National Register of Historic Places Inventory
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Trait Ridge Road Guide
Sign No. 9 Medicine Bow Curve (11,640 feet) succeeded more than 80 years ago in bringing water from Never The sign here points northwest to the Medi Summer streams through the Grand Ditch and La Poudre Pass Rocky Mountain National Park cine Bow Mountains which extend into Wyo to irrigate the semiarid lands east of the Rockies. He failed to 9 ming, 44 miles away. The Cache la Poudre find sufficient precious metals in Lulu City diggings to establish River twists through the glacial gorge before profitable mines. Broken stone chimneys and rotting founda you, separating this point from rounded, tion logs are all that remain of this once bustling mining camp. v 7 This country is also a favorite home of the beaver. Trait Ridge brownish Specimen Mountain to the west. Its color provides a clue to the mountain's orgin, Sign No. 12 Shadow Mountain National as a volcano, and the cliffs at Iceberg Lake Recreation Area are of lava from this source. Shadow Mountain Lake and Lake Granby Road Guide Sign No. 10 Continental Divide, Milner Pass are two reservoirs of the Colorado — Big (10,758 feet) 12 Thompson Project, built and operated by the Bureau of Reclamation, U.S. Department of Surprise! You thought the Continental Divide \ 7 the Interior. From here water flows through would be the highest point on your trip. But Grand Lake and the 13.1-mile Adams Tunnel this delightful spot where an undecided rain to Estes Park. There, east of the Continental drop might flow either to the Atlantic or to \10/ Divide, it stairsteps down through penstocks the Pacific is more than a thousand feet below and turbines producing electric power and finally emptying into the Alpine Visitor Center, and 1,425 feet be- reservoirs and irrigation canals east of the Front Range. -
Stanley Hotel: Tourism and Building in the West 2
1.Title / Content Area: Stanley Hotel: Tourism and Building in the West 2. Historic Site: Stanley Hotel 3. Episode: https://www.pbs.org/video/colorado-experience-stanley-hotel/ 3. Developed by: Laura Israelsen, Denver Public Schools Michelle Pearson, Adams 12 Five Star Schools 4. Grade Level and 6-8: Standards: 6th: History 1.1, 1.2, Geography 2.1, 2.2 7th: History 1.1, 1.2, Geography 2.1, 2.2, Civics 4.1 8th: History 1.1, 1.2, Geography 2.1 5. Assessment Why does the Stanley hotel play an iconic role in the landscape of upper Estes Park Question(s): and the region as a whole? 6. Contextual Paragraph F.O. Stanley was an inventor and a visionary for his time. After coming to Colorado because of health reasons, he not only established and built the iconic Stanley Hotel, but was responsible for the development of the site of Estes Park as well through his involvement in the development of the road systems, financing the water system, and launching a major advertising campaign to bring tourists to the city via motor coaches which traveled through the canyon from Estes Park. Known as a resort hotel, the Stanley was a “draw” to tourists from across the nation who were looking for a comfortable and luxurious way to travel in the Colorado Rockies at the turn of the century. The hotel has been a host to contemporary travelers and moviemakers and is known today as the setting for the movie based on Stephen King's novel The Shining. -
The Stanley Hotel History
The Stanley Hotel History: The property of the Stanley hotel was a favorite of Mr. Windham Thomas Whydham‐Quin the fourth Earl of Dunraven. He would come to the area for his summer hunting. “Lord Dunraven” wanted to put a Hunting lodge and game preserve. Wyndham Thomas Quinn the 4th Earl of Dunraven Dunraven hired some local Agents and purchased 15,000 acres from the U.S. Government. Soon after the purchase there were claims filed by twenty‐one different parties including Mr. R.Q. McGregor. They all claimed that Dunraven had no right to the land because he was not a U.S. citizen. Mr. Dunraven lost the property due to the claims of Mr. McGregor. F.O. Stanley A local who wanted to purchase the land for himself had hired R.Q. McGregor. This was Mr. Freelan Oscar Stanley. Freelan Oscar (F.O.) Stanley was born in 1849; he was diagnosed with tuberculosis in 1903 and was told to move to Colorado because the “fresh mountain air” would help his condition. Mr. Stanley and his wife moved to a home located at 1401 Gilpin St in Denver. After a month in Denver, he was showing no signs of change. Arrangements were made for him to visit a friend’s cabin in Estes Park. Mr. & Mrs. Stanley fell in love with the area and in 1904 purchased 8.4 acres of their own. F.O. Stanley’s sister Flora Jane Record Tileston, who would become Mrs. Stanley (1848‐1949) was an active member of the community, she was known for dressing up as a Gypsy and doing fortune telling at fundraisers for the Estes Park Women’s Club They purchased the property with the assistance of Mr. -
