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2009Nature Notes Vol. 9, No. 3 RH Final.Pub
Zion National Park News National Park Service U.S. Department of the Interior Nature Notes The Lush Desert High noon. A blazing sun burns rippling waves of heat across the sandy earth making the distance appear almost fluid. Tumble- weeds bounce over the land past bare bones, bleached white, crisp, and brittle in the scorching sun. Flies buzz past. A small group of turkey vultures peck at coyote carrion. A dry wind blows any sense of well-being away, and even the air smells empty. This is the desert. What Mary Austin called “a land of little rain” is an environment that often seems forbidding. We perceive these lands with words in mind such as harsh, barren, unin- viting, and scarce. Yet in the desert that is Zion National Park, people have been living for thousands of years. The plant life in Zion, at first glance, may also seem harsh and mini- The abundant medicinal and edible uses of the prickly pear cactus and datil yucca hide behind the malistic—certainly anything but lush. In dig- plants' defensive spines and sharp tips. Photo by Sally Wier ging deeper, however, we see that these plants, so symbolic of the desert, are a key encounter with a skunk. The strongly candies, and syrups. Supporting pads of the part of what has made this place a home to scented smoke not only cleansed humans of cacti, though intimidating to the touch, are humans for so long. surface odors, it had the ability to cleanse the a rich resource as well. Once rid of their soul as well. -
How It Works: 1
Join us as Team Challenge San Diego takes on Zion National Park this spring! Whether you’re an experienced camper, or you’ve never hiked before in your life, our coach and team manager will have you ready to experience the natural beauty at Angel’s Landing and The Narrows— two iconic destinations in Utah’s first National Park! What’s Included? • 6-week training plan and coach support • 3 in-person group training hikes in San Diego • Professional fundraising support, including your own personal fundraising website • Full-time staff support to help you reach your goals • Campsite reservation at Zion National Park (May 10-12, 2019) • Team Challenge inspirational campfire • Team Challenge finisher patch How it works: 1. Register: It’s only $25 to reserve your spot** to hike Zion National Park with Team Challenge, but you have an upfront commitment to reach the minimum fundraising goal of $500/person. **Any participant or guest under the age of 18 will be required to be accompanied by a parent/guardian for the entirety of the weekend. All participants and guests are required to sign our Team Challenge waiver. 2. Fundraise: Ask your friends and family to donate! You will have until April 30th to raise your goal—any remaining balance at that time will be charged to your credit card on file, as a self-donation to the Crohn’s & Colitis Foundation. 3. Train: You will receive a training plan from your coach that you can use at home/at your gym. Participation at our 3 Sunday group trainings is highly encouraged, so you can meet your teammates and staff, as well as prepare for our weekend at Zion National Park. -
Proquest Dissertations
REGIONAL CORRELATION OF DIAGENETIC COLORATION FACIES AND ANALYSIS OF IRON OXIDE CEMENTATION PROCESSES, JURASSIC NAVAJO SANDSTONE, SOUTHWESTERN UTAH by Gregory Barry Nielsen A dissertation submitted to the faculty of The University of Utah in partial fulfillment of the requirements for the degree of Doctor of Philosophy in Geology Department of Geology and Geophysics The University of Utah May 2010 UMI Number: 3407485 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. In the unlikely event that the author did not send a complete manuscript and there are missing pages, these will be noted. Also, if material had to be removed, a note will indicate the deletion. JLJMT Dissertation Publishing UMI 3407485 Copyright 2010 by ProQuest LLC. All rights reserved. This edition of the work is protected against unauthorized copying under Title 17, United States Code. ProQuest LLC 789 East Eisenhower Parkway P.O. Box 1346 Ann Arbor, Ml 48106-1346 Copyright © Gregory Barry Nielsen 2010 All Rights Reserved The Graduate School u THE UNIVERSITY OF UTAH SUPERVISORY COMMITTEE APPROVAL of a dissertation submitted by Gregory Barry Nielsen This dissertation has been read by each member of the following supervisory committee and by a majority vote has been found to be satisfactory. 3-/-7-/d ' y^u/U^^/iC Date Chair: Marforie A. Chan 2-IG'ZOlO £*M &b Date Erich U. Petersen 3M'S? -'ZPIO osLj^tu? Date Allan A. Ekdale ?-<3o-,o Date *W2o(Q, Date Brenda Beitler Bowen The Graduate School u THE UNIVERSITY OF UTAH FINAL READING APPROVAL To the Graduate Council of the University of Utah: I have read the dissertation of Gregory Barry Nielsen in its final form and have found that (1) its format, citations, and bibliographic style are consistent and acceptable; (2) its illustrative materials including figures, tables, and charts are in place; (3) the final manuscript is satisfactory to the supervisory committee and is ready for submission to The Graduate School. -
