Trevico is a town and comune in the province of Avellino , Campania , southern Italy .
96-770: Located in the Apennines upon a steep hill at 3,576 feet (1,090 m) altitude, Trevico is the highest inhabited place in Campania. Its main produce are hams, chestnuts and potatoes, each of them is awarded PAT quality mark. The town is part of the Roman Catholic Diocese of Ariano Irpino-Lacedonia and its territory borders with the municipalities of Carife , Castel Baronia , San Nicola Baronia , San Sossio Baronia , Scampitella , Vallata , and Vallesaccarda . Trevico has an oceanic climate ( Köppen : Cfb ) with cold winters, mild summers, and evenly spread precipitation throughout
192-606: A mountain range consisting of parallel smaller chains extending c. 1,200 km (750 mi) the length of peninsular Italy . In the northwest they join the Ligurian Alps at Altare . In the southwest they end at Reggio di Calabria , the coastal city at the tip of the peninsula. Since 2000 the Environment Ministry of Italy, following the recommendations of the Apennines Park of Europe Project, has defined
288-444: A broad labial (for example, lebor /ˈLʲev u r/ "book"; domun /ˈdoṽ u n/ "world"). The phoneme /ə/ occurred in other circumstances. The occurrence of the two phonemes was generally unrelated to the nature of the corresponding Proto-Celtic vowel, which could be any monophthong: long or short. Long vowels also occur in unstressed syllables. However, they rarely reflect Proto-Celtic long vowels, which were shortened prior to
384-423: A complex sound system involving grammatically significant consonant mutations to the initial consonant of a word. Apparently, neither characteristic was present in the preceding Primitive Irish period, though initial mutations likely existed in a non-grammaticalised form in the prehistoric era. Contemporary Old Irish scholarship is still greatly influenced by the works of a small number of scholars active in
480-429: A consonant ensures its unmutated sound. While the letter ⟨c⟩ may be voiced / ɡ / at the end of some words, but when it is written double ⟨cc⟩ it is always voiceless / k / in regularised texts; however, even final /ɡ/ was often written "cc", as in bec / becc "small, little" (Modern Irish and Scottish beag , Manx beg ). In later Irish manuscripts, lenited f and s are denoted with
576-584: A high diversity of flora and fauna. These mountains are one of the last refuges of the big European predators such as the Italian wolf and the Marsican brown bear , now extinct in the rest of Central Europe . The mountains lend their name to the Apennine peninsula that forms the major part of Italy. They are mostly verdant, although one side of the highest peak, Corno Grande , is partially covered by Calderone glacier ,
672-534: A picked corps) on special police duty with a detachment of twenty men from the Ravenna fleet. Snow lies on the highest peaks of the Apennines for almost the whole year. The range produces no minerals, but there are a considerable number of good mineral springs , some of which are thermal (such as Bagni di Lucca , Montecatini , Monsummano , Porretta, Telese), while others are cool (such as Nocera, Sangemini , Cinciano),
768-681: A series of tunnels have been constructed to conduct "the Bologna-Florence rail line", which is neither a single line nor a single tunnel. The Porrettana Line went into service in 1864, the Direttissima in 1934 and the High Speed in 1996. A few dozen tunnels support the three of them, the longest on the High-Speed Line being the Voglia Tunnel at 16.757 km (10.412 mi). The longest is on
864-454: A sound / h / and a letter h , there is no consistent relationship between the two. Vowel-initial words are sometimes written with an unpronounced h , especially if they are very short (the Old Irish preposition i "in" was sometimes written hi ) or if they need to be emphasised (the name of Ireland, Ériu , was sometimes written Hériu ). On the other hand, words that begin with
960-676: A stone marks the top of the pass. In the vicinity are fragments of the old road and three ruins of former fortifications. At Carcare , the main roads connect with the upper Bormida valley (Bormida di Mallare) before turning west. The Scrivia , the Trebbia and the Taro , tributaries of the Po River , drain the northeast slopes. The range contains dozens of peaks. Toward the southern end the Aveto Natural Regional Park includes Monte Penna . Nearby
1056-469: A word containing it being variably spelled with ⟨au, ai, e, i, u⟩ across attestations. Tulach "hill, mound" is the most commonly cited example of this vowel, with the spelling of its inflections including tulach itself, telaig , telocho , tilchaib , taulich and tailaig . This special vowel also ran rampant in many words starting with the stressed prefix air- (from Proto-Celtic *ɸare ). Archaic Old Irish (before about 750) had
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#17331054831481152-608: Is a technology complex in central and southern Italy from the Italian Middle Bronze Age (15th–14th centuries BC). In the mid-20th century the Apennine was divided into Proto-, Early, Middle and Late sub- phases , but now archaeologists prefer to consider as "Apennine" only the ornamental pottery style of the later phase of Middle Bronze Age (BM3). This phase is preceded by the Grotta Nuova facies (central Italy) and by
