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Somerset · G. W. Wade — chapter 3 of 27 · ~4,878 words · public domain

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Roads.--Everywhere highways and byways are numerous, and some districts are prodigally supplied with footpaths. With the exception of Exmoor, which is best explored on foot, even the remotest parts are accessible to the wheelman. But the cyclist will find the travelling somewhat unequal. Like the curate's fabled egg, the roads are best described as "good in parts." Amongst the hills they are firm but arduous, in the plains easy but soft. The main thoroughfares, however, can be recommended both for breadth and surface.

Railways.--The Somerset railway system is extensive. The G.W.R. (the chief service of the county) unites Bath with Bristol, and throwing itself round the N.W. extremity of the Mendips, runs down an almost ideal track to Taunton and Wellington. A loop from Worle to Uphill serves Weston-super-Mare, whilst short branches, one from Bristol and a second from Yatton, afford communication with Portishead and Clevedon. Another section skirts the E. side of the county from Frome to Yeovil, and by taking a short cross-country cut from Castle Cary to Langport unites again with the trunk line near Taunton. From Taunton branches radiate to Minehead, Dulverton, Chard, and Yeovil. A branch line again connects Bristol with Frome, and access is obtained to Wells and Cheddar by a line from Yatton, skirting the W. base of the Mendips as far as Witham. The S. & D. constitutes a link between the Midland on the N. and the L. & S.W. on the S. It boldly attacks the Mendips from Bath, and after clambering over the summit at Masbury, drops down suddenly to Evercreech, from which point it diverges either westwards to Burnham (with branches to Wells and Bridgewater), or southwards to Templecombe. A light railway serves the Wrington Vale, and another connects Weston with Clevedon.

IV. PHYSICAL FEATURES AND GEOLOGY

There is a prevalent belief that the picturesque part of the West of England begins with Devon and ends with Cornwall, to which Somerset is merely a stepping-stone. This opinion is no doubt fostered by the impression which the tourist derives of the county through the carriage windows of the "Cornishman." But the considerations that appeal to the railway engineer are mechanical rather than aesthetic; and, unfortunately for the reputation of Somerset for scenery, the line of least resistance is the line of least interest--the dead level skirting the coast between Bristol and Taunton. As a matter of fact, there are few districts which afford such a variety of physical features as Somerset. Hill and valley, cliff and chasm, moor and seaboard, are all to be found there; and, in addition to its wealth of scenery, Somerset is rich in antiquities of different kinds; whilst it has also been the theatre of some of the most stirring events in English history.

The physical skeleton of the county may be roughly described as consisting of three parallel ranges of hills running transversely across it--the Mendips and their outliers in the N.E., the insignificant Poldens in the centre, and the Quantocks and Exmoor in the W., with the Blackdowns occupying the S.W. corner. The intervening basins are filled with a rich alluvial deposit washed down from the hills or left by the receding sea. The Mendips spread themselves across the E. end of the county in a N.W. direction from Frome to Weston-super-Mare, where they lose themselves in the Channel, to re-appear as the islets of the Steep and Flat Holms. On their S.W. side they descend into the plain with considerable abruptness; and when viewed from the lower parts of the county, present a hard sky-line, like some enormous earthwork. On the opposite side their aspect in general is far less impressive, and towards Bath they lose themselves in a confusion of elevations and declivities. The main ridge is an extended tableland, some 25 m. long, and in places 3 m. broad. It rises to its greatest heights at Blackdown (1067 ft.) and Masbury (958). Geologically, it consists of mountain limestone superimposed on old red sandstone, which here and there comes to the surface. Near Downhead there is an isolated outburst of igneous rock. The Mendips are honeycombed with caverns, the most notable being at Banwell, Harptree, and Burrington; and a large one has been recently discovered some 4 m. from Wells. At Cheddar their W. edge is broken by a remarkable gorge, in the sides of which caves also occur. The level of the tableland is indented with "swallet holes," the chief of which are the East Water Swallet and the Devil's Punch-Bowl. The Quantocks are much less extensive, though their highest summits rise to a greater altitude. Like the Mendips, they turn their steepest flank westwards, the ascent on the E. being gradual; and on this side they are cut by a number of well-timbered and delightful combes. Few caves have been discovered in them, though there is one at Holwell near Asholt. W. of the Quantocks are the Brendons and the highlands of Exmoor, the latter extending into Devon, though their highest point, Dunkery Beacon, is included in Somerset. Dunkery is 1707 ft. above the sea-level; and other conspicuous hills in this district are Lucott Hill (1516), Elworthy Barrow (1280), Selworthy Beacon (1014), and Grabbist Hill. The Quantocks, Brendons, and Exmoor consist of older rocks than the Mendips, belonging as they do to the Devonshire series of old red sandstones. Bordering the Brendons are found the red marls of the Permian series; whilst between Dunster and Williton, and along the base of the Quantocks, in the neighbourhood of Taunton Dean, as well as in some other localities, Keuper and Rhaetic beds occur. The Blackdowns in the S.W. are not quite so elevated as their neighbours; near Otterford and Chard they consist of greensand, whilst chalk appears at Combe St Nicholas and Cricket St Thomas. The centre of the county is alluvial, and beneath it the limestone of the Mendips sinks, coming to the surface again in the W. only at a single spot, near Cannington. Out of this central plain rise several isolated, cone-like hills, the most notable being Glastonbury Tor and Brent Knoll. These belong to the lias and lower oolite rocks. The Poldens consist of lias; and the same formation constitutes the rising ground that bounds the plain on the S. and E. of the county. The southern side of the Poldens is edged with Rhaetic beds, which also extend to High Ham. Oolite rocks occur abundantly near Bath, furnishing the famous Bath building-stone; and they likewise form the prominent eminence of Dundry. Near Frome they rest upon the mountain limestone. The same series of rocks occupies the S.E. corner of the county, extending from Milborne Port to Bruton. On the E. they are flanked with the Oxford clay, which reaches from Henstridge to Witham Friary, whilst a ridge of higher ground near Penselwood consists of greensand. Near Radstock coal is found.

