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Deil's Dyke

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29: 346: 279: 768: 358:'in-field' and 'out-field' are sometimes applied and both are clearly marked on the landscape as green lush vegetation on lower lying land against the more complex colours of bare rock, heather, bracken, etc. on the moors or out-fields. The development of field boundaries meant that head-dykes were no longer necessary and they fell out of use in the 18th and 19th centuries. 159:
accompanies the bank it is usually an inconsequential 0.5 m (1.6 ft) or so in width on average and around 0.4 m (1.3 ft) deep, more often located on the uphill or outfield side. As a defensive structure the dyke has no obvious military value and its erratic route militates against
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or elricks may have consisted of banks and ditches several kilometres long that were used to direct deer for the purpose of capture and the Deil's Dyke fits this description. "Deer hunting has left physical traces on the landscape in the form of banks and dykes used either as park boundaries or for
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In 1981 a section was excavated and was shown to consist of an earth bank only, likely to have been constructed on one single occasion. The turves used in its construction were taken from either side giving a width of 4.5 feet (1.4m) at the base with a maximum original height estimated at around 6.5
751:
A March House stands near the dyke at Burnmouth and the name 'Eliock' is given to the nearby wood. The word 'Elerc' in Gaelic originally meant 'ambush' and later meant a 'deer trap' described as a funnel-like defile, artificial or natural into which deer were herded so that they could be contained
357:
In a number of places along its route it has been utilised and modified or possibly originally built as a head-dyke which physically separated the arable lower lying land from the upland pastures which were grazed by sheep and cattle which would have otherwise eaten any arable crops. The terms
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that roughly follows the contours that divide upland pasture from lowland arable land, effectively acting like the head-dykes of medieval and later times although its true purpose has not been settled. The Deil's Dyke, sometimes written as 'dike', is formed from an earthen
725:
were credited with building many unusual or megalithic structures; as previously stated it can also be a variant of a word meaning a march or head-dyke that divides or separate into one or more parts. The term 'Pict's Dyke' is mainly applied in the parish of
306:
Some of the gaps in the course of the dyke may be due to the historical presence of dense woodland. Areas of once extensive woodland in Nithsdale are indicated on old maps such as in the 1660s when a Cashogill Wood (sic) is recorded near
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Local tradition states that the dyke was used to hide cattle from raiders or to interfere with raiders returning with stolen sheep, cattle, horses and other goods, delaying them long enough for pursuers to catch up with them.
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The name 'Deil's Dyke' or 'Devil's Dyke' is commonly associated in myth and legend with structures of this scale however it has also been noted that a name similar or identical to 'Deil's Dyke' can mean a 'march dyke'.
382:, southern Scotland, has a number of similarities with the Deil's Dyke and consists of a bank and a ditch and runs for 11.5 mi (18.5 km). It is considered to be a territorial land boundary dating from the 298:
function or a hunting forest demarcation fits the evidence better. It has been noted that a considerable number of similar earthworks exist in the vicinity of the dyke making interpretation a challenge.
220:, amongst others, for the description of what survived at the time and for recognising its significance, ambiguous as that remains. In 1841 a second report was published as an appendix in MacKenzie's 367:
The course of the Deil's Dyke is not noticeably associated with the many defensive features that exist in Nithsdale, such as Iron Age forts, medieval mottes, etc. although the linear earthwork near
1325: 718:'an oak copse', literally the "dark wood of the oak copse." This description would be relevant in terms of the termination of a detached section of the Deil's Dyke in a wooded area. 247:, watchtowers and forts however this has been shown to be incorrect as a number of the linear features included were shown to be head-dykes and other unrelated landscape features. A 1417:
The Royal Commission on the Ancient and Historical Monuments and Constructions of Scotland. Seventh report with inventory of monuments and constructions in the county of Dumfries
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No one single feudal land holder is known to have controlled such a large area so its construction as an estate boundary is implausible, but a mediaeval head-dyke function or a
825: 756:' is linked to such deer traps. A section of the dyke here is recorded by the RCAHMS in 1920 as having a foundation of large stones that indicate a width of seven feet. 364:
The dyke has also been proposed as a tribal territorial boundary or as a medieval land boundary however the irregular course of this linear feature makes this unlikely.
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of rounded form that varies from 2.0 to 4.0 m (6.6 to 13.1 ft) wide and a maximum of 0.7 m (2.3 ft) high, sometimes having a stone core. Where a
1481: 275:. This section is considered to have some credibility as a single structure constructed and planned through the control of a single controlling authority. 53: 47: 441:: In 1978 this section had a bank that on the north or downhill side enclosed an area of rig and furrow and lies close to the Hawkcleuch Burn. 1107: 208:
village, ending short of the Durisdeer Roman fortlet. The dyke follows contours that lie typically from 500 to 900 ft above sea level.
