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Fell (from , "mountain → landscape over the tree line"; , , ) is a high and barren landscape feature, such as a mountain or -covered hill, often mountain landscape over the , etc. The term is most often employed in , , the Isle of Man, parts of , and .


Etymology
The word "fell", including fell, comes from fell (in fell, felle) with the same or similar meaning as its descendants. Its root meaning is "", especially steep mountain, in some later glossaries translated as "", etc, however, its descendants in English and Swedish, etc, both independently refer to "open mountain landscapes" of similar nature, indicating a common ancestral sense. sources often use the word in regards to high mountains or the Scandinavian Mountains, etc, and in later Swedish the given base definition is "landscape above the ", etc. The 1956 Scottish National Dictionary gives the definitions for fell in both and dialectal English during the 18th–19th century as: "a hill, especially a rocky, rather precipitous hill (1808); a tract of hill-moor; a level piece of ground on the side or top of a hill (1825, )".

Scots forms found in place-names includes: fiel and field, and fiold. The Orcadian form fiold is also found independently as "a hill; upland pasturage" (1887), especially in (1942). These probably stem from a form akin to *fiel but may have intermixed with English "field", as given for the cognate fjeld in the dictionary , or an Old Norse analog, etc. The Norse cognate to English "field" is listed in the Swedish Academy's dictionary (SAOB) as fiælder (), to the stem fiæll-, modern , meaning "plot, divided piece of land".

Other Old Norse forms include: fjall and fiæl. Inherited forms include: , fjæld; , fjøll; , fell; , with Norwegian dialects: fjøll, fjødd, fjedd, fjedl, fjill, fil(l), and fel; and ; all referring to mountains rising above the and the corresponding nature, etc.Bjorvand and Lindeman (2007:270–271).


Types
Fells can be divided into various types based on various arbitrary parameters. In , fells are commonly divided into high, low and fore fell based on elevation properties.


High fell
High fell () denotes fell above the (at least above sea level). Such areas usually feature significant elevation differences, sharp peaks, glaciers, snow, and bare mountain devoid of vegetation due to not having been deposited there by the . These areas are usually crossed by .

High fell is covered with snow for most of the year and may even receive snowfall during the summer, which, if there is a lot of snowfall, sometimes leads to the snow not having time to melt during the summer, which over time forms due to the constant build up of snow. These glaciers may be 30 meters thick and consist of compressed ice. While not always covered in glaciers, high fell is characterized by such, and glaciers have a major impact on how the shape of the high mountains changes over time.

The term is recorded as early as the 15th century (1460-1480), as høghfiæl, denoted as "high mountain or fell" ().


Low fell
Low fell () denotes fell below the (< above sea level) but above the . It is the most common type of fell and may cover very extensive areas, often made up of undulating mountain plains. These are sometimes devoid of vegetation due to not having been deposited there by the .

Low fell rarely have , however, they may occur under certain conditions.


Fore fell
Fore fell () denotes the corresponding nature below and in the fell . Fore fell areas are characterized by large flat areas and numerous and large . The flat bedrock surfaces, which often dominate these areas, prevent rapid water runoff and provide conditions for a high groundwater level and extensive bog formation.

Intrinsically, fell should be above the tree line to be considered fell, which is not the case for fore fell, however, such is still usually included by extension due to their direct affiliation and many similarities to proper fell, both in terms of character and terrain. Fore fell is such that has previously been above the tree line, and thus bare fell proper; however, since the tree line has increased in elevation over time, such have become vegetated, while still being reminiscent of fell.

Generally, fore fell do not surpass above the . As a geomorphic unit, fore fell extends across Sweden as a -long and -broad belt from in the south to in the north.


British Isles
In northern England, especially in the and in the Dales, the word "fell" originally referred to an area of uncultivated high ground used as common usually on and above the timberline. Today, generally, "fell" refers to the and of the Lake District and the Pennine Dales.

Names that originally referred to grazing areas have been applied to these hilltops. This is the case with , for example, which would be the common grazing land used by the farmers of Seathwaite. The fellgate marks the road from a settlement onto the fell (see photograph for example), as is the case with the Seathwaite Fell. In other cases the reverse is true; for instance, the name of , in the , though understood to refer to the mountain as a whole, strictly speaking refers to the summit; the slopes have names such as Tilberthwaite High Fell, Low Fell and Above Beck Fells.

The word "fell" is also used in the names of various breeds of , bred for life on the uplands, such as Rough Fell sheep, and .


Place names
Fell is also found in many place names across the north of England, often attached to the name of a community; thus the township of . In northern England, there is a Lord of the Fells – this ancient aristocratic title being associated with the Lords of Bowland.

Groups of are a common feature on many fells, often marking the summit – there are fine examples on Wild Boar Fell in Dale, , and on Nine Standards Rigg just outside , Cumbria.

There are examples of fells named "Beacon Fell": Beacon Fell, Lancashire and Beacon Fell, Cumbria.


Activities
As the most mountainous region of England, the Lake District is the area most closely associated with the sport of fell running, which takes its name from the fells of the district. Fellwalking is also the term used locally for the activity known in the rest of as .


Scotland
The word "fell" also enjoys limited use in Scotland; with, for example, the in central Scotland, to the north-east of Glasgow. One of the most famous examples of the use of the word "fell" in Scotland is , the highest point on the Isle of Arran. and the nearby Long Fell in Galloway may be seen from the northern Lake District of England. in the Kielder Forest is on the border between the Scottish Borders to the north and the English county of Northumberland to the south.

