Campsites of the Big Bend Ranch State Park This Document Was Written and Produced by Gary Nored for the Big Bend Ranch State Park in Texas
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Geomorphological Studies of the Sedimentary Cuddapah Basin, Andhra Pradesh, South India
SSRG International Journal of Geoinformatics and Geological Science (SSRG-IJGGS) – Volume 7 Issue 2 – May – Aug 2020 Geomorphological studies of the Sedimentary Cuddapah Basin, Andhra Pradesh, South India Maheswararao. R1, Srinivasa Gowd. S1*, Harish Vijay. G1, Krupavathi. C1, Pradeep Kumar. B1 Dept. of Geology, Yogi Vemana University, Kadapa-516005, Andhra Pradesh, India Abstract: The crescent shaped Cuddapah basin located Annamalai Surface - at an altitude of over 8000’ (2424 mainly in the southern part of Andhra Pradesh and a m), ii. Ootacamund Surface – at 6500’-7500’ (1969- little in the Telangana State is one of the Purana 2272 m) on the west and at 3500’ (1060m) on the east basins. Extensive work was carried out on the as noticed in Tirumala hills, iii. Karnataka Surface - stratigraphy of the basin, but there is very little 2700’-3000’ (Vaidynathan, 1964). 2700-3300 reference (Vaidynathan,1964) on the geomorphology of (Subramanian, 1973) 2400-3000 (Radhakrishna, 1976), the basin. Hence, an attempt is made to present the iv. Hyderabad Surface – at 1600’ – 2000’v. Coastal geomorphology of the unique basin. The Major Surface – well developed east of the basin.vi. Fossil Geomorphic units correspond to geological units. The surface: The unconformity between the sediments of the important Physiographic units of the Cuddapah basin Cuddapah basin and the granitic basement is similar to are Palakonda hill range, Seshachalam hill range, ‘Fossil Surface’. Gandikota hill range, Velikonda hill range, Nagari hills, Pullampet valley and Kundair valley. In the Cuddapah Basin there are two major river systems Key words: Topography, Land forms, Denudational, namely, the Penna river system and the Krishna river Pediment zone, Fluvial. -
ACTIVITY 7 – MARKING GUIDELINE: 1. a – Cuesta B – Homoclinal Ridge C
ACTIVITY 7 – MARKING GUIDELINE: 1. A – Cuesta B – Homoclinal ridge C – Hogsback 2. Sedimentary 3. Inclined rocks with different resistance to erosion. Soft rock erodes away more quickly than hard rock. 4. The dip slope is 10–25° to the horizontal. Folding can result in cuesta basins and cuesta domes. 5. Farming can take place on dip slopes. Roads and railways can be built parallel to these landscapes. Gaps or poorts between homoclinal ridges can be good sites to build dams. Cuesta basins yield artesian water. Cuesta domes may contain oil and natural gas (fracking). Fertile valleys and plains between cuestas are suitable for human settlements. These ridges are used for forestry, tourism, recreation and nature conservation. These ridges can be used for defence purposes. (Accept any relevant answer) ACTIVITY 8 – MARKING GUIDELINE: 1. It occurs when strata are subjected to stress (compression, tension, volcanic intrusion, or tectonic movement) and they become tilted relative to their original (horizontal) position. Faulting or folding causes the strata to be tilted. The beds may be inclined in any direction with the angle of the dip slope between 0º to 90º. 2. Cuesta dome 3. The scarp slope faces inward, and dip slopes faces outward. 4. HOMOCLINICAL RIDGE: HOGSBACK: 5. HOMOCLINICAL RIDGE: HOGSBACK: • The angle of the dip slope lies 25º – 45º; • The angle of the dip slope is more than 45º; • Rivers cut poorts through the ridges; • There is very little difference in the gradient of the scarp and dip slopes ACTIVITY 9 – MARKING GUIDELINE: 1. A ridge that develop in tilted sedimentary rock characterised by a gentle slope and a steep slope 2. -
Part 629 – Glossary of Landform and Geologic Terms