1248-601: Is at about 3,200 m (10,500 ft), leaving the Apennines below it, except for the one remaining glacier. Snow may fall from October to May. Rainfall increases with latitude. The range's climates, depending on elevation and latitude, are the Oceanic climate and Mediterranean climate . The mammal fauna is mainly composed of Italian wolves (endemic), Corsican hare , badgers , weasels , foxes , marmots , Etruscan shrew , Crested porcupine , European snow vole and Apennine shrews (endemic), Marsican brown bears (endemic),
1344-605: Is deep and separates the Apennines on the left bank from a lesser range, the Tuscan Anti-Apennines (Sub-Apennines) on its right. The Apennine System forms an irregular arc with centers of curvature located in the Tyrrhenian Sea. The northern and southern segments comprise parallel chains that can be viewed as single overall mountain ridges, such as the Ligurian Mountains. The center, being thicker and more complex,
1440-643: Is geologically divided into an inner and an outer arc with regard to the centers of curvature. The geologic definition, however, is not the same as the geographic. Based on rock type and orogenic incidents, the northern segment of the arc is divided into the Outer Northern Apennines (ONA) and the Inner Northern Apennines (INA). The Central Apennines are divided into the Umbrian–Marchean ( Appennino umbro-marchigiano ) or Roman Apennines in
1536-465: Is mainly grasslands of the Montane grasslands and shrublands biome; with Temperate broadleaf and mixed forests, and Mediterranean forests, woodlands, and scrub below it. The tree line in the Apennines can be found in the range 1,600 m (5,200 ft) to 2,000 m (6,600 ft). About 5% of the map area covered by the Apennines is at or above the tree line—or in the treeline ecotone. The snow line
1632-533: Is part of the Monti Sibillini , incorporated into Parco Nazionale dei Monti Sibillini . Further north is the parco naturale regionale della Gola della Rossa e di Frasassi [ it ] , in which are the Gola della Rossa ("Red Gorge") and Frasassi Caves . Still further north is Parco Sasso Simone e Simoncello. The Italian Park Service calls it the "green heart" of Italy. The region is heavily forested , such as
1728-508: Is shown in the chart below. The complexity of Old Irish phonology is from a four-way split of phonemes inherited from Primitive Irish, with both a fortis–lenis and a "broad–slender" ( velarised vs. palatalised ) distinction arising from historical changes. The sounds /f v θ ð x ɣ h ṽ n l r/ are the broad lenis equivalents of broad fortis /p b t d k ɡ s m N L R/ ; likewise for the slender (palatalised) equivalents. (However, most /f fʲ/ sounds actually derive historically from /w/ , since /p/
1824-431: Is subject to u -affection, becoming ⟨éu⟩ or ⟨íu⟩ , while /e₁ː/ is not. A similar distinction may have existed between /o₁ː/ and /o₂ː/ , both written ⟨ó⟩ , and stemming respectively from former diphthongs (*eu, *au, *ou) and from compensatory lengthening. However, in later Old Irish both sounds appear usually as ⟨úa⟩ , sometimes as ⟨ó⟩ , and it
1920-506: Is that it derives from the Celtic penn , 'mountain', 'summit': A-penn-inus , which could have been assigned during the Celtic domination of north Italy in the 4th century BC or before. The name originally applied to the north Apennines. However historical linguists have never found a derivation with which they all agree. Wilhelm Deecke said: "[…] its etymology is doubtful but some derive it from
2016-547: Is the Bocca Serriola Pass in northern Umbria , which links Fano and Città di Castello . The Tiber River at Rome flows from Monte Fumaiolo in the Tuscan-Romagnol Apennine from northeast to southwest, projecting into the Tyrrhenian Sea at right angles to the shore. The upper Tiber, however, flows from northwest to southeast, gradually turning through one right angle clockwise. The northern Tiber Valley
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#17331054831482112-745: Is the Italian sparrow . The reasons for this choice are related to the fact that the Italian wolf, which inhabits the Apennine Mountains and the Western Alps , features prominently in Latin and Italian cultures, such as in the legend of the founding of Rome . In Italy the transhumance took place mainly starting from the Abruzzi Apennines, moving both towards the Tuscan and Lazio Maremma and above all towards
2208-457: Is the ancestor of all modern Goidelic languages: Modern Irish , Scottish Gaelic and Manx . A still older form of Irish is known as Primitive Irish . Fragments of Primitive Irish, mainly personal names, are known from inscriptions on stone written in the Ogham alphabet. The inscriptions date from about the 4th to the 6th centuries. Primitive Irish appears to have been very close to Common Celtic ,
2304-421: Is the highest point of Ligurian Apennines, Monte Maggiorasca at 1,800 m (5,900 ft). The main and only feasible overland route connecting the coastal plain of Liguria to the north Italian plain runs through Bocchetta di Altare. It has always been of strategic importance. Defenders of north Italy have had to control it since ancient times, as the various fortifications placed there testify. Trenitalia ,
