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UMNP Mountains Manual 2017
Mountain Adventures Manual utahmasternaturalist.org June 2017 UMN/Manual/2017-03pr Welcome to Utah Master Naturalist! Utah Master Naturalist was developed to help you initiate or continue your own personal journey to increase your understanding of, and appreciation for, Utah’s amazing natural world. We will explore and learn aBout the major ecosystems of Utah, the plant and animal communities that depend upon those systems, and our role in shaping our past, in determining our future, and as stewards of the land. Utah Master Naturalist is a certification program developed By Utah State University Extension with the partnership of more than 25 other organizations in Utah. The mission of Utah Master Naturalist is to develop well-informed volunteers and professionals who provide education, outreach, and service promoting stewardship of natural resources within their communities. Our goal, then, is to assist you in assisting others to develop a greater appreciation and respect for Utah’s Beautiful natural world. “When we see the land as a community to which we belong, we may begin to use it with love and respect.” - Aldo Leopold Participating in a Utah Master Naturalist course provides each of us opportunities to learn not only from the instructors and guest speaKers, But also from each other. We each arrive at a Utah Master Naturalist course with our own rich collection of knowledge and experiences, and we have a unique opportunity to share that Knowledge with each other. This helps us learn and grow not just as individuals, but together as a group with the understanding that there is always more to learn, and more to share. -
Monument Valley Meander
RV Traveler's Roadmap to Monument Valley Meander However you experience it, the valley is a wonder to behold, a harsh yet hauntingly beautiful landscape. View it in early morning, when shadows lift from rocky marvels. Admire it in springtime,when tiny pink and blue wildflowers sprinkle the land with jewel-like specks of color. Try to see it through the eyes of the Navajos, who still herd their sheep and weave their rugs here. 1 Highlights & Facts For The Ideal Experience Agathla Peak Trip Length: Roughly 260 miles, plus side trips Best Time To Go: Spring - autumn What To Watch Out For: When on Indian reservations abide by local customs. Ask permission before taking photos, never disturb any of the artifacts. Must See Nearby Attractions: Grand Canyon National Park (near Flagstaff, AZ) Petrified Forest National Park (near Holbrook, AZ) Zion National Park (Springdale, UT) 2 Traveler's Notes Monument Valley Navajo Tribal Park The stretch of Rte. 163 called the Trail of the Ancients in honor of the vanished Anasazis cuts across Monument Valley at the Utah border on its way to the little town of Mexican Hat. Named for a rock formation there that resembles an upside-down sombrero a whimsical footnote to the magnificence of Monument Valley—Mexican Hat is the nearest settlement to Goosenecks State Park, just ahead and to the west via Rtes. 261 and 316. The monuments in the park have descriptive names. They are based on ones imagination. These names were created by the early settlers of Monument Valley. Others names portray a certain meaning to the Navajo people. -
Reevaluating Evidence for the Pre-Lllinoian Entrenchment of Northeastern Iowa River Valleys
Journal of the Iowa Academy of Science: JIAS Volume 95 Number Article 3 1988 Reevaluating Evidence for the Pre-lllinoian Entrenchment of Northeastern Iowa River Valleys Curtis M. Hudak University of Iowa Let us know how access to this document benefits ouy Copyright © Copyright 1989 by the Iowa Academy of Science, Inc. Follow this and additional works at: https://scholarworks.uni.edu/jias Part of the Anthropology Commons, Life Sciences Commons, Physical Sciences and Mathematics Commons, and the Science and Mathematics Education Commons Recommended Citation Hudak, Curtis M. (1988) "Reevaluating Evidence for the Pre-lllinoian Entrenchment of Northeastern Iowa River Valleys," Journal of the Iowa Academy of Science: JIAS, 95(4), 109-113. Available at: https://scholarworks.uni.edu/jias/vol95/iss4/3 This Research is brought to you for free and open access by the Iowa Academy of Science at UNI ScholarWorks. It has been accepted for inclusion in Journal of the Iowa Academy of Science: JIAS by an authorized editor of UNI ScholarWorks. For more information, please contact [email protected]. ]our. Iowa Acad. Sci. 95(4): 109-113, 1988 Reevaluating Evidence for the Pre-lllinoian Entrenchment of Northeastern Iowa River Valleys 1 CURTIS M. HUDAK2 Department of Geology, University of Iowa, Iowa City, Iowa 52242 Previous workers have proposed a pre-Illinoian age for the deepest bedrock entrenchment of northeastern Iowa valleys. Lines of evidence used ro support a pre-Illinoian age of entrenchment are: ( 1) deep bedrock-entrenchment interpreted ro take "long" periods of time, (2) "valleys" filled with "red-weathered drift", which was interpreted as "old", (3) differences in cross-valley profiles supposedly related to glacial advances, (4) thick beds of gravel could only be deposited by outwash streams, and (5) glacially buried (drift-filled) bedrock valleys exist outside of the Paleozoic Plateau ro the west and south. -
