Bradford-on-Avon
site maintenance 25/11/17
A fine, if cold,
morning was spent removing leaves and clay, washed-down from the sides of the
pit, to uncover a ‘hard-ground’ limestone seafloor in the Forest Marble
Formation. The latter is made up of
alternating limestones and clays. The
surface is very uneven and, because it was solid, a diverse assemblage of
bottom-dwelling sea creatures lived there until they were entombed by an
influx of clay (The Bradford Clay). An
earthquake may have triggered slumping of a nearby clay deposit, resulting in
a turbidity current which, as the mud settled, buried the fauna in situ
165 million years ago - see diagram below (d) & (e).
Twelve people came
along to help, from the Bath Geological Society and the WGG, which was great
– any more and the pit would have been too crowded!
Thanks to everyone and
in particular to Sam Medworth, who sieved some of the clay at home and sent
these brilliant photos of a selection of fossils: brachiopods, sponges,
echinoid spines, fish vertebrae and a sea-lily stem ossicle he found!
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Talks, field trips and events organised by west country geological organisations are publicised on this blog. Discussion about geological topics is encouraged. Anything of general geological interest is included.
Friday, 8 December 2017
Wiltshire Geology Group in the field
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