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The photo above shows a section of the River Hull’s floodplain between the River’s west bank and a section of the Beverley and Barmston Drain to the west of the River in the middle distance, this photo taken in November 2016 with geese (possibly migrating) appreciating the standing water. Across the winter of 2016-2017 I […]

The River Ancholme is a canalised river flowing north from Bishopbridge, on the road between Gainsborough and Market Rasen, north-east of Lincoln. The River exits into the Humber Estuary and is fed by a number of headwater streams south of the Market Rasen road. For the whole of its length the River Ancholme has been

Today’s blog is taking stock – of the 24 blogs under this heading 10 were about the chalk rock country (20/7/’21 to 11/8/’21) and 14 about Holderness (14/9/’21 to 18/10/’21). Referencing back to my chart reproduced on 11/08/’21 (which, incidentally, shows the most common type of village on Holderness to be a ‘composite village’, my

I will make this the last blog on the Holderness section of the above title and I admit to drifting off theme somewhat, although the inter-connection between geology and many aspects of landscape history remains. The above photo. shows part of Barrow Blow Wells just north of Barrow on Humber village in North Lincolnshire, this

Most of the historic villages of Holderness took the form of linear settlements, i.e. building plots straddling a road or lane, or villages around a simple grid-plan, i.e. building plots alongside a routeway with the entrances to the land at the rear of the plot becoming a lane itself. Ottringham is an example of the

Hedon is/was the one town of Holderness (Withernsea and Hornsea were certainly villages up until the coming of their railways, now long gone, they remain as small towns with their secondary schools each having a considerable proportion of students from the surrounding rural area). Hedon, like Barton, was a medieval new town created by Lords