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The lakes of the Lake District are creations of nature; beautiful and inspiring. The National Park is home to the deepest lake. It is also home to the four largest lakes in England and Wales.<ref>Smith (2012) p.3.</ref> Set against a backdrop of Lakeland mountains, known locally as fells, one can easily conjure up thoughts of bygone authors and poets who so loved their craft; forever sealing a picturesque impression of a romanticised setting in one of the wettest parts of the UK. |
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It is a misconception that the Lake District has "lakes." It is much more than that. If you go by name alone it has only one lake, [[Bassenthwaite Lake]]. Semantics aside, the Lake District ''does'' has more than one lake. In fact it has multiple lakes of different sizes in the form of [[mere]]s, [[water]]s and [[tarn]]s, dotted throughout this rugged, yet beautiful landscape. These words are synonymous with the bodies of water that were born is this wide open land, either by glacial withdrawal or by human intervention. |
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Water is abundant here; reason alone for its green hues in summer and long, grey winters. There are hundreds of bodies of water in the Lake District, ranging in size from the largest lakes to the smallest pools, many more than most people would ever care to visit. The popular destinations are what brings the masses here to break away from everyday routine. From hardcore hikers and cyclists to the casual, fair-weather day trippers, visitors to the area who explore this great outdoors, do so because its appeal draws them in, time and time again. The lakes are just one, albeit predominantly so, reason for this influx of people every year. |
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Thanks to the {{w2|Last Glacial Period|last glacial period}} of 10,000 years ago, the retreating ice left us with glacially erodes valleys that formed the lake district we see today. Not only the ice but people too are responsible for changing the landscape. [[Haweswater]] and [[Thirlmere]] are reservoirs, although the former was once a natural lake. It was dammed to raise the water level in a bid to supply fresh water for the people of Manchester, at a price that flooded two cumbrian villages, now lost to the murky darkness. The once ebb and flow of ice and, in much more recent times, people, continue to have an effect on the natural backdrop of the second oldest<ref group="lower-alpha">The Lake District National Park was formed on 9 May, 1951, second after that of the Peak District, which was formed on 17 April, 1951.</ref> national park in England. |
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By name alone, the Lake district has only one ''[[Origin of the word "lake"|lake]]'' of the 17 main lakes throughout the National Park – [[Bassenthwaite Lake]], which is nestled in the northern region of the park's periphery. There is a general misconception that [[Windermere]], the largest of the lakes, is prefixed with the word ''Lake'' to differentiate it from the small town of the same name. ''Lake Windermere'' or ''Windermere Lake'' are not official titles, but are used extensively as a means of identifying the lake instead of the town. This grammatical construct ({{w2|Tautology (language)|tautology}}) typifies the redundancy of the word ''lake'', which is not needed due to ''mere'' already being present. Also, ''Windermere Town'' just sounds a little odd, with ''town'' being superfluous. |
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The larger of the lakes usually carry the suffix of [[mere]] or [[water]], whilst the humble [[tarn]] is usually reserved for the smaller bodies of water. However, there are some tarns larger than lakes, just confuse matters.<ref>[https://www.lakedistrict.gov.uk/learning/factsandfigures Lake District Fact and Figures] The Lake District National Park Authority. Accessed 15 January, 2023.</ref> An example of this is evident in [[Blea Water]] (a tarn) being slightly lager than [[Elter Water]], which is the smallest of the lakes. Each body of water, large and small, encompassed by neighbouring fells, woodland and moors, bestow a natural beauty individual in character. One of the best ways to experience this is on foot. |
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Although the Lake District has only one body of water with ''lake'' in the title, the remaining 16 of the big lakes are named with ''[[Origin of the word "mere"|mere]]'' or ''[[Origin of the word "water"|water]]''. These words are synonymous with the lakes born in this wide open land, either by glacial withdrawal or by human intervention. |
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==Where do the names come from?== |
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===Mere=== |
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'''Mere''': Pool, small lake, pond. From Old English ''mere'' meaning "sea, ocean; lake, pool, pond, cistern," from Proto-Germanic ''mari''. Also from: |
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*Old Norse: ''marr'' |
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*Old Saxon: ''meri'' → "sea" |
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*Middle Dutch: → ''maer'' / Dutch: ''meer'' → "lake, sea, pool" |
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*Old High German: ''mari'' / German: ''meer'' → "sea" |
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*Gothic: ''marei'' → "sea," ''mari-saiws'' → "lake" |
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The source of these come from the Proto-Indo-European root word ''mori'', meaning "[[Bodies of water|body of water]]." The larger sense of "sea, or arm of the sea" has been obsolete since Middle English.<ref>{{oed|title1=mere|title2=Mere|day=22|month=January|year=2022}}</ref> Mere in this instance refers to the names [[Buttermere]], [[Grasmere]], [[Windermere]], [[Kentmere]], which are recorded from the late 12th or 13th century. The term "water" is used more often for the larger of the lakes.<ref>{{whaley|411}}</ref> |
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== |
==Etymology== |
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Before we move on, it is interesting to learn from where these words are derived. Lake District place names take a lot of influence from {{w1|Old Norse}} as well as {{w1|Old English}}. Some words follow a natural progression through time, others do not and can change dramatically with entirely different meanings. Words can also be cognate with, and influenced by, other languages. A simple appreciation of these can provide a broader understanding of the words we use today. |
