7.5' QUADRANGLES, GRAND COUNTY, UTAH by Hellmut H
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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. -
Relation of Sediment Load and Flood-Plain Formation to Climatic Variability, Paria River Drainage Basin, Utah and Arizona
Relation of sediment load and flood-plain formation to climatic variability, Paria River drainage basin, Utah and Arizona JULIA B. GRAF U.S. Geological Survey, Water Resources Division, 375 S. Euclid, Tucson, Arizona 85719 ROBERT H. WEBB U.S. Geological Survey, 1675 W. Anklam Road, Tucson, Arizona 85745 RICHARD HEREFORD U.S. Geological Survey, Geologic Division, 2255 North Gemini Drive, Flagstaff, Arizona 86001 ABSTRACT sediment load for a given discharge declined fill that rises 1-5 m above the modern channel abruptly in the early 1940s in the Colorado bed. Flood-plain deposits are present in all Suspended-sediment load, flow volume, River at Grand Canyon (Daines, 1949; Howard, major tributaries of the Paria River. The area of and flood characteristics of the Paria River 1960; Thomas and others, 1960; Hereford, flood plains is slightly greater than 20 km2, and were analyzed to determine their relation to 1987a). The decline in suspended-sediment sediment volume is estimated to be about 40 climate and flood-plain alluviation between loads has been attributed to improved land use million m3 (Hereford, 1987c). Typically, flood 1923 and 1986. Flood-plain alluviation began and conservation measures initiated in the 1930s plains are not present in first-order drainage ba- about 1940 at a time of decreasing magnitude (Hadley, 1977). A change in sediment-sampler sins but are present in basins of second and and frequency of floods in winter, summer, type and in methods of analysis have been higher order where the stream channel is uncon- and fall. No floods with stages high enough to discounted as causes for the observed decrease fined and crosses nonresistant bedrock forma- inundate the flood plain have occurred since (Daines, 1949; Thomas and others, 1960). -
Utah's Mighty Five from Salt Lake City
Utah’s Mighty Five from Salt Lake City Utah’s Mighty Five from Salt Lake City (8 days) Explore five breathtaking national parks: Arches, Canyonlands, Capitol Reef, Bryce Canyon & Zion, also known as Utah's Mighty 5. You’ll get a chance to explore them all on this 8-day guided tour in southern Utah. Join a small group of no more than 14 guests and a private guide on this adventure. Hiking, scenic viewpoints, local eateries, hidden gems, and other fantastic experiences await! Dates October 03 - October 10, 2021 October 10 - October 17, 2021 October 17 - October 24, 2021 October 24 - October 31, 2021 October 31 - November 07, 2021 November 07 - November 14, 2021 November 14 - November 21, 2021 November 21 - November 28, 2021 November 28 - December 05, 2021 December 05 - December 12, 2021 December 12 - December 19, 2021 December 19 - December 26, 2021 December 26 - January 02, 2022 Highlights Small Group Tour 5 National Parks Salt Lake City Hiking Photography Beautiful Scenery Professional Tour Guide Comfortable Transportation 7 Nights Hotel Accommodations 7 Breakfasts, 6 Lunches, 2 Dinners Park Entrance Fees Taxes & Fees Itinerary Day 1: Arrival in Salt Lake City, Utah 1 / 3 Utah’s Mighty Five from Salt Lake City Arrive at the Salt Lake Airport and transfer to the hotel on own by hotel shuttle. The rest of the day is free to explore on your own. Day 2: Canyonlands National Park Depart Salt Lake City, UT at 7:00 am and travel to Canyonlands National Park. Hike to Mesa Arch for an up-close view of one of the most photographed arches in the Southwestern US. -
Geomorphological Evolution of Phlegrean Volcanic Islands Near Naples, Southern Italy1