Hiking in the Kawuneeche Valley Rocky Mountain
National Park Rocky Mountain National Park Service Hiking in the Kawuneeche Valley Adams Falls (East Inlet Trailhead) This easy 1/3 mile hike leads to a small, pleasant waterfall. If you wish to go further, past the falls, you will come to a large, grassy, glaciated valley with a river running through it. Moose are sometimes sighted in this valley. Many types of wildflowers are found in this area. (79’gain) Cascade Falls (North Inlet Trailhead) Photogenic Cascade Falls is 3.4 miles into the North Inlet trail. This easy hike passes through an open meadow where marmots are often found, and by a river that winds through a lodgepole pine forest. Fishing is good for small brook trout and an occasional brown trout. Allow about 3-4 hours for hiking this trail. (300’gain) Lulu City (Colorado River Trailhead) A flowered field is all that remains of this once booming mining town. Pass by the remains of log cabins and look for tailings from Shipler Mine about 2 miles into the trail. The trail parallels the Colorado River and passes meadows on this easy to moderately difficult 7.4-mile round trip hike. (350’gain) Lulu City/Yellowstone Loop (Colorado River Trailhead) After passing Shipler’s cabins, you will come to a sign that will designate Lulu City to the left and Little Yellowstone to the right. Stay right at the Y. Follow the trail all the way to the Grand Ditch. Little Yellowstone is a miniature version of the Grand Canyon of Yellowstone, formed of stark gray volcanic rock. -
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. -
National Register of Historic Places Registration Form
NPS Form 10-900 OMB No. 10024-0018 United States Department of the Interior National Park Service National Register of Historic Places Registration Form This form is for use in nominating or requesting determination for individual properties and districts. See instruction in How to Complete the National Register of Historic Places Registration Form (National Register Bulletin 16A). Complete each item by marking ``x'' in the appropriate box or by entering the information requested. If an item does not apply to the property being documented, enter ``N/A'' for ``not applicable.'' For functions, architectural classification, materials and areas of significance, enter only categories and subcategories from the instructions. Place additional entries and narrative items on continuation sheets (NPS Form 10-900a). Use a typewriter, word processor, or computer, to complete all items. 1. Name of Property historic name East Longs Peak Trail; Longs Peak Trail; Keyhole Route; Shelf Trail other names/site number 5LR.11413; 5BL.10344 2. Location street & number West of State Highway 7 (ROMO) [N/A] not for publication city or town Allenspark [X] vicinity state Colorado code CO county Larimer; Boulder code 069; 013 zip code 3. State/Federal Agency Certification As the designated authority under the National Historic Preservation Act, as amended, I hereby certify that this [X] nomination [ ] request for determination of eligibility meets the documentation standards for registering properties in the National Register of Historic Places and meets the procedural and professional requirements set forth in 36 CFR Part 60. In my opinion, the property [ ] meets [ ] does not meet the National Register criteria. I recommend that this property be considered significant [ ] nationally [ ] statewide [X] locally. -
Appendix C Table 1, Camp Area Summary
Backcountry/Wilderness Management Plan and Environmental Assessment Appendix C Appendix C Table 1, Camp Area Summary Designated Areas/Sites Individual Camp Areas Campsites People East Side 60 109 763 West Side 59 88 616 Total 119 197 1379 Group Camp Areas Campsites People East Side 10 10 120 West Side 11 11 132 Total 21 21 252 Accessible Camp Areas Campsites People East Side 1 1 12 West Side 0 0 0 Total 1 1 12 Wood Fire Camp Areas Campsites East Side 8 13 West Side 9 13 Total 17 26 Stock Areas/Sites Individual Camp Areas Campsites People Stock East Side 3 3 18 24 West Side 3 3 18 24 Total 6 6 36 48 Group Camp Areas Campsites People Stock East Side 2 2 24 32 West Side 2 2 24 32 Total 4 4 48 64 Llama only Camp Areas Campsites People Stock East Side 2 2 14 10 West Side1175 Total 3 3 21 15 Wood Fire Camp Areas Campsites East Side 8 13 West Side 9 13 Total 17 26 Rocky Mountain National Park C-1 Backcountry/Wilderness Management Plan and Environmental Assessment Appendix C Crosscountry Areas Areas Parties People East Side 9 16 112 West Side 14 32 224 Total 23 48 336 Summer Totals for Designated, Stock and Crosscountry Areas Camp Areas Campsites/Parties People East Side 80 136 1004 West Side 84 131 969 Total 164 267 1973 Bivouac Areas Areas People East Side 11 88 West Side 0 0 Total 11 88 Winter Areas Areas Parties People East Side 32 136 1632 West Side 23 71 852 Total 55 207 2484 Rocky Mountain National Park C-2 Backcountry/Wilderness Management Plan and Environmental Assessment Appendix C Appendix C Table 2, Designated Camp Area/Sites Number -
