Reasons for Designation
Palaeolithic caves and rock shelters provide some of the earliest evidence of
human activity in the period from about 400,000 to 10,000 years ago. The
sites, all natural topographic features, occur mainly in hard limestone in the
north and west of the country, although examples also exist in the softer
rocks of south-east England. Evidence for human occupation is often located
near the cave entrances, close to the rock walls or on the exterior platforms.
The interiors sometimes served as special areas for disposal and storage or
were places where material naturally accumulated from the outside. Because of
the special conditions of deposition and preservation, organic and other
fragile materials often survive well and in stratigraphic association. Caves
and rock shelters are therefore of major importance for understanding this
period. Due to their comparative rarity, their considerable age and their
longevity as a monument type, all examples with good survival of deposits are
considered to be nationally important.
Details
Aveline's Hole is situated on the east side of Burrington Combe, 88m below
the plateau and c.2m below the present level of the road. It consists of a
passage, c.43m long and averaging 3m wide, divided into two chambers by a
constriction c.27m into the cave. The cave slopes steeply downwards for the
first 20m then rises and levels off before descending into a choked passage
at the back of the cave. The cave entrance was first opened in 1797 when a
number of extended human skeletons were discovered, some encased in tufa,
lying on the cave floor. Later excavations undertaken between 1919-27
uncovered a rich Late Upper Palaeolithic deposit in a 3 foot thick cave
earth under a thin stalagmite floor. The finds included lithic artefacts
and a rare example of a biserial antler harpoon. Unfortunately, many of
these items, formerly in the Bristol Museum, were destroyed by wartime
action. Some of the skeletal material has been radiocarbon dated and found
to be of Mesolithic age. Cut-marked animal bone, radiocarbon dated to about
12,000 years ago, provides an age for the Later Upper Palaeolithic
occupation evidence. Although the cave has been extensively excavated,
original deposits are considered to survive beneath archaeological tip up to
18m into the cave and also outside to a distance of 10m either side
of the entrance and in the 6m wide area between the road and the cave mouth.
All of these deposits and the cave are included in the scheduling.
Legacy
The contents of this record have been generated from a legacy data system.
Legacy System number:
13259
Legacy System:
RSM
Sources
Books and journals
Legal
This monument is scheduled under the Ancient Monuments and Archaeological Areas Act 1979 as amended as it appears to the Secretary of State to be of national importance. This entry is a copy, the original is held by the Department for Culture, Media and Sport.
End of official list entry
