View allAll Photos Tagged Include
Viajes al Otro Mundo. Ciclo de Aventuras Oníricas de Randolph Carter
(Travel to the Other World. Cycle of Dream Adventures of Randolph Carter)
Alianza Editorial / Libro de Bolsillo
Alliance Publishing / Paperback
2003
Includes A Través de las Puertas de la Llave de Plata (Through the Gates of the Silver Key) by H. P. Lovecraft and E. Hoffmann Price
From the August 2016 return trip to Siem Reap and the Angkor complex:
I love the Angkor complex, Siem Reap, and the Cambodian people so much that I returned again for about a week to photograph as much of the “non-major” sites as I could. Some of them are slightly far from Angkor Wat (by that, I mean to say more than 10 kilometers away), and usually require a little more money to get to. Also, some of the sites (Beng Mealea, Phnom Kulen) are not included in the Angkor ticket price and have an additional admission fee.
I don’t know if there’s a set number of how many sites belong in the Angkor complex, though I’m sure it would vary. (Do you only count the major sites like Angkor Wat, Bayon, Ta Prohm? Do you add the sites that aren’t included in the standard “Angkor Pass,” but are clearly of the same era? Do you include sites that aren’t even named (as are one of the sites in this series)? All in all, I’ll put a very rough number at…50 sites in the Siem Reap area, and that includes the sites that are about 100 km away. Of those, I would say I’ve been to all but 5-10 now. All are included here with the exception, obviously, of the sites that I didn’t visit. (Off the top of my head, I can say they include Koh Ker & that respective group, which is about 120 km ENE of Siem Reap; Phnom Krom, one of the three “mountains” with temples; Ta Prohm Kel; and Mangalartha.)
In practical terms, I’m afraid that with the volume of shooting (about 1,500 frames in the past 7 days), photos will start to look redundant to those who don’t have the same interest in ancient/historical architecture or Angkor as I do. That being said, there are a few things besides temples here. The Old Market area (now Night Market/Pub Street) is represented – a little – and Phnom Kulen has a pretty nice waterfall which is also in this series. Also, I tried to catch a few people in here, though didn’t get as many as I would’ve liked.
I had my friend Mao (tuktuk driver) take me around for 5 of these 7 days this time around. As I mentioned last time, he may cost a little more than what you can arrange through a hotel/guesthouse, but he’s well worth the money (and, in the grand scheme of things, not too expensive; I paid less than $200 for the five days, two of which were “long” trips). He loves his country and heritage, he knows what he’s showing you, he’s flexible, he gives you enough ice water to keep you hydrated, and he’s just a good guy. (He even bought me a birthday cake for cryin’ out loud…) Anyway, I highly recommend Mao. You can find him here: www.facebook.com/mao.khvan (or on Trip Advisor: www.tripadvisor.com/Attraction_Review-g297390-d10726821-R... )
Now that shameless plugs and other assorted rhetoric are out of the way, it’s time to get on to the temples, ruins, and other miscellany.
The fifth day (and last time I’ll see Mao unless I go back to Siem Reap again) started just the same as my birthday. Chhiengmai brought me a ham & cheese omelette at the hotel, then Mao picked me up and off we went.
Following the same route to Banteay Kdei, we took a right and headed out on the grand loop. The first stop was at Pre Rup, which I’d seen in May, but wanted to photograph again this time around. I love the May shots because it’s in afternoon light, so there are some nice silhouette shots in there. This time, however, was early morning. We didn’t shoot as extensively as we did in May; only staying on the eastern side of the temple and not ascending it. Still, it’s a rather striking temple and worth seeing, even with the restoration that looks as if it hasn’t been touched since May – and didn’t look like it was being touched then, either.
Pre Rup is on the southeast corner of the Grand Loop. From there, continue north. Right before you reach East Mebon is a road going east. (This is the road that would lead you to Banteay Samré if taken straight, or Banteay Srei, Phnom Kulen, and Kbal Spean, if you turn left at the first intersection about 1 kilometer east from here.)
Our second destination, though, was Phnom Bok. To reach here, continue east on the aforementioned road – pass Banteay Samré – taking the first left, then continuing north about 5-10 minutes. All in all, it’s about 20 minutes from the Grand Loop road.
Having seen snow-capped mountains enough in my life, I chuckle to call these mountains instead of hills. However, Angkor is in a large plain, as you can see in these pictures, so any hill looks like a mountain. In the same breath, these aren’t baby hills.
Mao’s wife and daughter stayed with the tuktuk while we went clambering up the hill. I was giving Mao a good ribbing about him not being my friend for making me climb a mountain in tropical heat, but it really wasn’t too bad. He said, “there are only 100 stairs to the top!” I laughed and said there’s no way that’s a mountain then. We walked up a hill for about five minutes before getting to the bottom of the staircase on the south side of the mountain that goes to the summit. He still insisted it was only 100 steps. I counted, just for fun. Turns out, there are 626 steps, give or take one, to the top of the hill and, even when you get to the top, you still have to climb up…a little farther.
As I mentioned, though, it wasn’t a bad climb. The first 400 or so steps are forested, so you’re in shade, though it’s hot and humid. After that, the views of the surrounding plains open up which are quite nice. Mostly, you can see to the south or southeast. I couldn’t see any of the main temples which would be southwest from here. (I couldn’t see them from the peak when looking southwest, though, either…)
At the top of Phnom Bok, there’s a little shelter/rest area where you can sit and buy ice cold drinks. There’s a new Hindu temple up there, and also the ruins of an Angkor-era temple. Sadly, there are also remnants of the Khmer Rouge era, too; machine gun mounts and the like, surrounding the temple.
After 30-45 minutes on the mountaintop, we went back down and I was glad to have a rest in the tuktuk while we made our way back to the Grand Loop. It was a good chance to rest up and enjoy the scenery (in addition to waving like a fool at every passerby as I’m wont to do).
Upon returning to the Grand Loop road, we made a quick right heading north for about 200 meters to the East Mebon. In May, we stopped here, but didn’t do anything other than climb the main stairs, take a few shots, and head off to lunch. (We were tired by that point.)
Because of that, I told Mao I wanted to take time to extensively go around the East Mebon. It’s a surprisingly nice temple mount. (I don’t know how the West Mebon compares; unlike this one, there is still water in the west baray, and I didn’t go out there.) All told, Mao and I wandered our separate ways here for about half an hour or so. I got back to the tuktuk right before one of the daily summer downpours. Mao was stuck out in the rain, but had my backpack, P&S, and umbrella, so was fine.
After a 5-10 minute rest, a Coke and a smile later, the four of us went back on our way around the Grand Loop continuing clockwise. We bypassed Ta Seo (which I’d shot well enough in May) and stopped for a very quick shoot at Prasat Krol Ko. This is a very small temple built in the late 12th and early 13th century by Jayavarman VII. It looks like many of the other temples, so most don’t stop here as it’s not terribly interesting. It’s a temple surrounded by two concentric enclosures, in the Bayon style, and rather small. However, it’s near Neak Pean and Preah Khan, so there’s no reason not to stop. This is a Hindu (I believe) temple, as it’s named/dedicated to a cow. I enjoyed it.
The next stop – Neak Pean – was less than two minutes down the road. (Again, no reason not to stop at both. Neak Pean (sometimes spelled “Neak Poan” and pronounced “neek poh-an”) is architecturally different than most of the other sites, as is the setting. Neak Pean is a cruciform arrangement of ponds that centers on a sanctuary tower on a circular island in the middle. Currently, access is limited and you can’t go all the way around it. You approach from the north over a boardwalk – this crosses over the Jayatataka baray, which offers some nice panoramic views of Phnom Bok about 5 kilometers to the east – and finally arrive at the north end of the monument. You can walk around either side to the eastern and western corners, but can go no farther. There are (were) four different sculpted animals on each of the four small ponds around the sanctuary. Eavesdropping a tour guide, he said the four ponds represent earth, air, fire, and water. I had read somewhere what the four animals were, but can’t seem to find that information now. I was very pleased with this stop, too, mainly because it offered a little variety.
After the nice stroll over the boardwalk back to the tuktuk, we continued heading west. At the turn off for Preah Khan (which I skipped this time since we spent a bit of time here in May), there are also two other nearby, rarely visited temples: Banteay Prei and Prasat Prei. These are immediately north of Preah Khan on the outside of the Loop road. Preah Khan is about 200 meters south on the inside of the loop. Neither of these two temples are listed in either LP Cambodia or my Ancient Angkor guidebook, so I unfortunately can’t tell you a thing about them, but would venture to say they were probably built by Jayavarman VII…but, that’s pure conjecture. They were both rather nice to see, and in a fair state of decomposition, so it lent to nice photography. As they are so close to Preah Khan, again…I don’t see why you wouldn’t visit here. You can see both temples in about 20 minutes without going out of your way to do so.
