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Glenridding Dodd

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70-566: Glenridding Dodd ( the rounded hill above Glenridding ) is a small fell in the English Lake District , at the end of a ridge descending from the Helvellyn range in the Eastern Fells . It stands above the village of Glenridding and on the western shore of Ullswater . Although small and not of great elevation, its top is a fine viewpoint for Ullswater and for the fells clustered round

140-701: A change known as Holtzmann's law . An epenthetic vowel became popular by 1200 in Old Danish, 1250 in Old Swedish and Old Norwegian, and 1300 in Old Icelandic. An unstressed vowel was used which varied by dialect. Old Norwegian exhibited all three: /u/ was used in West Norwegian south of Bergen , as in aftur , aftor (older aptr ); North of Bergen, /i/ appeared in aftir , after ; and East Norwegian used /a/ , after , aftær . Old Norse

210-632: 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. For all practical purposes, fjell can be translated as "mountain" and the Norwegian language has no other commonly used word for mountain. In Sweden, fjäll generally refers to any mountain or upland high enough that forest will not naturally survive at

280-572: A community; thus the township of Cartmel Fell . In northern England, there is a Lord of the Fells – this ancient aristocratic title being associated with the Lords of Bowland . Groups of cairns are a common feature on many fells, often marking the summit – there are fine examples on Wild Boar Fell in Mallerstang Dale, Cumbria , and on Nine Standards Rigg just outside Kirkby Stephen , Cumbria. As

350-417: A female raven or a male crow. All neuter words have identical nominative and accusative forms, and all feminine words have identical nominative and accusative plurals. The gender of some words' plurals does not agree with that of their singulars, such as lim and mund . Some words, such as hungr , have multiple genders, evidenced by their determiners being declined in different genders within

420-412: A front vowel to be split into a semivowel-vowel sequence before a back vowel in the following syllable. While West Norse only broke /e/ , East Norse also broke /i/ . The change was blocked by a /w/ , /l/ , or /ʀ/ preceding the potentially-broken vowel. Some /ja/ or /jɔ/ and /jaː/ or /jɔː/ result from breaking of /e/ and /eː/ respectively. When a noun, pronoun, adjective, or verb has

490-409: A given sentence. Nouns, adjectives, and pronouns were declined in four grammatical cases – nominative , accusative , genitive , and dative  – in singular and plural numbers. Adjectives and pronouns were additionally declined in three grammatical genders. Some pronouns (first and second person) could have dual number in addition to singular and plural. The genitive

560-584: A long vowel or diphthong in the accented syllable and its stem ends in a single l , n , or s , the r (or the elder r - or z -variant ʀ ) in an ending is assimilated. When the accented vowel is short, the ending is dropped. The nominative of the strong masculine declension and some i-stem feminine nouns uses one such -r (ʀ). Óðin-r ( Óðin-ʀ ) becomes Óðinn instead of * Óðinr ( * Óðinʀ ). The verb blása ('to blow'), has third person present tense blæss ('[he] blows') rather than * blæsr ( * blæsʀ ). Similarly,

630-399: A low fell the view is "delightful." Beyond Glenridding are the claw-shaped end of Birkhouse Moor , and Keldas, its subsidiary top closer to the lake. Further south, the fells clustered around the valleys above Patterdale are seen. A stone boundary marker, just west of the summit, is inscribed with the letters M (on the side facing Glenridding) and H (on the side facing Glencoyne). This marked

700-474: A noun must mirror the gender of that noun , so that one says, " heill maðr! " but, " heilt barn! ". As in other languages, the grammatical gender of an impersonal noun is generally unrelated to an expected natural gender of that noun. While indeed karl , "man" is masculine, kona , "woman", is feminine, and hús , "house", is neuter, so also are hrafn and kráka , for "raven" and "crow", masculine and feminine respectively, even in reference to