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*'''Water''': |
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The three words lake, mere, and water all come from a Proto-Germanic background, however, ''lake'' is a little more complicated as it is a merger of two different words from French and English. The French lineage ascends back to Proto-Italic, which spawned the Romance languages (Italian, French, Spanish etc.) What is interesting, all three of these words ultimately refer to a "body of water" of some sort, with subtle variations depending on size and usage. Cognates are also strikingly similar as to be expected, which show how these words developed and changed through time to mean something similar to, or even the same as, their ancestor equivalent. |
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Rather than discuss this in length here, it is best if these are broken down into more detail separately. |
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*[[Origin of the word "lake"]] |
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*[[Origin of the word "mere"]] |
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*[[Origin of the word "water"]] |
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Words prefixed with a * are [[Wiktionary:Reconstructed terms|reconstructed words]]. This means they have not been directly attested, but instead are hypothesised to have existed based on comparative evidence. |
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==Glacial origins== |
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The term "ice age" can be somewhat ambiguous. The earth is in an ice age called the Quaternary glaciation, which began around 2.58 million years ago and has had many periods of glacial advance and retreat. We are still in this ice age, as suggested by the ice caps present at the poles. However, we are currently experiencing an interglacial or warmer period. In the UK this period is called the {{w1|Flandrian interglacial}}.<ref group="lower-alpha">The {{w1|Flandrian interglacial}} period started at the end of the Devensian glaciation (also known as the {{w2|Last Glacial Period|last glacial period}}) which was at its maximum approximately 22,000 years ago. This cold period had come to end around 11,700 years ago after which the earth saw a period of warming, the period that we are currently in.</ref> This led to retreating ice that left us with glacially "plucked" and eroded valleys that formed the lake district we see today. |
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===Plucking and abrasion=== |
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[[File:Arranque glaciar-en.svg|thumb|300px|Graphic showing the process of plucking and abrasion (Image:Wikimedia Commons)]] |
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The whole process of ice excavation can be described in fairly simple terms, when in reality, it involves a complex set of stages working together. Essentially, the movement of glaciers' grinds and pulls apart the bedrock on which it sits. Dr Alan Smith's book, ''The Big Lakes of Lakeland'', describes this process clearly, without over complicating an already complex set of processes. With nowhere else to go except to follow the flow of ice, the broken pieces of rock were then transported as the ice moved along the valleys, in the case of the Lake District, radially in an outward direction from a central core. This core was so thick that maybe only the tips of the highest peaks of [[Scafell]], [[Helvellyn]], [[Bowfell]], and [[Great Gable]] were visible.<ref name="smith12">Smith (2012) p.12</ref> The Last Glacial Maximum was approximately 22,000 years ago and up to that point in time, the ice had been steadily increasing until it reached its maximum, hence the name. All the big lakes were excavated by the ice during this Last Glacial Maximum, a segment of the Last Glacial Period, which encompassed a timeframe between 115,000 - 11,700 years ago. By 13,550 years ago, the ice sheets had retreated and the "valley glaciers had melted away and a new landscape of ice scoured fells and lakes left impounded in the valley floors was revealed."<ref name="smith12"/> |
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So, what is plucking? Plucking is a process that removes large fragments of rock under immense pressures and moves them to other locations, sometimes lengthy distances from their original position. This is similar to quarrying, except instead of explosives and heavy machinery, ice does all the hard work. For plucking to be most effective, '''Fracturing''' needs to take place. This is a separate process that weakens the bedrock along naturally occurring joints and fractures, prior to being broken up.<ref name="smith13">Smith (2012) p.13</ref> As Dr Smith explains, these weaknesses in the rocks may be enough for the ice break away these weakened fragments. However, not all rocks were made equal, and because of this, harder and softer rocks are broken up differently. As the upper layers of bedrock are plucked, the lower layers of rock 'relaxes' and 'unloads' as the pressure of weight is relieved.<ref name="smith13"/> This then results in the lower layers eventually fracturing and weakening for further plucking to take place. This cycle could repeat for many thousands of years. |
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Another process that aids plucking is the '''Entraining''' of rock fragments as they are pulled away by the ice. '''Abrasion''' occurs when these loose fragments are "incorporated into the flowing ice at the base of the glacier" where they become "tools to abrade and scrape the bedrock they pass over," effectively acting as a "rough file or piece of coarse sandpaper, wearing away at the valley floor."<ref name="smith14">Smith (2012) p.14</ref> Plucking can remove more volume of rock than abrasion, but the two working together provides an effective system to radically redesign a landscape. Meltwater from crevasses can also aid plucking, with constant erosion from the movement of water. 'Warm glaciers' are those with a temperature close to zero degrees, or the melting point. Larger volumes of water provides a greater flow of ice across the bedrock, and an increase in speed in which the ice travels.<ref name="smith14"/> This was the case with the lakes in Lakeland, although some were created with more complex processes, such as those with two basins: [[Windermere]] and [[Ullswater]]. |
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===Human interference=== |
