Hull Geological Society
Mike Horne FGS
This is unfinished work that has not been edited or peer reviewed by the Society.
A thin Chalk layer at Gransmoor Quarry
by Mike Horne
During a visit to Gransmoor Quarry ( grid
reference TA113597 )
noticed a layer of chalk rubble towards the top of the
peat bed.
The peaty beds at Gransmoor formed in a kettle
hole, due to the melting of a large block of trapped ice, on the top of an
esker. This was one of the many meres that were formed about the glacial
deposits of Holderness, which have all filled up, with the exception of Hornsea
Mere. The deposits at Gransmoor provide a record which spans the last 15,000
years (Ellis 1993).
Fossil fish bones of Perch and Pike have been
found in the beds as well as a harpoon point. Fish scales and pieces of wood are
common in the deposits. In total there are just over 2 metres of the mere
deposits,which overly glacial sands and gravels. The beds of peat and clay form
a continuous sequence from the Late Devensian Lateglacial interstadial through
the Loch Lomond (Younger Dryas) Stadial. A full description of the deposits,
with dating of the pollen and coleoptera, will be published in the …Quaternary
Science Review„ by M Walker,
G Coope and J Lowe.
The layer of Chalk was about 3 cm thick and the
chalk was very
On examining the sample after washing and
sieving it, I found a well preserved microfauna which included the following :
References :
Ellis S [ed.] 1993. …Wetland Heritage. Humber
Wetalands Project, School of Geography and Earth
Resources, University
of Hull. 181pp.
Walker MJC, Coope CR & Lowe JJ, (in press) 1994. The
Late Devensian
(Late Weichselian) palaeoenvironmental record from
Gransmoor, East Yorkshire, England. …Quaeternay
Science Review.
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