770-472: A similar development influenced by Middle Low German . Various languages unrelated to Old Norse and others not closely related have been heavily influenced by Norse, particularly the Norman language ; to a lesser extent, Finnish and Estonian . Russian, Ukrainian , Belarusian , Lithuanian and Latvian also have a few Norse loanwords. The words Rus and Russia , according to one theory, may be named after

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840-601: A voiced velar fricative [ɣ] in all cases, and others have that realisation only in the middle of words and between vowels (with it otherwise being realised [ɡ] ). The Old East Norse /ʀ/ was an apical consonant , with its precise position unknown; it is reconstructed as a palatal sibilant . It descended from Proto-Germanic /z/ and eventually developed into /r/ , as had already occurred in Old West Norse. The consonant digraphs ⟨hl⟩ , ⟨hr⟩ , and ⟨hn⟩ occurred word-initially. It

910-460: A vowel or semivowel of a different vowel backness . In the case of i-umlaut and ʀ-umlaut , this entails a fronting of back vowels, with retention of lip rounding. In the case of u-umlaut , this entails labialization of unrounded vowels. Umlaut is phonemic and in many situations grammatically significant as a side effect of losing the Proto-Germanic morphological suffixes whose vowels created

980-403: 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 livestock , bred for life on the uplands, such as Rough Fell sheep, Fell terriers and Fell ponies . It is also found in many place names across the north of England, often attached to the name of

1050-468: A word limited to far-Northern dialects of Finnish and Karelian, is a loan from Sami , compare Proto-Sami *tuontër , South Sami doedtere , Northern Sami duottar , Inari Sami tuodâr "uplands, mountains, tundra", Kildin Sami tūndâr , which means "uplands, treeless mountain tract" and is cognate with Finnish tanner "hard ground". From this Sami word, the word " tundra " is borrowed, as well, through

1120-448: A word. Strong verbs ablaut the lemma 's nucleus to derive the past forms of the verb. This parallels English conjugation, where, e.g., the nucleus of sing becomes sang in the past tense and sung in the past participle. Some verbs are derived by ablaut, as the present-in-past verbs do by consequence of being derived from the past tense forms of strong verbs. Umlaut or mutation is an assimilatory process acting on vowels preceding

1190-529: Is a dialect word of unknown origin, but common in hill names in the Lake District and the Scottish Borders for bare rounded summits, either free standing or subsidiary shoulders to higher neighbours. Mossdale is 'boggy valley' from the dialect word moss (from Old Norse mosi or Old English mos ), 'bog', and the dialect word dale (from Old Norse dalr ), 'valley.' The Rake is 'the track' from

1260-422: Is a fine viewpoint over Ullswater, nearly 300 m below. The top of Glenridding Dodd is a short ridge, with patches of heather, rocky knolls and marshy hollows. The highest point, at the western end, is marked by a small cairn , but better views of Glenridding and almost the whole of Ullswater may be had from the eastern end of the ridge where the ground falls steeply away, just above the 400 m contour. For

1330-461: Is expected to exist, such as in the male names Ragnarr , Steinarr (supposedly * Ragnarʀ , * Steinarʀ ), the result is apparently always /rː/ rather than */rʀ/ or */ʀː/ . This is observable in the Runic corpus. In Old Norse, i/j adjacent to i , e , their u-umlauts, and æ was not possible, nor u/v adjacent to u , o , their i-umlauts, and ǫ . At

1400-574: Is more common in Old West Norse in both phonemic and allophonic positions, while it only occurs sparsely in post-runic Old East Norse and even in runic Old East Norse. This is still a major difference between Swedish and Faroese and Icelandic today. Plurals of neuters do not have u-umlaut at all in Swedish, but in Faroese and Icelandic they do, for example the Faroese and Icelandic plurals of the word land , lond and lönd respectively, in contrast to