417:: In 1985 this section had been removed by ploughing and was indistinguishable in other sections. Ardoch Farm and the A76 lie to the east. 286:
often started at such points so that the animals could be driven from that area along the route that would lead to their point of capture.
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Areas of once extensive woodland in Nithsdale indicated on old maps such as in the 1660s a Cashogill Wood (sic) is recorded near
579:: In 1956 this section had no fosse, but it did have a clearly visible bank, 6 ft-9 ft thick and up to 3 ft high. 1438: 28: 1471: 690:: The dyke is thought to have started on the left bank of the Burnsands Burn in the area of its confluence with the 1208:
Transactions and Journal of Proceedings of the Dumfriesshire and Galloway Natural History and Antiquarian Society
786: 791: 361:
The often erratic route may be explained by the need to enclose as much good quality arable land as possible.
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feet (2m). although both late Iron Age and medieval dating evidence was found it was not conclusive.
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As a common place name the name 'Deil' can mean the 'Devil' who together with the semi-mythological
480:: The route was not possible to follow. A 230 yard gap may have existed if the OS route is ignored. 216:
In 1824 the Deil's Dyke is first recorded in print by Chalmers in his 'Caledonia' where he credits
147: 87: 1215: 1130: 1085: 796: 549:: A contemporary wall runs along the route of the Dyke. The site is close to the Glengenny Burn. 1486: 1476: 495:: In 1978 this section was hard to follow with minimal evidence. The Cowan Burn lies near by. 345: 248: 251:
survey of 1956 proposed that the dyke runs along a 16 miles route from near Burnmouth Farm (
745: 738: 636:: In 1956 the Dyke could be followed from the start of a sike tributary to Cubie's Cleuch. 312: 168:
The earthwork is not continuous; however, it is generally regarded as running from east of
204:. A detached section ran from the site of the old Durisdeer Castle to the Kirk Burn above 8: 1187: 1466: 884: 278: 1270:
Seventh Report with inventory of Monuments and Constructions in the County of Dumfries
1255:
Seventh Report with inventory of Monuments and Constructions in the County of Dumfries
1069:
Seventh Report with inventory of Monuments and Constructions in the County of Dumfries
853:
Seventh Report with inventory of Monuments and Constructions in the County of Dumfries
450:: In 1978 modern drains obscured the junction and the bank was 0.4m hugh and 2m wide. 1434: 744:
The March Cleugh is a small burn with a name meaning 'boundary' that flows from near
383: 333:
are sections of another similar linear earthwork there known as the 'Deil's Jingle'.
397: 1122: 801: 432:: In 1978 this length consisted of a stone and earth bank, 0.5m high and 4m wide. 773: 707: 741:(sic). A 'Priest Wood' is recorded on a map of 1832 lying below the old church. 402:
In 1956 much of the route was walked and the following observations recorded -
1451: 1126: 1460: 390: 379: 350: 323: 319: 295: 283: 734: 519:: The Dyke ran from the Cowan Burn to the northern side of Giengenny Hill. 308: 232: 217: 1232: 330: 272: 262: 258: 240: 193: 179: 169: 64: 34: 1389:
Caledonia: Or, An Account, Historical and Topographic, of North Britain.
1347:"Dumfriesshire on Sheet XIV. Survey date - 1856 Publication date - 1860" 928:"Dumfriesshire on Sheet XIV. Survey date - 1856 Publication date - 1860" 691: 353:
in Galloway is a natural feature once utilised for red deer management.
197: 564:: Arable land is taken in here and the dyke course was rather random. 879: 465:: In 1978 on the steep burn side slope the dyke was mostly obscured. 368: 228: 205: 189: 68: 1346: 1283: 1046: 1004: 927: 1304: 1025: 727: 603:: In 1978 This section had a clear profile, 2m wide and 0.7m high. 244: 201: 781: 627:: In 1978 the course was not discernible from more recent dykes. 398:
The surveyed section of the New Cumnock to Durisdeer Parish route
375: 1108:"The head-Dyke : A Fundamental line in Scottish Geography" 753: 1201:"The Celts (British and Gael) in Dumfriesshire and Galloway" 722: 236: 156: 152: 1284:"Blaeu Atlas Maior 1662-5, Volume 6. Nithia Vicecomitatvs" 1047:"Blaeu Atlas Maior 1662-5, Volume 6. Nithia Vicecomitatvs" 1005:"Blaeu Atlas Maior 1662-5, Volume 6. Nithia Vicecomitatvs" 874: 386:
and was once considered to link up with the Deil's Dyke.
