Characterization of the Physical and Hydraulic Properties of Peat Impacted by a Temporary Access Road
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Landscape Character Assessment
OUSE WASHES Landscape Character Assessment Kite aerial photography by Bill Blake Heritage Documentation THE OUSE WASHES CONTENTS 04 Introduction Annexes 05 Context Landscape character areas mapping at 06 Study area 1:25,000 08 Structure of the report Note: this is provided as a separate document 09 ‘Fen islands’ and roddons Evolution of the landscape adjacent to the Ouse Washes 010 Physical influences 020 Human influences 033 Biodiversity 035 Landscape change 040 Guidance for managing landscape change 047 Landscape character The pattern of arable fields, 048 Overview of landscape character types shelterbelts and dykes has a and landscape character areas striking geometry 052 Landscape character areas 053 i Denver 059 ii Nordelph to 10 Mile Bank 067 iii Old Croft River 076 iv. Pymoor 082 v Manea to Langwood Fen 089 vi Fen Isles 098 vii Meadland to Lower Delphs Reeds, wet meadows and wetlands at the Welney 105 viii Ouse Valley Wetlands Wildlife Trust Reserve 116 ix Ouse Washes 03 THE OUSE WASHES INTRODUCTION Introduction Context Sets the scene Objectives Purpose of the study Study area Rationale for the Landscape Partnership area boundary A unique archaeological landscape Structure of the report Kite aerial photography by Bill Blake Heritage Documentation THE OUSE WASHES INTRODUCTION Introduction Contains Ordnance Survey data © Crown copyright and database right 2013 Context Ouse Washes LP boundary Wisbech County boundary This landscape character assessment (LCA) was District boundary A Road commissioned in 2013 by Cambridgeshire ACRE Downham as part of the suite of documents required for B Road Market a Landscape Partnership (LP) Heritage Lottery Railway Nordelph Fund bid entitled ‘Ouse Washes: The Heart of River Denver the Fens.’ However, it is intended to be a stand- Water bodies alone report which describes the distinctive March Hilgay character of this part of the Fen Basin that Lincolnshire Whittlesea contains the Ouse Washes and supports the South Holland District Welney positive management of the area. -
Information Sheet on Ramsar Wetlands (RIS)
Information Sheet on Ramsar Wetlands (RIS) Categories approved by Recommendation 4.7 (1990), as amended by Resolution VIII.13 of the 8th Conference of the Contracting Parties (2002) and Resolutions IX.1 Annex B, IX.6, IX.21 and IX. 22 of the 9th Conference of the Contracting Parties (2005). Notes for compilers: 1. The RIS should be completed in accordance with the attached Explanatory Notes and Guidelines for completing the Information Sheet on Ramsar Wetlands. Compilers are strongly advised to read this guidance before filling in the RIS. 2. Further information and guidance in support of Ramsar site designations are provided in the Strategic Framework for the future development of the List of Wetlands of International Importance (Ramsar Wise Use Handbook 7, 2nd edition, as amended by COP9 Resolution IX.1 Annex B). A 3rd edition of the Handbook, incorporating these amendments, is in preparation and will be available in 2006. 3. Once completed, the RIS (and accompanying map(s)) should be submitted to the Ramsar Secretariat. Compilers should provide an electronic (MS Word) copy of the RIS and, where possible, digital copies of all maps. 1. Name and address of the compiler of this form: FOR OFFICE USE ONLY. DD MM YY Joint Nature Conservation Committee Monkstone House City Road Designation date Site Reference Number Peterborough Cambridgeshire PE1 1JY UK Telephone/Fax: +44 (0)1733 – 562 626 / +44 (0)1733 – 555 948 Email: [email protected] 2. Date this sheet was completed/updated: Designated: 28 November 1985 3. Country: UK (England) 4. Name of the Ramsar site: Martin Mere 5. -
World Reference Base for Soil Resources 2014 International Soil Classification System for Naming Soils and Creating Legends for Soil Maps
ISSN 0532-0488 WORLD SOIL RESOURCES REPORTS 106 World reference base for soil resources 2014 International soil classification system for naming soils and creating legends for soil maps Update 2015 Cover photographs (left to right): Ekranic Technosol – Austria (©Erika Michéli) Reductaquic Cryosol – Russia (©Maria Gerasimova) Ferralic Nitisol – Australia (©Ben Harms) Pellic Vertisol – Bulgaria (©Erika Michéli) Albic Podzol – Czech Republic (©Erika Michéli) Hypercalcic Kastanozem – Mexico (©Carlos Cruz Gaistardo) Stagnic Luvisol – South Africa (©Márta Fuchs) Copies of FAO publications can be requested from: SALES AND MARKETING GROUP Information Division Food and Agriculture Organization of the United Nations Viale delle Terme di Caracalla 00100 Rome, Italy E-mail: [email protected] Fax: (+39) 06 57053360 Web site: http://www.fao.org WORLD SOIL World reference base RESOURCES REPORTS for soil resources 2014 106 International soil classification system for naming soils and creating legends for soil maps Update 2015 FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2015 The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of FAO. -
