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Windermere
Windermere (historically Winder Mere) is a ribbon lake in Cumbria, England. It is within the Lake District and is the largest lake in England by length, area, and volume, although considerably smaller than the largest Scottish lochs and Northern Irish loughs.
Windermere is about 11 miles (18 km) in length and 1 mile (1.6 km) at its widest, has a maximum depth of 64 metres (210 ft), and has an elevation of 39 metres (128 ft) above sea level. Its outflow is the River Leven, which drains into Morecambe Bay. For administrative purposes the lake is in the unitary authority area of Westmorland and Furness, and it historically formed part of the boundary between Westmorland and Lancashire.
The lake has been popular with tourists since the Kendal and Windermere Railway's branch line opened in 1847. The Freshwater Biological Association was established on the shore of Windermere in 1929 and much of the early work on lake ecology, freshwater biology and limnology was conducted here.
The word 'Windermere' is thought to translate as "'Winand or Vinand's lake'... The specific has usually been identified with an Old Swedish personal name 'Vinandr', genitive singular 'Vinandar'"... although "the personal noun is of very restricted distribution even in Sweden." Another possibility is that it refers to a "Continental Germanic personal noun, 'Wīnand'...Since this name could not have been current until the 12th century, the fact that the Old Norse genitive singular '-ar-' has been added to it, it would suggest that Old Norse was still a living language in the area at that time." Alternative spellings may be 'Wynhendermere' and 'Wynenderme' The second element is Old English 'mere', meaning 'lake' or 'pool'. It was known as "Winander Mere" or "Winandermere" until at least the 19th century.
Its name suggests it is a mere, a lake that is broad in relation to its depth, but despite the name this is not the case for Windermere, which in particular has a noticeable thermocline, distinguishing it from typical meres. Until the 19th century, the term "lake" was, indeed, not much used by or known to the native inhabitants of the area, who referred to it as Windermere/Winandermere Water, or (in their dialect) Windermer Watter. The name Windermere or Windermer was used of the parish that had clearly taken its name from the water. The poet Norman Nicholson comments on the use of the phrase 'Lake Windermere': "a certain excuse for the tautology can be made in the case of Windermere, since we need to differentiate between the lake and the town, though it would be better to speak of 'Windermere Lake' and Windermere Town', but no one can excuse such ridiculous clumsiness as 'Lake Derwentwater' and 'Lake Ullswater."
The extensive parish included most of Undermilbeck (that is, excepting Winster and the part of Crook chapelry that lay west of the Gilpin, which were part of Kirkby Kendal parish), Applethwaite, Troutbeck and Ambleside-below-Stock, that is, the part of Ambleside that lay south of Stock Beck. The parish church was at Bowness in Undermilbeck.
Windermere is long and narrow, like many other ribbon lakes, and lies in a steep-sided pre-glacial river valley that has become deepened by successive glaciations. The current lake was formed after the Last Glacial Maximum during the retreat of the British and Irish Ice Sheet some time between 17,000 and 14,700 years ago, just before the start of the Windermere Interstadial. The lake water was sourced from the meltwater of retreating ice in the catchment, which receded up the Troutbeck valley and up the valleys that now contain the rivers Rothay and Brathay. There were at least nine ice retreat phases, indicated by buried recessional moraines. The lake has two separate basins – north and south – with different characteristics influenced by the geology. This consists of hard volcanic rocks in the north basin and softer shales in the south.
The lake is drained from its southernmost point by the River Leven. It is replenished by the rivers Brathay, Rothay, Trout Beck, Cunsey Beck and several other lesser streams. The lake is largely surrounded by foothills of the Lake District which provide pleasant low-level walks; to the north and northeast are the higher fells of central Lakeland.
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Windermere AI simulator
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Windermere
Windermere (historically Winder Mere) is a ribbon lake in Cumbria, England. It is within the Lake District and is the largest lake in England by length, area, and volume, although considerably smaller than the largest Scottish lochs and Northern Irish loughs.
Windermere is about 11 miles (18 km) in length and 1 mile (1.6 km) at its widest, has a maximum depth of 64 metres (210 ft), and has an elevation of 39 metres (128 ft) above sea level. Its outflow is the River Leven, which drains into Morecambe Bay. For administrative purposes the lake is in the unitary authority area of Westmorland and Furness, and it historically formed part of the boundary between Westmorland and Lancashire.
The lake has been popular with tourists since the Kendal and Windermere Railway's branch line opened in 1847. The Freshwater Biological Association was established on the shore of Windermere in 1929 and much of the early work on lake ecology, freshwater biology and limnology was conducted here.
The word 'Windermere' is thought to translate as "'Winand or Vinand's lake'... The specific has usually been identified with an Old Swedish personal name 'Vinandr', genitive singular 'Vinandar'"... although "the personal noun is of very restricted distribution even in Sweden." Another possibility is that it refers to a "Continental Germanic personal noun, 'Wīnand'...Since this name could not have been current until the 12th century, the fact that the Old Norse genitive singular '-ar-' has been added to it, it would suggest that Old Norse was still a living language in the area at that time." Alternative spellings may be 'Wynhendermere' and 'Wynenderme' The second element is Old English 'mere', meaning 'lake' or 'pool'. It was known as "Winander Mere" or "Winandermere" until at least the 19th century.
Its name suggests it is a mere, a lake that is broad in relation to its depth, but despite the name this is not the case for Windermere, which in particular has a noticeable thermocline, distinguishing it from typical meres. Until the 19th century, the term "lake" was, indeed, not much used by or known to the native inhabitants of the area, who referred to it as Windermere/Winandermere Water, or (in their dialect) Windermer Watter. The name Windermere or Windermer was used of the parish that had clearly taken its name from the water. The poet Norman Nicholson comments on the use of the phrase 'Lake Windermere': "a certain excuse for the tautology can be made in the case of Windermere, since we need to differentiate between the lake and the town, though it would be better to speak of 'Windermere Lake' and Windermere Town', but no one can excuse such ridiculous clumsiness as 'Lake Derwentwater' and 'Lake Ullswater."
The extensive parish included most of Undermilbeck (that is, excepting Winster and the part of Crook chapelry that lay west of the Gilpin, which were part of Kirkby Kendal parish), Applethwaite, Troutbeck and Ambleside-below-Stock, that is, the part of Ambleside that lay south of Stock Beck. The parish church was at Bowness in Undermilbeck.
Windermere is long and narrow, like many other ribbon lakes, and lies in a steep-sided pre-glacial river valley that has become deepened by successive glaciations. The current lake was formed after the Last Glacial Maximum during the retreat of the British and Irish Ice Sheet some time between 17,000 and 14,700 years ago, just before the start of the Windermere Interstadial. The lake water was sourced from the meltwater of retreating ice in the catchment, which receded up the Troutbeck valley and up the valleys that now contain the rivers Rothay and Brathay. There were at least nine ice retreat phases, indicated by buried recessional moraines. The lake has two separate basins – north and south – with different characteristics influenced by the geology. This consists of hard volcanic rocks in the north basin and softer shales in the south.
The lake is drained from its southernmost point by the River Leven. It is replenished by the rivers Brathay, Rothay, Trout Beck, Cunsey Beck and several other lesser streams. The lake is largely surrounded by foothills of the Lake District which provide pleasant low-level walks; to the north and northeast are the higher fells of central Lakeland.