The Somerset sea-coast, though destitute of ruggedness and grandeur, possesses undeniable charm, at least at its W. and E. extremities; but it lapses into unquestioned tameness where the sea washes the central flats. The waters of the Bristol Channel as far down as Minehead are discoloured; and, with the exception of a range of low cliffs near St Andries and Watchet and a stony foreshore at Clevedon, there are no rocks worth mentioning. Brean Down and the North Hill near Minehead are the only headlands, but notwithstanding this, the watering places of Somerset are breezy and healthy. Weston-super-Mare in particular has a high reputation for salubrity, and has long been one of the most popular seaside resorts in England.

Somerset is peculiarly deficient in large rivers, for the Avon can hardly be included amongst its belongings, since it is the dividing line between the county and Gloucestershire. The Parrett is the one stream of any moment. It is a sluggish and uninteresting bit of water, rising in Dorset, entering Somerset near Crewkerne, and flowing, when it meets the tide near Bridgwater, with a wearisomely circuitous course of some 12 m. before it mixes with the Bristol Channel. The other rivers, the Frome and Chew, which join the Avon; the Axe, which rises in Wookey Hole and enters the sea near Brean Down; the Brue and Cary, which empty themselves into the estuary of the Parrett; and the Parrett's own tributaries, the Yeo, Ivel, and Tone, are unimportant. Exmoor is drained by the Exe and Barle, which, when united, flow southward into Devon.

Such, however, is the character of Somerset scenery that the absence of water in it is hardly noticed. From what has been said it will be seen that the county has much in it to arrest the attention of the traveller who can appreciate quiet beauty, and, as will appear, even more to appeal to one who is interested in his country's-past, whilst upon the affection of its sons its hold is indisputable. As one of them writes:--

"Fair winds, free way, for youth the rover; We all must share the curse of Cain: But bring me back when youth is over To the old crooked shire again.

Ay, bring me back in life's declining To the one home that's home for me, Where in the west the sunset shining Goes down into the Severn sea."