Zion Scenic Byway Interpretive Plan FINAL
Zion Scenic Byway Interpretive Plan FINAL Prepared for: Zion Canyon Corridor Council February, 2015 i Table of Contents Acknowledgements ................................................................................................................................................... iv 1. Introduction and Project Overview........................................................................................................................ 1 Partners and Stakeholders ................................................................................................................................. 3 Interpretive Plan Process.................................................................................................................................... 4 2. Research and Gathering Existing Data ................................................................................................................... 5 “Listening to Springdale - Identifying Visions for Springdale” Project .................................................................. 5 Interpretive Sites Field Review ........................................................................................................................... 6 Other Coordination ............................................................................................................................................ 6 3. Marketing and Audience Analysis.......................................................................................................................... 7 Zion Scenic Byway Corridor -
Diagenetic Coloration Facies and Alteration History of the Jurassic Navajo Sandstone, Zion National Park and Vicinity, Southwestern Utah
DIAGENETIC COLORATION FACIES AND ALTERATION HISTORY OF THE JURASSIC NAVAJO SANDSTONE, ZION NATIONAL PARK AND VICINITY, SOUTHWESTERN UTAH Gregory B. Nielsen, Marjorie A. Chan, and Erich U. Petersen Department of Geology and Geophysics University of Utah 115 S. 1460 E., Rm. 383 FASB Salt Lake City, Utah 84112-0102 [email protected] [email protected] [email protected] ABSTRACT Coloration patterns in the Jurassic Navajo Sandstone of Zion National Park and vicinity are examined using a broad variety of geochemical, geospatial, petrographic, and bedform analysis techniques. Six diagenetic coloration facies (including 12 subfacies) are defined and characterized. Results indicate a prolonged and complex diagenetic history with variations in color resulting largely from changes in the concentration and distri- bution of iron oxides. In the northern Kolob Plateau, the Navajo Sandstone has a uniform red pigmentation (red primary facies) that formed during early diagenesis to produce the “primary” sandstone color. In contrast, Navajo Sandstone of main Zion Canyon displays “secondary” alteration features occurring in three distinct vertical coloration facies: brown (lower), pink (middle), and white (upper). The white and pink facies in Zion Canyon are characterized by a combination of prevalent bleaching, areas of remnant “primary” sandstone, and small concretionary iron-enriched lenses. Bleaching is concentrated in the upper Navajo Sandstone where alteration occurred during middle diagenesis (deep burial). Widespread bleaching and alteration in Zion Canyon terminates abruptly in the central park but narrow, well-defined, white bleached bands locally follow high-permeability beds northward for several kilometers into the red-colored Kolob Plateau (red/white facies). The brown facies is characterized by widespread dark iron oxide cement concentrations precipitated beneath a well-defined subhorizontal boundary. -
Zion National Park Which Stirs the Imagination with a Singular Power ...’ Clarence E Dutton
‘There is an elegance to their forms Zion National Park which stirs the imagination with a singular power ...’ Clarence E Dutton Towers of the Virgin 91 Heaven on earth As we set out from Springdale, dawn was bathing the spires of the West Temple, The Sentinel and the Towers of the Virgin in a golden, glowing light. It augured well for a day when we were going to explore the inner sanctuaries of Zion, the 15-mile-long, half-mile-deep canyon cut into the Kayenta and Navajo sandstones of the Colorado Plateau. Formed over millions of years by the uplift of the surrounding plateau, aided by the tremendous erosive power of the North Fork of the Virgin River, Zion Canyon was named by the first Mormon settler, Isaac Behunin in the mid-19th century. It was the nearest thing to heaven that he had seen, so he named it after the city of his God. The exalted names given to the golden, red and white sandstone walls and bristling peaks reflect the reverential awe in which they were held by those first visitors: East and West Temples, Great White Throne, Altar of Sacrifice, Court of the Patriarchs, Organ, Pulpit and the vertiginous viewpoint of Angel’s Landing. The latter, a 5790-foot-high spur which hangs over the Upper Canyon, was given its celestial name by a Methodist minister, the Rev Frederick Vining Fisher on a day trip in 1916, after one of his companions had commented: ‘only an angel could land on it’. Angel’s Landing on the north western rim of the canyon was our destination, and we set off from the site of Behunin’s log cabin at Zion Lodge along the river to The Grotto, and over the sturdy metal footbridge across the rushing waters of the Virgin River. -
