When and How Did the Grand Canyon Form?
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Lecture 21: Glaciers and Paleoclimate Read: Chapter 15 Homework Due Thursday Nov
Learning Objectives (LO) Lecture 21: Glaciers and Paleoclimate Read: Chapter 15 Homework due Thursday Nov. 12 What we’ll learn today:! 1. 1. Glaciers and where they occur! 2. 2. Compare depositional and erosional features of glaciers! 3. 3. Earth-Sun orbital parameters, relevance to interglacial periods ! A glacier is a river of ice. Glaciers can range in size from: 100s of m (mountain glaciers) to 100s of km (continental ice sheets) Most glaciers are 1000s to 100,000s of years old! The Snowline is the lowest elevation of a perennial (2 yrs) snow field. Glaciers can only form above the snowline, where snow does not completely melt in the summer. Requirements: Cold temperatures Polar latitudes or high elevations Sufficient snow Flat area for snow to accumulate Permafrost is permanently frozen soil beneath a seasonal active layer that supports plant life Glaciers are made of compressed, recrystallized snow. Snow buildup in the zone of accumulation flows downhill into the zone of wastage. Glacier-Covered Areas Glacier Coverage (km2) No glaciers in Australia! 160,000 glaciers total 47 countries have glaciers 94% of Earth’s ice is in Greenland and Antarctica Mountain Glaciers are Retreating Worldwide The Antarctic Ice Sheet The Greenland Ice Sheet Glaciers flow downhill through ductile (plastic) deformation & by basal sliding. Brittle deformation near the surface makes cracks, or crevasses. Antarctic ice sheet: ductile flow extends into the ocean to form an ice shelf. Wilkins Ice shelf Breakup http://www.youtube.com/watch?v=XUltAHerfpk The Greenland Ice Sheet has fewer and smaller ice shelves. Erosional Features Unique erosional landforms remain after glaciers melt. -
Scoping Report: Grand Staircase-Escalante National
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 ................................................................................................... 4 2.6 National Historic Preservation Act and Tribal Consultation ....................................................... 5 3 Submission Processing and Comment Coding .................................................................................... 5 -
Canyon Formation Constraints on the Discharge of Catastrophic Outburst
PUBLICATIONS Journal of Geophysical Research: Planets RESEARCH ARTICLE Canyon formation constraints on the discharge of catastrophic 10.1002/2016JE005061 outburst floods of Earth and Mars Key Points: Mathieu G. A. Lapotre1, Michael P. Lamb1, and Rebecca M. E. Williams2 • A new model for canyon formation through waterfall retreat combines 1Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California, USA, 2Planetary flood hydraulics and erosional mechanics Science Institute, Tucson, Arizona, USA • The model is used as a paleohydraulic tool to estimate the discharge of megafloods on Earth and Mars Abstract Catastrophic outburst floods carved amphitheater-headed canyons on Earth and Mars, and the • Compared with previous estimates, steep headwalls of these canyons suggest that some formed by upstream headwall propagation through predicted discharges are lower, fl durations higher, and water waterfall erosion processes. Because topography evolves in concert with water ow during canyon erosion, volumes are similar we suggest that bedrock canyon morphology preserves hydraulic information about canyon-forming floods. In particular, we propose that for a canyon to form with a roughly uniform width by upstream headwall retreat, erosion must occur around the canyon head, but not along the sidewalls, such that canyon width is fl fl Correspondence to: related to ood discharge. We develop a new theory for bedrock canyon formation by mega oods based M. G. A. Lapotre, on flow convergence of large outburst floods toward a horseshoe-shaped waterfall. The model is developed [email protected] for waterfall erosion by rock toppling, a candidate erosion mechanism in well fractured rock, like columnar basalt. We apply the model to 14 terrestrial (Channeled Scablands, Washington; Snake River Plain, Idaho; Citation: and Ásbyrgi canyon, Iceland) and nine Martian (near Ares Vallis and Echus Chasma) bedrock canyons and Lapotre, M. -
