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==Glacial origins== |
==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 |
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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===Human interference=== |
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==List of the main lakes== |
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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 national park in England after the Peak District.<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> |
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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 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> 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. |
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 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> 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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