Middle Park Stratigraphic Chart

Total Page:16

File Type:pdf, Size:1020Kb

Middle Park Stratigraphic Chart Middle Park Hydrogeologic Geologic Period Phase Stratigraphic Unit Unit Modern Alluvium and outwash deposits Alluvial Aquifer Quaternary Glacial deposits Glacial deposits Glaciation Older stream and outwash terrace Local perched deposits aquifer Grouse Mountain Basalt Volcanics Neogene Extension Troublesome Troublesome Formation Aquifer Rabit Ears Volcanics Volcanics Transition White River White River Formation Paleogene Aquifer Middle Park Middle Park Formation Aquifer Laramide Windy Gap Volcanic Volcanics Formation Middle ParkMiddle Member Pierre Shale Pierre confining Niobrara Formation unit Cretaceous Interior Seaway Benton Group Dakota Sandstone Dakota Aquifer Jurassic Morrison Formation Morrison Aquifer Mesozoic Triassic Sandstones Permian Ancestral Pennsylvanian Rocky Mountains Mississippian No strata Devonian Silurian Stable Ordovician Cambrian Crystalline rocks of igneous and Crystalline Precambrian Precambrian metamorphic origin in mountainous bedrock region Table 12a-06-02. Middle Park stratigraphic chart. Middle Park Unit Thickness Hydrogeologic Geologic Period Phase Stratigraphic Unit Physical Characteristics Hydrologic Characteristics (ft) Unit Well to poorly-sorted, uncemented sands, silts and gravels along modern Modern Alluvium and outwash deposits Alluvial Aquifer streams and as valley-fill Unstratified sand, gravel, and silt within, and at the mouths of, mountain Glacial deposits Glacial deposits Quaternary valleys Glaciation Older stream and outwash terrace Well to poorly-sorted, uncemented sands, silts and gravels on bedrock- Local perched deposits cored terraces above modern streams aquifer Grouse Mountain Basalt Basalt flow caprock Volcanics Neogene Extension Tuffaceous siltstone, fine-grained sandstone, glass shards, weathered ash, Troublesome Unconfined aquifer where tuffaceous siltstone is absent, confined where Troublesome Formation 0-1,000 and conglomerate Aquifer siltstone is present Interbeded tuff, tuff breccia and volcanic breccia interlayered with flows of Rabit Ears Volcanics 0 - 1,500 Volcanics intermediate composition Transition White River White River Formation Continental lakebed deposit Limited aquifer Paleogene Aquifer Middle Park Middle Park Formation 2,500-5,000 Sandstone, conglomerate and shale Aquifer Laramide Windy Gap Volcanic 0-700 Gray volcanic breccia, conglomearte and andesitic flows Volcanics Formation Middle Park Middle Park Member Pierre Shale 200-5,000 Dark-gray to brown shale, sandstone 1,500 feet above base Pierre confining Sandstone and limestone beds might yield limited water Niobrara Formation 400-500 Calcareous shale and limestone unit Cretaceous Interior Seaway Benton Group 0->300 Calcareous shale and limestone Lower sandstone, local basal conglomerate, middle shale, and upper Dakota Sandstone 140-400 Dakota Aquifer sandstone Jurassic Morrison Formation 25-400 Variegated clay shale and mudstone, sandstone at base and top Morrison Aquifer Limited aquifer Mesozoic Triassic Sandstones Permian Ancestral Pennsylvanian Rocky Mountains Mississippian No strata Devonian Silurian Stable Ordovician Cambrian Crystalline Precambrian Precambrian Crystalline rocks of igneous and metamorphic origin in mountainous region bedrock Table 12a-06-02. Middle Park stratigraphic chart, detailed. Colorado Geological Survey ON-010 Colorado Groundwater Atlas. Sources: Tweto (1957); Voegeli (1965); Izett (1966); Glover and others (1998); Kellogg and others (2008); Cole and Braddock (2009); Cole and others (2010); Raynolds and Hagadorn (2017).
