55. Can Flood Geology and Catastrophic Plate
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Hydrogeology of Jurassic and Triassic Wetlands in the Colorado Plateau and the Origin of Tabular Sandstone Uranium Deposits
Hydrogeology of Jurassic and Triassic Wetlands in the Colorado Plateau and the Origin of Tabular Sandstone Uranium Deposits U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1548 AVAILABILITY OF BOOKS AND MAPS OF THE U.S. GEOLOGICAL SURVEY Instructions on ordering publications of the U.S. Geological Survey, along with prices of the last offerings, are given in the current-year issues of the monthly catalog "New Publications of the U.S. Geological Survey." Prices of available U.S. Geological Survey publications re leased prior to the current year are listed in the most recent annual "Price and Availability List." Publications that may be listed in various U.S. Geological Survey catalogs (see back inside cover) but not listed in the most recent annual "Price and Availability List" may no longer be available. Reports released through the NTIS may be obtained by writing to the National Technical Information Service, U.S. Department of Commerce, Springfield, VA 22161; please include NTIS report number with inquiry. Order U.S. Geological Survey publications by mail or over the counter from the offices listed below. BY MAIL OVER THE COUNTER Books Books and Maps Professional Papers, Bulletins, Water-Supply Papers, Tech Books and maps of the U.S. Geological Survey are available niques of Water-Resources Investigations, Circulars, publications over the counter at the following U.S. Geological Survey offices, all of general interest (such as leaflets, pamphlets, booklets), single of which are authorized agents of the Superintendent of Docu copies of Earthquakes & Volcanoes, Preliminary Determination of ments. Epicenters, and some miscellaneous reports, including some of the foregoing series that have gone out of print at the Superintendent of Documents, are obtainable by mail from • ANCHORAGE, Alaska-Rm. -
Definition of Chalk
1.1: Introduction: 1.1.1: Definition of chalk: Chalk is a soft, white, porous sedimentary carbonate rock, a form of limestone composed of the mineral calcite. Calcite is calcium carbonate or CaCO3. It forms under reasonably deep marine conditions from the gradual accumulation of minute calcite shells (coccoliths) shed from micro-organisms called coccolithophores. Flint (a type of chert unique to chalk) is very common as bands parallel to the bedding or as nodules embedded in chalk. It is probably derived from sponge spicules or other siliceous organisms as water is expelled upwards during compaction. Flint is often deposited around larger fossils such as Echinoidea which may be silicified (i.e. replaced molecule by molecule by flint). Chalk as seen in Cretaceous deposits of Western Europe is unusual among sedimentary limestone in the thickness of the beds. Most cliffs of chalk have very few obvious bedding planes unlike most thick sequences of limestone such as the Carboniferous Limestone or the Jurassic oolitic limestones. This presumably indicates very stable conditions over tens of millions of years. Figure (1-1): Calcium sulphate 1 "Nitzana Chalk curves" situated at Western Negev, Israel are chalk deposits formed at the Mesozoic era's Tethys Ocean Chalk has greater resistance to weathering and slumping than the clays with which it is usually associated, thus forming tall steep cliffs where chalk ridges meet the sea. Chalk hills, known as chalk downland, usually form where bands of chalk reach the surface at an angle, so forming a scarp slope. Because chalk is well jointed it can hold a large volume of ground water, providing a natural reservoir that releases water slowly through dry seasons. -
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 -
Upper Paleozoic and Cretaceous Stratigraphy of the Hidalgo County Area, New Mexico Eugene Greenwood, F
New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/21 Upper Paleozoic and Cretaceous stratigraphy of the Hidalgo County area, New Mexico Eugene Greenwood, F. E. Kottlowski, and A. K. Armstrong, 1970, pp. 33-44 in: Tyrone, Big Hatchet Mountain, Florida Mountains Region, Woodward, L. A.; [ed.], New Mexico Geological Society 21st Annual Fall Field Conference Guidebook, 176 p. This is one of many related papers that were included in the 1970 NMGS Fall Field Conference Guidebook. Annual NMGS Fall Field Conference Guidebooks Every fall since 1950, the New Mexico Geological Society (NMGS) has held an annual Fall Field Conference that explores some region of New Mexico (or surrounding states). Always well attended, these conferences provide a guidebook to participants. Besides detailed road logs, the guidebooks contain many well written, edited, and peer-reviewed geoscience papers. These books have set the national standard for geologic guidebooks and are an essential geologic reference for anyone working in or around New Mexico. Free Downloads NMGS has decided to make peer-reviewed papers from our Fall Field Conference guidebooks available for free download. Non-members will have access to guidebook papers two years after publication. Members have access to all papers. This is in keeping with our mission of promoting interest, research, and cooperation regarding geology in New Mexico. However, guidebook sales represent a significant proportion of our operating budget. Therefore, only research papers are available for download. Road logs, mini-papers, maps, stratigraphic charts, and other selected content are available only in the printed guidebooks. Copyright Information Publications of the New Mexico Geological Society, printed and electronic, are protected by the copyright laws of the United States. -
