Hydrogeological Field Guide to the Wessex Basin
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233 08 SD50 Decision Document New Bespoke
Permitting decisions Variation to permit We have decided to issue the variation for Kimmeridge wellsite operated by Perenco UK Limited. The variation number is EPR/ZP3230CE/V002 We have also carried out an Environment Agency initiated variation to the permit. We consider in reaching that decision we have taken into account all relevant considerations and legal requirements and that the permit will ensure that the appropriate level of environmental protection is provided. This variation is required as the Environment Agency has a duty, under the Environmental Permitting (England and Wales) Regulations 2016, regulation 34(1), to periodically review permits. As a result of that review we have identified a number of necessary changes we must make to reflect current legislation and best practice. These changes principally relate to: Implementation of the Mining Waste Directive namely the addition of extractive waste management activities, Oil storage activities The variation also aim to: Consolidate all previous variations to the original permit so as to bring them together into one permit so the requirements will be clearer. Formalise changes to monitoring requirements and compliance limits where we have agreed them in writing, for example as the result of a hydrogeological risk assessment review. Address site specific issues which result in a change to the current permit, for example incorporating completed improvement conditions into the permit and removing inconsistencies. This permit relates to the Kimmeridge Wellsite which forms part of the Perenco UK Limited’s Wytch Farm operation based on the Isle of Purbeck in Dorset. Kimmeridge Wellsite is located on top of the coastal cliffs surrounding Kimmeridge Bay, approximately 9km from the main Wytch Farm operations, which are the subject of a separate permit. -
A Model for the Evolution of the Weald Basin
A model for the evolution of the Weald Basin DAVID L. HANSEN, DEREK J. BLUNDELL & S0REN B. NIELSEN Hansen, D.L., Blundell, D.J. & Nielsen, S.B. 2002-12-02. A Model for the evolution of the Weald Basin. Bulletin of the Geological Society of Denmark, Vol. 49, pp. 109-118. Copenhagen. https://doi.org/10.37570/bgsd-2003-49-09 The Weald Basin developed through the Jurassic-Lower Cretaceous as an extensional basin founded upon E-W trending low-angle faults that were probably Variscan thrusts, subsequently reactivated as normal faults. Later, the basin was inverted and uplifted into a broad dome, whilst the London Basin to the north, and the Hampshire-Dieppe Basin to the south, subsided as flanking basins during the late Palaeocene-Eocene. Seismic sections across the Weald indicate that inversion resulted from north-directed stress. A stratigraphic reconstruction based on a N-S profile across the Weald and flanking basins serves as a template for a forward, 2D thermo-mechanical model that simulates the evolution of the Weald Basin through crustal extension and its inversion, and subsidence of the flanking basins, through compression. The model provides a physical explanation for this sequence of events, requiring a region of crust of reduced strength relative to its flanks. This weak region is the location of crustal-scale Variscan thrusts that have been reactivated subsequently. The strong crust on the flanks is essential for the development of flanking basins during inversion and uplift of the Weald. Keywords: Basin inversion, lithosphere, thermo-mechanical modelling, finite elements, visco-elas tic-plastic, sedimentation, erosion. -
Wytch Farm Landscape and Access Enhancement Fund the Dorset
