I am in the middle of spending a happy couple of weeks back out in the Yorkshire Dales in the vicinity of Ingleborough. We are doing another landscape survey in advance of a programme of peatland restoration works. The survey involves looking at peat erosion scars and any drainage gullies for exposed artefacts such as flint flake scatters. I haven’t managed to get to the summit of Ingleborough so far this year but I should do, weather permitting, by the end of the project.
As I have previously mentioned I am quite partial to limestone scenery and the patterns of erosion and the forces of nature that have shaped it greatly over time. The gorge at Trow Gill is a fine example and is located sandwiched between Ingleborough Cave and the Gaping Gill pot hole. It is particularly scenic at the southern mouth where you follow the footpath up into its narrow confines.
The shake hole pocked area is a contrast between elevated sparse grassland with swathes of blanket peat and lower scarp slopes with exposed limestone pavement fringes. It is on these lower slopes where the greatest concentration of archaeological sites are to be found.
Today I was quite taken with the colour differentiations between the grassland, eroded areas of peat, standing water and sphagnum mosses.