Front Range Floods Teach Guide
National Park Service Rocky Mountain U.S. Department of Interior Rocky Mountain National Park Front Range Floods Teacher Guide Table of Contents Rocky Mountain National Park.................................................................................................1 Teacher Guides..............................................................................................................................2 Rocky Mountain National Park Education Program Goals...................................................2 Schedule an Education Program with a Ranger.......................................................................2 Front Range Floods Introduction........................................................................................................................4 Precipitation Patterns Along The Front Range..............................................................5 Colorado Flood Events.....................................................................................................6 Flooding in Rocky Mountain National Park...............................................................12 History of Floodplain Management in the United States..........................................14 Front Range Floods Resources Glossary.............................................................................................................................20 References.........................................................................................................................22 Rocky Mountain National Park Rocky Mountain -
A Natural Resource Condition Assessment for Rocky Mountain National Park
National Park Service U.S. Department of the Interior Natural Resource Program Center A Natural Resource Condition Assessment for Rocky Mountain National Park Natural Resource Report NPS/NRPC/WRD/NRR—2010/228 ON THE COVER Rocky Mountain National Park Photograph by: Billy Schweiger A Natural Resource Condition Assessment for Rocky Mountain National Park Natural Resource Report NPS/NRPC/WRD/NRR—2010/228 David M. Theobald1,2 Jill S. Baron2,3 Peter Newman1 Barry Noon4 John B. Norman III1,2 Ian Leinwand1 Sophia E. Linn1 Richard Sherer4 Katherine E. Williams2,5 Melannie Hartman2 1Department of Human Dimensions of Natural Resources, Colorado State University, Fort Collins, CO 80523-1480 2Natural Resource Ecology Lab, Colorado State University, Fort Collins, CO 80523-1499 3U.S. Geological Survey, Fort Collins, CO 80523 4Department of Fish, Wildlife, and Conservation Biology, Colorado State University, Fort Collins, CO 80523-1474 5Current address: Department of Biology, University of Wyoming, Laramie, WY 82071 This report was prepared under Task Order J2380060103 (Cooperative Agreement #H1200040001) July 2010 U.S. Department of the Interior National Park Service Natural Resource Program Center Fort Collins, Colorado The Natural Resource Publication series addresses natural resource topics that are of interest and applicability to a broad readership in the National Park Service and to others in the management of natural resources, including the scientific community, the public, and the NPS conservation and environmental constituencies. Manuscripts are peer-reviewed to ensure that the information is scientifically credible, technically accurate, appropriately written for the intended audience, and is designed and published in a professional manner. Natural Resource Reports are the designated medium for disseminating high priority, current natural resource management information with managerial application. -
Download This
NPS Form 10-900 —. OMB No. 10024-0018 United States Department of the Interior National Park Service National Register of Historic Places Registration Form This form is for use in nominating or requesting determination for individual properti.es aTfa^IslftcTST6ee<iie^truction in How to Complete the National Register of Historic Places Registration Form (National Register Bulletin 16A). Complete each item by marking "x" in the appropriate box or by entering the information requested. If an Item does not apply to the property being documented, enter' N/A for "not applicable." For functions, architectural classification, materials and areas of significance, enter only categories and subcategories from the instructions. Place additional entries and narrative items on continuation sheets (NPS Form 10-900a). Use a typewriter, word processor, or computer, to complete all items. 