Washington's Channeled Scabland
t\D l'llrl,. \·· ~. r~rn1 ,uR\fEY Ut,l\n . .. ,Y:ltate" tit1Washington ALBEIT D. ROSEWNI, Governor Department of Conservation EARL COE, Dlnctor DIVISION OF MINES AND GEOLOGY MARSHALL T. HUNTTING, Supervisor Bulletin No. 45 WASHINGTON'S CHANNELED SCABLAND By J HARLEN BRETZ 9TAT• PIUHTIHO PLANT ~ OLYMPIA, WASH., 1"511 State of Washington ALBERT D. ROSELLINI, Governor Department of Conservation EARL COE, Director DIVISION OF MINES AND GEOLOGY MARSHALL T. HUNTTING, Supervisor Bulletin No. 45 WASHINGTON'S CHANNELED SCABLAND By .T HARLEN BRETZ l•or sate by Department or Conservation, Olympia, Washington. Price, 50 cents. FOREWORD Most travelers who have driven through eastern Washington have seen a geologic and scenic feature that is unique-nothing like it is to be found anywhere else in the world. This is the Channeled Scab land, a gigantic series of deeply cut channels in the erosion-resistant Columbia River basalt, the rock that covers most of the east-central and southeastern part of the state. Grand Coulee, with its spectac ular Dry Falls, is one of the most widely known features of this ex tensive set of dry channels. Many thousands of travelers must have wondered how this Chan neled Scabland came into being, and many geologists also have speculated as to its origin. Several geologists have published papers outlining their theories of the scabland's origin, but the geologist who has made the most thorough study of the problem and has ex amined the whole area and all the evidence having a bearing on the problem is Dr. J Harlen Bretz. Dr. -
Energy and Mineral Resources, Grand Staircase
Circular 93 Utah Geological Survey Illustration Captions View figure: Circular 93 1., 2., 3., 4., 5., 6., 7., 8., 9., 10., 11., 12., 13., 14., 15. A Preliminary Assessment of Energy and Table of Contents 1.Preface Mineral Resources within the Grand 2.Summary 3.Introduction Staircase - Escalante National Monument 4.Geology 5.Kaiparowits Plateau coal Compiled by M. Lee Allison, State Geologist field 6.Oil and Gas Potential Contributors: 7.Tar-sand Resources Robert E. Blackett, Editor 8.Non-fuel Minerals and Thomas C. Chidsey Jr., Oil and Gas Mining David E. Tabet, Coal and Coal-Bed Gas 9.Acknowledgments Robert W. Gloyn, Minerals 10.References Charles E. Bishop, Tar-Sands January 1997 UTAH GEOLOGICAL SURVEY a division of UTAH DEPARTMENT OF NATURAL RESOURCES CONTENTS PREFACE SUMMARY INTRODUCTION Background Purpose and Scope GEOLOGY Regional Structure Permian through Jurassic Stratigraphy Cretaceous and Tertiary Stratigraphy THE KAIPAROWITS PLATEAU COAL FIELD History of Mining and Exploration Coal Resources Coal Resources on School and Institutional Trust Lands Sulfur Content of Kaiparowits Coal Coal-bed Gas Resources Further Coal Resource Assessments Needed OIL AND GAS POTENTIAL Source Rocks Potential Reservoirs Trapping Mechanisms Exploration and Development Carbon Dioxide Further Oil and Gas Resource Assessments Needed TAR-SAND RESOURCES OF THE CIRCLE CLIFFS AREA NON-FUEL MINERALS AND MINING Manganese Uranium-Vanadium Zirconium-Titanium Gold Copper, Lead and Zinc Industrial and Construction Materials Mining Activity Further Non-Fuel Mineral Resource Assessments Needed ACKNOWLEDGMENTS REFERENCES APPENDIX A: Presidential proclamation APPENDIX B: Summary of the coal resource of Kaiparowits Plateau and its value APPENDIX C: Summary of coal resources on School and Institutional Trust Lands APPENDIX D: Authorized Federal Oil and Gas Leases in the monument ILLUSTRATIONS Figure 1. -
Grand Circle