Wytch Farm Landscape and Access Enhancement Fund The Dorset Area of Outstanding Natural Beauty is a nationally important protected landscape, with vibrant communities and a wealth of wildlife and heritage. Within the AONB is the largest on-shore oilfield in Europe, at Wytch Farm near Corfe Castle. As part of a planning application to extend the working life of the oilfield by a further 20 years, the oilfield operator, Perenco UK has provided a sum of £1.7 million for landscape, biodiversity and sustainable transport projects to enhance the landscape. This sum is to be used to fund projects that compensate for the environmental impacts of the further retention of the oilfields infrastructure in the landscape. How to Apply If you would like to apply to this fund, please assess your project against the information below to check whether you fulfil the criteria. Applications are to be made on a form downloadable from the Dorset AONB website. What kinds of project can be funded? Projects can be funded which: • Strengthen the character of the surrounding landscape by heathland and acid grassland mosaic creation, conservation, enhancement and management. • Enhance biodiversity by the conservation, enhancement and management of boundary features (hedgerows, veteran trees and earthbanks), woodlands (e.g. through Rhododendron control) and rural lanes. • Improve rights of way and / or facilities for no-car access and conserving tranquillity. Funding is to be targeted to physical works which achieve these aims. Project management time to deliver a practical project can be included within the overall proposal but funds will not be awarded to projects with a disproportionate amount of revenue costs (e.g. -
Swanage and Portland: Historical
1 Swanage and Portland: Historical IN THE BEGINNING On the 6th of January 1786 two men scaled the cliff near Seacombe. Unlike climbers today this pair were not driven by challenge but by necessity. They were crew of the Dutch East Indiaman Halsewell, which had been blown onto the rocks by a violent gale. They raised help and, although the captain’s daughters perished, being too terrified to leave their cabin, another eighty of the ship’s complement of 240 were saved from the sea. One of their number was coloured and therefore a rare sight for the insular locals. Unfortunately, he was not to survive the short journey to shelter up at Worth Matravers; the stile where he died is still known as Black Man’s Gate. Interest in the considerable extent of limestone along the Dorset coastline near Swanage can be traced back to the obscure origins of the cliffstone trade in medieval times. Serious quarrying activity dates from about 1700 and continued up to the mid-nineteenth century. It was during this period that the platforms at Tilly Whim, Dancing Ledge, Winspit, etc. were cut, a legacy later to be enjoyed by the climbing fraternity and in those days put to extensive use by the smugglers whose affairs were rife all along the Dorset coast. Quarrying of the cliffs themselves finally ceased with the closing of Seacombe in the 1920s and of Winspit in the 1950s. For the first documented ascent of any part of the Swanage cliffs other than for commercial gain, we have to go back to the latter part of the nineteenth century, the time of the Empire and the great Victorian pioneers, when famous alpinists such as Mummery, Tyndall, Whymper, and the notorious Aleister Crowley were practising their alpine climbing on the chalk precipices of Beachy Head and at St Margaret’s Bay. -
The Strawberry Bank Lagerstätte Reveals Insights Into Early Jurassic Lifematt Williams, Michael J
XXX10.1144/jgs2014-144M. Williams et al.Early Jurassic Strawberry Bank Lagerstätte 2015 Downloaded from http://jgs.lyellcollection.org/ by guest on September 27, 2021 2014-144review-articleReview focus10.1144/jgs2014-144The Strawberry Bank Lagerstätte reveals insights into Early Jurassic lifeMatt Williams, Michael J. Benton &, Andrew Ross Review focus Journal of the Geological Society Published Online First doi:10.1144/jgs2014-144 The Strawberry Bank Lagerstätte reveals insights into Early Jurassic life Matt Williams1, Michael J. Benton2* & Andrew Ross3 1 Bath Royal Literary and Scientific Institution, 16–18 Queen Square, Bath BA1 2HN, UK 2 School of Earth Sciences, University of Bristol, Bristol BS8 2BU, UK 3 National Museum of Scotland, Chambers Street, Edinburgh EH1 1JF, UK * Correspondence: [email protected] Abstract: The Strawberry Bank Lagerstätte provides a rich insight into Early Jurassic marine