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The once ebb and flow of ice and, in much more recent times, people, continue to have an effect on the natural backdrop of the second oldest national park in England.<ref group="lower-alpha">The Lake District National Park was formed on 9 May, 1951, second after that of the Peak District, which was formed on 17 April, 1951.</ref> The reservoirs of [[Haweswater]] and [[Thirlmere]] were once natural lakes. They were dammed to raise the water level in a bid to supply fresh water for the people of Manchester, at a price that flooded the valleys, damaging the flora and fauna within them. |
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<!--THIS SECTION REQUIRES MORE DETAIL--> |
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==List of the main lakes== |
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The lakes have been immortalised in text and image by the very people, past and present, with a passion for this rugged landscape. The big lakes are the quintessence of Lakeland, and listed below are 17 bodies of water that give this National Park its name. How these are classified, one could rightly surmise, is by size. Whilst the humble [[tarn]] is usually reserved for the smaller bodies of water, size alone is not the only trait for the lakes. Some tarns are bigger than the smallest of the big lakes, for example, [[Burnmoor Tarn]] near [[Wast Water]], and [[Seathwaite Tarn]] near the [[Old Man of Coniston]], both of which are bigger than [[Elter Water]] and [[Brothers Water]].<ref>Smith (2014) p.8.</ref> |
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One could easily say that each of the lakes have their own distinctive character, companioned by the landscape in which they sit. Size, depth, inflows, outflows, location, and human intervention all play a vital role in our understanding of these expanses of water, which, seen from above, appear to radiate outwards from a central point near the fell of [[High Raise (Langdale)|High Raise]] in Langdale. |
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Each lake below is the subject of a brief overview, with a link to the lake's main article (when these have been written). |
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===Bassenthwaite Lake=== |
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:''Main article: [[Bassenthwaite Lake]]'' |
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The only lake is our list with "lake" in its title. The lake's origins relate directly to the {{w1|last glacial period}} and the effects of a glacially eroded valley that possibly linked Bassenthwaite Lake with that of [[Derwentwater]] as one much larger body of water, seen similarly with [[Buttermere]] and [[Crummock Water]]. Today, they are connected only by the [[River Derwent]], which meanders through the long-ago silted up alluvial plain that separates the two lakes. |
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The name of this lake has changed several times since the Middle Ages.T he name ''Bassenthwaite'' means ''Bastun's clearing'' where ''Bassen'' comes from the Anglo-French surname ''Bastun'', which originally meant stick, and ''[[wiktionary:thwaite|thwaite]]'' is related to Old Norse ''[[wiktionary:þveit|þveit]]'' meaning ''a clearing'' or more accurately, ''forest land cleared for agriculture or habitation''.<ref>Whaley, p.20.</ref> The lake took its name from the village of [[Bassenthwaite]]. |
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===Brothers Water=== |
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<div class="res-img-1200">[[File:Brothers Water - panoramio.jpg]]</div> |
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:''Main article: [[Brothers Water]]'' |
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'''Brothers Water''', also known as '''Brotherswater''', and historically '''Broad Water''', is one of the smallest lakes in Lakeland. It is located in the picturesque Patterdale valley, approximately 4 kilometres (2.5 miles) south of [[Patterdale]] near [[Glenridding]]. The lake's name may derive from the Old Norse ''[[wiktionary:bróðir|bróðir]]'', which means ''brother''. It is claimed that the name of the lake comes from the unfortunate brothers that happened to drown here. Of this widespread tragedy, Harriet Martineau's ''Complete Guide to the English Lakes'' (1855) states: "Brothers Water derives its name from the accident — which is said to have happened twice, — of brothers being lost in it, in the attempt of one to save the other. On one of the two occasions, the accident happened through the breaking of the ice, when the brothers were making a venturesome short cut across it to church." <ref>Martineau (1855) p.105</ref> |
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Although only a fraction larger than [[Elter Water]], Brothers Water was at one time much larger than its current size. Due to a high sedimentary inflow and the natural creation of an alluvial fan (new land formed by sedimentary build up), the lake's size has been reduced by around 900 metres.<ref>Smith (2012) p.100</ref> The lake itself is relatively shallow at 16.7 metres at its deepest point. Its shape is unlike the other lakes, which usually takes the ribbon form, carved by the ice many millennia ago. Here, however, the lake takes on a distinctly more rectangular shape, caused by nature and time. |
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It can be reached via the A592 [[Kirkstone Pass]], which connects [[Windermere]] and [[Ullswater]] through some of the most stunning and rugged mountain scenery. The descent into [[Hartsop]] is indeed dramatic, the drystone walled road winding its way ever downwards, surrounded by vast open slopes; [[Hartsop Dodd]] to the east and [[High Hartsop Dodd]] to the west. |
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===Buttermere=== |
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:''Main article: [[Buttermere]]'' |
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Buttermere is a photogenic and naturally beautiful ribbon lake, set amongst the backdrop of striking fells and picturesque countryside, with "some of the finest glacial features of the district."<ref name="smith78">Smith (2012) p.78</ref> The 12th largest lake from our list is located at the head of the Buttermere Valley where it sits in a glacial trough along with its neighbours [[Crummock Water]] and [[Loweswater]]; the only valley in Lakeland with three lakes. The name ''Buttermere'' means ''the lake with good pasture-land'', which comes from Old English ''[[wiktionary:butere#Old_English|butere]]'' (butter) and ''[[wiktionary:mere#Old_English|mere]]'' (lake, pool).<ref name="whaley61">Whaley (2006) p.61</ref> Another possible origin of the name has links with Jarl Boethar (also known as "Buthar"), an 11th century Norse Earl who'd attained lands around Buttermere, and was the leader of an Anglo-Scandinavian resistance against the Normans under Ranulf le Meschin, Lord of Cumberland.<ref name="whaley61"/> |
