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11E5: Dubmill Point to Silloth
Cumbria Coastal Strategy Technical Appraisal Report for Policy Area 11e5 Dubmill Point to Silloth (Technical report by Jacobs) CUMBRIA COASTAL STRATEGY - POLICY AREA 11E5 DUBMILL POINT TO SILLOTH Policy area: 11e5 Dubmill Point to Silloth Figure 1 Sub Cell 11e St Bees Head to Scottish Border Location Plan of policy units. Baseline mapping © Ordnance Survey: licence number 100026791. 1 CUMBRIA COASTAL STRATEGY - POLICY AREA 11E5 DUBMILL POINT TO SILLOTH 1 Introduction 1.1 Location and site description Policy units: 11e5.1 Dubmill Point to Silloth (priority unit) Responsibilities: Allerdale Borough Council Cumbria County Council United Utilities Location: This unit lies between the defended headland of Dubmill Point and Silloth Harbour to the north. Site overview: The shoreline is mainly low lying, characterised by a wide mud, sand and shingle foreshore, fronting low lying till cliffs and two belts of dunes; at Mawbray and at Silloth. The lower wide sandy foreshore is interspersed by numerous scars, including Dubmill Scar, Catherinehole Scar, Lowhagstock Scar, Lee Scar, Beck Scar and Stinking Crag. These scars are locally important for wave dissipation and influence shoreline retreat. The behaviour of this shoreline is strongly influenced by the Solway Firth, as the frontage lies at the estuary’s lower reaches. Over the long term, the foreshore has eroded across the entire frontage due to the shoreward movement of the Solway Firth eastern channel (Swatchway), which has caused narrowing of the intertidal sand area and increased shoreline exposure to tidal energy. The Swatchway currently lies closer to the shoreline towards the north of the frontage. There is a northward drift of sediment, but the southern arm of Silloth Harbour intercepts this movement, which helps stabilise the beach along this section. -
Lake Windermere Guided Trail
Lake Windermere Guided Trail Tour Style: Guided Trails Destinations: Lake District & England Trip code: CNLWI Trip Walking Grade: 2 HOLIDAY OVERVIEW The Lake Windermere Trail is a circular walk that takes you on a lovely journey around Lake Windermere. The route takes in a mixture of lakeside paths and higher ground walking, all whilst experiencing some of the Lake District’s most stunning views. Lake Windermere is the largest lake in the Lake District and the largest in England. At 10½ miles long it has one end in the mountains and the other almost on the coast and is surrounded by very varied scenery. On the penultimate day we walk to the well known Bowness Bay. WHAT'S INCLUDED • High quality en-suite accommodation in our country house • Full board from dinner upon arrival to breakfast on departure day • The services of an HF Holidays' walks leader • All transport on walking days HOLIDAYS HIGHLIGHTS • Follow lakeside paths and higher routes around Lake Windermere www.hfholidays.co.uk PAGE 1 [email protected] Tel: +44(0) 20 3974 8865 • Take a boat trip on Lake Windermere • Views of the Coniston; Langdale and Ambleside Fells • Visit Bowness on Windermere TRIP SUITABILITY This Guided Walking /Hiking Trail is graded 3 which involves walks /hikes on well-defined paths, though often in hilly or upland areas, or along rugged footpaths. These may be rough and steep in sections and will require a good level of fitness. It is your responsibility to ensure you have the relevant fitness required to join this holiday. Fitness We want you to be confident that you can meet the demands of each walking day and get the most out of your holiday. -
Mountain Ringlet Survey Squares 2010
MOUNTAIN RINGLET SURVEY SQUARES 2014 – NOTES FOR SURVEYORS ----------------------------------------------------------------------------- Please note: The following relates only to dedicated Mountain Ringlet searches. For casual records please use our website “Sightings” page where possible. Click on sightings report on: www.cumbria-butterflies.org.uk/sightings/ ----------------------------------------------------------------------------- We’d welcome surveys in any of the squares listed below, but are particularly interested in those marked * and +, ie where there have been recent positive sightings well away from known colonies or discovery of possible new colonies. The