Recommended publications
  • Blue River Valley Stratigraphic Chart
    Blue River Valley Hydrogeologic Geologic Period Phase Stratigraphic Unit Unit Modern Alluvium and outwash deposits Alluvial Aquifer Quaternary Glacial deposits Glacial deposits Glaciation Older stream and outwash terrace Local perched deposits aquifer Troublesome Formation Local aquifer Neogene Extension Volcanic rocks Volcanics Paleogene Transition Paleogene and Cretaceous intrusive Crystalline rocks bedrock Laramide Pierre Shale Smoky Hill Member Fort Hayes Limestone Pierre confining Niobrara Niobrara Formation Cretaceous unit Interior Carlile Shale Seaway Greenhorn Limestone Graneros Shale Benton Group Dakota Sandstone Dakota Aquifer Morrison Formation Morrison Aquifer Jurassic Mesozoic Entrada Sandstone Entrada Aquifer Sandstones Chinle confining Triassic Chinle Formation unit Permian Maroon Formation Ancestral Maroon-Minturn Rocky Aquifer Mountains Minturn Formation Pennsylvanian Mississippian No strata Devonian Chaffee Group Paleozoic Silurian Mississippian- Carbonates Cambrian Ordovician Manitou Formation carbonate aquifer Dotsero Formation and Cambrian Sawatch Sandstone Crystalline rocks of igneous and Crystalline Precambrian Precambrian metamorphic origin in mountainous bedrock region Table 12a-05-01. Blue River Valley stratigraphic chart. Blue River Valley Unit Thickness Hydrogeologic Geologic Period Phase Stratigraphic Unit Physical Characteristics Hydrologic Characteristics (ft) Unit Well to poorly-sorted, uncemented sands, silts and gravels along modern Modern Alluvium and outwash deposits >35 Alluvial Aquifer streams and
    [Show full text]
  • 8.4.0 Wolford Mountain Site C 8.4.1 Location And
    8.4.0 WOLFORD MOUNTAIN SITE C 8.4.1 LOCATION AND TOPOGRAPHY Wolford Mountain Site C is located on Muddy Creek, 5 miles north of Kremmling, Colorado and 3.8 miles upstream from Site A'. The dam site is a 250-foot wide canyon with sides that rise steeply to a height of approximately 80 feet. At that point, the left abutment is relatively flat for about 500 feet, continuing east to the base of Wolford Mountain. The right abutment slopes gently upwards towards Highway U.S. 40, located 0.7 miles west of the site. Figure 8.4.1 presents a plan view of the Wolford Mountain Site C. A 120-foot high dam at Site C would impound a reservoir of 60,000 af capacity with a water surface elevation of 7485 feet. This is 10 feet higher than the water surface elevation proposed for an alternative reservoir at Site A'. Approximately 1900 acres would be occupied by the reservoir and lake shore area. An area-capacity curve is presented on Figure 8.4.2. 8.4.2 PRIOR STUDIES Wolford Mountain Site C has been under investigation by the CRWCD. A report titled "Rock Creek Dam Project", prepared by Morrison-Knudsen Engineers, Inc. (1986) for the River District, considered three reservoir capacities for this Muddy Creek Site: 60,000, 46,800 and 30,400 af. The feasibility report illustrates a preliminary design for the selected 46,800 af size. Information from this report has been liberally incorporated into this section on Wolford Mountain Site C. The report titled "Seismotectonic Hazard Evaluation, Rock Creek Project Near Kremmling, Grand And Routt Counties, Colorado", was prepared by Michael West and Associates (1986) for Morrison-Knudsen Engineers as part of their study for the CRWCD.
