Untitled - Council for British Archaeology
Untitled - Council for British Archaeology
Untitled - Council for British Archaeology
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28<br />
that there was some continuity of site into<br />
the Saxon period until later nucleation onto<br />
the present village sites. In addition<br />
several small middle Saxon sites have been<br />
discovered, but none large enough to justify<br />
the title of 'village', excepting the Newton<br />
Willows site discussed previously in Newsletter<br />
4 (1974).<br />
The iron slag and charcoal patches first<br />
studied some years ago in the Easton Maudit<br />
area, were the subject of much speculation as<br />
to date. A carbon 14 test suggested C12th.<br />
The more extensive surveys undertaker since<br />
show that these slag and charcoal areas occur<br />
only in the vicinity of the known area of<br />
medieval woodland, i.e. near Rockingham,<br />
Salcey, and Whittlewood <strong>for</strong>ests.<br />
Nearly all the parishes were completely<br />
ploughed in medieval times except <strong>for</strong><br />
flooding meadows. Only Pilton has a small<br />
area, Bearshank wood, representing part of<br />
the Rockingham Forest. Almost all the<br />
parishes show characteristic shrunken earth7<br />
works.<br />
Astwell and Falcutt A late Neolithic<br />
domestic site was found on a pocket of grayel<br />
at the NE of Astwell, and there are two R.B.<br />
sites with the usual scatter Of domestic<br />
rubbish. Both settlements are d.m.vs.<br />
reduced to 'a mansion house and farmstead.<br />
They appear to be late C15th sheep desertions.<br />
Falcutt earthworks are well-preserved but<br />
those of Astwell are unusual - perhaps<br />
destroyed by C16th gardens of which there is<br />
some evidence.<br />
At the F side of Astwell parish are 13<br />
black charcoal areas representing the<br />
clearance of medieVal. woodland (Whittlewood<br />
Forest). At Old Mountains is an extraordinary<br />
moated site with linear ramparts<br />
running <strong>for</strong> over -1- mile away from it. The.<br />
main site is well-preserved and covered by .<br />
trees but the ramparts are now mostly demar-.<br />
cated by soil marks. The moat is marked as ,a<br />
wooded copse on a late Cl6th map at Merton<br />
College Ox<strong>for</strong>d. This map also marks the pale<br />
of the park created by the Lovett.family; the<br />
boundary is still represented by modern hedge<br />
lines without banks. Perhaps the Old<br />
Mountains ramparts, b'elong to an earlier<br />
medieval deer emparkment, although they do<br />
not enclose an obvious park-like area.<br />
Blisworth This parish is much mutilated by<br />
quarrying and parts are suffering from deep.<br />
plough damage. Two R.B. sites were noted,<br />
one on a restored hand-dug quarry. Some good<br />
examples of ridge and furrow survive at the N<br />
and SW of the parish.<br />
The village is noted <strong>for</strong> the course of a<br />
very early horse drawn railway linking the<br />
two ends of the Grand Union Canal which is<br />
still clear from cuttings and embankments.<br />
In 1812 the railway'was replaced by a tunnel,<br />
the earth being disposed at intervals through<br />
vertical shafts and left in great heaps which<br />
remain on the fields above.<br />
Church Brampton Like adjacent Chapel Brompton<br />
the light soils of this parish abound in<br />
prehistoric sites. Four complexes have been<br />
identified, some with cropmarks yielding<br />
Beaker period flints.<br />
The S part of the parish was described as<br />
heathland in the C16th, but nevertheless<br />
contains ridge and furrow, surviving on a<br />
golf course. To the W is a long tongue of<br />
land, alongside a brook which was presumably<br />
originally meadow, but now contains a series<br />
of very short lands or butts.<br />
Crick An early I.A. site was found on clay<br />
and 2 R.B. sites on a ridge of gravel, one<br />
partly destroyed,by the Ml. An A.S. burial<br />
was uncovered during road works <strong>for</strong> an M1<br />
feeder carriage way.<br />
The parish is mostly grass with Some very<br />
exceptional ridge. and furrow surviving to a<br />
height of 3'. Many furlongs have 'double- -<br />
headed' headlands which were caused by<br />
leaving the headland to grass over and turning<br />
the plough around d short distance away.<br />
There are good village earthworks and sunken<br />
roads E of the church; also well-preserved<br />
are the fishponds and a windmill mound. Some<br />
of the small quarries- (mostly <strong>for</strong> gravel) are<br />
quite early because ridge and furrow originally<br />
disturbed was reploughed into them. -<br />
There is a canal tunnel (1812), which, like<br />
Blisworth, is marked by a line of spoil heaps<br />
on the fields above it. One of these heaps<br />
appearS to have ridge and furrow crudely<br />
.ploughed onto it, even though the parish was<br />
inclosed in 1775.<br />
Doddington There are 3 previously known R.B.<br />
sites and an I.A. enclosure here. The latter<br />
produced a limestone loom weight and also some<br />
R.B. sherds. A new site was found to the NI<br />
of.the village which yielded a few R.B. and<br />
some hand-made Saxon sherds. The'red-land<br />
contained a few worked flints of late date.<br />
There are good village earthworks and