DOCSLIB.ORG

Little Colorado River Tribal Park

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
Little Colorado River Tribal Park LITTLE COLORADO RIVER TRIBAL PARK Cameron, Arizona “Pictures Speaks a Thousand Words” LCR VIEWPOINTS • Shadow Mountain Viewpoint • Second Viewpoint (No specific name yet) • Hell Hole Bend (Need to come up with a better name) This is where Nik Wallenda walked the tightrope. This is Little Colorado River Gorge LCR Shadow Mountain Viewpoint This is at our viewpoint where our Fee Station is at, we have the viewpoint down into the canyon, some arts and crafts vendors vend here. This picture here shows the Jumbotron that was set up on June 23, 2013 to view the Wallenda Skywire walk; and we had audience to view it here. Storm Trooper at LCR Entrance Station at Shadow Mountain Viewpoint One of our unique visitor. Shadow Mountain Conceptual Plan This Shadow Mountain viewpoint conceptual site plan that we are still working on accomplishing; actually there are a number of different plans; and a number of attempts been made as well. The problem is lack of funds to make it a reality. LCR is a Park that makes the least amount of revenue so it’s not a priority to the Tribe as far as funding for development; but yet you would think it would be for that reason. LCR Second Viewpoint Again, another conceptional site plan for LCR second viewpoint. This place is pretty much under develop but yet we do get a lot of visitors here. That blue line, and portion of the brown line are trails that our visitors walk. Google Map of Hell Hole Bend We envision this place to be a major viewpoint development; where the Skywire Walk happen. Didn’t have a picture available. LCR Hiking Trails • Salt Trail • Blue Springs Trail • Eminence Break • Shinuma Wash • Jackass Canyon • Tatahatso Canyon Where we are on the map…. Salt Trail Salt Trail is the most accessible of the Little Colorado River routes, although it is very challenging hikers has to be experienced and in good condition or accompanied by those that are experienced. The Salt Trail is also the most scenic of the routes. Blue Canyon –Emerald Pool The spring which gush out of the red wall limestone at river level is the main attraction on this trail. These springs are the main source of water for the Little Colorado during the dry season, although they are augmented by a number of other springs before the Colorado River is reached 13.5 miles downstream. The water from these springs is fit to drink, although it has a heavy mineral taste. This trail is for experience hikers. Eminence Canyon Also known as Eminence Break, this route is a rugged but scenic side hike in the Marble Canyon Tribal Park. The route starts at river level and follows a rough cairned trail to the canyon rim near Tatahatso Point. Most visitors to Grand Canyon do not venture up the route as it is quite rugged and free climbing is required at several locations, especially in portions through the Supai, Coconino, and Kaibab Formations. Eminence Canyon Shinuma Canyon Also known as Shinuma Wash; it begins by making a long pass up shinuma wash then switch back down the bed of the canyon. It follows the bottom of the canyon until the red wall lime stone is reached. This is where it leaves the bed and follows the top of the red wall. At break in the wall the trail descends to the river. Another branch of the trail continues along the top of the red wall for several miles. The trail drops 3,500 feet from rim to the river. Jackass Canyon –Marble Canyon Tribal Park The canyon deepens fairly quickly and it’s easy walking. About 45 minutes after the start of your hike you will arrive at a drop off of 40 feet. There were several fixed ropes in place at this point for use as a hand line. You could also try to climb down; however, this could be tricky if the rock were wet. Below the drop off is a nice, if short, stretch of narrows and you will begin to hear the faint roar of the Colorado River below you. Lower in the canyon you will encounter a number of boulders which require some scrambling to negotiate, but nothing difficult, and just beyond is the Colorado River. Jackass Canyon Tatahatso Canyon The view from top of the canyon is beautiful and you’ll make your way down the canyon and look over the edge at the Colorado River snaking its way around the sandstone domes and limestone pinnacles. This site will seem something out of a movie or a picture. Tatahatso Canyon Confluence: Where LCR flows into the Colorado River Beautiful, beautiful site but the most controversial site as well. The turquoise water coming out is the Little Colorado River and the dark green is the Colorado River. You have probably heard of the Confluence Escalade – this is the place they are talking about. Little Colorado River LCR LCR today, after all the rain Little Colorado River Gorge Overlooking LCR March 27, 1962 –March 27, 2012 On April 28, 2012 we celebrated the 50th Golden Anniversary for Little Colorado River Tribal Park. Celebrated with a day long activities, Entertainment, horseback ride, special speakers, etc. The day before we provided