1470-569: Is present-day Denmark and Sweden, most speakers spoke Old East Norse. Though Old Gutnish is sometimes included in the Old East Norse dialect due to geographical associations, it developed its own unique features and shared in changes to both other branches. The 12th-century Icelandic Gray Goose Laws state that Swedes , Norwegians , Icelanders , and Danes spoke the same language, dǫnsk tunga ("Danish tongue"; speakers of Old East Norse would have said dansk tunga ). Another term

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1540-456: Is that the nonphonemic difference between the voiced and the voiceless dental fricative is marked. The oldest texts and runic inscriptions use þ exclusively. Long vowels are denoted with acutes . Most other letters are written with the same glyph as the IPA phoneme, except as shown in the table below. Ablaut patterns are groups of vowels which are swapped, or ablauted, in the nucleus of

1610-515: Is the case with Seathwaite Fell , 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 Wetherlam , in the Coniston Fells , though understood to refer to the mountain as

1680-557: Is unclear whether they were sequences of two consonants (with the first element realised as /h/ or perhaps /x/ ) or as single voiceless sonorants /l̥/ , /r̥/ and /n̥/ respectively. In Old Norwegian, Old Danish and later Old Swedish, the groups ⟨hl⟩ , ⟨hr⟩ , and ⟨hn⟩ were reduced to plain ⟨l⟩ , ⟨r⟩ , ⟨n⟩ , which suggests that they had most likely already been pronounced as voiceless sonorants by Old Norse times. The pronunciation of ⟨hv⟩

1750-603: Is unclear, but it may have been /xʷ/ (the Proto-Germanic pronunciation), /hʷ/ or the similar phoneme /ʍ/ . Unlike the three other digraphs, it was retained much longer in all dialects. Without ever developing into a voiceless sonorant in Icelandic, it instead underwent fortition to a plosive /kv/ , which suggests that instead of being a voiceless sonorant, it retained a stronger frication. Primary stress in Old Norse falls on

1820-466: The Isle of Man , parts of northern England , and Scotland . The English word "fell" comes from Old Norse fell and fjall (both forms existed). It is cognate with Danish fjeld , Faroese fjall and fjøll , Icelandic fjall and fell , Norwegian fjell with dialects fjøll , fjødd , fjedd , fjedl , fjill , fil(l) , and fel , and Swedish fjäll , all referring to mountains rising above

1890-525: The Latin alphabet , there was no standardized orthography in use in the Middle Ages. A modified version of the letter wynn called vend was used briefly for the sounds /u/ , /v/ , and /w/ . Long vowels were sometimes marked with acutes but also sometimes left unmarked or geminated. The standardized Old Norse spelling was created in the 19th century and is, for the most part, phonemic. The most notable deviation

1960-582: The Ordovician Period. All the rocks on the fell belong to the Birker Fell Andesite Formation . This was formed predominantly by eruptions of mobile andesitic lava from shallow-sided volcanoes. These rocks are part of a thick succession of lava sheets found around the western and northern sides of the Lake District. Among these andesitic lavas were some small quantities of dacitic lavas, formed when more viscous (more silica-rich) magma

2030-657: The Rus' people , a Norse tribe, probably from present-day east-central Sweden. The current Finnish and Estonian words for Sweden are Ruotsi and Rootsi , respectively. A number of loanwords have been introduced into Irish , many associated with fishing and sailing. A similar influence is found in Scottish Gaelic , with over one hundred loanwords estimated to be in the language, many of which are related to fishing and sailing. Old Norse vowel phonemes mostly come in pairs of long and short. The standardized orthography marks

2100-579: The Russian language . 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, e.g. Rukatunturi is technically a vaara , as it lacks alpine tundra. The term förfjäll (literally "fore-fell") is used in Sweden and Finland to denote mountainous zones lower and less dissected than

2170-493: The University of Bergen , Anders Lundeberg, has summed up the problem by stating, "There simply is no fixed and unambiguous definition of fjell ." Ivar Aasen defined fjell as a "tall berg ", 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