    [Show full text]
  • Vol. 7 National Family Farm Discovery Dox
    Case: 19-70115, 08/13/2019, ID: 11396549, DktEntry: 36-7, Page 1 of 233 No. 19-70115 UNITED STATES COURT OF APPEALS FOR THE NINTH CIRCUIT NATIONAL FAMILY FARM COALITION, et al., Petitioners, v. UNITED STATES ENVIRONMENTAL PROTECTION AGENCY, et al., Respondents, and MONSANTO COMPANY, Intervenor-Respondent. ON PETITION FOR REVIEW FROM THE UNITED STATES ENVIRONMENTAL PROTECTION AGENCY PETITIONERS’ EXCERPTS OF RECORD VOLUME VII of IX ______________________ CENTER FOR FOOD SAFETY CENTER FOR BIOLOGICAL George A. Kimbrell DIVERSITY Sylvia Shih-Yau Wu Stephanie M. Parent Amy van Saun PO Box 11374 2009 NE Alberta St., Suite 207 Portland, OR 97211 Portland, OR 97211 T: (971) 717-6404 T: (971) 271-7372 [email protected] [email protected] [email protected] [email protected] Counsel for Petitioners Case: 19-70115, 08/13/2019, ID: 11396549, DktEntry: 36-7, Page 2 of 233 INDEX TO PETITIONERS’ EXCERPTS OF RECORD VOLUME I Admin. R. ER Date 1 Document Description Doc. No. Page No. 2 11/1/2018 M.8 Registration Decision for the ER 0001 Continuation of Uses of Dicamba on Dicamba Tolerant Cotton and Soybean 11/1/2018 M.9 Approval Master Label for EPA ER 0025 Registration No. 524-617, Primary Brand Name: M1768 Herbicide Alternate Brand Name: XtendiMax® With VaporGrip® Technology 11/5/2018 M.4 Notice of Conditional Registration ER 0065 and Approved Master Label for EPA Registration No. 524-617, Primary Brand Name: M1768 Herbicide Alternate Brand Name: XtendiMax® With VaporGrip® Technology 11/5/2018 M.3 Notice of Conditional Registration ER 00121 EPA Reg Number 352-913 DuPont FeXapan Herbicide Decision 545658 and Approved Label 11/1/2018 M.5 Notice of Conditional Registration ER 0167 EPA Registration Number 7969- 345 Engenia Herbicide Decision No.
    [Show full text]
  • Geologic Map of the Southern Espanola Basin
    GEOLOGIC MAP OF THE SOUTHERN ESPAÑOLA BASIN, SANA FE COUNTY, NEW MEXICO By Daniel J. Koning and Adam S. Read October, 2010 OPEN-FILE REPORT 531 DESCRIPTION OF MAP UNITS Descriptive terminology Below are descriptions of the units depicted on the geologic map. Grain sizes follow the Udden- Wentworth scale for clastic sediments (Udden, 1914; Wentworth, 1922) and are based on field estimates. Pebbles are subdivided as shown in Compton (1985). The term “clast(s)” refers to the grain size fraction greater than 2 mm in diameter and the term “matrix” refers to the particles less than 2 mm in size. Clast percentages are based on percent volume and were estimated in the field with the aid of percentage charts. Descriptions of bedding thickness follow Ingram (1954). Colors of unconsolidated sediment are based on visual comparison of dry samples to the Munsell Soil Color Charts (Munsell Color, 1994). Soil horizon designations and descriptive terms follow those of the Soil Survey Staff (1992). Birkeland (1999), and Birkeland et al. (1991). Stages of pedogenic calcium carbonate morphology follow those of Gile et al. (1966) and Birkeland (1999). Metric units are used in this report (see Table 1 for conversion of English units to metric units). The divisions of geologic time used in this report are provided below (Table 2). Table 1. Factors for conversion of metric units to English units _______________________________________________________ Multiply By To obtain _______________________________________________________ centimeters (cm) 0.3937 inches
    [Show full text]
  • Permophiles Issue #58 November 2013 EXECUTIVE NOTES Notes from the SPS Secretary Museum of Natural History and Science, Albuquerque, New Mexico, USA, May 20-22, 2013