V. FAUNA AND FLORA

The really interesting fauna of Somerset belongs to a past age, when mammoths, elephants, and rhinoceroses, cave lions, bisons, bears, and hyaenas roamed over its surface. Their remains have been found in the caverns of Hutton, Bleadon, Banwell, and Wookey, and are preserved in Taunton Museum. Of the wild creatures which at present occur in the county, the only one which confers real distinction upon it is the red deer, which roams at large on both Exmoor and the Quantocks. Badgers are not uncommon near Dulverton and in the more uncultivated districts. The very diversified character of Somerset makes it the home of a large variety of birds, the Quantocks and Exmoor sheltering many of the predatory kinds, the long coast-line attracting numerous seafowl, and the fenny country of the centre affording a feeding ground for the different kinds of waders. Of the resident species which are comparatively uncommon elsewhere may be mentioned the hawfinch, the greater and lesser spotted woodpecker, the carrion crow, the raven, the buzzard, the hen-harrier, and the peregrine falcon. Among the regular visitors are included the white wagtail, the pied flycatcher, the nightjar, the black redstart, the lesser redpole, the snow bunting, the redwing, the reed, marsh, and grasshopper warblers, the siskin, the dotterel, the sanderling, the wryneck, the hobby, the merlin, the bittern, and the shoveller. As occasional visitors may be reckoned the wax-wing, golden oriole, cross-bill, hoopoe, white-tailed eagle, honey buzzard, ruff, puffin, great bustard, Iceland gull, glaucous gull, and Bewick's swan. Visitors that may be supposed to have reached the county only by accident have scarcely a claim to be noticed here, though perhaps allusion may be made to an Egyptian vulture seen at Kilve in 1825, and specimens of Pallas's sand-grouse observed near Bridgwater, Weston-super-Mare, and Bath.

As regards the flora the elevated position of parts of the county makes it the home of a number of plants which do not commonly occur in the South of England. Thus there are found on Exmoor the crowberry (Empetrum nigrum), the parsley fern (Cryptogramme crispa), and the oak fern (Phegopteris dryopteris). Asplenium septentrionale is found at Culbone; Listera cordata grows on Dunkery and near Chipstable; and the cranberry (Oxycoccus palustris) is said to occur at Selworthy and on the Brendons. On the other hand, Somerset likewise furnishes congenial conditions for those plants that love low-lying, marshy ground, and on the peat-moors in the Glastonbury district the flowering fern (Osmunda regalis) and the bog myrtle (Myrica Gale) are met with. Within the British Isles the following are found only in Somerset: Dianthus gratianopolitanus, Hieracium stinolepis, Verbascum lychnitis, and Euphorbia pilosa. Arabis stricta occurs only on the limestone near Clifton; Helianthemum polifolium is confined to Somerset and Devon; Pirus latifolia to Somerset and Denbigh.

For the birds of Somerset, see a paper by the Rev. Murray A. Mathew, M.A., F.L.S., in the "Proceedings of the Somerset Archaeological and Natural History Society," vol. xxxix., from which we have borrowed.

For fuller information, see "The Flora of Somerset," by the Rev. R.P. Murray, M.A., F.L.S., from which the above facts are taken.

VI. HISTORY

Somerset gets its name from a Saxon tribe, but its earliest inhabitants, like those of the southern half of bur island generally, were Britons or Celts, and the Saxon invasion was preceded by the Roman. Reminders that the county was once occupied by a Welsh--speaking race occur in the constituents of many place-names, such as Pen Selwood, Maes Knoll, and the numerous combes (cp. Welsh cwm). The name of the British king, Arthur, is associated with Cadbury (near Sparkford); and the neighbouring villages of Queen Camel and West Camel recall the legendary Camelot. The earliest church at Glastonbury (Avalon) is believed to have been of British origin, and it is Arthur's reputed burial-place. In the dedication of the churches at Porlock (Dubricius or Dyfrig) and Watchet (Decuman or Tegfan) is preserved the memory of certain British saints, though these probably came on an evangelistic mission from the other side of the Bristol Channel. But of the primitive population the most trustworthy memorials are the numerous earthworks and other material remains which survive in various parts of the county, and these will be more appropriately noticed under another heading (see pp. 20-21).

Of the Roman occupation the traces are more varied. Bath and Ilchester are Roman towns, and from and through them Roman roads run across the county. In constructing these, the Romans probably used in many instances existing British trackways. The principal was the Fosse Way (as it is called), entering the county near Chard from Seaton, and leaving it at Bath for Lincoln. Within Somerset it is still a very important artery of traffic. From near Chard a road is thought to have diverged from it to the N.W., towards the Quantocks, passing by Castle Neroche. The Fosse Way was, and is, cut at Ilchester by a road coming from Dorchester and continuing to Glastonbury, and near Masbury, on the Mendips, by a second, connecting Old Sarum with Axium (Uphill, near Brean Down). At Bath it was joined by two more roads, one coming from London and the other (the Via Julia) from Aust and South Wales. The road along the Mendips was doubtless largely used for the transport of the lead which was mined at Priddy and elsewhere, and shipped at Uphill. Somerset, during its occupation by the Romans, seems to have enjoyed tranquillity, for their villas, pavements, and other remains indicative of peaceful possession are not confined to the neighbourhood of their large cities (see p. 21).

