Battle of Byland: building up the evidence

A fascinating story here…

The official blog for the North York Moors National Park

Graham Lee – Senior Archaeological Conservation Officer

Sutton Bank areaThis story of mounting evidence starts in 1996 when a survey was commissioned of the east end of a boundary earthwork known as the Casten Dyke North, to the east of the Hambleton Inn at the top of Sutton Bank. Long thought to be prehistoric, probably Iron Age, in date, the Casten Dyke North runs from the escarpment edge above Sutton Bank (north east) into the head of Flassen Gill, a classic cross-ridge type boundary well known for dividing up areas of prehistoric landscape.

The survey results show that the line of the dyke at the eastern end appears to be marked by two shallow ditches and a relatively gentle north-facing break of slope, cut by numerous later hollow-ways. However, running into the steep sides of Flassen Gill itself, is recorded a much more prominent ditch c.4m wide and about 1m…

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