Horse Clinic for the riders that were entering. NPRD Staff THE END We are thankful for the Promises and this beautiful land we have. The Mission of Navajo Parks and Recreation Department is to Protect, Preserve and Manage Tribal Parks, Monuments, and Recreation areas; to accomplish this, we will: •Provide quality visitor services •Enhance visitor experience •Enforce Tribal Laws •Strengthen community partnership •Provide quality interpretation •Enhance staff development Commercial Filming and Photography • Nik Wallenda Tightrope Walk • CBS Eye Too Production • Godfrey Entertainment • Teton Gravity Research • And many more Nik Wallenda Our most challenging Commericial Filming LCR ever encountered and taken on is the Skywire Walk that Wallenda did at a place call Hell Hole Bend within LCR. The request for this filming came to us in September 2012 and all the planning started through June 2013; the actual walk took place on June 23, 2013. At beginning, this picture was taken at the site. Wallenda Walk Pyramid This pyramid was put in at two places, one from where the walk begin and one to where the walk ended; the wire was over the top of this pyramid from point A to B which Wallenda walked on across the canyon. Day of the Event Day of the Event The Walk The Walk Do you see him? Wallenda – I walk the Line (Rope) Wallenda doing autograph at end of the walk NN Parks @ Time Square NYC.
Load more

Recommended publications
  • Influence of a Dam on Fine-Sediment Storage in a Canyon River Joseph E
    JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 111, F01025, doi:10.1029/2004JF000193, 2006 Influence of a dam on fine-sediment storage in a canyon river Joseph E. Hazel Jr.,1 David J. Topping,2 John C. Schmidt,3 and Matt Kaplinski1 Received 24 June 2004; revised 18 August 2005; accepted 14 November 2005; published 28 March 2006. [1] Glen Canyon Dam has caused a fundamental change in the distribution of fine sediment storage in the 99-km reach of the Colorado River in Marble Canyon, Grand Canyon National Park, Arizona. The two major storage sites for fine sediment (i.e., sand and finer material) in this canyon river are lateral recirculation eddies and the main- channel bed. We use a combination of methods, including direct measurement of sediment storage change, measurements of sediment flux, and comparison of the grain size of sediment found in different storage sites relative to the supply and that in transport, in order to evaluate the change in both the volume and location of sediment storage. The analysis shows that the bed of the main channel was an important storage environment for fine sediment in the predam era. In years of large seasonal accumulation, approximately 50% of the fine sediment supplied to the reach from upstream sources was stored on the main-channel bed. In contrast, sediment budgets constructed for two short-duration, high experimental releases from Glen Canyon Dam indicate that approximately 90% of the sediment discharge from the reach during each release was derived from eddy storage, rather than from sandy deposits on the main-channel bed.
    [Show full text]
  • The Little Colorado River Project: Is New Hydropower Development the Key to a Renewable Energy Future, Or the Vestige of a Failed Past?
    COLORADO NATURAL RESOURCES, ENERGY & ENVIRONMENTAL LAW REVIEW The Little Colorado River Project: Is New Hydropower Development the Key to a Renewable Energy Future, or the Vestige oF a Failed Past? Liam Patton* Table of Contents INTRODUCTION ........................................................................................ 42 I. THE EVOLUTION OF HYDROPOWER ON THE COLORADO PLATEAU ..... 45 A. Hydropower and the Development of Pumped Storage .......... 45 B. History of Dam ConstruCtion on the Plateau ........................... 48 C. Shipping ResourCes Off the Plateau: Phoenix as an Example 50 D. Modern PoliCies for Dam and Hydropower ConstruCtion ...... 52 E. The Result of Renewed Federal Support for Dams ................. 53 II. HYDROPOWER AS AN ALLY IN THE SHIFT TO CLEAN POWER ............ 54 A. Coal Generation and the Harms of the “Big Buildup” ............ 54 B. DeCommissioning Coal and the Shift to Renewable Energy ... 55 C. The LCR ProjeCt and “Clean” Pumped Hydropower .............. 56 * J.D. Candidate, 2021, University oF Colorado Law School. This Note is adapted From a final paper written for the Advanced Natural Resources Law Seminar. Thank you to the Colorado Natural Resources, Energy & Environmental Law Review staFF For all their advice and assistance in preparing this Note For publication. An additional thanks to ProFessor KrakoFF For her teachings on the economic, environmental, and Indigenous histories of the Colorado Plateau and For her invaluable guidance throughout the writing process. I am grateFul to share my Note with the community and owe it all to my professors and classmates at Colorado Law. COLORADO NATURAL RESOURCES, ENERGY & ENVIRONMENTAL LAW REVIEW 42 Colo. Nat. Resources, Energy & Envtl. L. Rev. [Vol. 32:1 III. ENVIRONMENTAL IMPACTS OF PLATEAU HYDROPOWER ...............