File:Campsie Fells (154725510).jpg| , north-east of , Scotland File:Summit of Goatfell (geograph 4953152).jpg|Summit of , Isle of Arran, Scotland File:Carter Fell - geograph.org.uk - 1468356.jpg| , , England–Scotland


Fennoscandia

Finland
In Finnish, the fells are called tunturi (plural: tunturit). A tunturi is a hill high enough that its top is above the and has . In Finnish, the geographical term vuori is used for mountains recently uplifted and with jagged terrain featuring permanent glaciers, while tunturi refers to the old, highly eroded, gently shaped terrain without glaciers, as found in Finland.Web-Facta, WSOY 2003. They are round rising from the otherwise flat surroundings. The tree line can be at a rather low altitude, such as 600 m in Enontekiö, owing to the high latitude. The fells in Finnish Lapland form vestiges of the mountains, formed two billion years ago. The term tunturi is also generally used to refer to treeless plains at high altitudes in far north regions.

The term tunturi, originally a word limited to far-Northern dialects of Finnish and Karelian, is a from , compare Proto-Sami *tuontër, South Sami doedtere, duottar, Inari Sami tuodâr "uplands, mountains, tundra", tūndâr, which means "uplands, treeless mountain tract" and is cognate with Finnish tanner ("hard ground"). From this Sami word, the word "" is borrowed, as well, through the .

Hills that are over 50 m high, but do not reach the tree line are referred to as vaara, while the general term for hills including hills of 50 m or less is mäki.

In place names, however, tunturi, vaara and vuori are used inconsistently, for example: is technically a vaara, as it lacks alpine tundra.


Norway
In Norway, fjell, in common usage, is generally interpreted as simply a summit or area of greater altitude than a hill, which leads to a great deal of local variation in what is defined as a fjell. Fjell is mostly used about areas above the . Distinct summits can be referred to as et fjell (a mountain). High plateaus ( vidde landscape) such as are also regarded as fjell. Professor of geography at the University of Bergen, Anders Lundeberg, has summed up the problem by stating, "There simply is no fixed and unambiguous definition of fjell."

defined fjell as a "tall ", primarily referring to a berg that reaches an altitude where trees do not grow, lower berg are referred to as "berg", ås (hill, ridge) or hei (moor, heathland). The fixed expression til fjells refers to mountains (or uplands) as a collective rather than a specific location or specific summit (the "s" in til fjells is an old genitive form remaining only in fixed expressions). According to Ivar Aasen, berg refers to cliffs, bedrock and notable elevations of the surface underpinned by bedrock; berg also refers to the substance of bedrock.Nesset, Kåre (1964). No lærer vi grammatikk. Oslo: Aschehoug.Aasen, Ivar (1918): Norsk ordbog med dansk forklaring. Vestmannalaget/Cammermeyer.

For all practical purposes, fjell can be translated as "mountain" and the Norwegian language has no other commonly used word for mountain.


Sweden
In Sweden, fjäll generally refers to any mountain or upland high enough that forest will not naturally survive at the top, in effect a mountain . Fjäll is primarily used to describe mountains in the Nordic countries, but also more generally to describe mountains shaped by massive ice sheets, primarily in Arctic and subarctic regions. There are however dialectal differences in usage, with comparatively low mountains or plateaus, sometimes tree-covered, in Bohuslän and Västergötland (e.g. and ) being referred to as "fjäll", similar to how the word is used in Norwegian

The gave the following definition in 1924:

"Fell – mountain (or mountain range) of such height that it exceeds the tree line; sometimes especially of a mountain that reaches above the snow line (high fell) as opposed to those that do not reach there (low fell); compare alp, highland; in some areas (especially in Bohuslän and ) also of lower mountains (of a comparatively bare or wild and desolate nature); in the definite plural especially of the North Scandinavian mountains, formerly sometimes approaching the sense of a proper name, synonymous with the Scandinavian Mountains

Despite the 1924 source's claim that the definite plural form, fjällen, "formerly" approached being a proper name for the North Scandinavian mountains, the term has lived on as an informal proper name for the Scandinavian Mountains, now also being used in a singular collective sense: de svenska fjällen: "the Swedish fells", vs den svenska fjällen, "the Swedish fell collectively". The term is often used in conjunction with going on holiday to in , as is given by the Swedish 1998 music hit Vi drar till fjällen ("We're headin' to fjällen).

A related term is vål, which roughly mean "", found in placenames such as , , etc.


See also
  • List of fells in the Lake District
  • List of Wainwrights (the 214 fells described in A. Wainwright's Pictorial Guide to the Lakeland Fells)
  • The Outlying Fells of Lakeland
  • List of Birketts (the 541 fells in Bill Birketts Complete Lakeland Fells)
  • Middlesex Fells, a rocky highland just north of Boston, Massachusetts
  • , Isle of Man


Notes

Books
  • Wainwright, A. (2003). "Coniston Old Man" in A Pictorial Guide to the Lakeland Fells, Book Four: The Southern Fells, p. 15. London: Francis Lincoln.
  • Bjordvand, Harald; Lindeman, Fredrik Otto (2007). Våre arveord. Novus.
  • Falk, Hjalmar; Torp, Alf (2006). Etymologisk ordbog over det norske og det danske sprog. Bjørn Ringstrøms Antikvariat.

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