areas to be surveyed fall into 3 groups, in colour below, but also suffixed (1), (2) or (3) for those with black & white printers etc. 1. Grid squares that have previous positive sightings (shown in red) (1) 2. Grid squares adjacent to the above (shown in blue) (2) 3. Grid squares that are previously unrecorded but may have potential to hold Mountain Ringlet populations (shown in green) (3) The objective of these surveys is to try to determine the geographical spread of some known colonies, but also to survey areas that have suitable geology and which may hold previously unrecorded Mountain Ringlet populations. All the 1-km grid squares listed below lie in the 100-km square: NY AREA 1 - LANGDALE 2608 Martcrag Moor / Stake Pass (2) 2607 (north-east corner only) Part of Martcrag Moor (2) 2806 (northern edge) Raven Crag (1) 2807 Harrison Stickle (1) 2710 (eastern half only) -
Peat Database Results Cumbria
Allonby, Cumbria Record ID 528 Authors Year Tooley, M. 1985b Location description Deposit location Deposit description Deposit stratigraphy Associated artefacts Early work Sample method Depth of deposit 14C ages available No Notes Moor log. Bibliographic reference Tooley, M. 1985b 'Sea level changes and coastal morphology in North-west England' in 'The Geomorphology of North-west England', (ed.s) Johnson, R., 94-121, Manchester: Manchester University Press. Coastal peat resource database (Hazell, 2008) Page 1 of 23 Annas Mouth, Cumbria Record ID 527 Authors Year Tooley, M. 1985b Location description Deposit location SD 0768 8841 Deposit description Deposit stratigraphy Associated artefacts Early work Sample method Depth of deposit 14C ages available +6.6 m OD No Notes Bibliographic reference Tooley, M. 1985b 'Sea level changes and coastal morphology in North-west England' in 'The Geomorphology of North-west England', (ed.s) Johnson, R., 94- 121, Manchester: Manchester University Press. Coastal peat resource database (Hazell, 2008) Page 2 of 23 Barrow Harbour, Cumbria Record ID 406 Authors Year Kendall, W. 1900 Location description Deposit location [c. SD 217 653 - middle of harbour] Deposit description Deposit stratigraphy Buried peats. Hard, consolidated, dry, laminated deposit overlain by marine clays, silts and sands. Valves of intertidal mollusc (Scrobularia) and vertebrae of whales in silty clay overlying the peat. Associated artefacts Early work Sample method Depth of deposit 14C ages available No Notes Referred to in Tooley (1974). Bibliographic reference Kendall, W. 1900 'Submerged peat mosses, forest remains and post-glacial deposits in Barrow Harbour', Tranactions of the Barrow Naturalists' Field Club, 3(2), 55-63. -
Windermere Way
WINDERMERE WAY AROUND ENGLAND’S FINEST LAKE WINDERMERE WAY - WALKING SHORT BREAK SUMMARY The Windermere Way combines a delightful series of linked walks around Lake Windermere, taking in some of the finest views of the Lake District. Starting in the pretty town of Ambleside, the Windermere Way is made up of four distinct day walks which are all linked by ferries across the Lake. So you not only get to enjoy some wonderful walking but can also sit back and relax on some beautiful ferry journeys across Lake Windermere! The Windermere Way is a twin-centre walking holiday combining 2 nights in the lively lakeside town of Ambleside with 3 nights in the bustling Bowness-on-Windermere. Each day you will do a different walk and use the Windermere Ferries to take you to or from Ambleside or Bowness. From Ambleside, you will catch your first ferry to the lovely lakeside town of Bowness, where you will begin walking. Over the next four days you will take in highlights such as the magnificent views from Wansfell Pike, the glistening Loughrigg Tarn, and some delightful lakeshore walking. Most of the time you are walking on well maintained paths and trails and this is combined with some easy sections of road walking. Sometimes you will be climbing high up into the hills and at others you will be strolling along close to the lake on nice flat paths. Tour: Windermere Way Code: WESWW The Windermere Way includes hand-picked overnight accommodation in high quality B&B’s or Type: Self-Guided Walking Holiday guesthouses in Ambleside and Bowness. -
Assessing the Chronostratigraphic Fidelity of Sedimentary Geological Outcrops in the Pliocene–Pleistocene Red Crag Formation, Eastern England