    [Show full text]
  • Arizona Fishing Regulations 3 Fishing License Fees Getting Started
    2019 & 2020 Fishing Regulations for your boat for your boat See how much you could savegeico.com on boat | 1-800-865-4846insurance. | Local Offi ce geico.com | 1-800-865-4846 | Local Offi ce See how much you could save on boat insurance. Some discounts, coverages, payment plans and features are not available in all states or all GEICO companies. Boat and PWC coverages are underwritten by GEICO Marine Insurance Company. GEICO is a registered service mark of Government Employees Insurance Company, Washington, D.C. 20076; a Berkshire Hathaway Inc. subsidiary. TowBoatU.S. is the preferred towing service provider for GEICO Marine Insurance. The GEICO Gecko Image © 1999-2017. © 2017 GEICO AdPages2019.indd 2 12/4/2018 1:14:48 PM AdPages2019.indd 3 12/4/2018 1:17:19 PM Table of Contents Getting Started License Information and Fees ..........................................3 Douglas A. Ducey Governor Regulation Changes ...........................................................4 ARIZONA GAME AND FISH COMMISSION How to Use This Booklet ...................................................5 JAMES S. ZIELER, CHAIR — St. Johns ERIC S. SPARKS — Tucson General Statewide Fishing Regulations KURT R. DAVIS — Phoenix LELAND S. “BILL” BRAKE — Elgin Bag and Possession Limits ................................................6 JAMES R. AMMONS — Yuma Statewide Fishing Regulations ..........................................7 ARIZONA GAME AND FISH DEPARTMENT Common Violations ...........................................................8 5000 W. Carefree Highway Live Baitfish
    [Show full text]
  • Trip Planner
    National Park Service U.S. Department of the Interior Grand Canyon National Park Grand Canyon, Arizona Trip Planner Table of Contents WELCOME TO GRAND CANYON ................... 2 GENERAL INFORMATION ............................... 3 GETTING TO GRAND CANYON ...................... 4 WEATHER ........................................................ 5 SOUTH RIM ..................................................... 6 SOUTH RIM SERVICES AND FACILITIES ......... 7 NORTH RIM ..................................................... 8 NORTH RIM SERVICES AND FACILITIES ......... 9 TOURS AND TRIPS .......................................... 10 HIKING MAP ................................................... 12 DAY HIKING .................................................... 13 HIKING TIPS .................................................... 14 BACKPACKING ................................................ 15 GET INVOLVED ................................................ 17 OUTSIDE THE NATIONAL PARK ..................... 18 PARK PARTNERS ............................................. 19 Navigating Trip Planner This document uses links to ease navigation. A box around a word or website indicates a link. Welcome to Grand Canyon Welcome to Grand Canyon National Park! For many, a visit to Grand Canyon is a once in a lifetime opportunity and we hope you find the following pages useful for trip planning. Whether your first visit or your tenth, this planner can help you design the trip of your dreams. As we welcome over 6 million visitors a year to Grand Canyon, your
    [Show full text]
  • Grand Canyon-Parashant National Monument Foundation Document
    NATIONAL PARK SERVICE • U.S. DEPARTMENT OF THE INTERIOR Foundation Document Overview Grand Canyon-Parashant National Monument Arizona Contact Information For more information about the Grand Canyon-Parashant National Monument Foundation Document, contact: [email protected] or 435-688-3226 or write to: Superintendent, Grand Canyon-Parashant National Monument, 345 E. Riverside Drive, St. George, UT 84790 Purpose Significance Significance statements express why Grand Canyon-Parashant National Monument resources and values are important enough to merit designation as a national monument. Statements of significance describe the distinctive nature of the monument and why an area is important within a global, national, regional, and systemwide context. They focus on the most important resources and values that will assist in planning and management for the monument. • Spanning 320 million years, the exposed rock layers at Parashant National Monument