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Pdf Brochure twriver.com Tour West is truly a family-run business, with decades of river experience under our collective belts. We currently have three generations of our family still actively involved in providing adventurers with truly Grand Canyon remarkable and memorable river running experiences! page 1 Tour West is truly a family-run business, with decades of river experience under our collective belts. We currently have three generations of our family still actively involved in providing adventurers with truly remarkable and memorable river running experiences! photo courtesy of joe bennion callcall { { 1.800.453.91071.800.453.9107 }} today!today! twriver.com tour west photo courtesy of courtesy photo bennion joe Your family of river adventurers The great outdoors like you ve never seen them Tour West’s history is as storied as the rivers we’ve run for Since those early days, Tour West has fi ne-tuned its trips to While many things have changed in the river running close to 40 years. A family-owned and operated business provide each guest with the ultimate in outdoor experiences–– business over the years, Tour West’s philosophy of discovery since the very beginning, Tour West has thrilled whitewater from the use of top-quality equipment to serving up the best in has remained the same. We recognize that a trip on the enthusiasts in some of the most picturesque settings in outdoor cuisine, to witnessing thrilling vistas and exhilarating river is more than just a vacation; it is a meaningful and the American West. rapids. But what really sets Tour West apart from all the others life-changing experience our guests treasure for the rest of are our guides––friendly professionals who have chosen to their lives. We invite you to join us on the ride of your life Founder Frank Stratton has always carried a deep love for the make the river their true home away from home, and who carry and discover this one-of-a-kind experience for yourself. outdoors. Having spent much of his life hiking, camping, decades of adventuring experience. On average, Tour West fi shing, Frank even took his new bride to the Grand Canyon trip leaders have close to 20 years of experience successfully for their honeymoon in 1943. Frank had spent most of his navigating the rivers of the American West. And while our life as a farmer and teacher until he and a friend took their guides may come from many different backgrounds, the one fi rst rafting trip down the Grand Canyon and needless to say, thing they all share is a deep and abiding love for the river. that experience opened up a whole new world of adventure and discovery. Since then, Frank has shared that dream with 2page Our story the world and has passed on that passion for the river to his This service is operated by Tour West, Inc. a concessionaire under contract with the family, who runs the business today. Currently there are three U.S. Government and administered by the National Park Service. The concessionaire generations involved in Tour West, with a fourth on its way. is responsible for conducting these operations in a satisfactory manner. Prices are approved by the National Park Service. please address comments to: Superintendent Grand Canyon National Park P.O. Box 129 Grand Canyon, AZ 86023 twriver.com callcall {{ 1.800.453.91071.800.453.9107 } } today! today! “Waking up from a dream to find yourself on the beach by the river in the middle of Grand Canyon was out of this world.” Tracey , IL grand c photo courtesy of courtesy photo bennion joe photo courtesy of courtesy photo bennion joe page 1 photo courtesy of courtesy photo bennion joe callcall { { 1.800.453.91071.800.453.9107 }} today!today! twriver.com to Salt Lake City St. George 8WDK /DNH3RZHOO Kanab Fredonia Marble TRIP ENTRY/EXIT POINT Canyon Point of Interest LEE'S FERRY {map not to scale} {illustration by Ruthann Stoner} I-15 anyon 1 ZH 1RUWK5LP Lava Falls Rapid Las Vegas Havasu Phantom V $UL]RQD Canyon Ranch /DNH 0HDG Bar Ten SOUTH Ranch COVE WHITMORE South Rim 1HYDGD WASH to Los Angeles DIAMOND CREEK to Albuquerque to Phoenix Grand ccanyon adventures cchoose from a variety of exciting Grand ccanyon trips to Flagstaff I-40 I-40 The Grand Canyon is one of those rare and powerful 6 { motorized trip } morning you will launch out on the river at Lee’s Ferry &DOLIRUQLDnight Flagstaff places that can be literally labeled as awe-inspiring and spend the next 12 days traveling 187 miles downriver, and life changing. Its grandeur and magnifi cence are Tour West’s 6-night motorized trip winds its way 187 miles enjoying river rafting at its natural and leisurely