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SHARPENHOE,
BEDS.
When
the coprolite was first discovered in this area is uncertain but the diggings
had spread southwestwards from the Shillington area
through Higham Gobion in the 1870s. There were records of workings in
Barton-le-Clay at that time but it was the geological account of the area in
the early 1880‘s that revealed there had been workings in this parish.
”When
followed eastwards the upper gault is found to
diminish in thickness so that the basement nodule bed is gradually brought
nearer to the chalk. A nodule bed surmounted by light grey marly
clay was seen in a shallow excavation by the roadside northwest of Grange Mill
near Sharpenhoe. The same bed outcrops on the surface
Northwest of Great Faldo Farm and has been found by trial borings about 18 feet
below the the surface of the ground near Brook End
and not far from the outcrop at the base of the Chalk Marl, which bed was
formerly worked for coprolites in this place. "
(Pennings and Jukes-Brown, Cretaceous
Rocks of Great Britain,‘Mem.Geol.Surv.1881,p286)
Unfortunately
there was no indication as to who was responsible for the operation, whether a
local landowner had allowed the tenant to have then raised
or whether a contractor was allowed to work them. The subsequent mapping of the
local geology by A.C. Cameron located the extent of the workings running
northwest to southeast about half a mile to the northeast of the village. (1” gelogical map 46NE 1886; I.O‘Dell,
‘A Vanished Industry,• Beds Mag.1951)