considerably altered from pre-European settler conditions. 3—43 Developing Monitoring Plans— Chapter 3 Figure 2: Comparison of a hydrograph from a regulated section of the South Platte River downstream of Eleven-mile Canyon to a more natural flow regime in Tarryall Creek, a tributary to the South Platte River. -
Collbran at a Glance
DRAFT DOCUMENT I. Acknowledgments The Town of Fairplay Comprehensive Plan would not have been possible without the substantial time generously donated by the Comprehensive Plan Steering Committee, town of Fairplay staff and the public. The long-term challenge is to maintain Plan ownership as Town Trustees and staff transition and to ensure that plan information is retained and communicated to future decision-makers and residents. A successful plan will include regular use, application of the vision and implementation of the goals and policies to land use decisions. The following participants are individually recognized for their contributions to this planning process. Maria Sims Board of Trustees Pat Poius Mayor - Fred Boyce Tommy DeBonis Mayor Pro-tem - Frank Just Trevor Messa Trustee - John Deagan Town Staff Trustee - LaNita French Town Administrator/Clerk - Tina Darrah Trustee - Gabby Lane Deputy Clerk - Claudia Werner Steering Committee Treasurer - Kim Wittbrodt Michael Simpson - Chair Police Chief - Dave Gottschalk Bill Davis Park County Staff Carmen Johnson Planning Director - John Deagan Charlie Schultz GIS - Kat Hererra Dale Fitting Greg Johnson Comprehensive Plan Consultants Jim Carpenter Western Slope Consulting, LLC Stephanie Carpenter RRC Associates Julie Bullock Lamont Planning Services Linda Balough Sopris Land-Use, LLC Page - 1 DRAFT DOCUMENT Community Vision Statement Town of Fairplay. Steering Committee Version Fairplay – The place we choose to live We are a self-sufficient, resilient and strong willed historic mining town in the heart of Colorado with a passionate sense of community and a connection to the mountains and surrounding beauty. We cultivate our entrepreneurial spirit and embrace tourism, economic growth and prosperity to create an attractive and vibrant community for residents and visitors. -
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 -
TOWN of BRECKENRIDGE OPEN SPACE ADVISORY COMMISSION Monday, February 11, 2008 BRECKENRIDGE COUNCIL CHAMBERS 150 Ski Hill Road
TOWN OF BRECKENRIDGE OPEN SPACE ADVISORY COMMISSION Monday, February 11, 2008 BRECKENRIDGE COUNCIL CHAMBERS 150 Ski Hill Road 5:30 Call to Order, Roll Call 5:35 Discussion/approval of Minutes – January 14th 5:40 Discussion/approval of Agenda 5:45 Public Comment (Non-Agenda Items) 5:50 Staff Summary • Peak 6 Expansion Scoping letter • Cucumber Gulch Preserve signage 6:00 Open Space and Trails • Nature Series update • Trails Plan revision • 2008 Work Plan 8:15 Commissioner Issues 8:20 Adjourn For further information, please contact the Open Space and Trails Program at 547.3110 (Heide) or 547.3155 (Scott). Memorandum To: Breckenridge Open Space Advisory Commission From: Heide Andersen, Open Space and Trails Planner III Mark Truckey, Asst. Director of Community Development Scott Reid, Open Space and Trails Planner II Re: February 11, 2008 meeting Staff Summary Peak 6 Expansion Scoping letter At Council’s direction, staff drafted a Peak 6 expansion scoping letter to identify questions and issues of concern that the Town would like to be addressed in the U.S. Forest Service Environmental Impact Statement for the proposed expansion. The draft letter and memo are attached for BOSAC’s review, although this topic will be discussed at the 2/12 Council meeting, rather than the BOSAC meeting. Cucumber Gulch Preserve signage Staff has hired Erin McGinnis of McGraphix to review and design the sign family for the Cucumber Gulch Preserve. We anticipate receiving design work and sample materials from Erin in the coming weeks and may need to schedule a second BOSAC meeting in February (on 2/24) to review Erin’s work. -