697: 651:: In 1978 the 2m wide bank of the dyke ran to the burn. 318:
The RCAHMS have mapped sections of the Deil's Dyke near
1183: 1181: 763: 1381: 1326:"Ordnance Survey Dumfriesshire Name Book Volume 14" 1080: 1078: 1178: 282:Deer come to drink at sheltered water courses and 1396:Hunting and hunting reserves in medieval Scotland 33:A section of the Deil's Dyke on Dalhanna Hill at 1458: 1075: 371:is linked with the site of the medieval castle. 1424:Ayrshire Place-Names: a rich seam still to mine 681:: A farm track had obscured the dyke's course. 1433:. Dumfries: Dumfries & Galloway Council. 1431:Old Sanquhar Tales - A Collection of Folklore 752:and then killed. The personal or place name ' 1482:Archaeological sites in the Scottish Borders 1452:Durisdeer Roman Road, Fort and the Well Path 1403:Dumfriesshire - Cambridge County Geographies 1398:. Edinburgh. RCAHMS Shelf Number: C.3.52.GIL 978: 976: 974: 257:), north of Enterkinfoot to Dalhanna Hill, 146:in south-west lowland Scotland is a linear 952: 950: 948: 946: 944: 802:Devil's Dyke - Hungary, Romania and Serbia 27: 1105: 971: 870: 868: 866: 864: 862: 846: 844: 842: 160:it being a practical political boundary. 1405:. Cambridge: Cambridge University Press. 1305:"John Thomson's Atlas of Scotland, 1832" 1026:"John Thomson's Atlas of Scotland, 1832" 534:: In 1978 little of the route remained. 344: 277: 192:, having passed through the parishes of 941: 1459: 1276: 1267: 1252: 1198: 1156:"History of the Parish of New Cumnock" 1148: 1066: 1060: 1039: 907:"History of the Parish of New Cumnock" 859: 850: 839: 1412:. London: Cambridge University Press. 698:Cartographic evidence and place names 588:: No sign of the dyke survived here. 504:: No evidence of the route remained. 1410:The Gaelic Notes in the Book of Deer 1188:History of the Parish of New Cumnock 997: 899: 16:Ancient linear earthwork in Scotland 227:Originally it was said to run from 13: 1233:"Dictionary of the Scots Language" 818: 702:In 1328 Durisdeer was recorded as 14: 1503: 1445: 920: 1382:Bibliography and further reading 1106:Robertson, Isobel M. L. (1948). 766: 666:: Nothing remained of the dyke. 121:0.7 m (2 ft 4 in) 1426:. Ayrshire Notes. No. 38. ANHS. 1369: 1360: 1339: 1318: 1297: 1261: 1246: 1225: 1192: 1169: 1099: 311:, extending at least as far as 235:and was a boundary between the 1115:Scottish Geographical Magazine 1018: 1: 876:Historic Environment Scotland 812: 105:Up to 16 mi (26 km) 1408:Jackson, Kenneth H. (1972). 1401:Hewison, James King (1912). 787:Devil's Dyke, Cambridgeshire 7: 1199:Watson, William J. (1925). 792:Devil's Dyke, Hertfordshire 759: 336: 231:to the shores of the inner 163: 10: 1508: 807:Carsphairn and Scaur Hills 211: 1387:Chalmers, George (1824). 1127:10.1080/00369224908735398 125: 117: 109: 101: 93: 83: 75: 60: 45: 41: 26: 1472:History of Dumfriesshire 1268:RCAHMS, Francis (1920). 1253:RCAHMS, Francis (1920). 1067:RCAHMS, Francis (1920). 851:RCAHMS, Francis (1920). 618:: Visible here in 1950. 737:and extended as far as 1422:Taylor, Simon (2009). 1394:Gilbert, J M. (1979). 880:"Deil's Dyke (101258)" 354: 287: 113:3 m (9.8 ft) 97:Earth, stones and turf 1257:. HMSO. p. lvii. 1214:: 147. Archived from 348: 281: 249:Dumfries and Galloway 1272:. HMSO. p. lvi. 1071:. HMSO. p. Map. 855:. HMSO. p. lvi. 797:Devil's Dyke, Sussex 394:trapping the deer". 