Downloaded from http://jgs.lyellcollection.org/ by guest on September 25, 2021 Research article Journal of the Geological Society Published Online First https://doi.org/10.1144/jgs2019-056 Where does the time go? Assessing the chronostratigraphic fidelity of sedimentary geological outcrops in the Pliocene–Pleistocene Red Crag Formation, eastern England Neil S. Davies1*, Anthony P. Shillito1 & William J. McMahon2 1 Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK 2 Faculty of Geosciences, Utrecht University, Princetonlaan 8a, Utrecht 3584 CB, Netherlands NSD, 0000-0002-0910-8283; APS, 0000-0002-4588-1804 * Correspondence: [email protected] Abstract: It is widely understood that Earth’s stratigraphic record is an incomplete record of time, but the implications that this has for interpreting sedimentary outcrop have received little attention. Here we consider how time is preserved at outcrop using the Neogene–Quaternary Red Crag Formation, England. The Red Crag Formation hosts sedimentological and ichnological proxies that can be used to assess the time taken to accumulate outcrop expressions of strata, as ancient depositional environments fluctuated between states of deposition, erosion and stasis. We use these to estimate how much time is preserved at outcrop scale and find that every outcrop provides only a vanishingly small window onto unanchored weeks to months within the 600–800 kyr of ‘Crag-time’. Much of the apparently missing time may be accounted for by the parts of the formation at subcrop, rather than outcrop: stratigraphic time has not been lost, but is hidden. The time-completeness of the Red Crag Formation at outcrop appears analogous to that recorded in much older rock units, implying that direct comparison between strata of all ages is valid and that perceived stratigraphic incompleteness is an inconsequential barrier to viewing the outcrop sedimentary-stratigraphic record as a truthful chronicle of Earth history. -
North West Inshore and Offshore Marine Plan Areas
Seascape Character Assessment for the North West Inshore and Offshore marine plan areas MMO 1134: Seascape Character Assessment for the North West Inshore and Offshore marine plan areas September 2018 Report prepared by: Land Use Consultants (LUC) Project funded by: European Maritime Fisheries Fund (ENG1595) and the Department for Environment, Food and Rural Affairs Version Author Note 0.1 Sally First draft desk-based report completed May 2015 Marshall Paul Macrae 1.0 Paul Macrae Updated draft final report following stakeholder consultation, August 2018 1.1 Chris MMO Comments Graham, David Hutchinson 2.0 Paul Macrae Final report, September 2018 2.1 Chris Independent QA Sweeting © Marine Management Organisation 2018 You may use and re-use the information featured on this website (not including logos) free of charge in any format or medium, under the terms of the Open Government Licence. Visit www.nationalarchives.gov.uk/doc/open-government- licence/ to view the licence or write to: Information Policy Team The National Archives Kew London TW9 4DU Email: [email protected] Information about this publication and further copies are available from: Marine Management Organisation Lancaster House Hampshire Court Newcastle upon Tyne NE4 7YH Tel: 0300 123 1032 Email: [email protected] Website: www.gov.uk/mmo Disclaimer This report contributes to the Marine Management Organisation (MMO) evidence base which is a resource developed through a large range of research activity and methods carried out by both MMO and external experts. The opinions expressed in this report do not necessarily reflect the views of MMO nor are they intended to indicate how MMO will act on a given set of facts or signify any preference for one research activity or method over another. -
Complete 230 Fellranger Tick List A
