Kayenta Township Comprehensive Plan
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Narbonapass.Pdf
FIRST-DAY ROAD LOG 1 FIRST-DAY ROAD LOG, FROM GALLUP TO GAMERCO, YAH-TA-HEY, WINDOW ROCK, FORT DEFIANCE, NAVAJO, TODILTO PARK, CRYSTAL, NARBONA PASS, SHEEP SPRINGS, TOHATCHI AND GALLUP SPENCER G. LUCAS, STEVEN C. SEMKEN, ANDREW B. HECKERT, WILLIAM R. BERGLOF, First-day Road Log GRETCHEN HOFFMAN, BARRY S. KUES, LARRY S. CRUMPLER AND JAYNE C. AUBELE ������ ������ ������ ������� ������ ������ ������ ������ �������� Distance: 141.8 miles ������� Stops: 5 ���� ������ ������ SUMMARY ������ �� ������ �� ����� �� The first day’s trip takes us around the southern �� �� flank of the Defiance uplift, back over it into the �� southwestern San Juan Basin and ends at the Hogback monocline at Gallup. The trip emphasizes Mesozoic— especially Jurassic—stratigraphy and sedimentation in NOTE: Most of this day’s trip will be conducted the Defiance uplift region. We also closely examine within the boundaries of the Navajo (Diné) Nation under Cenozoic volcanism of the Navajo volcanic field. a permit from the Navajo Nation Minerals Department. Stop 1 at Window Rock discusses the Laramide Persons wishing to conduct geological investigations Defiance uplift and introduces Jurassic eolianites near on the Navajo Nation, including stops described in this the preserved southern edge of the Middle-Upper guidebook, must first apply for and receive a permit Jurassic depositional basin. At Todilto Park, Stop 2, from the Navajo Nation Minerals Department, P.O. we examine the type area of the Jurassic Todilto For- Box 1910, Window Rock, Arizona, 86515, 928-871- mation and discuss Todilto deposition and economic 6587. Sample collection on Navajo land is forbidden. geology, a recurrent theme of this field conference. From Todilto Park we move on to the Green Knobs diatreme adjacent to the highway for Stop 3, and then to Stop 4 at the Narbona Pass maar at the crest of the Chuska Mountains. -
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. -
Hydrogeology of the Chinle Wash Watershed, Navajo Nation Arizona, Utah and New Mexico
Hydrogeology of the Chinle Wash Watershed, Navajo Nation Arizona, Utah and New Mexico Item Type Thesis-Reproduction (electronic); text Authors Roessel, Raymond J. Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 07/10/2021 19:50:22 Link to Item http://hdl.handle.net/10150/191379 HYDROGEOLOGY OF THE CHINLE WASH WATERSHED, NAVAJO NATION, ARIZONA, UTAH AND NEW MEXICO by Raymond J. Roessel A Thesis Submitted to the Faculty of the DEPARTMENT OF HYDROLOGY AND WATER RESOURCES In Partial Fulfillment of the Requirements For the Degree of MASTER OF SCIENCE WITH A MAJOR IN HYDROLOGY In the Graduate College THE UNIVERSITY OF ARIZONA 1994 2 STATEMENT BY AUTHOR This thesis has been submitted in partial fulfillment of requirements for an advanced degree at The University of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Library. Brief quotations from this thesis are allowable without special permission, provided that accurate acknowledgment of source is made. Requests for permission for extended quotation from or reproduction of this manuscript in whole or in part may be granted by the head of the major department or the Dean of the Graduate College when in his or her judgment the proposed use of the material is in the interests of scholarship. In all other instances, however, permission must be obtained from the author. -
The Moenave Formation: Sedimentologic and Stratigraphic Context of the Triassic–Jurassic Boundary in the Four Corners Area, Southwestern U.S.A
Palaeogeography, Palaeoclimatology, Palaeoecology 244 (2007) 111–125 www.elsevier.com/locate/palaeo The Moenave Formation: Sedimentologic and stratigraphic context of the Triassic–Jurassic boundary in the Four Corners area, southwestern U.S.A. ⁎ Lawrence H. Tanner a, , Spencer G. Lucas b a Department of Biology, Le Moyne College, 1419 Salt Springs Road, Syracuse, NY 13214, USA b New Mexico Museum of Natural History, 1801 Mountain Road, N.W., Albuquerque, NM 87104, USA Received 20 February 2005; accepted 20 June 2006 Abstract The Moenave Formation was deposited during latest Triassic to earliest Jurassic time in a mosaic of fluvial, lacustrine, and eolian subenvironments. Ephemeral streams that flowed north-northwest (relative to modern geographic position) deposited single- and multi-storeyed trough cross-bedded sands on an open floodplain. Sheet flow deposited mainly silt across broad interchannel flats. Perennial lakes, in which mud, silt and carbonate were deposited, formed on the terminal floodplain; these deposits experienced episodic desiccation. Winds that blew dominantly east to south-southeast formed migrating dunes and sand sheets that were covered by low-amplitude ripples. The facies distribution varies greatly