The next stop on today’s private tour is Krol Romeas. This is a very unassuming structure that is less than five minutes outside the North Gate of Angkor Thom. I’m a little confused about what “romeas” means. At first Mao’s wife told me it meant sheep. Then I believe she said it meant hippopotamus. Either way, this structure was an animal pen for one of those. Given the size and depth, I’ll say hippo enclosure is probably correct. Currently, it’s just a very nice setting in the forest. It’s a round enclosure about 20 meters in diameter, just east of the Grand Loop road.
After Krol Romeas, our next stops were the remaining (for me) gates of Angkor Thom: first, the North Gate for a very quick shoot, then down to Bayon and due west on a relaxing, rarely traveled road to the West Gate. The West Gate is supposed to be the one in the most pristine (unrestored) state, though I thought it looked fine. The setting was good.
By this time, it was getting to be early afternoon, probably around 4:00. The next – and last – stop of the day was south of town, away from the majority of Angkor sites. Going south from the Night Market area of Siem Reap along the river, there are two sites of interest: The main one Is the third of the “major” hills – Phnom Krom. This is supposed to be a nice place to see the sunset. However, from having climbed Phnom Bok earlier in the day, I wasn’t inclined to go here, though it was on my original “wish list” that I gave to Mao. Instead, we just went to the other temple in the area: Wat Athvea (sometimes also written Athwea). This is a very tranquil temple and is great in the late afternoon. It’s attached to a functioning monastery, but isn’t noisy. There is a pagoda built on the site of an ancient temple here. What you see here is a 12th century Hindu temple. There is a cemetery adjacent, but that’s not included in this set.
Upon finishing for the day, Mao dropped me back off at my guesthouse. This would be the last time I saw Mao on this trip, though his wife and daughter insisted on taking me to the airport on Tuesday, so I would see them one more time. I’ve said it before, and I’ll say it again. Mao’s a good man (Cambodian Mao, that is…)
As always, I hope you enjoy this set. I appreciate you taking time to look. If you have any questions, please feel free to send me a message or leave it via comment.
The northern gannet (Morus bassanus) is a seabird and the largest member of the gannet family. It has the same colours as the Australasian gannet and is similar in appearance. Nesting in colonies as large as 60,000 pairs on both sides of the north Atlantic this bird undertakes seasonal migrations and is a spectacular high-speed diver.
Old names for the northern gannet include solan and solan goose.
Adults are 81–110 cm (32–43 in) long, weigh 2.2–3.6 kg (4.9–7.9 lb) and have a 165–180 cm (65–71 in) wingspan.
Before fledging, the immature birds (at about 10 weeks of age) can weigh more than 4 kg (8.8 lb). Each wing measures between 47 and 53 cm (19 and 21 in) when outstretched and the beak measures between 9 and 11 cm (3.5 and 4.3 in) (measured from the head). The two sexes are a similar size.
The plumage of the adults is white with dark wing tips, with colours that range from brown to black. The colour of the head, cheeks and side of the neck depends on the season and the individual; during breeding, the head and neck are brushed in a delicate yellow, although this colouring may not be evident in some individuals. The feathers are waterproof, which allows the birds to spend long periods in water. A water-impermeable secretion produced by a sebaceous gland covers the feathers and the birds spread it across their body using their beak or their head. The eye is light blue, and it is surrounded by bare, black skin, which gives the birds their characteristic facial expression.
Young birds are dark brown
Fledglings are brown with white wing tips. They have white spots on their head and on their back and a v-shaped white area underneath. The plumage of one-year-olds can be almost completely brown. In the second year the birds’ appearance changes depending on the different phases of moulting: they can have adult plumage at the front and continue to be brown at the rear. They gradually acquire more white in subsequent seasons until they reach maturity after five years.
Newborn chicks are featherless and are dark blue or black in colour. In the second week of life they are covered in white down.[8] From the fifth week they are covered in dark brown feathers flecked with white.
Their beak is long, strong and conical with a slight downward curve at the end. The front part has a sharp edge. In adults, the beak is blue-grey with dark grey or black edges. It is brownish in immature birds.
The northern gannet’s eyes are large and point forwards, and they have a light blue to light grey iris surrounded by a thin black ring. The four toes of their feet are joined by a membrane that can vary from dark grey to dark brown. There are yellow lines running along the toes that continue along their legs; these lines probably have a role in mating. The rear toe is strong and faces inwards allowing the birds to firmly grip onto vertical cliff faces.
When feeding, these birds are spectacular high-speed divers. They can locate their prey from heights of up to 45 m (148 ft), but they normally search from a height of between 10 and 20 m (33 and 66 ft). When they see a fish they will dive into the water. They dive with their bodies straight and rigid, wings tucked close to the body but reaching back, extending beyond the tail, before piercing the water like an arrow. They control the direction of the dive using their wings. Just as it is going to hit the water a bird will fold its wings against its body. A bird’s head and neck are stretched out in front of the body and the beak is shut. Birds can hit the water at speeds of up to 100 km/h (62 mph). This allows them to penetrate 3–5 m (10–16 ft) below the surface, and occasionally they will swim down to 12–15 m (40–50 ft).
They usually push their prey deeper into the water and capture it as they return to the surface. When a dive is successful, gannets swallow the fish underwater before surfacing, and never fly with the fish in their bill. Larger fish are swallowed headfirst, smaller fish are swallowed sideways or tail first. The bird’s subcutaneous air bags aid their rapid return to the surface.
Their white colour helps other gannets to identify one of their kind and they can deduce the presence of a shoal of fish by this diving behaviour; this in turn facilitates group foraging, which makes capturing their prey easier. Northern gannets also forage for fish while swimming with their head under water.
Some studies have found that the duration and direction of flights made while foraging for food are similar for both sexes. However, there are significant differences in the search behaviour of males and females. Female northern gannets are not only more selective than males in choosing a search area: they also make longer and deeper dives and spend more time floating on the surface than males.[
Scottish kilt provides a wide range of Kilt Accessories which includes Fly Plaid, Pin, Socks, Shoes & Flashes
Fly Plaid
Those who wear kilt outfits know that there are a number of different aspects to the kilts that tie them together and give them a completed look. One of those things is plaid flies. Fly Plaid reaches far past Scottish heritage, extending as far back as the Roman times, but they have become an integral part of kilt-wearing culture. At Scottish Kilt Shop, we offer a huge assortment of kilt flies for you to choose from, ranging from all different sorts of tartan colors, so you can find the one that best suits your style. Each one of the kilt flies is made out of the highest quality materials that are sure to last for years. You can get a full- or mini-sized version.
Kilt Pins
Look ultra stylish the next time you step out of the house in your favorite kilt ensemble with these Kilt Pin from Scottish Kilt Shop! We know that your individuality is important to you, and that is why we offer so many choices of kilt pins to take home with you. While our pins are certainly stylish and will have you standing out in the crowd of kilt wearers around you, they also serve their practical purpose in that they keep the bottom of your kilt closed and looking nice and neat. Choose from a selection of kilt pins including the Lion Rampant , the Scottish thistle pin, Masonic kilt pin, silver chrome Celtic cross and many other fashionable pins that your heart may desire.
Kilt Flashes
Find your new favorite hose socks accessories here at Scottish Kilt Shop! No matter what style of kilt you enjoy wearing, you can find a flash that will match your attire. Our Kilt flashes consist of a wide selection of different tartan styles for you to choose from, from the darkest of blacks to the most vibrant of greens and even the sunny MacLeod of Lewis tartan . Perfect for any size of kilt hose, these stylish flashes are ready to spice up your favorite kilt look. While they are great decorative garments, our flashes also serve their practical purpose of ensuring that your kilt hose does not sag or otherwise slip down from the space around your leg in which they are supposed to fit.
Kilt Socks
When it comes to choosing pairs of hose to go along with your kilts, you need something heavy weight and durable, and that is exactly what you will find here at Scottish Kilt Shop. We offer a number of high quality kilt socks that promise to retain their color, even through several washes. The kilt hose features a premium ribbed patterning that runs throughout the whole length of the socks. They are ultra soft and won’t cause itching, making them perfect for wearing for long periods of time, even when the weather is warm and humid. Kilt hose styles available at Scottish Kilt Shop are available in colors that are perfectly suited for absolutely any style of kilt, making our store your premier shop for your kilt accessories .
Kilt Shoes
When it comes to wearing a full kilt dress, attention should be paid as much to the rest of the outfit as it is to the kilt itself. With these Oxford Kilt Shoes, you can feel confident knowing that you are wearing only the most in-style and high-quality oxford shoes with your kilts, helping you not only look your best but also feel your best. The Oxford Shoes here at Scottish Kilt Shop are made in the traditional oxford style and are crafted out of 100 percent natural leather, giving you the assurance you need to know they will last for many wears to come. Every style of Oxford Shoes we sell are made with classic lacing patterns that allow you to fit into the traditional lace-up styles of kilt wearing. The shoes are designed for wear at formal events and will keep you comfortable and looking your best all night long.
