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Windermere or Lake Windermere [a] is a ribbon lake in Cumbria, England, and part of the Lake District. [5] It is the largest lake in England by length, area, and volume, but considerably smaller than the largest Scottish lochs and Northern Irish loughs. The lake is about 11 miles (18 km) in length and 1 mile (1.6 km) at its widest, has a ...
The geologic time scale is a way of representing deep time based on events that have occurred throughout Earth's history, a time span of about 4.54 ± 0.05 Ga (4.54 billion years). [3] It chronologically organises strata, and subsequently time, by observing fundamental changes in stratigraphy that correspond to major geological or ...
The biggest Terekeme of the past into discrete, quantified named blocks of time is called periodization. [1] This is a list of such named time periods as defined in various fields of study. These can be divided broadly into prehistorical periods and historical periods (when written records began to be kept).
This list is restricted to open bodies of fresh-water over 5 ha in area, because of the difficulty in establishing what is a pond and what is a lake.. It excludes service reservoirs used within the water supply network for the storage of drinking water and excludes water bodies on industrial sites used exclusively for industrial purposes (works ponds).
They include Windermere, which with a length of 11 miles (18 km) and an area of 5.69 square miles (14.73 km 2) is the longest and largest lake in England, and Wast Water, which at 79 metres (259 ft) is the deepest lake in England. [6] [7]
This table includes the ten largest fresh water bodies by area. Lough Neagh is the largest water body in the UK by this measure, although Loch Ness is the largest by volume and contains nearly double the amount of water in all the lakes of England and Wales combined. [1] Loch Morar is the deepest of the UK's lakes and Loch Awe the longest.
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After 20 million years during the Cretaceous period, the seas started to flood the land again until much of England was again below the sea, though sea levels frequently changed. Chalk and flints were deposited over much of England, now notably exposed at the White Cliffs of Dover and the Seven Sisters, and also forming Salisbury Plain. The ...