2400-594: Is unclear whether /o₂ː/ existed as a separate sound any time in the Old Irish period. /ou/ existed only in early archaic Old Irish ( c. 700 or earlier); afterwards it merged into /au/ . Neither sound occurred before another consonant, and both sounds became ⟨ó⟩ in later Old Irish (often ⟨ú⟩ or ⟨u⟩ before another vowel). The late ⟨ó⟩ does not develop into ⟨úa⟩ , suggesting that ⟨áu⟩ > ⟨ó⟩ postdated ⟨ó⟩ > ⟨úa⟩ . Later Old Irish had
2496-559: The eclipsis consonants also denoted with a superdot: Old Irish digraphs include the lenition consonants: the eclipsis consonants: the geminatives : and the diphthongs : The following table indicates the broad pronunciation of various consonant letters in various environments: When the consonants b, d, g are eclipsed by the preceding word (always from a word-initial position), their spelling and pronunciation change to: ⟨mb⟩ / m / , ⟨nd⟩ /N/ , ⟨ng⟩ / ŋ / Generally, geminating
2592-507: The Alpine system . Prior to the explosion of data on the topic from about the year 2000, many authors took the approach that the Apennines had the same origin as the Alps. Even today, some authors use the term Alpine-Apennine system. They are not, however, the same system and did not have the same origin. The Alps were millions of years old before the Apennines rose from the sea. The northward movement of
2688-612: The Aterno from the north-west and the Gizio from the south-east, is more important; and so is the Sangro . The central Apennines are crossed by the railway from Rome to Pescara via Avezzano and Sulmona: the railway from Orte to Terni (and thence to Foligno ) follows the Nera valley; while from Terni a line ascends to the plain of Rieti, and thence crosses the central chain to Aquila, whence it follows
2784-475: The Book of Leinster , contain texts which are thought to derive from written exemplars in Old Irish now lost and retain enough of their original form to merit classification as Old Irish. The preservation of certain linguistic forms current in the Old Irish period may provide reason to assume that an Old Irish original directly or indirectly underlies the transmitted text or texts. The consonant inventory of Old Irish
2880-649: The Eurasian eagle-owl There are also numerous amphibians such as the Apennine yellow-bellied toad (endemic), the Italian cave salamander (endemic), the Italian newt (endemic), the Italian stream frog (endemic) and the Spectacled salamander (endemic), the Italian tree frog (endemic), the Agile frog , the Italian edible frog (endemic), the Common toad , the Balearic green toad ,
2976-658: The European fallow deer , the European mouflon and the Pyrenean chamois . There are also numerous birds such as the golden eagle , the Bonelli's eagle , the Eurasian goshawk , the hoopoe , the hawk , the European roller , the White-backed woodpecker , the European green woodpecker , the Alpine chough , the Egyptian vulture , the European nightjar , the Italian sparrow (endemic) and
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3072-621: The Ligurian Sea in the Gulf of Genoa , from about Savona below the upper Bormida River valley to about La Spezia ( La Cisa pass ) below the upper Magra River valley. The range follows the Gulf of Genoa separating it from the upper Po Valley . The northwestern border follows the line of the Bormida River to Acqui Terme . There the river continues northeast to Alessandria in the Po Valley , but
3168-672: The Majella Massif. Among them are two national parks: Gran Sasso e Monti della Laga National Park and Majella National Park ; and the Regional Park of the Monti Simbruini. Gran Sasso contains Corno Grande , the highest peak of the Apennines (2912 m). Other features between the western and central ranges are the plain of Rieti , the valley of the Salto, and the Lago Fucino ; while between
3264-798: The Northern spectacled salamander (endemic), the Fire salamander , the Smooth newt , the Alpine newt , and the Italian crested newt . The reptile fauna is mainly composed of suc as the Italian Aesculapian snake (endemic), the Dice snake , the Green whip snake , the Aesculapian snake , the Smooth snake , the Vipera ursinii , the Vipera aspis , the Italian wall lizard (endemic),
3360-479: The Po Valley in northern Italy. Compressional forces have been acting from north to south in the Alps and from south to north in the Apennines, but instead of being squeezed into mountains the valley has been subsiding at 1 to 4 mm (0.16 in) per year since about 25 mya , before the Apennines existed. It is now known to be not an erosional feature, but is a filled portion of the Adriatic Trench, called
3456-504: The Podarcis muralis , the European green lizard . Notable Apennine freshwater fishes are the Brook lamprey (endemic), Lombardy lamprey , Italian bleak (endemic), Horse barbel (endemic), Eurasian carp , Scardola scardafa (endemic), European perch , Chubius Chub , Tench and Northern pike . The Italian wolf is the national animal of Italy, while the national bird of the country