The Beacon opened to the public on 28 March 2013
The Beacon is 80ft high and has seven floors
There are 132 steps (and a lift!)
The Beacon took 12 months to build
It includes a two-storey café with open terraces offering 360 degree views
There are four floors of business space
A sky lounge for meetings and events
The top floor is an open roof terrace offering fantastic views all year round
Eco features include an energy efficient heat recovery system and solar reflective glazing
The Beacon is included in a LED lights installation which runs the full length of the seafront to the bandstand
The project is part funded by the Council, One North East and the European Regional Development Fund 2007-2013.
Redcar is a seaside town on the Yorkshire Coast in the Redcar and Cleveland unitary authority in the ceremonial county of North Yorkshire, England. It is located 7 miles (11 km) east of Middlesbrough.
The Teesside built-up area's Redcar subdivision had a population of 37,073 at the 2011 Census. The town is made up of Coatham, Dormanstown, Kirkleatham, Newcomen, West Dyke, Wheatlands and Zetland.
It gained a town charter in 1922, from then until 1968 it was governed by the municipal borough of Redcar. Since the abolition of County Borough of Teesside, which existed from 1968 until 1974, the town has been unparished.
Redcar occupies a low-lying site by the sea; the second element of its name is from Old Norse kjarr, meaning 'marsh', and the first may be either Old English (Anglo-Saxon) rēad meaning 'red' or OE hrēod 'reed'. The town originated as a fishing hamlet in the 14th century, trading with the larger adjacent hamlet of Coatham. Until the mid-19th century it was within the parish of Marske-by-the-Sea – mentioned in the Domesday Book of 1086.
Numerous ships have foundered off the Redcar coastline and many of their wrecks still exist. The Zetland is the world's oldest surviving lifeboat. It was built by Henry Greathead of South Shields and is housed in a volunteer-led sea-front museum. The lifeboat was first stationed at Redcar in 1802.
As seaside holidays became fashionable in the early 19th century, Redcar's facilities expanded. By 1841, Redcar had 794 inhabitants. In 1846, work was completed on the Middlesbrough and Redcar Railway and the presently named Redcar Central station, created to attract tourism and trade.
Redcar's population expansion corresponded with Middlesbrough's, with the discovery in 1850 of iron ore in the Eston area of Cleveland Hills. Redcar prospered as a seaside town drawing tourists attracted by eight miles of sands stretching from South Gare to Saltburn-by-the-Sea.
Plans for a pier were drawn up in 1866, but lay dormant until prompted by the announcement of plans to build a pier at Coatham in 1871. Coatham Pier was wrecked before it was completed when two sailing ships were driven through it in a storm. It had to be shortened because of the cost of repairs and was re-opened with an entrance with two kiosks and a roller-skating rink on the Redcar side, and a bandstand halfway along its length.
Redcar Racecourse was created in 1875. Redcar Pier, another pier as well as Coatham Pier, was built in the late 1870s. In October 1880 the brig Luna caused £1,000 worth of damage to this pier. In New Year's Eve 1885 SS Cochrane demolished the landing stage. and in 1897 the schooner Amarant went through the pier. A year later, its head and bandstand burned down.
In October 1898 the Coatham Pier was almost wrecked when the barque Birger struck it and the pier was thereafter allowed to disintegrate. An anchor from the Birger can be seen on the sea front pavement close to the Zetland Lifeboat Museum.
In 1907 a pavilion ballroom was built on Redcar Pier behind the entrance kiosks and in 1928 it was extended. A glass house for concerts was added to the remains of Coatham Pier's entrance. The presently named Redcar East railway station was built in 1929.
In 1929 Coatham Pier's glasshouse was replaced by the New Pavilion theatre. After the war, comedian and entertainer Larry Grayson coined his catchphrase "Shut that Door!" while performing there, since the stage door was open to the cold North Sea breeze.
Redcar Pier was deliberately breached (sectioned) in 1940 to prevent its use by enemy invasion forces. As a result of sectioning, damage by a mine explosion and deterioration it was never reconnected and instead allowed to become even more dilapidated.
In 1964 the New Pavilion Theatre was transformed into the Regent Cinema. The Redcar Pier pavilion continued in use after the war but storm damage led to it being declared unsafe and it was demolished in 1980–1981.
The town's main employers in the post-war era were the nearby Teesside Steelworks at Warrenby, founded by Dorman Long in 1917, and the ICI Wilton chemical works. The steel produced at Dorman Long was used to build the Sydney Harbour Bridge, Tyne Bridge, Auckland Harbour Bridge and many others. Both the Warrenby and Lackenby sites became part of Tata Steel when Corus was taken over in 2007, but continued to trade under the Corus name until at least February 2008. SSI bought the plant from Tata Steel in February 2011, for £320 million.
After a two-year hiatus following the mothballing of the plant in February 2010, steel was once again being made at Redcar. The Thai owners of the former Corus Plant at Lackenby, Sahaviriya Steel Industries (SSI), re-ignited the blast furnace, one of the largest in Europe, on 15 April 2012.
On 18 September 2015, production was paused due to the decline in steel prices. On 28 September 2015, the plant was "mothballed" amid poor steel trading conditions across the world and a drop in steel prices. On 2 October, the owner of the site, SSI UK, entered liquidation. On 12 October 2015 the administrator announced that there was no realistic prospect of finding a buyer and the ovens would be extinguished.
Wards periodically change, as of 2018 the town is made up of Coatham, Dormanstown, Kirkleatham, Newcomen, West Dyke, Wheatlands and Zetland. Redcar is made up of areas that do not lend their name to a ward: Warrenby, Lakes Estate, Redcar East, The Ings, Ings Farm, Mickledales and Westfield.
On 5 May 2011 Redcar elected its councillors to Redcar & Cleveland Borough Council. There was a by-election on 18 November 2011 for two vacant seats in the Zetland ward, held onto by the Liberal Democrats, and on 19 January 2012 there was a by-election for a vacant seat in Newcomen ward subsequently gained by Labour from the Liberal Democrats.
Redcar was formerly a township and chapelry in the parishes of Marske and Upleatham, in 1866 Redcar became a separate civil parish. A district in Redcar's name formed in 1885. Three years after the district was formed, the centuries-old Yorkshire authority was replaced by the North Riding of Yorkshire county council. The district became an urban district in 1894.
The settlement's town charter occurred in 1922, the district was able to be styled as a municipal borough and the settlement as a town. On 1 April 1974 the parish was abolished and merged with Teesside and Marske. On 1 April 1968 the municipal borough was abolished merged into the County Borough of Teesside, part also went to Saltburn and Marske by the Sea Urban District. This removed it from the administrative county however still ceremonially in the area. In 1961 the parish had a population of 31,460.
The 1974 reform created the non-metropolitan County of Cleveland, under the Langbaurgh non-metropolitan district. The county was also inserted into the North East England region. After further changes in 1996, the district became a unitary authority called Redcar & Cleveland in the ceremonial county of North Yorkshire, the county straddling two regions of England.
The North East England region was sub-divided into combined authorities, in May 2017 the Tees Valley area voted for their first mayor. The Conservative candidate, Ben Houchen, won the election and is now in his second term.
From 1987 to 2001, the local Member of Parliament (MP) was Mo Mowlam. From 2001 to 2010 the MP was Vera Baird. In the 2010 general election there was a swing to the Liberal Democrats with Ian Swales being elected. But, in the 2015 general election, Anna Turley, a Labour MP, won back Redcar. In the snap 2017 general election, Anna Turley held onto that seat. In the general election on 12 December 2019, Anna Turley lost her seat to Conservative candidate Jacob Young with a majority of 3,527 votes. Young becomes the third conservative MP to represent Redcar, the first being Royal Naval Commander Robert Tatton Bower 1931 to 1945 and Scarborough businessman Wilfred Proudfoot between 1959 and 1964 when Redcar was part of the Cleveland constituency.
The Palace Hub, on the beach front, was built by Redcar and Cleveland Council for the creative and cultural sector of the town. An art gallery and business start up centre are located in the building. The main library is in the Redcar Heart building in the centre of the town and there is a long-standing Redcar Literary Institute, which was founded in 1896.
Redcar is home to the Tuned In! Centre, which opened in 2011 and overlooks the sea front. The multi purpose venue hosts live music as well as creative workshops for young people. The annual event Clubland on the Beach, which showcases dance acts attracting visitors from across the country, has been held at Majuba Road in Redcar for the past three years.
The town has had several parks built for tourism: Coatham Enclosure, Locke Park, Zetland Park, Lily Park, an Amusement Park with a roller coaster, and a small sea front park known locally as Titty Bottle Park. The Amusement Park near the railway closed decades ago, and Titty Bottle Park was absorbed into the redeveloped sea front around Redcar Beacon.
