Travelodge Waterford - Cork Road(N25), Waterford, Co. Waterford
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Cork Road(N25), Waterford, Co. Waterford |
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Waterford |
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Waterford |
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Newly Approved |
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Lismore House Hotel - Main Street, Lismore, Co. Waterford
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Main Street, Lismore, Co. Waterford |
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Waterford |
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Lismore |
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3 Star |
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The Fitzwilton Hotel - Bridge Street, Waterford, Co. Waterford
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Bridge Street, Waterford, Co. Waterford |
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Waterford |
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Waterford |
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3 Star |
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Genealogy In Waterford
Waterford comes from the Norsic word, Vethrafjorthr - weather haven. Waterford bounded N by Kilkenny and Tipperary, E by Wexford, S by the sea, and W by Cork. It presents a diversity of soil and prospect, but in general is pleasant and fertile, yet in many parts mountainous and rocky; even on the sides of the mountains, however, there is good pasture for cattle. It sends 2 members to the imperial parliament. The city of Waterford (Accommodation, Waterford, Ireland) was founded by Vikings and was used as a naval base. Seven watchtowers are still visible around the city today.
Waterford’s strong sea-faring traditions meant that migration was common here long before the nineteenth century. As early as the 1650s there was a settlement from the county in Newfoundland, and strong links with Canada, and the particularly its Atlantic provinces of Newfoundland, Nova Scotia and New Brunswick, have continued down to the present.
County Facts
Land Area: 713 sq. miles
County Capital: Waterford City
Main Towns: Dungarvan, Tramore, Waterford
Pubs in Waterford
Beautifully situated on the River Suir, Waterford is one of Ireland’s leading ports and harbors. Its also Ireland’s fastest growing city and has been recognised for many years as one of the
richest cultural areas of Ireland, with many festivals, exhibitions and plays. The city is famous for its art galleries, marine museum with its Viking artifacts. There is so much to do in this county from golfing to horse riding, walking to angling. Waterford (Hotels, Waterford, Ireland) is well worth seeing, the people are exceptionally friendly and welcoming, not to forget its many fabulous pubs.
Cove bar situated on Dunmore East Road is a lively and comfortable place to unwind and relax over a drink with friends. Part of the Rustic Trail, combining the best of traditional features with modern comforts, it was originally established in the early 1800s. Whether it is for a quiet
comforting drink or to listen to traditional music, Cove bar is definitely the place to visit! You can experience a real Irish welcome in one of Irelands oldest pubs T&H Doolans that has been a licensed establishment for over 300 years. This pub is renowned for the quality and freshness of its Irish cuisine and for the best in traditional live music. While at night enjoy a creamy pint of Guinness at this award-winning pub! Henry Downes is rich in old world character and charm. Downes is famous for having blended its own range of whiskeys, so be sure to try a glass of the last remaining blend, No. 9. Madden’s Bar was first established in 1850 and is one of Lismore’s oldest and most famous establishments. The menu reveals a wonderful choice of Mediterranean foods. A popular haven for those who love a warm welcoming ambiance and enjoy the craic. 
You can either enjoy a quiet pint in the one of Waterford (Holiday Cottages, Waterford, Ireland) classical traditional pubs or if you are looking for a more exciting night out, why not venture at Waterford’s most elegant nightspots. You certainly wont be disappointed.
Antiquities In Waterford
Borlase assigns fifteen dolmens to Co. Waterford (Holiday Apartments, Waterford, Ireland) ; of these Knockeen is remarkable. Situated about a mile from Waterford city, it is of great size and in good preservation. One of the covering slabs is 13 ft. long by 8 ft. wide, and weighs about ten tons; it is supported by six uprights. This dolmen belongs to a type, fairly common in Waterford (Bed and Breakfasts, Waterford, Ireland), which has a main chamber and an
outer chamber or portico. About two miles further, on the main road, is another dolmen in the town land of Gaulstown ; it is of the same type as that at Knockeen, its cap-stone weighs about six tons. Close to this is a smaller monument of the cistvaen type, and about two miles further from these, at Ballymotey, is a remarkable pillar stone. One other large dolmen in the same district, situated in the town-land of Ballynagccragh, a mile to the west of Dunhill, may be mentioned. It is well preserved ; its cap-stone, which measures 12 by 8
Architecture In Waterford
The cathedral consists of a nave and chancel; it has a remarkable series of panels on the outer west face, containing representations of various scriptural and other scenes. The pointed east window of the chancel has been built up ; the chancel arch is a fine piece of transitional architecture. An ogham inscribed stone was found in the north wall of the chancel.
History In Waterford
The city of Waterford, in the county of Waterford, is known as Irelands First City. Founded by the Vikings in 853, it is the oldest city on the Emerald Isle.