3552-1148: The Pollino National Park , the Vesuvius National Park , the Cilento, Vallo di Diano and Alburni National Park , the Appennino Lucano - Val d'Agri - Lagonegrese National Park , the Sila National Park , the Aspromonte National Park . Important rivers originate from the Apennines are the Panaro , the Secchia , the Reno , the Marecchia , the Rubicon , the Metauro , the Arno , the Tiber ,
3648-863: The Savio , the Nera , the Velino , the Tronto , the Aterno-Pescara , the Aniene , the Liri , the Sangro and the Volturno . Among the lakes of glacial origin of the Alpine type is Lago di Pilato . The Apennines were created in the Apennine orogeny beginning in the early Neogene (about 20 mya , the middle Miocene ) and continuing today. Geographically they are partially (or appear to be) continuous with
3744-399: The Tavoliere delle Puglie . The Apennines are to some extent covered with forests, though these were probably more extensive in classical times ( Pliny mentions especially pine , oak and beech woods, Hist. Nat . xvi. 177); they have indeed been greatly reduced in comparatively modern times by indiscriminate timber-felling, and though serious attempts at reforestation have been made by
3840-405: The abbey of Reichenau , now in St. Paul in Carinthia (Austria), contains a spell and four Old Irish poems. The Liber Hymnorum and the Stowe Missal date from about 900 to 1050. In addition to contemporary witnesses, the vast majority of Old Irish texts are attested in manuscripts of a variety of later dates. Manuscripts of the later Middle Irish period, such as the Lebor na hUidre and
3936-409: The orogeny . These extend in a northwest–southeast direction from the River Tronto to the River Sangro , which drain into the Adriatic . The coastal hills of the east extend between San Benedetto del Tronto in the north and Torino di Sangro in the south. The eastern chain consists mainly of the southern part of the Monti Sibillini , the Monti della Laga , the Gran Sasso d'Italia Massif and
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4032-417: The orthography of Old Irish is not fixed, so the following statements are to be taken as generalisations only. Individual manuscripts may vary greatly from these guidelines. The Old Irish alphabet consists of the following eighteen letters of the Latin alphabet : in addition to the five long vowels , shown by an acute accent (´): the lenited consonants denoted with a superdot (◌̇): and
4128-418: The Adriatic foredeep after its function as a subduction zone was discovered. Old Irish Old Irish , also called Old Gaelic ( Old Irish : Goídelc , Ogham script : ᚌᚑᚔᚇᚓᚂᚉ; Irish : Sean-Ghaeilge ; Scottish Gaelic : Seann-Ghàidhlig ; Manx : Shenn Yernish or Shenn Ghaelg ), is the oldest form of the Goidelic/Gaelic language for which there are extensive written texts. It
4224-421: The African Plate and its collision with the European Plate then caused the Alpine Orogeny , beginning in the late Mesozoic. The band of mountains created extends from Spain to Turkey in a roughly east–west direction and includes the Alps. The Apennines are much younger, extend from northwest to southeast, and are not a displacement of the Alpine chain. The key evidence of the difference is the geologic behavior of
4320-538: The Apennine range, and so are Cilento hills on the west. On the converse the promontory of Mount Gargano , on the east, is completely isolated, and so are the Campanian volcanic arc near Naples . The district is traversed from north-west to south-east by the railway from Sulmona to Benevento and on to Avellino , and from south-west to northeast by the railways from Caianello via Isernia to Campobasso and Termoli, from Caserta to Benevento and Foggia, and from Nocera Inferiore and Avellino to Rocchetta Sant'Antonio,
4416-426: The Apennines System to include the mountains of north Sicily , a total distance of 1,500 kilometres (930 mi) . The system forms an arc enclosing the east of the Ligurian and Tyrrhenian seas. The Apennines conserve some intact ecosystems that have survived human intervention. In these are some of the best-preserved forests and montane grasslands in Europe, now protected by national parks and, within them,
4512-435: The Calabrian southern Apennine Mountains extend along the northern coast of Sicily (the Sicilian Apennines, Italian Appennino siculo )— Pizzo Carbonara (6,493 feet (1,979 m)) being the highest peak. The number of vascular plant species in the Apennines has been estimated at 5,599. Of these, 728 (23.6%) are in the treeline ecotone . Hemicryptophytes predominate in the entire Apennine chain. The tree line ecotone
4608-434: The Direttissima, the Great Apennine Tunnel, which at 18.5 kilometres (11.5 miles) is the longest entirely within Italy, although the Simplon Tunnel , which connects Italy and Switzerland, is longer. Automobile traffic is carried by the Autostrada del Sole, Route A1, which goes through numerous shorter tunnels, bypassing an old road, originally Roman, through Futa Pass. In December 2015, a new Route A1 called Variante di Valico