THE LAKE DISTRICT FELLS – PAGE 1 A-F CICERONE Fell name Height Volume Date completed Fell name Height Volume Date completed Allen Crags 784m/2572ft Borrowdale Brock Crags 561m/1841ft Mardale and the Far East Angletarn Pikes 567m/1860ft Mardale and the Far East Broom Fell 511m/1676ft Keswick and the North Ard Crags 581m/1906ft Buttermere Buckbarrow (Corney Fell) 549m/1801ft Coniston Armboth Fell 479m/1572ft Borrowdale Buckbarrow (Wast Water) 430m/1411ft Wasdale Arnison Crag 434m/1424ft Patterdale Calf Crag 537m/1762ft Langdale Arthur’s Pike 533m/1749ft Mardale and the Far East Carl Side 746m/2448ft Keswick and the North Bakestall 673m/2208ft Keswick and the North Carrock Fell 662m/2172ft Keswick and the North Bannerdale Crags 683m/2241ft Keswick and the North Castle Crag 290m/951ft Borrowdale Barf 468m/1535ft Keswick and the North Catbells 451m/1480ft Borrowdale Barrow 456m/1496ft Buttermere Catstycam 890m/2920ft Patterdale Base Brown 646m/2119ft Borrowdale Caudale Moor 764m/2507ft Mardale and the Far East Beda Fell 509m/1670ft Mardale and the Far East Causey Pike 637m/2090ft Buttermere Bell Crags 558m/1831ft Borrowdale Caw 529m/1736ft Coniston Binsey 447m/1467ft Keswick and the North Caw Fell 697m/2287ft Wasdale Birkhouse Moor 718m/2356ft Patterdale Clough Head 726m/2386ft Patterdale Birks 622m/2241ft Patterdale Cold Pike 701m/2300ft Langdale Black Combe 600m/1969ft Coniston Coniston Old Man 803m/2635ft Coniston Black Fell 323m/1060ft Coniston Crag Fell 523m/1716ft Wasdale Blake Fell 573m/1880ft Buttermere Crag Hill 839m/2753ft Buttermere -
Trip Notes ------Believe Achieve Inspire ------Lake District Peaks Challenge Uk
TRIP NOTES ------------------------- BELIEVE ACHIEVE INSPIRE ------------------------- LAKE DISTRICT PEAKS CHALLENGE UK Sat 05 Sep - Sat 05 Sep 2020 OVERVIEW LAKE DISTRICT PEAKS CHALLENGE - UK 2 In aid of your choice of charity 05 Sep - 05 Sep 2020 1 DAYS | UK | CHALLENGING Challenge yourself to take on three, five or · Choose between 3, 5 or 8 peaks in one challenging day! · Summit Scafell Pike, England’s highest mountain EIGHT peaks of the Lake District – and in just · Trek in Greater Langdale, one of the Lake Districts most one day! This is one of the toughest challenges stunning areas · Celebrate with a buffet dinner in a beautiful Lake District that the UK has to offer, putting you through the pub ultimate test of strength, endurance and determination. You will tackle some of England’s most rugged and demanding mountains over a matter of hours. Scafell Pike and Great End will be among the peaks you ascend on this journey through the majestic Lake District. The terrain is extremely varied and involves some very steep ascents and descents so trekkers must be fit and confident. This is a tough challenge which is not for the faint-hearted, but the sense of achievement is immense. +44 (0)20 8346 0500 facebook.com/charitychallenge [email protected] twitter.com/charitychall www.charitychallenge.com ITINERARY LAKE DISTRICT PEAKS CHALLENGE - UK 3 YOUR CHALLENGE DAY BY DAY DAY 1 Sat 05 Sep - The challenge! Pit yourself against one of the toughest challenges that the UK has to offer, as you take on up to eight of the Lake District’s most famous peaks. -
Assessing the Chronostratigraphic Fidelity of Sedimentary Geological Outcrops in the Pliocene–Pleistocene Red Crag Formation, Eastern England
Downloaded from http://jgs.lyellcollection.org/ by guest on September 27, 2021 Research article Journal of the Geological Society Published online August 14, 2019 https://doi.org/10.1144/jgs2019-056 | Vol. 176 | 2019 | pp. 1154–1168 Where does the time go? Assessing the chronostratigraphic fidelity of sedimentary geological outcrops in the Pliocene–Pleistocene Red Crag Formation, eastern England Neil S. Davies1*, Anthony P. Shillito1 & William J. McMahon2 1 Department of Earth Sciences, University of Cambridge, Downing Street, Cambridge CB2 3EQ, UK 2 Faculty of Geosciences, Utrecht University, Princetonlaan 8a, Utrecht 3584 CB, Netherlands NSD, 0000-0002-0910-8283; APS, 0000-0002-4588-1804 * Correspondence: [email protected] Abstract: It is widely understood that Earth’s stratigraphic record is an incomplete record of time, but the implications that this has for interpreting sedimentary outcrop have received little attention. Here we consider how time is preserved at outcrop using the Neogene–Quaternary Red Crag Formation, England. The Red Crag Formation hosts sedimentological and ichnological proxies that can be used to assess the time taken to accumulate outcrop expressions of strata, as ancient depositional environments fluctuated between states of deposition, erosion and stasis. We use these to estimate how much time is preserved at outcrop scale