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Derivation of the word 
The word mere is recorded in Old English, corresponding to Old Saxon meri, Old Low Franconian *meri (Dutch meer), Old High German mari / meri (German Meer), Goth. mari-, marei, Old Norse marr (Swedish mar-, French mare). They derive from reconstituted Proto-Germanic *mari, itself from Indo-European *mori, the same root as marsh and moor. The Indo-European root gave also birth to similar words in the other European languages : Latin mare 'sea' (Italian mare, French mer), Old Celtic *mori 'sea' (Gaulish mori-, more, Irish muir, Welsh môr, Breton mor), Old Slavic morje. The word has been also loaned to Finno-Ugric languages as Finnish and Estonian meri, meaning sea.
The word once included the sea or an arm of the sea, in its range of meaning but this marine usage is now obsolete (OED). It is a poetical or dialect word meaning a sheet of standing water, a lake or a pond (OED). The OED's fourth definition betrays a confusion[original research?] between mere and wetland such as fen in the minds of users of the word which is reflected in the lexicographers' recording of it[original research?]. In a quotation from the year 598, mere is contrasted against moss (bog) and field against fen. The OED quotation from 1609 does not say what a mere is, except that it looks black. In 1629 mere and marsh were becoming confused. But in 1876 mere was 'heard, at times, applied to ground permanently under water': in other words, a very shallow lake[original research?]. The online edition of the OED's quoted examples relate to:
- the sea: Old English to 1530: 7 quotations
- standing water: Old English to 1998: 22 quotations
- arm of the sea: 1573 to 1676: 4 quotations
- marsh or fen: 1609 to 1995: 7 quotations
From this it is clear[original research?] that the balance of the way the word has been interpreted has changed with time but that the 'lake' view of it is the predominant and persistent one[original research?].
A good indication of what people of the past thought the word meant can be found in place-names[original research?]. Though care must be taken[original research?] to avoid confusion with words derived from the same root as the Latin murus (wall) which generally include the concept of 'boundary'. Also, the Anglo-Saxon ‘mŏr’, from which the modern 'moor' derives, also refers to low-lying wetlands (such as Sedgemoor, SW England) of which people are no longer generally conscious because[original research?] they were almost all drained long ago. It is only in place names such as Morton that they are preserved. Conceivably, the Cheshire meres take their name from ‘mŏr’, In the traditional Lancashire, this is unlikely since[original research?] the nomenclature in that part of the country tends to be Scandinavian rather than Anglo-Saxon so that the lowland moors were called mosses. In early medieval England, its neighbour Cheshire was more of a cultural borderland[original research?]. However, the mere, Bar Mere is a neighbour of Willey Moor, both well below 500 feet altitude. The Mercian Angles who settled there appear to have recognized the difference[original research?]. It is also near Bickley Moss, so it appears that the Scandinavians who followed them also found lowland moor[original research?] but the mere remains a lake.
However 'meres' are found in the south western part of England and were called meres meaning lake despite that the lakes dried up there just before the Roman period, suggesting a possibly Germanic language that developed into old English was spoken in the area. Moors and Meres mean different things and settlers knew this. Also names are hard to change once established especially geographical features, so in Lancashire a change from an Old English name to a Viking one would be difficult considering original names usually stick as is the case for most placenames and names of rivers, streams, mountains etc.
The name Windermere makes it clear[original research?] that the narrow meaning adopted by this article has not invariably been taken. Windermere is a lake as much as sixty metres deep in a glacially over-deepened valley. In summer there is a distinct thermocline (M&W). On Wimbledon Common in London, there are two meres, Rushmere and Kingsmere which almost certainly result from gravel extraction by hand as deeply as the ground water permitted[original research?]. Kingsmere is beside the A3 road, the king's road from London to Portsmouth. They are quite uniformly shallow. In the same place however, Queensmere is dammed in a small valley so that it is a little deeper and narrower. The pre-drainage Martin Mere, in its shallow depression in the sheets of glacial deposits and the ‘flashes’ of Cheshire, caused by subsidence when underground rock salt deposits have been dissolved away are meres but the archetypal mere is that of fenland which possibly explains[original research?] the confusion between it and fen. The mere in which Grendel and his mother lived seems clearly to have been of this sort. The Beowulf story, in which we read of them, was probably written in the seventh or eighth century (C-H p. 29 though this date is far from secure). OED (Supplement) quotes use of the word mere in translations of the Beowulf story from 1849 onwards.
The populations from the English Danelaw who settled in Normandy around the 10th Century used the Old Norse marr 'sea' combined with the Old English mere to mean 'stagnant water' or 'pond', that became mare. They dug out such ponds in every property especially in The Caux region and the Roumois region. That is the reason why the place-names ending with -mare in these regions resemble so much those ending with -mere in England . A part of them are composed of the owner's name (mainly Scandinavian or Anglo-Saxon), for instance : Alvimare 'Alwin's pond'; Colmare 'koli's pond'; Vicquemare 'Vigi's pond'; etc. or adjectives (Romance or Anglo-Norse) like Brémare 'large pond' or Houllemare 'hollow pond'.
Where land similar to that of Martin Mere, gently undulating glacial till, becomes flooded and develops fen and bog, the remnants of the original mere remain until the whole is filled with peat. This can be delayed where the mere is fed by lime-rich water from chalk or limestone upland and a significant proportion of the outflow from the mere takes the form of evaporation. In these circumstances, the lime (typically calcium carbonate) is deposited on the peaty bed and inhibits plant growth therefore peat formation. A typical feature of these meres is that they are alongside a river rather than having the river flowing through them. In this way, the mere is replenished by seepage from the bed of the lime-rich river, through the river's natural levée, or by winter floods. The water of the mere is then static through the summer, when the concentration of the calcium carbonate rises until it is precipitated on the bed of the mere.