4704-446: The Greek Pindus Mountains from the same root, but *kwen- < *kwi- is not explained by any rule. By some, English pin , as well as pen and Latin pinna or penna , 'feather' (in the sense of the horn of the quill), have been connected to the name. This view has the word originating in Latium inconsistently with the theory of the northern origin. None of these derivations is accepted unquestionably. The Apennine culture
4800-434: The Greeks and Sicilians with timber for shipbuilding. The railway from South Eufemia to Catanzaro and Catanzaro Marina crosses the isthmus, and an ancient road may have run from Squillace to Monteleone. The second group extends to the south end of the Italian Peninsula , culminating in the Aspromonte (1,960 metres (6,420 ft)) to the east of Reggio di Calabria . In both groups the rivers are quite unimportant. Finally,
4896-411: The Late Bronze Age as it is defined in Greece and the Aegean. The people of the Apennine culture were alpine cattle herdsmen grazing their animals over the meadows and groves of mountainous central Italy. They lived in small hamlets located in defensible places. On the move between summer pastures they built temporary camps or lived in caves and rock shelters. Their range was not necessarily confined to
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#17331054831484992-505: The Ligurian-Celtish Pen or Ben , which means mountain peak." A large number of place names seem to reflect pen : Penarrig, Penbrynn, Pencoid, Penmon, Pentir, etc. or ben : Beanach, Benmore, Benabuird, Benan, Bencruachan, etc. In one derivation Pen/Ben is cognate with Old Irish cenn , 'head', but an original *kwen- would be required, which is typologically not found in languages that feature labio-velars . Windisch and Brugmann reconstructed Indo-European *kwi- , deriving also
5088-516: The Modern Irish and Scottish dialects that still possess a four-way distinction in the coronal nasals and laterals . /Nʲ/ and /Lʲ/ may have been pronounced [ɲ] and [ʎ] respectively. The difference between /R(ʲ)/ and /r(ʲ)/ may have been that the former were trills while the latter were flaps . /m(ʲ)/ and /ṽ(ʲ)/ were derived from an original fortis–lenis pair. Old Irish had distinctive vowel length in both monophthongs and diphthongs . Short diphthongs were monomoraic , taking up
5184-403: The Old Irish period, but merged with /u/ later on and in many instances was replaced with /o/ due to paradigmatic levelling. It is attested once in the phrase i r ou th by the prima manus of the Würzburg Glosses . /æ ~ œ/ arose from the u-infection of stressed /a/ by a /u/ that preceded a palatalized consonant. This vowel faced much inconsistency in spelling, often detectable by
5280-415: The Protoapennine B facies (southern Italy) and succeeded by the Subapennine facies of 13th-century ("Bronzo Recente"). Apennine pottery is a burnished ware incised with spirals, meanders and geometrical zones, filled with dots or transverse dashes. It has been found on Ischia island in association with LHII and LHIII pottery and on Lipari in association with LHIIIA pottery, which associations date it to
5376-487: The Riserva Naturale Statale Gola del Furlo, where Furlo Pass on the Via Flaminia is located. Both the Etruscans and the Romans constructed tunnels here. The Abruzzi Apennines, located in Abruzzo , Molise and southeastern Lazio , contain the highest peaks and most rugged terrain of the Apennines. They are known in history as the territory of the Italic peoples first defeated by the city of Rome . Coincidentally they exist in three parallel folds or chains surviving from
5472-410: The Romans used the Via Flaminia between Rome and Rimini . The montane distance between Florence in Tuscany and Bologna in Emilia-Romagna is shorter, but exploitation of it required the conquest of more rugged terrain, which was not feasible for the ancients. Railway lines were constructed over the mountains in the early 19th century but they were of low capacity and unimprovable. Since 1856,
5568-411: The Sele—joined by the Negro and Calore—on the west, and the Bradano , Basento , Agri, Sinni on the east, which flow into the gulf of Taranto; to the south of the last-named river there are only unimportant streams flowing into the sea east and west, inasmuch as here the width of the peninsula diminishes to some 64 kilometres (40 mi). The railway running south from Sicignano to Lagonegro, ascending
5664-439: The Tuscan Apennines. They extend to the upper Tiber River . The highest point is Monte Cimone at 2,165 m (7,103 ft). A separate branch, the Apuan Alps , goes southwest, bordering the coast south of La Spezia . Whether they are to be considered part of the Apennines is a matter of opinion; certainly, they are part of the Apennine System. Topographically only the valley of the River Serchio , which running parallel to
5760-501: The ancestor of all Celtic languages , and it had a lot of the characteristics of other archaic Indo-European languages. Relatively little survives in the way of strictly contemporary sources. They are represented mainly by shorter or longer glosses on the margins or between the lines of religious Latin manuscripts , most of them preserved in monasteries in Germany, Italy, Switzerland, France and Austria, having been taken there by early Irish missionaries . Whereas in Ireland, many of