Status and Ecology of Mexican Spotted Owls in the Upper Gila Mountains Recovery Unit, Arizona and New Mexico
Status and Ecology of Mexican Spotted Owls in the Upper Gila Mountains Recovery Unit, Arizona and New Mexico Joseph L. Ganey James P. Ward, Jr. David W. Willey United States Forest Rocky Mountain General Technical Report Department Service Research Station RMRS-GTR-256WWW of Agriculture May 2011 Ganey, Joseph L.; Ward, James P. Jr.; Willey, David W. 2011. Status and ecology of Mexican spotted owls in the Upper Gila Mountains recovery unit, Arizona and New Mexico. Gen. Tech. Rep. RMRS-GTR-256WWW. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 94 p. Abstract This report summarizes current knowledge on the status and ecology of the Mexican spot- ted owl within the Upper Gila Mountains Recovery Unit (UGM RU). It was written at the request of U.S. Forest Service personnel involved in the Four Forests Restoration Initia- tive (4FRI), a collaborative, landscape-scale restoration effort covering approximately 2.4 million ac (1 million ha) across all or part of four National Forests (Apache-Sitgreaves, Coconino, Kaibab, and Tonto National Forests) located within the UGM RU. The UGM RU supports >50% of the known population of Mexican spotted owls, and the central location of the UGM RU within the overall range of the owl appears to facilitate gene flow throughout that range. Consequently, the UGM population is viewed as important to stability within the overall range of the owl, and management that impacts owls within the UGM RU could affect owl populations beyond that RU. Keywords: abundance, demography, habitat selection, diet composition, movements Authors Joseph L. -
The Origin of Comb Ridge
THE ZEPHYR/ JUNE-JULY 2011 THE ORIGIN OF COMB RIDGE Robert Fillmore, Western State College of Colorado in Gunnison, CO (An excerpt and images from his new book: Geological Evolution of the Colorado Plateau) Comb Ridge is a lofty sinuous spine of red sandstone that stretch- ramp of Comb Ridge. Another notable result of this uplift is the es over 80 miles across northern Arizona and southeast Utah. This ensuing deep incision into the uplift by energized rivers as their monocline, as these structures are called, begins near Kayenta and runoff seeks a path to lower elevations. The deep narrow canyons snakes northward to fade away near the west flank of the Abajo of Cedar Mesa owe their existence to Monument Upwarp. Mountains. Monoclines are a peculiar component of the Colorado Plateau, with their long ridges of steeply tilted strata in a region otherwise known for its miles of flat-lying sedimentary rocks. They Monoclines are a peculiar component are hard to miss. Although not confined to the Colorado Plateau, of the Colorado Plateau, with their long ridges their concentration here is unique. Similar structures make up the of steeply tilted strata in a region San Rafael Swell, Capitol reef, and Colorado National monument otherwise known for its miles of near Grand Junction. All are closely related in origin and timing. flat-lying sedimentary rocks. They are hard to miss. The term monocline refers to a single-limbed fold; in simple geometric terms, a gargantuan ramp. The ramp of steeply tilted strata separates uplifted regions from those that have dropped The monoclines formed at the same time as the jagged Rocky downwards, relatively speaking. -
Historical Geomorphology of the Verde River
Historical Geomorphology of the Verde River by Philip A. Pearthree Arizona Geological Survey Open-File Report 96-13 June, 1996 Arizona Geological Survey 416 W. Congress, Suite #100, Tucson, Arizona 85701 Research conducted in cooperation with CH2MHILL as part of the basic data collection for assessment of river navigability in Arizona at the time of Statehood (1912 J. Funding was provided by the Arizona State Land Department This report is preliminary and has not been edited or reviewed for conformity with Arizona Geological Survey standards Introduction The Verde River drainage is a major river system that heads in Big Chino Valley in north central Arizona, flows generally southeast through the rugged terrain of central Arizona, and empties into the Salt River east of the Phoenix metropolitan area. It is unusual in Arizona because much the main channel of the Verde River is perennial for much its length. Data summarized in this report were gathered to aid in the assessment of the navigability of the Verde River in February, 1912, when Arizona became a State. These investigations were conducted in cooperation with CH2MHill and were funded by the Arizona State Land Department. The purposes of this report are to (1) outline the geologic and geomorphic framework of the Verde River, (2) to describe the physical character of the channel of the Verde River, and (3) to evaluate how channel morphology and position have changed in the past century. Physiography, Geology, and General Geomorphology of the River The Verde River heads in and flows through the rugged highlands and valleys of central Arizona (Figure 1). -
