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Inveralligin.Pdf INVERALLIGIN WESTER ROSS LOCAL PLAN I ADOPTED I JUNE 2006 SETTLEMENT 183800 184000 184200 184400 184600 184800 185000 185200 Settlement Development Area (Policy 1) 0 0 0 0 0 0 8 8 5 Waterfalls 5 8 Torridon Forest 8 a h n d s i l l m a i a f h u r r e t Issues m D a a W t U l l - A COUNTRYSIDE h k c a r International importance (Policy 2.3) T National importance (Policy 2.2) Waterfall Local/regionally Waterfalls 0 Local/regional 0 important features 0 0 8 importance 8 7 7 e h A 5 5 c l l ` t i r No local designation (Policy 2.1) 8 D 8 C r u a i m Issues Clachan n Blaroor t l n l a A h - U Issues a in m ra D h a i d h Issues Stronvar Drain Heather Cliff Inveralligin Baile Thormaid Creag Bhan Sunny Bank Camas Glaise The Shalimar House Dorran Grianan Birchlea Glen Lean 0 0 Issues 0 Craigard 0 6 6 7 7 Rudha Dubh 5 5 Allt na Criche 8 8 Wave Crest Shingle Seaview e ingl Pier Sh End The Mission House lo pe DEVELOPMENT FACTORS (Policy 4.8) Craig Coastal S Rock Loiste Boulders Baldarroch Kwato Rock Leach S Rock l P i a p t Shingle and Boulders Shingle and Boulders h Blaroor Cottage Ivy Cottage w (u a M Carnalean Criche m y H ) Shore Cottage W Cottage S Rock • Views across the loch from the lower road Sheep Wash Broom Cottage Jetty BM 5.02m Rock The The Cabin Park Cottage le Boat House g should be protected. in Sh Rocky Bank Riverside Jetty (disused) Po st Shingle e TCB l g • n A number of natural and cultural heritage i h S A Rock bh ai features, as listed in Box 1, may occur nn A `i lig in FB S 0 h 0 i within the SDA boundary (see Background n Path (um ) g 0 0 l e 4 Maps). 4 7 7 5 Alligin 5 8 e 8 Free l g n Church i h Shingle S s g n i r p S r e t NTL a W w o L Seaforth M n L a W e S M PO Ben View P a t h LB Path Upper Culdarroch Pier Inveralligin Field Centre BM 5.65m 0 0 0 0 Rock Shingle 2 2 7 7 5 Upper Loch Torridon 5 8 INSET MAP 8 A' Chailleach Rock U n d Sh ing le & y R Bd EE t Rock ns Co Co Rock R o c S k W L M 0 0 0 0 0 0 7 7 5 5 8 8 PLANNING & DEVELOPMENT SERVICE THE HIGHLAND COUNCIL GLENURQUHART ROAD INVERNESS IV3 5NX Tel. (01463) 702250 www.highland.gov.uk © Crown Copyright. The Highland Council 100023369 2005. All OS base maps are the most up-to-date available to The Highland Council at the time of the production of this Local Plan. In some instances they may not reflect exactly what is on the ground and have not been altered in any way by The Council. Information provided by other agencies for use in determining some of the mapped features 183800 184000 184200 184400 184600 184800 185000 185200 is also the most up-to-date available to The Highland Council at the time of the production of this Local Plan..
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  • Scottish Journal of Geology
    Scottish Journal of Geology On the origin and stability of remanence and the magnetic fabric of the Torridonian Red Beds, NW Scotland T. H. Torsvik and B. A. Sturt Scottish Journal of Geology 1987; v. 23; p. 23-38 doi: 10.1144/sjg23010023 Email alerting click here to receive free e-mail alerts when service new articles cite this article Permission click here to seek permission to re-use all or request part of this article Subscribe click here to subscribe to Scottish Journal of Geology or the Lyell Collection Notes Downloaded by on January 24, 2012 © 1987 Scottish Journal of Geology On the origin and stability of remanence and the magnetic fabric of the Torridonian Red Beds, NW Scotland T. H. TORSVIK1 and B. A. STURT2 institute of Geophysics, University of Bergen, N-5014 Bergen-U, Norway 2Geological Survey of Norway, Leif Eirikssons vei 39, P.O. Box 3006, N-7001 Trondheim, Norway SYNOPSIS Primary (compactional) magnetic fabrics and multicomponent rem- anences are recognized in the Stoer and Torridon Groups. Low tempera- ture (LT) blocking remanences are randomized around 400-600°C and relate to a post-Torridonian magnetic overprint, possibly of early Mesozoic age. In the Stoer Group (and some Stoer boulders in the basal Torridon Group) LT remanences are partly or fully carried by magnetite (titanomagnetite). High temperature (HT) remanences are characterized by discrete unblocking above 600°C, having a specular haematite remanence carrier. Results of a conglomerate test of some Stoer boulders provides a positive stability test for HT remanences in the Torridon Group, and a convergence of evidence suggests that remanence acquisi- tion of both the Stoer and Torridon Groups was facilitated by both detrital and early diagenetic processes.
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