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The main settlement is the village of [[Buttermere (village)|Buttermere]]. It was named after the lake. The civil parish of the same name encompasses a large area including Honister in the east, the southern aspect of Dale Head, the northern aspect of High Stile and Haystacks, Grasmoor and Whiteside in their entirety, and both Buttermere and Crummock Water. The countryside within this boundary offers substantial walking opportunities, which makes this a popular place for visitors. One of easiest is the casual walk around the lake, with its slightly undulating and well-maintain gravel paths. |
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The village and environs offer accommodation with two hotels, a youth hostel, holiday cottages, and a campsite. There is also a small church dedicated to St. James, and light refreshments are served in the local farm cafe and tea room respectively. There are three car parks, five with hotel parking facilities. One of the car parks belongs to the National Trust and provides free parking to members. Access is via the B5289 (Honister Pass) or Newlands Pass if coming from [[Keswick]]. |
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===Coniston Water=== |
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:''Main article: [[Coniston Water]]'' |
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===Crummock Water=== |
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:''Main article: [[Crummock Water]]'' |
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===Derwentwater=== |
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<div class="res-img-1200">[[File:Derwentwater and Cat Bells from Friar's Crag (2304).jpeg]]</div> |
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:''Main article: [[Derwentwater]]'' |
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===Elter Water=== |
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<div class="res-img-1200">[[File:Elter Water (5267).jpg]]</div> |
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:''Main article: [[Elter Water]] – The smallest of the lakes'' |
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'''[[Elter Water]]''' is a small lake on the main thoroughfare to the valley of [[Great Langdale]] where the dominant and striking [[Langdale Pikes]] are situated. It is connected via the A593 and lies approximately 5.6 kilometres (3.5 miles) west of [[Ambleside]] and one kilometre southeast from the village of [[Elterwater]]. Both the lake and the village are popular with walkers and cyclists alike, which can be busy all year round but particularly so during the more clement months. |
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The smallest of the lakes in the Lake District, Elter Water is 75 times smaller than [[Windermere]]<ref>Smith (2012) p.5</ref> yet it is by no means lacking in other areas, offering stunning views from the eastern shore looking towards [[Lingmoor Fell]] and the aforementioned Pikes. It is made of three distinct sections and only has a maximum depth of around 6 metres (20 ft). The [[River Brathay]] flows through the southern part of the lake at The Nab, while the [[Great Langdale Beck]] flows from the north. They converge at the eastern section of the lake before continuing southeast towards [[Skelwith Force]] waterfalls at [[Skelwith Bridge]] and on towards Ambleside and [[Windermere (town)|Windermere]]. The majestic Whooper Swans winter on the lake here.<ref name="whaley">Whaley (2006) pp.108-109</ref> |
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===Ennerdale Water=== |
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:''Main article: [[Ennerdale Water]]'' |
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===Esthwaite Water=== |
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<div class="res-img-1200">[[File:Esthwaite Water aerial photograph July 2019.jpg]]</div> |
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:''Main article: [[Esthwaite Water]]'' |
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'''Esthwaite Water''' is a privately-owned, picturesque lake, nestled between [[Windermere]] and [[Coniston Water]] in relatively lowland areas, set against a backdrop of beautiful, rolling hills, with coniferous and deciduous woodlands to the east, south and west. The 11th largest lake from our list has a surface area of 100 hectares (247 acres), 7 kilometres (4.35 miles) of shoreline, and has a maximum depth of 15.5 metres (50 feet). The simplest meaning of ''Esthwaite Water'' would be the ''lake by the eastern clearing'', with the first and second elements coming from Old Norse, and the third from Old English.<ref>Gambles (1985) p.17</ref> |
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Esthwaite Water lies in a fairly open valley that was carved by a separate tongue of ice from the Langdale fells. The ice continued to excavate in a southerly direction before joining with the Windermere flow, south of Claife Heights.<ref>Smith (2012) p.66</ref> This openness gives a feeling of space from some of the various vantage points that offer fine views across the landscape in almost every direction. In 1987 is was designated Site of Special Scientific Interest (SSSI) status, which is protected under conservation. It was London-born Helen Beatrix Potter’s favourite lake, which was handy given the proximity of her 17th-century writing retreat of [[Hilltop]], a modest, picture-perfect farmhouse set within the beautiful village of [[Near Sawrey]]. The main settlement is that of [[Hawkshead]], situated at the northern end of the lake. |
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===Grasmere=== |
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:''Main article: [[Grasmere]]''' |
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===Haweswater=== |
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:''Main article: [[Haweswater]] (Reservoir)'' |
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Haweswater was once a much smaller natural lake, sitting against a backdrop of farmland and a diverse habitat for flora and fauna. A natural promontory called an arcuate delta, formed by sedimentary deposits from Measand Beck, almost divided the lake in two with only a narrow section called ''the straits'' separating the smaller basins of High Water and Low Water, evident in the old OS maps. |