Berlin .Stuttgart Geomorphological evolution of Phlegrean volcanic islands near Naples, southern Italy1 by G.AIELLO, D.BARRA, T.DE PIPPO, C.DONADIO, and C.PETROSINO with 9 figures and 5 tables Summary. Using volcanological, morphological, palaeoecological and geoarchaeological data we reconstructed the complex evolution of the island volcanic system of Procida-Vivara, situated west of Naples betweenthe lsland of lschia and the PhlegreanFields, far the last 75 ky. Late Pleistocenemorphological evolution was chiefly controlled by a seriesof pyroclas tic eruptions that resulted in at least eight volcanic edifices, mainly under water. Probably the eruptive centresshifted progressively clockwise until about 18 ky BP when volcanic develop ment on the islands ceased. The presenceof stretches of marine terraces and traces of wave cut notches, both be low and abovè'current sea levels, the finding of exposed infralittoral rnicrofossils, and the identification of three palaeo-surfacesburied by palaeosoilsindicates at least three differen tial uplift phases.These phases interacted with postglacial eustaticfIuctuations, and were sep arated by at least two periods of generai stability in vertical movements. A final phase of ground stability, characterisedby the deposition of Phlegrean and lschia pyroclastics, start ed in the middle Holocene. Finally, fIattened surfacesand a sandy tombolo developedup to the present-day. Recent archaeological surveys and soil-borings at Procida confirm the presence of a lagoon followed by marshland at the back of a sandy tombolo that were formed after the last uplift between the Graeco-Roman periodandthe15di_16dicentury. These areaswere gradu ally filled with marine and continental sedimentsup to the 20di century. ' Finally, our investigation showed that the volcanic sector of Procida-Vivara in the late Pleistocene-Holocenewas affected by vertical displacementswhich were independent of and less marked than the concurrent movement in the adjacent sectors of lschia and of the Phle grean Fields. -
Executive Summary U.S
Glen Canyon Dam Long-Term Experimental and Management Plan Environmental Impact Statement PUBLIC DRAFT Executive Summary U.S. Department of the Interior Bureau of Reclamation, Upper Colorado Region National Park Service, Intermountain Region December 2015 Cover photo credits: Title bar: Grand Canyon National Park Grand Canyon: Grand Canyon National Park Glen Canyon Dam: T.R. Reeve High-flow experimental release: T.R. Reeve Fisherman: T. Gunn Humpback chub: Arizona Game and Fish Department Rafters: Grand Canyon National Park Glen Canyon Dam Long-Term Experimental and Management Plan December 2015 Draft Environmental Impact Statement 1 CONTENTS 2 3 4 ACRONYMS AND ABBREVIATIONS .................................................................................. vii 5 6 ES.1 Introduction ............................................................................................................ 1 7 ES.2 Proposed Federal Action ........................................................................................ 2 8 ES.2.1 Purpose of and Need for Action .............................................................. 2 9 ES.2.2 Objectives and Resource Goals of the LTEMP ....................................... 3 10 ES.3 Scope of the DEIS .................................................................................................. 6 11 ES.3.1 Affected Region and Resources .............................................................. 6 12 ES.3.2 Impact Topics Selected for Detailed Analysis ........................................ 6 13 ES.4 -
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. -
Utah History Encyclopedia
ARCHES NATIONAL PARK Double Arch Although there are arches and natural bridges found all over the world, these natural phenomena nowhere are found in such profusion as they are in Arches National Park, located in Grand County, Utah, north of the town of Moab. The Colorado River forms the southern boundary of the park, and the LaSal Mountains are visible from most viewpoints inside the park`s boundaries. The park is situated in the middle of the Colorado Plateau, a vast area of deep canyons and prominent mountain ranges that also includes Canyonlands National Park, Colorado National Monument, Natural Bridges National Monument, and Dinosaur National Monument. The Colorado Plateau is covered with layers of Jurassic-era sandstones; the type most prevalent within the Park is called Entrada Sandstone, a type that lends itself to the arch cutting that gives the park its name. Arches National Park covers more than 73,000 acres, or about 114 square miles. There are more than 500 arches found inside the park′s boundaries, and the possibility exists that even more may be discovered. The concentration of arches within the park is the result of the angular topography, much exposed bare rock, and erosion on a major scale. In such an arid area - annual precipitation is about 8.5 inches per year - it is not surprising that the agent of most erosion is wind and frost. Flora and fauna in the park and its immediate surrounding area are mainly desert adaptations, except in the canyon bottoms and along the Colorado River, where a riverine or riparian environment is found. -