best. At unrivaled, and the opportunity to witness the sheer into the heart of this beautiful natural wonder. Sporting the end of your trip you will helicopter out of the canyon majesty of the place should not be missed. the biggest rapids and most spectacular sites in the Grand and board a plane to either Las Vegas or Marble Canyon. Canyon, you’ll start in beautiful Marble Canyon, where you A river-rafting trip through this natural wonder combines the will spend your fi rst night at the Marble Canyon Lodge and synergy of world-class whitewater adventure with humbling meet your guide. The next day puts you in the rafts at Lee’s 8 { motorized trip } and breathtaking scenery to make for a truly unforgettable Ferry and sends you on your adventure. You will spend the night river experience. Along with the exhilarating whitewater next six days rafting, hiking, enjoying delicious meals, and Tour West’s 8-night motorized trip is perfect for the traveler rapids, courtesy of the mighty Colorado River, Tour West sleeping under a blanket of spectacular stars. At trip’s end, who wants to see the entire length of the Grand Canyon. Grand Canyon tours also feature access to hidden side canyons you will helicopter out of the canyon at Whitmore Wash and This trip creatively combines the best of our 6- and and ancient Native American ruins, accessible only from the board a plane back to either Las Vegas or Marble Canyon. 3-night motorized trips, allowing you to experience the river. We have been guiding thrill seekers through the Grand 4page Grand Canyon Canyon for nearly 40 years, and with almost 300 miles of Canyon’s stunning vistas like never before. This trip starts river contained within the canyon, our guides can show you a at Marble Canyon where you will spend your fi rst night wholly unique and invigorating experience time and time again. 12 night { oar powered trip } and meet your guide. The next morning you will launch out on the river at Lee’s Ferry and spend the next 8 days With four distinctively unique river trips to choose from, For those who have a bit more time and would like to traveling 295 through the entire length of the canyon. Tour West can provide you with the Grand Canyon move through the Canyon at a slower pace and on smaller Your trip will ultimately take you to Lake Mead, where you adventure that is just right for you––complete with stops rafts, Tour West offers an unforgettable 12-night rowing will be picked up and taken back to Las Vegas by bus. at breathtaking side canyons, mouthwatering meals, and all trip. This excursion begins at Marble Canyon where you the exhilarating class III, IV, and V rapids you can handle! will spend your fi rst night and meet your guide. The next twriver.com call { 1.800.453.9107 } today! ranch / “I must say I thought so many days on the river was going to be too much but I wouldn’t have traded one minute of that time for anything. There was never a dull moment.” Fred , TX callcall { { 1.800.453.91071.800.453.9107 }} today!today! twriver.com / river trips Combining river trips and ranches has become a great way to enjoy the river at its best, and offers adventurers a wholly unique and memorable vision of the Great American West. Tour West now offers wonderful ranch/river combination trips for each of the rivers we run. & cchoose from a variety of exciting Ranch & River trips GRAND CANYON AND BAR TEN RANCH two full days and nights of rafting and camping. Although most Canyon. On your rafting adventure you will spend your time 3 night { motorized trip } of the larger whitewater river rapids are found above Lava Falls, enjoying thrilling rapids, scenic hikes, and the best in outdoor this 3-night adventure gives travelers an excellent introduction cooking. The last morning of your trip will take you to Hite As the Colorado River winds its way between the Shivwits to river running with a chance to sample one-of-a-kind outdoor Marina, where you’ll have the option to either fl y back to and Hualapai plateaus, it cascades into the lower gorge cooking and the chance to sleep under brilliant starry skies. At Moab or have your vehicle shuttled to meet you at Hite. of the Grand Canyon, creating a vision of delightful and trip’s end, you will be transported to Las Vegas airport by bus. unexpected beauty. On this Tour West Grand Canyon 3-night motorized trip, you will travel 97 miles from Whitmore Wash SALMON RIVER AND MACKAY BAR LODGE to South Cove on Lake Mead, which features an enjoyable CATARACT CANYON AND RED CLIFFS LODGE 4 night { rowing trip } range of river that includes a variety of exciting rapids 4 night { motorized trip } and tranquil fl owing waters.
