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Built in 1934 by William Gray & Co in Hartlepool, the PS Tattershall Castle was one of an order for three built to operate the Humber Ferry between New Holland and Hull. They were ultimately withdrawn in 1974 and then the then world's longest suspension bridge the "Humber Bridge" which opened in 1981 crossed the Humber Estuary at the same point. Following withdrawal the old paddle steamer was towed to London in 1976. Initially she was the venue for a floating art gallery, however it probably says something about the British attitude to drink that she soon became a very successful pub and restaurant.
If you look closely at the centre of the boat you will be able to see that a viewing gallery has replaced the original bridge. No doubt that can accommodate more paying punters. Her capacity as a ferry was 1,050 but quite how many she is licensed to hold these days I don't know.
Of the other two paddle steamers withdrawn at the same time, the PS Lincoln Castle was scrapped as recently as 2010 after it had effectively rotted away at its birth within the Alexandra Dock in Grimsby. The third example the PS Wingfield Castle has been a little luckier. It now has a home within the Hartlepool Maritime Museum and is shortly due to benefit from a refurbishment.
Stagecoach has almost all but finished with its massive fleet of PS`s... odd pockets of them remain but not for much longer. It would be perhaps nice if they realised the significance of R792DHB down in Wales as the last step entry / PS for Stagecoach.......This is 20926 R926XVM seen operating the 07.55 Fiscavaig - Portree in September 2012. The service runs once in a morning and reverse at night serving the very isolated West fork of the island where the vehicle lives at an outstation near the drivers house. Stagecoach through no failing of their own have lost much work on the island of late and the operation has been trimmed back to secure to remaining work, hopefully the situation will improve again given time.
The lovely PS Waverley was sadly in the news recently when it was in a collision with a shore installation, I believe.
I remembered that I had re-worked an image I had taken back in September 2017 when PS Waverley visited Harwich.
This is the re-worked image I made in January 2018.
Copyright photo PS
Old slide.
Castle Coombe in the Brook Valley, Cotswolds, England.
Once a weaving centre.
Enlarge
Click diagonal arrows upper-right.
PS Waverley is the last seagoing passenger-carrying paddle steamer in the world. Built in 1946, she sailed from Craigendoran on the Firth of Clyde to Arrochar on Loch Long until 1973. Bought by the Paddle Steamer Preservation Society (PSPS), she has been restored to her 1947 appearance and now operates passenger excursions around the British coast.
Since 2003 Waverley has been listed in the National Historic Fleet by National Historic Ships UK as "a vessel of pre-eminent national importance". She appeared in the 2011 film Sherlock Holmes: A Game of Shadows.
I'm not sure exactly where this is but I spotted it somewhere between Cowes and Yarmouth when we were on our way to pick up the passengers who had gone to explore Yarmouth. There was some mention of it on the PA system as we went past, but I couldn't hear it clearly.
Olanda...Tulipani !
Parco Keukenhof....
Fotocamera Nikon D700
Esposizione0,013 sec (1/80)
Aperturef/8.0
Lente105 mm Lente 105 Macro.
ISO800
Exposure Bias0 EV
The Emmyloo and the Pevensey were used in the television series “All the Rivers Run” as the Providence and Philadelphia respectively.
The Murray River Flag is flown from paddle steamers and other vessels in the Australian States of New South Wales, Victoria and South Australia that ply the waters of the Murray-Darling river system. Little is known about the flag's early history but it may have originated as far back as 1850 when the formation of the Murray River League was announced.
Lofoten is an archipelago and a traditional district in the county of Nordland, Norway. Though lying within the Arctic Circle, the archipelago experiences one of the world's largest elevated temperature anomalies relative to its high latitude.
Lofoten (Norse Lófót) was originally the old name of the island Vestvågøya. The first element is ló (i.e., "lynx") and the last element is derived from Norse fótr (i.e., "foot"), as the shape of the island must have been compared with a foot of a lynx. (The old name of the neighbouring island Flakstadøya was Vargfót, "the foot of a wolf", from vargr "wolf". See also Ofoten.)
"There is evidence of human settlement extending back at least 11,000[ yrs in Lofoten, and] the earliest archaeological sites ... are only about 5,500 yrs old, at the transition from the early to late Stone Age." Iron Age agriculture, livestock, and significant human habitation can be traced back to ~250 BC.
The town of Vågan (Norse Vágar) is the first known town formation in northern Norway. It existed in the early Viking Age, maybe earlier, and was located on the southern coast on eastern Lofoten, near today's village Kabelvåg in Vågan municipality. However, the Lofotr Viking Museum with the reconstructed 83-meter-long longhouse (the largest known) is located near Borg on Vestvågøy, which have many archeological finds from the Iron Age and Viking Age.
The islands have for more than 1,000 years been the centre of great cod fisheries, especially in winter, when the cod migrates south from the Barents Sea and gathers in Lofoten to spawn. Bergen in southwestern Norway was for a long time the hub for further export south to large parts of Europe, particularly so when trade was controlled by the Hanseatic League. In the lowland areas, particularly Vestvågøy, agriculture plays a significant role, as it has done since the Bronze Age.
