R6 Geomorphology Legend and Glossary
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The Geology of the Enosburg Area, Vermont
THE GEOLOGY OF THE ENOSBURG AREA, VERMONT By JOlIN G. DENNIS VERMONT GEOLOGICAL SURVEY CHARLES G. DOLL, State Geologist Published by VERMONT DEVELOPMENT DEPARTMENT MONTPELIER, VERMONT BULLETIN No. 23 1964 TABLE OF CONTENTS PAGE ABSTRACT 7 INTRODUCTION ...................... 7 Location ........................ 7 Geologic Setting .................... 9 Previous Work ..................... 10 Method of Study .................... 10 Acknowledgments .................... 10 Physiography ...................... 11 STRATIGRAPHY ...................... 12 Introduction ...................... 12 Pinnacle Formation ................... 14 Name and Distribution ................ 14 Graywacke ...................... 14 Underhill Facics ................... 16 Tibbit Hill Volcanics ................. 16 Age......................... 19 Underhill Formation ................... 19 Name and Distribution ................ 19 Fairfield Pond Member ................ 20 White Brook Member ................. 21 West Sutton Slate ................... 22 Bonsecours Facies ................... 23 Greenstones ..................... 24 Stratigraphic Relations of the Greenstones ........ 25 Cheshire Formation ................... 26 Name and Distribution ................ 26 Lithology ...................... 26 Age......................... 27 Bridgeman Hill Formation ................ 28 Name and Distribution ................ 28 Dunham Dolomite .................. 28 Rice Hill Member ................... 29 Oak Hill Slate (Parker Slate) .............. 29 Rugg Brook Dolomite (Scottsmore -
1961 Climbers Outing in the Icefield Range of the St
the Mountaineer 1962 Entered as second-class matter, April 8, 1922, at Post Office in Seattle, Wash., under the Act of March 3, 1879. Published monthly and semi-monthly during March and December by THE MOUNTAINEERS, P. 0. Box 122, Seattle 11, Wash. Clubroom is at 523 Pike Street in Seattle. Subscription price is $3.00 per year. The Mountaineers To explore and study the mountains, forests, and watercourses of the Northwest; To gather into permanent form the history and traditions of this region; To preserve by the encouragement of protective legislation or otherwise the natural beauty of Northwest America; To make expeditions into these regions in fulfillment of the above purposes; To encourage a spirit of good fellowship among all lovers of outdoor Zif e. EDITORIAL STAFF Nancy Miller, Editor, Marjorie Wilson, Betty Manning, Winifred Coleman The Mountaineers OFFICERS AND TRUSTEES Robert N. Latz, President Peggy Lawton, Secretary Arthur Bratsberg, Vice-President Edward H. Murray, Treasurer A. L. Crittenden Frank Fickeisen Peggy Lawton John Klos William Marzolf Nancy Miller Morris Moen Roy A. Snider Ira Spring Leon Uziel E. A. Robinson (Ex-Officio) James Geniesse (Everett) J. D. Cockrell (Tacoma) James Pennington (Jr. Representative) OFFICERS AND TRUSTEES : TACOMA BRANCH Nels Bjarke, Chairman Wilma Shannon, Treasurer Harry Connor, Vice Chairman Miles Johnson John Freeman (Ex-Officio) (Jr. Representative) Jack Gallagher James Henriot Edith Goodman George Munday Helen Sohlberg, Secretary OFFICERS: EVERETT BRANCH Jim Geniesse, Chairman Dorothy Philipp, Secretary Ralph Mackey, Treasurer COPYRIGHT 1962 BY THE MOUNTAINEERS The Mountaineer Climbing Code· A climbing party of three is the minimum, unless adequate support is available who have knowledge that the climb is in progress. -
Geographic Features Positive Effects Negative Effects