Recommended publications
  • 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.
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  • Geologic Map and Upper Paleozoic Stratigraphy of the Marble Canyon Area, Cottonwood Canyon Quadrangle, Death Valley National Park, Inyo County, California
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  • Quantifying the Base Flow of the Colorado River: Its Importance in Sustaining Perennial Flow in Northern Arizona And
    1 * This paper is under review for publication in Hydrogeology Journal as well as a chapter in my soon to be published 2 master’s thesis. 3 4 Quantifying the base flow of the Colorado River: its importance in sustaining perennial flow in northern Arizona and 5 southern Utah 6 7 Riley K. Swanson1* 8 Abraham E. Springer1 9 David K. Kreamer2 10 Benjamin W. Tobin3 11 Denielle M. Perry1 12 13 1. School of Earth and Sustainability, Northern Arizona University, Flagstaff, AZ 86011, US 14 email: [email protected] 15 2. Department of Geoscience, University of Nevada, Las Vegas, NV 89154, US 16 3. Kentucky Geological Survey, University of Kentucky, Lexington, KY 40506, US 17 *corresponding author 18 19 Abstract 20 Water in the Colorado River is known to be a highly over-allocated resource, yet decision makers fail to consider, in 21 their management efforts, one of the most important contributions to the existing water in the river, groundwater. This 22 failure may result from the contrasting results of base flow studies conducted on the amount of streamflow into the 23 Colorado River sourced from groundwater. Some studies rule out the significance of groundwater contribution, while 24 other studies show groundwater contributing the majority flow to the river. This study uses new and extant 1 25 instrumented data (not indirect methods) to quantify the base flow contribution to surface flow and highlight the 26 overlooked, substantial portion of groundwater. Ten remote sub-basins of the Colorado Plateau in southern Utah and 27 northern Arizona were examined in detail.
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  • Cogjm.Pre Film 1963-09-24.Pdf (216.9Kb)
    UNITED STATES DEPARTMENT of the INTERIOR * * * * * * * * * * * * * ********news release BUREAU OF RECLPJ.AATION Peterson - Interior 4662 WATE For Release SEPTEMBER 24, 1963 BUREAU OF RECLAMATION TO PREMIERE NEW~~IN NEVADA DURING PRESIDENT'S VISIT The world premiere of the Bureau ~lamation's new documentary motion held in- Las-Vegas, Nev .. -,--durin President Kennedy's visit there September 28, the Department of the Interior announced today. The 13!-minute 16 mm. color-and-sound film will be shown on a large screen in the Las Vegas Convention Center rotunda immediately preceding the President's address. On his way to Las Vegas during his conservation tour, the President will fly over nearby Hoover Dam, pioneer Reclamation multipurpose structure, and its reservoir, Lake Mead, for an aerial inspection. The dam and reservoir, along with Glen Canyon Dam and Lake Powell, 370 miles upstream, are featured in the film. "Clear Water on the Colorado 11 presents spectacular scenes of the once-muddy and almost inaccessible Colorado River in the canyons of Arizona and southern Utah, now desilted and cleared by Glen Canyon Dam which began storing water March 13, 1963. The film portrays the miracle of a silt-free Colorado River between the headwaters of Lake Mead and the headwaters of Lake Powell. The film points out that Glen Canyon Dam--topped out September 13, 1963, has desilted and cleared the Colorado River just as did Hoover Dam downstream 28 years ago. A tremendous load of sediment, varying from 24 to 270 million tons in different years, has been deposited at the head of Lake Mead since Hoover Dam was closed in 1935.
