HINDWELL VALLEY STONES
Approx. 2500 - 800 BC
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Burfa
Burfa Stone Grid ref SO 2754 6135 The destroyed remains of a possible standing stone. Identified and photographed by M Feryok in 1997. Bronze Age SMR ref 4226

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Kinnerton
Kinnerton Court Stone I Grid ref SO 245 627
A weathered standing stone about 1.2m high and 1m by 0.9m at the base. The stone sits in a circular depression 0.5m deep and 3m diameter. The stone can be seen from the Kinnerton-knapp lane in the field opposite Stone II, see below. Bronze Age SMR ref 1070
Kinnerton Stone I

Kinnerton Court Stone II Grid ref SO 244 628
A moss-covered standing stone 0.9m high by 0.7m at the base. The stone can be found in a ditch on a sharp bend in the Kinnerton-Knapp lane just below Kinnerton. Bronze Age SMR ref 1069
Kinnerton Stone II

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Four Stones
Four Stones Grid ref SO 245 608
.Four stones set in a circle with their flat surfaces facing the middle. The whole site measures 4m by 3m and the stones vary between 1.2-1.9m high. The SW stone has three probable cupmarks carved into it. There is a gap between 2 of the stones, suggesting that there may originally have been a fifth boulder. Folklore suggests that the font in the nearby Old Radnor Church may once have filled this gap Bronze Age, SMR ref 1072

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Hindwell
Hindwell Stone Grid ref SO 249 609
A possible recumbent stone measuring 1.6m by 1.1m by 0.9m high. Visible in the second field on the left in the lane leading from the Four Stones to Hindwell farm. Bronze Age SMR ref 1073

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Knobley
Knobley Stone Grid ref SO 263 613
A standing stone 1.2m high, 1.6m long by 1.3m wide at the base. The stone is in a field a short distance from the modern B4357 to the N of Hindwell Farm, It is beleived to be Bronze Age SMR ref 306

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Court Farm
Court Farm Boulder Grid ref SO 256 623 WEATHERED BOULDER. 0.8M BY 0.7M BY 0.2M. DEPRESSION ON UPWARD SURFACE (0.02M BY0.02M BY 0.01M DEEP) MAY POSS BE CUP MARK. Date unknown, thought to be Bronze Age. I went looking for it (feb 2004) but found no trace anywhere near the GR. GR may be incorrect or stone may have been moved.

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