    Table of Contents Notes from the SPS Secretary 1 Lucia Angiolini Notes from the SPS Chair 2 Shuzhong Shen Subcommission on Permian Stratigraphy Annual Report 2013 3 Shuzhong Shen, SPS Chairman Officers and Voting Members since August, 2012 5 The Reality of GSSPs 6 Stanley C. Finney GSSPs (Global Stratotype Section and Point) and Correlation 8 Stanley C. Finney We Need a New GSSP for the Base of the Permian 8 Spencer G. Lucas The GSSP at the Aidaralash section is solid and has no alternative 13 Vladimir I. Davydov The Aidaralash GSSP—Reply to Davydov 15 Spencer G. Lucas Proposal for the Global Stratotype Section and Point (GSSP) for the base-Sakmarian Stage (Lower Permian) 16 Valery V. Chernykh, Boris I. Chuvashov, Shuzhong Shen andCharles M. Henderson Proposal for the Global Stratotype Section and Point (GSSP) for the base-Artinskian Stage (Lower Permian) 26 Boris I. Chuvashov, Valery V. Chernykh, Shuzhong Shen and Charles M. Henderson Report of the Chinese, Iranian, Italian working group: The Permian-Triassic boundary sections of Julfa and Zal revisited 34 Lucia Angiolini, Shuzhong Shen, Maryamnaz Bahrammanesh, Syrus Abbasi, Mina Birjandi, Gaia Crippa, Dongxun Yuan and Claudio Garbelli Age assignment of section 4 of Teichert et al. (1973) at Ali Bashi Mountains (Julfa, NW Iran) 36 Abbas Ghaderi, Ali Reza Ashouri, Heinz W. Kozur and Dieter Korn Report of field excursions 2012/2013 of the “Sino-German Cooperation Group on the Late Palaeozoic Palaeobiology, Stratigraphy and Geochemistry” between Europe and China 40 Jun Wang, Shuzhong Shen, Joerg W. Schneider and Hans Kerp ANNOUNCEMENTS 42 SUBMISSION GUIDELINES FOR ISSUE 59 44 Photo 1: The Permian-Triassic succession of the Ali Bashi Mountains, Julfa, NW Iran.
    [Show full text]
  • Rocky Mountain National Park Geologic Resource Evaluation Report
    National Park Service U.S. Department of the Interior Geologic Resources Division Denver, Colorado Rocky Mountain National Park Geologic Resource Evaluation Report Rocky Mountain National Park Geologic Resource Evaluation Geologic Resources Division Denver, Colorado U.S. Department of the Interior Washington, DC Table of Contents Executive Summary ...................................................................................................... 1 Dedication and Acknowledgements............................................................................ 2 Introduction ................................................................................................................... 3 Purpose of the Geologic Resource Evaluation Program ............................................................................................3 Geologic Setting .........................................................................................................................................................3 Geologic Issues............................................................................................................. 5 Alpine Environments...................................................................................................................................................5 Flooding......................................................................................................................................................................5 Hydrogeology .............................................................................................................................................................6
    [Show full text]
  • Proposed Members of the Chamita Formation, North-Central New Mexico Daniel J
    New Mexico Geological Society Downloaded from: http://nmgs.nmt.edu/publications/guidebooks/56 Proposed members of the Chamita Formation, north-central New Mexico Daniel J. Koning and Scott B. Aby, 2005, pp. 258-278 in: Geology of the Chama Basin, Lucas, Spencer G.; Zeigler, Kate E.; Lueth, Virgil W.; Owen, Donald E.; [eds.], New Mexico Geological Society 56th Annual Fall Field Conference Guidebook, 456 p. This is one of many related papers that were included in the 2005 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.