At the west end of High Street is a Grade II listed clock tower, a memorial to King Edward VII who was a regular visitor to Redcar. The tower has now been refurbished.
Construction of the Redcar Beacon started in 2011. In 2013, when the building had been completed, it was nominated for the Building Design Carbuncle Cup for worst new building. It came third in the whole of the UK. In December 2015, the Beacon was damaged by winds from Storm Desmond, with several large pieces of panelling falling onto the beach below. It was also damaged in winter 2016, where a panel from the top fell off in a storm.
There are 23 listed buildings in Redcar. The Grade I Listed Sir William Turner's Hospital in Kirkleatham was built between 1674–1676 and listed on the 14 June 1952.
On the Esplanade is the Grade II-Listed Zetland Lifeboat Museum housing the world's oldest lifeboat Zetland Lifeboat.
The Victorian, former Coatham Hotel stands on Newcomen Terrace sea front.[36][37] The ballroom of the hotel was home to the Redcar Jazz Club, a venue for the up-and-coming bands of the late 1960s and early 1970s.
In the south-east of Redcar is an aircraft listening post built in 1916 during the First World War as part of a regional defence system to detect approaching aircraft, principally Zeppelins, and give early warning.It is an example of an acoustic mirror, of which other examples can be found along the east coast of Britain. The mirror was used up until the invention of radar and although it was built on open fields today a modern housing estate now surrounds it. Only the concrete sound mirror remains and is now a Grade II listed building.
To the east of Redcar is the grade II* listed Church of St Peter, designed by Ignatius Bonomi and built 1822–29. In 1818, Lord Dundas gave land for a church, St Peters. The foundation stone was laid by Lady Turner of Kirkleatham in 1823. Initially it was a daughter church of Marske, but became an independent parish in 1867. It has a window commemorating local benefactor Sir William Turner.
Redcar has two railway stations, on the Tees Valley line, with trains operated by Northern and TransPennine Express, namely Redcar Central and Redcar East. A third station Redcar British Steel, which closed in December 2019, served the steelworks.
The main roads through the town are the A1085 and the A1042, with the A174 bypassing. Redcar is served primarily by Arriva North East buses, connecting Redcar with the surrounding towns and villages.
The Pangea North and CANTAT-3 submarine telecommunication cables both come ashore between Redcar and Marske-by-the-Sea.
See also: List of schools in Redcar and Cleveland
The town's further education college is Redcar & Cleveland College.
The town's secondary schools are: Outwood Academy Redcar, Sacred Heart Catholic Secondary and Rye Hills Academy.
There are eleven primary schools in Redcar: Coatham, Dormanstown, Green Gates, Ings Farm, John E Batty, Lakes, Newcomen, Riverdale, St Benedict's, Wheatlands and Zetland.
Local news and television programmes are provided by BBC North East and Cumbria and ITV Tyne Tees, the local television station TalkTeesside also broadcasts to the area. Television signals are received from the Bilsdale TV transmitter.
Local radio stations are BBC Radio Tees, Heart North East, Capital North East, Smooth North East, Greatest Hits Radio Teesside, and Zetland FM, a community based radio station which broadcast from its studios on Newcomen Terrace in the town.
The town is served by the local newspapers, East Cleveland Herald & Post which is published by the TeessideLive. The Northern Echo also covers the area.
In Coatham is Cleveland Golf Club, the first golf club to be formed in Yorkshire. It was established in 1887 and is a links course. Also in Coatham is Redcar Cricket Club, which play in the NYSD league, and Redcar Running Club.
In association football, Redcar Athletic currently compete in the Northern League Division One while Redcar Town play in Northern League Division Two. Redcar Rugby Union Football club play at Mackinlay Park.
Redcar Racecourse is one of nine thoroughbred horse racecourses in Yorkshire. There is also a motorcycle speedway racing team, the Redcar Bears racing in the SGB Championship. The race track is at the South Tees Motorsport Park in Southbank Street, South Bank and is unusual in that one bend is more highly banked than the other. The team was formerly captained by 1992 World Champion Gary Havelock and was formerly managed by his father Brian.
The town is set to host the 2022 Tour of Britain stage four, UCI Europe Tour cycling race. The town was previously set to host a stage of the Tour de Yorkshire, the event was affected by the COVID-19 pandemic.
Notable people
Gertrude Bell, colonial administrator and contemporary of Lawrence of Arabia spent her youthful years at Red Barns House in Coatham,[ which became, for a time, the Red Barns Hotel and a listed building.
The surviving negatives of Redcar photographer Alfred Edward Graham (1882–1945) were acquired by Redcar Urban District Council's Library and Museum Committee and are now held by the Redcar and Cleveland Museum Service.
Rex Hunt, governor of the Falkland Islands during the 1982 invasion by Argentina, attended Coatham School.
The former Secretary of State for Northern Ireland, Mo Mowlam, represented Redcar parliamentary constituency in the House of Commons.
Film and television actors Pip Donaghy June Laverick, and Wendy Hall, and actor/director/producer Robert Porter were all born in Redcar.
Actor and radio actor Felicity Finch, famous for her part in the Archers BBC Radio 4 drama series, playing Ruth Archer, was also born and grew up in Redcar.
Singer David Coverdale, lead singer with Deep Purple and Whitesnake lived in Redcar as a youth and worked in the Gentry clothes shop on Coatham Road.
Chris Norman, founder member and former lead singer of Smokie was born in Redcar.
Pete York, drummer with the Spencer Davis Group and session drummer was born in Redcar.
Paralympian, Baroness Tanni Grey-Thompson, originally from Wales, lived in Redcar for a number of years with her husband and daughter.
2011 and 2016 UCI Downhill World Champion Danny Hart was born in and currently lives in Redcar, he is frequently nicknamed "The Redcar Rocket" by commentators.
David Wheater, Bolton Wanderers and England national football team central defender, grew up and still lives in Redcar.
Snooker player Mike Dunn was born in Middlesbrough but lives in Redcar.[citation needed]
Jordan Jones, Rangers FC and Northern Ireland national football team midfielder was born in Redcar
Hayden Hackney, Middlesbrough F.C. midfielder was born in Redcar
Dylan Cartlidge, singer and multi-instrumentalist grew up in Redcar
Film and television
A location from the film Atonement
In 2006, Redcar was used as a location for the film adaptation of the Ian McEwan novel Atonement. The Coatham Hotel, Regent Cinema, a section of Newcomen Terrace and part of the beach were dressed as 1940s Dunkirk. Filming took place across three days in August 2006, with local men playing the soldiers.
In 2010, Redcar was featured on the Channel 4 television programme The Secret Millionaire. David Jamilly a humanitarian, philanthropist and self-made millionaire, visited the Redcar community and gave £25,000 to Zoë's Place for a sensory room, £25,000 to Redcar Amateur Boxing Club to start an Olympic fund, and £25,000 to Sid's Place for special counselling.
There was a subsequent visit on 14 May to a screening at Redcar's cinema, attended by the mayor and mayoress along with all the charities and people involved. The feature of the documentary involved the closure of the nearby Corus steelworks as well as the charities. On 9 December 2011, Jamilly opened the new Redcar Education Development centre in Park Avenue, Redcar. The centre provides day care for adults with learning difficulties. He also opened the Redcar Primary Care Hospital on 9 December 2011 and the new Sid's Place on 15 December 2011.
The town was filmed for the 2018 BBC television documentary The Mighty Redcar. The four-part series followed young people from Redcar and surrounding towns as they completed their studies and looked for work.
North Yorkshire is a ceremonial county in the Yorkshire and the Humber and North East regions of England. It borders County Durham to the north, the North Sea to the east, the East Riding of Yorkshire to the south-east, South Yorkshire to the south, West Yorkshire to the south-west, and Cumbria and Lancashire to the west. Northallerton is the county town.
The county is the largest in England by land area, at 9,020 km2 (3,480 sq mi), and has a population of 1,158,816. The largest settlements are Middlesbrough (174,700) in the north-east and the city of York (152,841) in the south. Middlesbrough is part of the Teesside built-up area, which extends into County Durham and has a total population of 376,663. The remainder of the county is rural, and the largest towns are Harrogate (73,576) and Scarborough (61,749). For local government purposes the county comprises four unitary authority areas — York, Middlesbrough, Redcar and Cleveland, and North Yorkshire — and part of a fifth, Stockton-on-Tees.
The centre of the county contains a wide plain, called the Vale of Mowbray in the north and Vale of York in the south. The North York Moors lie to the east, and south of them the Vale of Pickering is separated from the main plain by the Howardian Hills. The west of the county contains the Yorkshire Dales, an extensive upland area which contains the source of the River Ouse/Ure and many of its tributaries, which together drain most of the county. The Dales also contain the county's highest point, Whernside, at 2,415 feet (736 m).