When the Saxons made themselves masters of England, Somerset became part of the kingdom of Wessex. Its subjugation was accomplished in three stages. The first is associated with the name of Ceawlin, who, after defeating the British at Deorham (in Gloucestershire), captured Bath, and by 577 reduced the northern part of the county between the Avon and the Axe. Englishcombe near Bath recalls this occupation, and the Wansdyke probably served as a barrier between Saxon and Briton. But between this conquered territory and Dorset, which was also Saxon, there still remained in the hands of the Britons a large strip of country; and from this they were not expelled until the time of Cenwealh (652), who defeated them in 658 at "The Pens" (identified by many with Penselwood), and drove them westward to the Parrett. Somerton now became the capital of the Somersaetas, the Saxon tribe that gave its name to the county (just as the Dorsaetas and Wilsaetas have done to Dorset and Wilts). The third stage of the conquest was completed by Ina (688-726), who subdued the rest of Somerset, forcing the British (whose king was Geraint) into Devon and Cornwall, and building Taunton as a fortress against them. Williton and Willsneck (in the Quantocks) perhaps preserve the name of the defeated Welsh. Ina is famous for more than his military prowess, for he was the first King of Wessex to issue written laws for the guidance of his subjects.

During the Saxon period Somerset did not escape the raids of the Danes; and in the reign of Alfred it was the scene of one of the most eventful crises in English history. Alfred, after many battles against the invaders, had at last seen Guthrum their leader retire from Wessex into Mercia. But in 878, in midwinter, Guthrum suddenly surprised Chippenham and made himself master of Wessex, and Alfred was forced to withdraw to the fens of Athelney. To the narrow limits of the "Isle of the Nobles" the Saxon dominions in the W. were for some months reduced. Here in the Eastertide of 879 Alfred, in the words of the "Saxon Chronicle," "wrought a fortress [of which perhaps the Mump at Borough Bridge is the site], and from that work warred on the (Danish) army, with that portion of the men of Somerset that was nearest." Seven weeks after Easter, Alfred emerged from his place of refuge to join the men of Somerset, Wilts, and Hants, who had gathered in force at "Ecgbryhtes Stane" (Brixton Deveril in Wilts). Putting himself at their head, he covered the distance that separated him from the foe in two stages; for, halting for the night at "Iglea," the next day he defeated the Danes at "Ethandune," and then besieged and reduced their fortress or fortified camp. Guthrum, after his defeat, was baptised at Aller; and at Wedmore subsequently a treaty of peace was concluded between him and Alfred. The site of the battle of "Ethandune" is unfortunately difficult to determine. There is an Edington in Somerset on the Polden Hills; and the fact that the battle was followed by Guthrum's baptism at Aller and the treaty at Wedmore (places near the Somerset Edington) is in favour of this being the scene of the encounter. Those who accept this identification assume that the Danes had moved from Chippenham to the Poldens, and here, whilst watching Athelney, were taken in the rear by Alfred, whose single night-halt at "Iglea" on the march from Brixton Deveril is placed at Edgarley, a locality near Glastonbury. But the distance between Brixton Deveril and Glastonbury seems too great to be accomplished by a large body of men along indifferent roads in a single day; and by many authorities "Ethandune" is identified with Edington, near Westbury, or Heddington, W. of Melksham, both in Wilts. However this may be, it was from the Somerset marshes that Alfred issued forth to his victory, and it was at a Somerset town that he secured the fruits of it.

The importance of Somerset during the reign of the Saxon kings who succeeded Alfred is evidenced by the many noteworthy incidents that are connected with its chief city, Bath, and its great abbey of Glastonbury. It was at Bath that King Edgar was crowned in 973; and at the same place at a later date (1013) the Danish king, Sweyn, received the submission of the western thegns. At Glastonbury were buried three of the Saxon kings, Edmund (son of Edward the Elder), Edgar, and Edmund Ironside. Here too was born Dunstan, who was so prominent an ecclesiastic in the reigns of the first Edmund and five of his successors. He was made abbot of the abbey by Edmund, and, after becoming Archbishop of Canterbury, was buried at Glastonbury (988). Two other Somerset men who filled the see of Canterbury during the Saxon period were Ethelgar and Alphege.

