Skipsea Meres
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The Skipsea meres were three lakes in and around the village of
Skipsea Skipsea is a village and civil parishes in England, civil parish on the North Sea coast of the East Riding of Yorkshire, England. It is situated approximately south of Bridlington and north of Hornsea on the B1242 road at its junction with the ...
in the
East Riding of Yorkshire The East Riding of Yorkshire, often abbreviated to the East Riding or East Yorkshire, is a Ceremonial counties of England, ceremonial county in the Yorkshire and the Humber region of England. It borders North Yorkshire to the north and west, S ...
, England. The meres that are known to have existed were ''Skipsea Bail Mere'', ''Skipsea Low Mere'' and ''Skipsea Withow Mere''. The name of the village, Skipsea, means lake, or harbour for ships. At least two of the meres were natural, filling with water in a post-glacial landscape, whilst the third, Skipsea Mere, was possibly created as part of the defences for the castle. All the water from the meres has either drained away naturally, or been removed by human intervention, most notably for agricultural purposes.


History

The three meres at Skipsea have existed since the
Holocene The Holocene () is the current geologic time scale, geological epoch, beginning approximately 11,700 years ago. It follows the Last Glacial Period, which concluded with the Holocene glacial retreat. The Holocene and the preceding Pleistocene to ...
period, when the glacial activity created the meres, sometimes in the form of kettle holes. Dried out post-glacial meres are common in
Holderness Holderness is an area of the East Riding of Yorkshire, on the north-east coast of England. An area of rich agricultural land, Holderness was marshland until it was drained in the Middle Ages. Topographically, Holderness has more in common wit ...
, with the low-lying land not able to adequately drain the water away, though most of the water did eventually flow through the Hull Valley and into the
Humber The Humber is a large tidal estuary on the east coast of Northern England. It is formed at Trent Falls, Faxfleet, by the confluence of the tidal rivers River Ouse, Yorkshire, Ouse and River Trent, Trent. From there to the North Sea, it forms ...
. In the post-glacial period, Holderness would have resembled the Norfolk Broads, with many areas having standing water. This is reflected in some of the place names: Marfleet, Marton, Redmere and Rowmere. Many of these meres disappeared due to human intervention through drainage schemes to provide land for agriculture and grazing. Withow Mere was the furthest east of the three, and the site is now suffering from
coastal erosion Coastal erosion is the loss or displacement of land, or the long-term removal of sediment and rocks along the coastline due to the action of Wind wave, waves, Ocean current, currents, tides, wind-driven water, waterborne ice, or other impacts ...
. Bail Mere separated the castle and the Church of All Saints, and Low Mere was further out towards the north-west of the village. Evidence from the various archaeological surveys have determined that Withow Mere was at some point possibly connected to Bail and Low Meres via a narrow channel feeding into Withow Gap, the stream that was at the western edge of Withow Mere. However, evidence of a ridge between Withow Mere and Skipsea itself, may have proved to be a block against the meres being joined. There is some conjecture that boats could sail through the meres from the sea, right up the edge of the village and to the castle. The name of the village itself, Skipsea, is either
Old English Old English ( or , or ), or Anglo-Saxon, is the earliest recorded form of the English language, spoken in England and southern and eastern Scotland in the Early Middle Ages. It developed from the languages brought to Great Britain by Anglo-S ...
(''Scip-sæ'') or
Old Norse Old Norse, also referred to as Old Nordic or Old Scandinavian, was a stage of development of North Germanic languages, North Germanic dialects before their final divergence into separate Nordic languages. Old Norse was spoken by inhabitants ...
(''Skip-siōr'') meaning the ''lake for ships, harbour for ships''. All of the meres show the same strata laid down over thousands of years: lacustrine clays, Skipsea Till (silt), peat, and a topsoil most likely due to run-off earth from deforestation. During
Medieval In the history of Europe, the Middle Ages or medieval period lasted approximately from the 5th to the late 15th centuries, similarly to the post-classical period of World history (field), global history. It began with the fall of the West ...
times, the various meres in Skipsea (and throughout Holderness), were an important source of food for those living around them. The eels in Skipsea Mere were recorded in the 14th century as being worthwhile to fish and sell them on, and as late as 1790, even when many of the 50 or so meres in Holderness had been drained, it was still possible to take many ducks for food.