North Yorkshire non-metropolitan and ceremonial county was formed on 1 April 1974 as a result of the Local Government Act 1972. It covered most of the North Riding of Yorkshire, as well as northern parts of the West Riding of Yorkshire, northern and eastern East Riding of Yorkshire and the former county borough of York. Northallerton, as the former county town for the North Riding, became North Yorkshire's county town. In 1993 the county was placed wholly within the Yorkshire and the Humber region.
Some areas which were part of the former North Riding were in the county of Cleveland for twenty-two years (from 1974 to 1996) and were placed in the North East region from 1993. On 1 April 1996, these areas (Middlesbrough, Redcar and Cleveland and Stockton borough south of the River Tees) became part of the ceremonial county as separate unitary authorities. These areas remain within the North East England region.
Also on 1 April 1996, the City of York non-metropolitan district and parts of the non-metropolitan county (Haxby and nearby rural areas) became the City of York unitary authority.
On 1 April 2023, the non-metropolitan county became a unitary authority. This abolished eight councils and extended the powers of the county council to act as a district council.
The York and North Yorkshire Combined Authority held its first meeting on 22 January 2024, assumed its powers on 1 February 2024 and the first mayor is to be elected in May 2024.
The geology of North Yorkshire is closely reflected in its landscape. Within the county are the North York Moors and most of the Yorkshire Dales, two of eleven areas in England and Wales to be designated national parks. Between the North York Moors in the east and the Pennine Hills. The highest point is Whernside, on the Cumbrian border, at 2,415 feet (736 m). A distinctive hill to the far north east of the county is Roseberry Topping.
North Yorkshire contains several major rivers. The River Tees is the most northerly, forming part of the border between North Yorkshire and County Durham in its lower reaches and flowing east through Teesdale before reaching the North Sea near Redcar. The Yorkshire Dales are the source of many of the county's major rivers, including the Aire, Lune, Ribble, Swale, Ure, and Wharfe.[10] The Aire, Swale, and Wharfe are tributaries of the Ure/Ouse, which at 208 km (129 mi) long is the sixth-longest river in the United Kingdom. The river is called the Ure until it meets Ouse Gill beck just below the village of Great Ouseburn, where it becomes the Ouse and flows south before exiting the county near Goole and entering the Humber estuary. The North York Moors are the catchment for a number of rivers: the Leven which flows north into the Tees between Yarm and Ingleby Barwick; the Esk flows east directly into the North Sea at Whitby as well as the Rye (which later becomes the Derwent at Malton) flows south into the River Ouse at Goole.
North Yorkshire contains a small section of green belt in the south of the county, which surrounds the neighbouring metropolitan area of Leeds along the North and West Yorkshire borders. It extends to the east to cover small communities such as Huby, Kirkby Overblow, and Follifoot before covering the gap between the towns of Harrogate and Knaresborough, helping to keep those towns separate.
The belt adjoins the southernmost part of the Yorkshire Dales National Park, and the Nidderdale AONB. It extends into the western area of Selby district, reaching as far as Tadcaster and Balne. The belt was first drawn up from the 1950s.
The city of York has an independent surrounding belt area affording protections to several outlying settlements such as Haxby and Dunnington, and it too extends into the surrounding districts.
North Yorkshire has a temperate oceanic climate, like most of the UK. There are large climate variations within the county. The upper Pennines border on a Subarctic climate. The Vale of Mowbray has an almost Semi-arid climate. Overall, with the county being situated in the east, it receives below-average rainfall for the UK. Inside North Yorkshire, the upper Dales of the Pennines are one of the wettest parts of England, where in contrast the driest parts of the Vale of Mowbray are some of the driest areas in the UK.
Summer temperatures are above average, at 22 °C. Highs can regularly reach up to 28 °C, with over 30 °C reached in heat waves. Winter temperatures are below average, with average lows of 1 °C. Snow and Fog can be expected depending on location. The North York Moors and Pennines have snow lying for an average of between 45 and 75 days per year. Sunshine is most plentiful on the coast, receiving an average of 1,650 hours a year. It reduces further west in the county, with the Pennines receiving 1,250 hours a year.
The county borders multiple counties and districts:
County Durham's County Durham, Darlington, Stockton (north Tees) and Hartlepool;
East Riding of Yorkshire's East Riding of Yorkshire;
South Yorkshire's City of Doncaster;
West Yorkshire's City of Wakefield, City of Leeds and City of Bradford;
Lancashire's City of Lancaster, Ribble Valley and Pendle
Cumbria's Westmorland and Furness.
The City of York Council and North Yorkshire Council formed the York and North Yorkshire Combined Authority in February 2024. The elections for the first directly-elected mayor will take place in May 2024. Both North Yorkshire Council and the combined authority are governed from County Hall, Northallerton.
The Tees Valley Combined Authority was formed in 2016 by five unitary authorities; Middlesbrough, Redcar and Cleveland Borough both of North Yorkshire, Stockton-on-Tees Borough (Uniquely for England, split between North Yorkshire and County Durham), Hartlepool Borough and Darlington Borough of County Durham.
In large areas of North Yorkshire, agriculture is the primary source of employment. Approximately 85% of the county is considered to be "rural or super sparse".
Other sectors in 2019 included some manufacturing, the provision of accommodation and meals (primarily for tourists) which accounted for 19 per cent of all jobs. Food manufacturing employed 11 per cent of workers. A few people are involved in forestry and fishing in 2019. The average weekly earnings in 2018 were £531. Some 15% of workers declared themselves as self-employed. One report in late 2020 stated that "North Yorkshire has a relatively healthy and diverse economy which largely mirrors the national picture in terms of productivity and jobs.
Mineral extraction and power generation are also sectors of the economy, as is high technology.
Tourism is a significant contributor to the economy. A study of visitors between 2013 and 2015 indicated that the Borough of Scarborough, including Filey, Whitby and parts of the North York Moors National Park, received 1.4m trips per year on average. A 2016 report by the National Park, states the park area gets 7.93 million visitors annually, generating £647 million and supporting 10,900 full-time equivalent jobs.
The Yorkshire Dales have also attracted many visitors. In 2016, there were 3.8 million visits to the National Park including 0.48 million who stayed at least one night. The parks service estimates that this contributed £252 million to the economy and provided 3,583 full-time equivalent jobs. The wider Yorkshire Dales area received 9.7 million visitors who contributed £644 million to the economy. The North York Moors and Yorkshire Dales are among England's best known destinations.
York is a popular tourist destination. A 2014 report, based on 2012 data, stated that York alone receives 6.9 million visitors annually; they contribute £564 million to the economy and support over 19,000 jobs. In the 2017 Condé Nast Traveller survey of readers, York rated 12th among The 15 Best Cities in the UK for visitors. In a 2020 Condé Nast Traveller report, York rated as the sixth best among ten "urban destinations [in the UK] that scored the highest marks when it comes to ... nightlife, restaurants and friendliness".
During February 2020 to January 2021, the average property in North Yorkshire county sold for £240,000, up by £8100 over the previous 12 months. By comparison, the average for England and Wales was £314,000. In certain communities of North Yorkshire, however, house prices were higher than average for the county, as of early 2021: Harrogate (average value: £376,195), Knaresborough (£375,625), Tadcaster (£314,278), Leyburn (£309,165) and Ripon (£299,998), for example.
This is a chart of trend of regional gross value added for North Yorkshire at current basic prices with figures in millions of British pounds sterling.
Unemployment in the county was traditionally low in recent years, but the lockdowns and travel restrictions necessitated by the COVID-19 pandemic had a negative effect on the economy during much of 2020 and into 2021. The UK government said in early February 2021 that it was planning "unprecedented levels of support to help businesses [in the UK] survive the crisis". A report published on 1 March 2021 stated that the unemployment rate in North Yorkshire had "risen to the highest level in nearly 5 years – with under 25s often bearing the worst of job losses".
York experienced high unemployment during lockdown periods. One analysis (by the York and North Yorkshire Local Enterprise Partnership) predicted in August 2020 that "as many as 13,835 jobs in York will be lost in the scenario considered most likely, taking the city's unemployment rate to 14.5%". Some critics claimed that part of the problem was caused by "over-reliance on the booming tourism industry at the expense of a long-term economic plan". A report in mid June 2020 stated that unemployment had risen 114 per cent over the previous year because of restrictions imposed as a result of the pandemic.
Tourism in the county was expected to increase after the restrictions imposed due the pandemic are relaxed. One reason for the expected increase is the airing of All Creatures Great and Small, a TV series about the vet James Herriot, based on a successful series of books; it was largely filmed within the Yorkshire Dales National Park. The show aired in the UK in September 2020 and in the US in early 2021. One source stated that visits to Yorkshire websites had increased significantly by late September 2020.
The East Coast Main Line (ECML) bisects the county stopping at Northallerton,Thirsk and York. Passenger service companies in the area are London North Eastern Railway, Northern Rail, TransPennine Express and Grand Central.