Salt Lake City Green River - Moab Salt Lake City - Green River 60min (56mile) Grand Junction 180min (183mile) Colorado Crescent Jct. NM Great Basin Green River NP Arches NP Moab - Arches Goblin Valley 10min (5mile) SP Corona Arch Moab Grand Circle Map Capitol Reef - Green River Dead Horse Point 100min (90mile) SP Moab - Grand View Point NP: National Park 80min (45mile) NM: National Monument NHP: National Histrocal Park Bryce Canyon - Capitol Reef Canyonlands SP: State Park Capitol Reef COLORADO 170min (123mile) NP NP Moab - Mesa Verde Monticello Moab - Monument Valley 170min (140mile) NEVADA UTAH 170min (149mile) Bryce Cedar City Canyon NP Natural Bridges Canyon of the Cedar Breaks NM Blanding Ancients NM Mesa Verde - Monument Valley NM Kodacrome Basin SP 200min (150mile) Valley of Hovenweep 40min 70min NM Cortez (24mile) (60mile) Grand Staircase- the Gods 100min Escalante NM Durango Mt. Carmel (92mile) Muley Point Snow Canyon Jct. SP Goosenecks SP Zion NP Kanab Lake Powell Mexican Hat Mesa Verde Rainbow Monument Valley NP Coral Pink Sand Vermillion Page Bridge NM Four Corners Las Vegas - Zion Dunes SP Cliffs NM Navajo Tribal Park Aztec Ruins NM 170min (167mile) Antelope Pipe Spring NM Horseshoe Shiprock Aztec Bend Canyon Mesa Verde - Chinle 200min (166mile) Mt.Carmel Jct. - North Rim Navajo NM 140min (98mile) Kayenta Farmington Monument Valley - Chinle Mesa Verde - Chaco Culture Valley of Fire Page - North Rim Page - Cameron Page - Monument Valley 140min (134mile) 230min (160mile) SP 170min (124mile) 90min (83mile) Grand Canyon- 130min -
MINERAL POTENTIAL REPORT for the Lands Now Excluded from Grand Staircase-Escalante National Monument
United States Department ofthe Interior Bureau of Land Management MINERAL POTENTIAL REPORT for the Lands now Excluded from Grand Staircase-Escalante National Monument Garfield and Kane Counties, Utah Prepared by: Technical Approval: flirf/tl (Signature) Michael Vanden Berg (Print name) (Print name) Energy and Mineral Program Manager - Utah Geological Survey (Title) (Title) April 18, 2018 /f-P/2ft. 't 2o/ 8 (Date) (Date) M~zr;rL {Signature) 11 (Si~ ~.u.. "'- ~b ~ t:, "4 5~ A.J ~txM:t ;e;,E~ 't"'-. (Print name) (Print name) J.-"' ,·s h;c.-+ (V\ £uA.o...~ fk()~""....:r ~~/,~ L{ ( {Title) . Zo'{_ 2o l~0 +(~it71 ~ . I (Date) (Date) This preliminary repon makes information available to the public that may not conform to UGS technical, editorial. or policy standards; this should be considered by an individual or group planning to take action based on the contents ofthis report. Although this product represents the work of professional scientists, the Utah Department of Natural Resources, Utah Geological Survey, makes no warranty, expressed or implied, regarding it!I suitability for a panicular use. The Utah Department ofNatural Resources, Utah Geological Survey, shall not be liable under any circumstances for any direct, indirect, special, incidental, or consequential damages with respect to claims by users ofthis product. TABLE OF CONTENTS SUMMARY AND CONCLUSIONS ........................................................................................................... 4 Oil, Gas, and Coal Bed Methane ........................................................................................................... -
INTERIOR/GEOLOGICAL SURVEY USGS· INF -72- 2 !R I) - Electric City-Grand Coulee, Washington the CHANNELED SCABLANDS of EASTERN WASHINGTON