Trails Plan | 2009 Town of Breckenridge | Trails Plan
TOWN OF BRECKENRIDGE | TRAILS PLAN | 2009 TOWN OF BRECKENRIDGE | TRAILS PLAN TOWN OF BRECKENRIDGE TRAILS PLAN Introduction 4 Plan Philosophy 4 Plan Prioritization 5 Plan Goals and Objectives 5 Role of the Plan 5 Plan Assumptions 6 Plan Implementation 6 Plan Organization 6 How This PlanW as Developed 6 Winter and Summer Elements 7 Disclaimer 7 Planning Areas 7 Area 1: Ski Hill Road/Peak 7/8 Base Area 7 Peaks Trailhead and Trails 7 Freeride Park 8 Shock Hill/Nordic Center 8 Cucumber Gulch Preserve 9 Claimjumper/Recreation Center Connection 9 Peak 7 Neighborhood Connection 10 New Nordic World/Peak 6 Expansion 10 Iowa Hill Trailhead 10 American Way Access 10 Area 2: Core/Upper Four Seasons Area 11 Riverwalk Connection 11 Klack Placer 11 The Cedars/Trails End Connection 11 F&D Placer to Burro Connection 12 Maggie Pond Access 12 Four O’Clock Ski Run 12 Timber Trail 12 Maggie Placer Trail 13 Area 3: Breckenridge South 13 Aspen Grove/Aspen Alley Trail 13 Wakefield Trailhead 13 Little Mountain 13 Blue River/Hoosier Pass Recpath 14 The Burro Trail Accesses 14 Bekkedal/Gold King (lots 1&2) to Burro Connection 14 Ski Area Equestrian Trails 14 Now Colorado/Silver Queen Connection 15 Riverwood Trail 15 PAGE 1 TRAILS PLAN | TOWN OF BRECKENRIDGE TOWN OF BRECKENRIDGE | TRAILS PLAN Area 3: Breckenridge South (continued) Breckenridge Park Estates Trailhead 15 Fredonia Gulch Trailhead 16 Bemrose Ski Circus 16 Wheeler Trail Resurrection 16 Pennsylvania Gulch and Indiana Creek Road Winter Access 16 Spruce Creek Trail Spur 16 Lehman Gulch Trail 17 Monte Cristo -
History of the Baker/Steiner Barn
3. Historical Background Please provide historical background information for the property. The Baker/Steiner Barn, constructed circa 1885, is one of the largest surviving and best preserved nineteenth-century log hay barns in the northern South Park. Connected with the Bakers and Schattingers, early pioneer families that played an important role in the historical development of ranching in the South Park, the barn is a highly visible reminder of the significant impact these families had on the area and the important role ranching, and more specifically hay production, played in the development of the Jefferson area. Early on, American Indians recognized the nutritious nature of the native grasses that sustained the large herds of game that roamed the South Park. In the 1840s, Anglo visitors such as Rufus B. Sage observed the healthy herds of bison, elk, deer, and antelope found throughout the park and identified the area as ideal for stockraising.1 However, the harsh climate conditions and remote location of the park discouraged Colorado’s earliest ranchers from settling in Park County. The discovery of gold along Tarryall Creek in 1859 made ranching in the South Park a far more attractive proposition. The gold strike at Tarryall brought hundreds of prospectors to the South Park. Seemingly overnight, large mining camps sprang up at Hamilton, Fairplay, Buckskin Joe, and other sites where gold had been found. The prospectors that flooded these rapidly growing communities needed food, creating a demand that encouraged the establishment of large cattle ranching operations in the wide open expanse of the South Park. Enterprising ranchers claimed land near reliable water sources and natural hay meadows, established their homesteads, and began raising cattle and growing hay.2 The success of these ventures attracted a growing number of settlers like David Baker and his wife Emily Vance to the South Park.