Name: ________________________________________ Date: ____________ Study Guide: Geography KEY Ms. Carey Geographic Features: Geographic Positive Effects Negative Effects Features Rivers, Oceans, Seas Easy trade, travel, fertile Vulnerable to attacks (easy to invade), soil (can grow food) floods Desert Protection from invaders Difficult to trade, hot, dry (arid), can’t farm (hard to travel) Mountains Protection from invaders Isolated from other people, difficult to trade, travel and difficult to farm Plains Easy trade, travel, fertile Vulnerable to attacks (easy to invade) soil (can grow food) Continents and Oceans: Vocabulary: River Archipelago Ocean Island Continent Pangaea Desert Plains Peninsula Mountain 1. Island: An area of land completely surrounded by water. 2. Peninsula: An area of land completely surrounded by water on three (3) sides and connected to the mainland by an isthmus. 3. Archipelago: A chain of islands, such as Japan and Greece. 4. Continent: A large body of LAND. (hint: there are seven) 5. Ocean: A large body of salt water. (hint: there are four main ones) 6. Desert: A large, arid (dry) area of land which receives less than 10 inches of rain annually. 7. River: A freshwater body of water which flows from a higher elevation to a lower one. 8. Mountain: An area that rises steeply at least 2,000 feet above sea level; usually wide at the bottom and rising to a narrow peak or ridge. 9. Plains: A large area of flat or gently rolling land which is fertile and good for farming. 10. Pangaea: The name of a huge super continent that scientists believe split apart about 200 million years ago, forming different continents. -
Physical Geography of Southeast Asia
Physical Geography of Southeast Asia Creating an Annotated Sketch Map of Southeast Asia By Michelle Crane Teacher Consultant for the Texas Alliance for Geographic Education Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 Guiding Question (5 min.) . What processes are responsible for the creation and distribution of the landforms and climates found in Southeast Asia? Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 2 Draw a sketch map (10 min.) . This should be a general sketch . do not try to make your map exactly match the book. Just draw the outline of the region . do not add any features at this time. Use a regular pencil first, so you can erase. Once you are done, trace over it with a black colored pencil. Leave a 1” border around your page. Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 3 Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 4 Looking at your outline map, what two landforms do you see that seem to dominate this region? Predict how these two landforms would affect the people who live in this region? Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 5 Peninsulas & Islands . Mainland SE Asia consists of . Insular SE Asia consists of two large peninsulas thousands of islands . Malay Peninsula . Label these islands in black: . Indochina Peninsula . Sumatra . Label these peninsulas in . Java brown . Sulawesi (Celebes) . Borneo (Kalimantan) . Luzon Texas Alliance for Geographic Education; http://www.geo.txstate.edu/tage/ September 2013 6 Draw a line on your map to indicate the division between insular and mainland SE Asia. -
The Destiny of Orogen-Parallel Streams in the Eastern Alps: the Salzach–Enns Drainage System
Earth Surf. Dynam., 8, 69–85, 2020 https://doi.org/10.5194/esurf-8-69-2020 © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License. The destiny of orogen-parallel streams in the Eastern Alps: the Salzach–Enns drainage system Georg Trost1, Jörg Robl2, Stefan Hergarten3, and Franz Neubauer2 1Department of Geoinformatics, Paris Lodron University of Salzburg, 5020 Salzburg, Austria 2Department of Geography and Geology, Paris Lodron University of Salzburg, 5020 Salzburg, Austria 3Institute of Earth and Environmental Sciences, Albert Ludwig University of Freiburg, 79104 Freiburg, Germany Correspondence: Georg Trost ([email protected]) Received: 1 August 2019 – Discussion started: 7 August 2019 Revised: 7 November 2019 – Accepted: 3 January 2020 – Published: 28 January 2020 Abstract. The evolution of the drainage system in the Eastern Alps is inherently linked to different tectonic stages of the alpine orogeny. Crustal-scale faults imposed eastward-directed orogen-parallel flow on major rivers, whereas late orogenic surface uplift increased topographic gradients between the foreland and range and hence the vulnerability of such rivers to be captured. This leads to a situation in which major orogen-parallel alpine rivers such as the Salzach River and the Enns River are characterized by elongated east–west-oriented catchments south of the proposed capture points, whereby almost the entire drainage area is located west of the capture point. To determine the current stability of drainage divides and to predict the potential direction of divide migration, we analysed their geometry at catchment, headwater and hillslope scale covering timescales from millions of years to the millennial scale. -