Wilderness Guide
National Park Service Zion National Park U.S. Department of the Interior Wilderness Guide The official wilderness guide of Zion National Park 2016-2017 Plan Your Trip Wilderness Permit Hours Zion Canyon Visitor Center Kolob Canyons Visitor Center Welcome to Zion National Park. Zion is a spectacular network of 435 772-0170 435 586-9548 colorful canyons, forested mesas, and striking deserts. All of the land within the park boundary is preserved by the National Park Service for March 5 to April 16 8:00 am to 5:00 pm 8:00 am to 5:00 pm the benefit of the public. In addition, a remarkable 84 percent of this 7:00 am to 6:00 pm 8:00 am to 5:00 pm extraordinary landscape is preserved as wilderness. This designation April 17 to May 27 ensures that over 124,000 acres of the park will continue to be a place May 28 to September 5 7:00 am to 7:30 pm 8:00 am to 6:00 pm where nature and its “community of life are untrammeled by man, a place where man himself is a visitor who does not remain.” September 6 to September 25 7:00 am to 6:00 pm 8:00 am to 6:00 pm September 26 to October 8 7:00 am to 6:00 pm 8:00 am to 5:00 pm PREPARE AND PLAN AHEAD October 9 to November 26 8:00 am to 5:00 pm 8:00 am to 4:30 pm Traveling into the wilderness, even on short November 27- March 2017 8:00 am to 4:30 pm 8:00 am to 4:30 pm trips, can be challenging Permits are required for overnight trips in the wilderness, including climbing bivouacs, through- and risky and requires careful planning hikes of The Narrows and its tributaries, and canyons requiring the use of descending gear or before you begin. -
Winter 2004/2005
Park Planner National Park Service U.S. Department of the Interior The official planner of Zion National Park Zion Map & Guide Winter 2004/2005 Planning Your Winter Visit What’s Inside Information and Services . .2 BE PREPARED FOR A WIDE RANGE OF WEATHER CONDITIONS. SNOW Clear days may become quite warm, reaching 60°F; nights are conditions and temperatures vary at different elevations. often in the 20s and 30s. Winter storms can last several days and Hiking . .3 cause roads to be icy. Be prepared for winter driving conditions Fall days are usually clear and mild; nights are often cold. Fall color from November through March. Weather . .3 displays begin in September in the high country and peak in Zion Canyon by late October. Spring is unpredictable. Stormy, wet days are common, but warm, Maps & Trail sunny weather may also occur. Precipitation peaks in March. The Guide . 4-5 Winters in Zion Canyon are fairly mild. Storms bring rain or light spring wildflower bloom usually starts in April. snow to the canyon, but heavier snow to the higher elevations. Park Profile . .6 Zion Canyon Field Making The Most of Your Time Institute Classes . .7 Tunnel Information. .8 Drives Visitor Centers Winter Hiking The shuttle system does not operate in Zion Canyon Visitor Center Hikers should be flexible and plan to turn Large Vehicle winter. It will begin again in April. The Zion At the south entrance; across the river back if trail conditions are unsafe or falling Restrictions . .8 Canyon Scenic Drive is open to private from Springdale. Exhibits and a three- ice is a hazard. -
The Far Side of the Sky
The Far Side of the Sky Christopher E. Brennen Pasadena, California Dankat Publishing Company Copyright c 2014 Christopher E. Brennen All rights reserved. No part of this publication may be reproduced, transmitted, transcribed, stored in a retrieval system, or translated into any language or computer language, in any form or by any means, without prior written permission from Christopher Earls Brennen. ISBN-0-9667409-1-2 Preface In this collection of stories, I have recorded some of my adventures on the mountains of the world. I make no pretense to being anything other than an average hiker for, as the first stories tell, I came to enjoy the mountains quite late in life. But, like thousands before me, I was drawn increasingly toward the wilderness, partly because of the physical challenge at a time when all I had left was a native courage (some might say foolhardiness), and partly because of a desire to find the limits of my own frailty. As these stories tell, I think I found several such limits; there are some I am proud of and some I am not. Of course, there was also the grandeur and magnificence of the mountains. There is nothing quite to compare with the feeling that envelopes you when, after toiling for many hours looking at rock and dirt a few feet away, the world suddenly opens up and one can see for hundreds of miles in all directions. If I were a religious man, I would feel spirits in the wind, the waterfalls, the trees and the rock. Many of these adventures would not have been possible without the mar- velous companionship that I enjoyed along the way. -
