(OS 1: 10000 a SP 56 SE, b SP 66 SW, c SP 65 NW)
The parish, of some 560 hectares, lies W. of Watling Street
which forms much of the E. boundary, though a small area
extends across the Roman road as far as an S.-flowing
stream. Most of the parish lies astride the valley of an
E.-flowing brook which, together with a number of small
tributaries, has cut deeply into the underlying Middle Lias
clays and silts between 120 m. and 80 m. above OD. To
the N. and S. of the stream the land rises to more than
130 m. above OD and there are extensive spreads of glacial
clays, sands and gravels. A small S. projection of the parish
extends across a ridge into the valley of the R. Nene.
The major monument of the parish was the settlement
remains (1). These have been almost entirely destroyed, and
thus the main contribution to the understanding of the
complex history of the village's structure has been lost.
Prehistoric and Roman
Several Roman coins, some of Constantine and one of
Tetricus, have been found in the parish, mostly along
Watling Street which forms part of the E. boundary
(Morton, Nat. Hist. of Northants. (1712), 532; J. Bridges,
Hist. of Northants., I (1791), 50).
For Roman Road 1f, Watling Street, see Appendix.
Medieval and Later
A 14th-century coin, identified as a Burgundian
imitation of an English quarter-noble of the type struck in
Flanders for Philip the Bold was found in 1955 in the N. of
the village (SP 61356085; BM; Brit. Num. J., 28 (1955),
b(1) Settlement remains (centred SP 615606; Figs. 12,
59 and 60), formerly part of Dodford, lay in and around
the existing village on the sides of a small E.-flowing
stream and its tributaries, on glacial sands and gravels and
Jurassic Clay between 90 m. and 120 m. above OD. Most
of the earthworks have been ploughed out in recent years
and the accompanying plan has been compiled, in great
part, from air photographs taken before destruction.
The remains suggest either a large-scale depopulation at
some time or, more likely, a considerable movement of the
village over the centuries. However the surviving
documents do not give any clue as to which of these
alternatives is correct. Dodford is first mentioned in an
Anglo-Saxon charter of 944 (BCS 792). It is recorded in
Domesday Book as a manor of three hides belonging to the
Count of Mortain, with a recorded population of 22
including a priest (VCH Northants., I (1902), 326).
Thereafter no certain indication of its size is ascertainable
until 1673 when 39 people paid the Hearth Tax (PRO,
E179/254/41). By the early 18th century there were 21
houses in the village (J. Bridges, Hist. of Northants., I (1791),
50). In 1801 two hundred and five people lived in the
parish. A map of 1742 (NRO; Fig. 60) shows the village
exactly as it is today with the settlement remains already
The surviving earthworks, together with those which
have been destroyed, fall into four distinct groups. To the
S. of the stream and E. of the main through street ('a' on
plan) was a series of long rectangular paddocks bounded by
shallow ditches. These have all been destroyed but stone-rubble and pottery, mainly of the 13th and 14th centuries,
has been found at the W. and N. ends of some of them
indicating that they were once tofts and crofts of the
village. In 1742 many of these were still hedged closes.
To the N. of the stream ('b' on plan) and now also
destroyed were some unusual rectangular tofts and crofts
extending up the hillside. These too have scatters of stone
and medieval pottery at their S. ends and must be the
remains of former houses and gardens. The extremely
regular plan of the earthworks implies an element of
Fig. 59 Dodford (1) Settlement remains, (2) Deer park
Immediately N. of the church are other slight
earthworks which may be former closes ('c' on plan)
though little remains on the ground. Only to the W. of the
church and the N. of the manor house do earthworks
survive ('d' on plan). Here a shallow hollow-way, which
perhaps once extended S. to the present main
Northampton-Daventry road, runs N. down the valley
side to meet the E.–W. village street. Slight banks on either
side may be former closes (RAF VAP CPE/UK/1994, 1269–70).
b(2) Deer park (centred SP 613603; Figs. 59 and 60), lies
immediately S. of the village, between it and the A45 road
on glacial sands and gravels, between 100 m. and 120 m.
above OD. Its exact extent is not known.
Bridges (Hist. of Northants., I (1791), 50) records that
'there was formerly a park including 30 acres of wood ...
but the ground hath long since been applied to other uses'.
It was apparently enclosed by William de Keynes who
acquired the manor of Dodford in 1222. By the 14th
century it was said to be 50 acres in extent (Cal. IPM xii,
49–50). The location of the park is partly shown on the
map of Dodford of 1742 (NRO); the latter gives the name
Park to the large pasture field S. of the manor house.
However as this field is relatively small the park must have
extended further W. than the present field. The S. side of
the park is formed by a precipitous slope with a small bank
below it immediately N. of the main A45 road. Along the
E. side of the park a low bank or scarp runs along the W.
side of the road to Dodford village. No other convincing
boundaries survive, though a very low bank extends W.,
N. of and roughly parallel to the A45 (SP 61056026) for
some 200 m. The park may have occupied the land N. of
this bank as far as the marshy area N.W. of the village. In
the bottom of the valley, near the N.E. corner of the park
(SP 61376032), is a rectangular pond embanked on its S.E.
and N.E. sides (Northants. P. and P., 5 (1975), 221).
Fig. 60 Dodford (1, 2) Village and deer park in 1742 (from a map in NRO)
(3) Cultivation remains. The common fields of
Dodford were enclosed by private agreement in 1623
(NRO, Grant (Li) H5), though the earliest map of the
parish is of 1742 (NRO). Ridge-and-furrow of these fields
survives on the ground or can be traced on air photographs
immediately N., E. and S. of the village. The furlongs to
the S. are mainly orientated N.–S. as the land falls S. to the
R. Nene but elsewhere they interlock, in response to the
more broken terrain (RAF VAP CPE/UK/1994, 1166–8,