provide a distinctly identifiable view of the geologic boundaries of the Colorado Plateau and Basin and Range regions, including evidence of the interaction between volcanic processes and native cultural communities. The extensive natural history reveals a robust fossil record and preserves museum-quality marine and ice age fossils. At GRAND CANYON-PARASHANT NATIONAL • Encompassing more than 1 million acres, a dramatic MONUMENT, the Bureau of Land elevational gradient from 1,200 to 8,000 feet, and transitional Management and the National zones of the Sonoran, Mojave, Great Basin, and Colorado Park Service cooperatively protect Plateau ecoregions, Parashant National Monument protects undeveloped, wild, and remote a biologically rich system of plant and animal life. northwestern Arizona landscapes • Parashant National Monument is one of the most rugged and their resources, while providing and remote landscapes remaining in the southwestern opportunities for solitude, primitive United States.
    [Show full text]
  • Grand Canyon.Com's Spring Travel Guide
    Grand Canyon.com’s Spring Travel Guide Second Edition Helping You Get Even More Out of Your Grand Canyon Vacation! Thank you for choosing Grand Canyon.com as your Southwest destination specialist! You’ve chosen a truly extraordinary place for your spring vacation, and our mission is to help you get the most out of your trip. Having helped thousands of busy people like you plan their Grand Canyon vacations for over 20 years, our staff has made a few observations and picked up a few insider tips that can help save you time, money and hassle - sometimes all three at once! It was to that end that we presented our First Annual Spring Break Travel Guide in February. Since then, peoples’ response has been nothing short of overwhelming. But with spring break extending well into April this year, we realized that a few things needed updating in order for you to be as well informed as possible before hitting the road. It is to that end that we present: Grand Canyon.com’s First Annual Spring Travel Guide: The Second Edition Before you dig in, we recommend that you grab a few things: a map or road atlas, a pen and/or a highlighter, maybe a beverage, a few minutes of quiet time, and your “Grand Canyon Top Tours Brochure.” Let’s get started and get YOU* to the Grand Canyon! *Got most of your trip figured out already? Skip to Chapter 8 Traveler Tip 1 - Where’s It At and What Side Am I On? The Grand Canyon is in Northern Arizona.
    [Show full text]
  • Quaternary Geology and Geomorphology of the Nankoweap Rapids Area, Marble Canyon, Arizona
    U.S. DEPARTMENT OF THE INTERIOR TO ACCOMPANY MAP 1-2608 U.S. GEOLOGICAL SURVEY QUATERNARY GEOLOGY AND GEOMORPHOLOGY OF THE NANKOWEAP RAPIDS AREA, MARBLE CANYON, ARIZONA By Richard Hereford, Kelly J. Burke, and Kathryn S. Thompson INTRODUCTION sion elsewhere in Grand Canyon {Hereford and oth­ ers, 1993; Fairley and others, 1994, p. 147-150). The Nankoweap Rapids area along the Colorado River {fig. 1) is near River Mile 52 {that is 52 mi or 83 km downstream of Lees Ferry, Arizona) in Grand Canyon National Park {west bank) and the Navajo METHODS Indian Reservation {east bank). Geologic mapping and [See map sheet for Description of Map Units] related field investigations of the late Quaternary geo­ morphology of the Colorado River and tributary A variety of methods were used to date the de­ streams were undertaken to provide information about posits. Radiocarbon dates were obtained from char­ the age, distribution, and origin of surficial deposits. coal and wood recovered from several of the mapped These deposits, particularly sandy alluvium and closely units (table 1). Several of these dates are not defini­ related debris-flow sediment, are the substrate for tive as they are affected by extensive animal bur­ riparian vegetation, which in turn supports the eco­ rowing in the alluvial deposits that redistributed burnt system of the Colorado River (Carothers and Brown, roots of mesquite trees, giving anomalous dates. The 1991, p. 111-167). late Pleistocene breccia (units be and bf) and re­ Closure of Glen Canyon Dam {109 km or 68 lated terraces were dated by Machette and Rosholt mi upstream of the study area) in 1963 and subse­ (1989; 1991) using the uranium-trend method.
