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Windermere (drink)
Windermere (sometimes tautologically called Lake Windermere to distinguish it from the nearby town of Windermere) is a ribbon lake in Cumbria, England, and part of the Lake District. 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 in length and at its widest, has a maximum depth of , and has an elevation of above sea level. Its outflow is the River Leven, which drains into Morecambe Bay. The lake is in the administrative council area of Westmorland and Furness and the historic county of Westmorland, with the lake forming part of the boundary between the historic counties of Westmorland and Lancashire. It has been one of the country's most popular places for holidays and summer homes since the arrival of the Kendal and Windermere Railway's branch line in 1847. The Freshwater Biological Association was established on the shore of Windermere in 1929 an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake District National Park
The Lake District National Park is a national park in North West England that includes all of the central Lake District, though the town of Kendal, some coastal areas, and the Lakeland Peninsulas are outside the park boundary. The area was designated a national park on 9 May 1951 (less than a month after the first UK national park designation — the Peak District). It retained its original boundaries until 2016 when it was extended by 3% in the direction of the Yorkshire Dales National Park to incorporate areas such as land of high landscape value in the Lune Valley. It is the most visited national park in the United Kingdom with 16.4 million visitors per year and more than 24 million visitor-days per year, the largest of the thirteen national parks in England and Wales, and the second largest in the UK after the Cairngorms National Park. Its aim is to protect the landscape by restricting unwelcome change by industry or commerce. Most of the land in the park is in pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Morecambe Bay
Morecambe Bay is a large estuary in northwest England, just to the south of the Lake District National Park. It is the largest expanse of intertidal mudflats and sand in the United Kingdom, covering a total area of . In 1974, the second largest gas field in the UK was discovered west of Blackpool, with original reserves of over 7 trillion cubic feet (tcf) (200 billion cubic metres). At its peak, 15% of Britain's gas supply came from the bay but production is now in decline. It is also one of the homes of the high brown fritillary butterfly. Natural features The rivers Leven, Kent, Keer, Lune and Wyre drain into the Bay, with their various estuaries making a number of peninsulas within the bay. Much of the land around the bay is reclaimed, forming salt marshes used in agriculture. Morecambe Bay is also an important wildlife site, with abundant birdlife and varied marine habitats, and there is a bird observatory at Walney Island. The bay has rich cockle beds, which have been ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Norman Nicholson
Norman Cornthwaite Nicholson (8 January 1914 – 30 May 1987) was an English poet associated with the Cumbrian town of Millom. His poetry is noted for local concerns, straightforward language, and elements of common speech. Although known chiefly for poetry, Nicholson wrote much in other forms: novels, plays, essays, topography and criticism. Life Nicholson lived in 14 St George's Terrace, a Victorian terraced house and shop in the small industrial town of Millom on the edge of the Lake District, the son of Joseph Nicholson, a gentleman's outfitter, and his wife Edith Cornthwaite (died 1919). Nicholson was educated at Holborn Hill School and Millom Secondary School, but his education was interrupted at the age of 16, when he needed treatment for pulmonary tuberculosis. He then spent two years at a sanatorium in Linford, Hampshire. Nicholson was influenced by the social and religious community around the local Wesleyan Methodist chapel in Millom, to which belonged Rosetta Sobe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thermocline
A thermocline (also known as the thermal layer or the metalimnion in lakes) is a thin but distinct layer in a large body of fluid (e.g. water, as in an ocean or lake; or air, e.g. an atmosphere) in which temperature changes more drastically with depth than it does in the layers above or below. In the ocean, the thermocline divides the upper mixed layer from the calm deep water below. Depending largely on season, latitude, and turbulent mixing by wind, thermoclines may be a semi-permanent feature of the body of water in which they occur, or they may form temporarily in response to phenomena such as the radiative heating/cooling of surface water during the day/night. Factors that affect the depth and thickness of a thermocline include seasonal weather variations, latitude, and local environmental conditions, such as tides and currents. Oceans Most of the heat energy of the sunlight that strikes the Earth is absorbed in the first few centimeters at the ocean's surface, which ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the la ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old English Language