LNER and Grand Central operate services to the capital on the ECML, Leeds Branch Line and the Northallerton–Eaglescliffe Line. LNER stop at York, Northallerton and on to County Durham or spur over to the Tees Valley Line for Thornaby and Middlesbrough. The operator also branch before the county for Leeds and run to Harrogate and Skipton. Grand Central stop at York, Thirsk Northallerton and Eaglescliffe then over to the Durham Coast Line in County Durham.
Northern operates the remaining lines in the county, including commuter services on the Harrogate Line, Airedale Line and York & Selby Lines, of which the former two are covered by the Metro ticketing area. Remaining branch lines operated by Northern include the Yorkshire Coast Line from Scarborough to Hull, York–Scarborough line via Malton, the Hull to York Line via Selby, the Tees Valley Line from Darlington to Saltburn via Middlesbrough and the Esk Valley Line from Middlesbrough to Whitby. Last but certainly not least, the Settle-Carlisle Line runs through the west of the county, with services again operated by Northern.
The county suffered badly under the Beeching cuts of the 1960s. Places such as Richmond, Ripon, Tadcaster, Helmsley, Pickering and the Wensleydale communities lost their passenger services. Notable lines closed were the Scarborough and Whitby Railway, Malton and Driffield Railway and the secondary main line between Northallerton and Harrogate via Ripon.
Heritage railways within North Yorkshire include: the North Yorkshire Moors Railway, between Pickering and Grosmont, which opened in 1973; the Derwent Valley Light Railway near York; and the Embsay and Bolton Abbey Steam Railway. The Wensleydale Railway, which started operating in 2003, runs services between Leeming Bar and Redmire along a former freight-only line. The medium-term aim is to operate into Northallerton station on the ECML, once an agreement can be reached with Network Rail. In the longer term, the aim is to reinstate the full line west via Hawes to Garsdale on the Settle-Carlisle line.
York railway station is the largest station in the county, with 11 platforms and is a major tourist attraction in its own right. The station is immediately adjacent to the National Railway Museum.
The main road through the county is the north–south A1(M), which has gradually been upgraded in sections to motorway status since the early 1990s. The only other motorways within the county are the short A66(M) near Darlington and a small stretch of the M62 motorway close to Eggborough. The other nationally maintained trunk routes are the A168/A19, A64, A66 and A174.
Long-distance coach services are operated by National Express and Megabus. Local bus service operators include Arriva Yorkshire, Stagecoach, Harrogate Bus Company, The Keighley Bus Company, Scarborough & District (East Yorkshire), Yorkshire Coastliner, First York and the local Dales & District.
There are no major airports in the county itself, but nearby airports include Teesside International (Darlington), Newcastle and Leeds Bradford.
The main campus of Teesside University is in Middlesbrough, while York contains the main campuses of the University of York and York St John University. There are also two secondary campuses in the county: CU Scarborough, a campus of Coventry University, and Queen's Campus, Durham University in Thornaby-on-Tees.
Colleges
Middlesbrough College's sixth-form
Askham Bryan College of agriculture, Askham Bryan and Middlesbrough
Craven College, Skipton
Middlesbrough College
The Northern School of Art, Middlesbrough
Prior Pursglove College
Redcar & Cleveland College
Scarborough Sixth Form College
Scarborough TEC
Selby College
Stockton Riverside College, Thornaby
York College
Places of interest
Ampleforth College
Beningbrough Hall –
Black Sheep Brewery
Bolton Castle –
Brimham Rocks –
Castle Howard and the Howardian Hills –
Catterick Garrison
Cleveland Hills
Drax Power Station
Duncombe Park – stately home
Eden Camp Museum –
Embsay & Bolton Abbey Steam Railway –
Eston Nab
Flamingo Land Theme Park and Zoo –
Helmsley Castle –
Ingleborough Cave – show cave
John Smith's Brewery
Jorvik Viking Centre –
Lightwater Valley –
Lund's Tower
Malham Cove
Middleham Castle –
Mother Shipton's Cave –
National Railway Museum –
North Yorkshire Moors Railway –
Ormesby Hall – Palladian Mansion
Richmond Castle –
Ripley Castle – Stately home and historic village
Riverside Stadium
Samuel Smith's Brewery
Shandy Hall – stately home
Skipton Castle –
Stanwick Iron Age Fortifications –
Studley Royal Park –
Stump Cross Caverns – show cave
Tees Transporter Bridge
Theakston Brewery
Thornborough Henges
Wainman's Pinnacle
Wharram Percy
York Castle Museum –
Yorkshire Air Museum –
The Yorkshire Arboretum
Juneteenth Parade & Celebration,
Evanston, Illinois, USA
Evanston, a suburb 12 miles north of Chicago, became the first American city to approve reparations to be paid to black residents which will include housing grants. On June 19, the city held its first in-person Juneteenth parade and celebration where local leaders, musicians, and residents participated.
Photo credit: Poppy Seed Photography
--------------------
Visit our website : Weddings at the Arb
Celebrate your wedding at the premier Minnesota Landscape Arboretum, 20 miles west of the Twin Cities. The arboretum includes 1,200 acres of gardens, tree collections, prairies and indoor venue spaces with a full catering and event team to help plan your memorable day! Schedule your tour today!
--------------------
Connect with us on our other platforms!
This monument includes an animal pound at the south west corner of All Saint's churchyard, on the village green. It is now used as a public rest area and garden.
The animal pound is a square walled enclosure, adjoining the churchyard to its east. It is entered by a gateway on the north side with one free-standing gatepost of rough schist. The pound walls of mortared schist rubble are 0.5m thick and stand up to 1.05m high.
A number of small holes on the west side have been opened out from recesses opening into the pound, measuring from 0.4m to 0.5m wide and set 0.6m from the ground. It is understood that these are rifle loops from the World War II, when the pound was adapted for use as a Home Guard post.
---
The term animal pound is derived from the Anglo-Saxon word `pund' meaning enclosure, and is used to describe stock-proof areas for confining stray or illegally pastured stock and legally-kept animals rounded up at certain times of the year from areas of common grazing.
The earliest documentary references to pounds date from the 12th century, and they continued to be constructed and used throughout the medieval and post-medieval periods. Most surviving examples are likely to be less than three centuries old, and most will have fallen into disuse in the late 19th or early 20th century.
Animal pounds are usually located in villages or towns though some lie in more open locations, particularly on the edge of old woodlands and commons.
---------
Originally taken and posted for the GWUK group.
Now replaced with the un-edited version
Guessed by Janet G48
Schweiz / Berner Oberland - Allmendhubel
Eiger, Mönch and Jungfrau
Eiger, Mönch und Jungfrau
The Allmendhubel (1,932 m) is a hill above Mürren, overlooking the valley of Lauterbrunnen in the canton of Bern. Its summit is easily accessible from Mürren by a funicular, the Allmendhubelbahn, which reaches a height of 1,907 metres. A restaurant is also located near the top.
In winter, the Allmendhubel is part of a ski area and includes several ski lifts.
(Wikipedia)
The Eiger (German pronunciation: [ˈaɪ̯ɡɐ]) is a 3,967-metre (13,015 ft) mountain of the Bernese Alps, overlooking Grindelwald and Lauterbrunnen in the Bernese Oberland of Switzerland, just north of the main watershed and border with Valais. It is the easternmost peak of a ridge crest that extends across the Mönch to the Jungfrau at 4,158 m (13,642 ft), constituting one of the most emblematic sights of the Swiss Alps. While the northern side of the mountain rises more than 3,000 m (10,000 ft) above the two valleys of Grindelwald and Lauterbrunnen, the southern side faces the large glaciers of the Jungfrau-Aletsch area, the most glaciated region in the Alps. The most notable feature of the Eiger is its nearly 1,800-metre-high (5,900 ft) north face of rock and ice, named Eiger-Nordwand, Eigerwand or just Nordwand, which is the biggest north face in the Alps.] This huge face towers over the resort of Kleine Scheidegg at its base, on the eponymous pass connecting the two valleys.
The first ascent of the Eiger was made by Swiss guides Christian Almer and Peter Bohren and Irishman Charles Barrington, who climbed the west flank on August 11, 1858. The north face, the "last problem" of the Alps, considered amongst the most challenging and dangerous ascents, was first climbed in 1938 by an Austrian-German expedition.The Eiger has been highly publicized for the many tragedies involving climbing expeditions. Since 1935, at least 64 climbers have died attempting the north face, earning it the German nickname Mordwand, literally "murder(ous) wall"—a pun on its correct title of Nordwand (North Wall).
Although the summit of the Eiger can be reached by experienced climbers only, a railway tunnel runs inside the mountain, and two internal stations provide easy access to viewing-windows carved into the rock face. They are both part of the Jungfrau Railway line, running from Kleine Scheidegg to the Jungfraujoch, between the Mönch and the Jungfrau, at the highest railway station in Europe. The two stations within the Eiger are Eigerwand (behind the north face) and Eismeer (behind the south face), at around 3,000 metres. The Eigerwand station has not been regularly served since 2016.
