Rocky Mountain National Park
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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. -
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. -
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. -
Rocky Mountain National Park
A Resource Assessment ROCKY MOUNTAIN NATIONAL PARK NATIONAL PARKS CONSERVATION ASSOCIATION JULY 2002 State of the Parks Program More than a century ago, Congress established Yellowstone as C ONTENTS the world’s first national park. That single act was the begin- ning of a remarkable and ongoing effort to protect this nation’s natural, historical, and cultural heritage. Summary page 1 But over the years, Americans have learned that designat- I. ALPINE WONDER 4 ing national parks does not automatically ensure the well being of the resources parks are meant to protect and the his- II. ROCKY MOUNTAIN ASSESSMENT 6 tory those resources represent. Many parks are threatened by incompatible development of adjacent lands, air and water Natural Resources 7 pollution, skyrocketing visitation, and rapid increases in Native Biodiversity 7 motorized recreation. Historic structures suffer from deterio- Terrestrial Communities and Systems 9 ration. Most cultural landscapes have yet to be adequately Freshwater Communities and Systems 12 inventoried. Only a small part—usually less than 10 percent—of the Cultural Resources 14 National Park Service budget each year is earmarked for man- History and Historic Structures 14 agement of natural, historical, and cultural resources. And in Collections and Archives 16 most years, only about 7 percent of permanent park employ- Archaeological Sites 17 ees work in jobs directly related to preserving park resources. The National Parks Conservation Association initiated Ethnography 18 the State of the Parks program in 2000 to assess the condition Cultural Landscapes 19 of natural and cultural resources in the parks, forecast the like- Stewardship Capacity 20 ly future condition of those resources, and determine how well equipped the National Park Service is to protect the Funding and Staffing 20 park—its stewardship capacity. -
Little Buckaroo Ranch Barn National Register
United States Department of the Interior NATIONAL PARK SERVICE 2280 National Register of Historic Places 1201 "I" (Eye) Street, NW Washington D.C. 20005 The Director of the National Park Service is pleased to announce actions on the following properties for the National Register of Historic Places. For further information contact Edson Beall at (202) 354-2255 or E-mail: [email protected] Visit our web site at http://www.cr.nps.gov/nr WEEKLY LIST OF ACTIONS TAKEN ON PROPERTIES: 7/06/09 THROUGH 7/10/09 KEY: State, County, Property Name, Address/Boundary, City, Vicinity, Reference Number, NHL, Action, Date, Multiple Name ARIZONA, PIMA COUNTY, Agua Caliente Ranch Rural Historic Landscape, 12325 E. Roger Rd., Tucson vicinity, 04001246, LISTED, 7/09/09 (Cattle Ranching in Arizona MPS) CALIFORNIA, ORANGE COUNTY, Cogged Stone Site--CA-ORA-83, Address Restricted, Huntington Beach vicinity, 01001455, DETERMINED ELIGIBLE, 7/10/09 COLORADO, EL PASO COUNTY, North Cheyenne Canon Park, 2120 N. Cheyenne Canon Rd., Colorado Springs, 09000489, LISTED, 7/08/09 COLORADO, GRAND COUNTY, Little Buckaroo Ranch Barn, 20631 Trail Ridge Rd., Rocky Mountain National Park, Grand Lake vicinity, 09000490, LISTED, 7/08/09 GEORGIA, CHATHAM COUNTY, Eureka Club--Farr's Point, 2326 E. Blvd., Savannah vicinity, 09000491, LISTED, 7/08/09 GEORGIA, JASPER COUNTY, Pope-Talmadge House, 2560 Calvin Rd., Monticello vicinity, 09000492, LISTED, 7/08/09 ILLINOIS, COOK COUNTY, Ethnic (European) Historic Settlements of the City of Chicago, 1861-1930 MPS 64501044, COVER DOCUMENTATION ACCEPTED, 6/26/09 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. -
Ecosystem Restoration of Select Sites in the Kawuneeche Valley
Stream Management Plan Grantee Project Summary Ecosystem Restoration of Select Sites in the Kawuneeche Valley Geographic Description: Project Homepage: Colorado River Basin: northernwater.org North Fork Colorado Watershed Primary Contact: Size: Kimberly Mihelich 102 square miles Source Water Protection Specialist [email protected] Project Timeline Define Purpose Assess Conditions and Identify and Implement and and Scope Select Objectives Prioritize Actions Monitor Actions Completed December 2020- March- January 2022 December 2021 December 2021 Stakeholder Groups Involved in Current Planning Phase Planning Process: Agricultural producers Riparian landowners Aquatic and riparian science Environmental advocacy Utilities or other water management Recreation & tourism Local government & land use planners Last updated: 4/12/2021 Restoration in the Kawuneeche Valley Summary | 1 Project Goals • Assess