Snodhill Castle, Peterchurch
Has been described as a Certain Timber Castle (Motte), and also as a Certain Masonry Castle
There are masonry footings remains
| Name | Snodhill Castle, Peterchurch |
| Alternative Names | Strate; Castle of Staddle; Snothill |
| Historic Country | Herefordshire |
| Modern Authority | Herefordshire |
| 1974 Authority | Hereford and Worcester |
| Civil Parish | Peterchurch |
Earthwork, buried, and ruined remains of a shell keep castle, occupying a spur of high ground overlooking the River Dore, near the head of the Golden Valley, and east of the settlement of Snodhill. The shell keep was constructed on the site of an earlier motte and bailey castle, which is believed to have been established in the 11th century, and included a motte on the summit of the spur, with a bailey to the west and an outer enclosure extending eastwards below the level of the bailey. It is recorded as being in the hands of the crown in 1195-7, and was restored to Robert de Chandos in 1197. The keep dates from around 1200, and some remodelling of the masonry defences was carried out by the Chandos family in the 14th century. In 1403 it was ordered to be held against Owain Glendwr. The manor and castle of Snodhill were granted by Elizabeth I to Robert Dudley, Earl of Leicester, who sold the estate to a branch of the Vaughan family. When they sold it to Thomas Prosser of London the castle was ruinous, and Prosser moved into a nearby house known as The Court. The remains of the motte and bailey castle include an earthen motte mound, which is roughly oval in form, and has a maximum diameter of 35m. The motte is steep sided and c.3.5m high, and is defended to the east by a c.20m stretch of dry ditch which is up to 5m wide and 2m deep. A path up the west side of the motte now leads to the ruinous gateway of the shell keep, and was probably the original access to the motte's timber tower. East of the ditch the ground drops away steeply before levelling out into a roughly triangular area defined by artifical steepening of the hillslope, a feature which is most clearly visible around the north east and south east quarters. The enclosure thus defined would have been further defended by a timber palisade around the top of the scarp slopes
The sub-rectangular bailey was formed by terracing the natural hillside to the west of the motte, and measures roughly 25m east-west by 18m transversely. Below this terrace the bailey is surrounded to south, west and north by a second level terrace, which has a maximum width of c.10m on the western side. A slight causeway is visible leading from this terrace up to the bailey terrace in the south west quarter, which may represent the original access to the castle. Below the outer terrace the already steep slope has been artificially scarped to the north where it drops away through a wooded area to the road beyond. Roughly one third of the way down this slope, on the north side of the eastern enclosure, is a series of rectilinear fishponds aligned east-west and terraced into the hillslope. The three ponds are contained by an earthen bank up to 1.5m high. They measure roughly 25m x 8m, 30m x 10m, and 35m x 10m, the smallest being the most easterly. The fishponds are separated by earthen banks forming dams which will originally have housed sluices. These dams are roughly 10m and 15m wide, and survive up to 1m high. The western end of the largest fishpond is formed by a substantial earthen bank up to 3m high, with an opening at the north west corner of the pond which was probably an outlet channel running past the west end of the east-west retaining bank. The density of vegetation in the pond makes the exact relationship of these features unclear, however it is likely that this outlet also housed a sluice, evidence for which will survive buried within the earthen banks. The cracked surface in the bottom of the ponds suggest they are still seasonally wet and were probably spring-fed. As well as providing a food supply for the occupants of the castle, these fishponds would have been a further indication of the high status of its owner. Downslope of the fishponds the hillside is crossed by a number of roughly level trackways, which will have provided access to the ponds and perhaps to the castle itself. The most easily visible of these appears as a terrace running east-west for some 200m, passing immediately downslope of the retaining bank of the fishponds and continuing down to the modern road. At the foot of the slope to the west of the bailey, outside the intermediate terrace, is a platform with scarped sides, with the earthwork remains of at least two structures built into its western end, near the modern access to the castle from the road. The scarp which defines this platform can be seen continuing south east through the adjacent pasture field, eventually becoming indistinguishable from the steep natural slope around the southern side of the castle hill. The standing remains of the shell keep are Listed Grade II-star, and include the ruins of an irregular ten-sided keep of stone rubble construction. Its external plan was an irregular ten-sided polygon, with a gateway in the west side flanked by two circular towers. A stone curtain wall followed the line of the bailey and ran up the motte to join the keep at its north west and south west corners. On the southern side the south west circular tower remains standing to a height of c.3.5m. The tower retains the jambs of the outer and inner doorways, a portcullis groove and the corner of a pointed archway above, and a slot for the drawbar of the inner door. A low stretch of wall connects the tower to another tall section of masonry which has a small square headed window at basement level. A later buttress survives in this angle, while round to the north and north east only low portions of wall survive to show the outline of the keep. Contemporary with the keep is the bailey wall which replaced the original timber defences. The southern stretch of this wall survives at a low level to the south. The eastern end was demolished in the 14th century and a new wall erected with a circular bastion at the south east angle, where the wall runs down the side of the motte. This later stretch survives almost to its full height and is ashlar faced. Parts of two square headed recesses can be seen inside the remains of the bastion. The western and northern stretches of bailey wall are represented, for the most part, by a bank within which the masonry foundations will survive. At the north angle of the west section a block of masonry with dressed quoins survives, while at the north west angle of the northern section, part of a 14th century bastion stands to a height of c.3.5m. Some 2m inside the bank which marks the northern bailey wall is a second roughly parallel bank, which may represent its original line, or one side of a building within the bailey itself. Evidence for further structures within the bailey will survive as buried features. At the foot of the causeway up the west side of the motte is a depression c.5m across with a bank on its north and north west sides, which may represent the foundations of a guardhouse defending the gateway above. Snodhill Castle is one of a concentration of medieval defensive monuments at the head of the Golden Valley, and forms part of a chain of similar examples strategically placed above the River Dore. Its nearest neighbour is the motte and bailey castle at Dorstone 1.5km to the north west, with Urishay Castle some 3km to the south. (Scheduling Report)
There is a castell a mile and more benethe Dorston apon the right ripe of Dour. It is called Snothill, and ther is a parke wallyd, and a castle in it on an hill caulled Sowthill, and therby in undar the castle a quarrey of marble. The castle is somewhat in ruine. Ther is a Fre Chappell. This castle longyd to Chandos. (Leland)
This site is a scheduled monument protected by law
This is a Grade 2* listed building protected by law
Historic England Scheduled Monument Number
Historic England Listed Building number(s)
Images Of England
Historic England (PastScape) Defra or Monument number(s)
County Historic Environment Record
| OS Map Grid Reference | SO322403 |
| Latitude | 52.0575485229492 |
| Longitude | -2.99025988578796 |
| Eastings | 332200 |
| Northings | 240370 |
