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In profile, the earthwork consists of a ditch about 6–12 ft wide and 2–4.5 ft deep, and a parallel embankment about 8–13 ft wide and 2 ft high. There is generally a lesser bank running along the other side of the ditch which is quite wide but only a few inches high. The main bank
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The
Catrail is discontinuous and although the various sections are not fully aligned they are considered parts of a single structure on the grounds that the profile is similar from section to section. Between sections, the line generally seems to follow the courses of streams and rivers.
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It is not known when or by whom the
Catrail was made, or for what purpose. However, since it is not substantial enough to be an effective military barrier, it seems likely to have been a territorial boundary marker, possibly dating from the
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The
Catrail cuts across the upper Teviot valley, separating the low-lying farmland to the north-east around Hawick in Teviotdale from the hillier up-river country to the south-west.
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149:, Volume 1 (1893). He believed that it had been constructed early in 7th Century to mark the south-eastern boundary of the territory held by the
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undertook a survey of the
Catrail in the late 19th Century and devoted a chapter to it in his
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Royal
Commission on the Ancient and Historical Monuments of Scotland (1956).
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Inventory of the
Ancient Monuments: Roxburghshire (Appendix D)
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109:was once considered to extend to the Catrail.
221:Archaeological sites in the Scottish Borders
16:Archaeological linear earthwork in Scotland
199:History and Poetry of the Scottish Border
147:History and Poetry of the Scottish Border
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122:is on the north-east side of the ditch.
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141:The philosopher, poet and historian
66:), a burn (stream) flowing into the
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231:Scheduled monuments in Scotland
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35:. It runs from Robert's Linn (
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203:William Blackwood and Sons
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175:Stationery Office Books
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101:), a tributary of the
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197:Veitch, John (1893),
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25:earthwork
33:Scotland
21:Catrail
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179:ISBN
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