Etymology
The first mention of Eiger, appearing as "mons Egere", was found in a property sale document of 1252, but there is no clear indication of how exactly the peak gained its name. The three mountains of the ridge are commonly referred to as the Virgin (German: Jungfrau – translates to "virgin" or "maiden"), the Monk (Mönch), and the Ogre (Eiger; the standard German word for ogre is Oger). The name has been linked to the Latin term acer, meaning "sharp" or "pointed".
Geographic setting and description
The Eiger is located above the Lauterbrunnen Valley to the west and Grindelwald to the north in the Bernese Oberland region of the canton of Bern. It forms a renowned mountain range of the Bernese Alps together with its two companions: the Jungfrau (4,158 m (13,642 ft)) about 5.6 kilometres (3.5 mi) southwest of it and the Mönch (4,107 m (13,474 ft)) about in the middle of them. The nearest settlements are Grindelwald, Lauterbrunnen (795 m (2,608 ft)) and Wengen (1,274 m (4,180 ft)). The Eiger has three faces: north (or more precisely NNW), east (or more precisely ESE), and west (or more precisely WSW). The northeastern ridge from the summit to the Ostegg (lit.: eastern corner, 2,709 m (8,888 ft)), called Mittellegi, is the longest on the Eiger. The north face overlooks the gently rising Alpine meadow between Grindelwald (943 m (3,094 ft)) and Kleine Scheidegg (2,061 m (6,762 ft)), a mountain railways junction and a pass, which can be reached from both sides, Grindelwald and Lauterbrunnen/Wengen – by foot or train.
Politically, the Eiger (and its summit) belongs to the Bernese municipalities of Grindelwald and Lauterbrunnen. The Kleine Scheidegg (literally, the small parting corner) connects the Männlichen-Tschuggen range with the western ridge of the Eiger. The Eiger does not properly form part of the main chain of the Bernese Alps, which borders the canton of Valais and forms the watershed between the Rhine and the Rhône, but constitutes a huge limestone buttress, projecting from the crystalline basement of the Mönch across the Eigerjoch. Consequently, all sides of the Eiger feed finally the same river, namely the Lütschine.
Eiger's water is connected through the Weisse Lütschine (the white one) in the Lauterbrunnen Valley on the west side (southwestern face of the Eiger), and through the Schwarze Lütschine (the black one) running through Grindelwald (northwestern face), which meet each other in Zweilütschinen (lit.: the two Lütschinen) where they form the proper Lütschine. The east face is covered by the glacier called Ischmeer, (Bernese German for Ice Sea), which forms one upper part of the fast-retreating Lower Grindelwald Glacier. These glaciers' water forms a short creek, which is also confusingly called the Weisse Lütschine, but enters the black one already in Grindelwald together with the water from the Upper Grindelwald Glacier. Therefore, all the water running down the Eiger converges at the northern foot of the Männlichen (2,342 m (7,684 ft)) in Zweilütschinen (654 m (2,146 ft)), about 10 kilometres (6.2 mi) northwest of the summit, where the Lütschine begins its northern course to Lake Brienz and the Aare (564 m (1,850 ft)).
Although the north face of the Eiger is almost free of ice, significant glaciers lie at the other sides of the mountain. The Eiger Glacier flows on the southwestern side of the Eiger, from the crest connecting it to the Mönch down to 2,400 m (7,900 ft), south of Eigergletscher railway station, and feeds the Weisse Lütschine through the Trümmelbach. On the east side, the Ischmeer–well visible from the windows of Eismeer railway station–flows eastwards from the same crest then turns to the north below the impressive wide Fiescherwand, the north face of the Fiescherhörner triple summit (4,049 m (13,284 ft)) down to about 1,600 m (5,200 ft) of the Lower Grindelwald Glacier system.
The massive composition of the Eiger, Mönch, and Jungfrau constitutes an emblematic sight of the Swiss Alps and is visible from many places on the Swiss Plateau and the Jura Mountains in the northwest. The higher Finsteraarhorn (4,270 m (14,010 ft)) and Aletschhorn (4,190 m (13,750 ft)), which are located about 10 kilometres (6.2 mi) to the south, are generally less visible and situated in the middle of glaciers in less accessible areas. As opposed to the north side, the south and east sides of the range consist of large valley glaciers extending for up to 22 kilometres (14 mi), the largest (beyond the Eiger drainage basin) being those of Grand Aletsch, Fiesch, and Aar Glaciers, and is thus uninhabited. The whole area, the Jungfrau-Aletsch protected area, comprising the highest summits and largest glaciers of the Bernese Alps, was inscribed as a UNESCO World Heritage Site in 2001.
In July 2006, a piece of the Eiger, amounting to approximately 700,000 cubic metres of rock, fell from the east face. As it had been noticeably cleaving for several weeks and fell into an uninhabited area, there were no injuries and no buildings were hit.
Climbing history
While the summit was reached without much difficulty in 1858 by a complex route on the west flank, the battle to climb the north face has captivated the interest of climbers and non-climbers alike. Before it was successfully climbed, most of the attempts on the face ended tragically and the Bernese authorities even banned climbing it and threatened to fine any party that should attempt it again. But the enthusiasm which animated the young talented climbers from Austria and Germany finally vanquished its reputation of unclimbability when a party of four climbers successfully reached the summit in 1938 by what is known as the "1938" or "Heckmair" route.
The climbers that attempted the north face could be easily watched through the telescopes from the Kleine Scheidegg, a pass between Grindelwald and Lauterbrunnen, connected by rail. The contrast between the comfort and civilization of the railway station and the agonies of the young men slowly dying a short yet uncrossable distance away led to intensive coverage by the international media.
After World War II, the north face was climbed twice in 1947, first by a party of two French guides, Louis Lachenal and Lionel Terray, then by a Swiss party consisting of H. Germann, with Hans and Karl Schlunegger.
First ascent
In 1857, a first recorded attempt was made by Christian Almer, Christian Kaufmann, Ulrich Kaufmann guiding the Austrian alpinist Sigismund Porges. They did manage the first ascent of neighboring Mönch instead. Porges, however, successfully made the second ascent of the Eiger in July 1861 with the guides Christian Michel, Hans and Peter Baumann.
The first ascent was made by the western flank on August 11, 1858 by Charles Barrington with guides Christian Almer and Peter Bohren. On the previous afternoon, the party walked up to the Wengernalp hotel. From there they started the ascent of the Eiger at 3:30 a.m. Barrington describes the route much as it is followed today, staying close to the edge of the north face much of the way. They reached the summit at about noon, planted a flag, stayed for some 10 minutes and descended in about four hours. Barrington describes the reaching of the top, saying, "the two guides kindly gave me the place of first man up." After the descent, the party was escorted to the Kleine Scheidegg hotel, where their ascent was confirmed by observation of the flag left on the summit. The owner of the hotel then fired a cannon to celebrate the first ascent. According to Harrer's The White Spider, Barrington was originally planning to make the first ascent of the Matterhorn, but his finances did not allow him to travel there as he was already staying in the Eiger region.
Mittellegi ridge
Although the Mittellegi ridge had already been descended by climbers (since 1885) with the use of ropes in the difficult sections, it remained unclimbed until 1921. On the 10th of September of that year, Japanese climber Yuko Maki, along with Swiss guides Fritz Amatter, Samuel Brawand and Fritz Steuri made the first successful ascent of the ridge. The previous day, the party approached the ridge from the Eismeer railway station of the Jungfrau Railway and bivouacked for the night. They started the climb at about 6:00 a.m. and reached the summit of the Eiger at about 7:15 p.m., after an over 13 hours gruelling ascent. Shortly after, they descended the west flank. They finally reached Eigergletscher railway station at about 3:00 a.m. the next day.
Attempts on the north face
1935
In 1935, two young German climbers from Bavaria, Karl Mehringer and Max Sedlmeyer, arrived at Grindelwald to attempt the ascent of the north face. After waiting some time for the weather to improve, they set off, reaching the height of the Eigerwand station before stopping for their first bivouac. The following day, facing greater difficulties, they gained little height. On the third day, they made hardly any vertical gain. That night, the weather deteriorated, bringing snow and low cloud that shrouded the mountain from the observers below. Avalanches began to sweep the face. Two days later, the weather briefly cleared, and the two men were glimpsed a little higher and about to bivouac for the fifth night, before clouds descended again. A few days later, the weather finally cleared, revealing a completely white north face.: 225 Weeks later, the German World War I ace Ernst Udet went searching for the missing men with his aircraft, eventually spotting one of them frozen to death in what became known as the "Death Bivouac". Sedlmeyer's body was found at the foot of the face the following year by his brothers Heinrich and Martin Meier, who were part of a group looking for the victims of the 1936 climbing disaster. Mehringer's remains were found in 1962 by Swiss climbers below the "Flat Iron" (Bügeleisen) at the lefthand end of the second ice field.