9 INTERIOR/GEOLOGICAL SURVEY USGS· INF -72- 2 !R I) - Electric City-Grand Coulee, Washington THE CHANNELED SCABLANDS OF EASTERN WASHINGTON - The Geologic Story of the Spokane Flood- '(( U.S. GOVERNMENT PRINTING OFFICE , 1976 0 -208-172 F'or sale by the uperint.endent. of Documents, .S. Government Printing Office Washington, D.. 20402- Pric~ 70 cents Lock No. 024 - 001-02507- I nL nlog o. I 19.2: W27/6/974 There is n minimum charge of $1.00 for each mail order A trave ler enterin g th e tal f W as hington fro m th e Eas t crosses a flat-to-rolling country sid o f deep, fertil so il commonly sown with w heat. ontinuing wes twa rd , he abruptly nters a d eply scar red land o f bare bl a k ro k ut by labyrin thine ca nyons and chann el , plunge pools and ro k bas in s, ca ca de and ca tara t ledges, and di playi ng ragged buttes and li ffs, alcoves, im men e gravel bars, and giant ripple marks. Th e traveler has reached the starkly sceni " Chan neled cab lands," and this d ramatic hange in th e landscape may well ca use him to w onder " w hat happ n d here? " Th e answ er- th e grea te t fl ood documented by man. This publica tion, summari zin g th e equence of geologic events that culminated in th e so-call ed ''Spokan Fl ood," w as prepar d in res ponse to a ge neral int re t in geology and a particul ar interes t in th e o ri gin of th e Scab land o ften ex pre sed by th ose ross in g th e State of W as hington. -
Conserving the Grand Canyon Watershed a Proposal for National Monument Designation
Conserving the Grand Canyon Watershed A Proposal for National Monument Designation r! Photo: Marti&v& w, Kaibab Plateau, north rim of tlx Grand Canyon, Arizona 02010 GCWC WIL L1N COUNCIL W1DERNESS cnCtotr- Conserving the Grand Canyon Watershed A Proposal for National Monument Designation EXECUTIVE SUMMARY A 12,000-year Human Record A Unique Landscape The proposed Monument holds lands of great signifi- Ranging from the arid Sonoran and Great Basin Des- cance to the Kaibab Paiute tribe, as well as Hopi, Zuni, erts to lush, boreal Rocky Mountain forests, the proposed Hualapi, Havasupai, and Navajo tribes, and was home Grand Canyon Watershed National Monument is an eco- to the Clovis, Basketmaker, and Puebloan peoples. More logical wonder. The proposed Monument embraces one than three thousand ancient Native American archaeo- of the most spectacular American landscapes— the Grand logical sites have been documented in the region, repre- Canyon— and encompasses a wild, rugged array of tower- senting just a fraction of the human history of the area. ing cliffs, deeply incised tributary canyons, grasslands, Ranging from settlements or habitations, to temporary and numerous springs that flow into the Colorado River camps, granaries and caches, and rock art, some of the in Grand Canyon. Unique geologic formations contribute sites date from as far back as the Paleo- Indian period— substantially to the proposed Monument' s spectacular 11, 000 BCE. biological diversity, with escarpments and canyons dating Kanab Creek falls within the traditional territory of back millions ofyears. At least twenty-two sensitive species call " Certain [ lanad] of theforest redereee dhoula the landscape home, including the endangered California condor and also be made predereed for the wigforest the rare northern goshawk. -
Desert Semidesert* Upland* Mountain
MLRA 35 - Colorado and Green River Plateaus MLRA 35 - Colorado and Green River Plateaus (Utah portion) Ecological Zone Desert Semidesert* Upland* Mountain Precipitation 5 -9 inches 9 -13 inches 13-16 inches Elevation 3,000 -5,000 4,500 -6,500 5,800 - 7,000 NONE Soil Moisture Regime Typic Ardic Ustic Aridic Aridic Ustic Soil Temp Regime Mesic/Thermic Mesic Mesic Freeze free Days 120-220 120-160 100-130 Percent of Pinyon Percent of Juniper production is Shadscale and production is usually usually greater than blackbrush Notes greater than the Pinyon the Juniper production production 300 – 500 lbs/ac 400 – 700 lbs/ac 100 – 500 lbs/ac 800 – 1,000 lbs/ac *the aspect (north or south) can greatly influence site characteristics. All values in this table are approximate and should be used as guidelines. Different combinations of temperature, precipitation and soil type can place an ecological site into different zones. Rocky Mountains Major Land ResourceBasins and Plateaus Area (MLRA) D35 D36 - Southwestern Plateaus, Mesas, and Foothills D35 - Colorado Plateau Desert 07014035 Miles 35—Colorado Plateau This area is in Arizona (56 percent), Utah (22 percent), New Mexico (21 percent), and Colorado (1 percent). It makes up about 71,735 square miles (185,885 square kilometers). The cities of Kingman and Winslow, Arizona, Gallup and Grants, New Mexico, and Kanab and Moab, Utah, are in this area. Interstate 40 connects some of these cities, and Interstate 17 terminates in Flagstaff, Arizona, just outside this MLRA. The Grand Canyon and Petrified Forest National Parks and the Canyon de Chelly and Wupatki National Monuments are in the part of this MLRA in Arizona. -