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Due to Manchester’s increasing demand for drinking water, parliament granted the Manchester Corporation permission to dam the northern end of the lake, and create a water supply reservoir. This came at a cost to the long-time residents of the valley. The original water level of the lake was raised by 29 metres,<ref>Smith (2012) p.101</ref> the damming resulted in the relocation of the residents who lived in the villages of Mardale, Measand and a scattering of other farmsteads. Abandoned buildings were demolished by the Royal Engineers, including the Dun Bull Inn and Holy Trinity Church, but the drystone field boundary walls and the old chapel bridge still survive, seen when the water levels are unusually low.<ref>Smith (2012) p.103</ref> |
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Nature finds a way to recover and today, Haweswater is a haven for wildlife including red squirrels and small mountain ringlet butterflies. It is the highest lake in the National Park<ref>[https://www.unitedutilities.com/about-us/acres-of-nature/Haweswater/ Haweswater Reservoir] United Utilities. Accessed 26 April, 2023.</ref> and the landowners, United Utilities, are working in partnership with the RSPB<ref>[https://www.rspb.org.uk/reserves-and-events/reserves-a-z/haweswater-reserve/ Haweswater Reservoir] RSPB. Accessed 26 April, 2023.</ref> to ensure the area is protected for the future – see [https://wildhaweswater.co.uk/ Wild Haweswater] There is a circular walking route around the reservoir along with various trails through ancient woodland. |
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===Loweswater=== |
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:''Main article: [[Loweswater]]'' |
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===Rydal Water=== |
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:''Main article: [[Rydal Water]]'' |
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===Thirlmere=== |
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:''Main article: [[Thirlmere]] (Reservoir)'' |
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===Ullswater=== |
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:''Main article: [[Ullswater]] – The 2nd largest of the lakes'' |
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===Wast Water=== |
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:''Main article: [[Wast Water]] – The deepest of the lakes'' |
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===Windermere=== |
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:''Main article: [[Windermere]] – The largest of the lakes'' |
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===Tarn=== |
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The word '''tarn''', used extensively throughout the northwest and in particularly the Lake District, comes from the late 14 century and typically means a small mountain lake. It is also a dialectal word popularised by the Lake poets.<ref>{{oed|title1=tarn|title2=Tarn|day=22|month=January|year=2022}}</ref> |
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*Old Norse ''[[wiktionary:tjörn|tjörn]]'' → meaning a small mountain lake, pond or pool |
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*Middle English ''terne'' / ''tarne'' → meaning a lake, pond or pool |
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*Proto-Germanic ''[[wiktionary:Reconstruction:Proto-Germanic/ternō|ternō]]'' → a reconstructed word meaning a small lake or water hole |
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''Tarn'' is also cognate with Danish ''[[wiktionary:tjern|tjern]]'', Faroese ''[[wiktionary:tjørn|tjørn]]'' (pond), Icelandic ''[[wiktionary:tjörn|tjörn]]'' (pond), Norwegian Bokmål ''tjern'' (small forest or mountain lake) (Norwegian Nynorsk ''tjern'', ''tjørn''), Swedish ''[[wiktionary:tjärn|tjärn]]'' (small forest lake). |
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{{lakes table}} |
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==Notes== |
==Notes== |
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{{reflist|group=lower-alpha}} |
{{reflist|group=lower-alpha}} |
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==Citations== |
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{{reflist|20em}} |
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==References== |
==References== |
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*Smith, Alan (2012). ''The Big Lakes of Lakeland''. The Landscapes of Cumbria No.5. Keswick: Rigg Side Publications |
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{{reflist}} |
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*Smith, Alan (2014). ''The Smaller Lakes and Tarns of Lakeland''. The Landscapes of Cumbria No.6. Keswick: Rigg Side Publications |
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*Whaley, Diana (2006). ''A Dictionary of Lake District Place-Names''. English Place-Name Society. School of English Studies, University of Nottingham |
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[[Category:Lakes of the Lake District]] |
Latest revision as of 14:07, 8 July 2023
The lakes of the Lake District are creations of nature; beautiful and inspiring. The National Park is home to the deepest lake. It is also home to the four largest lakes in England and Wales.[1] Set against a backdrop of Lakeland mountains, known locally as fells, one can easily conjure up thoughts of bygone authors and poets who so loved their craft; forever sealing a picturesque impression of a romanticised setting in one of the wettest parts of the UK.
Water is abundant here; reason alone for its green hues in summer and long, grey winters. There are hundreds of bodies of water in the Lake District, ranging in size from the largest lakes to the smallest pools, many more than most people would ever care to visit. The popular destinations are what brings the masses here to break away from everyday routine. From hardcore hikers and cyclists to the casual, fair-weather day trippers, visitors to the area who explore this great outdoors, do so because its appeal draws them in, time and time again. The lakes are just one, albeit predominantly so, reason for this influx of people every year.
By name alone, the Lake district has only one lake of the 17 main lakes throughout the National Park – Bassenthwaite Lake, which is nestled in the northern region of the park's periphery. There is a general misconception that Windermere, the largest of the lakes, is prefixed with the word Lake to differentiate it from the small town of the same name. Lake Windermere or Windermere Lake are not official titles, but are used extensively as a means of identifying the lake instead of the town. This grammatical construct (tautology) typifies the redundancy of the word lake, which is not needed due to mere already being present. Also, Windermere Town just sounds a little odd, with town being superfluous.