    [Show full text]
  • Geologic Map and Upper Paleozoic Stratigraphy of the Marble Canyon Area, Cottonwood Canyon Quadrangle, Death Valley National Park, Inyo County, California
    Geologic Map and Upper Paleozoic Stratigraphy of the Marble Canyon Area, Cottonwood Canyon Quadrangle, Death Valley National Park, Inyo County, California By Paul Stone, Calvin H. Stevens, Paul Belasky, Isabel P. Montañez, Lauren G. Martin, Bruce R. Wardlaw, Charles A. Sandberg, Elmira Wan, Holly A. Olson, and Susan S. Priest Pamphlet to accompany Scientific Investigations Map 3298 2014 U.S. Department of the Interior U.S. Geological Survey Cover View of Marble Canyon area, California, showing dark rocks of Mississippian Indian Springs Formation and Pennsylvanian Bird Spring Formation overlying light rocks of Mississippian Santa Rosa Hills Limestone in middle distance. View is southeast toward Emigrant Wash and Tucki Mountain in distance. U.S. Department of the Interior SALLY JEWELL, Secretary U.S. Geological Survey Suzette M. Kimball, Acting Director U.S. Geological Survey, Reston, Virginia: 2014 For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment—visit http://www.usgs.gov or call 1–888–ASK–USGS For an overview of USGS information products, including maps, imagery, and publications, visit http://www.usgs.gov/pubprod To order this and other USGS information products, visit http://store.usgs.gov Suggested citation: Stone, P., Stevens, C.H., Belasky, P., Montanez, I.P., Martin, L.G., Wardlaw, B.R., Sandberg, C.A., Wan, E., Olson, H.A., and Priest, S.S., 2014, Geologic map and upper Paleozoic stratigraphy of the Marble Canyon area, Cottonwood Canyon quadrangle, Death Valley National Park, Inyo County, California: U.S. Geological Survey Scientific Investigations Map 3298, scale 1:24,000, 59 p., http://dx.doi.org/10.3133/sim3298.
    [Show full text]
  • Of North Rim Pocket
    Grand Canyon National Park National Park Service Grand Canyon Arizona U.S. Department of the Interior Pocket Map North Rim Services Guide Services, Facilities, and Viewpoints Inside the Park North Rim Visitor Center / Grand Canyon Lodge Campground / Backcountry Information Center Services and Facilities Outside the Park Protect the Park, Protect Yourself Information, lodging, restaurants, services, and Grand Canyon views Camping, fuel, services, and hiking information Lodging, camping, food, and services located north of the park on AZ 67 Use sunblock, stay hydrated, take Keep wildlife wild. Approaching your time, and rest to reduce and feeding wildlife is dangerous North Rim Visitor Center North Rim Campground Kaibab Lodge the risk of sunburn, dehydration, and illegal. Bison and deer can Park in the designated parking area and walk to the south end of the parking Operated by the National Park Service; $18–25 per night; no hookups; dump Located 18 miles (30 km) north of North Rim Visitor Center; open May 15 to nausea, shortness of breath, and become aggressive and will defend lot. Bring this Pocket Map and your questions. Features new interpretive station. Reservation only May 15 to October 15: 877-444-6777 or recreation. October 20; lodging and restaurant. 928-638-2389 or kaibablodge.com exhaustion. The North Rim's high their space. Keep a safe distance exhibits, park ranger programs, restroom, drinking water, self-pay fee station, gov. Reservation or first-come, first-served October 16–31 with limited elevation (8,000 ft / 2,438 m) and of at least 75 feet (23 m) from all nearby canyon views, and access to Bright Angel Point Trail.