5856-461: The central and eastern ranges are the valleys of Aquila and Sulmona . The chief rivers on the west are the Nera , with its tributaries the Velino and Salto, and the Aniene , both of which fall into the Tiber. On the east there is at first a succession of small rivers which flow into the Adriatic , from which the highest points of the chain are some 20 km distant, such as the Tronto , Tordino, Vomano and others. The Pescara , which receives
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#17331054831485952-480: The coast turns and exits into the Tyrrhenian Sea north of Pisa , separates the Apuan Alps from the Apennines; geologically the rock is of a slightly different composition, marble . The Roman marble industry was centered at Luna , and is now active in Carrara . As the Tuscan Apennines divide the peninsula between the Po Valley and the plains and hills of Tuscany and Lazio , transportation over them has been used to achieve political and economic unity. Historically
6048-448: The complexities of PIE verbal conjugation are also maintained, and there are new complexities introduced by various sound changes (see below ). Old Irish was the only known member of the Goidelic branch of the Celtic languages , which is, in turn, a subfamily of the wider Indo-European language family that also includes the Slavonic , Italic / Romance , Indo-Aryan and Germanic subfamilies, along with several others. Old Irish
6144-468: The deletion (syncope) of inner syllables. Rather, they originate in one of the following ways: Stress is generally on the first syllable of a word. However, in verbs it occurs on the second syllable when the first syllable is a clitic (the verbal prefix as- in as·beir /asˈberʲ/ "he says"). In such cases, the unstressed prefix is indicated in grammatical works with a following centre dot ( ⟨·⟩ ). As with most medieval languages ,
6240-411: The early 9th century. Important Continental collections of glosses from the 8th and 9th century include the Würzburg Glosses (mainly) on the Pauline Epistles , the Milan Glosses on a commentary to the Psalms and the St Gall Glosses on Priscian 's Grammar. Further examples are found at Karlsruhe (Germany), Paris (France), Milan, Florence and Turin (Italy). A late 9th-century manuscript from
6336-433: The following consonant (in certain clusters) or a directly following vowel in hiatus . It is generally thought that /e₁ː/ was higher than /e₂ː/ . Perhaps /e₁ː/ was [eː] while /e₂ː/ was [ɛː] . They are clearly distinguished in later Old Irish, in which /e₁ː/ becomes ⟨ía⟩ (but ⟨é⟩ before a palatal consonant). /e₂ː/ becomes ⟨é⟩ in all circumstances. Furthermore, /e₂ː/
6432-409: The following inventory of long vowels: Both /e₁ː/ and /e₂ː/ were normally written ⟨é⟩ but must have been pronounced differently because they have different origins and distinct outcomes in later Old Irish. /e₁ː/ stems from Proto-Celtic *ē (< PIE *ei), or from ē in words borrowed from Latin. /e₂ː/ generally stems from compensatory lengthening of short *e because of loss of
6528-470: The following inventory of long vowels: Early Old Irish /ai/ and /oi/ merged in later Old Irish. It is unclear what the resulting sound was, as scribes continued to use both ⟨aí⟩ and ⟨oí⟩ to indicate the merged sound. The choice of /oi/ in the table above is somewhat arbitrary. The distribution of short vowels in unstressed syllables is a little complicated. All short vowels may appear in absolutely final position (at
6624-423: The government, much remains to be done. They also furnish considerable summer pastures, especially in the Abruzzi : Pliny ( Hist. Nat . xi. 240) praises the cheese of the Apennines. In the forests Italian wolves were frequent, and still are found, the flocks being protected against them by large sheep-dogs; Marsican brown bears , however, which were known in Roman times, have almost entirely disappeared. Nor are
6720-429: The hills; their pottery has been found on the Capitoline Hill in Rome as well as on the islands mentioned above. The Apennines are divided into three sectors: northern ( Appennino settentrionale ), central ( Appennino centrale ), and southern ( Appennino meridionale ). A number of long hiking trails wind through the Apennines. Of note is European walking route E1 coming from northern Europe and traversing
6816-422: The junction for Foggia, Spinazzola (for Barletta, Bari, and Taranto ) and Potenza. Roman roads followed the same lines as the railways: the Via Appia ran from Capua to Benevento, whence the older road went to Venosa and Taranto and so to Brindisi , while the Via Traiana ran nearly to Troia (near Foggia) and thence to Bari. The valley of the Ofanto , which runs into the Adriatic close to Barletta , marks
6912-643: The late 19th and early 20th centuries, such as Rudolf Thurneysen (1857–1940) and Osborn Bergin (1873–1950). Notable characteristics of Old Irish compared with other old Indo-European languages , are: Old Irish also preserves most aspects of the complicated Proto-Indo-European (PIE) system of morphology. Nouns and adjectives are declined in three genders (masculine, feminine, neuter); three numbers (singular, dual, plural); and five cases (nominative, vocative, accusative, dative and genitive). Most PIE noun stem classes are maintained ( o -, yo -, ā -, yā -, i -, u -, r -, n -, s -, and consonant stems). Most of
