Whitby Rock |
Richard Bell's Wild West Yorkshire nature diary, Wednesday, 16th May, 2007, North Yorkshire |

THE
PROFILE of Kettleness Nab, the headland at Sandsend,
two miles west of Whitby,
has been nibbled into by quarrying activity. The Jurassic
shales of the cliff top were processed, by a complicated process
that involved baking
and
soaking,
to make alum, an essential ingredient in dying textiles and
leatherworking. In the mid-nineteenth century the alum industry moved to the
coalfields when a more efficient
process of producing the salts was developed.
In the 1880s, long after the collapse
of the local alum industry, a railway was constructed along the cliff top
with the intention of transporting iron
ore to Teeside but the scheme never flourished and the line closed
in 1958.
In
Cornish and Dartmoor granites the large fleshy-looking feldspar crystals are
often rectangular, dotted around in the matrix of smaller rock
crystals like a scattering of matchboxes seen edge-on. In Rapakivi
granite – which
is found in parts of Scandinavia – the feldspars have been remelted during
the process of crystallisation, giving them rounded edges, like half-melted
ice cubes. The tables at Trencher's Fish and Chip restaurant
in Whitby are made of
slabs of this granite.
Dinosaur
Delta
There are layers of nodular ironstone in buff sandstone 100 yards
west of the beach huts at Westcliff. The Jurassic sandstones around
Whitby date from about 180 million years ago. They were laid down in a river
delta at a time when dinosaurs such as Megalosaurus, Cetiosaurus and Camptosaurus
roamed on land.