Greenback Cutthroat Trout Recovery Plan
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Rocky Mountain U.S
National Park Service Rocky Mountain U.S. Department of Interior Rocky Mountain National Park Camping 2012 Enjoy a night under the stars in Rocky Mountain National Park! It is important to note that in 2012, Glacier Basin Campground is closed due to Bear Lake Road Reconstruction, and Moraine Park Campground Loop B is first-come, first-served. Except for Longs Peak Campground which accepts tents only, all campgrounds can accommodate tent trailers, tents, pickup campers, trailers, and motorhomes. Every park campsite has a tent pad, picnic table and fire grate. More than one tent is allowed, as long as they all fit on the tent pad. No more than eight people may camp at a given site, except for designated group sites at Moraine Park Campground. Maximum length of stay is 7 nights total parkwide between June 1 - September 30. Campers can stay an additional 14 nights between October 1 - May 31. The most popular time for camping in the park is from early July to early September. Campgrounds are frequently full from July 4th weekend through Labor Day and on fall weekends during the elk rut and colorful foliage. Reservable campgrounds are often full by reservation, and the first-come, first-served campgrounds can often fill by noon. Check at a visitor center, park newspaper or park website for evening ranger program schedules at campgrounds. Reservations Have peace of mind knowing a campsite is waiting Website www.recreation.gov Summer 2012 for you in beautiful Rocky Mountain National Calls from within the U. S. 877-444-6777 Calls from outside the U. -
To See the Hike Archive
Geographical Area Destination Trailhead Difficulty Distance El. Gain Dest'n Elev. Comments Allenspark 932 Trail Near Allenspark A 4 800 8580 Allenspark Miller Rock Riverside Dr/Hwy 7 TH A 6 700 8656 Allenspark Taylor and Big John Taylor Rd B 7 2300 9100 Peaks Allenspark House Rock Cabin Creek Rd A 6.6 1550 9613 Allenspark Meadow Mtn St Vrain Mtn TH C 7.4 3142 11632 Allenspark St Vrain Mtn St Vrain Mtn TH C 9.6 3672 12162 Big Thompson Canyon Sullivan Gulch Trail W of Waltonia Rd on Hwy A 2 941 8950 34 Big Thompson Canyon 34 Stone Mountain Round Mtn. TH B 8 2100 7900 Big Thompson Canyon 34 Mt Olympus Hwy 34 B 1.4 1438 8808 Big Thompson Canyon 34 Round (Sheep) Round Mtn. TH B 9 3106 8400 Mountain Big Thompson Canyon Hwy 34 Foothills Nature Trail Round Mtn TH EZ 2 413 6240 to CCC Shelter Bobcat Ridge Mahoney Park/Ginny Bobcat Ridge TH B 10 1500 7083 and DR trails Bobcat Ridge Bobcat Ridge High Bobcat Ridge TH B 9 2000 7000 Point Bobcat Ridge Ginny Trail to Valley Bobcat Ridge TH B 9 1604 7087 Loop Bobcat Ridge Ginny Trail via Bobcat Ridge TH B 9 1528 7090 Powerline Tr Boulder Chautauqua Park Royal Arch Chautauqua Trailhead by B 3.4 1358 7033 Rgr. Stn. Boulder County Open Space Mesa Trail NCAR Parking Area B 7 1600 6465 Boulder County Open Space Gregory Canyon Loop Gregory Canyon Rd TH B 3.4 1368 7327 Trail Boulder Open Space Heart Lake CR 149 to East Portal TH B 9 2000 9491 Boulder Open Space South Boulder Peak Boulder S. -
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 -
Rocky Mountain National Park News U.S
National Park Service Rocky Mountain National Park News U.S. Department of the Interior The official newspaper of Rocky Mountain National Park Summer - 2013 July 19 - September 2 2nd Edition Bear Lake Road Reconstruction continues. Expect up to two, 20 minute delays in each direction between Moraine NPS/Ann Schonlau Park Visitor Center and the Park & Ride. Welcome to Your Park! Visitor Centers Rocky Mountain National Park is a special place in the hearts of many people. These mountains are home to flowers, forests and wildlife. For East of the Divide – Estes Park Area generations, this place has nourished the human spirit and connected us to the natural world. We invite you to explore your park, make your own Alpine Visitor Center memories, and discover what Rocky means to you. Enjoy it, protect it Open daily 9 a.m.-5 p.m. (weather permitting) Features extraordinary views of alpine tundra, displays, information, and be safe out there. bookstore, adjacent gift shop, cafe, and coffee bar. Call (970) 586-1222 for The Staff of Rocky Mountain National Park Trail Ridge Road conditions. Beaver Meadows Visitor Center Looking for Fun? Open daily 8 a.m.- 6 p.m. Features spectacular free park movie, Rocky Mountain National Park has something for everyone! Make information, bookstore, large park orientation your trip memorable with these tips: map, and backcountry permits in an adjacent building. Be inspired – How many times can you say, “Wow!” Find out by driving Fall River Visitor Center Alpine Visitor Center up Trail Ridge Road for spectacular views. Open daily 9 a.m.-5 p.m. -
COLORADO CONTINENTAL DIVIDE TRAIL COALITION VISIT COLORADO! Day & Overnight Hikes on the Continental Divide Trail