Although the Lake District has only one body of water with lake in the title, the remaining 16 of the big lakes are named with mere or water. These words are synonymous with the lakes born in this wide open land, either by glacial withdrawal or by human intervention.
Etymology
Before we move on, it is interesting to learn from where these words are derived. Lake District place names take a lot of influence from Old Norse as well as Old English. Some words follow a natural progression through time, others do not and can change dramatically with entirely different meanings. Words can also be cognate with, and influenced by, other languages. A simple appreciation of these can provide a broader understanding of the words we use today.
The three words lake, mere, and water all come from a Proto-Germanic background, however, lake is a little more complicated as it is a merger of two different words from French and English. The French lineage ascends back to Proto-Italic, which spawned the Romance languages (Italian, French, Spanish etc.) What is interesting, all three of these words ultimately refer to a "body of water" of some sort, with subtle variations depending on size and usage. Cognates are also strikingly similar as to be expected, which show how these words developed and changed through time to mean something similar to, or even the same as, their ancestor equivalent.
Rather than discuss this in length here, it is best if these are broken down into more detail separately.
Words prefixed with a * are reconstructed words. This means they have not been directly attested, but instead are hypothesised to have existed based on comparative evidence.
Glacial origins
The term "ice age" can be somewhat ambiguous. The earth is in an ice age called the Quaternary glaciation, which began around 2.58 million years ago and has had many periods of glacial advance and retreat. We are still in this ice age, as suggested by the ice caps present at the poles. However, we are currently experiencing an interglacial or warmer period. In the UK this period is called the Flandrian interglacial.[a] This led to retreating ice that left us with glacially "plucked" and eroded valleys that formed the lake district we see today.
Plucking and abrasion
The whole process of ice excavation can be described in fairly simple terms, when in reality, it involves a complex set of stages working together. Essentially, the movement of glaciers' grinds and pulls apart the bedrock on which it sits. Dr Alan Smith's book, The Big Lakes of Lakeland, describes this process clearly, without over complicating an already complex set of processes. With nowhere else to go except to follow the flow of ice, the broken pieces of rock were then transported as the ice moved along the valleys, in the case of the Lake District, radially in an outward direction from a central core. This core was so thick that maybe only the tips of the highest peaks of Scafell, Helvellyn, Bowfell, and Great Gable were visible.[2] The Last Glacial Maximum was approximately 22,000 years ago and up to that point in time, the ice had been steadily increasing until it reached its maximum, hence the name. All the big lakes were excavated by the ice during this Last Glacial Maximum, a segment of the Last Glacial Period, which encompassed a timeframe between 115,000 - 11,700 years ago. By 13,550 years ago, the ice sheets had retreated and the "valley glaciers had melted away and a new landscape of ice scoured fells and lakes left impounded in the valley floors was revealed."[2]
So, what is plucking? Plucking is a process that removes large fragments of rock under immense pressures and moves them to other locations, sometimes lengthy distances from their original position. This is similar to quarrying, except instead of explosives and heavy machinery, ice does all the hard work. For plucking to be most effective, Fracturing needs to take place. This is a separate process that weakens the bedrock along naturally occurring joints and fractures, prior to being broken up.[3] As Dr Smith explains, these weaknesses in the rocks may be enough for the ice break away these weakened fragments. However, not all rocks were made equal, and because of this, harder and softer rocks are broken up differently. As the upper layers of bedrock are plucked, the lower layers of rock 'relaxes' and 'unloads' as the pressure of weight is relieved.[3] This then results in the lower layers eventually fracturing and weakening for further plucking to take place. This cycle could repeat for many thousands of years.
Another process that aids plucking is the Entraining of rock fragments as they are pulled away by the ice. Abrasion occurs when these loose fragments are "incorporated into the flowing ice at the base of the glacier" where they become "tools to abrade and scrape the bedrock they pass over," effectively acting as a "rough file or piece of coarse sandpaper, wearing away at the valley floor."[4] Plucking can remove more volume of rock than abrasion, but the two working together provides an effective system to radically redesign a landscape. Meltwater from crevasses can also aid plucking, with constant erosion from the movement of water. 'Warm glaciers' are those with a temperature close to zero degrees, or the melting point. Larger volumes of water provides a greater flow of ice across the bedrock, and an increase in speed in which the ice travels.[4] This was the case with the lakes in Lakeland, although some were created with more complex processes, such as those with two basins: Windermere and Ullswater.
Human interference
The once ebb and flow of ice and, in much more recent times, people, continue to have an effect on the natural backdrop of the second oldest national park in England.[b] The reservoirs of Haweswater and Thirlmere were once natural lakes. They were dammed to raise the water level in a bid to supply fresh water for the people of Manchester, at a price that flooded the valleys, damaging the flora and fauna within them.
