A Neolithic Site at Craike Hill, Garton Slack, East Riding of Yorkshire

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Abstract
Craike or Crayke Hill stands on the southern slope of Garton Slack, in the north-western corner of the parish of Kirkburn, three miles west of Great Driffield (Nat. Grid. ref. SE 972576) (fig. 1). Garton Slack is a wide dry valley penetrating the central chalk Wolds of the East Riding of Yorkshire between Wetwang and Driffield. Scattered over the flat floor of the Slack are the much-ploughed remains of Mortimer's Garton Slack Group of round barrows. Once Craike Hill, which is a natural hill of fine chalk similar to the rest of the Slack floor, was a prominent landmark, but gravel digging since 1938 has reduced it to a crater. Originally it stood about 50 ft. above the floor of the Slack and was composed of beds of fine chalk gravel interspersed with sandy layers towards the base. The beds show a dip towards the north. Over the top of the hill was a fine sandy brown soil containing chalk, flint, and greenstone pebbles. Much of this remains as overburden dumped on the lower slopes.

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