across the outcrop belt. The lacustrine facies of the terminal floodplain are limited to the northern part of the study area. In a southward direction along the outcrop belt (along the Echo Cliffs and Ward Terrace in Arizona), dominantly fluvial–lacustrine and subordinate eolian facies grade mainly to eolian dune and interdune facies. This transition records the encroachment of the Wingate erg. Moenave outcrops expose a north–south lithofacies gradient from distal, (erg margin) to proximal (erg interior). The presence of ephemeral stream and lake deposits, abundant burrowing and vegetative activity, and the general lack of strongly developed aridisols or evaporites suggest a climate that was seasonally arid both before and during deposition of the Moenave and the laterally equivalent Wingate Sandstone. -
Index 1 INDEX
Index 1 INDEX A Blue Spring 76, 106, 110, 115 Bluff Spring Trail 184 Adeii Eechii Cliffs 124 Blythe 198 Agate House 140 Blythe Intaglios 199 Agathla Peak 256 Bonita Canyon Drive 221 Agua Fria Nat'l Monument 175 Booger Canyon 194 Ajo 203 Boundary Butte 299 Ajo Mountain Loop 204 Box Canyon 132 Alamo Canyon 205 Box (The) 51 Alamo Lake SP 201 Boyce-Thompson Arboretum 190 Alstrom Point 266, 302 Boynton Canyon 149, 161 Anasazi Bridge 73 Boy Scout Canyon 197 Anasazi Canyon 302 Bright Angel Canyon 25, 51 Anderson Dam 216 Bright Angel Point 15, 25 Angels Window 27 Bright Angel Trail 42, 46, 49, 61, 80, 90 Antelope Canyon 280, 297 Brins Mesa 160 Antelope House 231 Brins Mesa Trail 161 Antelope Point Marina 294, 297 Broken Arrow Trail 155 Apache Junction 184 Buck Farm Canyon 73 Apache Lake 187 Buck Farm Overlook 34, 73, 103 Apache-Sitgreaves Nat'l Forest 167 Buckskin Gulch Confluence 275 Apache Trail 187, 188 Buenos Aires Nat'l Wildlife Refuge 226 Aravaipa Canyon 192 Bulldog Cliffs 186 Aravaipa East trailhead 193 Bullfrog Marina 302 Arch Rock 366 Bull Pen 170 Arizona Canyon Hot Springs 197 Bush Head Canyon 278 Arizona-Sonora Desert Museum 216 Arizona Trail 167 C Artist's Point 250 Aspen Forest Overlook 257 Cabeza Prieta 206 Atlatl Rock 366 Cactus Forest Drive 218 Call of the Canyon 158 B Calloway Trail 171, 203 Cameron Visitor Center 114 Baboquivari Peak 226 Camp Verde 170 Baby Bell Rock 157 Canada Goose Drive 198 Baby Rocks 256 Canyon del Muerto 231 Badger Creek 72 Canyon X 290 Bajada Loop Drive 216 Cape Final 28 Bar-10-Ranch 19 Cape Royal 27 Barrio -
Tetrapod Biostratigraphy and Biochronology of the Triassic–Jurassic Transition on the Southern Colorado Plateau, USA
Palaeogeography, Palaeoclimatology, Palaeoecology 244 (2007) 242–256 www.elsevier.com/locate/palaeo Tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau, USA Spencer G. Lucas a,⁎, Lawrence H. Tanner b a New Mexico Museum of Natural History, 1801 Mountain Rd. N.W., Albuquerque, NM 87104-1375, USA b Department of Biology, Le Moyne College, 1419 Salt Springs Road, Syracuse, NY 13214, USA Received 15 March 2006; accepted 20 June 2006 Abstract Nonmarine fluvial, eolian and lacustrine strata of the Chinle and Glen Canyon groups on the southern Colorado Plateau preserve tetrapod body fossils and footprints that are one of the world's most extensive tetrapod fossil records across the Triassic– Jurassic boundary. We organize these tetrapod fossils into five, time-successive biostratigraphic assemblages (in ascending order, Owl Rock, Rock Point, Dinosaur Canyon, Whitmore Point and Kayenta) that we assign to the (ascending order) Revueltian, Apachean, Wassonian and Dawan land-vertebrate faunachrons (LVF). In doing so, we redefine the Wassonian and the Dawan LVFs. The Apachean–Wassonian boundary approximates the Triassic–Jurassic boundary. This tetrapod biostratigraphy and biochronology of the Triassic–Jurassic transition on the southern Colorado Plateau confirms that crurotarsan extinction closely corresponds to the end of the Triassic, and that a dramatic increase in dinosaur diversity, abundance and body size preceded the end of the Triassic. © 2006 Elsevier B.V. All rights reserved. Keywords: Triassic–Jurassic boundary; Colorado Plateau; Chinle Group; Glen Canyon Group; Tetrapod 1. Introduction 190 Ma. On the southern Colorado Plateau, the Triassic– Jurassic transition was a time of significant changes in the The Four Corners (common boundary of Utah, composition of the terrestrial vertebrate (tetrapod) fauna. -
Tse' Nikani Draft Corridor Management