The Science Behind Volcanoes
The Science Behind Volcanoes A volcano is an opening, or rupture, in a planet's surface or crust, which allows hot magma, volcanic ash and gases to escape from the magma chamber below the surface. Volcanoes are generally found where tectonic plates are diverging or converging. A mid-oceanic ridge, for example the Mid-Atlantic Ridge, has examples of volcanoes caused by divergent tectonic plates pulling apart; the Pacific Ring of Fire has examples of volcanoes caused by convergent tectonic plates coming together. By contrast, volcanoes are usually not created where two tectonic plates slide past one another. Volcanoes can also form where there is stretching and thinning of the Earth's crust in the interiors of plates, e.g., in the East African Rift, the Wells Gray-Clearwater volcanic field and the Rio Grande Rift in North America. This type of volcanism falls under the umbrella of "Plate hypothesis" volcanism. Volcanism away from plate boundaries has also been explained as mantle plumes. These so- called "hotspots", for example Hawaii, are postulated to arise from upwelling diapirs with magma from the core–mantle boundary, 3,000 km deep in the Earth. Erupting volcanoes can pose many hazards, not only in the immediate vicinity of the eruption. Volcanic ash can be a threat to aircraft, in particular those with jet engines where ash particles can be melted by the high operating temperature. Large eruptions can affect temperature as ash and droplets of sulfuric acid obscure the sun and cool the Earth's lower atmosphere or troposphere; however, they also absorb heat radiated up from the Earth, thereby warming the stratosphere. -
Evaporation from Salty Lagoons (Case Study: Qattara Depression)
The British University in Egypt BUE Scholar Civil Engineering Engineering Spring 4-2017 Evaporation from Salty Lagoons (Case Study: Qattara Depression) Mohamed Abdelhamid Eizeldin Dr. [email protected] Heba Abdelazim M.Sc Sherif Eldidy Prof. Cairo University Follow this and additional works at: https://buescholar.bue.edu.eg/civil_eng Part of the Civil Engineering Commons, and the Hydraulic Engineering Commons Recommended Citation Eizeldin, Mohamed Abdelhamid Dr.; Abdelazim, Heba M.Sc; and Eldidy, Sherif Prof., "Evaporation from Salty Lagoons (Case Study: Qattara Depression)" (2017). Civil Engineering. 7. https://buescholar.bue.edu.eg/civil_eng/7 This Conference Proceeding is brought to you for free and open access by the Engineering at BUE Scholar. It has been accepted for inclusion in Civil Engineering by an authorized administrator of BUE Scholar. For more information, please contact [email protected]. Al-Azhar University Civil Engineering Research Magazine (CERM) Vol. (39) No. (2) April, 2017 Evaporation from Salty Lagoons (Case Study: Qattara Depression) Abdel Azeem, H.S1, El-Didy, S.M2, Eizeldin, M.A3, and Helmi, A.M4 ﻣﻠﺨﺺ ﻋﺮﺑﻲ ﺗﻢ إﻋﺪاد اﻟﻌﺪﯾﺪ ﻣﻦ اﻟﺪراﺳﺎت - ﻓﻲ ﺑﺪاﯾﺔ اﻟﻘﺮن اﻟﻌﺸﺮﯾﻦ - ﻟﺪراﺳﺔ ﺗﻮﺻﯿﻞ ﻣﯿﺎه اﻟﺒﺤﺮ اﻟﻤﺘﻮﺳﻂ ﻣﻦ ﺧﻼل ﻗﻨﺎة ﺗﻮﺻﯿﻞ ﻟﻤﻨﺨﻔﺾ اﻟﻘﻄﺎرة ﺑﮭﺪف ﺗﻮﻟﯿﺪ اﻟﻄﺎﻗﺔ اﻟﻜﮭﺮﺑﺎﺋﯿﺔ وذﻟﻚ ﺑﺈﺳﺘﻐﻼل ﻓﺮق اﻟﻤﻨﺎﺳﯿﺐ ﺑﯿﻦ اﻟﻤﻨﺨﻔﺾ واﻟﺒﺤﺮ اﻟﻤﺘﻮﺳﻂ ، وﺗﮭﺪف اﻟﺪراﺳﺔ اﻟﺤﺎﻟﯿﺔ إﻟﻰ :-أ) إﻧﺸﺎء ﻣﻨﻈﻮﻣﺔ ﻣﻌﻠﻮﻣﺎت ھﯿﺪروﻟﻮﺟﯿﺔ ﻟﻠﻤﻨﺨﻔﺾ ب) ﺣﺴﺎب ﻣﻌﺪﻻت اﻟﺒﺨﺮ اﻟﻤﺘﻮﻗﻊ ﻣﻦ اﻟﻤﯿﺎه اﻟﻤﺎﻟﺤﺔ اﻟﻤﺠﻤﻌﺔ ﻓﻲ ﺑﺤﯿﺮة اﻟﻤﻨﺨﻔﺾ. وﻗﺪ ﺗﻢ إﻋﺪاد ﻣﻨﮭﺞ اﻟﺪراﺳﺔ ﺑﺎﺳﺘﺨﺪام اﻟﺒﺮاﻣﺞ اﻟﺤﺪﯾﺜﺔ اﻟﺘﻲ ﻟﻢ ﺗﻜﻦ ﻣﺘﺎﺣﺔ ﻟﻠﺪراﺳﺎت اﻟﺴﺎﺑﻘﺔ ﻟﻠﻤﺸﺮوع ﺣﯿﻨﮭﺎ، وھﺬه اﻟﺒﺮاﻣﺞ ﻣﺜﻞ اﻟﻨﻤﺎذج اﻟﻌﺪدﯾﺔ اﻟﻔﻌﺎﻟﺔ، ﻧﻈﺎم اﻟﻤﻌﻠﻮﻣﺎت اﻟﻌﺪدﯾﺔ ( GIS) ، وﻧﻤﺎذج اﻹرﺗﻔﺎﻋﺎت اﻟﺮﻗﻤﯿﺔ (DEM). -
Alaska Range