Nature-Directed Approach to Hydrology and Hydraulics of Extreme Floods and Megafloods
Nature-Directed Approach to Hydrology and Hydraulics of Extreme Floods and Megafloods Item Type text; Electronic Dissertation Authors Liu, Tao 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, presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 01/10/2021 17:03:45 Link to Item http://hdl.handle.net/10150/632582 NATURE-DIRECTED APPROACH TO HYDROLOGY AND HYDRAULICS OF EXTREME FLOODS AND MEGAFLOODS by Tao Liu __________________________ Copyright © Tao Liu 2019 A Dissertation Submitted to the Faculty of the DEPARTMENT OF HYDROLOGY AND ATMOSPHERIC SCIENCES In Partial Fulfillment of the Requirements For the Degree of DOCTOR OF PHILOSOPHY WITH A MAJOR IN HYDROLOGY In the Graduate College THE UNIVERSITY OF ARIZONA 2019 2 THE UNIVERSITY OF ARIZONA GRADUATE COLLEGE Tao Liu, Nature-Directed Approach to Hydrology and Hydraulics of As members of the Dissertation Committee, we certify that we have read the dissertation Extreme Floods and Megajloods prepared by titled and recommend that it be accepted as fulfilling the dissertation requirement fo ec of Doctor of Philosophy. a� (04/08/2019) Date: (04/08/2019) Date: (04/08/2019) Date: (04/08/2019) Date: Final approva"-- �-�-�--��� of the final co 3 ACKNOWLEDGEMENT It is the time to say “thank you” to all people who have made a great contribution to this work and my time in the hydrology program. Dr. Vic Baker is the most important person for me to pursue the “Ph. -
ESCI-1510: Historical Geology 1
ESCI-1510: Historical Geology 1 ESCI-1510: HISTORICAL GEOLOGY Cuyahoga Community College Viewing: ESCI-1510 : Historical Geology Board of Trustees: February 2019 Academic Term: Fall 2021 Subject Code ESCI - Earth Science Course Number: 1510 Title: Historical Geology Catalog Description: Historical geology focuses on the evolution of land forms and life-forms through geologic time. The course includes a study of evolutionary changes occurring in plant and animal life as documented by fossil remains and the interpretation of geologic forces by means of topographic and geologic maps. Topics include plate tectonics, relative and absolute dating, fossils and fossilization, rocks and their significance as indicators of the environmental past. Emphasis will be placed on North America, dealing with the growth of continents and mountain building. To fulfill the laboratory science requirement, students should also enroll in a Historical Geology laboratory course. Credit Hour(s): 3 Lecture Hour(s): 3 Lab Hour(s): 0 Other Hour(s): 0 Requisites Prerequisite and Corequisite ENG-0985 Introduction to College Literacies, or appropriate score on English Placement Test; and ESCI-1410 Physical Geology or ESCI-1310 Physical Geography. Note: ENG-0980 Language Fundamentals I taken prior to Fall 2021 will also meet prerequisite requirements. Outcomes Course Outcome(s): Apply the principles of geology to understand the Earth's history. Essential Learning Outcome Mapping: Critical/Creative Thinking: Analyze, evaluate, and synthesize information in order to consider problems/ideas and transform them in innovative or imaginative ways. Objective(s): 1. Recognize that the Earth system is characterized by change over a variety of time scales. 2. Explain the use of minerals and rocks to decipher the Earth's history.