List of the main lakes
The lakes have been immortalised in text and image by the very people, past and present, with a passion for this rugged landscape. The big lakes are the quintessence of Lakeland, and listed below are 17 bodies of water that give this National Park its name. How these are classified, one could rightly surmise, is by size. Whilst the humble tarn is usually reserved for the smaller bodies of water, size alone is not the only trait for the lakes. Some tarns are bigger than the smallest of the big lakes, for example, Burnmoor Tarn near Wast Water, and Seathwaite Tarn near the Old Man of Coniston, both of which are bigger than Elter Water and Brothers Water.[5]
One could easily say that each of the lakes have their own distinctive character, companioned by the landscape in which they sit. Size, depth, inflows, outflows, location, and human intervention all play a vital role in our understanding of these expanses of water, which, seen from above, appear to radiate outwards from a central point near the fell of High Raise in Langdale.
Each lake below is the subject of a brief overview, with a link to the lake's main article (when these have been written).
Bassenthwaite Lake
- Main article: Bassenthwaite Lake
The only lake is our list with "lake" in its title. The lake's origins relate directly to the last glacial period and the effects of a glacially eroded valley that possibly linked Bassenthwaite Lake with that of Derwentwater as one much larger body of water, seen similarly with Buttermere and Crummock Water. Today, they are connected only by the River Derwent, which meanders through the long-ago silted up alluvial plain that separates the two lakes.
The name of this lake has changed several times since the Middle Ages.T he name Bassenthwaite means Bastun's clearing where Bassen comes from the Anglo-French surname Bastun, which originally meant stick, and thwaite is related to Old Norse þveit meaning a clearing or more accurately, forest land cleared for agriculture or habitation.[6] The lake took its name from the village of Bassenthwaite.
Brothers Water
- Main article: Brothers Water
Brothers Water, also known as Brotherswater, and historically Broad Water, is one of the smallest lakes in Lakeland. It is located in the picturesque Patterdale valley, approximately 4 kilometres (2.5 miles) south of Patterdale near Glenridding. The lake's name may derive from the Old Norse bróðir, which means brother. It is claimed that the name of the lake comes from the unfortunate brothers that happened to drown here. Of this widespread tragedy, Harriet Martineau's Complete Guide to the English Lakes (1855) states: "Brothers Water derives its name from the accident — which is said to have happened twice, — of brothers being lost in it, in the attempt of one to save the other. On one of the two occasions, the accident happened through the breaking of the ice, when the brothers were making a venturesome short cut across it to church." [7]
Although only a fraction larger than Elter Water, Brothers Water was at one time much larger than its current size. Due to a high sedimentary inflow and the natural creation of an alluvial fan (new land formed by sedimentary build up), the lake's size has been reduced by around 900 metres.[8] The lake itself is relatively shallow at 16.7 metres at its deepest point. Its shape is unlike the other lakes, which usually takes the ribbon form, carved by the ice many millennia ago. Here, however, the lake takes on a distinctly more rectangular shape, caused by nature and time.
It can be reached via the A592 Kirkstone Pass, which connects Windermere and Ullswater through some of the most stunning and rugged mountain scenery. The descent into Hartsop is indeed dramatic, the drystone walled road winding its way ever downwards, surrounded by vast open slopes; Hartsop Dodd to the east and High Hartsop Dodd to the west.
Buttermere
- Main article: Buttermere
Buttermere is a photogenic and naturally beautiful ribbon lake, set amongst the backdrop of striking fells and picturesque countryside, with "some of the finest glacial features of the district."[9] The 12th largest lake from our list is located at the head of the Buttermere Valley where it sits in a glacial trough along with its neighbours Crummock Water and Loweswater; the only valley in Lakeland with three lakes. The name Buttermere means the lake with good pasture-land, which comes from Old English butere (butter) and mere (lake, pool).[10] Another possible origin of the name has links with Jarl Boethar (also known as "Buthar"), an 11th century Norse Earl who'd attained lands around Buttermere, and was the leader of an Anglo-Scandinavian resistance against the Normans under Ranulf le Meschin, Lord of Cumberland.[10]
The main settlement is the village of Buttermere. It was named after the lake. The civil parish of the same name encompasses a large area including Honister in the east, the southern aspect of Dale Head, the northern aspect of High Stile and Haystacks, Grasmoor and Whiteside in their entirety, and both Buttermere and Crummock Water. The countryside within this boundary offers substantial walking opportunities, which makes this a popular place for visitors. One of easiest is the casual walk around the lake, with its slightly undulating and well-maintain gravel paths.
The village and environs offer accommodation with two hotels, a youth hostel, holiday cottages, and a campsite. There is also a small church dedicated to St. James, and light refreshments are served in the local farm cafe and tea room respectively. There are three car parks, five with hotel parking facilities. One of the car parks belongs to the National Trust and provides free parking to members. Access is via the B5289 (Honister Pass) or Newlands Pass if coming from Keswick.
Coniston Water
- Main article: Coniston Water
Crummock Water
- Main article: Crummock Water
Derwentwater
- Main article: Derwentwater
Elter Water
- Main article: Elter Water – The smallest of the lakes
Elter Water is a small lake on the main thoroughfare to the valley of Great Langdale where the dominant and striking Langdale Pikes are situated. It is connected via the A593 and lies approximately 5.6 kilometres (3.5 miles) west of Ambleside and one kilometre southeast from the village of Elterwater. Both the lake and the village are popular with walkers and cyclists alike, which can be busy all year round but particularly so during the more clement months.