Chapter 2 Paleozoic Stratigraphy of the Grand Canyon
CHAPTER 2 PALEOZOIC STRATIGRAPHY OF THE GRAND CANYON PAIGE KERCHER INTRODUCTION The Paleozoic Era of the Phanerozoic Eon is defined as the time between 542 and 251 million years before the present (ICS 2010). The Paleozoic Era began with the evolution of most major animal phyla present today, sparked by the novel adaptation of skeletal hard parts. Organisms continued to diversify throughout the Paleozoic into increasingly adaptive and complex life forms, including the first vertebrates, terrestrial plants and animals, forests and seed plants, reptiles, and flying insects. Vast coal swamps covered much of mid- to low-latitude continental environments in the late Paleozoic as the supercontinent Pangaea began to amalgamate. The hardiest taxa survived the multiple global glaciations and mass extinctions that have come to define major time boundaries of this era. Paleozoic North America existed primarily at mid to low latitudes and experienced multiple major orogenies and continental collisions. For much of the Paleozoic, North America’s southwestern margin ran through Nevada and Arizona – California did not yet exist (Appendix B). The flat-lying Paleozoic rocks of the Grand Canyon, though incomplete, form a record of a continental margin repeatedly inundated and vacated by shallow seas (Appendix A). IMPORTANT STRATIGRAPHIC PRINCIPLES AND CONCEPTS • Principle of Original Horizontality – In most cases, depositional processes produce flat-lying sedimentary layers. Notable exceptions include blanketing ash sheets, and cross-stratification developed on sloped surfaces. • Principle of Superposition – In an undisturbed sequence, older strata lie below younger strata; a package of sedimentary layers youngs upward. • Principle of Lateral Continuity – A layer of sediment extends laterally in all directions until it naturally pinches out or abuts the walls of its confining basin. -
Havasu Canyon Watershed Rapid Watershed Assessment Report June, 2010
Havasu Canyon Watershed Rapid Watershed Assessment Report June, 2010 Prepared by: USDA Natural Resources Conservation Service University of Arizona, Water Resources Research Center In cooperation with: Coconino Natural Resource Conservation District Arizona Department of Agriculture Arizona Department of Environmental Quality Arizona Department of Water Resources Arizona Game & Fish Department Arizona State Land Department USDA Forest Service USDA Bureau of Land Management Released by: Sharon Megdal David L. McKay Director State Conservationist University of Arizona United States Department of Agriculture Water Resources Research Center Natural Resources Conservation Service Principle Investigators: Dino DeSimone – NRCS, Phoenix Keith Larson – NRCS, Phoenix Kristine Uhlman – Water Resources Research Center Terry Sprouse – Water Resources Research Center Phil Guertin – School of Natural Resources The United States Department of Agriculture (USDA) prohibits discrimination in all its programs and activities on the basis of race, color, national origin, gender, religion, age, disa bility, po litica l be lie fs, sexua l or ien ta tion, an d mar ita l or fam ily s ta tus. (No t a ll prohibited bases apply to all programs.) Persons with disabilities who require alternative means for communication of program information (Braille, large print, audiotape, etc.) should contact USDA’s TARGET Center at 202-720-2600 (voice and TDD). To file a complaint of discrimination, write USDA, Director, Office of Civil Rights, Room 326W, Whitten Building, 14th and Independence Avenue, SW, Washington, D.C., 20250-9410 or call (202) 720-5964 (voice or TDD). USDA is an equal employment opportunity provider and employer. Havasu Canyon Watershed serve as a platform for conservation 15010004 program delivery, provide useful 8-Digit Hydrologic Unit information for development of NRCS Rapid Watershed Assessment and Conservation District business plans, and lay a foundation for future cooperative watershed planning. -
Michael Kenney Paleozoic Stratigraphy of the Grand Canyon
Michael Kenney Paleozoic Stratigraphy of the Grand Canyon The Paleozoic Era spans about 250 Myrs of Earth History from 541 Ma to 254 Ma (Figure 1). Within Grand Canyon National Park, there is a fragmented record of this time, which has undergone little to no deformation. These still relatively flat-lying, stratified layers, have been the focus of over 100 years of geologic studies. Much of what we know today began with the work of famed naturalist and geologist, Edwin Mckee (Beus and Middleton, 2003). His work, in addition to those before and after, have led to a greater understanding of sedimentation processes, fossil preservation, the evolution of life, and the drastic changes to Earth’s climate during the Paleozoic. This paper seeks to summarize, generally, the Paleozoic strata, the environments in which they were deposited, and the sources from which the sediments were derived. Tapeats Sandstone (~525 Ma – 515 Ma) The Tapeats Sandstone is a buff colored, quartz-rich sandstone and conglomerate, deposited unconformably on the Grand Canyon Supergroup and Vishnu metamorphic basement (Middleton and Elliott, 2003). Thickness varies from ~100 m to ~350 m depending on the paleotopography of the basement rocks upon which the sandstone was deposited. The base of the unit contains the highest abundance of conglomerates. Cobbles and pebbles sourced from the underlying basement rocks are common in the basal unit. Grain size and bed thickness thins upwards (Middleton and Elliott, 2003). Common sedimentary structures include planar and trough cross-bedding, which both decrease in thickness up-sequence. Fossils are rare but within the upper part of the sequence, body fossils date to the early Cambrian (Middleton and Elliott, 2003). -
