As seen in the previous blogs/posts the traditional man-made structure to reduce flooding in lowland areas across the Humberside Region was the linear clay bank, shaped to improve its effectiveness (s.p.b.s). Sections of the Humber Lowlands are still protected by clay banks including the south coast of Holderness, the Lincolnshire Marsh, apart from the sand […]

The Lincolnshire Marsh (s.p.b.s) has a history of flooding across many centuries. Here is a selection of recorded events’ 1176 ‘sea burst forth – engulfing men and herds’, this extract from the Louth Abbey Archives. 1253 ‘Great flood from the sea’. This storm surge wiped out a string of low-lying coastal islands, now the foundation

Today’s photo shows the point alongside Sluice Road, South Ferriby that was the site of a small medieval port near the mouth of the then River Ancholme which had meandered sluggishly north from Brigg. A now shallow causeway links the site to the spring line village seen beyond the bungalows to the foot of the

The sketch above dated 1805 shows Waterside House and stables in the parish of Barton on Humber alongside the mouth of Barton Haven flowing into the Humber. The two sailing boats are sailing to/from two jetties, one serving the Barton to Hessle ferry, the other the Barton to Hull ferry. A vague image of the

The Meaux Abbey Chronicle further records that in the 1340s Burstall Priory suffered the ‘ruin of much of their property by inundation’. Burstall Priory was an ‘alien cell’ (monastic site belonging to a foreign order) in the parish of Skeffling between Patrington and Kilnsea. Despite the above it was still mentioned in the documents covering

The above photo was taken on 7th December, 2013, two days after the great flood resulting from the combination of a spring tide and coastal surge happening at the same time in the Humber Estuary. The view is looking west from a point east of the working clay tile works east of Barton’s coastal nature