Site of 13th Century fortified house known as Tarset Castle.
Location: NY 7883 8549
The remains of the castle are situated upon a steep-sided promontory which points westwards and which commands the valley of the Tarset Burn to the north, and the valley of the River North Tyne to the west, south and east. The promontory is cut off from the rising ground to the east by a broad deep ditch, 22m wide, and of an average depth of 5m. The southern end of this ditch has been destroyed by the construction of a railway cutting.
Upon the east side of the site, are foundations of a building, of which the south end and north east corner are exposed, and stand to a maximum height of 1.5m. The rest of the site has been subjected to ravaging for stone and is covered with pits and spoil heaps, now turf covered.
Scheduled Monument: 1015528
Keys to the Past: N6995
Tarset Archive Group - Tarset Castle Exhibition
Tarset Archive Group - Tarset Castle Heritage at Risk
Gatehouse record: 2832
Carlton, R. J. (2004). Tarset and Greenhaugh, Northumberland; An Archaeological and Historical Study of Two Border Communities.
The Archaeological Practice, Newcastle upon Tyne.
Geograph (snippet): 25590
"The apparent problem posed by the apparently conflicting records is easily resolved if it is assumed that the earlier record refers to an earth and timber ‘ringwork’ castle probably constructed by Richard Comyn when the family first acquired the manor in the 12th century.
Ringworks, which simply comprise a massively ditched and embanked enclosure, are more common in North Tynedale and Redesdale than the better known type of motte-and-bailey castles, with both the Mote Hill at Wark and Warden Castle adopting this form. Even the earthwork castle at Elsdon - traditionally thought of as a motte-and-bailey - has been re-evaluated more recently and shown to be a ringwork and bailey."
R. Carlton (2004).
Contour models from lidar
Below that are two profiles created by the profile tool in QGIS in directions N-S and W-E across the castle mound and surrounding structures. The nearby farm buildings, disused railway cutting, viaduct, and roads remind us that modern changes to the landscape are often superimposed on what has gone before. The major landslip on the N slope, which rises 17m on the left bank of the Tarset Burn, is clearly visible in the lidar. It took place around 1862-1895 and remains unstable, placing the remains of Tarset Castle at further risk.










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