Holme Fen Nature Reserve the Lost Lake and Other
Today, Holme Fen is the largest lowland Once the Mere had been 3 The gamekeeper’s plantation drained, over half the silver birch woodland in England, but it has After the drainage, Holme Fen was not farmed had a very different history. wildlife recorded in the area became extinct here. because it was still too wet and boggy. As it One example was the dried out, Holme Fen turned from reeds to 1 Whittlesea Mere and the Holme Posts Swallowtail butterfly raised bog and then to birch woodland. Swallowtail butterfly. by Matt Berry The ground beneath your feet was once level with 2 Disappearing houses Earlier this century, this area was used for the top of the Holme Posts. At that time, game. In the gamekeeper’s plantation (also One of the most dramatic changes here has been Whittlesea Mere was a short distance away to the know as ‘Ballard’s Covert’) you will see a mix of the drop in ground levels following the drainage, as east. At three miles across, it was a spectacular different trees including oak, birch, and alder. the peat dried out and eroded. Tony Redhead, sight - the largest lake in lowland England. whose family grew up here, remembers some of The variety of trees makes it a good place to You might have come to the effects: hear and see woodland birds, such as Blackcaps, take part in one of the "There was one house, in the 1950s, that had to Woodpeckers and Redpolls. Holme Fen was famous ice skating races be pulled down because you could walk bought for the nation in 1952. -
Coppermine River Nomination Document
Coppermine River Nomination Document Government of Nunavut Parks and Tourism Division Department of Sustainable Development Coppermine River, Nunavut Nomination Document Parks and Tourism Division Department of Sustainable Development Community of Kugluktuk 1 2 Canadian Heritage Rivers System The Canadian Heritage Rivers System has been established by federal, provincial and territorial governments to recognize Canada’s outstanding rivers, and to ensure future management which will protect these rivers and enhance their significant heritage values for long-term benefit and enjoyment of Canadians. To qualify for inclusion in the Canadian Heritage Rivers System a river or a section of river must be of outstanding significance in one or more area; human heritage, natural heritage or recreational values. The nominated section should also be large enough to encompass these values and to provide the user with an appreciation of the river’s resources, as well as an enjoyable recreational experience. The responsibility for the collection and analysis of information to determine heritage values and for subsequent nomination of the river rests with the particular government within whose jurisdiction the nominated river lies. The Canadian Heritage Rivers Board, composed of federal, provincial and territorial repre- sentatives, will examine each nomination document and advise the Minister responsible for Parks Canada and the Minister(s) of the nominating agency (ies) on the suitability of the nominated river for inclusion within the Canadian Heritage Rivers System. When consider- ing a river, the Board will determine the degree to which the nominated river satisfies the “Guidelines for the selection of Canadian Heritage Rivers”. The Board will consider both the river and its surrounding landscape which together capture the heritage values. -
Glacial Dispersal of Gold and Arsenic from an Unknown Source Near Wheatcroft Lake, Manitoba, Including Reference to Overlying Lake Agassiz Clay
Glacial Dispersal of Gold and Arsenic from an Unknown Source Near Wheatcroft Lake, Manitoba, Including Reference to Overlying Lake Agassiz Clay By Wayne C. Suttner Department of Geological Sciences McGill University, Montreal April, 1989 A thesis submitted to the Faculty of Graduate Studies and Research in partial fulfillment of the requirements for the degree of Master of Science @ Wayne C. Suttner, 1989 -------------------------------------- ----- # ' • • .... Glacial Dispersal of Gold and Arsenic Near Wheatcroft Lake. Manitoba 11 ABSTRACT In 1986, a zone of high arsenic values in till was outlined south of Wheatcroft Lake in northwestem Manitoba. This zone was based on 8 anomalous samples taken over an area of approximately ~OO km2• As a folIow-up to this study, 128 additional till samples were collected in the same area. Dispersal patterns of go Id and arsenic are parallel to sub-parallel to Wisconsinan ice-flow directions. No one source area or bedrock lithology has been outlined. Several sources probably contribute to anomalous gold and arsenic values. Much of the study area is overlain by clay of glacial Lake Agassiz. Overlying clay was sampled in addition to till to determine whether clay geochemistry reflects the geochemistry of underlying till. For most trace clements, Lake Agassiz clay is unreliable for detecting the geochemical signal of underlying till. Uranium levels in overlying clay may reflect uranium concentrations in till. 1ll RÉSUMÉ En 1986, de hautes teneurs en arsenic furent observées dans une région dc till au sud du Lac Wheatcroft, dans le nord-ouest du Manitoba. Cette région de till fut délimité par 8 échantillons à teneurs anomaliques et couvre une superficie d'environ 800 km2. -
