Prehistoric cairnfield south west of Water Crag, 290m north west of the confluence of Linbeck Gill and Devoke Water

Reasons for Designation

The Cumbrian uplands comprise large areas of remote mountainous terrain, much of which is largely open fellside. As a result of archaeological surveys between 1980 and 1990 within the Lake District National Park, these fells have become one of the best recorded upland areas in England. On the open fells there is sufficient well preserved and understood evidence over extensive areas for human exploitation of these uplands from the Neolithic to the post- medieval period. On the enclosed land and within forestry the archaeological remains are fragmentary, but they survive sufficiently well to show that human activity extended beyond the confines of the open fells. Bronze Age activity accounts for the most extensive use of the area, and evidence for it includes some of the largest and best preserved field systems and cairn fields in England, as well as settlement sites, numerous burial monuments, stone circles and other ceremonial remains. Taken together, their remains can provide a detailed insight into life in the later prehistoric period. Of additional importance is the well-preserved and often visible relationship between the remains of earlier and later periods, since this provides an understanding of changes in land use through time. Because of their rarity in a national context, excellent state of preservation and inter-connections, most prehistoric monuments on the Lake District fells will be identified as nationally important.

Cairnfields are concentrations of cairns sited in close proximity to one another. They often consist largely of clearance cairns, built with stone cleared from the surrounding landsurface to improve its use for agriculture, and on occasion their distribution pattern can be seen to define field plots. They were constructed from the Neolithic period (from about 3400 BC) although the majority of examples appear to be the result of field clearance which began during the Bronze Age (2000-700 BC). The considerable longevity and variation in the size, content and associations of cairnfields provide important information on the development of land use and agricultural practices. Cairnfields also retain information on the diversity of beliefs and social organisation during the prehistoric period. The prehistoric cairnfield south west of Water Crag, 290m north west of the confluence of Linbeck Gill and Devoke Water survives reasonably well and forms part of a large area of well-preserved prehistoric landscape extending along the fellsides of south west Cumbria. In conjunction with a wide range of other prehistoric remains in the vicinity the monument represents evidence of long term management and exploitation of this area in prehistoric times.

Details

The monument includes a small prehistoric cairnfield located on the south western slopes of Water Crag 340m south west of the summit. It represents Bronze Age exploitation of this landscape and includes a group of five circular and oval-shaped clearance cairns up to 0.5m high. The circular cairns measure between 3.2m to 5.4m in diameter while the oval-shaped cairns measure between 5.6m to 6m long by 3.2m to 4m wide. Pollen cores taken from the sediments of nearby Devoke Water have revealed the changing vegetational history of this area over the last 5000 years and show evidence of forest clearance and a development of grassland during the prehistoric period. During one of these episodes most trees were cut down and were soon replaced by extensive grassland. This clearance is associated with the Bronze Age on the basis of its similarity to a clearance episode from Seathwaite Tarn 9km to the east, which has been scientifically dated to around 1000 BC.

MAP EXTRACT The site of the monument is shown on the attached map extract. It includes a 2 metre boundary around the archaeological features, considered to be essential for the monument's support and preservation.

Legacy

The contents of this record have been generated from a legacy data system.

Legacy System number:

32879

Legacy System:

RSM

Sources

Books and journals
Quartermaine, J, Leech, R H, Upland Settlement of the Lake District: Result of Recent Surveys, (1997), 60-73
Leech, R, Birkby Fell Survey Catalogue, (1982)
Leech, R, Trans Cumb and West Antiq and Arch Soc. New Ser. in Settlement And Groups Of Small Cairns On Birkby And Birker Fells, Vol. LXXXIII, (1983), 15-23

End of official list entry

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