Tour Options~
14848 Seven Oaks Lane Draper, UT 84020 1-888-517-EPIC [email protected] APMA Annual Scientific Meeting (The National) ~Tour Options~ Zion National Park 1 Day Tour 6-10am Depart Salt Lake City and travel to Zion 10am-5pm Zion National Park We will leave Springdale and head in to the park and enjoy our first hike together up to Emerald Pools. This mild warm up is a beautiful loop trail that will take us along a single track trail, past waterfalls and pools of cool blue water all nesting beneath the massive monolith cliffs of Zion. Afterward we will drive up canyon and walk two trails known as the Riverwalk and Big Bend. The Virgin River, descending from the upper plateau, has worked its way over time through the sandstone carving out the main Zion corridor. You’ll be amazed by the stunning views as we walk along the river. Following these hikes, we will stop for lunch at the Zion Lodge which sits in the park. After lunch, we will drive to the eastern side of the park and through the Carmel Tunnel which was carved out of the solid cliff face in the 1920’s. We will start first at Checkerboard Mesa where you can explore the massive sandstone monoliths. Lastly, we walk along the Overlook Trail until we reach the stunning viewpoint overlooking the entire canyon. 5-6pm Dinner 6-10pm Travel to Salt Lake City Arches National Park 1 Day Tour 6-10am Travel from Salt Lake City to Arches National 10am-5pm Arches National Park In Arches National Park, we begin at the Wall Street trail head. -
The Colorado River a NATURAL MENACE BECOMES a NATIONAL RESOURCE ' '
The Colorado River A NATURAL MENACE BECOMES A NATIONAL RESOURCE ' ' I Comprehensive Report on the Development of ze Water Resources of the Colorado River Basin for rrigation, Power Production, and Other Beneficial Ises in Arizona, California, Colorado, Nevada, New Mexico, Utah, and Wyoming By THE UNITED STATES DEPARTMENT OF THE INTERIOR J . A . Krug, Secretary SPONSORED BY AND PREPARED UNDER THE GENERAL SUPERVISION OF THE BUREAU OF RECLAMATION Michael W. Straus, Commissioner E. A. Morit-, Director, Region 3 ; E. O. Larson, Director, Region 4 MARCH 1 946 1P 'A m 4„ M 1i'leming Library Grand Canyon Colleg P . )x 11097 Contents Page PROPOSED REPORT OF THE SECRETARY OF THE Explorations 46 INTERIOR Settlement 48 Page Population 49 Letter of June 6,1946, from the Acting Commissioner, Chapter III . DIVIDING THE WATER 53 3 Bureau of Reclamation Virgin Conditions 55 REGIONAL DIRECTORS' REPORT Early Development of the River 56 Summary of Conditions in the Early 1920's . 59 Map of Colorado River Basin Facing 9 Between the Upper and Lower Basins 59 Scope and Purpose 9 Between United States and Mexico . 66 Authority for the Report 9 DEVELOPING THE BASIN Cooperation and Acknowledgments 9 Chapter IV. 69 Description of Area 10 Upper Basin 72 Problems of the Basin 11 Labor Force 72 Water Supply 12 Land Ownership and Use 73 Division of Water 13 Soils 73 Future Development of Water Resources 13 Agriculture 73 Table I, Present and Potential Stream Depletions in Minerals and Mining 80 the Colorado River Basin 14 Lumbering 85 Potential Projects 14 Manufacturing 86 Table II, Potential Projects in the Colorado River Transportation and Markets . -
AN INTERNSHIP with the US GEOLOGICAL SURVEY by Justin
ABSTRACT NAMES AND GEOGRAPHIC FEATURES: AN INTERNSHIP WITH THE U.S. GEOLOGICAL SURVEY by Justin Arthur Bedocs Place names are vital to orienting ourselves in the world. In ancient times, people must have had names for places like hunting grounds or berry groves. This act of naming roughly delineates geographic features which can be revisited and described to others, affixing an added cultural meaning to that place. Place naming has since come a long way. Official place names for the United States and its territories are managed by the United States Geological Survey (USGS), National Geospatial Technical Operations Center (NGTOC). This report details my experience working in the Geographic Names Unit. As a Pathways Career Intern, my main duties were to manage the Geographic Names Information System (GNIS), a database containing official place names for features outlined on federal