Lofotr was originally the name of the island of Vestvågøy only. Later it became the name of the chain of islands. The chain of islands with its pointed peaks looks like a lynx foot from the mainland. In Norwegian, it is always a singular. Another name one might come across, is "Lofotveggen" or the Lofoten wall. The archipelago looks like a closed wall when seen from elevated points around Bodø or when arriving from the sea, some 100 km long, and 800-1,000 m. high.
In 1941 the islands were raided by British Commandos during Operation Claymore in March and a subsequent diversionary attack to support the Vaagso raid in December.
Lofoten is located at the 68th and 69th parallels north of the Arctic Circle in North Norway. It is well known for its natural beauty within Norway. Lofoten encompasses the municipalities of Vågan, Vestvågøy, Flakstad, Moskenes, Værøy, and Røst. The principal islands, running from north to south, are
Southern tip of Hinnøya.
Southern 60% (approx.) of Austvågøy (526.7 km² in total 68°20′N 14°40′E),
Gimsøy (46.4 km² 68°18′N 14°11′E),
Vestvågøy (411.1 km² 68°10′N 13°45′E),
Flakstadøya (109.8 km² 68°5′N 13°20′E),
Moskenesøya (185.9 km² 67°55′N 13°0′E),
whilst further to the south are the small and isolated islands of Værøy (67°40′N 12°40′E) and Røst (67°37′N 12°7′E). The total land area amounts to 1,227 km², and the population totals 24,500. Many will argue that Hinnøya, the northern part of Austvågøy and several hundred smaller islands, skerries and rocks to the east of Austvågøy are also part of the Lofoten complex. Historically the territorial definition of Lofoten has changed significantly. Between the mainland and the Lofoten archipelago lies the vast, open Vestfjorden, and to the north is Vesterålen. The principal towns in Lofoten are Leknes in Vestvågøy and Svolvær in Vågan. The Lofoten Islands are characterised by their mountains and peaks, sheltered inlets, stretches of seashore and large virgin areas. The highest mountain in Lofoten is Higravstinden (1,161 m / 3,800 ft) in Austvågøy; the Møysalen National Park just northeast of Lofoten has mountains reaching 1,262 meters. The famous Moskstraumen (Malstrøm) system of tidal eddies is located in western Lofoten, and is indeed the root of the term maelstrom.
The sea is rich with life, and the world's largest deep water coral reefis located west of Røst. Lofoten has a very high density of sea eagles and cormorants, and millions of other sea birds, among them the colourful puffin. Otters are common, and there are moose on the largest islands. There are some woodlands with Downy birch and Rowan. There are no native conifer forests in Lofoten, but some small areas with private spruce plantations. Sorbus hybrida ("Rowan whitebeam") and Malus sylvestris occur in Lofoten, but not further north.
The animals mistaken as the extinct Great Auk turned out to be some of the nine King penguins released around Norway’s Lofoten Islands in August 1936, there until at least 1944.
Winter temperatures in Lofoten are very mild considering their location north of the Arctic Circle – Lofoten has the largest positive temperature anomaly in the world relative to latitude. This is a result of the Gulf Stream and its extensions: the North Atlantic Current and the Norwegian Current. Røst and Værøy are the most northerly locations in the world where average temperatures are above freezing all year. May and June are the driest months, while October has three times as much precipitation. The warmest recording in Svolvær is 30.4°C (87°F).
Strong winds can occur in late autumn and winter. Snow and sleet are not uncommon in winter, the mountains can have substantial amounts of snow, and in some winters, avalanches might come down from steep mountain slopes. Two of the top ten deadliest rainstorms ever recorded passed through Lofoten.
In Svolvær, the sun is above the horizon continuously ("midnight sun") from 25 May to 17 July, and in winter the sun does not rise from 4 December to 7 January. In Leknes, the sun is above the horizon from 26 May to 17 July, and in winter the sun does not rise from 9 December to 4 January.
The temperature in the sea has been recorded since 1935. At 1 m depth in the sea near Skrova, water temperatures varies from a low of 3°C in March to 14°C in August. Some years peaking above 17°C. November is around 7-8°C. At a depth of 200 m the temperature is near 8°C all year.
Mountaineering and rock climbing
Lofoten offers many rock climbing and mountaineering opportunities. It has 24 hours of daylight in the summer and has Alpine-style ridges, summits and glaciers, but at a height of less than 1,200 metres. The main centre for rock climbing is Henningsvær on Austvågøya.
The main areas for mountaineering and climbing are on Austvågøya and Moskenesøya. Moskenesøya is the most complete area for climbing. For more information, see the books by Dyer and Webster.
Surfing
Unstad is one of its better known locations for surfing.
Cycling
There is a well marked cycling route that goes from Å in the south and continues past Fiskebøl in the north. The route is part public road, part cycle-path with the option to bypass all of the tunnels by either cycle-path (tunnels through mountains) or boat. Traffic is generally light, although in July there may be a lot of campervans. Some of the more remote sections are on gravel roads. There is a dedicated cycling ferry which sails between Ballstad and Nusfjord, allowing cyclists to avoid the long, steep Nappstraum tunnel. The route hugs the coastline for most of its length where it is generally flat. As it turns inland through the mountain passes there are a couple of 3-400 meter climbs.
The Lofoten Insomnia Cycling Race takes place every year around midsummer, possible in the midnight sun, but surely in 24-hr daylight, along the whole Lofoten archipelago.