existing geomorphic, ecological, water quality conditions, and human dimensions relating to ecological restoration in the project area, including parts of the watershed affected by the East Troublesome Fire • Complete feasibility analyses of the suitability of available restoration approaches throughout the watershed • Identify and prioritize sites where restoration should be pursued Overview Geography: The project is focused on geomorphological and ecological restoration of the riverine environment of the North Fork Colorado River (North Fork) watershed. Excessive sediment and nutrients enter Shadow Mountain Reservoir from the North Fork, and this will likely increase due to the recent East Troublesome Fire. While certain problem areas within Rocky Mountain National Park have been documented, conditions in much of the North Fork watershed are largely unknown, particularly within the burned area. Users: The Kawuneeche Valley Ecosystem Restoration Collaborative is a reactionary plan with a diverse stakeholder group representing agricultural users, municipal water use, industry, environmental and recreation stakeholders. -
Black Canyon of the Gunnison Great Sand Dunes Mesa Verde Rocky
COLORADO NATIONAL PARK TRIP PLANNER Black Canyon of the Gunnison Great Sand Dunes Mesa Verde Rocky Mountain TOP 4 ROAD TRIPS 14 Cody Dinosaurs and Deserts Thermopolis GETTING Wildlife and Natural Wonders 120 Best of Colorado Loop Idaho Land of Enchantment Falls 26 THERE Lander Dinosaur National Monument Plan your dream vacation Laramie with our top routes to Colorado’s national parks and monuments. Grand Estes Park 40 Lake Learn more at Steamboat Lyons 40 Glenwood Springs MyColoradoParks.com. Springs 133 Delta Cripple Creek Colorado National Montrose Monument Park and Preserve. For 25 BEST OF a unique wildlife 550 Great Sand Dunes COLORADO LOOP experience, drive east National Park 160 Alamosa and Preserve from Denver to Pagosa Miles 1,130 Springs Keenesburg to visit The Farmington The ultimate Colorado Wild Animal Sanctuary, road trip includes home to more than 450 550 Taos 25 Bandelier charming mountain rescued tigers, lions, National Monument towns, hot springs, wolves and bears. Santa Fe desert scenery and impressive peaks. Head straight to Rocky DINOSAURS Mountain National Park AND DESERTS from Denver and take Trail Ridge Road west Miles 1,365 to Grand Lake. Soak in Go from red-rock the pools of Hot canyons to alpine Phoenix Sulphur Springs before meadows on this loop. heading to Winter Park Abilene Start in Salt Lake City Carlsbad Caverns and Dillon. Stop in National Park and drive southeast to Glenwood Springs to Vernal, Utah, the experience the town’s Flaming Gorge National Map by Peter Sucheski legendary hot springs Recreation Area and and adventure park. Just south you’ll find with New Mexican stunning San Luis Dinosaur National Continue west to the WILDLIFE AND Grand Teton National deserts on this Valley. -
A Guide to the Geology of Rocky Mountain National Park, Colorado
A Guide to the Geology of ROCKY MOUNTAIN NATIONAL PARK COLORADO For sale by the Superintendent of Documents, Washington, D. C. Price 15 cents A Guide to the Geology of ROCKY MOUNTAIN NATIONAL PARK [ COLORADO ] By Carroll H. Wegemann Former Regional Geologist, National Park Service UNITED STATES DEPARTMENT OF THE INTERIOR HAROLD L. ICKES, Secretary NATIONAL PARK SERVICE . NEWTON B. DRURY, Director UNITED STATES GOVERNMENT PRINTING OFFICE WASHINGTON : 1944 Table of Contents PAGE INTRODUCTION in BASIC FACTS ON GEOLOGY 1 THE OLDEST ROCKS OF THE PARK 2 THE FIRST MOUNTAINS 3 The Destruction of the First Mountains 3 NATURE OF PALEOZOIC DEPOSITS INDICATES PRESENCE OF SECOND MOUNTAINS 4 THE ROCKY MOUNTAINS 4 Time and Form of the Mountain Folding 5 Erosion Followed by Regional Uplift 5 Evidences of Intermittent Uplift 8 THE GREAT ICE AGE 10 Continental Glaciers 11 Valley Glaciers 11 POINTS OF INTEREST ALONG PARK ROADS 15 ROAD LOGS 18 Thompson River Entrance to Deer Ridge Junction 18 Deer Ridge Junction to Fall River Pass via Fall River .... 20 Fall River Pass to Poudre Lakes 23 Trail Ridge Road between Fall River Pass and Deer Ridge Junction 24 Deer Ridge Junction to Fall River Entrance via Horseshoe Park 29 Bear Lake Road 29 ILLUSTRATIONS LONGS PEAK FROM BEAR LAKE Front and back covers CHASM FALLS Inside back cover FIGURE PAGE 1. GEOLOGIC TIME SCALE iv 2. LONGS PEAK FROM THE EAST 3 3. PROFILE SECTION ACROSS THE ROCKY MOUNTAINS 5 4. ANCIENT EROSIONAL PLAIN ON TRAIL RIDGE 6 5. ANCIENT EROSIONAL PLAIN FROM FLATTOP MOUNTAIN ... 7 6. VIEW NORTHWEST FROM LONGS PEAK 8 7. -
Summits on the Air – ARM for USA - Colorado (WØC)
