PALAEONTOLOGY
Three or four hundred years ago caves were regarded with superstition
and fear and it wasn't until the 19th Century that systemmatic cave exploration
for fossil remains began. The first cave to be examined for fossils in
Britain was a limestone fissure at Oreston near Plymouth.

Dean William Buckland, 1784 - 1856
William Buckland pioneered scientific cave exploration in Britain.
He recognised that caves were formed as a result of natural processes
and that there are several types of bone deposits in caves; water-lain
deposits, talus cones, and the deposits of inhabited caves.
His views on the origins of these deposits in caves were condemned
by many as being " inconsistent with the Scriptures".
The conventional view was that the bones had been drifted into
the caves by the waters of the Biblical Deluge, which had carries
the carcases of the tropical animals northwards.
Despite his many new theories on the origins of bone deposits
in caves, Buckland never accepted the evidence that proved that
man had co-existed with the extinct mammals. Man was regarded
as a very recent creation (4004 B.C. was quoted as the most likely
year) and therefore any evidence that showed that man had existed
in geological time must be incorrect.
In 1825 Buckland visited Pixies Hole, Chudleigh; Kents Cavern,
Torquay; Ash Hole, Brixham; Ansteys Cove Cave, Torbryan; and
the Oreston Caves near Plymouth. |
 |
William Pengelly, F.R.S. 1812 - 1894
William Pengelly was the genius behind some of the earliest systemmatic
cave research in England. He spent most of his life in Devon and his
major research projects took place in Devonshire caves.
Pengelly's most significant work took place in Kent's Cavern at Torquay
from 1865. Over a period of sixteen years, Pengelly accumulated a mass
of evidence on the animal and men of prehistoric Devon.
His work established beyond all doubt that man had existed during the
Pleistocene Period (1 million years ago) and caused the whole of the
scientific world to awake to the fact of the vast antiquity of the human
race.
Pengelly's cave work was of special value by the virtue of the facts
and methods he used and the conclusions he reached. He showed that caves,
especially newly discovered caves, could reveal more valuable information
by systematic investigation than by just poking around in the deposits.
His excavations involved the entire deposits to be removed from the cave
and to do it layer by layer so that evidence from different deposits
could not be muddled. He also kept the strictest check on the position
of every object found.
After the Kent's Cavern excavations Pengelly continued to investigate
other Devonshire caves and he wrote a number of scientific papers.
Links List:
James Lyon Widger, 1823 - 1892
James Lyon Widger was born in Broadhempston near Totnes and during his
childhood explored many of the caves in that district, discovering many
bones and artifacts.
The memory of his boyhood adventures in the Torbryan caves was never
far from Widger's thoughts and in 1865 he proceeded to carry out excavations.
By William Pengelly's standards he was inexperienced, ignorant of geology
and excavations and completely unknown to scientific circles. He always
chose to work alone, desiring no companionship, no advice nor any assistance
in his work. Despite the fact that Torbryan was only ten miles away from
Kent's Cavern, William Pengelly had no knowledge of the cave excavations
being carried out by Widger until 1870. Widger is known to have met Pengelly,
but the two workers had little in common and there was no co-operation
between them.
Although unrecognised at the time, the importance of Widger's work at
Torbryan was the remarkable sequence of deposits he exposed. They include
an inter-glacial layer sandwiched between two cold layers and the excavations
revealed the most complete sequence of deposits ever to be found in a
British cave.
Widger's discovery of a hyaena den has been referred to as one of the
most remarkable of British examples.
Bone and Tooth Remains from Joint Mitnor Cave
River Dart Scene

A composite diorama showing a scene from the River Dart as it must have
appeared during the last inter-glacial period a hundred thousand years
ago.
|