Back to Bedfordshire publications
THE
COPROLITE INDUSTRY IN AMPTHILL, BEDS.
As early
as 1872 there were a group of local men and children employed in a new type of
extractive industry which few people fully understood. It was the digging of
coprolites or phosphatic nodules which contained an assortment of fossils which
even included dinosaur bones. Many at the time took them, from their shape, to
be fossilized dinosaur droppings and the 1930 “Ampthill News,” which included the
first written article on the subject, showed that there were even more obscure
ideas about it.
“Probably
few people in Ampthill will remember that some 60 or more years ago there was
considerable activity in what the workers called “fossiliting. The work took
place in some of the fields between the station and Fordfield Road and a number
of men were employed under the supervision of the late Mr. Abraham Britten of
Oliver Street, Ampthill who represented a firm of manure manufacturers.
Fossiliting consisted of digging in these fields for fossilised human bones which
were found in quite large quantities. They were sorted out from the stones, washed,
loaded into wagons on a light railway leading to the station, and sent to a
factory to be ground into manure.” (Beds.Mag.20 p.232 )
Human bones
being used to make manure? Pretty morbid stuff and shocking enough to prompt a
reply the following week which was a bit closer to the truth.
“ Fossiliting continued.
Our
thanks are due to Miss S.F.George for the following response to our note last
week. She writes: “The excavations for so called human bones near Fordfield Road
were, no doubt, for fossilised animal droppings known as coprolites. These
contained, in many cases, bones and teeth of extinct animals. When found in
large quantities they were exploited for fertilising purposes, particularly in
Cambridgeshire and Suffolk. The colour of the coprolites was affected by iron in
the soil and they were formed by chemical accretions round animal and vegetable
remains lying in water charged with phosphorous.”
(Ibid.)
They
were not actually the droppings but the phosphatised remains of prehistoric
creatures such as the megalosaurus, dakosaurus, craterosaurus, stegosaurus and
iguanadon. There were also ichthyosaurus, plesiosaurs, pliosaurs and
pterodactyl. Whales, sharks, crocodiles, hippopotami, elephants etc. and an
assortment of marine organisms were also dug up from the Greensand. According
to many geologists, the fossils and phosphatic nodules had been washed out of
the Wealden clays to accumulate in beds in a wide belt across southern
Bedfordshire. They were in great demand by manure manufacturers across the
country as they could be converted into superphosphate, a valuable fertiliser, by
mixing it with sulphuric acid.
The
Ampthill coprolite diggings were started by 1872 as a result of similar excavations
in the Shillington area where they were found in the greensand formation. When
the same deposit was discovered here “the firm of manure manufacturers”
arranged to extract them. Evidence shows that this was John Bennet Lawes, of
Rothamsted, who had patented the technique of converting them into
superphosphate. Such was the success of his business that it was taken over in
1872 by a group of businessmen for £300,000. Part of this enormous fortune he used
to set up the Rothamsted Agricultural Research Station. He and the analytical
chemist, Augustus Voelcker, were the founders of the similar experimental farm on
the Duke of Bedford’s Woburn Farm in 1876. (See author’s account of the
industry in Shillington, Woburn, and Rothamsted)
The
new company’s investigation of the coprolite side of the business revealed that
by 1873 £1,611 13s.3d. had been expended on developing the Ampthill works and
that there were 40 acres yet to be worked. (Valence House Museum, Dagenham, Lawes
Chemical Manure Co. Private Ledger,1873,p.98
According
to the report they were dug around 700 yards southwest of Ampthill Station between
Station Road and Woburn Road/Fordfield Road. This necessitated the cutting down
of some pinewoods. The seam, extending over 200 acres, was found dispersed
through a six foot band of pebbly sand about 15 feet above the base of the sands,
which would have involved specialised washing plant. (Teall, H. (1873),
‘Description of Phosphatic Bed as it occurs at Potton and Wicken,’ p.11;
Bonney, (1875), ‘Cambridgeshire Geology,’ Cambridge, p.23; Oakley, K. (1941),
‘British Phosphates’, Wartime Pamphlets Vol.8 No.3 see fig.3; O’Dell, I.J.
(1951), ‘A Vanished Industry’, Beds.Mag. and his ms. notes in Luton Museum)
The geologist, J. Teall, visited the pits in
the early 1870s hoping to find interesting fossils. His paper on the fossils
being unearthed from the Bedfordshire pits won a Cambridge University Prize in
1875. He revealed that the seam was quite shallow but also of varying
thickness.
“In the neighbourhood of Ampthill several
good sections are exposed; one at the crossroads near Millbrook gave the
following succession:
1.
Red and yellow sands, false-bedded. 8
- 10 ft.
2.
Phosphatic nodule bed, containing a great number of
lydian-stone pebbles. 4 in.
3. Yellow and white sand, intensely fine-bedded,
with
occasional
argillaceous layers. 15 ft. to
bottom of pit.
The junction with the Oxford clay can be seen
a little further down the hill.
In a
field adjoining the section above I was fortunate enough to find some 20 to 30
trial pits which had been sunk for the purpose of testing the value of these
phosphatic deposits. These showed that the bed varied in thickness within very short
distances; in one pit being as much as three feet, and in another, not 40 yards
distant, only a few inches. They also showed that the thickness of the sands
below the bed varied considerably, and that in some cases it rested directly on
the Oxford clay. The nodules consisted, for the most part, of rolled fossils,
exactly as at Potton, and with them were associated pebbles of lydianstone,
quartz, etc.
A section at the coprolite-working about half
a mile west of the Midland station showed six feet of a reddish brown sand, with
concretions, throughout which phosphatic nodules and pebbles were distributed.
The nodules here are separated with the sandy matrix by sifting, and then the
phosphatic nodules are picked out by children.”
(Teall, J. (1875), ‘The Potton and Wicken
Phosphatic Deposits’, Sedgwick Prize Essay of 1873, Camb. Deighton and Bell.
Co.,p.26)
With
200 acres to be worked it must have entailed a large workforce which included
considerable numbers of the local children. These were needed in separating the
fossils from the pebbles. This explained the reports in one of the teacher’s
books of the Secondary School Board that several children were absenting
themselves from classes to work in the coprolite pits. (Author’s communication
with Barbara Howard, Ampthill
The
photograph on page .. shows tumbrils loaded with the washed fossils coasting down
the hill into Millbrook. From here they would have been taken to Millbrook station.
As this Bedford Branch connected easily with the London and Birmingham line
there is a likelihood that the contractors were Morris and Griffin,
Wolverhampton manure manufacturers, who were responsible for hiring Britten.
They had numerous workings to the southwest and into Buckinghamshire where the seam
was similarly exploited. (O’Connor, B. (1990), ‘The Coprolite Industry in
Bucks”, Bucks Record)
How
long the work went on is not known but it was still going in 1881 as the census
revealed that William Disbrey was a “coprolite foreman.” (Beds.C.R.O. 1881
census)
Whether
this was on the same workings as Britten is uncertain but he had been born in
Barton, Cambridgeshire, which was one of the earliest villages dug for fossils
so it’s possible that he had been attracted to the Bedfordshire diggings when it
became apparent there was many years’ work available.
When
the bypass was constructed around Ampthill, in the cutting just above Little
Park Farm, the same seam of fossils was exposed but there was no indication the
workings had extended to this side of the railway.
Back
to Bedfordshire publications