N Red Rock Beauty N Salt Lake City N Outdoor Adventure N Dinosaurs
n Red Rock Beauty n Salt Lake City n Outdoor Adventure n Dinosaurs Plus: Arts, Winter Sports, Golf A SPECIAL SUPPLEMENT TO THE JANUARY 2009 ISSUE OF When you come to Utah, visit TEMPLE SQUARE In the heart of Salt Lake City many venues to choose from... All are Free Brigham Young Historic Park Church Office Building State Street Conference Center Relief Society Building Main Street Lion House and Beehive House North Temple Street Salt Lake Temple Joseph Smith Memorial Building West Temple Street North Visitors' Center Tabernacle South Temple Street South Visitors' Center Museum of Church History and Art Assembly Hall Family History Library Hear the world-famous Mormon See the magnificent spires of the Find your roots in the world’s Tabernacle Choir. Salt Lake Temple. largest collection of genealogical information. Enjoy the imposing 11-foot marble Christus statue at the North Visitors' Center. For information, go to visittemplesquare.com, lds.org/placestovisit, or call 1-800-537-9703 For information about The Church of Jesus Christ of Latter-day Saints, visit mormon.org © 2008 by IRI. 7/08. Printed in the USA. 04089. Illustration of Temple Square by Dilleen Marsh © 1999 IRI. Photo of Mormon Tabernacle Choir © 2001 Busath Photography UTAH Life Elevated Utah. 4 Life Elevated Northern Utah. 8 Salt Lake, Dinosaurland & Everything Inbetween Central Utah . 14 Nordic Traditions & Outdoor Wilderness Southwestern Utah . 16 National Parks, Western History & Rugged Beauty Southeastern Utah . 22 Dinosaurs, Swells & Desert Beauty UTAH – A SPECIAL SUPPLEMENT TO THE JANUARY 2009 ISSUE OF CANADIAN TRAVELLER Published 12 times a year by 88 East Pender Street, Suite 555 Vancouver, BC Canada, V6A 3X3 Contents © 2009 by ACT Communications Inc. -
Creating Memorable Travel Experiences Since 1979 2021
2021 DREAM BOOK LLC CREATING MEMORABLE TRAVEL EXPERIENCES SINCE 1979 One from the Road… When we returned to the road in August, one of our first trips was By the end of the tour, you feel like you just watched Ellen, Dr. Phil across Nevada to pick up the historic (which later and Saturday Night Live. You have truly met the locals once you Lincoln Highway SUCCESS STORIES—A SpECIAl AdvERTISIng SECTIOn became U.S. 50) and make our way back to Sacramento. Small finish walking among the headstones. towns proved to be a good way to gently try and return to traveling. Sure, we would all I didn’t know Wally would even be in town. Last I heard he was prefer not to have to wear a mask and wash buying a camper and heading out to see the world when he retired. our hands every 20 minutes. But if you love For reasons I’m hopeful I’ll hear about some day, he was back in to travel, right now you have to make a few Eureka. compromises. With any luck, those will be short term and we will be able to travel more It’s possible the folks on the trip may have noticed the tear in my eye freely soon. or the crack in my voice when my friend showed up to say hi. Or when he starting telling a couple members of our group about the Our trip went well. We slipped in and out of a cemetery tour and I broke out laughing really loud. -
How Great Were Cedar Mesa Great House Communities, A.D
HOW GREAT WERE CEDAR MESA GREAT HOUSE COMMUNITIES, A.D. 1060-1270? By NATALIE ROCHELLE FAST A thesis submitted in partial fulfillment of the requirements for the degree of MASTER OF ARTS IN ANTHROPOLOGY WASHINGTON STATE UNIVERSITY Department of Anthropology MAY 2012 To the Facultyof WashingtonState University: The membersof the Committeeappointed to examinethe thesisof NATALIE ROCHELLE FAST flnd it satisfactoryand recommendthat it be accepted. WilliamD. Lipe,Ph.D. *p,a/2/a R.G.Matson. Ph.D. ACKNOWLEDGEMENTS I owe many thanks to the numerous people and organizations who assisted and supported my work on the Cedar Mesa Cultural Landscapes Survey and this thesis. First and foremost, I would like to thank my thesis committee, Drs. Andrew Duff, Bill Lipe, and R.G. Matson. Their thoughtful guidance and time spent discussing ideas with me has been invaluable. I thank Andrew for his consistent encouragement, and Bill and R.G. for sharing their immense knowledge of all things Cedar Mesa with me. Allowing me to tap into the 40-plus years of their work on Cedar Mesa is an honor. Many years have led me to this point, and I cannot forget to thank the people who guided me here. First, to Drs. Ruth Van Dyke and Richard Wilshusen, who showed me the wonderful world of archaeology in the Southwest, and especially to Rich, who gently turned me toward work in the Mesa Verde region. At the Anasazi Heritage Center and Canyons of the Ancients National Monument, I would like to thank Tracy Murphy and Linda Farnsworth, who gave me my first real jobs in curation and archaeology- their wisdom has shaped my knowledge of archaeology in the Four Corners to this day. -
1 August 26, 2019 Sent Via E-Planning and Overnight Mail