The smallest of the lakes in the Lake District, Elter Water is 75 times smaller than Windermere[11] yet it is by no means lacking in other areas, offering stunning views from the eastern shore looking towards Lingmoor Fell and the aforementioned Pikes. It is made of three distinct sections and only has a maximum depth of around 6 metres (20 ft). The River Brathay flows through the southern part of the lake at The Nab, while the Great Langdale Beck flows from the north. They converge at the eastern section of the lake before continuing southeast towards Skelwith Force waterfalls at Skelwith Bridge and on towards Ambleside and Windermere. The majestic Whooper Swans winter on the lake here.[12]
Ennerdale Water
- Main article: Ennerdale Water
Esthwaite Water
- Main article: Esthwaite Water
Esthwaite Water is a privately-owned, picturesque lake, nestled between Windermere and Coniston Water in relatively lowland areas, set against a backdrop of beautiful, rolling hills, with coniferous and deciduous woodlands to the east, south and west. The 11th largest lake from our list has a surface area of 100 hectares (247 acres), 7 kilometres (4.35 miles) of shoreline, and has a maximum depth of 15.5 metres (50 feet). The simplest meaning of Esthwaite Water would be the lake by the eastern clearing, with the first and second elements coming from Old Norse, and the third from Old English.[13]
Esthwaite Water lies in a fairly open valley that was carved by a separate tongue of ice from the Langdale fells. The ice continued to excavate in a southerly direction before joining with the Windermere flow, south of Claife Heights.[14] This openness gives a feeling of space from some of the various vantage points that offer fine views across the landscape in almost every direction. In 1987 is was designated Site of Special Scientific Interest (SSSI) status, which is protected under conservation. It was London-born Helen Beatrix Potter’s favourite lake, which was handy given the proximity of her 17th-century writing retreat of Hilltop, a modest, picture-perfect farmhouse set within the beautiful village of Near Sawrey. The main settlement is that of Hawkshead, situated at the northern end of the lake.
Grasmere
- Main article: Grasmere'
Haweswater
- Main article: Haweswater (Reservoir)
Haweswater was once a much smaller natural lake, sitting against a backdrop of farmland and a diverse habitat for flora and fauna. A natural promontory called an arcuate delta, formed by sedimentary deposits from Measand Beck, almost divided the lake in two with only a narrow section called the straits separating the smaller basins of High Water and Low Water, evident in the old OS maps.
Due to Manchester’s increasing demand for drinking water, parliament granted the Manchester Corporation permission to dam the northern end of the lake, and create a water supply reservoir. This came at a cost to the long-time residents of the valley. The original water level of the lake was raised by 29 metres,[15] the damming resulted in the relocation of the residents who lived in the villages of Mardale, Measand and a scattering of other farmsteads. Abandoned buildings were demolished by the Royal Engineers, including the Dun Bull Inn and Holy Trinity Church, but the drystone field boundary walls and the old chapel bridge still survive, seen when the water levels are unusually low.[16]
Nature finds a way to recover and today, Haweswater is a haven for wildlife including red squirrels and small mountain ringlet butterflies. It is the highest lake in the National Park[17] and the landowners, United Utilities, are working in partnership with the RSPB[18] to ensure the area is protected for the future – see Wild Haweswater There is a circular walking route around the reservoir along with various trails through ancient woodland.
Loweswater
- Main article: Loweswater
Rydal Water
- Main article: Rydal Water
Thirlmere
- Main article: Thirlmere (Reservoir)
Ullswater
- Main article: Ullswater – The 2nd largest of the lakes
Wast Water
- Main article: Wast Water – The deepest of the lakes
Windermere
- Main article: Windermere – The largest of the lakes
Notes
- ↑ The Flandrian interglacial period started at the end of the Devensian glaciation (also known as the last glacial period) which was at its maximum approximately 22,000 years ago. This cold period had come to end around 11,700 years ago after which the earth saw a period of warming, the period that we are currently in.
- ↑ The Lake District National Park was formed on 9 May, 1951, second after that of the Peak District, which was formed on 17 April, 1951.
Citations
- ↑ Smith (2012) p.3.
- ↑ 2.0 2.1 Smith (2012) p.12
- ↑ 3.0 3.1 Smith (2012) p.13
- ↑ 4.0 4.1 Smith (2012) p.14
- ↑ Smith (2014) p.8.
- ↑ Whaley, p.20.
- ↑ Martineau (1855) p.105
- ↑ Smith (2012) p.100
- ↑ Smith (2012) p.78
- ↑ 10.0 10.1 Whaley (2006) p.61
- ↑ Smith (2012) p.5
- ↑ Whaley (2006) pp.108-109
- ↑ Gambles (1985) p.17
- ↑ Smith (2012) p.66
- ↑ Smith (2012) p.101
- ↑ Smith (2012) p.103
- ↑ Haweswater Reservoir United Utilities. Accessed 26 April, 2023.
- ↑ Haweswater Reservoir RSPB. Accessed 26 April, 2023.
References
- Smith, Alan (2012). The Big Lakes of Lakeland. The Landscapes of Cumbria No.5. Keswick: Rigg Side Publications
- Smith, Alan (2014). The Smaller Lakes and Tarns of Lakeland. The Landscapes of Cumbria No.6. Keswick: Rigg Side Publications
- Whaley, Diana (2006). A Dictionary of Lake District Place-Names. English Place-Name Society. School of English Studies, University of Nottingham