Alaska Range Introduction The heavily glacierized Alaska Range consists of a number of adjacent and discrete mountain ranges that extend in an arc more than 750 km long (figs. 1, 381). From east to west, named ranges include the Nutzotin, Mentas- ta, Amphitheater, Clearwater, Tokosha, Kichatna, Teocalli, Tordrillo, Terra Cotta, and Revelation Mountains. This arcuate mountain massif spans the area from the White River, just east of the Canadian Border, to Merrill Pass on the western side of Cook Inlet southwest of Anchorage. Many of the indi- Figure 381.—Index map of vidual ranges support glaciers. The total glacier area of the Alaska Range is the Alaska Range showing 2 approximately 13,900 km (Post and Meier, 1980, p. 45). Its several thousand the glacierized areas. Index glaciers range in size from tiny unnamed cirque glaciers with areas of less map modified from Field than 1 km2 to very large valley glaciers with lengths up to 76 km (Denton (1975a). Figure 382.—Enlargement of NOAA Advanced Very High Resolution Radiometer (AVHRR) image mosaic of the Alaska Range in summer 1995. National Oceanic and Atmospheric Administration image mosaic from Mike Fleming, Alaska Science Center, U.S. Geological Survey, Anchorage, Alaska. The numbers 1–5 indicate the seg- ments of the Alaska Range discussed in the text. K406 SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD and Field, 1975a, p. 575) and areas of greater than 500 km2. Alaska Range glaciers extend in elevation from above 6,000 m, near the summit of Mount McKinley, to slightly more than 100 m above sea level at Capps and Triumvi- rate Glaciers in the southwestern part of the range. -
Flat-Top Butte Juniper Encroachment
Worksheet Determination of NEPA Adequacy (DNA) U.S. Department of the Interior Bureau of Land Management BLM Office: Casper Field Office, Wyoming Lease/Serial/Case File No.: Range Improvement Project No. 17657 Tracking Number: DOI-BLM-WY-P060-2016-0033-DNA Proposed Action Title/Type: Flat-top Butte Juniper Encroachment Location of Proposed Action: T30N/ R79W Sec 6 and T30N/R80W, Section 1-2, Natrona County Applicant: BLM A. Description ofProposed Action: The BLM is proposing to treat 562 acres of juniper which has encroached into sagebrush grassland habitat located on Flat-Top Butte located in southern Natrona County. The proposed treatments are located within the Corral Creek (#10106) and Sheep Creek (#10131) grazing allotments. The purpose ofthe vegetative treatment is to enhance sagebrush habitat conditions for wildlife in the Bates Hole area, particularly Greater sage-grouse nesting habitat, big game crucial winter range, as well as improve the hydrologic function of associated drainages. The emphasis ofthis project is to maintain and enhance stands of sagebrush grassland habitat. Treatments would involve contract crews utilizing chainsaws to cut and scatter encroaching junipers on approximately 455 acres, IAW the attached Statement of Work (Appendix 1). Denser stands (-107 acres) may be treated mechanically utilizing a rubber tracked skid steer equipped with a masticator to shred the trees. Total treatment area would include approximately 562 acres, as depicted on the attached map. Treatment areas would be clearly delineated. Treatments are expected to take 2-4 months to 1 111 complete and would occur after July 15 \ ending no later than November 15 to minimize wildlife impacts during sensitive periods. -
Geology and Stratigraphy Column
Capitol Reef National Park National Park Service U.S. Department of the Interior Geology “Geology knows no such word as forever.” —Wallace Stegner Capitol Reef National Park’s geologic story reveals a nearly complete set of Mesozoic-era sedimentary layers. For 200 million years, rock layers formed at or near sea level. About 75-35 million years ago tectonic forces uplifted them, forming the Waterpocket Fold. Forces of erosion have been sculpting this spectacular landscape ever since. Deposition If you could travel in time and visit Capitol Visiting Capitol Reef 180 million years ago, Reef 245 million years ago, you would not when the Navajo Sandstone was deposited, recognize the landscape. Imagine a coastal you would have been surrounded by a giant park, with beaches and tidal flats; the water sand sea, the largest in Earth’s history. In this moves in and out gently, shaping ripple marks hot, dry climate, wind blew over sand dunes, in