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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 undertaken 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 earthworks.<br />

Astwell and Falcutt A late Neolithic<br />

domestic site was found on a pocket of gravel<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 earthwork's 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 E 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 + mile away from it. The.<br />

main site is well-preserved and covered by<br />

trees but the ramparts are Jmw 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.helong 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 />

1)140 44p, 5Q la ;iitQ5 nro ptvil<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 'doubleheaded'<br />

headlands which were caused by<br />

leaving .the headland to grass over and turning<br />

the plough around a 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 />

the fields above it. 'One of these heaps on<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 NW<br />

of.the village which yielded a few R.B. and<br />

some hand-made Saxon sherds,<br />

The red-land<br />

contained a few worked flints of late date.

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