Title 430 – National Soil Survey Handbook Part 629 – Glossary of Landform and Geologic Terms Subpart A – General Information 629.0 Definition and Purpose This glossary provides the NCSS soil survey program, soil scientists, and natural resource specialists with landform, geologic, and related terms and their definitions to— (1) Improve soil landscape description with a standard, single source landform and geologic glossary. (2) Enhance geomorphic content and clarity of soil map unit descriptions by use of accurate, defined terms. (3) Establish consistent geomorphic term usage in soil science and the National Cooperative Soil Survey (NCSS). (4) Provide standard geomorphic definitions for databases and soil survey technical publications. (5) Train soil scientists and related professionals in soils as landscape and geomorphic entities. 629.1 Responsibilities This glossary serves as the official NCSS reference for landform, geologic, and related terms. The staff of the National Soil Survey Center, located in Lincoln, NE, is responsible for maintaining and updating this glossary. Soil Science Division staff and NCSS participants are encouraged to propose additions and changes to the glossary for use in pedon descriptions, soil map unit descriptions, and soil survey publications. The Glossary of Geology (GG, 2005) serves as a major source for many glossary terms. The American Geologic Institute (AGI) granted the USDA Natural Resources Conservation Service (formerly the Soil Conservation Service) permission (in letters dated September 11, 1985, and September 22, 1993) to use existing definitions. Sources of, and modifications to, original definitions are explained immediately below. 629.2 Definitions A. Reference Codes Sources from which definitions were taken, whole or in part, are identified by a code (e.g., GG) following each definition. -
The Integration of Campsites in Cultural Landscapes: Architectural Actions on the Catalan Coast, Spain
sustainability Article The Integration of Campsites in Cultural Landscapes: Architectural Actions on the Catalan Coast, Spain Xavier Martín * , Anna Martínez and Isabela de Rentería IAR Group, School of Architecture La Salle, Ramon Llull University, 08022 Barcelona, Spain; [email protected] (A.M.); [email protected] (I.d.R.) * Correspondence: [email protected] Received: 29 June 2020; Accepted: 6 August 2020; Published: 12 August 2020 Abstract: Over the last 60 years, the development of tourism in Spain has produced an unprecedented occupation of the territory. Urban growth, hotels and infrastructures have transformed much of the natural environment. This phenomenon has irreversibly altered conditions of regions with great landscape value, putting their cultural heritage at risk. Yet, the campsite is a model of tourist settlement based on shared living in the open natural space. It promotes minimal and temporary interventions in the territory, by means of transportable accommodations with precise occupations of place, leaving a slight footprint. Therefore, architecture contributes to affording the order and services that these individual artifacts cannot provide by themselves. In terms of slight land occupation and natural qualities preservation, the campsite has proven to be one of the most responsible tourist models. It is an opportunity for the future: a resource for landscape integration and local dynamics reactivation. We present a set of architectural actions for the integration of campsites in cultural landscapes along the Catalan coast. These are recommendations catalogued by means of a diagnosis tool that proposes strategies at different levels, from enclosure to lodgings. Focusing on end-users, this research fosters cultural identity preservation and responsible communal living in nature. -
65Th Annual Tri-State Geological Field Conference 2-3 October 2004
65th Annual Tri-State Geological Field Conference 2-3 October 2004 Weis Earth Science Museum Menasha, Wisconsin The Lake & The Ledge Geological Links between the Niagara Escarpment and Lake Winnebago Joanne Kluessendorf & Donald G. Mikulic Organizers The Lake & The Ledge Geological Links between the Niagara Escarpment and Lake Winnebago 65th Annual Tri-State Geological Field Conference 2-3 October 2004 by Joanne Kluessendorf Weis Earth Science Museum, Menasha and Donald G. Mikulic Illinois State Geological Survey, Champaign With contributions by Bruce Brown, Wisconsin Geological & Natural History Survey, Stop 1 Tom Hooyer, Wisconsin Geological & Natural History Survey, Stops 2 & 5 William Mode, University of Wisconsin-Oshkosh, Stops 2 & 5 Maureen Muldoon, University of Wisconsin-Oshkosh, Stop 1 Weis Earth Science Museum University of Wisconsin-Fox Valley Menasha, Wisconsin WELCOME TO THE TH 65 ANNUAL TRI-STATE