The Land Potential Data Base for Canada Users' Handbook V
The land potential data base for Canada Users' handbook v. KIRKWOOD, J. DUMANSKI, A. BOOTSMA, R.B. STEWART, and R. MUMA Land Resource Research Centre Ottawa, Ontario Technical Bulletin 1983-4 E LRRC Contribution No. 86-29 Research Branch Agriculture Canada 1989 Copies of this publication are available from Director Land Resource Research Centre Research Branch, Agriculture Canada Ottawa, Ontario KIA OC6 Produced by Research Program Service © Minister of Supply and Services Canada 1989 Cat. No. A54-81l983-4-1989E ISBN 0-662-16782-1 Printed 1983 Revised 1989 Cover illustration The dots on the map represent Agriculture Canada research establishments. TABLE OF CONTENTS Page SUMMARy............................................................... 3 RESUME , , '" " .... 4 ACKNOWLEDGEMENTS 5 INTRODUCTION. ......................................................... 7 DATA FILES CONTAINED IN THE LAND POTENTIAL DATA BASE Cl imate. ......................................................... 7 Soil Description And Soil Climate 8 Actual yield..................................................... 9 Degradation 10 Constraint-Free yield 10 CLI Capability For Agriculture 11 Provincial Proportion 11 Soil Suitability 11 DATA RETRIEVAL ·............................ .................. 11 APPENDIX I - Associated Files 13 APPENDIX II - Data Dictionary Of Variable Names 15 APPENDIX III - Additional Definitions For Variables In the Data Base .. 41 APPENDIX IV - Alphabetical Listing Of Variable Names 50 3 SUMMARY The Land Potential Data Base (LPDB) is a computerized information -
Pokagon State Park Guide
KETTLES AND KAMES The distinctive landscape of Indiana’s Pokagon State Park is a legacy of the most recent Ice Age. Although the Pleistocene Epoch began about 2.6 million years ago, today one can see only the effects of the most recent continental glacier from the Wisconsin age. The irregularly shaped hills, bogs, and lakes are underlain by an assortment of materials that melted from a rugged disintegrating ice sheet a mere 14,000 years ago. Kettle lakes Lake Lonidaw is one of the kettle lakes that formed as the Wisconsin-age glacier retreated. Large blocks of ice broke free from the glacier and were buried under insulating debris. The ice slowly melted, leaving behind a water-filled depression. Morainal landscape The steeply rolling hills, bogs, and interconnected lakes of the park bear witness to the massive ice sheets that advanced over and then melted from this part of the Midwest. & Water Survey. Glacial erratics This former Canadian resident arrived in one of the glacial advances into central Indiana. Many of these trans- ported rocks and boulders, known as “glacial erratics,” are in evidence throughout the park. Lake James THE GEOLOGIC STORY The Northern Moraine and Lake Region, in which Pokagon State Park is located, is noted of Pokagon State Park for its beautiful scenery and lakes — a land- scape created by glaciers. The third largest natural lake in Indiana, Lake James covers 1,140 acres and is 88 feet deep. It is one of the many kettle lakes in the region and was formed by the slow melting of a buried ice block. -
Maine's Coastal Wetlands
Program Support from: Maine Department of Environmental Protection NOAA Coastal Services Center Maine Coastal Program, Maine State Planning Office Maine Department of Marine Resources MAINE'S COASTAL WETLANDS: I. TYPES, DISTRIBUTION, RANKINGS, FUNCTIONS AND VALUES by Alison E. Ward NOAA Coastal Management Fellow Bureau of Land & Water Quality Division of Environmental Assessment Augusta, ME September 1999 DEPLW1999 - 13 TABLE OF CONTENTS Page # ACKNOWLEDGEMENTS .........................................................................................................................ii SUMMARY..................................................................................................................................................iii INTRODUCTION ........................................................................................................................................ 1 COASTAL DEVELOPMENT..................................................................................................................... 7 NRPA PERMITTED ACTIVITY IN COASTAL WETLANDS ............................................................................... 8 NRPA PERMITTED ACTIVITY IN COASTAL WETLANDS BY REGIONAL OFFICE .......................................... 11 COASTAL WETLAND IMPACT..................................................................................................................... 14 TYPES & DISTRIBUTION OF INTERTIDAL HABITATS................................................................. 17 TYPES AND ACREAGE OF INTERTIDAL -
Pennsylvania Accomplishments 2019