The name Waterford (Holiday Homes, Waterford, Ireland) comes from the Viking word, Vethrafjorthr, or weather haven. The history of Waterford is that of versatility. Its location, function as a port, and continuing waterways into the heartland of the island made Waterford a prime target for Viking and Anglo-Norman invasion. In spite of centuries of foreign cultural presence and domination, an exclusively gaelic speaking presence survived and remains significant to this day, unique to the southeast of Ireland.
Co. Waterford 
A fertile and picturesque area. The River Suir forms much of the northern boundary, and the Blackwater traverses the eastern part of the county. Much of the centre and east is occupied by the lofty ridges of the Comeragh (2597 ft.) and Knockmcaldown (2609 ft.) mountains. The coast-line is extensive, and often cliff-bound. On the eastern edge, the spacious inlet of Waterford Haven forms the estuary of the Suir, Barrow, and Nore. The western limit of the coast is the smaller inlet of Youghal Harbour, through which the Blackwater reaches the ocean.
Waterford (Accommodation, Waterford, Ireland) is one of the foremost cities and ports in the southern half of Ireland. It stands on the southern bank of the Suir, 6 miles above the point where that stream pins the Barrow and 17 miles from the open sea. It has a considerable export trade, and is a railway centre of increasing importance. Part of the town, including the railway station, lies on the north or Kilkenny side of the river, across which a new ferro-concrete bridge has recently replaced the old wooden toll bridge. Portlaw stands near the Suir ; Dungarvan is at the head of the shallow Dungarvan Harbour ; Lismorc and Cappoquin are beautifully situated on the Blackwater. Tramore, on the open sea 7 miles south of Waterford, is a much-frequented watering-place
Waterford Geology
In the earliest or Ordovician period a sea with islands scattered over it occupied the British area. Near the shores sands and muds accumulated to form sandstones and shales. In the clearer waters shell-fish of obsolete types abounded, and from their dead shells were formed bands of limestones. Corals, too, were present in this sea, which goes to prove that our islands were then bathed by warmer waters than those which surround them to-day.
Great volcanic activity prevailed at this time. In Wales and Cumberland, in counties Dublin and Kildare volcanoes existed. In Waterford (Bed and Breakfasts, Waterford, Ireland) we have a grand series of volcanic rocks which burst their way through the sea-floor and mingled their lavas and ashes with the sands and muds, causing destruction among the shell-fish and coral polyps. Slates of Ordovician age are found in the vicinity of Waterford.
The Silurian period was a more peaceful time here and in the British area generally, but in the Dingle peninsula the final struggles of these plutonic forces were enacted. At Clogher Head, and along the coast north and south, the Atlantic has laid bare old lavas and ashes that were poured out upon the bottom of the sea. Now and again came paroxysmic eruptions sufficient to blot out of existence the abundant animal life of those waters, but it soon returned, and so we find sediments again forming on top of an old lava flow. In addition to this district already mentioned, Silurian rocks are also found on the plateau between the Commcragh mountains and Portlaw, in the district cast of Slieve-namann and in the region west of the Galtec mountains. The highlands west and south of the Devils Bit reveal large areas of Silurian rocks, and we find them abundantly displayed in the Arra and Silvermine mountains in Tipperary and also in the Slieve Bernagh and Slieve Aughty mountains west of the Shannon. In all cases their exposure is due to the removal by denudation of the Old Red Sandstone rocks which rested upon them
At the beginning of the glacial period the sea stood at approximately the same level as now. The annual snowfall was greater than the heat of summer could melt, and hence an ice-sheet was formed. This ice-sheet appeared much earlier in the north than in the south. Gradually, however, invasions of ice from the great Central Plain and of Irish Sea ice took place, the former finding a way at first through the passes of the hills, but afterwards mounting and overtopping most of them, the latter occupying and riding over the country along the coasts of Waterford (Accommodation, Waterford, Ireland) and Cork.
Erratics are abundant, especially in the south-west of Munstcr. These are. blocks, often of great size, that have been carried from their place of origin by ice. When they occupy precarious positions they are termed perched blocks. At Cloughlowrish Bridge, in Co. Waterford (Hotels, Waterford, Ireland), is an erratic of Old Red Sandstone resting upon an igneous rock. Near Kenmare is another of sandstone resting upon a limestone surface. The limestone has been artificially cut away all round at a remote period, so that the large erratic now rests on a slender pedestal. On Knockbrack mountain are a large number of them, and about Glengariff and westwards towards Adrigole they are perched in all kinds of positions.
At the end of the Mer de Glace, near Chamounix, are rocks which present a smooth and polished surface and on which striations are also observable. The smoothing has been effected by the sand which the ice contained in its base, and the striations are due to the chiselling action of fragments of rocks held as in a vice by the glacier as it moved forward.
One of the surest forms of evidence concerning the lotion of glaciers is to he found in such smoothed surfaces of rock upon which are striations more or less deeply incised. Some of these begin as fine lines and increase in thickness until they come to an abrupt termination. In this case the striation becomes coarser in the direction in which the. glacier was moving
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- Travelodge Waterford - Cork Road(N25), Waterford, Co. Waterford
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