Details

The Farway Hill barrows are situated in south east Devon, 8km south of
Honiton, on the high ground of an extensive Greensand plateau where it forms
the watershed of the south-flowing River Sid. The monument includes two ring
cairns and the area of archaeologically sensitive ground between them,
situated on the crest of the north eastern end of the long ridge forming
Farway Hill. They lie on level ground and are 3.5m apart.
The south east ring cairn survives as an earth bank up to 1.2m in height and
2.5m wide with a sloping outer face and a vertical inner face, enclosing an
area of recessed ground 9m in diameter and c.0.5m lower than the surrounding
ground surface. On the south east side a 4m long section of the bank lies 1m-
2m further out than the rest of the bank.
The north west ring cairn survives as an earth bank up to 0.6m in height and
2m wide with a sloping outer face and a vertical inner face, enclosing an area
of recessed ground 6m-7m in diameter and 0.3m lower than the surrounding
ground surface.
An embanked trench 7m long and 2m-4m in width (stepped on its north side)
connects the two ring cairns.
The ring cairns were discovered in 1965 when the heath was ploughed by the
Forestry Commission for tree planting. A rescue excavation was undertaken to
record the cairns which included an investigation of their interiors, sampling
of their enclosing banks, and the excavation of a trench between them. They
were subsequently landscaped into their present form with banks being heaped
over the two exposed rings of stone and along the edge of the excavation. The
area of the excavation is visible as recessed ground within the two cairns and
the embanked trench between them.
As excavated, the south east ring cairn was composed of an irregular ring of
flinty stones 1m-2.5m wide and 13.5m-15m in external diameter, enclosing a
central open area of 9.5m-11m diameter. The central area contained a number of
small pits, with some intercut and extending beneath and beyond the bank of
the cairn. Forty of the pits contained charcoal in their fills. One cremation
consisting of poorly preserved bone mixed with charcoal and fragments of heat
shattered flint, was located in a small pit towards the western side of the
cairn. Two other pits may have contained cremations.
As excavated, the north west ring cairn was composed of an irregular ring of
flinty stones 1m-2m wide and 9m-10m in external diameter, enclosing a central
open area of 6m-7m diameter. The western side of the ring contained a number
of slabs of flint which may have originally composed a cist (stone lined
burial chamber). The open area contained a number of small pits, with some
extending beneath and beyond the bank of the cairn. None of the pits contained
charcoal.
The area of ground between the cairns is archaeologically sensitive in that
it has been demonstrated by excavation to contain features relating to the
construction and use of the cairns.
A small assemblage of worked flint containing some tools was recovered from
the cairns.

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.

Source: Historic England

Reasons for Scheduling

Round barrow cemeteries date to the Bronze Age (c.2000-700 BC). They comprise
closely-spaced groups of up to 30 round barrows - rubble or earthen mounds
covering single or multiple burials. Most cemeteries developed over a
considerable period of time, often many centuries, and in some cases acted as
a focus for burials as late as the early medieval period. They exhibit
considerable diversity of burial rite, plan and form, frequently including
several different types of round barrow, occasionally associated with earlier
long barrows. Where large scale investigation has been undertaken around them,
contemporary or later "flat" burials between the barrow mounds have often been
revealed. Round barrow cemeteries occur across most of lowland Britain, with a
marked concentration in Wessex. In some cases, they are clustered around other
important contemporary monuments such as henges. Often occupying prominent
locations, they are a major historic element in the modern landscape, whilst
their diversity and their longevity as a monument type provide important
information on the variety of beliefs and social organisation amongst early
prehistoric communities. They are particularly representative of their period
and a substantial proportion of surviving or partly-surviving examples are
considered worthy of protection.

The Farway Hill barrows, a number of which form a barrow cemetery, comprise
the central area of one of the most extensive and densest concentrations of
barrows in Devon. Limited archaeological excavations of some of the barrows
have revealed that they have a remarkable diversity in size and form, and in
the nature of their funerary contents.
Although partly excavated, the two ring cairns remain reasonably well
preserved examples of this class of monument. Their banks remain largely
intact and will preserve underlying features. The ring cairns lie on the far
northern edge of the Farway Hill barrow group and are the only ring cairns
identified in that group.

Source: Historic England

Sources

Books and journals
Grinsell, L V, 'Proceedings of the Devon Archaeological Society' in The Barrows of South and East Devon, , Vol. 41, (1983), 5-46
Pollard, S, 'Proceedings of the Devon Archaeological Society' in Seven Prehistoric Sites, Near Honiton, Devon. Pt 2., , Vol. 29, (1971), 162-180

Source: Historic England