    [Show full text]
  • Origin and Migration of Petroleum in the Gidgealpa Ridge Area, Cooper/Eromanga Basins, South Australia
    ORIGIN AND MIGRATION OF PETROLEUM IN THE GIDGEALPA RIDGE AREA, COOPER/EROMANGA BASINS, SOUTH AUSTRALIA A thesis presented by CHRISTIAN OLIVIER EDUARD HALLMANN To the Geological Institute In partial fulfilment of the requirements for the degree of DIPLOM In the subject GEOLOGIE-PALAEONTOLOGIE Diplomarbeit Diploma thesis University of Cologne Cologne, Germany WS ’04 / ’05 ORIGIN AND MIGRATION OF PETROLEUM IN THE GIDGEALPA RIDGE AREA, COOPER/EROMANGA BASINS, SOUTH AUSTRALIA Christian O.E. Hallmann _________________________________________ Nothing in nature is random… A thing appears random only through the incompleteness of our knowledge Spinoza, Ethics I ____________________________________________________ CONTENTS Contents Contents I List of Figures IV List of Tables VII Declaration VIII Acknowledgements IX Abstract (English) X Abstract (German) XII CHAPTER ONE INTRODUCTION 1 1.1 Scope of this thesis 2 1.2 Location of the study area 3 1.3 History of petroleum exploration 4 CHAPTER TWO REGIONAL GEOLOGY 5 2.1 Geological evolution of Australia 5 2.2 Tectonic setting 6 2.2.1 Warburton Basin 7 2.2.2 Cooper Basin 9 2.2.3 Eromanga Basin 9 2.2.4 Study area 9 2.3 Sedimentary record 10 2.3.1 Warburton Basin units 10 2.3.2 Cooper Basin units 12 2.3.3 Eromanga Basin units 16 CHAPTER THREE PETROLEUM GEOLOGY 19 3.1 Introduction 19 3.2 Source rocks 19 I CONTENTS 3.3 Reservoirs 20 3.4 Traps 21 3.5 Oils 21 3.6 Thermal and subsidence history and expulsion events 22 3.7 Study area 23 CHAPTER FOUR EXPERIMENTAL 26 4.1 Sample selection 26 4.2 Sequential flow
    [Show full text]
  • Geologic Map of Washington - Northwest Quadrant
    GEOLOGIC MAP OF WASHINGTON - NORTHWEST QUADRANT by JOE D. DRAGOVICH, ROBERT L. LOGAN, HENRY W. SCHASSE, TIMOTHY J. WALSH, WILLIAM S. LINGLEY, JR., DAVID K . NORMAN, WENDY J. GERSTEL, THOMAS J. LAPEN, J. ERIC SCHUSTER, AND KAREN D. MEYERS WASHINGTON DIVISION Of GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-50 2002 •• WASHINGTON STATE DEPARTMENTOF 4 r Natural Resources Doug Sutherland· Commissioner of Pubhc Lands Division ol Geology and Earth Resources Ron Telssera, Slate Geologist WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES Ron Teissere, State Geologist David K. Norman, Assistant State Geologist GEOLOGIC MAP OF WASHINGTON­ NORTHWEST QUADRANT by Joe D. Dragovich, Robert L. Logan, Henry W. Schasse, Timothy J. Walsh, William S. Lingley, Jr., David K. Norman, Wendy J. Gerstel, Thomas J. Lapen, J. Eric Schuster, and Karen D. Meyers This publication is dedicated to Rowland W. Tabor, U.S. Geological Survey, retired, in recognition and appreciation of his fundamental contributions to geologic mapping and geologic understanding in the Cascade Range and Olympic Mountains. WASHINGTON DIVISION OF GEOLOGY AND EARTH RESOURCES GEOLOGIC MAP GM-50 2002 Envelope photo: View to the northeast from Hurricane Ridge in the Olympic Mountains across the eastern Strait of Juan de Fuca to the northern Cascade Range. The Dungeness River lowland, capped by late Pleistocene glacial sedi­ ments, is in the center foreground. Holocene Dungeness Spit is in the lower left foreground. Fidalgo Island and Mount Erie, composed of Jurassic intrusive and Jurassic to Cretaceous sedimentary rocks of the Fidalgo Complex, are visible as the first high point of land directly across the strait from Dungeness Spit.
