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    The Lake District area saw repeated glaciations during the Quaternary period, with the development of an ice cap. The most recent glaciation occurred over the period 115,000 to 11,700 years ago, which resulted in the current landscape of the Lake District. The Lake District was an upland area and was unaffected by the main British-Irish ice sheet, which flowed around the margins of the massif. The most recent glaciation lasted from 26,000 to 10,000 years ago, and the ice sheets and glaciers covered the Lake District, spreading out in a radial drainage pattern that has given rise to the pattern of lakes we see today. The rocks of today's national park sat well south of the equator about 500 million years ago. In much more recent geologic time 2 million years ago Pleistocene glaciers crept southward to cover most of mainland Britain. The glaciers advanced and retreated multiple times, carving deep valleys that later filled with meltwater and rain.
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