Dichotomous Keys and Mapping Codes for Wetland Landscape Position, Landform, Water Flow Path, and Waterbody Type: Version 3.0
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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 -
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. -
Wind Turbines, Sensitive Bird Populations and Peat Soils
Charity No. 229 325 Wind Turbines, Sensitive Bird Populations and Peat Soils: A Spatial Planning Guide for on-shore wind farm developments in Lancashire, Cheshire, Greater Manchester and Merseyside. July 2008 For more details, contact Tim Youngs [email protected] or Steve White [email protected] Produced by the RSPB and The Wildlife Trust for Lancashire, Manchester & North Merseyside (LWT), in partnership with Lancashire County Council, Natural England and the Merseyside Environmental Advisory Service (EAS) 1 Contents Section Map Annex Page Background 2 How to use the alert maps 4 Introduction 4 Key findings 5 Maps showing ‘important populations’ of ‘sensitive bird 1-5 6- 10 species’ and deep peat sensitive areas in Lancashire, Cheshire, Greater Manchester and Merseyside Legal protection for birds and habitats 11 Methodology and definitions 12- 15 Caveats and notes 16 Distribution of Whooper Swan, Bewick’s Swan and Pink- 17- 22 footed Goose in inland areas of Lancashire, Cheshire, Greater Manchester and Merseyside Thresholds for ‘important’ populations’ (of sensitive species) 1 23 Definition of terms relating to ‘sensitive species’ of bird 2 24 Background The Inspectors who carried out the Examination in Public of the draft NW Regional Spatial Strategy (RSS) between December 06 to February 07, proposed that 'Maps of broad areas where the development of particular types of renewable energy may be considered appropriate should be produced as a matter of urgency and incorporated into an early review of RSS'. This proposal underpins the North West Regional Assembly’s (NWRA) research that is being carried out by Arup consultants. The Secretary of State's response is 'In line with PPS22, we consider that an evidence-based map of broad locations for installation of renewable energy technologies would benefit planning authorities and developers. -
Wetland Restoration USING the Ground Water TECHNIQUE
Wetland ResTORATION USING THE Ground water TECHNIQUE How to build a ground water wetland three important vernal pool zones A ground water wetland fills with water the way a hand-dug well does, by exposing a high water table near the surface. Check for a high water table near a woodland oasis The vernal pool basin or depression is the area that floods in the fall or the center of a potential restoration site. Dig a hole at least 3 feet deep with a spring. This is where vernal pool amphibians and invertebrates breed and post-hole digger, soil auger, or shovel. Watch for water seeping into the hole A vernal pool is like a small oasis of food, water, and shelter for all kinds of lay their eggs, and their young hatch out, feed, and develop (Brown and from the bottom and sides. A high water table will fill the hole partially or woodland wildlife. Large game species such as turkeys, deer, and bears frequent Jung, 2005). The vernal pool basin is the core wetland area protected by state completely with water; listen for the slurp of water as a soil auger is removed. vernal pools, along with a variety of other wildlife including bats, ducks, and federal regulations. The vernal pool basin should be designated as a ‘no Clay soils are not needed to build a ground water wetland because the songbirds, turtles, and snakes. Vernal pools are unique among wetlands disturbance zone.’ depression simply exposes the water table. A seasonally high water table can because they support specialized pool-breeding salamanders, frogs, insects, The vernal pool envelope is the upland habitat immediately surrounding be hard to detect during the summer or any period of drought (Biebighauser, and crustaceans. -
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). -
Field Indicators of Hydric Soils
United States Department of Field Indicators of Agriculture Natural Resources Hydric Soils in the Conservation Service United States In cooperation with A Guide for Identifying and Delineating the National Technical Committee for Hydric Soils Hydric Soils, Version 8.2, 2018 Field Indicators of Hydric Soils in the United States A Guide for Identifying and Delineating Hydric Soils Version 8.2, 2018 (Including revisions to versions 8.0 and 8.1) United States Department of Agriculture, Natural Resources Conservation Service, in cooperation with the National Technical Committee for Hydric Soils Edited by L.M. Vasilas, Soil Scientist, NRCS, Washington, DC; G.W. Hurt, Soil Scientist, University of Florida, Gainesville, FL; and J.F. Berkowitz, Soil Scientist, USACE, Vicksburg, MS ii In accordance with Federal civil rights law and U.S. Department of Agriculture (USDA) civil rights regulations and policies, the USDA, its Agencies, offices, and employees, and institutions participating in or administering USDA programs are prohibited from discriminating based on race, color, national origin, religion, sex, gender identity (including gender expression), sexual orientation, disability, age, marital status, family/parental status, income derived from a public assistance program, political beliefs, or reprisal or retaliation for prior civil rights activity, in any program or activity conducted or funded by USDA (not all bases apply to all programs). Remedies and complaint filing deadlines vary by program or incident. Persons with disabilities who require alternative means of communication for program information (e.g., Braille, large print, audiotape, American Sign Language, etc.) should contact the responsible Agency or USDA’s TARGET Center at (202) 720-2600 (voice and TTY) or contact USDA through the Federal Relay Service at (800) 877-8339. -