CONTINENTAL DIVIDE NATIONAL SCENIC TRAIL DAY & OVERNIGHT HIKES: COLORADO CONTINENTAL DIVIDE TRAIL COALITION VISIT COLORADO! Day & Overnight Hikes on the Continental Divide Trail THE CENTENNIAL STATE The Colorado Rockies are the quintessential CDT experience! The CDT traverses 800 miles of these majestic and challenging peaks dotted with abandoned homesteads and ghost towns, and crosses the ancestral lands of the Ute, Eastern Shoshone, and Cheyenne peoples. The CDT winds through some of Colorado’s most incredible landscapes: the spectacular alpine tundra of the South San Juan, Weminuche, and La Garita Wildernesses where the CDT remains at or above 11,000 feet for nearly 70 miles; remnants of the late 1800’s ghost town of Hancock that served the Alpine Tunnel; the awe-inspiring Collegiate Peaks near Leadville, the highest incorporated city in America; geologic oddities like The Window, Knife Edge, and Devil’s Thumb; the towering 14,270 foot Grays Peak – the highest point on the CDT; Rocky Mountain National Park with its rugged snow-capped skyline; the remote Never Summer Wilderness; and the broad valleys and numerous glacial lakes and cirques of the Mount Zirkel Wilderness. You might also encounter moose, mountain goats, bighorn sheep, marmots, and pika on the CDT in Colorado. In this guide, you’ll find Colorado’s best day and overnight hikes on the CDT, organized south to north. ELEVATION: The average elevation of the CDT in Colorado is 10,978 ft, and all of the hikes listed in this guide begin at elevations above 8,000 ft. Remember to bring plenty of water, sun protection, and extra food, and know that a hike at elevation will likely be more challenging than the same distance hike at sea level. -
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 -
1 Andrews Glacier in August 2016 Tyndall Glacier Lidar Scan in May
Final Report for “Glacier and perennial snowfield mass balance of Rocky Mountain National Park (ROMO): Past, Present, and Future” Task Agreement Number P16AC00826 PI Dr. Daniel McGrath June 28, 2019 Department of Geosciences Colorado State University [email protected] Andrews Glacier in August 2016 Tyndall Glacier LiDAR scan in May 2016 1 Summary of Key Project Outcomes • Over the past ~50 years, geodetic glacier mass balances for four glaciers along the Front Range have been highly variable; for example, Tyndall Glacier thickened slightly, while Arapaho Glacier thinned by >20 m. These glaciers are closely located in space (~30 km) and hence the regional climate forcing is comparable. This variability points to the important role of local topographic/climatological controls (such as wind-blown snow redistribution and topographic shading) on the mass balance of these very small glaciers (~0.1-0.2 km2). • Since 2001, glacier area (for 11 glaciers on the Front Range) has varied ± 40%, with changes most commonly driven by interannual variability in seasonal snow. However, between 2001 and 2017, the glaciers exhibited limited net change in area. Previous work (Hoffman et al., 2007) found that glacier area had started to decline starting in ~2000. • Seasonal mass turnover is very high for Andrews and Tyndall glaciers. On average, the glaciers gain and lose ~9 m of elevation each year. Such extraordinary amounts of snow accumulation is primarily the result of wind-blown snow redistribution into these basins (and to a certain degree, avalanching at Tyndall Glacier) and exceeds observed peak snow water equivalent at a nearby SNOTEL station by 5.5 times. -
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. -
Relationship Between Sediment Supply and Sediment Transport for the Roaring River, Colorado, USA
Relationship between sediment supply and sediment transport for the Roaring River, Colorado, USA J.C. BATHURST NERC Water Resource Systems Research Unit, Department of Civil Engineering, University of Newcastle upon Tyne, UK G.J.L, LEEKS & M.D. NEWSON Institute of Hydrology, Staylittle, Powys, UK ABSTRACT A 1-km long gorge, cut into a glacial moraine by a dambreak flood wave, has provided the setting for a study of the relationship between supply of sediment from the gorge cliffs and the sediment transport along the Roaring River. Measurements during two snowmelt seasons have indicated two major supply systems. The initial snowmelt flows, peaking at about 5 m s~1 in May-June, carry relatively large bed and suspended loads, composed of material supplied to the channel bed and margins by winter erosion processes. Rapid depletion of these supplies, though, means that the sediment loads of later flows are reduced by an order of magnitude. This trend may be reversed in July and August when heavy rainstorms can dramatically increase cliff erosion and thence sediment transport. Relatively high transport rates may then persist for several days. External supply of sediment can thus cause two orders of magnitude variation in sediment transport for a given flow discharge. A full understanding of the relationship between supply and transport is obtained only by considering events in chronological order. INTRCDUCTION Until recently, studies of fluvial sediment transport processes have concentrated on lowland rather than mountain rivers. However, development pressures throughout the world's mountain areas are increasingly altering the naturally sensitive balance between sediment supply and transport at the upper ends of river systems (e.g. -
