Untitled - Council for British Archaeology
Untitled - Council for British Archaeology
Untitled - Council for British Archaeology
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D.H.,Kennètt;. 'The Ang107Saxon 'cemetery found at<br />
Kempston,- Bed<strong>for</strong>dshire:, a reconsideration'i,typescript,.<br />
1968,'availabla <strong>British</strong> Museum, Department of Medieval<br />
and Later Antiquitiea-.<br />
Kettering: Proc. Soc. Ant. 19 (1903), 307-310; Ant. J., 10 (1930)<br />
254.<br />
THE NORTHAMPTONSHIRE SURVEY<br />
David Hall and Paul Martin<br />
The season.of 1978-9 was fraught with weather unsuitable <strong>for</strong> fieldwork.<br />
A dry autumn caused a iate startand.there-Was much loss of time<br />
because of froat.and snow. There<strong>for</strong>e the equivalent of only 7 parishes<br />
was Surveyed.; Ashby-St..'Ledgers,.GeAdington,.Grafton Undarwood, Warkton,<br />
Weekley, Welton and parts of Little Oakley, Stanion and West Haddon. .<br />
Archaeological results were consistertwith previbus conclusions.<br />
The boulderclays of Rockingham Forest were richin'ircin Age and Roman<br />
remains but the north-west parishes were almost devoid of premedieval<br />
settlement. Welton differs from the north-west. trend in having a.known<br />
Saxon'Oemetery and a 'Roman villa (neWlY discOvered)..'Hgre *there was<br />
stone building"material, various kinds of tile and,slate and painted architectural<br />
fragments of tufa. -<br />
°Perhaps the most important.discoveries were the earthwork sites<br />
founapin the' woods, Most of theM likely to be prehistorié.The finest<br />
earOlwork Was found in. Grafton Park Wood. It would seem, to be a typical<br />
Iron Age farmatead in a rOughly,circular'enolosure about50.m diameter,<br />
consisting of a:bank'and.ditch.. The bank, stands about iim. high. Parts of<br />
square endlosures.were found in Geddington Chase and Castor Hanglands -<br />
both medieval. ..Grafton Park als000ntains IronAge earthworks(partly<br />
excavated by D.-Jackson see abre).<br />
-These earthworks ara' similar io the one diseoyered in Salcey Forest<br />
on the boundary of Hartwell parish- (thia Journal 1975).-It is Clear that..<br />
in areas* of Meaieval woodland and parkland, where.there are Many thousands'<br />
of acres never subjected to ploughing'since at least Roman times, there<br />
is great-potential <strong>for</strong> the survival of early earthworks.:<br />
.Thewoods also contained an'abundanca of MedieVal ramparts, especially<br />
the parks. Thus Grafton Park Wood, Boughton Wood and Brigstock Park are<br />
enclosad','but Geddington Chase is not; The old ridings'Of the latter'did<br />
have low ramparts and <strong>for</strong>med wide cUrving tracks quite Unlike the straight<br />
'modern' onesi . Many parts of these woods were shown to be postmedieval<br />
with ridge-and-furrow in them.<br />
'NASEBY PARISH.SURVEY 1976- DaVid'HalI,' Ruth Haraing and Paul Martin<br />
The survey followed the techniques described in previous'Newaletters.<br />
Naseby contains 3324 acres and lies.on one of'the.highest parts of the<br />
,Northamptonshire.Uplands; most of the parish is above-500 feet OD and<br />
about a third is well over 600 feet. Both the Avon and the Nene Tlse here.<br />
The geology consists mainly of bOulder-clay drift-,deposits with areas<br />
of gravel,,especially to the south,. Some Of the highest hills, including<br />
-48-