Walking to the White Cliffs of Dover
Walking to The White Cliffs of Dover The White Cliffs of Dover, Take a walk through Dover, Langdon Cliffs, Upper Road, past the museum and along the Dover seafront to the iconic White Cliffs. On your way you'll see the historic TRAIL medieval castle while viewing the Walking hustle and bustle of the world's busiest passenger port. When GRADE you get to the cliffs, call in to our Moderate visitor centre to collect a free walking map and grab a bite to DISTANCE eat or treat yourself to something 2 miles (3.3km) from our shop. TIME Terrain 50 The walk is mostly on paved surfaces with some steps; mostly flat, with one very steep section. The route is challenging with a pushchair. OS MAP 138 Things to see Contact 01304 207326 [email protected] Facilities The White Cliffs are open to walkers free of charge everyday of the year. Dover Museum The seafront The Port of Dover The cafe, gift shop and toilets Why not visit Dover Museum? Enjoy views of the harbour and Take a moment to look at the are open daily 10-5pm, March The museum has a fascinating castle. From the promenade you’ll bustle of the port below you. to October with shorter hours in collection of items from the be able to see the ships coming Ferries arrive and depart 24hrs winter. local area, including the world's and going from the ferry terminal a day traveling to France and A short walk from the visitor oldest seagoing vessel the Dover and may even see a giant cruise Belgium. -
Analysis of a Sponge Bioherm from the Hermosa Group, Molas Lake Area, Colorado
Bowling Green State University ScholarWorks@BGSU Honors Projects Honors College Spring 2014 Analysis of a Sponge Bioherm from the Hermosa Group, Molas Lake Area, Colorado Joanna Hamilton [email protected] Follow this and additional works at: https://scholarworks.bgsu.edu/honorsprojects Part of the Paleobiology Commons Repository Citation Hamilton, Joanna, "Analysis of a Sponge Bioherm from the Hermosa Group, Molas Lake Area, Colorado" (2014). Honors Projects. 116. https://scholarworks.bgsu.edu/honorsprojects/116 This work is brought to you for free and open access by the Honors College at ScholarWorks@BGSU. It has been accepted for inclusion in Honors Projects by an authorized administrator of ScholarWorks@BGSU. Analysis of a Sponge Bioherm from the Hermosa Group, Molas Lake Area, Colorado Joanna Hamilton Bowling Green State University Department of Geology April 2013 Introduction: The Hermosa Group The Hermosa Group is a Pennsylvanian (~310 Ma) rock unit found in the southwestern San Juan Mountains and the Paradox Basin. The Paradox Basin is a northwest-southeast trending basin related to the Uncompahgre Uplift in the north, salt deposition and movement throughout, and a Precambrian fault system in the underlying basement rocks (Brown 2002, Trudgill and Arbuckle 2009). The Uncompahgre Uplift occurred in response to the Ouachita – Marathon Orogeny (related to the Ancestral Rocky Mountains Orogeny) caused by the collision of North America and South America-Africa during the Late Mississippian (~ 320 Ma) (Trudgill and Arbuckle 2009, Pazzaglia et al. 1999). The Paradox Basin formed as a complimentary subsidence basin alongside the uplifted area (Brown 2002). When the basin subsided, smaller structural features formed within it, including step-down grabens close to the uplift and folded areas further away (Baars and Stevenson 1981, Brown 2002). -
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. -
Chemistry of Chalk and Mgco3, Explored Through the Sport of Weightlifting
Teacher Notes: Chemistry of chalk and MgCO3, explored through the sport of weightlifting Sport: Weightlifting Age group: 11 - 14 These notes are designed as a guide on how to lead the session, and are written in a script format. If you wish to lead the session in a different way please feel free to do so. The red text indicates what each slide includes, while the blue text highlights the key points being discussed in each slide. The owl symbol demonstrates where students are required to perform a task (eg questions, experiment, etc.). These are used to help you observe the students learning and recap any information which the students have found difficult to understand. Depending on the level of student understanding this module may require two lessons to complete. Slide 1 Opening slide The first slide provides the title of the session and a picture of a weightlifter dusting chalk containing title of off his hands, introducing the topic and drawing a visual picture of the link between the session and background sport and chemistry. picture as a visual introduction. Slides 2 & 5 – Introduction – Weightlifting and the link to chemistry Weightlifting, the sport of lifting weights in a variety of ways to a variety of different positions, has routes back to ancient times, with the lifting of heavy stones to determine a person’s strength. This has continued through the ages and in many strongman contests today heavy stones are lifted, or attempted to be lifted. Slide 2 gives a small amount of Weightlifting as we know of it today started in Germany in the mid-1800s and quickly background to spread through the rest of Continental Europe. -
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