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2240-627: The alpine tree line . In northern England, especially in the Lake District and in the Pennine Dales , the word "fell" originally referred to an area of uncultivated high ground used as common grazing usually on common land and above the timberline. Today, generally, "fell" refers to the mountains and hills of the Lake District and the Pennine Dales. Names that originally referred to grazing areas have been applied to these hilltops. This

2310-653: The language into the region by the time of the Second Swedish Crusade in the 13th century at the latest. The modern descendants of the Old West Norse dialect are the West Scandinavian languages of Icelandic , Faroese , Norwegian , and the extinct Norn language of Orkney and Shetland , although Norwegian was heavily influenced by the East dialect, and is today more similar to East Scandinavian (Danish and Swedish) than to Icelandic and Faroese. The descendants of

2380-654: The word stem , so that hyrjar would be pronounced /ˈhyr.jar/ . In compound words, secondary stress falls on the second stem (e.g. lærisveinn , /ˈlɛːɾ.iˌswɛinː/ ). Unlike Proto-Norse, which was written with the Elder Futhark , runic Old Norse was originally written with the Younger Futhark , which had only 16 letters. Because of the limited number of runes, several runes were used for different sounds, and long and short vowels were not distinguished in writing. Medieval runes came into use some time later. As for

2450-551: The 11th century in most of Old East Norse. However, the distinction still holds in Dalecarlian dialects . The dots in the following vowel table separate the oral from nasal phonemes. Note: The open or open-mid vowels may be transcribed differently: Sometime around the 13th century, /ɔ/ (spelled ⟨ǫ⟩ ) merged with /ø/ or /o/ in most dialects except Old Danish , and Icelandic where /ɔ/ ( ǫ ) merged with /ø/ . This can be determined by their distinction within

2520-957: The 12th-century First Grammatical Treatise but not within the early 13th-century Prose Edda . The nasal vowels, also noted in the First Grammatical Treatise, are assumed to have been lost in most dialects by this time (but notably they are retained in Elfdalian and other dialects of Ovansiljan ). See Old Icelandic for the mergers of /øː/ (spelled ⟨œ⟩ ) with /ɛː/ (spelled ⟨æ⟩ ) and /ɛ/ (spelled ⟨ę⟩ ) with /e/ (spelled ⟨e⟩ ). Old Norse had three diphthong phonemes: /ɛi/ , /ɔu/ , /øy ~ ɛy/ (spelled ⟨ei⟩ , ⟨au⟩ , ⟨ey⟩ respectively). In East Norse these would monophthongize and merge with /eː/ and /øː/ , whereas in West Norse and its descendants

2590-794: The 12th-century Icelandic sagas in the original language (in editions with normalised spelling). Old Icelandic was very close to Old Norwegian , and together they formed Old West Norse , which was also spoken in Norse settlements in Greenland , the Faroes , Ireland , Scotland , the Isle of Man , northwest England, and in Normandy . Old East Norse was spoken in Denmark, Sweden, Kievan Rus' , eastern England, and Danish settlements in Normandy. The Old Gutnish dialect

2660-552: The Old East Norse dialect are the East Scandinavian languages of Danish and Swedish . Among these, the grammar of Icelandic and Faroese have changed the least from Old Norse in the last thousand years, though their pronunciations both have changed considerably from Old Norse. With Danish rule of the Faroe Islands, Faroese has also been influenced by Danish. Both Middle English (especially northern English dialects within

2730-479: The Old Norse phonemic writing system. Contemporary Icelandic-speakers can read Old Norse, which varies slightly in spelling as well as semantics and word order. However, pronunciation, particularly of the vowel phonemes, has changed at least as much in Icelandic as in the other North Germanic languages. Faroese retains many similarities but is influenced by Danish, Norwegian, and Gaelic ( Scottish and/or Irish ). Although Swedish, Danish and Norwegian have diverged