and find that every outcrop provides only a vanishingly small window onto unanchored weeks to months within the 600–800 kyr of ‘Crag-time’. Much of the apparently missing time may be accounted for by the parts of the formation at subcrop, rather than outcrop: stratigraphic time has not been lost, but is hidden. The time-completeness of the Red Crag Formation at outcrop appears analogous to that recorded in much older rock units, implying that direct comparison between strata of all ages is valid and that perceived stratigraphic incompleteness is an inconsequential barrier to viewing the outcrop sedimentary-stratigraphic record as a truthful chronicle of Earth history. -
Lecturer in Forestry Institute of Science, Natural Resources and Outdoor Studies
Lecturer in Forestry Institute of Science, Natural Resources and Outdoor Studies Location: Ambleside Starting Salary: £33,797 with incremental progression to £38,017 Post Type: Full Time Contract Type: Permanent Release Date: Friday 25 June 2021 Closing Date: 23.59 hours BST on Sunday 25 July 2021 Interview Date: Thursday 05 August 2021 Reference: XX037921 The Institute of Science, Natural Resources and Outdoor Studies is seeking to recruit a Lecturer in Forestry and woodland management with strong links to the sector. Details of the post can be found at: XX037921 Lecturer in Forestry - Jobs at University of Cumbria We are the University of Cumbria, a place where people are at the heart of all we do, where enriching the lives of our students, staff and the communities we serve means we make a difference that really matters. Now is a very exciting time to be joining us because we are delivering a new strategic plan focused on making the most of our three most valuable assets; People, Place and Partnerships, to become a catalyst for economic well-being for our region, nationally and internationally. We are seeking innovative, creative, high quality researchers, and scholars to foster a culture of exploration, discovery and intellectual challenge that generates international recognition, respect and engagement. The Institute of Science, Natural Resources and Outdoor Studies is one of five Institutes within the University. It is a busy and vibrant Institute which has strong links with a number of professional bodies and employers which is reflected in the high level of employment our students enjoy. The Institute is split across two sites, Ambleside and Carlisle, to suit the academic portfolio and delivery needs of the programmes. -
A Tectonic History of Northwest England
A tectonic history of northwest England FRANK MOSELEY CONTENTS Introduction 56x Caledonian earth movements 562 (A) Skiddaw Slate structures . 562 (B) Borrowdale Volcanic structures . 570 (C) Deformation of the Coniston Limestone and Silurian rocks 574 (D) Comment on Ingleton-Austwick inlier 580 Variscan earth movements. 580 (A) General . 580 (B) Folds 584 (C) Fractures. 587 4 Post Triassic (Alpine) earth movements 589 5 References 59 ° SUMMARY Northwest England has been affected by the generally northerly and could be posthumous Caledonian, Variscan and Alpine orogenies upon a pre,Cambrian basement. The end- no one of which is entirely unrelated to the Silurian structures include early N--S and later others. Each successive phase is partially NE to ~NE folding. dependent on earlier ones, whilst structures The Variscan structures are in part deter- in older rocks became modified by succeeding mined by locations of the older massifs and in events. There is thus an evolutionary structural part they are likely to be posthumous upon sequence, probably originating in a pre- older structures with important N-S and N~. Cambrian basement and extending to the elements. Caledonian wrench faults were present. reactivated, largely with dip slip movement. The Caledonian episodes are subdivided into The more gentle Alpine structures also pre-Borrowdale Volcanic, pre-Caradoc and follow the older trends with a N-s axis of warp end-Silurian phases. The recent suggestions of or tilt and substantial block faulting. The latter a severe pre-Borrowdale volcanic orogeny are was a reactivation of older fault lines and rejected but there is a recognizable angular resulted in uplift of the old north Pennine unconformity at the base of the volcanic rocks.