topographic maps. Most of the work involved duplicate names; an issue where there are two name records for one feature, often indicating that one record is a copy and should be deleted. Sometimes the two records were not copies, and the correct locations were identified by visually analyzing historic and recent maps. The coordinates were then updated respectively in the GNIS. I gained valuable experience reading topographic maps, identifying features and managing a large database of geographic names. NAMES AND GEOGRAPHIC FEATURES: AN INTERNSHIP WITH THE U.S. GEOLOGICAL SURVEY An Internship Report Submitted to the Faculty of Miami University in partial fulfillment of the requirements for the degree of Master of Environmental Science by Justin Arthur Bedocs Miami University Oxford, Ohio 2016 Advisor: Robbyn Abbitt, MS Reader: Suzanne Zazycki, JD Reader: Mark Allen Peterson, PhD ©2016 Justin Arthur Bedocs This internship report titled NAMES AND GEOGRAPHIC FEATURES: AN INTERNSHIP WITH THE U.S. -
Canyonlands M National Park the Headquarters Knoll
Unpaved Overlook/ Rapids Boat launch Self-guiding trail Drinking water 2-wheel-drive road Paved road Ranger station Campground Drink one gallon of water per person per Unpaved Trail Locked gate Picnic area Primitive campsite day in this semi-desert 4-wheel-drive road environment. Horseshore Canyon Unit to 70 Moab to 70 and Green River Island in the Sky Visitor Center to 70 30mi 49mi 48km North 79km 45mi ARCHES NATIONAL PARK 73km 191 Visitor L Center A B Moab Y Moab to Areas in the Park R via SR 313 128 0 1 5 Kilometers BOWKNOT I Island in the Sky Visitor Center 32mi/51km N Needles Visitor Center 76mi/121km BEND T N Horseshoe Canyon Unit via I-70 101mi/162km 0 1 5 Miles O H Y 313 Horseshoe Canyon Unit via State 24 119mi/191km N 279 A Hans Flat 133mi/74km C T N G N Moab D I I E O R T Information A A N D P I M N O Center A R O P L L N E L Y O H A MOAB N R 4025ft A E Petroglyphs 1227m C N I Canyonlands M National Park The Headquarters Knoll C A N Y O N G N O L 191 N N Y O Y O N A N Pucker Pass A k C C ree L C A E E R I N O M H ier S arr BIG FLAT Moab to Monticello E B 53mi S Mineral Bottom rail) 85km thief T R (Horse Potash O T R Road I N H U Mineral P O P E F S H I DEAD HORSE POINT E T R S Potash H O STATE PA RK W O N L N Visitor Center O O Horseshoe Y Y Canyon N Unit to 24 A N C RED SEA 32mi Moses and A T A Y L O R FLAT Road C 51km Zeus S Potash F 5920ft C H E Island in the Sky A A I C 1804m N F A Y ER H N Visitor Center O Dead Horse Point Overlook R T B Y N Anticline E U U O 5680ft E S PH N Overlook Upheaval EA C 1731m D R VAL K A il No river access along this 5745ft O S Tra Gooseneck Great Gallery Bottom M E afer portion of Potash Road. -
Copyright Pearson Education Iii
Contents Introduction v The natural environment (Section A) Chapter 1: River environments 1 Chapter 2: Coastal environments 11 Chapter 3: Hazardous environments 21 People and their environments (Section B) Chapter 4: Economic activity and energy 31 Chapter 5: Ecosystems and rural environments 41 Chapter 6: Urban environments 50 Global issues (Section D) Chapter 7: Fragile environments 60 Chapter 8: Globalisation and migration 71 Chapter 9: Development and human welfare 81 Contents Preparing for the exam 91 Glossary Sample 95 Index 99 Copyright Pearson Education iii Geog_Rev_Guide-5thProof.indb 3 22/01/2013 13:29 Chapter 2: Coastal environments The coast as a system The coast is an open system. For example, sediment comes into the system (input) from a river delta. Waves transport the sediment or it is stored in beaches or sand dunes. Sediment may be lost to the coastal system if it moves into the open sea (output). Coastal processes are divided into marine processes (waves) and sub-aerial processes (weathering and mass movement). Waves and erosion and deposition Constructive waves Destructive waves weak tall waves with short swash long wavelength strong swash shallow wavelength gradient steep gradient waves waves h sh as wa ackw ack d) ak b g b de we ron ero st ach beach built up by (be deposition of material brought up in wash (Section A) Figure 2.1 Constructive and destructive waves Constructive waves build the beach by deposition. Destructive waves erode the beach. Their backwash Their swash is stronger than their backwash so they is stronger than their swash, so they drag material carry material up the beach and deposit it there.