Tse'nikani Scenic Byway Corridor Management Plan DRAFT August 2013 Introduction Purpose Tse’nikani Scenic Byway was established The purpose of a byway corridor as an Arizona Byway in 2005 and given the management plan is not to create more name Tse’nikani ‘Flat Mesa Rock’ Scenic regulations or taxes. Rather, a corridor Byway. management plan documents the goals, strategies, and responsibilities for preserving and enhancing the byway’s most Byway Description valuable qualities. Promoting tourism can Tse’nikani Scenic Byway, U.S. Highway be one target, but so are issues of safety or (US) 191 is located in northeast Arizona preserving historic or cultural structures. in Apache County and entirely within the 160 The Corridor Management Plan can: Navajo Nation. The portion of US 191 that 1 160 Tse’nikani is a designated Arizona Scenic Byway is Scenic Road ◊ document community interest from Milepost (MP) 467.0, south of Many ◊ document existing conditions and Farms, to MP 510.4, at the junction with history US 160, near Mexican Water. The highway ◊ guide enhancement and safety is the primary route to access Canyon de improvement projects ARIZONA Chelly National Monument, about 13 miles mexico new south of the south end of the byway. ◊ promote partnerships for conservation Chinle and enhancement activities US 191 is a two-lane asphalt paved road for ◊ suggest resources for project development almost its entire length with no median and programs and few left-turn lanes. The roadway is ◊ promote coordination between residents, managed by the Arizona Department communities, and agencies of Transportation (ADOT) through the 264 Ganado ◊ support application for National Scenic Navajo Nation. -
FEIS for Arizona Snowbowl Facilities Improvements
United States Department of Agriculture Final Environmental Forest Service Impact Statement Southwestern Region for Arizona Snowbowl February 2005 Facilities Improvements Volume 2 Response to Comments on the Draft Environmental Impact Statement Coconino National Forest Coconino County, Arizona FINAL ENVIRONMENTAL IMPACT STATEMENT FOR THE ARIZONA SNOWBOWL FACILITIES IMPROVEMENTS PROPOSAL VOLUME 2 RESPONSE TO COMMENTS ON THE DRAFT ENVIRONMENTAL IMPACT STATEMENT COCONINO NATIONAL FOREST COCONINO COUNTY, ARIZONA FEBRUARY 2005 TABLE OF CONTENTS INTRODUCTION .......................................................................................................................................................1 1.0 NEPA PROCESS...........................................................................................................................................3 2.0 USFS POLICY.............................................................................................................................................13 3.0 DOCUMENT STRUCTURE......................................................................................................................19 4.0 MODIFIED ALTERNATIVES..................................................................................................................21 5.0 CULTURAL RESOURCES .......................................................................................................................25 6.0 WATER RESOURCES ..............................................................................................................................40 -
Summits on the Air – ARM for the USA (W7A
Summits on the Air – ARM for the U.S.A (W7A - Arizona) Summits on the Air U.S.A. (W7A - Arizona) Association Reference Manual Document Reference S53.1 Issue number 5.0 Date of issue 31-October 2020 Participation start date 01-Aug 2010 Authorized Date: 31-October 2020 Association Manager Pete Scola, WA7JTM Summits-on-the-Air an original concept by G3WGV and developed with G3CWI Notice “Summits on the Air” SOTA and the SOTA logo are trademarks of the Programme. This document is copyright of the Programme. All other trademarks and copyrights referenced herein are acknowledged. Document S53.1 Page 1 of 15 Summits on the Air – ARM for the U.S.A (W7A - Arizona) TABLE OF CONTENTS CHANGE CONTROL....................................................................................................................................... 3 DISCLAIMER................................................................................................................................................. 4 1 ASSOCIATION REFERENCE DATA ........................................................................................................... 5 1.1 Program Derivation ...................................................................................................................................................................................... 6 1.2 General Information ..................................................................................................................................................................................... 6 1.3 Final Ascent -
GWEC Global Wind Report 2016