2800-468: The Swedish plural land and numerous other examples. That also applies to almost all feminine nouns, for example the largest feminine noun group, the o-stem nouns (except the Swedish noun jord mentioned above), and even i-stem nouns and root nouns , such as Old West Norse mǫrk ( mörk in Icelandic) in comparison with Modern and Old Swedish mark . Vowel breaking, or fracture, caused

2870-500: The area of the Danelaw ) and Early Scots (including Lowland Scots ) were strongly influenced by Norse and contained many Old Norse loanwords . Consequently, Modern English (including Scottish English ), inherited a significant proportion of its vocabulary directly from Norse. The development of Norman French was also influenced by Norse. Through Norman, to a smaller extent, so was modern French. Written modern Icelandic derives from

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2940-541: The beginning of words, this manifested as a dropping of the initial /j/ (which was general, independent of the following vowel) or /v/ . Compare ON orð , úlfr , ár with English word, wolf, year . In inflections, this manifested as the dropping of the inflectional vowels. Thus, klæði + dat -i remains klæði , and sjáum in Icelandic progressed to sjǫ́um > sjǫ́m > sjám . The * jj and * ww of Proto-Germanic became ggj and ggv respectively in Old Norse,

3010-685: The boundary between the lands of the Marshall family of Patterdale and the Howard family of Greystoke. Much of the land above the village of Glenridding, including the Stybarrow Oaks, is privately owned, but above the wall the fell is Open Access land. Ascents can begin from Glenridding, with its large pay-and-display car park, up the path known as The Rake, or from the lay-by on the A592 road immediately north of Stybarrow Crag, beside Mossdale Beck. Both paths meet at

3080-411: The cluster */Crʀ/ cannot be realized as /Crː/ , nor as */Crʀ/ , nor as */Cʀː/ . The same shortening as in vetr also occurs in lax = laks ('salmon') (as opposed to * lakss , * laksʀ ), botn ('bottom') (as opposed to * botnn , * botnʀ ), and jarl (as opposed to * jarll , * jarlʀ ). Furthermore, wherever the cluster */rʀ/

3150-428: The consolidation of Scandinavian kingdoms from about the 8th to the 15th centuries. The Proto-Norse language developed into Old Norse by the 8th century, and Old Norse began to develop into the modern North Germanic languages in the mid- to late 14th century, ending the language phase known as Old Norse. These dates, however, are not absolute, since written Old Norse is found well into the 15th century. Old Norse

3220-490: The dialect word rake , 'track.' This is used elsewhere in the Lake District for a narrow path on a hill. Bleas Crag may be 'the dark crag' from the dialect work blea (from Old Norse blár ), 'dark,' plus crag. Fell A fell (from Old Norse fell , fjall , "mountain" ) is a high and barren landscape feature, such as a mountain or moor -covered hill. The term is most often employed in Fennoscandia , Iceland ,

3290-449: The diphthongs remained. Old Norse has six plosive phonemes, /p/ being rare word-initially and /d/ and /b/ pronounced as voiced fricative allophones between vowels except in compound words (e.g. veðrabati ), already in the Proto-Germanic language (e.g. * b *[β] > [v] between vowels). The /ɡ/ phoneme was pronounced as [ɡ] after an /n/ or another /ɡ/ and as [k] before /s/ and /t/ . Some accounts have it

3360-462: The fell proper. However, its more pronounced relief, its often higher amount of plateaux, and its coherent valley systems distinguishes the förfjäll also from the undulating hilly terrain ( bergkullsterräng ) and the plains with residual hills ( bergkullslätt ). Generally, the förfjäll do not surpass 1000 m ASL. As a geomorphic unit, the förfjäll extends across Sweden as a 650 km-long and 40 km to 80 km-broad belt from Dalarna in

3430-399: The long vowels with an acute accent. In medieval manuscripts, it is often unmarked but sometimes marked with an accent or through gemination . Old Norse had nasalized versions of all ten vowel places. These occurred as allophones of the vowels before nasal consonants and in places where a nasal had followed it in an older form of the word, before it was absorbed into a neighboring sound. If