GEOLOGICAL FIELD CONFERENCE. The Tri-State Geological Field Conference was founded in 1933 as an informal geological field trip for professionals and students in Iowa, Illinois and Wisconsin. The first Tri-State examined the LaSalle Anticline in Illinois. Fifty-two geologists from the University of Chicago, University of Iowa, University of Illinois, Northwestern University, University of Wisconsin, Northern Illinois State Teachers College, Western Illinois Teachers College, and the Illinois State Geological Survey attended that trip (Anderson, 1980). The 1934 field conference was hosted by the University of Wisconsin and the 1935 by the University of Iowa, establishing the rotation between the three states. The 1947 Tri-State visited quarries at Hamilton Mound and High Cliff, two of the stops on this year’s field trip. -
Morphometric Factors in the Formation of Great Lakes Coastal Wetlands C
P1: GIM TJ1095-03 TJ-AEM.cls May 27, 2004 9:29 Morphometric factors in the formation of Great Lakes coastal wetlands C. E. Herdendorf Department of Geological Sciences, The Ohio State University, Columbus, Ohio 43210, USA; E-mail: [email protected] The Great Lakes basins were carved from ancient river valleys by continental ice sheets that receded from the region less than 10,000 years ago. Not only did the glaciers create the basins now holding the lakes, but they are responsible for many of the shallow depressions in the coastal margin that have since developed as coastal wetlands of various types. For the past four thousand years, coastal processes in the lakes have further modified the shore topography to form embayments, coastal lagoons, estuaries, deltas, and solution basins where thousands of hectares of wetlands have become established. This paper will explore the origin of the various morphometric forms which these wetlands have taken and their characteristic hydrologic processes. Keywords: estuaries, geomorphology, karst, lacustrine, palustrine, physiography Physiography of the Great Lakes gin of the waning ice sheet retreated northward into the newly carved lake basins, some of which were dammed The five adjoining Laurentian Great Lakes— by glacial end moraines. The early ice-margin lakes ex- Superior, Michigan, Huron, Erie, and Ontario—extend panded as the glacial ice masses shrank. However, as 1,370 km from westernmost point to easternmost point new and lower outlets were uncovered to the north, the and 1,130 km from north to south (Figure 1). With lakes drained to ever lowering levels except during peri- a total surface area of 244,160 km2, this is the largest ods of minor readvances of the ice front (Hough, 1962). -
LAND by the LAKES Nearshore Terrestrial Ecosystems
State of the Lakes Ecosystem Conference 1996 Background Paper THE LAND BY THE LAKES Nearshore Terrestrial Ecosystems Ron Reid Bobolink Enterprises Washago, Ontario Canada Karen Holland U.S. Environmental Protection Agency Chicago, Illinois U.S.A. October 1997 ISBN 0-662-26033-3 EPA 905-R-97-015c Cat. No. En40-11/35-3-1997E ii The Land by the Lakes—SOLEC 96 Table of Contents Acknowledgments ................................................................. v 1. Overview of the Land by the Lakes .................................................. 1 1.1 Introduction ............................................................ 1 1.2 Report Structure ......................................................... 2 1.3 Conclusion ............................................................. 2 1.4 Key Observations ........................................................ 3 1.5 Moving Forward ......................................................... 5 2. The Ecoregional Context .......................................................... 6 2.1 Why Consider Ecoregional Context? .......................................... 6 2.2 Classification Systems for Great Lakes Ecoregions ............................... 7 3. Where Land and Water Meet ....................................................... 9 3.1 Changing Shapes and Structures ............................................. 9 3.1.1 Crustal Tilting ................................................. 10 3.1.2 Climate ....................................................... 10 3.1.3 Erosion ...................................................... -
