Knowledge (XXG)

Neath Disturbance

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crossing the region, that is to say that it is responsible for a number of significant landscape features along its 100 km length. Prominent amongst these is the
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The Neath Disturbance is possibly the southernmost geological feature within Britain which can be described as following the Caledonoid trend. The phrase describes a
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British Geological Survey 1:50,000 map sheets 214, 215, 231 'Merthyr Tydfil', 232 'Abergavenny', 247 'Swansea' & accompanying memoirs
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Howells, M.F. 2007 'British Regional Geology: Wales' Keyworth, Nottingham, British Geological Survey
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valley on the English/Welsh border are also excavated along this line of weakness.
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and giving rise to the Caledonian orogeny or mountain-building period. The
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also lies on the Disturbance a little further east. A part of the Vale of
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along this line of weakness in the Earth's crust and now occupied by the
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are similar features found a little further north in south Wales. The
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which were active during the mountain-building period known as the
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and perhaps reflects a more ancient line of weakness in the
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is a geological structure which stretches across south
102:and the northeast-southwest aligned section of the 182:Ordnance Survey Explorer maps 165, OL12, OL13, 189 8: 113:associated with the closure of the former 166: 16:Geological structure in Great Britain 7: 111:suite of major geological structures 39:. It consists of a series of both 14: 62:The Disturbance gives rise to a 1: 70:, a deep valley incised by a 224: 131:Carreg Cennen Disturbance 31:northeastwards as far as 157:structures of Britain. 147:Highland Boundary Fault 143:Southern Uplands Fault 129:Disturbance and the 139:Menai Strait Fault 53:Caledonian Orogeny 21:Neath Disturbance 215: 208:Geology of Wales 192: 189: 183: 180: 174: 171: 153:are other major 151:Great Glen Fault 49:Variscan orogeny 223: 222: 218: 217: 216: 214: 213: 212: 198: 197: 196: 195: 190: 186: 181: 177: 172: 168: 163: 90:. The hill of 43:and associated 17: 12: 11: 5: 221: 219: 211: 210: 200: 199: 194: 193: 184: 175: 165: 164: 162: 159: 127:Swansea Valley 119:Palaeozoic Era 117:in the middle 84:Pontneddfechan 15: 13: 10: 9: 6: 4: 3: 2: 220: 209: 206: 205: 203: 188: 185: 179: 176: 170: 167: 160: 158: 156: 152: 148: 144: 140: 136: 132: 128: 124: 120: 116: 115:Iapetus Ocean 112: 107: 105: 101: 100:The Sugarloaf 97: 93: 92:Moel Penderyn 89: 85: 81: 77: 73: 69: 68:Vale of Neath 65: 60: 58: 54: 50: 46: 42: 38: 34: 30: 26: 22: 187: 178: 169: 108: 61: 20: 18: 88:Swansea Bay 80:River Neath 74:during the 35:in western 29:Swansea Bay 161:References 155:Caledonoid 135:Bala Fault 98:north of 64:lineament 202:Category 123:Cribarth 82:between 76:ice ages 57:basement 33:Hereford 72:glacier 59:rocks. 37:England 104:Monnow 96:Grwyne 41:faults 45:folds 27:from 25:Wales 149:and 86:and 19:The 125:or 204:: 145:, 141:, 137:,

Index

Wales
Swansea Bay
Hereford
England
faults
folds
Variscan orogeny
Caledonian Orogeny
basement
lineament
Vale of Neath
glacier
ice ages
River Neath
Pontneddfechan
Swansea Bay
Moel Penderyn
Grwyne
The Sugarloaf
Monnow
suite of major geological structures
Iapetus Ocean
Palaeozoic Era
Cribarth
Swansea Valley
Carreg Cennen Disturbance
Bala Fault
Menai Strait Fault
Southern Uplands Fault
Highland Boundary Fault

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