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  • A Sand Budget for Marble Canyon, Arizona—Implications for Long-Term Monitoring of Sand Storage Change
    A Sand Budget for Marble Canyon, Arizona—Implications for Long-Term Monitoring of Sand Storage Change ecent U.S. Geological Survey Rresearch is providing important insights into how best to monitor changes in the amount of tributary- derived sand stored on the bed of the Colorado River and in eddies in Marble Canyon, Arizona. Before the construction of Glen Canyon Dam and other dams upstream, sandbars in Glen, Marble, and Grand Canyons were replenished each year by sediment- rich floods. Sand input into the Colorado River is crucial to protecting endangered native fish, animals, and plants and cultural and recreational resources along the river in Glen Canyon National Recreation Area and Grand Canyon National Park. View of the Colorado River in Grand Canyon, Arizona, showing sandbars that form downstream from There is longstanding interest in tributary debris fans, which constrict the flow of the river and cause eddies. The view is looking upstream the condition and trend of river-related at a point approximately 217 miles downstream from Glen Canyon Dam. (Photo by Sam Jansen.) resources in and along the Colorado River in Glen Canyon National Recreation Area and Grand Canyons are maintained by occurred because releases of water from and Grand Canyon National Park, Arizona. replenishment of sand that is supplied by Lake Powell are virtually free of sediment. These resources include endangered native tributaries and redistributed by occasional The tributaries that enter the Colorado River fish, native riparian flora and fauna (plants controlled floods released from Lake downstream from the dam supply only a and animals that live along streams), Powell.
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  • Glen Canyon Unit, CRSP, Arizona and Utah
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  • Monitoring the Effects of the Spring 2000 Habitat Maintenance Flow on Colorado River Ecosystem Sand Bars
    Monitoring the Effects of the Spring AMDOR 2000 Habitat Maintenance Flow on N Colorado River Ecosystem Sand Bars Department of Geology Sand Bar Studies Fact Sheet January 2001 1200 The magnitude and timing of controlled floods required to ) s / distribute large amounts of sand into eddies and rebuild eroded sand 3 1000 m bars is a critical objective of research and monitoring in the Colorado ( Powerplant Capacity (940 m3/s) e g River ecosystem, downstream from Glen Canyon Dam. Aggradation r 800 a h Pre-LSSF Spike Flow Post-LSSF Spike Flow of sand bars at higher elevations is dependent on the size and abundance c Measurements Measurements s i 600 of sand temporarily stored on the channel bottom and the duration D s and stage of the high release. New and existing deposits are valued u o 400 components of the riverine ecosystem. They provide habitat for native e n a and non-native fish, the substrate for riparian vegetation, erosion- t n 200 a t protection for archeological sites, and are used for camping by river s n runners. The 1995 Glen Canyon Dam Environmental Impact Statement I 0 March April May June recommends scheduled high releases of short duration be implemented 2000 for environmental purposes (U.S. Department of Interior, 1995). Habitat maintenance flows (HMF) are within powerplant capacity Figure 1. Instantaneous discharge at USGS streamflow gaging station 3 Colorado River at Lees Ferry, Arizona, March-June, 2000. The timing of (~940 m /s), whereas those above this discharge are beach/habitat- measurements made before and after the spring 2000 HMF are shown.
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  • Glen Canyon Report
    The Degraded Reach: Rate and Pattern of Bed and Bank Adjustment of the Colorado River in the 25 km Immediately Downstream from Glen Canyon Dam Paul E. Grams1, John C. Schmidt1, David J. Topping2, and Sara Goeking1 1 Department of Aquatic, Watershed, and Earth Resources, Utah State University 2Water Resources Division, U. S. Geological Survey July 2004 in partial fulfillment of cooperative agreement 1425-98-FC-40-22640 and modifications, between Utah State University and the Grand Canyon Monitoring and Research Center CONTENTS CONTENTS........................................................................................................................ 2 ABSTRACT........................................................................................................................ 4 INTRODUCTION .............................................................................................................. 6 STUDY AREA ................................................................................................................... 7 Physiographic Setting ..................................................................................................... 7 Streamflow Regulation ................................................................................................... 9 Sediment Supply ............................................................................................................. 9 Previous Geomorphic Investigations in Glen Canyon.................................................. 11 METHODS ......................................................................................................................
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  • Chapter 3 – Affected Environment
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  • The Colorado River in Grand Canyon: How Fast Does It Flow?