Under the Plantagenets the history of the county was not very eventful, though some localities suffered severely in the disturbances of the Norman period. In William Rufus' reign it was the scene of several of the movements directed against the king in favour of his brother Robert. The powerful baron-bishop, Geoffrey of Coutances, with his nephew Robert of Mowbray, after seizing Bristol, burnt Bath, but was unsuccessful in the siege of Ilchester (1088). On the death of Henry I. Somerset favoured the claims of Matilda, and the castles at Cary, E. Harptree, and Dunster were held by their owners for her against Stephen, to the no small discomfort of their respective neighbourhoods. Castle Cary and Harptree were taken by Stephen, but he seems to have regarded Dunster (defended by William of Mohun) as impregnable.

In Tudor times Somerset witnessed the attempt made on the throne by Perkin Warbeck in 1497, who was supported by Lord Audley of Nether Stowey and other Somerset gentlemen. The pretender advanced from Devonshire to seize Taunton; but when Henry VII. entered Somerset, passing in his progress through Bath, Wells (where he stayed with the Dean), and Glastonbury, to Taunton, Warbeck lost heart and fled. When captured and brought into Henry's presence he was spared; but the king's clemency did not extend to his supporter Lord Audley, who was executed on Tower Hill.

During the Great Rebellion in the 17th cent. Somerset was the field of many important operations. At the outbreak of war in August 1642, the royal cause was maintained by the Marquis of Hertford, who was supported by Lord Powlett, Sir Ralph Hopton, Sir John Stawell, and other leading gentlemen of the county. But the sympathies of the yeomen and manufacturers were with the Parliament, and Hertford had to withdraw from Wells, where he had taken up his position, to Sherborne. In 1643, however, the king's Cornish army entered Somerset, and was joined by the Marquis and Prince Maurice at Chard; and the Royalists then rapidly became masters of Taunton, Bridgwater, and Dunster. To oppose them, Sir William Waller was despatched to the West, and a cavalry skirmish between the two forces took place on the Mendips near Chewton. Waller's main army was posted at Bath; and the Royalists, advancing by way of Wells and Frome, had another skirmish near Claverton. They kept E. of Bath and reached Marshfield in Gloucestershire, 5 m. N. of the city. Then on July 5 Waller gave battle on Lansdowne Hill, and was forced to retire back to Bath, abandoning a quantity of arms and stores; but the triumph of the victors was clouded by the loss of Sir Bevil Grenville, who was killed in the fight. (The monument to him on the site of the encounter was erected in 1720.) The next year the king's cause in Somerset was less prosperous, for Taunton was lost, and repelled all the efforts of Colonel Wyndham, Governor of Bridgwater, to recover it. In 1645 the siege of Taunton was undertaken by Goring. The town was defended by Blake, who vowed (it is said) that he would eat his boots before he would surrender it, but he was saved from that extremity by Fairfax. On the approach of the latter Goring drew off from Taunton, and fixed his quarters at Langport, where he was attacked and defeated. This success on the part of Fairfax not only saved Taunton, but enabled him to besiege Bridgwater, which was defended by Wyndham with little resolution, and fell on July 23, within a fortnight of Goring's defeat at Langport. Fairfax also took Nunney Castle; and as in 1646 Dunster, the last place in Somerset supporting the king, also submitted, the entire county passed into the hands of the Parliament. Dunster was defended by another Wyndham, but he offered a much more prolonged resistance than his brother at Bridgwater, and withstood the besiegers for 160 days. After the execution of the king the small rising in favour of Charles II., under Colonel Penruddock and Sir Joseph Wagstaff, was crushed near Chard in 1655.

