" the NON-CELTIC PLACE-NAIVES of the SCOTTISH BORDE-A COUNTIES. .A Thesis for the Degree of Ph. D. in the University Of

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" THE NON-CELTIC PLACE-NAIVES OF THE SCOTTISH BORDE-a COUNTIES. k.. .A thesis for the degree of Ph. D. in the University of Edinburgh .q submitted by MAY GORDON WILLIAMSON, " L. A. \' * October, 1942. 'Yjo3 . rý .I LIST OF CONTENTS. Page. i I. Preface .... .... Dialect II. Geography and ... iv III The Roman Period . .... .. xv IV. The Anglian Settlement of'Bernicia . xxvii V. Early Types of Place-Names as evidence Anglian Settlement of ... xxxv VI. The Battle Degsastan of .. .0 xli VII. The Ruthwell Cross . .... xliv VIII. Scandinavian Settlement and Place-Names xlix Ix. The Battle Brunanburh lix of .. .0 Personal Names in Place-Names lxv x. .. XI. Note Sources on .... .. lxviii List Sources Abbreviations lxxii xiz. of and .. XIII. OE Place-Name endings .... 1 XIV. Middle English Place-Name endings 171 XV. Scandinavian Place-Name endings .. 281 XVI. Index to Place-Names treated in Detail in Text .-.. .. 326 r i. PREFACE. This thesis has been produced under the conditi of the Gatty (Florence Emily and Charles Tindal) Memorial Scholarship, the holder of which "must pursue advanced study or research in Scottish Language and Literature with special reference to dialects on both sides of the border and to such border antiquities and music as bear on the subject". In order to satisfy these requirements as far as possible, rather more attention has been given to historical and dialectal notes than is usual or neces- sary in place-name studies. The following work is intended as a survey of Anglo-Saxon and Scandinavian place-name. material in the Border Counties. I have tried to demonstrate ; chat types of names occur, where they are situated, and roughly to what period they belong. Thus it has been more convenient to group the names under their endings than to arrange them by parishes in the mannet of the English Place-Name Society's volumes. It is almost impossible to date Scottish place- s with any certainty since spellings for the jority are not found before the 13th Century, but iii. they be under three headings generally may classified (a) Old English; (b) Middle English i (c) Scandinavian, and Middle English of Scandinavian origin. Between the first two classes is there must be a good deal of overlapping. It known that names in -Ling, -ingahäm, -i, ngtün and -ham the OE but probably ceased to be formed after period, in Eng- many of the other habitational endings which land belong. to this time must have continued to be formed at a much later date in the North. Similarly many of the names classified as Middle English may belong to the OE period. It has been my practice to count as an ending second element of each name if a habitative or topo- graphical term.. Thus Torvioodlee is discussed under 1-wood and Capehope Burn under -hope. Only the main, or original, parts of names are of importance in a survey of this kind, and so where groups occur such as Caverton, C, Mains, C--- Hillhead, Ce.. Mill, I ha dealt only with the basic name, Caverton. Names which do not appear in the 1 inch. Ordnance Survey maps, but which are found in sources before 1600, have been used for purposes of illustration and comparison. In most cases I have not consulted the 6 inch maps in attempts to locate these or other minor names .- The phonetic symbols used in the transcription of place-name pronunciations are those normally employed by the E. P. N. S. 6 iv. GEOGRAPHY and DIALECT. The Border area of Scotland divides into three main sections, the lowlands of Berwick and the Tweed- Teviot river basins on the north, a central mass of mountainous country, and the plain of Dumfries in the south. Berwickshire is cut off from Lothian by the Lammermoor Hills, through the western part of which, however, runs the valley of Lauderdale, the main in- land route from Lower Tweeddale to the north. The Merse is the continuation of the Northumbrian plain and stretches to the base of the Lammermoors. The parishes of Stichill, Ednam, Smailholm and Makerstoun, although part of this area, belong to Roxburghshire. The dialect of Berwick and Lothian is known as East Mi Scots. The main districts of Roxburgh are the valleys of the Tweed, Teviot and their tributaries. ' In the south are the Cheviot Hills through which passes lead to England.. To the. west is the watershed between Rox- burgh and Dumfries. At least half the area of the county lies more than 500 feet above