7008-516: The lengths of the northern and central Apennines. The Grand Italian Trail begins in Trieste and after winding through the Alpine arc traverses the entire Apennine system, Sicily and Sardinia. The northern Apennines consist of three subchains : the Ligurian ( Appennino ligure ), Tuscan-Emilian ( Appennino tosco-emiliano ), and Umbrian Apennines ( Appennino umbro ). The Ligurian Apennines border
7104-422: The letter h ⟨fh⟩ , ⟨sh⟩ , instead of using a superdot ⟨ḟ⟩ , ⟨ṡ⟩ . When initial s stemmed from Primitive Irish *sw- , its lenited version is ⟨f⟩ [ ɸ ] . The slender ( palatalised ) variants of the 13 consonants are denoted with / ʲ / marking the letter. They occur in the following environments: Although Old Irish has both
7200-626: The mountains bend away to the southeast. The upper Bormida can be reached by a number of roads proceeding inland at a right angle to the coast southwest of Savona , the chief one being the Autostrada Torino-Savona. They ascend to the Bocchetta di Altare , sometimes called Colle di Cadibona , 436 m (1,430 ft), the border between the Ligurian Alps along the coast to the west and the Ligurian Apennines. A bronze plaque fixed to
7296-568: The north and the Abruzzi Apennines ( Appennino abruzzese ) in the south. It extends from Bocca Serriola pass in the north to Forlì pass in the south. The west border of the Umbria-Marche Apennines (or Appennino umbro-marchigiano )) runs through Cagli . They extend south to the Tronto River, the south border of the ONA. The highest peak, Monte Vettore , at 2,478 m (8,130 ft),
7392-630: The northern termination of the first range of the Lucanian Apennines (now Basilicata ), which runs from east to west, while south of the valleys of the Sele (on the west) and Basento (on the east)—which form the line followed by the railway from Battipaglia via Potenza to Metaponto —the second range begins to run due north and south as far as the plain of Sibari . The highest point is the Monte Pollino 2,233 metres (7,325 ft). The chief rivers are
7488-518: The older manuscripts appear to have been worn out through extended and heavy use, their counterparts on the Continent were much less prone to the same risk because once they ceased to be understood, they were rarely consulted. The earliest Old Irish passages may be the transcripts found in the Cambrai Homily , which is thought to belong to the early 8th century. The Book of Armagh contains texts from
7584-524: The only glacier in the Apennines. The eastern slopes down to the Adriatic Sea are steep, whilst the western slopes form foothills on which most of the towns of peninsular Italy are located. The mountains tend to be named after the province or provinces in which they are located; for example the Ligurian Apennines are in Liguria . The etymology most frequently repeated, because of its semantic appropriateness,
7680-563: The same amount of time as short vowels, while long diphthongs were bimoraic, the same as long vowels. (This is much like the situation in Old English but different from Ancient Greek whose shorter and longer diphthongs were bimoraic and trimoraic, respectively: /ai/ vs. /aːi/ .) The inventory of Old Irish long vowels changed significantly over the Old Irish period, but the short vowels changed much less. The following short vowels existed: The short diphthong ŏu likely existed very early in
7776-531: The sea, occurs on the east coast, extending halfway across the peninsula. Here the limestone Apennines proper cease and the granite mountains of Calabria begin. The first group extends as far as the isthmus formed by the gulfs of South Eufemia and Squillace; it is known as the Sila, and the highest point reached is 1,930 metres (6,330 ft) (the Botte Donato ). The forests which covered it in ancient times supplied
7872-408: The sound /h/ are usually written without it: a ór /a hoːr/ "her gold". If the sound and the spelling co-occur , it is by coincidence, as ní hed /Nʲiː heð/ "it is not". The voiceless stops of Old Irish are c, p, t . They contrast with the voiced stops g, b, d . Additionally, the letter m can behave similarly to a stop following vowels. These seven consonants often mutate when not in
7968-553: The state railway system, highly developed on the coastal plain, now traverses the mountains routinely through a number of railway tunnels, such as the one at Giovi Pass . The southeastern border of the Ligurian Apennines is the Fiume Magra , which projects into the Tyrrhenian Sea south of La Spezia , and the Fiume Taro , which runs in the opposite direction to join the Po. The divide between
8064-656: The three parallel chains are broken up into smaller groups; among them may be named the Matese , the highest point of which is the Monte Miletto 2,050 metres (6,725 ft). The chief rivers on the south-west are the Liri or Garigliano with its tributary the Sacco, the Volturno , Sebeto, Sarno, on the north the Trigno, Biferno and Fortore . Daunian mountains , in Apulia , are connected with