3500-519: 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 Great Britain as hillwalking . The word "fell" also enjoys limited use in Scotland; with, for example, the Campsie Fells in central Scotland, to

3570-433: The most, they still retain considerable mutual intelligibility . Speakers of modern Swedish, Norwegian and Danish can mostly understand each other without studying their neighboring languages, particularly if speaking slowly. The languages are also sufficiently similar in writing that they can mostly be understood across borders. This could be because these languages have been mutually affected by each other, as well as having

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3640-503: The nasal was absorbed by a stressed vowel, it would also lengthen the vowel. This nasalization also occurred in the other Germanic languages, but were not retained long. They were noted in the First Grammatical Treatise , and otherwise might have remained unknown. The First Grammarian marked these with a dot above the letter. This notation did not catch on, and would soon be obsolete. Nasal and oral vowels probably merged around

3710-482: The north it is bounded by Mossdale Beck, and to the south by the village of Glenridding, and Glenridding Beck. The lower slopes on the south and east sides are wooded with deciduous trees (the Stybarrow Oaks), and on the north side larch trees reach almost to the summit Glenridding Dodd is a small fell measuring only 1 km in length and less than that in width, and its highest point rises to only 442 m. Yet it

3780-557: The north-east of Glasgow. One of the most famous examples of the use of the word "fell" in Scotland is Goat Fell , the highest point on the Isle of Arran . Criffel and the nearby Long Fell in Galloway may be seen from the northern Lake District of England. Peel Fell in the Kielder Forest is on the border between the Scottish Borders to the north and the English county of Northumberland to

3850-715: The old, highly eroded, gently shaped terrain without glaciers, as found in Finland. They are round inselbergs 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 Karelides 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

3920-536: The root vowel, ǫ , is short. The clusters */Clʀ, Csʀ, Cnʀ, Crʀ/ cannot yield */Clː, Csː, Cnː, Crː/ respectively, instead /Cl, Cs, Cn, Cr/ . The effect of this shortening can result in the lack of distinction between some forms of the noun. In the case of vetr ('winter'), the nominative and accusative singular and plural forms are identical. The nominative singular and nominative and accusative plural would otherwise have been OWN * vetrr , OEN * wintrʀ . These forms are impossible because

3990-542: The south to Norrbotten in the north. Old Norse Old Norse , also referred to as Old Nordic , or Old Scandinavian , was a stage of development of North Germanic dialects before their final divergence into separate Nordic languages. Old Norse was spoken by inhabitants of Scandinavia and their overseas settlements and chronologically coincides with the Viking Age , the Christianization of Scandinavia , and

4060-451: The south. 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 forest line . Distinct summits can be referred to as et fjell (a mountain). High plateaus ( vidde landscape) such as Hardangervidda are also regarded as fjell. Professor of geography at

4130-672: The top, in effect a mountain tundra . 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. Safjällets nationalpark  [ sv ] and Kynnefjäll  [ sv ] ) being referred to as "fjäll", similar to how

4200-497: The umlaut allophones . Some /y/ , /yː/ , /ø/ , /øː/ , /ɛ/ , /ɛː/ , /øy/ , and all /ɛi/ were obtained by i-umlaut from /u/ , /uː/ , /o/ , /oː/ , /a/ , /aː/ , /au/ , and /ai/ respectively. Others were formed via ʀ-umlaut from /u/ , /uː/ , /a/ , /aː/ , and /au/ . Some /y/ , /yː/ , /ø/ , /øː/ , and all /ɔ/ , /ɔː/ were obtained by u-umlaut from /i/ , /iː/ , /e/ , /eː/ , and /a/ , /aː/ respectively. See Old Icelandic for information on /ɔː/ . /œ/