Summits on the Air – ARM for USA - Colorado (WØC) Summits on the Air USA - Colorado (WØC) Association Reference Manual Document Reference S46.1 Issue number 3.2 Date of issue 15-June-2021 Participation start date 01-May-2010 Authorised Date: 15-June-2021 obo SOTA Management Team Association Manager Matt Schnizer KØMOS Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Page 1 of 11 Document S46.1 V3.2 Summits on the Air – ARM for USA - Colorado (WØC) Change Control Date Version Details 01-May-10 1.0 First formal issue of this document 01-Aug-11 2.0 Updated Version including all qualified CO Peaks, North Dakota, and South Dakota Peaks 01-Dec-11 2.1 Corrections to document for consistency between sections. 31-Mar-14 2.2 Convert WØ to WØC for Colorado only Association. Remove South Dakota and North Dakota Regions. Minor grammatical changes. Clarification of SOTA Rule 3.7.3 “Final Access”. Matt Schnizer K0MOS becomes the new W0C Association Manager. 04/30/16 2.3 Updated Disclaimer Updated 2.0 Program Derivation: Changed prominence from 500 ft to 150m (492 ft) Updated 3.0 General information: Added valid FCC license Corrected conversion factor (ft to m) and recalculated all summits 1-Apr-2017 3.0 Acquired new Summit List from ListsofJohn.com: 64 new summits (37 for P500 ft to P150 m change and 27 new) and 3 deletes due to prom corrections. -
TRATL RIDGE ROAD Rocky' Mountain National Park Between
TRATL RIDGE ROAD HAER No. CO-31 Rocky' Mountain National Park Between Estes Park and Grand Lake Estes Park vicinity Larimer County COLO Colorado 7- y PHOTOGRAPHS WRITTEN HISTORICAL AND DESCRIPTIVE DATA HISTORIC AMERICAN ENGINEERING RECORD National Park Service U.S. Department of the Interior P.O. Box 37127 Washington, D.C. 20013-7127 HISTORIC AMERICAN ENGINEERING RECORD TRAIL RIDGE ROAD Rocky Mountain National Park 7- HAER NO. CO-31 Location: Traversing Rocky Mountain National Park from Estes Park to Grand Lake, Colorado. Quadrangle and UTM: East end: Fall River Entrance Estes Park quad 13/448191/4470700 West end: Grand Lake Entrance Grand Lake quad 13/428765/4456351 Construction Date 1926-1949 Present Owner: Rocky Mountain National Park, National Park Service Present Use: Park scenic highway Significance: Trail Ridge Road has national, state, and local significance as an engineering feat-- the highest continuous highway in the United States—and for its role in the development of the Rocky Mountain National Park road system. Project Information: Documentation of Trail Ridge Road is part of the National Park Service Roads and Bridges Recording Project, conducted during the summer of 1993 under the co-sponsorship of HABS/HAER and Rocky Mountain National Park. Richard Quin, HAER Historian, August 1993 TRAIL RIDGE ROAD HAER NO. CO-31 (page 2) II. HISTORY The highest road in the national park system, and the highest continuous paved highway in the United States, the Trail Ridge Road is the principal highway crossing Rocky Mountain National Park between the park border communities of Estes Park and Grand Lake. The road was constructed largely between 1929 and 1932 to replace the Fall River Road; after its completion, the western portion of the old road was abandoned, and the eastern segment became a one-way uphill road. -
Rocky Mountain National Park Geologic Resource Evaluation Report
National Park Service U.S. Department of the Interior Geologic Resources Division Denver, Colorado Rocky Mountain National Park Geologic Resource Evaluation Report Rocky Mountain National Park Geologic Resource Evaluation Geologic Resources Division Denver, Colorado U.S. Department of the Interior Washington, DC Table of Contents Executive Summary ...................................................................................................... 1 Dedication and Acknowledgements............................................................................ 2 Introduction ................................................................................................................... 3 Purpose of the Geologic Resource Evaluation Program ............................................................................................3 Geologic Setting .........................................................................................................................................................3 Geologic Issues............................................................................................................. 5 Alpine Environments...................................................................................................................................................5 Flooding......................................................................................................................................................................5 Hydrogeology .............................................................................................................................................................6