The Cretaceous Geology of the East Texas Basin Ronald D
Thesis Abstracts thinking is more important than elaborate FRANK CARNEY, PH.D. PROFESSOR OF GEOLOGY BAYLOR UNIVERSITY 1929-1934 Objectives of Geological Training at Baylor The training of a geologist in a university covers but a few years; his education continues throughout his active life. The purposes of train ing geologists at Baylor University are to provide a sound basis of understanding and to foster a truly geological point of view, both of which are essential for continued professional growth. The staff considers geology to be unique among sciences since it is primarily a field science. All geologic research in cluding that done in laboratories must be firmly supported by field observations. The student is encouraged to develop an inquiring ob jective attitude and to examine critically all geological concepts and principles. The development of a mature and professional attitude toward geology and geological research is a principal concern of the department. Cover: Trinity Group isopach map illustrating depositional trends of Trinity rocks. (From French) THE BAYLOR PRINTING SERVICE WACO, TEXAS BAYLOR GEOLOGICAL STUDIES BULLETIN NO. 52 THESIS ABSTRACTS These abstracts are taken from theses written in partial fulfillment of degree requirements at Baylor University. The original, unpublished versions of the theses, complete with appendices and bibliographies, can be found in the Ferdinand Roemer Library, Department of Geology, Baylor University, Waco, Texas. BAYLOR UNIVERSITY Department of Geology Waco, Texas Fall Baylor Geological Studies EDITORIAL STAFF Janet L. Burton, Editor O. T. Hayward, Ph.D., Advisor, Cartographic Editor Stephen I. Dworkin, Ph.D. general and urban geology and what have you geochemistry, diagenesis, and sedimentary petrology Joe C. -
Sample Itineraries for Bold & Gold Expeditions All Backpacking Trips
*Note: The itineraries given therein are intended to be a sample schedule of each type of trip. These may change due to circumstances such as weather and the skill level of participants. *SAMPLE ITINERARIES FOR BOLD & GOLD EXPEDITIONS ALL BACKPACKING TRIPS DAILY TRAVEL TIME Hiking mileage will vary from trip to trip, but groups will cover between 3-10 miles a day *SAMPLE ITINERARY Day 1: Arrive at base camp, gear check, safety briefing, lunch, shuttle to trail head campsite Days 2-4: Hike to new camping destination, explore around their campsite, cook dinner, enjoy team-building activities Day 3, 4 or 5: Layover Day: a chance to camp at the same spot 2 nights in a row. Day hiking, exploring the area, outdoor skills, games FOR 1-WEEK TRIPS: Day 6-7: Final backpacking day Day 8: Return to Basecamp in Seattle, unpack gear, closing circle FOR 2-WEEK TRIPS: Days 6-7: Participants continue to learn about each other through team-building activities and take turns being “leader of the day” on the trail Day 8: A staff member will meet the group at a front country campsite with a re-ration of food and supplies Days 9-13: Participants will take on more responsibility and leadership, practicing Leave No Trace principles, cooking meals for the group and navigating the terrain. There will be another layover day Day 14: Final backpacking day Day 15: Return to Basecamp in Seattle, unpack gear, closing circle 1 WEEK TRIPS: 2 WEEK TRIPS: • Backpacking & Fishing • American Alps • Backpacking & Yoga • Backpacking & Leadership • Beyond City Limits • Backpacks, Beaches & Boulders** • Call of the North Cascades • Backpacks & Kayaks*** • Cascade Challenge • Mountain & Music • Fierce & Fabulous • Powerful Gifts**** • Make A Scene: Art & Backpacking • Olympic Coastal Backpacking • Olympic Coastal Challenge • Poets & Peaks • She-Nannigans! *Note: The itineraries given therein are intended to be a sample schedule of each type of trip. -
Cuesta Del Cura Limestone
BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA VOL. 49, PP. 1651-1694. 7 PLS., 6 FIGS. NOVEM BER 1, 1938 STUDIES OF THE MEXICAN GEOSYNCLINE BY EALPH W. IMLAY CONTENTS Page Abstract....................................................................................................................................... 1652 Introduction............................................................................................................................... 1652 Acknowledgments..................................................................................................................... 1654 Earlier investigations............................................................................................................... 1654 Geography................................................................................................................................... 1654 Topography and drainage.............................................................................................. 1654 Culture................................................................................................................................ 1655 Sedimentary rocks..................................................................................................................... 1657 General discussion.......................................................................................................... 1657 Jurassic system................................................................................................................. 1657 Zuloaga -
Pleistocene Geology of Kansas
3 6 3 7 Pleistocene Geology of Kansas By JOHN C. FRYE and A. BYRON LEONARD UNIVERSITY OF KANSAS PUBLICATIONS STATE GEOLOGICAL SURVEY OF KANSAS BULLETIN 99 1952 THE UNIVERSITY OF KANSAS STATE GEOLOGICAL SURVEY OF KANSAS FRANKLIN D. MURPHY, M. D. Chancel/or of the University, and ex officio Director of the Survey JOHN C. FRYE, Ph.D., RAYMOND C. MOORE, Ph.D., Sc.D., Executive Director State Geologist and Director of Research. BULLETIN 99 PLEISTOCENE GEOLOGY OF KANSAS By JOHN C. FRYE AND A. BYRON LEONARD Printed by authority of the State of Kansas Distributed from Lawrence NOVEMBER, 1952 STATE OF KANSAS EDWARD F. AR N, Governor STATE BOARD OF REGENTS OSCAR STAUFFER, Chairman WALTER FEES DREW MCLAUGHLIN MRS. LEO HAUGHEY LESTER McCoy A. W. HERSHBERGER GROVER POOLE Wn.us N. KELLY LAVERNE B. SPAKE MINERAL INDUSTRIES COUNCIL B. 0. WEAVER ('53), Chairman BRIAN O'BRIAN ('55), Vice-Chairman LESTER McCoy ('52) M. L. BREIDEN'THAL ('54) J. E. MISSLMER ('52) HOWARD CAREY ('54) CHARLES COOK ('52) JOHN L. GARLOUGH ('54) K. A. SPENCER ('53) 0. W. BILHARZ ('55) W. L. STRYKER ('53) GEORGE K. MACKIE, JR. ('55) STATE GEOLOGICAL SURVEY OF KANSAS FRANKLIN D. MURPHY, M.D., Chancellor of the University of Kansas, and ex officio Director of the Survey JOHN C. FRYE, Ph.D. RAYMOND C. MOORE, Ph.D., Sc.D. Executive Director State Geologist and Director of Research BASIC GEOLOGY MINERAL RESOURCES STRATIGRAPHY, AREAL GEOLOGY, AND PA- OIL AND GAS LEONTOLOGY Edwin D. Goebel, M.S., Geologist John M. Jewett, Ph.D., Geologist Walter A. -
Family Electric Campground
North LEGEND POTATO CREEK STATE PARK Road Hiking Trail Family Electric Campground Fire Ring Water Filling Station 29 27 118 117 30 25 120 115 *Comfort Station 31 23 113 122 111 33 28 26 22 119 116 Mountain Biking 32 24 123 121 114 110 21 34 125 124 112 108 Vault Toilet 35 20 19 36 127 126 109 107 Beach 37 18 17 39 129 128 106 105 41 38 15 Accessible 16 130 104 40 131 103 11 42 5 7 9 14 13 132 102 Playground 134 101 133 General Store 1 2 3 4 6 8 10 136 99 100 12 135 138 97 98 Camp Gatehouse 51 50 48 46 44 43 94 53 137 92 rail 5 90 96 T 54 139 Dumping Station 88 95 56 52 49 47 45 55 86 91 93 87 89 Parking 57 59 84 85 Nature Center 58 61 82 83 60 Campground Host 63 81 62 65 80 Playfield Drinking Fountain 64 79 67 Emergency Call Box 66 78 77 69 68 76 73 75 Campfire Boat Rental 70 74 71 Circle *All comfort stations are accessible. 72 To Trail 1 212 211 214 209 215 207 213 well house 210 205 217 203 216 208 202 206 269 268 218 201 271 266 204 264 141 220 200 273 T 270 267 263 ra 140 222 229 275 272 265 il 143 227 228 274 262 5 142 219 277 145 221 276 287 261 223 224 225 226 279 281 283 285 144 198 199 230 259 146 184 286 260 196 278 280 282 284 148 147 183 197 231 232 185 182 194 258 257 149 186 181 195 192 233 234 256 1 150 187 180 193 255 151 188 179 235 152 189 191 237 254 253 153 190 236 239 154 177 250 252 242 178 248 155 175 238 243 246 251 157 173 176 2 156 249 174 241 247 159 244 245 • 158 170 172 l 171 i 160 161 168 ra 166 169 T 162 167 e r 163 165 to 164 3 S l ra e Trail Beach n e G Cabins 21 20 19 18 17 16 il 4 Tra .