<< Our Photo Pages >> Fridaythorpe Earthworks - Misc. Earthwork in England in Yorkshire (East)
Submitted by SumDoood on Monday, 01 May 2017 Page Views: 3401
Multi-periodSite Name: Fridaythorpe Earthworks Alternative Name: Holm Dale, Horse Dale, Harper DaleCountry: England
NOTE: This site is 1.915 km away from the location you searched for.
County: Yorkshire (East) Type: Misc. Earthwork
Nearest Village: Fridaythorpe
Map Ref: SE88425753
Latitude: 54.006232N Longitude: 0.652387W
Condition:
5 | Perfect |
4 | Almost Perfect |
3 | Reasonable but with some damage |
2 | Ruined but still recognisable as an ancient site |
1 | Pretty much destroyed, possibly visible as crop marks |
0 | No data. |
-1 | Completely destroyed |
5 | Superb |
4 | Good |
3 | Ordinary |
2 | Not Good |
1 | Awful |
0 | No data. |
5 | Can be driven to, probably with disabled access |
4 | Short walk on a footpath |
3 | Requiring a bit more of a walk |
2 | A long walk |
1 | In the middle of nowhere, a nightmare to find |
0 | No data. |
5 | co-ordinates taken by GPS or official recorded co-ordinates |
4 | co-ordinates scaled from a detailed map |
3 | co-ordinates scaled from a bad map |
2 | co-ordinates of the nearest village |
1 | co-ordinates of the nearest town |
0 | no data |
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Misc. Earthwork in Yorkshire (East)
I'd come here on 22 April 2017 to find "Earthworks" which I'd seen on the Ordnance Survey's 1:50000 and 1:25000 maps. I'd read elsewhere that they were Bronze Age (though I was wondering if they were medieval).
This is Holm Dale, south of Fridaythorpe. Down at the end there is Harper Dale to the left and Horse Dale to the right. These dry valleys of the Yorkshire Wolds were created at the end of the last Ice Age, c.18,000 years ago, when the action of fast-running streams flowing over frozen ground carved out these valleys. The chalk geology here allows water to drain so efficiently that the valleys run dry.
I am open to alternative suggestions, but have *assumed* that the purpose of the "Earthworks" (essentially ditches - photos to follow - generally along the upper edges of the valleys), was to prevent / reduce topsoil run-off from the fields (nowadays prairie-style agro-industrial intensively farmed flat areas), either side of each of the valleys and also to maintain grazing on the steep deforested sides of the valleys.
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