LANGTOFT
2
TF
126134
The
moat already described (Langtoft 1), is the surviving fragment of one which
surrounded the Hall itself. This one, situated some 250 metres further north
(Fig 72), seems unlikely to be connected with the main complex. At present it
holds a small plantation. It is situated on the Car Dyke amost abutting on the
southern side of the east-west boundary between the parishes of Langtoft and
Baston. Its eastern ditch coincides with the projected line of the Car Dyke
which was perhaps deliberately utilised. The location of this moat and its
unusual elongated form seem to preclude habitative use by man, yet it is likely
that it surrounded a manorial appurtenance of some kind. An estate map of 1890
appears to confirm this, for the field immediately to the south-west is called
Coneygree Piece (1). The size and form of the moated area is not inconsistent
with the recorded sizes of some rabbit warrens (2). It is however, much larger
than those recently published from Bryn Cysergfan (3). The use of a ditch,
either wet or dry, around an artificial warren is also known (4). There is
additional archaeological interest in the area because of the presence in the
immediate vicinity, not yet precisely located, of an early Anglo-Saxon burial
ground, but there is no evidence to suggest that this earthwork had its origins
at such an early date.
Both the moated sites lie at the
eastern end of the village at a common level of six metres OD, the same as that
of the surrounding fields. Langtoft 2 is of more or less rectangular shape,
enclosing an area 110 metres long (north/south alignment) by 35 metres
east/west (Fig 91). The dry ditches were in good condition when visited,
averaging 1.7 metres deep and varying from eight to fifteen metres wide. There
is no evidence that the enclosed platform was ever any higher than at present.
1. LAO, Ancaster 5/B/1/6/1.
2.
J. Sheail, Rabbits and their History, Newton Abbot, 1971, 40.
3. D.Austin, 1988 Excavations and Survey at
Bryn Cysergfan, Llanfair Clydogau, Dyfed, 1979, Med Archaeol 32, 130-165.