Mineral Resources of the Canaan Mountain and the Watchman Wilderness Study Areas, Washington and Kane Counties, Utah
Mineral Resources of the Canaan Mountain and The Watchman Wilderness Study Areas, Washington and Kane Counties, Utah U.S. GEOLOGICAL SURVEY BULLETIN 1746-A r UTAH -.S***' f. Jf .^^^-^^ s^w^*2^ ^;»a**?P!P*l :rj^4^ ^S^P^ :"¥>. \ * .3 %- ^4- * ^ s CHAPTER A Mineral Resources of the Canaan Mountain and The Watchman Wilderness Study Areas, Washington and Kane Counties, Utah By R.E. VAN LOENEN, E.G. SABLE, H.R. BLANK, Jr., and R.L TURNER U.S. Geological Survey T.J. KREIDLER and J.E. ZELTEN U.S. Bureau of Mines K.L. COOK University of Utah U.S. GEOLOGICAL SURVEY BULLETIN 1746 MINERAL RESOURCES OF WILDERNESS STUDY AREAS-SOUTHWESTERN UTAH DEPARTMENT OF THE INTERIOR DONALD PAUL MODEL, Secretary U. S. GEOLOGICAL SURVEY Dallas L. Peck, Director UNITED STATES GOVERNMENT PRINTING OFFICE: 1988 For sale by the Books and Open-File Reports Section U.S. Geological Survey Federal Center Box 25425 Denver, CO 80225 Library of Congress Cataloging-in-Publication Data Mineral resources of the Canaan Mountain and the Watchman Wilderness Study Areas, Washington and Kane Counties, Utah. (U.S. Geological Survey bulletin ; 1746-A) (Mineral resources of wilderness study areas southwestern Utah and part of adjacent Mohave County, Arizona ; ch. A) Bibliography: p. 1. Mines and mineral resources Utah Canaan Mountain Wilderness. 2. Mines and mineral resources Utah Watchman Wilderness. 3. Canaan Mountain Wilderness (Utah). 4. Watchman Wilderness (Utah) I. Van Loenen, Richard E. II. Series. III. Series: Mineral resources of wilderness study areas southwestern Utah and part of adjacent Mohave County, Arizona ; 1746-A. QE75.B9 no. -
The Colorado Plateau
The Colorado Plateau An OUGS Severnside Field Trip 2015 The Colorado Plateau 2015 Introduction This was to be another Severnside trip, but one with a new organiser! Janet Hiscott and Tom Sharpe had devised the idea for this trip when talking about what he would do in his retirement from the Museum of Wales. The large group of 27 members that collected in Denver at the end of September 2015 were the beneficiaries of this chat. We were all eager to explore the Colorado Plateau with Janet and Tom to guide us. The Colorado Plateau is an area between the Rockies and the Basin and Range Province and extends through parts of 4 states, Utah, Colorado, New Mexico and Arizona. (Fig. 1) It contains some of the most famous and most visited National Parks of the USA and we were here for 17 days to be introduced to the geology, paleontology and human interaction with and exploitation of the region. The Rockies have been through several cycles of uplift and erosion since the Precambrian, the most recent period of uplift started 5Ma ago and the area has seen a change in elevation of 5000ft. There was associated volcanic activity, building volcanoes and causing a redistribution of metals by heated fluids. The latter having been exploited by man in the Colorado Mineral Belt. The debris eroded from the Rockies during these successive periods of upift was deposited in the plains surrounding them. These sediments, and marine deposits from a period of inundation by an inland sea, form the level beds that comprise the Colorado plateau. -
Changing Landscapes Fifth Grade Pre- and Post-Visit Activity Guide
National Park Service U.S. Department of the Interior Zion National Park Utah Changing Landscapes Fifth Grade Pre- and Post-Visit Activity Guide NPS/MARC NEIDIG Changing Landscapes Fifth Grade Pre- and Post-Visit Activity Guide Zion National Park Springdale, Utah 84767 Contents Introduction 1 Core Connections 1 Background 1 Pre-Visit Activities 3 Earth’s Power Punches 3 Rock On Zion! 4 Then and Now 6 Post-Visit Activities 8 Map Minds 8 It Happened Here! 9 Future Forecasters 11 Glossary 12 References 14 Introduction Background Theme Zion National Park is located along the edge The Earth’s surface is a dynamic system that is of a region called the Colorado Plateau. Uplift, constantly changing due to weathering, tilting, and the erosion of rock layers formed erosion, earthquakes, volcanoes, and uplift. a feature called the Grand Staircase, a series of colorful cliffs stretching between Bryce Focus Canyon, Zion, and the Grand Canyon. The activities focus on relationship between NPS PHOTO geologic processes and changes on the Earth’s Zion has spectacular geology. The arid climate surface. and sparse vegetation expose bare rock and reveal the park’s geologic history. Evidence Pre-Visit Activities of deposition (sedimentation), lithification, 1. Earth’s Power Punches – Students view a uplift, weathering, erosion, tectonics, and presentation of digital images showing the volcanic activity make the park a showcase for forces that shape the Earth’s surface. Then changing landscapes. students view images from Zion and deter- mine which geologic forces have contributed Deposition (Sedimentation) to the landscapes shown. Finally, students Zion National Park was a relatively flat basin discuss which landscapes were formed slowly near sea level 275 million years ago, near the NPS PHOTO and which were formed quickly.