    [Show full text]
  • Colorado Headwaters Laramide Basin Stratigraphic Chart
    Colorado Headwaters Laramide Hydrogeologic Geologic Period Phase Stratigraphic Unit Unit Modern- Alluvium associated with present Quaternary Alluvial Aquifers Glaciation rivers Grouse Mountain Basalt Volcanics Neogene Extension Troublesome- Troublesome- North Park Formations North Park Aquifer Rabit Ears Volcanics Volcanics Transition White River White River Formation Aquifer Paleogene Coalmont Formation Coalmont Aquifer Laramide Middle Park Middle Park Formation Aquifer Windy Gap Volcanic Volcanics Formation Middle ParkMiddle Member Pierre confining Pierre Shale unit Cretaceous Interior Regional Cretaceous Seaway shale- Seaway dominated formations form multiple hydrogeologic units, most are confining units Colorado Piedmont Region Jurassic Multiple sedimentary units deposited Mesozoic in the stable continent interior may be Sandstones Triassic present that may form aquifers Permian Ancestral Rocky No strata Pennsylvanian Mountains Mississippian Devonian Paleozoic Silurian No strata Carbonates Ordovician Cambrian Crystalline rocks of igneous and Crystalline Precambrian Precambrian metamorphic origin in mountainous bedrock region Table 11b-02-08-01. Colorado Headwaters Laramide Basin stratigraphic chart. Colorado Headwaters Laramide Unit Thickness Hydrogeologic Geologic Period Phase Stratigraphic Unit Physical Characteristics Hydrologic Characteristics (ft) Unit Modern- Quaternary Alluvium associated with present rivers Alluvial Aquifers Glaciation Grouse Mountain Basalt Basalt flow caprock Volcanics Neogene Extension Troublesome- Unconfined
    [Show full text]
  • Mojave Miocene Robert E
    Mojave Miocene Robert E. Reynolds, editor California State University Desert Studies Center 2015 Desert Symposium April 2015 Front cover: Rainbow Basin syncline, with rendering of saber cat by Katura Reynolds. Back cover: Cajon Pass Title page: Jedediah Smith’s party crossing the burning Mojave Desert during the 1826 trek to California by Frederic Remington Past volumes in the Desert Symposium series may be accessed at <http://nsm.fullerton.edu/dsc/desert-studies-center-additional-information> 2 2015 desert symposium Table of contents Mojave Miocene: the field trip 7 Robert E. Reynolds and David M. Miller Miocene mammal diversity of the Mojave region in the context of Great Basin mammal history 34 Catherine Badgley, Tara M. Smiley, Katherine Loughney Regional and local correlations of feldspar geochemistry of the Peach Spring Tuff, Alvord Mountain, California 44 David C. Buesch Phytoliths of the Barstow Formation through the Middle Miocene Climatic Optimum: preliminary findings 51 Katharine M. Loughney and Selena Y. Smith A fresh look at the Pickhandle Formation: Pyroclastic flows and fossiliferous lacustrine sediments 59 Jennifer Garrison and Robert E. Reynolds Biochronology of Brachycrus (Artiodactyla, Oreodontidae) and downward relocation of the Hemingfordian– Barstovian North American Land Mammal Age boundary in the respective type areas 63 E. Bruce Lander Mediochoerus (Mammalia, Artiodactyla, Oreodontidae, Ticholeptinae) from the Barstow and Hector Formations of the central Mojave Desert Province, southern California, and the Runningwater and Olcott Formations of the northern Nebraska Panhandle—Implications of changes in average adult body size through time and faunal provincialism 83 E. Bruce Lander Review of peccaries from the Barstow Formation of California 108 Donald L.
    [Show full text]
  • EIS-0386-DEIS-02-2007.Pdf
    Draft WWEC PEIS September 2007 DOCUMENT CONTENTS VOLUME I Executive Summary Chapter 1: Why Are Federal Agencies Proposing to Designate Energy Corridors in the West? Chapter 2: What Are the Alternatives Evaluated in This PEIS? Chapter 3: What Are the Potential Environmental Consequences of Corridor Designation and Land Use Plan Amendment? Chapter 4: How Are Cumulative Impacts Evaluated? Chapter 5: What Unavoidable Adverse Impacts Might Be Caused by Corridor Designation and Land Use Plan Amendment? Chapter 6: The Relationship between Local Short-Term Uses of the Environment and Long-Term Productivity Chapter 7: What Irreversible and Irretrievable Commitment of Resources Would Be Involved with Implementation of the Alternatives? Chapter 8: List of Preparers Chapter 9: References Chapter 10: Glossary VOLUME II Appendix A: Proposed Land Use Plan Amendments Appendix B: Summary of Public Scoping Comments for the Programmatic Environmental Impact Statement, Designation of Energy Corridors on Federal Land in the 11 Western States (DOE/FS-0386) Appendix C: Tribal Consultation Appendix D: Federal and State Regulatory Requirements Potentially Applicable When Designating Energy Corridors Appendix E: Energy Transport Technologies and Hypothetical Energy Transport Projects Appendix F: Section 368 Corridor Parameters Appendix G: Sensitive Resource Areas That Would Be Intersected by Proposed West-wide Energy Corridors Appendix H: Geographic Information System Data Appendix I: Summary of WWEC PEIS Webcasts for Corridor Review and Revision, 6/19/06 to 4/24/07
    [Show full text]