1. Name of Property__________________________________________ historic name East Longs Peak Trail: Longs Peak Trail: Keyhole Route: Shelf Trail________ other names/site number 5LR.11413: 5BL.10344___________________________ 2. Location_______________________________________________ street & number West of State Highway 7 (ROMO)______________ [N/A] not for publication city or town Allenspark_________________________________ [X] vicinity state Colorado___ code CO county Larimer; Boulder code 069: 013 zip code 3. State/Federal Agency Certification __ As the designated authority under the National Historic Preservation Act, as amended, I hereby certify that this [X] nomination [ ] request for determination of eligibility meets the documentation standards for registering properties in the National Register of Historic Places and meets the procedural and professional requirements set forth in 36 CFR Part 60. In my opinion, the property [ ] meets [ ] does not meet the National Register criteria. -
Rocky Mountain National Park Lawn Lake Flood Interpretive Area (Elevation 8,640 Ft)
1 NCSS Conference 2001 Field Tour -- Colorado Rocky Mountains Wednesday, June 27, 2001 7:00 AM Depart Ft. Collins Marriott 8:30 Arrive Rocky Mountain National Park Lawn Lake Flood Interpretive Area (elevation 8,640 ft) 8:45 "Soil Survey of Rocky Mountain National Park" - Lee Neve, Soil Survey Project Leader, Natural Resources Conservation Service 9:00 "Correlation and Classification of the Soils" - Thomas Hahn, Soil Data Quality Specialist, MLRA Office 6, Natural Resources Conservation Service 9:15-9:30 "Interpretive Story of the Lawn Lake Flood" - Rocky Mountain National Park Interpretive Staff, National Park Service 10:00 Depart 10:45 Arrive Alpine Visitors Center (elevation 11,796 ft) 11:00 "Research Needs in the National Parks" - Pete Biggam, Soil Scientist, National Park Service 11:05 "Pedology and Biogeochemistry Research in Rocky Mountain National Park" - Dr. Eugene Kelly, Colorado State University 11:25 - 11:40 "Soil Features and Geologic Processes in the Alpine Tundra"- Mike Petersen and Tim Wheeler, Soil Scientists, Natural Resources Conservation Service Box Lunch 12:30 PM Depart 1:00 Arrive Many Parks Curve Interpretive Area (elevation 9,620 ft.) View of Valleys and Glacial Moraines, Photo Opportunity 1:30 Depart 3:00 Arrive Bobcat Gulch Fire Area, Arapaho-Roosevelt National Forest 3:10 "Fire History and Burned Area Emergency Rehabilitation Efforts" - Carl Chambers, U. S. Forest Service 3:40 "Involvement and Interaction With the Private Sector"- Todd Boldt; District Conservationist, Natural Resources Conservation Service 4:10 "Current Research on the Fire" - Colorado State University 4:45 Depart 6:00 Arrive Ft. Collins Marriott 2 3 Navigator’s Narrative Tim Wheeler Between the Fall River Visitors Center and the Lawn Lake Alluvial Debris Fan: This Park, or open grassy area, is called Horseshoe Park and is the tail end of the Park’s largest valley glacier. -
50 Years Celebrating Earth, Atmosphere, Astronomy, and Oceans: Stories of a Great Department
University of Northern Colorado Scholarship & Creative Works @ Digital UNC Earth & Atmospheric Sciences Faculty Publications Earth & Atmospheric Sciences 2020 50 Years Celebrating Earth, Atmosphere, Astronomy, and Oceans: Stories of a Great Department William Henry Hoyt Follow this and additional works at: https://digscholarship.unco.edu/easfacpub 50 Years Celebrating Earth, Atmosphere, Astronomy, and Oceans: Stories of a great Department By William H. Hoyt, Ph. D. University of Northern Colorado Department of Earth Sciences (Earth & Atmospheric Sciences) 1970-2020 1 1956-1970s: THE FIRST YEARS, Tollefson the Magnificent The first tale I ever heard about how the Department of Earth Sciences started hearkens out of the mid-1950s. Oscar W. Tollefson, who had almost graduated from the Univ. of Colorado (Ph D in geology), found himself sitting next to Colorado State College (CSC) President Bill Ross on a commercial flight between Washington, D.C. and Denver. Tolley, as he was universally known in professional circles, was the loquacious sort and so of course he struck up a conversation with a guy who, it turns out, was an amateur rock , fossil, and mineral collector. Bill Ross came from a background in buildings and grounds and knew a lot about earth materials and weather! Though we don’t know exactly what was said in that four hours, we do know that Bill Ross recognized a rare enthusiasm for teaching and learning in the young Tolley. Ross also probably recognized that Tolley’s persuasiveness and persistence would go a long way at the growing College. The Earth Sciences academic program was founded at Colorado State College (CSC) in 1956 by Dr.