Even quite shallow lake water can develop a thermocline in the short term but where there is a moderately windy climate, the circulation caused by wind drift is sufficient to break this up. (The surface is blown down-wind in a seiche and a return current passes either near the bottom or just above the thermocline if that is present at a sufficient depth.) This means that the bed of the shallow mere is aerated and bottom-feeding fish and wildfowl can survive, providing a livelihood for people around. Expressed more technically, the mere consists entirely of the epilimnion. This is quite unlike Windermere where in summer, there is a sharp thermocline at a depth of 9 to 15 metres, well above the maximum depth of 60 metres or so. (M&W p36)
At first sight, the defining feature of a mere is its breadth in relation to its shallow depth. This means that it has a large surface in proportion to the volume of water it contains. However, there is a limiting depth beyond which a lake does not behave as a mere since the sun does not warm the deeper water and the wind does not mix it. Here, a thermocline develops but where the limiting dimensions lie is influenced by the sunniness and windiness of the site and the murkiness of the water. This last usually depends on how eutrophic (rich in plant nutrients) the water is. Nonetheless, in general, with the enlargement of the extent of a mere, the depth has to become proportionately less if it is to behave as a mere.
English meres 
- Aqualate Mere, Staffordshire
- Horsey Mere, Norfolk
- Scoulton Mere, Norfolk
- Diss Mere, Norfolk
- Buttermere, Cumbria (Lake District)
- Grasmere, Cumbria (Lake District)
- Thirlmere, Cumbria (Lake District)
- Windermere, Cumbria (Lake District)
- Many examples in Cheshire, including:
- Comber Mere
- Tatton Mere
- Rostherne Mere
- Pick Mere
- Alsager Mere
- Budworth Mere
- Oak Mere
- Hatch Mere
- Shakerley Mere
- Redes Mere
- Radnor Mere
- Many examples in north Shropshire, especially around the town of Ellesmere
The Fens of eastern England, as well as fen, lowland moor (bog) and other habitats included a number of meres. As at Martin Mere in Lancashire, when the fens were being drained to convert the land to pasture and arable agriculture, the meres went too but some are easily traced owing to the characteristic soil. For the reasons given above, it is rich in both calcium carbonate and humus. On the ground, its paleness stands out against the surrounding black, humic soils and on the soil map, the former meres show as patches of the Willingham soil association, code number 372 (Soil Map).
Apart from those drained in the medieval period, they are shown in Saxton's map of the counties (as they were in his time) of Cambridgeshire and Huntingdonshire. The following is a list of known meres of the eastern English Fenland with their grid references.
Saxton's meres are named as:
- Trundle Mere TL2091
- Whittlesey Mere TL2291
- Stretham Mere TL5272
- Soham Mere. TL5773
- Ug Mere TL2487
- Ramsey Mere TL3189
In Jonas Moor's 'map of the Great Levell of the Fenns' of 1720, though Trundle Mere is not named, the above are all but one, included with the addition of:
- Benwick Mere TL3489
In the interval, Stretham Mere had gone and the main features of the modern drainage pattern had appeared.
Ugg, Ramsey and Benwick meres do not show in the soil map. Others which do but which appear to have been drained before Saxton's mapping in 1576, are at:
The last appears to be the "mare 'Wide' vocatum" of Robert of Swaffham's version of the Hereward story (Chapter XXVI). If it is, it will have been in existence in the 1070s, when the events of the story took place.
Meres in the Netherlands 
Meres similar to those of the English Fens but more numerous and extensive, used to exist in the Netherlands, particularly in Holland. See Haarlemmermeer, for example. However, the Dutch word meer is used more generally than the English 'mere'. It means 'lake'. When the Zuider Zee was enclosed and its salt water became fresh, it changed its status from a sea (zee) to being known as the IJsselmeer, the lake into which the River IJssel flows.
- English Etymology, T. F. Hoad, Oxford University Press
- Das Herkunftswörterbuch, Duden Band 7, Dudenverlag.
- Oliver Rackham/The History of the Countryside/Dent 1986/ISBN 978-1-8421-2440-6
- Oxford English Dictionary (OED)
- Ordnance Survey 1:50 000 Sheets 142 & 143
- Macan, T.T. and Worthington, E.B. Life in Lakes and Rivers Fontana (1972) (M&W)
- Crossley-Holland, K. The Poetry of Legend: Classics of the Medieval World Beowulf (1987) ISBN 0-85115-456-5 (C-H)
- Soils of England and Wales, Sheet 4 Eastern England Soil Survey of England and Wales (1983) (Soil Map)
- Saxton, C. Christopher Saxton's 16th Century Maps. The counties of England & Wales. With Introduction by William Ravenhill (Cambridgeshire map dated 1576 book 1992) ISBN 1-85310-354-3
- Moor, J. A Map of the Great Levell of the Fenns Extending into ye Countyes of Norfolk, Suffolke, Northampton, Lincoln, Cambridge, Huntingdon and the Isle of Ely facsimile edition by Cambridgeshire Library Service (c1980s)
- Swaffham, R. Gesta Herwardi (ca. 1260) (transcribed by S. H. Miller and translated by W. D. Sweeting (1895-7))
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