sea-level. The parish of Castleton is mainly on the Liddel which V. drains to the Solway, and is really a separate dialect in area from the rest of Roxburgh, having affinities speech and in place-name forms with Dumfries and Cumberland (Watson, 6). Selkirkshire, which comprises mainly the valleys of the Ettrick and Yarrow and of a short stretch of the Tweed, is separated from Roxburgh by a watershed, although the parish of Ashkirk is on the Ale which flows into the Teviot. The dialect of the shire be- longs to the Southern Scots group which includes Roxburgh, Eskdale and Annandale (SND, Map 2). The place-names show a marked proportion of Gaelic forms which links the area with Peeblesshire, rather than with the other three Border counties in this respect. The greater part of Dumfriesshire belongs geo- graphically to the plain of Cumberland. All the rivers drain to the Solway. To the north are the Lowther Hills which divide Dumfries from Lanark, Peebles, Selkirk and Roxburgh. Nithsdale, at the head of which a pass leads into Ayrshire, is a separate dialect unit mich belongs to the West Mid Scots group. Gaelic infiuencejs very strong in place-names north and west of the Nith. Place-name forms before 1600 do not give much vi. indication of dialect distinctions, since these did not occur to any great extent until the end of the M.: period. It is not until the 16th and 17th centuries that occasional spellings reveal phonetic variations. Distinctions are more noticeable in vocabulary, in thi choice of place-name elements rather than in their form. Differences in pronunciation are found in the modern spoken versions. of the names rather than in their present spellings which have been reduced to a common Scots form. KXK Modern Lowland Scots is a development of the Old Northumbrian dialect of Old English, through Northern Middle English and Middle Soots. ' Only some half dozen place-names have spellings which go back to the OE period. A few late 11th Con- spellings found in the Durham Chartulary may be classe as very late OE or early ME. From late 12th Cent. tc mid 14th Cent. the language of the examples is Norther ME. Middle Scots continues until the late 16th Cent. Below are listed some of the developments observ- able between 0 Nb. and Mod. Sc. in the place-name forms Which have been collected. vii. ab a, 1. ?1E ä, whether from OE or ON is frequently fronted toe in M Sc. or early Mod. Sc. ME braken (from ON brakni. ) becomes brecken in Breckenside: - (Glc): Brekensyd, 1636, and in the modern forms of Breconrae, Brecken Rig, etc. (No. XXXII). ME Alis is the first element of Ellisland (No. LII). 2. OE ä is already fronted to I E: J in N ME. In spellings up to 1400 it is still a, but in the hi Sc. period is represented ai, ay. The i, y is used with all vowels in M Sc. to represent length. Th t {£ ] j the pronunciation of ai, ay was or ýE: at th 3 Le: ] period, however, and not yet is seen by the frequent substitution of ai for the sound [E. ] for LSE iý, e. g. Graitnay, 1598; Kailsoo, Blaeu; Fairnilee, 1599; Haitschaw, 1536. 3. M ai and ei interchange to represent 1 14 from OE 99 or ON ei, e. g. - (a) OE rWje-; ONb. gr-e -denu, ME gre; -dene : Greidene, 1095-1100; Granden, e 1288. (b) OE ej-tUn: Eitun, 1095-1100; Eyton, 1253; Atone, 1296. (c) ON rein: Greynland, 1542; Graines, 1635. (d) weit: ON -thuayt, c 1218; -thwýeyte, 1304; viii. -twayt, 1317; -pheit, 1194-1214. 4. In O. Northumbrian there was no Breaking of a before 1 plus consonant. Mod. Sc. haugh, saug h are developments of 0 Nb. halh, salh (W. S. healh, sea 0 Nb. walh is seen in Wauchope (No. LX). Before b, Breaks in this r plus consonant a, rarely area , (in e. g. 0 Nb. fa"brn, a-brn, -ward pers. - n's. ) 5. In M. Sc. al, of are vocalised to au, ou. ?1E hal? h M hau; h; 0 Nb. MSc. -So. ald ) auld; ME hol M. Sc. how. An inverted form of this process frequently appears: of. Falside for ME f arr- side . 5. OE äe' is e In non-W. S. dialects. OE str 'St N ?1E strete: Derestrete, 1150. Leitholm: Le that L'Y 1165-1214, from OE leset, 0 Nb. 17et. i 7. ON au 7 NE ou, later o in some cases. Copland i; Coupland, c 1230 from ON kaupa-. " Gowkhall (KF) contains ON gaukr. 3. OE ea undergoes Smoothing toe before -h in 0 Nb. W. S. heah, 0 Nb. heh 7M Sc. h_e__iE,, hei, hie: of. Hielawes, 1621. W. S. 'leih, 0 Nb. leh 7M Sc 1, ley, Mod. Sc. -. lie. ix. i e 9. ME from any source is frequently lowered to it Mod. Sc., e. g. OE hrls-tun ) ME Ristun Reston; ME Iliveston Elliston. Cf. PN Nb. Du., 257, e para.
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