vertebrate life, revealing exquisite anatomical detail of marine reptiles and large pachycormid fishes thanks to exceptional preservation, and especially the uncrushed, 3D nature of the fossils. The site documents a fauna of Early Jurassic nektonic marine animals (five species of fishes, one species of marine crocodilian, two species of ichthyosaurs, cephalopods and crustaceans), but also over 20 spe- cies of insects. Unlike other fossil sites of similar age, the 3D preservation at Strawberry Bank provides unique evidence on palatal and braincase structures in the fishes and reptiles. The age of the site is important, documenting a marine ecosystem during recovery from the end-Triassic mass extinction, but also exactly coincident with the height of the Toarcian Oceanic Anoxic Event, a further time of turmoil in evolution. -
Natural Hydraulic Fractures in the Wessex Basin, SW England: Widespread Distribution, Composition and History Alain Zanella, Peter Robert Cobbold, Tony Boassen
Natural hydraulic fractures in the Wessex Basin, SW England: widespread distribution, composition and history Alain Zanella, Peter Robert Cobbold, Tony Boassen To cite this version: Alain Zanella, Peter Robert Cobbold, Tony Boassen. Natural hydraulic fractures in the Wessex Basin, SW England: widespread distribution, composition and history. Marine and Petroleum Geology, Elsevier, 2015, 68 (Part A), pp.438-448. 10.1016/j.marpetgeo.2015.09.005. insu-01200780 HAL Id: insu-01200780 https://hal-insu.archives-ouvertes.fr/insu-01200780 Submitted on 18 Sep 2015 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. ACCEPTED MANUSCRIPT Natural hydraulic fractures in the Wessex Basin, SW England: widespread distribution, composition and history A. Zanella 1, 2 *, P.R. Cobbold 1 and T. Boassen 4 1Géosciences-Rennes (UMR-6118), CNRS et Université de Rennes 1, Campus de Beaulieu, 35042 Rennes Cedex, France 2L.P.G., CNRS UMR 6112, Université du Maine, Faculté des Sciences, 72085 Le Mans Cedex 9, France 4 Statoil ASA Research Centre, NO-7005 Trondheim, Norway *Corresponding author, e-mail: [email protected] Abstract Bedding-parallel veins of fibrous calcite ('beef') are historical in the Wessex Basin. -
Beaches Where Dogs Are Allowed
Beaches where dogs are allowed • 1. Bowleaze Cove • 2. Chesil Beach • 3. Church Ope Cove • 4. Cogden • 5. Durdle Door West • 6. Durdle Door - East • 7. Durley Chine Bournemouth • 8. East Cliff Beach • 9. Eypemouth • 10. Fishermans Walk Bournemouth • 11. Gore Cove • 12. Harbour Lake Poole • 13. Hengistbury West • 14. Hive Beach (Burton Bradstock) • 15. Monmouth Beach Lyme Regis • 16. Mudeford Quay • 17. Mudeford Sandbank • 18. Mupe Bay • 19. Pier Beach Swanage • 20. Ringstead Bay • 21. Rockley Sands Poole • 22. South Beach Studland • 23. Southbourne Bournemouth • 24. St Gabriel’s Mouth • 25. Steamer Point Christchurch • 26. Studland - Knoll Beach • 27. Studland - Shell Bay • 28. White Nothe Please note that some beaches listed as dog friendly may still have certain restricted areas. Check the beach descriptions for further information. Beaches where dogs may be restricted • 1.Alum Chine Bournemouth • 2.Avon Beach Christchurch • 3.Boscombe Pier Bournemouth • 4.Bournemouth Pier • 5.Branksome Chine Poole • 6.Canford Cliffs Poole • 7.Charmouth • 8.Charmouth West • 9.Church Beach Lyme Regis • 10.Friars Cliff Christchurch • 11.Highcliffe • 12.Lyme Regis Beach • 13.Overcombe • 14.Preston Weymouth • 15.Sandbanks Poole • 16.Sandbanks Harbour Poole • 17.Seatown • 18.Shore Road - Sandbanks Poole • 19.Swanage • 20.Swanage North • 21.West Bay East • 22.West Bay West • 23.Weymouth Restrictions for dogs on beaches are generally seasonal with bans taking place between April/May and September. Check the beach descriptions for further information. Beaches where dogs are banned • 1.Shipstal Beach Beaches where we have no information • Castle Cove • Chapman's Pool • Chesil Cove • East Cliff Bournemouth • Greenhill Weymouth • Hengistbury Head Bournemouth • Highcliffe Castle Christchurch • Kimmeridge Bay • Lulworth Cove • Manor Steps Bournemouth • Sandsfoot Castle (Portland Harbour ) • Worbarrow Bay . -
