Slapton Ley Walks and Trails 2016 Copy
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Slapton Line Reinstatement
Slapton Line Reinstatement Project Bulletin 26 September 2018 Progress The realignment of the A379 between Slapton and Strete Gate is progressing well and is on schedule for completion in mid-October. The southern section of the road is complete and the northern section is well underway with all ecological and unexploded ordnance surveys undertaken. The junction of Sands Road with the A379 is almost complete having been moved inland by about 10 metres. Traffic lights will remain in place until Friday 5th October. Lights will then be used for short periods whilst finishing works, such as road markings, are undertaken. The Field Study Centre staff and contractors have been undertaking scrub management work to facilitate the re-routing of the South West Coast Path which has been temporarily diverted along the shingle beach. Want to get in touch? Your dedicated Public Liaison Officer for the A379 Slapton Line Reinstatement works is Rosemarie Harrod. She can be contacted by T: 0330 041 2184* The new carriageway looking from Slapton The old and new carriageways looking from E: [email protected] Junction towards Strete Strete towards Slapton Junction * Calls to this number are charged at national call rates Upcoming Works and included in inclusive minute plans from landlines On Thursday 27th September there will be a night time closure of the Sands Road and mobiles Junction with the A379, for one night only between 6pm and 6am. community.alungriffiths.co.uk On the 8th October we will commence works to repair and upgrade a 70 metre stretch of an existing sea defence immediately north of Torcross. -
CKW Report 9 Torcross to Kingswear
www.gov.uk/englandcoastpath England Coast Path Stretch: Cremyll to Kingswear Report CKW 9: Torcross to Kingswear Part 9.1: Introduction Start Point: Torcross (Grid reference SX 8233 4200) End Point: Kingswear (Grid reference SX 8785 5108) Relevant Maps: CKW 9a to CKW 9h 9.1.1 This is one of a series of linked but legally separate reports published by Natural England under section 51 of the National Parks and Access to the Countryside Act 1949, which make proposals to the Secretary of State for improved public access along and to this stretch of coast between Torcross and Kingswear. 9.1.2 This report covers length CKW 9 of the stretch, which is the coast between Torcross Point and the Dart Estuary at Kingswear. It makes free-standing statutory proposals for this part of the stretch, and seeks approval for them by the Secretary of State in their own right under section 52 of the National Parks and Access to the Countryside Act 1949. 9.1.3 The report explains how we propose to implement the England Coast Path (“the trail”) on this part of the stretch, and details the likely consequences in terms of the wider ‘Coastal Margin’ that will be created if our proposals are approved by the Secretary of State. Our report also sets out: any proposals we think are necessary for restricting or excluding coastal access rights to address particular issues, in line with the powers in the legislation; and any proposed powers for the trail to be capable of being relocated on particular sections (“roll- back”), if this proves necessary in the future because of coastal change. -
Slapton Coastal Zone Management Main Study Volume 1: Phase 1 Report (I)
Slapton Coastal Zone Management Main Study Volume 1: Phase 1 Report (I) Prepared by Scott Wilson For Slapton Line Partnership August 2006 DOCUMENT APPROVAL FORM Document Title: Slapton Coastal Zone Management Main Study Volume 1: Phase 1 Report (I) Author: Scott Wilson, with University of Plymouth, Roger Tym and Partners and Dr Mark Lee. Amendments Record and Author Approvals: Version Date Description Prepared Reviewed Approved 1 July 2004 Draft Scott Wilson Dr Damon D C Dales University of Plymouth O’Brien Atlantic Consultants E Williams Dr Mark Lee R Hein 2 October 2004 Scott Wilson Dr Damon D C Dales University of Plymouth O’Brien Atlantic Consultants E Williams Dr Mark Lee R Hein 3 October 2004 Revised Scott Wilson Dr Damon D C Dales with minor University of Plymouth O’Brien comments Atlantic Consultants E Williams Dr Mark Lee R Hein 4 August 2006 Re-titled as Scott Wilson Dr Damon D C Dales Volume 1 University of Plymouth O’Brien Roger Tym and Partners E Williams Dr Mark Lee R Hein Project D101963 This document has been prepared in accordance with the scope of Scott Wilson’s appointment with its client and is subject to the terms of that appointment. It is addressed to and for the sole use and reliance of Scott Wilson’s client. Scott Wilson accepts no liability for any use of this document other than by its client and only for the purposes, stated in the document, for which it was prepared and provided. No person other than the client may copy (in whole or in part) use or rely on the contents of this document, without the prior written permission of the Company Secretary of Scott Wilson Ltd. -
2098 Explore Start
You can easily see wave cut platforms The Rock of Ages which were formed when sea levels were higher. Extremely jagged rocks This is when our rocks were This is when the big mountain The red sandstones were formed The Earth History Trail fi rst formed. They’re called building period happened, caused during the permian and triassic line the ridge. The ice sheet which ‘Devonian’ – because they by continents colliding - rocks period when a desert or semi arid covered much of Britain in the last ice were fi rst studied here. were folded and compressed. environment covered most of age didn’t come this far south so the Britain and northern Europe. What can you see..? And where..? rocks were subjected to freezing and Start Point thawing causing massive movement of loose material on the surface. Limpet Rocks Torcross Igneous intrusions can be The ruined village of Hallsands is built seen here. Molten rock on wave cut platforms in the mica The rocks beneath your feet help determine the shape of the seeped into gaps in the schist rocks. A protective shingle beach Meadfoot Slates where created by sea level rise after the ice age land, what grows on it and how and where we live. At the coast folding has created cracks. was removed by dredging before the First World War to develop Plymouth the sea has shaped the landscape and also washed away the docks. This made the village vulnerable Castle Cove South Hallsands to storms. In the background you can soil, making it easier to see how the rocks have been formed.