    [Show full text]
  • 2010 General Management Plan
    Montezuma Castle National Monument National Park Service Mo n t e z u M a Ca s t l e na t i o n a l Mo n u M e n t • tu z i g o o t na t i o n a l Mo n u M e n t Tuzigoot National Monument U.S. Department of the Interior ge n e r a l Ma n a g e M e n t Pl a n /en v i r o n M e n t a l as s e s s M e n t Arizona M o n t e z u MONTEZU M A CASTLE MONTEZU M A WELL TUZIGOOT M g a e n e r a l C a s t l e M n a n a g e a t i o n a l M e n t M P o n u l a n M / e n t e n v i r o n • t u z i g o o t M e n t a l n a a t i o n a l s s e s s M e n t M o n u M e n t na t i o n a l Pa r k se r v i C e • u.s. De P a r t M e n t o f t h e in t e r i o r GENERAL MANA G E M ENT PLAN /ENVIRON M ENTAL ASSESS M ENT General Management Plan / Environmental Assessment MONTEZUMA CASTLE NATIONAL MONUMENT AND TUZIGOOT NATIONAL MONUMENT Yavapai County, Arizona January 2010 As the responsible agency, the National Park Service prepared this general management plan to establish the direction of management of Montezuma Castle National Monument and Tu- zigoot National Monument for the next 15 to 20 years.
    [Show full text]
  • Hells Canyon 5 Day to Heller
    Trip Logistics and Itinerary 5 days, 4 nights Wine & Food on the Snake River in Hells Canyon Trip Starts: Minam, OR Trip Ends: Minam, OR Put-in: Hell’s Canyon Dam, OR Take-out: Heller Bar, WA (23 miles south of Asotin, WA) Trip length: 79 miles Class III-IV rapids Each Trip varies slightly with size of group, interests of guests, etc. This is a “typical” trip itinerary that will vary. Day before Launch: Stop at Minam on your way to your motel in Wallowa or Enterprise to pick up your dry bag and go over the morning itinerary. Day 1: If staying in Wallowa at the Mingo Motel we will pick you up at 6:15 am. If staying in Enterprise we will pick you up at the Ponderosa Motel in our shuttle van at 6:45 am. Travel to Hells Canyon Dam Launch site (3hr drive from Minam) with a bathroom break at the Hells Canyon Overlook. Meet your guides, go over basic safety talk, and load into rafts between 10 and 11 am. Lunch will be served riverside. Enjoy awe inspiring geology, spot wildlife. Run some of the biggest whitewater of the trip, first up Wild Sheep Rapid. Stop to scout Granite Rapid and view Nez Perce pictographs. Arrive in camp between 3-4pm. Evening camp time: swim, hike, play games, relax! Approximately 6pm: Wine and Hor D’oevres presented by Chef Andrae and the featured Winery. Approximately 7 pm dinner presented by chef Andrae Bopp. Day 2: Coffee is ready by 6 am. Leisurely breakfast between 7 and 8 am.
    [Show full text]
  • Classifying Rivers - Three Stages of River Development
    Classifying Rivers - Three Stages of River Development River Characteristics - Sediment Transport - River Velocity - Terminology The illustrations below represent the 3 general classifications into which rivers are placed according to specific characteristics. These categories are: Youthful, Mature and Old Age. A Rejuvenated River, one with a gradient that is raised by the earth's movement, can be an old age river that returns to a Youthful State, and which repeats the cycle of stages once again. A brief overview of each stage of river development begins after the images. A list of pertinent vocabulary appears at the bottom of this document. You may wish to consult it so that you will be aware of terminology used in the descriptive text that follows. Characteristics found in the 3 Stages of River Development: L. Immoor 2006 Geoteach.com 1 Youthful River: Perhaps the most dynamic of all rivers is a Youthful River. Rafters seeking an exciting ride will surely gravitate towards a young river for their recreational thrills. Characteristically youthful rivers are found at higher elevations, in mountainous areas, where the slope of the land is steeper. Water that flows over such a landscape will flow very fast. Youthful rivers can be a tributary of a larger and older river, hundreds of miles away and, in fact, they may be close to the headwaters (the beginning) of that larger river. Upon observation of a Youthful River, here is what one might see: 1. The river flowing down a steep gradient (slope). 2. The channel is deeper than it is wide and V-shaped due to downcutting rather than lateral (side-to-side) erosion.
    [Show full text]