Dorset and East Devon Coast for Inclusion in the World Heritage List
Nomination of the Dorset and East Devon Coast for inclusion in the World Heritage List © Dorset County Council 2000 Dorset County Council, Devon County Council and the Dorset Coast Forum June 2000 Published by Dorset County Council on behalf of Dorset County Council, Devon County Council and the Dorset Coast Forum. Publication of this nomination has been supported by English Nature and the Countryside Agency, and has been advised by the Joint Nature Conservation Committee and the British Geological Survey. Maps reproduced from Ordnance Survey maps with the permission of the Controller of HMSO. © Crown Copyright. All rights reserved. Licence Number: LA 076 570. Maps and diagrams reproduced/derived from British Geological Survey material with the permission of the British Geological Survey. © NERC. All rights reserved. Permit Number: IPR/4-2. Design and production by Sillson Communications +44 (0)1929 552233. Cover: Duria antiquior (A more ancient Dorset) by Henry De la Beche, c. 1830. The first published reconstruction of a past environment, based on the Lower Jurassic rocks and fossils of the Dorset and East Devon Coast. © Dorset County Council 2000 In April 1999 the Government announced that the Dorset and East Devon Coast would be one of the twenty-five cultural and natural sites to be included on the United Kingdom’s new Tentative List of sites for future nomination for World Heritage status. Eighteen sites from the United Kingdom and its Overseas Territories have already been inscribed on the World Heritage List, although only two other natural sites within the UK, St Kilda and the Giant’s Causeway, have been granted this status to date. -
Notes to Accompany the Malvern U3A Fieldtrip to the Dorset Coast 1-5 October 2018
Notes to accompany the Malvern U3A Fieldtrip to the Dorset Coast 1-5 October 2018 SUMMARY Travel to Lyme Regis; lunch ad hoc; 3:00 pm visit Lyme Regis Museum for Monday 01-Oct Museum tour with Chris Andrew, the Museum education officer and fossil walk guide; Arrive at our Weymouth hotel at approx. 5-5.30 pm Tuesday 02 -Oct No access to beaches in morning due to tides. Several stops on Portland and Fleet which are independent of tides Visit Lulworth Cove and Stair Hole; Poss ible visit to Durdle Door; Lunch at Wednesday 03-Oct Clavell’s Café, Kimmeridge; Visit to Etches Collection, Kimmeridge (with guided tour by Steve Etches). Return to Weymouth hotel. Thur sday 04 -Oct Burton Bradstock; Charmouth ; Bowleaze Cove Beaches are accessible in the morning. Fri day 05 -Oct Drive to Lyme Regis; g uided beach tour by Lyme Regis museum staff; Lunch ad hoc in Lyme Regis; Arrive Ledbury/Malvern in the late afternoon PICK-UP POINTS ( as per letter from Easytravel) Monday 1 Oct. Activity To Do Worcester pick-up Depart Croft Rd at 08.15 Barnards Green pick-up 08.45 Malvern Splash pick-up 08.50 Colwall Stone pick-up 09.10 Pick-ups and travel Ledbury Market House pick-up 09.30 to Lyme Regis Arrive Lyme Regis for Lunch - ad hoc 13.00 – 14.00 Visit Lyme Regis Museum where Chris Andrew from the Museum staff will take us for a tour of 15.00 to 16.30 the Geology Gallery. Depart Lyme Regis for Weymouth 16.30 Check in at Best Western Rembrandt Hotel, 17.30 Weymouth At 6.15pm , we will meet Alan Holiday , our guide for the coming week, in the Garden Lounge of the hotel prior to dinner. -
Ringstead to Lulworth Cove.Cdr
1 1 Download the FREE Sports Tracker app, to keep a log of your activities 10 / 2 miles : 4 /2 hours : HARD 7. Follow the narrow trail Ringstead to Lulworth Notes: Steep climbs & descents! Close to cliff edges! through some dense undergrowth, then as it I have started this walk from the TOP car park at Ringstead, NOT down at the beach! opens up, turn right down Driving up the lane, do not turn right, follow all the way to the top, along the flat & over a to the valley bottom. In cattle grid into the field. Follow the gravel track & park on the left. the valley, turn left, uphill. Pass to the left of the 1. Walk to the far end of the parking area, to a large wooden gate & go over the style. h o u s e , u p s o m e Follow the gravel track past Falcon rudimentary steps & at Barn, down hill to a junction & the road, turn left. Head 1 p o s t b o x . B e a r r i g h t . A l m o s t down the hill, under the 2 13 12 immediately, bear left through a tree canopy & past the Obelisk 11 10 kissing gate. "millionaires row". 4 White Nothe 3 9 5 6 2. Pass between the house & barn, 8. As it opens up again Bat's Head 7 8 head straight up the hill to the top. bear right up towards Durdle Door Stair Hole Fantastic views across Weymouth Stair Hole viewing point. -