In the reign of James II. Somerset was the soil upon which was fought the last battle that has taken place in England. In 1680, the Duke of Monmouth, in the course of a tour through the county, greatly ingratiated himself with its people; and at Whitelackington held a great reception under a gigantic chestnut tree, which was standing as recently as 1897, when it was unfortunately blown down. When in 1685 Charles II. died, and Monmouth made his attempt to disturb the succession of James, it was to Somerset that he looked for support. After landing at Lyme, he entered the county at Chard, and passing through Ilminster, was proclaimed king at Taunton and Bridgwater. From the latter town (where he had stayed at the castle), he started on his luckless campaign, which was wholly confined within the borders of Somerset. He proceeded through Glastonbury (where some of his troops bivouacked in the Abbey), Wells, and Shepton Mallet, intending to attack Bristol, but at Keynsham he turned aside on finding the city defended by the Duke of Beaufort. He threatened Bath, but it refused to surrender; and he thereupon retired to Norton St Philip, intending to enter Wilts. There he had a skirmish with the advanced guard of the royal forces which had marched from London to meet him; and shirking a more general engagement, he withdrew to Frome. The townspeople of Frome, like those of Taunton and Bridgwater, gave him their sympathy, but nothing else; and disappointed at the lack of support, and wearied with his march along miry roads in drenching rain, he abandoned the advance into Wiltshire. A report that a rising in his favour had taken place at Axbridge decided him to return to Bridgwater. On the way he again passed through Wells, where some of his men tore the lead from the Cathedral roof to make bullets, and inflicted other damage on the building. Soon after his arrival at Bridgwater, the royalist general, Feversham, with about 4000 troops, reached Weston Zoyland from Somerton, disposing some of his forces at the neighbouring villages of Middlezoy and Chedzoy. As the royal troops were said to be in a state of disorder, Monmouth, who had about 6000 men, very badly armed, determined to attack him by night; and late on Sunday, July 5, he started from Bridgwater under cover of darkness. But in the passage of some of the "rhines" which cut up the Sedgemoor plain a mismanaged pistol gave the alarm; and in the engagement that followed his ill-equipped followers, though they fought bravely, had little chance against the regulars, and more than 1000 of them fell on the field. The battle had a sad sequel for Somerset. James knew no clemency; and Jeffreys' bloody assize left a crimson trail across the country, which even time found some difficulty in obliterating. Macaulay estimates that the number of the rebels hanged by Jeffreys was 320, and though the assize extended into Hampshire, Dorset, and Devon, most of its victims were Somerset folk. A certain poetic justice may perhaps be discerned in the fact that when, in 1688, the Prince of Orange drove James from his throne, his march took him through Somerset, and he had a skirmish with the royal troops at Wincanton. In connection with Somerset's share in the events of James's reign, it deserves to be mentioned that Bishop Ken, of Bath and Wells, was among the seven prelates who presented the famous petition against the king's Declaration of Indulgence.

The ecclesiastical history of Somerset may be briefly related. When Cenwealh of Wessex (who had been converted to Christianity by the King of East Anglia) established the bishopric of Winchester, such parts of Somerset as belonged to the West-Saxon kingdom were included in that see. Ina divided his augmented territories between two bishoprics, Winchester and Sherborne, the latter including Somerset, with Wilts, Berks, and Dorset. The first Bishop of Sherborne was Aldhelm (705), who only filled the see for four years, dying at Doulting in 709. Ina also founded Wells, but as a collegiate church of secular canons, not as the cathedral of a diocese. It was not until 909 that Somerset had a bishop all to itself, who was styled the Bishop of the Somersaetas, with his seat at Wells (the first appointed being Aethelm.) In 1088, in accordance with the policy of removing bishoprics from localities of little importance, the see was transferred from Wells to Bath, the bishop (John de Villula) at the same time becoming the abbot of the monastery. In 1192 Bishop Savaric procured for the see the rich abbey of Glastonbury, and became its abbot; and he and his immediate successor, Joceline, the builder of the W. front of Wells, were styled Bishops of Bath and Glastonbury. In 1224, however, another change was made, and the bishop took his title from Bath and Wells, as he has done ever since. Up to the Reformation the title was justified, both the monks of Bath and the canons of Wells taking part in episcopal elections; but, with the suppression of its monastery, Bath naturally lost this distinction.

Of religious houses Somerset possessed a fair proportion. The chief were Glastonbury, Bath, Bruton, Dunster, Muchelney, Stogursey (which were Benedictine), Cleeve, Barlynch (Cistercian), Hinton, Witham (Carthusian), Taunton, Woodspring, Stavordale (Augustinian), Montacute (Cluniac). The Templars had a preceptory at Templecombe, and the Knights of St John had establishments at Bridgwater and Mynchin Buckland (near Durston).

Thorpe's translation.

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