Pennsylvania Accomplishments 2019 ©NICHOLAS TONELLI ON THE COVER Tröegs Independent Brewing and The Nature Conservancy have been working together to raise awareness about the need to protect the Kittatinny Ridge, an important 185-mile superhighway for birds and other animals that runs from the Mason-Dixon line through the Delaware River Water Gap. Tröegs and TNC sponsored the creation of a mural in downtown Harrisburg that depicts bird species that migrate along the Kittatinny Ridge. In honor of this partnership, Tröegs also created a limited-edition beer called Trail Day to increase awareness about the Kittatinny Ridge. Trail Day was sold this fall in Pennsylvania and nine other states. “ Our brewery is a mere 10 miles from the ridge—we want generations to come to be able to enjoy the clean water and forests like we do.” —JOHN TROGNER Tröegs Independent Brewing ©JOHN TROGNER ©TRÖEGS INDEPENDENT BREWING ©TRÖEGS John Trogner, one of the founders of Tröegs Independent Brewing Company 2 Pennsylvania Accomplishments Report 2019 From the Desk of Bill DeWalt Board Chair of The Nature Conservancy in Pennsylvania ©BILL DEWALT The Nature Conservancy’s TNC Pennsylvania Pennsylvania staff wakes up every encompasses day thinking about protecting nature in the Keystone State. They maintain trails, manage forests, host events at our 13 preserves, 13 work with farmers, and promote preserves nature-friendly policies around the Commonwealth. Our staff here in Pennsylvania are part of a global conservation organization with Total number of acres of operations that extend into 72 countries, land TNC has protected in including a professional network that Pennsylvania: includes more than 400 scientists. -
Re-Assessing a Recently Proposed Turbary Ground
RE-ASSESSING A RECENTLY PROPOSED TURBARY GROUND A BATTY 2011 Front cover Proposed Turbary Ground at Humphry Bottom 2 TURBARY SITE A recently published article on the Ingleborough Archaeology Group Website entitled Turbary Ground (Web Ref 1) states that a new turbary area has been recognised at Humphrey Bottom (SD 743750). A photograph (Plate1) shows the feature being discussed, this is described as “a single abandoned bay possibly the last ever working”. The photograph clearly shows that the peat has liquified and the sod has collapsed into the base of the eroded section. This sod block now overlies waterlogged peat, this has changed the flora of the sod to almost solid sphagnum moss, as shown in Plate 2. There are a few remnants of the original grass sticking through the moss This area of the peat moss has become de-stabilised, caused by liquefaction of the peat due to water exuding from beneath the Arks scree slope (Plate 3). Adjacent to the above is another section, also about to collapse, that can be seen as a crescent-shaped crack that is full of water (Plate 4), This will probably result in a similar feature to the one already described so to suggest that the above feature “may well be medieval or early post-medieval” with this rate of erosion taking place is untenable. It is also stated that “there is no evidence of a peat ground closer to Southerscales than this one” this is incorrect as will be shown when current research into turbary areas is completed. A track is also mentioned as possibly being related to the peat ground (Plates 5/6) show 2 areas where scree has been levelled, one shows the track terminating at a shepherds shelter and the other is lower down the slope. -
The Last British Ice Sheet: a Review of the Evidence Utilised in the Compilation of the Glacial Map of Britain
This is a repository copy of The last British Ice Sheet: A review of the evidence utilised in the compilation of the Glacial Map of Britain . White Rose Research Online URL for this paper: http://eprints.whiterose.ac.uk/915/ Article: Evans, D.J.A., Clark, C.D. and Mitchell, W.A. (2005) The last British Ice Sheet: A review of the evidence utilised in the compilation of the Glacial Map of Britain. Earth-Science Reviews, 70 (3-4). pp. 253-312. ISSN 0012-8252 https://doi.org/10.1016/j.earscirev.2005.01.001 Reuse Unless indicated otherwise, fulltext items are protected by copyright with all rights reserved. The copyright exception in section 29 of the Copyright, Designs and Patents Act 1988 allows the making of a single copy solely for the purpose of non-commercial research or private study within the limits of fair dealing. The publisher or other rights-holder may allow further reproduction and re-use of this version - refer to the White Rose Research Online record for this item. Where records identify the publisher as the copyright holder, users can verify any specific terms of use on the publisher’s website. Takedown If you consider content in White Rose Research Online to be in breach of UK law, please notify us by emailing [email protected] including the URL of the record and the reason for the withdrawal request. [email protected] https://eprints.whiterose.ac.uk/ White Rose Consortium ePrints Repository http://eprints.whiterose.ac.uk/ This is an author produced version of a paper published in Earth-Science Reviews.