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MAP 14: VALLAY ISLANDHinterland Geology and Coastal Geomorphology:The Vallay strand and island are a conspicuous landscape element within this area.The island is largely sand-covered and consists of a lower western and higher easternend (30m OD). Sand ridges and coastal dunes dominate this area of land. Itsindented coastline contains a number of crescent-shaped beaches and sandyembayments on the west side of the island.Erosion Class:The island’s coastline has been recorded as eroding, or eroding or stable. The erodingcells correspond principally to the areas of sandy beach and dune. Eroding or stablecells include rocky stretches of coastline along the north-east of the island, theintertidal island of Morornish, and the east side of Aird Mhic Caoilt, where erosionwill be occurring at a much slower rate.Built Heritage & Archaeology:A number of sites of prehistoric date have been recorded on Vallay. These includetwo duns, middens and structures, and standing stones. Two chapels of possibleMedieval date, Teampull Mhuir and Teampull Orain, along with two stone crosseswere recorded. A possible Norse midden was recorded at Seidinish. The remainingsites consist of boat noosts, a jetty, buildings, enclosures and field boundaries relatingto the crofting landscape of the 18 th -20 th centuries.UISN/1051/0145CFA
MAP 14: HINTERLAND GEOLOGY AND COASTAL GEOMORPHOLOGYID Name of section NGR Length Typical deposit type on the foreshore Height of cliff Hinterland geomorphology Description86 East of TAIGHBHALAIGHNF 7828 7560 toNF 7762 76951.3km Marine sand Low edge(
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COASTAL ZONE ASSESSMENT SURVEYnorth
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CONTENTS1. Introduction 42. Methodo
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1. INTRODUCTION1.1 Background1.1.1
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incorporation into a GIS database t
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2.5.2 The GIS database incorporates
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3. THE PHYSICAL ENVIRONMENT OF THE
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Sea defences3.1.6 Concrete or woode
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4. ARCHAEOLOGICAL BACKGROUND OF THE
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Industrial Period4.11 There are ver
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MAP 1: HINTERLAND GEOLOGY AND COAST
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MAP 1: EROSIONID Name of coastal se
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MAP 1: BUILT HERITAGE AND ARCHAEOLO
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ID Name NMRS No. Source NGR Status
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MAP 2: RUBH’ A’ CHORRAIN TO BER
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NORTH UIST MAP 2 - HINTERLAND GEOLO
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NORTH UIST MAP 2 - EROSION CLASSRub
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NORTH UIST MAP 2 - BUILT HERITAGE A
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MAP 4: HORNAIS TO SGIOBANAISHinterl
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ID Name of section NGR Length Typic
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NORTH UIST MAP 4 - BUILT HERITAGE A
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NORTH UIST MAP 5 - EROSION CLASSSgi
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MAP 6: TRÀIGH IAR TO CAOLAS BHALAI
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NORTH UIST MAP 6 - EROSION CLASSTr
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MAP 7: CALARNAIS TO TRÀIGH STIRHin
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NORTH UIST MAP 7 - EROSION CLASSCal
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MAP 8: RUBHA MHÀNAIS TO HANGLAMHin
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ID Name of section NGR Length Typic
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MAP 9: HANGLAM TO HORISARY POINTHin
Page 96 and 97: ID Name of section NGR Length Typic
Page 98 and 99: MAP 9: EROSIONID Name of coastal se
Page 100 and 101: MAP 9: BUILT HERITAGE AND ARCHAEOLO
Page 102 and 103: ID Name NMRS No. Source NGR Status
Page 104 and 105: MAP 10: HORAISEARAIDH TO CLADACH IO
Page 106 and 107: NORTH UIST MAP 10 - HINTERLAND GEOL
Page 108 and 109: NORTH UIST MAP 10 - EROSION CLASSHo
Page 114 and 115: MAP 11: CLADACH IOĹARAIGH TO BALES
Page 118 and 119: MAP 11: EROSIONID Name of coastal s
Page 120 and 121: MAP 11: BUILT HERITAGE AND ARCHAEOL
Page 124 and 125: NORTH UIST MAP 11 - BUILT HERITAGE
Page 126 and 127: MAP 12: HINTERLAND GEOLOGY AND COAS
Page 134 and 135: MAP 13: BALESHARE CAUSEWAY TO BENBE
Page 150 and 151: NORTH UIST MAP 14 -HINTERLAND GEOLO
Page 152 and 153: NORTH UIST MAP 14 - EROSION CLASSVa
Page 156 and 157: NORTH UIST MAP 14 - BUILT HERITAGE
Page 158 and 159: 6.7 A potentially Norse period (10
Page 160 and 161: Period CategoriesUnknownMulti-phase
Page 162 and 163: 7. SUMMARY AND RECOMMENDATIONS7.1 S
Page 164 and 165: • Medium - Archaeological loss is
Page 166 and 167: previous visits by the Ordnance Sur
Page 168 and 169: 8. BIBLIOGRAPHY8.1 ReferencesArmit,
Page 170 and 171: Ritchie, W 1986 in Barber, J 2003 B
Page 172 and 173: Ordnance Survey 1904 Hebrides, Harr
Page 174 and 175: 8.4 Aerial Photographic RecordSorti
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Plate 1 - Erosion causing undercutt
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Plate 5 - Dune blowout, Port Scolpa
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Plate 9 - Site 113, abandoned settl
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Plate 13 - Site 360, eroding struct
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Plate 17 - Site 637, eroding struct
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