GLOBAL WIND REPORT ANNUAL MARKET UPDATE 2016 Opening up new markets for business: Mongolia 8TH NATIONAL RENEWABLE ENERGY FORUM Ulaanbaatar, Mongolia 5 May 2017 Mongolia’s wind has the technical potential of 1TW. GWEC is paving the road to that potential. www.gwec.net TABLE OF CONTENTS Preface . 4 Foreword from our sponsor . 6 Corporate Sourcing of Renewables – A New Market Driver for Wind . 8 Global Status of Wind Power in 2016 . 12 Market Forecast 2017-2021 . 20 Argentina . 26 Australia . 28 Brazil . 30 Canada . 32 Chile . 34 PR China . 36 Denmark . 40 The European Union . 42 Finland . 44 Germany . 46 India . 48 Japan . 50 Mexico . 52 Netherlands . 54 Norway . 56 Offshore Wind . 58 South Africa . 66 Turkey . 68 United States . 70 Vietnam . 72 About GWEC . 74 GWEC – Global Wind 2016 Report 3 PREFACE verall, the wind industry fi nished up 2016 in good installations of 8,203 MW were about the same as 2015’s, and shape, with solid prospects for 2017 and beyond. The despite the political goings-on, seem to be on track for a strong O economics of the industry continue to improve, with 2017, with 18+ GW either under construction or in advanced record low prices for the winning tender in Morocco last year stages of development. So far so good – fi ngers crossed! of about $30/MWh, and very competitive prices in auctions Europe’s numbers were surprisingly strong, actually sur- around the world, while more and more companies’ P&Ls have passing 2015 for Europe as a whole on the strength of Turkey’s come out of the red and into the black. -
Appendix H Public Comments and Responses to DEIS
APPENDIX H PUBLIC COMMENTS AND RESPONSES ON DRAFT ENVIRONMENTAL IMPACT STATEMENT According to NEPA, federal agencies are required to identify and formally respond to all substantive public comments. A standardized content analysis process was conducted to analyze the public comments on the Draft EIS. Each comment letter and email message received was read, analyzed and considered by BLM, Reclamation, and Western to ensure that all substantive comments were identified. In performing this analysis, the BLM, Reclamation, and Western relied on the Council on Environmental Quality’s regulations to determine what constituted a substantive comment. A substantive comment does one or more of the following: Questions, with a reasonable basis, the accuracy of the information and/or analysis in the EIS. Questions, with a reasonable basis, the adequacy of the information and/or analysis in the EIS. Presents reasonable alternatives other than those presented in the Draft EIS that meet the purpose and need of the proposed action and addresses significant issues. Questions, with a reasonable basis, the merits of an alternative or alternatives. Causes changes in or revisions to the proposed action. Questions, with a reasonable basis, the adequacy of the planning process itself. Thirty-seven individual comment letters and/or emails were submitted to the BLM during the 45-day comment period. Within the 37 comment letters, 322 comments were identified and addressed. Comments on the Draft EIS that failed to meet the above description were considered non-substantive because they expressed personal opinions or preferences that were not relevant to the adequacy or accuracy of the Draft EIS, or represented commentary regarding resource management unrelated to the Draft EIS. -
Rainfall-Runoff Model for Black Creek Watershed, Navajo Nation
Rainfall-Runoff Model for Black Creek Watershed, Navajo Nation Item Type text; Proceedings Authors Tecle, Aregai; Heinrich, Paul; Leeper, John; Tallsalt-Robertson, Jolene Publisher Arizona-Nevada Academy of Science Journal Hydrology and Water Resources in Arizona and the Southwest Rights Copyright ©, where appropriate, is held by the author. Download date 25/09/2021 20:12:23 Link to Item http://hdl.handle.net/10150/301297 37 RAINFALL-RUNOFF MODEL FOR BLACK CREEK WATERSHED, NAVAJO NATION Aregai Tecle1, Paul Heinrich1, John Leeper2, and Jolene Tallsalt-Robertson2 ABSTRACT This paper develops a rainfall-runoff model for estimating surface and peak flow rates from precipitation storm events on the Black Creek watershed in the Navajo Nation. The Black Creek watershed lies in the southern part of the Navajo Nation between the Defiance Plateau on the west and the Chuska Mountains on the east. The area is in the semiarid part of the Colorado Plateau on which there is about 10 inches of precipitation a year. We have two main purposes for embarking on the study. One is to determine the amount of runoff and peak flow rate generated from rainfall storm events falling on the 655 square mile watershed and the second is to provide the Navajo Nation with a method for estimating water yield and peak flow in the absence of adequate data. Two models, Watershed Modeling System (WMS) and the Hydrologic Engineering Center (HEC) Hydrological Modeling System (HMS) that have Geographic Information System (GIS) capabilities are used to generate stream hydrographs. Figure 1. Physiographic map of the Navajo Nation with the Chuska The latter show peak flow rates and total amounts of Mountain and Deance Plateau and Stream Gaging Stations.