30Th Anniversary of the Lawn Lake Dam Failure: a Look Back at the State and Federal Response July 27, 2012 Mark E
30th Anniversary of the Lawn Lake Dam Failure: A Look Back at the State and Federal Response July 27, 2012 Mark E. Baker, P.E. National Park Service, Denver, CO Bill McCormick, P.E., P.G., Colorado Division of Water Resources, Salida, CO ABSTRACT On July 15, 1982, deep in Rocky Mountain National Park, the 26-foot high Lawn Lake Dam failed. The resulting flood charged down a mountain carving deep ravines and depositing huge fields of rock. It also wiped out campsites, tragically killing 3 people. The flood inundated businesses in the town of Estes Park and caused $31 million in damages. This paper describes how the State of Colorado (State) and Federal agencies responded to the event. The many impacts of this dam failure are explored so that the dam safety community can be better prepared to handle the myriad of issues associated with dam failures efficiently. The paper reviews the State’s response including communications immediately following the failure and the details of conducting a dam failure investigation, including the forensic analysis to determine likely failure mechanisms. Changes to the State dam safety program as a result of the failure are described. The effects of the failure on the NPS dam safety program, including the decision to remove other dams within Rocky Mountain National Park are also explored. The role of FEMA in coordinating post- failure research studies conducted by Federal agencies, including the USGS, USBR, and the NPS are also discussed. Finally, the paper describes the types of legal investigations conducted and lawsuits filed following the failure. -
Rocky Mountain National Park Hikes for Families with Ratings 0 1,000 2,000 4,000 6,000 8,000
Rocky Mountain National Park Trail Map Corral Creek USFS Trail Head Rocky Moun!(tain National Park Hikes for Families LAKE HUSTED LOST LAKE LAKE LOUISE Lost Falls #* Rowe Mountain LAKE DUNRAVEN 13184 Dunraven USFS Trail Head LONG DRAW RESERVIOR D !( Rowe Peak 13404 D Hagues Peak 13560 D La Poudre Pass Trail Head !( Mummy Mountain 13425 D Fairchild Mountain 13502 D CRYSTAL LAKE LAWN LAKE Ypsilon Mountain 13514 D SPECTACLE LAKES Chiquita, Mount D 13069 34 Y W H S Crater Bighorn Family Hike U Chapin Pass Trail Head Bridal Veil Falls !( #* Cow Creek Trail Head !( Cache La Poudre Trail Head Crater Trail Head !( !( Horseshoe Falls Family Hike POUDRE LAKE !( Milner Pass Trail Head Chasm Falls #* Horseshoe Falls Rock Cut Trail Head #* !( Thousand Falls #* Lake Irene Family Hike Lawn Lake Trail Head FAN LAKE !( SHEEP LAKES !( !( Beaver Ponds Trail Head !( CASCADE LAKE HIDDEN VALLEY BEAVER PONDS Lumpy Ridge Trail Head !( Ute Crossing Trail Head U !( S HW FOREST LAKE Beaver Ponds Family Hike Y 34 Deer Mountain/ Deer Ridge Trail Head ARROWHEAD LAKE ROCK LAKE !( TOWN OF LAKE ESTES ESTES PARK INKWELL LAKE !( Upper Beaver Meadows Trail Head AZURE LAKE !( TROUT FISHING POND (ARTIFICIAL US HWY 36 US H 7 WY 36 Y W H O L Cub Lake Trail Head O !( !( Fern Lake Trail Head C !( Fern Falls Family Hike HOURGLASS LAKE Fern Falls #* CUB LAKE !( Hallowell Park Trail Head Marguerite Falls !( #* ODESSA LAKE BIERSTADT LAKE East Portal Trail Head Sprague Lake Family Hike !( Grace Falls #* Sprague Lake Trail Head !( !( Bear Lake Family Hike Bierstadt Lake Trail Head -
Rocky Mountain National Park Geologic Resources Evaluation
National Park Service U.S. Department of the Interior Natural Resource Program Center Rocky Mountain National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2004/004 THIS PAGE: Ypsilon Mountain, Rocky Mountain NP. ON THE COVER: Alpine Tundra looking west to the Never Summer Range, Rocky Mountain NP Photos by: NPS and Josh Heise Rocky Mountain National Park Geologic Resource Evaluation Report Natural Resource Report NPS/NRPC/GRD/NRR—2004/004 Geologic Resources Division Natural Resource Program Center P.O. Box 25287 Denver, Colorado 80225 September 2004 U.S. Department of the Interior Washington, D.C. 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. The series targets a general, diverse audience, and may contain NPS policy considerations or address sensitive issues of management applicability. Examples of the diverse array of reports published in this series include vital signs monitoring plans; "how to" resource management papers; proceedings of resource management workshops or conferences; annual reports of resource programs or divisions of the Natural Resource Program Center; resource action plans; fact sheets; and regularly-published newsletters.