4270-475: The valleys above Patterdale . Glenridding Dodd is the final subsidiary top on the east ridge of Stybarrow Dodd . It takes the form of a short east-west ridge above the village of Glenridding . To the east the ridge falls steeply and terminates in the precipitous rock face of Stybarrow Crag beside the A592 road on the shore of Ullswater . To the west a col separates it from the south-east ridge of Sheffield Pike . To

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4340-482: The verb skína ('to shine') had present tense third person skínn (rather than * skínr , * skínʀ ); while kala ('to cool down') had present tense third person kell (rather than * kelr , * kelʀ ). The rule is not absolute, with certain counter-examples such as vinr ('friend'), which has the synonym vin , yet retains the unabsorbed version, and jǫtunn (' giant '), where assimilation takes place even though

4410-537: The wall across the col to the west of the summit. A short climb from here leads to the summit. Alfred Wainwright noted that it had once been a much more popular ascent for the sake of its views, but that old paths had become overgrown and neglected in his day. The rocks of Glenridding Dodd are all part of the Borrowdale Volcanic Group , formed on the margin of an ancient continent during a period of intense volcanic activity, roughly 450 million years ago in

4480-479: The word is used in Norwegian In Finnish, the mountains characteristic of the region of Lapland are called tunturi (plural: tunturit ), i.e. "fell". A tunturi is a hill high enough that its top is above the tree line and has alpine tundra . In Finnish, the geographical term vuori is used for mountains recently uplifted and with jagged terrain featuring permanent glaciers, while tunturi refers to

4550-408: Was norrœnt mál ("northern speech"). Today Old Norse has developed into the modern North Germanic languages Icelandic , Faroese , Norwegian , Danish , Swedish , and other North Germanic varieties of which Norwegian, Danish and Swedish retain considerable mutual intelligibility . Icelandic remains the most conservative language, such that in present-day Iceland, schoolchildren are able to read

4620-404: Was a moderately inflected language with high levels of nominal and verbal inflection. Most of the fused morphemes are retained in modern Icelandic, especially in regard to noun case declensions, whereas modern Norwegian in comparison has moved towards more analytical word structures. Old Norse had three grammatical genders – masculine, feminine, and neuter. Adjectives or pronouns referring to

4690-452: Was divided into three dialects : Old West Norse (Old West Nordic, often referred to as Old Norse ), Old East Norse (Old East Nordic), and Old Gutnish . Old West Norse and Old East Norse formed a dialect continuum , with no clear geographical boundary between them. Old East Norse traits were found in eastern Norway , although Old Norwegian is classified as Old West Norse, and Old West Norse traits were found in western Sweden . In what

4760-511: Was erupted. Such dacitic rock is found on the lower parts of the southern and eastern slopes of the fell (but not including Stybarrow Crag). The name Glenridding Dodd is recorded from 1823 onwards. Glenridding is probably 'the valley full of bracken', from Cumbric glinn (or possibly Irish Gaelic gleann ), 'glen, valley' and the Cumbric equivalent of the Welsh rhedyn , 'fern, bracken.' Dod or dodd

4830-535: Was obtained through a simultaneous u- and i-umlaut of /a/ . It appears in words like gøra ( gjǫra , geyra ), from Proto-Germanic *garwijaną , and commonly in verbs with a velar consonant before the suffix like søkkva < *sankwijaną . OEN often preserves the original value of the vowel directly preceding runic ʀ while OWN receives ʀ-umlaut. Compare runic OEN glaʀ, haʀi, hrauʀ with OWN gler, heri (later héri ), hrøyrr/hreyrr ("glass", "hare", "pile of rocks"). U-umlaut

4900-703: Was spoken in Gotland and in various settlements in the East. In the 11th century, Old Norse was the most widely spoken European language , ranging from Vinland in the West to the Volga River in the East. In Kievan Rus' , it survived the longest in Veliky Novgorod , probably lasting into the 13th century there. The age of the Swedish-speaking population of Finland is strongly contested, but Swedish settlement had spread

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