    Grand Canyon Monitoring and Research Program The Colorado River U.S. Department of the Interior U.S. Geological Survey in Grand Canyon: How Fast Does It Flow? Opening the jet tubes at Glen Canyon Dam on March 26, 1996, released from Lake Powell a con- trolled flood of water that traveled down the Colorado River in Grand Canyon. How fast did the water move? How long did it take for water to reach a particular point along the river? The answers to these questions are important because the speed of river water affects the amount of physical and chemical changes, such as warming by sunlight, that the water will undergo as it moves downstream. Also, very fine particles and substances dissolved in the water travel along with the water, and the speed of the water tells us how fast these move downstream. How is the Water Speed Athough the dye is easy to see where it is first put into the river, it quickly mixes with the much larger mass of river water and becomes invisible. The highest concentration Measured? at sampling sites was between 5 and 35 parts per billion. One part per billion is about equal to one drop in a backyard swimming pool. One way to measure the speed of water is to tag it with a harmless Glen Paria Canyon 114° UTAH ° ° ° substance that is easily identified and 37° 113 112 Ri Dam 111 ve measured with the proper instruments. ARIZONA r River Lees Ferry These substances are called water tracers gin PAGE and are commonly used in both ground Vir water and surface water to track the water movement.
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  • Discovering the Colorado River
    Discovering the Colorado River Main Discovering The New Horizons On The Redefining The River: Lake Page River River Powell Norm Nevills was a hydraulic engineer who in 1936 began white water river expeditions down the San Juan River. In 1940 Nevills led an expedition that included Barry Goldwater down Colorado River through the Grand Canyon. Art Greene and Norm Nevills worked the Colorado River at the same time, touring in different directions. 1940s The Greene Family Collection ACC# 98-1937 3/8 Marble Canyon Lodge which included a lodge, caf�, trading post and dirt airstrip is pictured with the original Navajo Bridge over the Colorado River. Art Greene and family managed the lodge from 1943 to 1949. 1953 Photographer: J. H. McGibbney The Greene Family Collection ACC# 96-1771 Box 4 Album Art Greene (r) with his son-in-law Vern Baker (l) and Roman Hubbell, owner of the Marble Canyon Lodge, seated in the front. Son-in-law Earl Johnson at the helm (not pictured), started the river tour business with Art Greene in 1944. 1940s The Greene Family Collection New Accession First launch of a new airboat, Tseh Na-ni-ah-go Atin' I, at Lee's Ferry was the only airboat used for river trips. Named by Max Johnson. Translated from Navajo: Trail to the rock that goes over. Although the airboat traversed the river well it had drawbacks, such as the noise level and high gasoline consumption. 1947, Photographer: Charles C. Niehuis. The Greene Family Collection ACC# 96-1771 2/9 David and Joyce Muench, and Earl Johnson on a river trip to Forbidden (Aztec) Canyon which is now under water.
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  • Pacific Southwest Water Plan
    United States Department of the Interior Stewart L. Udall, Secretary Pacific Southwest b WATER PLAN = REPOR January 1964 BUREAU OF RECLAMATION Floyd E. Dominy, Commissioner UNITED STATES DEPARTMENT OF THE INTERIOR OFFICE OF THE SECRETARY WASHINGTON 25, D. C. January 21, 1964 8URE#U OF RECLAMATlON The Secretary LOWER COLORAOO REGION LIBRARY of the Int,erior Sir: On November 6, 1963, you directed me to supervise the preparation of a revised report to the President and the Congress proposing, on a regional basis, a plan of action designed to deal constructively with the acute water problems of the Pacific Southwest. The attached report of the Commissioner of Reclamation, in which I concur, was prepared under my direction. As you directed, we have been responsive to the views of the affected States, wherever possible. We have maintained coordination with other divisions of the Department, and considered the views of other Federal agencies. The report outlines a plan of action designed to meet the immediate and long-range water needs of the Pacific Southwest, defined in this report as the water service area of the Lower Colorado River Basin including southern California. It presents an initial plan for approval. We recommend prompt authorization of those features of the initial plan for which adequate engineering and economic investi- gations have been completed. Approval of the basic plan and authorization pf the recommended features will start the Pacific Southwest on the road back to water sufficiency. In 1930 the population of the Pacific Southwest was 3-1/2 million. In 1960 it had grown to 10-1/2 million.
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