8160-771: The two upper river valleys is the Cisa Pass . Under it (in two tunnels) runs the Autostrada della Cisa between Spezia and Parma . Starting at Cisa Pass , the mountain chain turns further to the southeast, to cross the peninsula along the border between the Emilia-Romagna and Tuscany regions. They are named the Tuscan–Emilian Apennines west of the Futa Pass and the Tuscan–Romagnol Apennines east of it, or just
8256-719: The valley of the Aterno to Sulmona. In ancient times the Via Salaria , Via Caecilia and Via Tiburtina all ran from Rome to the Adriatic coast . The volcanic mountains of the province of Rome are separated from the Apennines by the Tiber valley, and the Monti Lepini , part of the Volscian chain, by the valleys of the Sacco and Liri . In the southern Apennines, to the south of the Sangro valley,
8352-518: The valley of the Negro, is planned to extend to Cosenza, along the line followed by the ancient Via Popilia, which beyond Cosenza reached the west coast at Terina and thence followed it to Reggio. The Via Herculia [ it ] , a branch of the Via Traiana , ran from Aequum Tuticum to the ancient Nerulum . At the narrowest point the plain of Sibari, through which the rivers Coscile and Crati flow to
8448-431: The very end of a word) after both broad and slender consonants. The front vowels /e/ and /i/ are often spelled ⟨ae⟩ and ⟨ai⟩ after broad consonants, which might indicate a retracted pronunciation here, perhaps something like [ɘ] and [ɨ] . All ten possibilities are shown in the following examples: The distribution of short vowels in unstressed syllables, other than when absolutely final,
8544-795: The water of which is both drunk on the spot and sold as table water elsewhere. The Apennines are home to twelve Italian national parks : the Appennino Tosco-Emiliano National Park , the Foreste Casentinesi, Monte Falterona, Campigna National Park , the Monti Sibillini National Park , the Gran Sasso e Monti della Laga National Park , the Abruzzo, Lazio and Molise National Park , the Maiella National Park ,
8640-545: The wild goats called rotae , spoken of by Marcus Terentius Varro ( Rerum rusticarum II. i. 5), which may have been either Pyrenean chamois or steinbock , to be found. Brigandage appears to have been prevalent in Roman times in the more remote parts of the Apennines, as it was until recently. An inscription found near the Furlo pass was set up in AD 246 by an evocatus Augusti (a member of
8736-567: The word-initial position. In non-initial positions, the single-letter voiceless stops c, p, and t become the voiced stops / ɡ / , / b / , and / d / respectively unless they are written double. Ambiguity in these letters' pronunciations arises when a single consonant follows an l, n, or r . The lenited stops ch, ph, and th become / x / , / f / , and / θ / respectively. The voiced stops b, d, and g become fricative / v / , / ð / , and / ɣ / , respectively—identical sounds to their word-initial lenitions. In non-initial positions,
8832-415: The year. This Campanian location article is a stub . You can help Misplaced Pages by expanding it . Apennines The Apennines or Apennine Mountains ( / ˈ æ p ə n aɪ n / AP -ə-nyne ; Ancient Greek : Ἀπέννινα ὄρη or Ἀπέννινον ὄρος; Latin : Appenninus or Apenninus Mons – a singular with plural meaning; Italian : Appennini [appenˈniːni] ) are
8928-402: Was opened after many years of construction consisting of major tunnels (the longest being the new 8.6-kilometre (5.3-mile) 'Tunel Base') and new overpasses, shortening the traveling time between Florence and Bologna by road. The Foreste Casentinesi, Monte Falterona, Campigna National Park is in the southern part of the Tuscan–Romagnol Apennines. The southern limit of the Tuscan–Romagnol Apennines
9024-482: Was quite restricted. It is usually thought that there were only two allowed phonemes: /ə/ (written ⟨a, ai, e, i⟩ depending on the quality of surrounding consonants) and /u/ (written ⟨u⟩ or ⟨o⟩ ). The phoneme /u/ tended to occur when the following syllable contained an *ū in Proto-Celtic (for example, dligud /ˈdʲlʲiɣ u ð/ "law" (dat.) < PC * dligedū ), or after
9120-574: Was relatively rare in Old Irish, being a recent import from other languages such as Latin.) Some details of Old Irish phonetics are not known. /sʲ/ may have been pronounced [ɕ] or [ʃ] , as in Modern Irish. /hʲ/ may have been the same sound as /h/ or /xʲ/ . The precise articulation of the fortis sonorants /N/, /Nʲ/, /L/, /Lʲ/, /R/, /Rʲ/ is unknown, but they were probably longer, tenser and generally more strongly articulated than their lenis counterparts /n/, /nʲ/, /l/, /lʲ/, /r/, /rʲ/ , as in
9216-570: Was used from c. 600 to c. 900. The main contemporary texts are dated c. 700–850; by 900 the language had already transitioned into early Middle Irish . Some Old Irish texts date from the 10th century, although these are presumably copies of texts written at an earlier time. Old Irish is forebear to Modern Irish , Manx and Scottish Gaelic . Old Irish is known for having a particularly complex system of morphology and especially of allomorphy (more or less unpredictable variations in stems and suffixes in differing circumstances), as well as
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