August 26, 2019 Sent via e-Planning and overnight mail Director (210) Attention Protest Coordinator, WO-210 P.O. Box 71383 Washington D.C. 20024-1383 Re: Protest of the Bears Ears National Monument Indian Creek and Shash Jáa Units Proposed Monument Management Plans and Final Environmental Impact Statement Please accept this protest of the Bureau of Land Management’s Bears Ears National Monument (BENM) Indian Creek and Shash Jáa Units Proposed Monument Management Plans and Final Environmental Impact Statement (MMP/FEIS), submitted by the Access Fund, Archaeology Southwest, Conservation Lands Foundation, Friends of Cedar Mesa, National Trust for Historic Preservation, Society for Vertebrate Paleontology and Utah Diné Bikéyah (Protesting Parties or Protestors). The Protesting Parties incorporate by reference the points and arguments raised in the protests filed by the Wilderness Society (and their partners), as well as by any tribes or tribally affiliated organizations. INTERESTS AND INVOLVEMENT OF THE PARTIES The Access Fund is a national advocacy organization whose mission keeps climbing areas open and conserves the climbing environment. A 501(c)(3) non-profit supporting and representing over 7 million climbers nationwide in all forms of climbing—rock climbing, ice climbing, mountaineering, and bouldering—the Access Fund is the largest US climbing organization with nearly 20,000 members and 120 affiliates. We currently hold memorandums of understanding1 with the Bureau of Land Management, National Park Service, and Forest Service to work together regarding how climbing is managed on federal land. The Access Fund provides climbing management expertise, stewardship, project specific funding, and educational outreach for climbing areas across the country including the BENM region, and Utah is one of our largest member states. -
Bears Ears National Monument: Monument Management Plans And
U.S. Department of the Interior U.S. Department of Agriculture Bureau of Land Management U.S. Forest Service Bea rs Ears National Monument: Mon ument Management Plans and Environmental Impact Statement Sha sh Jaá and Indian Creek Units Scopi ng Report August 2018 CONTENTS 1 Introduction .............................................................................................................................................. 1 2 Scoping Process ....................................................................................................................................... 3 2.1 Purpose of Scoping ........................................................................................................................... 3 2.2 Scoping Outreach .............................................................................................................................. 3 2.2.1 Publication of the Notice of Intent ....................................................................................... 3 2.2.2 Other Outreach Methods ....................................................................................................... 3 2.3 Opportunities for Public Comment ................................................................................................ 3 2.4 Public Scoping Meetings .................................................................................................................. 4 2.5 Cooperating Agency Involvement .................................................................................................. -
Utah Geology: Making Utah's Geology More Accessible. View South-East
5/28/13 Utah Geology: Geologic Road Guides Utah Geology: Making Utah's geology more accessible. View south-east over St. George, Utah Road Guide Quick Select. Selection Map HW-160, 163 & 191 Tuba City to Kayenta, Bluff & Montecello, Utah (through Monument Valley) 0.0 Junction of U.S. Highways 160 and 89 , HW-160 Road Guide. follows U.S. Highway 160 east toward Tuba city and Kayenta. U.S. Highway 89 leads south toward the entrance to Grand Canyon National Park and Flagstaff. For a route description along U.S. Highway 89 northward from here see HW-89A Road Guide.. The road junction is in the Petrified Forest Member of the Chinle Formation. The member is composed of interbedded stream channel sandstone and varicolored shale and mudstone. This member erodes moderately easily and forms the strike valley to the north and south. From here the route of this guide leads upsection into younger and younger beds of the Chinle Formation. 0.7 Cross Hamblin Wash and rise from the Petrified Forest Member into the pinkish banded Owl Rock Member of the Chinle Formation. The upper member forms pronounced laminated pinkish gray and green badlands, distinctly unlike the rounded Painted Desert-type massive badlands of the underlying member. 1.6 Road rises up through the upper part of the Chinle Formation, a typical wavy to hummocky road. Highway construction is easy across the slope-forming parts of the formation, but holding the road after construction is difficult because the soft volcanic ash-bearing shales heave under load or after wetting and drying.