349:The Glen of the Bar 129:Medieval or Iron Age 126:Completion date 826:"Scotland's Places" 239:and the Britons of 222:History of Galloway 188:) in the parish of 23: 1429:Wood, Rog (2010). 1419:. Edinburgh: HMSO. 1391:London: T. Cadell. 1221:on 31 August 2014. 1086:"The Land we Made" 714:'a dark wood' and 355: 288: 21: 1492:Linear earthworks 1439:978-1-899316-74-8 1136:on 31 August 2014 984:"The Deil's Dyke" 384:Early Middle Ages 329:In the parish of 271:), south-west of 243:with a defensive 133: 132: 1499: 1376: 1373: 1367: 1364: 1358: 1357: 1355: 1353: 1343: 1337: 1336: 1334: 1332: 1322: 1316: 1315: 1313: 1311: 1301: 1295: 1294: 1292: 1290: 1280: 1274: 1273: 1265: 1259: 1258: 1250: 1244: 1243: 1241: 1239: 1229: 1223: 1222: 1220: 1210:. Third Series. 1205: 1196: 1190: 1185: 1176: 1173: 1167: 1166: 1164: 1162: 1152: 1146: 1145: 1143: 1141: 1135: 1129:. 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Issue 1. 331:Eskdalemuir 273:New Cumnock 263:Afton Water 259:New Cumnock 241:Strathclyde 194:New Cumnock 180:New Cumnock 170:Afton Water 144:Celt's Dyke 140:Pict's Dyke 136:Deil's Dyke 65:New Cumnock 35:New Cumnock 22:Deil's Dyke 1461:Categories 1352:22 January 1331:14 January 1310:22 January 1289:22 January 1238:22 January 1161:22 January 1140:22 January 1091:22 January 1052:22 January 1031:15 January 1010:22 January 989:16 January 963:16 January 933:22 January 912:22 January 891:16 January 831:16 January 813:References 692:River Nith 198:Kirkconnel 1467:Nithsdale 706:which in 704:Durrysder 369:Durisdeer 322:and near 229:Loch Ryan 206:Durisdeer 190:Durisdeer 148:earthwork 88:Earthwork 69:Durisdeer 760:See also 728:Sanquhar 337:Function 245:palisade 202:Sanquhar 164:Location 94:Material 76:Designer 61:Location 885:Canmore 782:Catrail 712:dubhros 376:Catrail 315:(sic). 284:elricks 212:History 178:) near 79:Unknown 1437:  754:Elrick 708:Gaelic 351:elrick 233:Solway 118:Height 102:Length 71:parish 1219:(PDF) 1204:(PDF) 1134:(PDF) 1121:: 6. 1111:(PDF) 723:Picts 716:doire 389:Some 237:Picts 157:fosse 110:Width 1435:ISBN 1354:2018 1333:2018 1312:2018 1291:2018 1240:2018 1163:2018 1142:2018 1093:2018 1054:2018 1033:2018 1012:2018 991:2018 965:2018 935:2018 914:2018 893:2018 833:2018 374:The 200:and 153:berm 84:Type 1123:doi 684:v. 675:to 669:u. 660:to 654:t. 645:to 639:s. 630:r. 621:q. 612:to 606:p. 597:to 591:o. 582:n. 573:to 567:m. 558:to 552:l. 543:to 537:k. 528:to 522:j. 513:to 507:i. 498:h. 489:to 483:g. 474:to 468:f. 459:to 453:e. 444:d. 435:c. 426:to 420:b. 411:to 405:a. 378:in 142:or 67:to 51:to 1463:: 1212:XI 1206:. 1180:^ 1119:65 1113:. 1077:^ 973:^ 943:^ 882:. 878:. 861:^ 841:^ 748:. 730:. 694:. 326:. 224:. 196:, 138:, 1441:. 1356:. 1335:. 1314:. 1293:. 1242:. 1165:. 1144:. 1125:: 1095:. 1056:. 1035:. 1014:. 993:. 967:. 937:. 916:. 895:. 835:. 265:( 172:(

Index


New Cumnock
NS 8000 0591
NS 8404 0526
New Cumnock
Durisdeer
Earthwork
earthwork
berm
fosse
Afton Water
NS 6169 1142
New Cumnock
NS 8400 0500
Durisdeer
New Cumnock
Kirkconnel
Sanquhar
Durisdeer
Joseph Train
Loch Ryan
Solway
Picts
Strathclyde
palisade
Dumfries and Galloway
NS 8400 0500
New Cumnock
Afton Water
NS 6169 1142

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