Old English (, ), or Anglo-Saxon, is the earliest recorded form of the English language, spoken in England and southern and eastern Scotland in the early Middle Ages. It was brought to Great Britain by Anglo-Saxon settlers in the mid-5th century, and the first Old English literary works date from the mid-7th century. After the Norman conquest of 1066, English was replaced, for a time, by Anglo-Norman (a relative of French) as the language of the upper classes. This is regarded as marking the end of the Old English era, since during this period the English language was heavily influenced by Anglo-Norman, developing into a phase known now as Middle English in England and Early Scots in Scotland. Old English developed from a set of Anglo-Frisian or Ingvaeonic dialects originally spoken by Germanic tribes traditionally known as the Angles, Saxons and Jutes. As the Germanic settlers became dominant in England, their language replaced the languages of Roman Britain: Common Br ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Windermere On A Misty Morning
A lake is an area filled with water, localized in a Depression (geology), basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the World Ocean, ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glacier, glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic dra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limnology
Limnology ( ; from Greek λίμνη, ''limne'', "lake" and λόγος, ''logos'', "knowledge") is the study of inland aquatic ecosystems. The study of limnology includes aspects of the biological, chemical, physical, and geological characteristics of fresh and saline, natural and man-made bodies of water. This includes the study of lakes, reservoirs, ponds, rivers, springs, streams, wetlands, and groundwater.Wetzel, R.G. 2001. Limnology: Lake and River Ecosystems, 3rd ed. Academic Press () Water systems are often categorized as either running (lotic) or standing (lentic). Limnology includes the study of the drainage basin, movement of water through the basin and biogeochemical changes that occur en route. A more recent sub-discipline of limnology, termed landscape limnology, studies, manages, and seeks to conserve these ecosystems using a landscape perspective, by explicitly examining connections between an aquatic ecosystem and its drainage basin. Recently, the need to underst ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Ecosystem
A lake ecosystem or lacustrine ecosystem includes biotic (living) plants, animals and micro-organisms, as well as abiotic (non-living) physical and chemical interactions. Lake ecosystems are a prime example of lentic ecosystems (''lentic'' refers to stationary or relatively still freshwater, from the Latin ''lentus'', which means "sluggish"), which include ponds, lakes and wetlands, and much of this article applies to lentic ecosystems in general. Lentic ecosystems can be compared with lotic ecosystems, which involve flowing terrestrial waters such as rivers and streams. Together, these two ecosystems are examples of freshwater ecosystems. Lentic systems are diverse, ranging from a small, temporary rainwater pool a few inches deep to Lake Baikal, which has a maximum depth of 1642 m. The general distinction between pools/ponds and lakes is vague, but Brown states that ponds and pools have their entire bottom surfaces exposed to light, while lakes do not. In addition, some lakes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Freshwater Biological Association
The Freshwater Biological Association (FBA) is an independent scientific organisation founded in 1929 in Cumbria by Felix Eugen Fritsch, William Harold Pearsall, Francis Balfour-Browne, and Robert Gurney among others. Whilst originally created to be a research station it has evolved into a learned society whose mission is "to promote the sustainable management of freshwater ecosystems and resources, using the best available science". It works closely alongside other organisations, notably Natural Environment Research Council. The FBA promotes freshwater science through innovative research, maintained specialist scientific facilities, a programme of scientific meetings, production of publications, and by providing sound independent scientific opinion. As of 2010, the FBA hosted both published and unpublished collections, two specialist libraries and varieties of long term data sets from sites of scientific significance. It is managed by the Chief Executive who was assisted by 25 sta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kendal And Windermere Railway
The Kendal and Windermere Railway built a branch line from the main line to Kendal and on to Windermere, in Cumbria in north-west England. It was promoted by local interests in Kendal when it became clear that the Lancaster and Carlisle Railway would not be routed through Kendal. It was built from a junction at Oxenholme to Kendal to a terminus near Windermere; at the time there was no settlement of that name. The line opened in April 1847. The engineer was Joseph Locke and the partnership of contractors consisted of Thomas Brassey, William Mackenzie, Robert Stephenson and George Heald. Excursion traffic and residential development was greatly encouraged by the branch line, and the town of Windermere flourished but the company was not commercially successful and sold its line to the London and North Western Railway. The leisure business on which the branch line depended declined considerably around 1960 and the infrastructure was simplified. It remains open as the Winder ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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