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The above photo shows the linear lowland between the two naturally occuring ranges of vegetated sand dunes, as viewed north with Cleethorpes Leisure Centre in the distance (s.p.b.). The flora in the lowland is non-saline whereas that of the dune ranges is dominated by wind and salt resistant species. The concrete footpath (s.p.b.) is off […]

Today’s illustration is a diagrammatic map of the Lincolnshire Marsh coastline between Cleethoepes and Donna Nook and is scanned from a chapter called ‘The Lonely Lands’ in the booklet by Larry Malkin ‘Wavelength Wanderings Along the Humber Estuary’ (1992). In fact the boundary between the two-tier unitary authority of North-East Lincolnshire and the three-tier county

Today’s photo, taken while standing at the base of the Humber bank and looking south, shows part of the expanse of Goxhill ‘Marsh’. From the top of the clay bank and turning to face north the view couldn’t be more different with Hull’s Humber frontage seeming to be so close, this an example of the

Beyond the end point of the Lincolnshire Marsh (s.p.b.) and beyond the neighbouring post-industrial site (s.p.b.) the ‘Marsh’ widens. The aerial photo shown above was reproduced on the cover of the book named and shows the next post-industrial area. This industry was directly connected to the drift geology of the ‘Marsh’ as the silt was

The Lincolnshire Marsh and Wallingfen will be the last two sections of this extended series of blogs. The term Lincolnshire Marsh refers to the lowland strip that edges the coast of North Lincolnshire, North-East Lincolnshire and the county of Lincolnshire. The photo above was taken roughly half-way between Barton on Humber and South Ferriby and

Having seen where the River Hull starts (s.p.b.) today the photo shows where it ends, this photo taken late in 2016 before the flood alleviation scheme started at Minerva pier/Nelson St. area. This section of Hull’s improved flood defenses is almost complete with the section in front of Minerva Pub now open to the public