the wet sand. This is the environment creating large, sweeping crossbeds now in which the sediments of the Moenkopi preserved in the sandstone of Capitol Dome Formation were deposited. and Fern’s Nipple. Now jump ahead 20 million years, to 225 All the sedimentary rock layers were laid million years ago. The tidal flats are gone and down at or near sea level. Younger layers were the climate supports a tropical jungle, filled deposited on top of older layers. The Moenkopi with swamps, primitive trees, and giant ferns. is the oldest layer visible from the visitor center, The water is stagnant and a humid breeze with the younger Chinle Formation above it. -
Taconic Physiography
Bulletin No. 272 ' Series B, Descriptive Geology, 74 DEPARTMENT OF THE INTERIOR . UNITED STATES GEOLOGICAL SURVEY CHARLES D. WALCOTT, DIRECTOR 4 t TACONIC PHYSIOGRAPHY BY T. NELSON DALE WASHINGTON GOVERNMENT PRINTING OFFICE 1905 CONTENTS. Page. Letter of transinittal......................................._......--..... 7 Introduction..........I..................................................... 9 Literature...........:.......................... ........................... 9 Land form __._..___.._.___________..___._____......__..__...._..._--..-..... 18 Green Mountain Range ..................... .......................... 18 Taconic Range .............................'............:.............. 19 Transverse valleys._-_-_.-..._.-......-....___-..-___-_....--_.-.._-- 19 Longitudinal valleys ............................................. ^...... 20 Bensselaer Plateau .................................................... 20 Hudson-Champlain valley................ ..-,..-.-.--.----.-..-...... 21 The Taconic landscape..................................................... 21 The lakes............................................................ 22 Topographic types .............,.....:..............'.................... 23 Plateau type ...--....---....-.-.-.-.--....-...... --.---.-.-..-.--... 23 Taconic type ...-..........-........-----............--......----.-.-- 28 Hudson-Champlain type ......................"...............--....... 23 Rock material..........................'.......'..---..-.....-...-.--.-.-. 23 Harder rocks ....---...............-.-.....-.-...--.-......... -
Hill and Upland Farming in the North of England
M4te1.174; Fi tirgy:CDATION OF AGRICULTURAtcEcoNom ICS SEP • HILL AND UPLAND FARMING IN THE NORTH OF ENGLAND S. ROBSON and D. C. JOHNSON Agricultural Enterprise Studies in England and Wales Economic Report No. 54 MAY 1977 — Price f1-50 UNIVERSITY OF NEWCASTLE UPON TYNE DEPARTMENT OF AGRICULTURAL ECONOMICS HILL AND UPLAND FARMING IN THE NORTH OF ENGLAND. 1973/74 and 1974/75. A two year review_ of financial and other results for an identical sample of 53 farms in the Hills and Uplands of Northern England, with results 'relating to the main enterprises on the farms. - The review also includes a comparison of certain data for the years 1973/74 to 1975//6. AGRICULTURAL ENTERPRISE STUDIES IN ENGLAND AND WALES. University Departments of Agricultural Economics in England and Wales have for many years undertaken economic studies of crop and livestock enterprises, receiving financial and techr4cal support for this work from the Ministry of Agriculture, Fisheries and Food. •The departments in different regions of the country conduct joint studies into those enterprises in which they have a particular interest. This community of interest is recognised by issuing enterprise reports prepared and published by individual departments in a common series entitled "Agricultural Enterprise Studies". Titles of recent publications in this series and the addresses of the Univprsity Departments are given at the end of this report. ACKNOWLEDGEMENTS. This report is based on financial and other data made available to the Agricultural Economics Department of the University of Newcastle upon Tyne by farmers who co-operated in the Farm Management Survey. The department takes this opportunity of thanking these _farmers for their willing co-operation and for providing the additional information required for the report.