Skipsea Bail Mere

Located at , the Skipsea Bail Mere (also known as the ''Mere of Skipsea'' or ''Skipsea Mere''), afforded
Skipsea Castle Skipsea Castle was a Norman motte and bailey castle near the village of Skipsea, East Riding of Yorkshire, England. Built around 1086 by Drogo de la Beuvrière, apparently on the remains of an Iron Age mound, it was designed to secure the ne ...
a defensive protection and was also on the western and northern side of the Church of All Saints in the village. The castle itself is in Skipsea Brough, a hamlet to the west of Skipsea, and part of the defences for the castle were known as bail, which gave the mere its name. A dam was built to the north west of the castle to trap water, with the castle sitting some above the mere, which some have stated was tidal. Other historiographies have stated that the mere was created entirely as a defence for the castle and as such, was man-made. The castle area was connected to the Church of All Saints by a causeway across the mere. A timber bridge over the mere also connected the keep with the bail gate, which was due south of the castle itself. Archaeological investigations have located the remains of the timber harbour used by the castle to transfer goods from ships. Studies conducted on the pollen from Bail Mere have determined that the temperature in the immediate post-glacial age was about 2°C warmer than at present. Due to the mere's potential for further study, it has been designated as an
SSSI A Site of Special Scientific Interest (SSSI) in Great Britain, or an Area of Special Scientific Interest (ASSI) in the Isle of Man and Northern Ireland, is a conservation designation denoting a protected area in the United Kingdom and Isle ...
. The Bail Mere was sometimes referred to as Skipsea Mere, and was also known to be the fishery for the castle. Most of the catch of eels and fish was recorded as having been sold on to the local area. The mere was drained in the early 18th century, () and the land reclaimed for agriculture.


Skipsea Low Mere

Located at . This mere may have been connected to Bail Mere through a channel providing drainage to the sea towards the north, then the east. This channel follows the line of what is now the Barmston and Skipsea drain. The Low Mere was the furthest away from Skipsea itself, and was about above sea level before it was drained.


Skipsea Withow Mere

Located at , the name of this mere dates back to the 13th century, when the name ''Whythow'' was recorded. The name means ''marsh near the white hill''. However, it has also been recorded as ''Fwitthouker'', ''Fitbouker'', and ''White Hole Carr''. The site of Skipsea Withow Mere is actively being eroded by the wave action of tides from the
North Sea The North Sea lies between Great Britain, Denmark, Norway, Germany, the Netherlands, Belgium, and France. A sea on the European continental shelf, it connects to the Atlantic Ocean through the English Channel in the south and the Norwegian Se ...
. Bones recovered from the eastern edge of Skipsea Withow Mere, have been determined to be of red deer (
cervus elaphus The red deer (''Cervus elaphus'') is one of the largest deer species. A male red deer is called a stag or Hart (deer), hart, and a female is called a doe or hind. The red deer inhabits most of Europe, the Caucasus Mountains region, Anatolia, Ir ...
) from the Mesolithic era. The archaeological survey of the area considered the bones were not there due to natural death, but more likely cast into the mere after human predation. Studies of the
stratigraphy Stratigraphy is a branch of geology concerned with the study of rock layers (strata) and layering (stratification). It is primarily used in the study of sedimentary and layered volcanic rocks. Stratigraphy has three related subfields: lithost ...
at the site of the mere indicated that it was – deep in the Late-Devensian period, and stretched to over in a north/south alignment at its widest point. Withow Mere was to the south east of Skipsea itself and was separated from the Bail Mere by a ridge south of the village. The outflow from the mere, known as Withow Hole, was some east of the present day coastline (now the North Sea) and the mere itself occupied a stretch of land that has been lost to coastal erosion since 1750.


Notes


References


Sources

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External links


Urban rim website about Withow MereMapping from 1910 showing causeway between vicarage and the keep (bottom left), and top left the place marked 'Lake Dwelling', is the site of Skipsea Low Mere
{{Lakes in Yorkshire Holderness Sites of Special Scientific Interest in the East Riding of Yorkshire Protected areas of the East Riding of Yorkshire Lakes of the East Riding of Yorkshire