Lulworth Cove Circular Via Tyneham and Durdle Door Lulworth Cove Circular – Wool Station Start and Finish
Lulworth Cove Circular via Tyneham and Durdle Door Lulworth Cove Circular – Wool Station Start and Finish 1st walk check 2nd walk check 3rd walk check 1st walk check 2nd walk check 3rd walk check 24th July 2019 Current status Document last updated Tuesday, 27th August 2019 This document and information herein are copyrighted to Saturday Walkers’ Club. If you are interested in printing or displaying any of this material, Saturday Walkers’ Club grants permission to use, copy, and distribute this document delivered from this World Wide Web server with the following conditions: • The document will not be edited or abridged, and the material will be produced exactly as it appears. Modification of the material or use of it for any other purpose is a violation of our copyright and other proprietary rights. • Reproduction of this document is for free distribution and will not be sold. • This permission is granted for a one-time distribution. • All copies, links, or pages of the documents must carry the following copyright notice and this permission notice: Saturday Walkers’ Club, Copyright © 2008-2019, used with permission. All rights reserved. www.walkingclub.org.uk This walk has been checked as noted above, however the publisher cannot accept responsibility for any problems encountered by readers. Lulworth Cove Circular via Tyneham and Durdle Door Start & Finish: Lulworth Cove bus stop Lulworth Cove bus stop, map reference SY 822 800, is 178 km south west of Charing Cross, 16m above sea level and in Dorset. Length: 22.2 km (13.8 mi). Cumulative ascent/descent: 974m. For a shorter walk and an Alternative Start or Finish at Wool Station, see below Walk options. -
The Geology Durdle Door, Dorset Chalk Stratigraphy, Sedimentology and Tectonic Structure New Marker Beds
Wessex OUGS Field Guide to Durdle Door, Dorset, May 2018 The Geology Durdle Door, Dorset Chalk stratigraphy, sedimentology and tectonic structure New marker beds Durdle Cove, Dorset looking west over Scratchy Bottom and Swyre Head to Bat’s Head. The line of caves at the foot of the cliff in Durdle Cove is formed on the Durdle Cove Thrust (see also Rowe 1901, Plate III, pp. 16-17). Open University Geological Society Wessex Group Field Excursion Sunday 13th May 2018 Leaders: Rory Mortimore and Jeremy Cranmer Field guide prepared by Rory Mortimore www.chalkrock.com Based on the paper Late Cretaceous stratigraphy, sediments and structure: gems of the Jurassic Coast of Devon and Dorset, England just going into press in the Proceedings of the Geologists’ Association, 2018. 1 Wessex OUGS Field Guide to Durdle Door, Dorset, May 2018 Wessex OUGS Field Trip Durdle Door, Durdle Cove, Scratchy Bottom and Bat’s Head Late Cretaceous stratigraphy, sediments and structure: gems of the Jurassic Coast of Devon and Dorset, England Introduction Extraordinary, long-distance litho-marker beds such as the Lewes and Shoreham Tubular Flints and associated marl seams and fossils (Fig.2), recognised in cliff exposures and cliff-fall boulders, are keys to unlocking the stratigraphy and tectonic structures in the Late Cretaceous (Fig.1) of the Jurassic Heritage Coast. Durdle Cove is a special gem exposing the Lewes and Seaford Chalk stratigraphy where these and new marker beds are identified and where sediments and tectonic structures provide clues to timing of movements that produced a Late Cretaceous pericline which grew into a Miocene monocline along the line of the underlying Purbeck Reverse Fault.