South Fox Meadow Drainage Improvement Project
VILLAGE OF SCARSDALE WESTCHESTER COUNTY, NEW YORK COMPREHENSIVE STORM WATER MANAGEMENT SOUTH FOX MEADOW STORMWATER IMPROVEMENT PROJECT In association with WESTCHESTER COUNTY FLOOD MITIGATION PROGRAM Rob DeGiorgio, P.E., CPESC, CPSWQ The Bronx River Watershed Fox Meadow Brook Bronx River Watershed Area in Westchester 48.3 square miles (30,932 acres) 15 Sub-watersheds Percent of undeveloped land in the Watershed 3.3% (0.8 acres in Fox Meadow Brook (FMB) FMB watershed) 928 acres (5.7% of watershed) Bronx River Watershed Fox Meadow Brook George Field Park High School Duck Pond Project Philosophy and Goals •Provide flood mitigation within the Fox Meadow Brook Drainage Basin. •Reduce peak run off rates in the Bronx River Watershed through dry detention storage. •Rehabilitate and preserve natural landscapes and wetlands through invasive species management and re- construction. •Improve water quality. • Petition for and obtain County grant funding to subsidize the project. Village of Scarsdale Fox Meadow Brook Watershed SR-2 BR-4 SR-3 BR-7 BR-8 SR-5 Village of Scarsdale History •In 2009 the Village completed a Comprehensive Storm Water Management Plan. •Critical Bronx River sub drainage basin areas identified inclusive of Fox Meadow Brook (BR-4, BR-7, BR-8). •26 Capital Improvement Projects were identified, several of which comprise the Fox Meadow Detention Improvement Project. •Project included in Village’s Capital Budget. •Project has been reviewed by the NYS DEC. •NYS EFC has approved financing for the project granting Scarsdale a 50% subsidy for their local share of the costs. Village of Scarsdale Site Locations – 7 Segments 7 Project Segments 1. -
Leaf Litter Decomposition in Vernal Pools of a Central Ontario Mixedwood Forest
Leaf Litter Decomposition in Vernal Pools of a Central Ontario Mixedwood Forest by Kirsten Verity Otis A Thesis presented to The University of Guelph In partial fulfilment of requirements for the degree of Master of Science in Environmental Science Guelph, Ontario, Canada © Kirsten V. Otis, July, 2012 ABSTRACT LEAF LITTER DECOMPOSITION IN VERNAL POOLS OF A CENTRAL ONTARIO MIXEDWOOD FOREST Kirsten V. Otis Advisors: University of Guelph, 2012 Dr. Jonathan Schmidt Dr. Shelley Hunt Vernal pools are small, seasonally filling wetlands found throughout forests of north eastern North America. Vernal pools have been proposed as potential 'hot spots' of carbon cycling. A key component of the carbon cycle within vernal pools is the decomposition of leaf litter. I tested the hypothesis that leaf litter decomposition is more rapid within vernal pools than the adjacent upland. Leaf litter mass losses from litterbags incubated in situ within vernal pools and adjacent upland habitat were measured periodically over one year and then again after two years. The experiment was carried out at 24 separate vernal pools, over two replicate years. This is a novel degree of replication in studies of decomposition in temporary wetlands. Factors influencing decomposition, such as duration of flooding, water depth, pH, temperature, and dissolved oxygen were measured. Mass loss was greater within pools than adjacent upland after 6 months, equal after 12 months, and lower within pools than adjacent upland after 24 months. This evidence suggests that vernal pools of Central Ontario are 'hot spots' of decomposition up to 6 months, but not after 12 and 24 months. In the long term, vernal pools may reduce decomposition rates, compared to adjacent uplands. -
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. -
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. -
Questioning Ten Common Assumptions About Peatlands
Questioning ten common assumptions about peatlands University of Leeds Peat Club: K.L. Bacon1, A.J. Baird1, A. Blundell1, M-A. Bourgault1,2, P.J. Chapman1, G. Dargie1, G.P. Dooling1,3, C. Gee1, J. Holden1, T. Kelly1, K.A. McKendrick-Smith1, P.J. Morris1, A. Noble1, S.M. Palmer1, A. Quillet1,3, G.T. Swindles1, E.J. Watson1 and D.M. Young1 1water@leeds, School of Geography, University of Leeds, UK 2current address: Centre GEOTOP, CP 8888, Succ. Centre-Ville, Montréal, Québec, Canada 3current address: Geography, College of Life and Environmental Sciences, University of Exeter, UK _______________________________________________________________________________________ SUMMARY Peatlands have been widely studied in terms of their ecohydrology, carbon dynamics, ecosystem services and palaeoenvironmental archives. However, several assumptions are frequently made about peatlands in the academic literature, practitioner reports and the popular media which are either ambiguous or in some cases incorrect. Here we discuss the following ten common assumptions about peatlands: 1. the northern peatland carbon store will shrink under a warming climate; 2. peatlands are fragile ecosystems; 3. wet peatlands have greater rates of net carbon accumulation; 4. different rules apply to tropical peatlands; 5. peat is a single soil type; 6. peatlands behave like sponges; 7. Sphagnum is the main ‘ecosystem engineer’ in peatlands; 8. a single core provides a representative palaeo-archive from a peatland; 9. water-table reconstructions from peatlands provide direct records of past climate change; and 10. restoration of peatlands results in the re-establishment of their carbon sink function. In each case we consider the evidence supporting the assumption and, where appropriate, identify its shortcomings or ways in which it may be misleading.