Records of Woodhall Spa and Neighbourhood: Historical, Anecdotal, Physiographical, and Archaeological, with Other MatterWalter, J. Conway (James Conway)
History
Records of Woodhall Spa and Neighbourhood: Historical, Anecdotal, Physiographical, and Archaeological, with Other Matter
Walter, J. Conway (James Conway)
Woodhall Spa (England)
The next lower formation is the Lincolnshire limestone. This enters
largely into the making of what is called “the Cliff,” which is the high
land running south from Lincoln (visible from Woodhall) to the west of
the Witham Valley and the Fens. It is a hard building stone, though once
the muddy bed of a sea. It is sub-divided into the Hibaldstow and Kirton
beds, so called because these strata are exposed in those parishes.
Dipping to the east, it underlies the Fens and other upper strata to be
found in the Woodhall well. It abounds in fossils, there being as many
as 340 species classified, {96a} and consists, indeed, very largely of
the hard parts of shells and corals compressed into a solid mass. To a
Lincolnshire person, it is sufficient to say of this stone that our grand
Cathedral is mainly built of it. We can only give here a few of the more
frequent species of fossils:—Three kinds of Echinus, Coral (Thecosmilia
gregarea), Serpula socialis, Lima (five kinds), Ostræa flabelloides,
Pecten (two kinds), Hinnites abjectus, Astarte elegans, Cardium Buckmani,
Ceromya Bajociana, Cyprina Loweana, Homomya Crassiuscula, Isocardia,
Cordata, Rhynconella (four kinds); among the bivalves are Avicula
Inequivalvis, and A Munsteri, Lima (three kinds), Lucina Bellona, Modiola
Gibbosa, Mytilus Imbricatus, Pholadomya (two kinds), Trigonia costata; of
univalves, Natica (two kinds), Nerinea Cingenda; of fishes, Strophodus
(two kinds). {96b} This is a most useful stone for building purposes.
The so-called “Lincoln stone” is largely used in our churches; whilst the
“Ancaster quarries,” which also belong to this formation, are famous.
The commissioners appointed in 1839 to report on the building stones of
England, for the new houses of Parliament, stated that “many buildings
constructed of material similar to the Oolite of Ancaster, such as Newark
and Grantham churches, have scarcely yielded to the effects of
atmospheric influences.” (“Old Lincolnshire,” vol. i., p. 23.) The
well-known Colly-Weston slates are the lowest stratum of this rock. The
fine old Roman “Newport Arch,” which for some 700 years has “braved the
battle and the breeze,” a pretty good test of its durability, is built of
this stone.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account