1936
The next year ten young climbers from Austria and Germany came to Grindelwald and camped at the foot of the mountain. Before their attempts started one of them was killed during a training climb, and the weather was so bad during that summer that, after waiting for a change and seeing none on the way, several members of the party gave up. Of the four that remained, two were Bavarians, Andreas Hinterstoisser and Toni Kurz, and two were Austrians, Willy Angerer and Edi Rainer. When the weather improved they made a preliminary exploration of the lowest part of the face. Hinterstoisser fell 37 metres (121 ft) but was not injured. A few days later the four men finally began the ascent of the face. They climbed quickly, but on the next day, after their first bivouac, the weather changed; clouds came down and hid the group to the observers. They did not resume the climb until the following day, when, during a break, the party was seen descending, but the climbers could be seen only intermittently from the ground. The group had no choice but to retreat, since Angerer had suffered serious injuries from falling rock. The party became stuck on the face when they could not recross the difficult Hinterstoisser Traverse, from which they had taken the rope they had first used to climb it. The weather then deteriorated for two days. They were ultimately swept away by an avalanche, which only Kurz survived, hanging on a rope. Three guides started on an extremely perilous rescue attempt. They failed to reach him but came within shouting distance and learned what had happened. Kurz explained the fate of his companions: one had fallen down the face, another was frozen above him, and the third had fractured his skull in falling and was hanging dead on the rope.
In the morning the three guides came back, traversing the face from a hole near the Eigerwand station and risking their lives under incessant avalanches. Toni Kurz was still alive but almost helpless, with one hand and one arm completely frozen. Kurz hauled himself off the cliff after cutting loose the rope that bound him to his dead teammate below and climbed back onto the face. The guides were not able to pass an unclimbable overhang that separated them from Kurz. They managed to give him a rope long enough to reach them by tying two ropes together. While descending, Kurz could not get the knot to pass through his carabiner. He tried for hours to reach his rescuers who were only a few metres below him. Then he began to lose consciousness. One of the guides, climbing on another's shoulders, was able to touch the tip of Kurz's crampons with his ice-axe but could not reach higher. Kurz was unable to descend further and, completely exhausted, died slowly.
1937
An attempt was made in 1937 by Mathias Rebitsch and Ludwig Vörg. Although the attempt was unsuccessful, they were nonetheless the first climbers who returned alive from a serious attempt on the face. They started the climb on 11 August and reached a high point of a few rope lengths above Death Bivouac. A storm then broke and after three days on the wall they had to retreat. This was the first successful withdrawal from a significant height on the wall.
First ascent of the north face
The north face was first climbed on July 24, 1938 by Anderl Heckmair, Ludwig Vörg, Heinrich Harrer and Fritz Kasparek in a German–Austrian party. The party had originally consisted of two independent teams: Harrer (who did not have a pair of crampons on the climb) and Kasparek were joined on the face by Heckmair and Vörg, who had started their ascent a day later and had been helped by the fixed rope that the lead team had left across the Hinterstoisser Traverse. The two groups, led by the experienced Heckmair, decided to join their forces and roped together as a single group of four. Heckmair later wrote: "We, the sons of the older Reich, united with our companions from the Eastern Border to march together to victory."
The expedition was constantly threatened by snow avalanches and climbed as quickly as possible between the falls. On the third day a storm broke and the cold was intense. The four men were caught in an avalanche as they climbed "the Spider," the snow-filled cracks radiating from an ice-field on the upper face, but all possessed sufficient strength to resist being swept off the face. The members successfully reached the summit at four o'clock in the afternoon. They were so exhausted that they only just had the strength to descend by the normal route through a raging blizzard.
Other notable events
1864 (Jul 27): Fourth ascent, and first ascent by a woman, Lucy Walker, who was part of a group of six guides (including Christian Almer and Melchior Anderegg) and five clients, including her brother Horace Walker[
1871: First ascent by the southwest ridge, 14 July (Christian Almer, Christian Bohren, and Ulrich Almer guiding W. A. B. Coolidge and Meta Brevoort).
1890: First ascent in winter, Ulrich Kaufmann and Christian Jossi guiding C. W. Mead and G. F. Woodroffe.
1924: First ski ascent and descent via the Eiger glacier by Englishman Arnold Lunn and the Swiss Fritz Amacher, Walter Amstutz and Willy Richardet.
1932: First ascent of the northeast face ("Lauper route") by Hans Lauper, Alfred Zürcher, Alexander Graven and Josef Knubel
1970: First ski descent over the west flank, by Sylvain Saudan.
1986: Welshman Eric Jones becomes the first person to BASE jump from the Eiger.
1988: Original Route (ED2), north face, Eiger (3970m), Alps, Switzerland, first American solo (nine and a half hours) by Mark Wilford.
1991: First ascent, Metanoia Route, North Face, solo, winter, without bolts, Jeff Lowe.
1992 (18 July): Three BMG/UIAGM/IFMGA clients died in a fall down the West Flank: Willie Dunnachie; Douglas Gaines; and Phillip Davies. They had ascended the mountain via the Mittellegi Ridge.
2006 (14 June): François Bon and Antoine Montant make the first speedflying descent of the Eiger.
2006 (15 July): Approximately 700,000 cubic metres (20 million cubic feet) of rock from the east side collapses. No injuries or damage were reported.
2015 (23 July): A team of British Para-Climbers reached the summit via the West Flank Route. The team included John Churcher, the world's first blind climber to summit the Eiger, sight guided by the team leader Mark McGowan. Colin Gourlay enabled the ascent of other team members, including Al Taylor who has multiple sclerosis, and the young autistic climber Jamie Owen from North Wales. The ascent was filmed by the adventure filmmakers Euan Ryan & Willis Morris of Finalcrux Films.
Books and films
The 1959 book The White Spider by Heinrich Harrer describes the first successful ascent of the Eiger north face.
The Climb Up To Hell, 1962, by Jack Olson, an account of the ill-fated 1957 attempted climb of the north face by an Italian four-man team and the dramatic rescue of the sole survivor mounted by an international all-volunteer group of rescuers.
Eiger Direct, 1966, by Dougal Haston and Peter Gillman, London: Collins, also known as Direttissima; the Eiger Assault
The 1971 novel The Ice Mirror by Charles MacHardy describes the second attempted ascent of the Eiger north face by the main character.
The 1972 novel The Eiger Sanction is an action/thriller novel by Rodney William Whitaker (writing under the pseudonym Trevanian), based around the climbing of the Eiger. This was then made into the 1975 film The Eiger Sanction starring Clint Eastwood and George Kennedy. The Eiger Sanction film crew included very experienced mountaineers (e.g., Mike Hoover, Dougal Haston, and Hamish MacInnes, see Summit, 52, Spring 2010) as consultants, to ensure accuracy in the climbing footage, equipment and techniques.
The Eiger, 1974, by Dougal Haston, London: Cassell
The 1982 book Eiger, Wall of Death by Arthur Roth is an historical account of first ascents of the north face.
The 1982 book Traverse of The Gods by Bob Langley is a World War II spy thriller where a group escaping from Nazi Germany is trapped and the only possible exit route is via the Nordwand.
Eiger, 1983, a documentary film by Leo Dickinson of Eric Jones' 1981 solo ascent of the north face.
Eiger Dreams, 1990, a collection of essays by Jon Krakauer, begins with an account of Krakauer's own attempt to climb the north face.
Eiger: The Vertical Arena (German edition, 1998; English edition, 2000), edited by Daniel Anker, a comprehensive climbing history of the north face authored by 17 climbers, with numerous photographs and illustrations.
The IMAX film The Alps features John Harlin III's climb up the north face in September 2005. Harlin's father, John Harlin II, set out 40 years earlier to attempt a direct route (the direttissima) up the 6,000-foot (1,800 m) face, the so-called "John Harlin route". At 1300 m, his rope broke, and he fell to his death. Composer James Swearingen created a piece named Eiger: Journey to the Summit in his memory.
The 2007 docu/drama film The Beckoning Silence featuring mountaineer Joe Simpson, recounting—with filmed reconstructions—the ill-fated 1936 expedition up the north face of the Eiger and how Heinrich Harrer's book The White Spider inspired him to take up climbing. The film followed Simpson's eponymous 2003 book. Those playing the parts of the original climbing team were Swiss mountain guides Roger Schäli (Toni Kurz), Simon Anthamatten (Andreas Hinterstoisser), Dres Abegglen (Willy Angerer) and Cyrille Berthod (Edi Rainer). The documentary won an Emmy Award the subsequent year.
The 2008 German historical fiction film Nordwand is based on the 1936 attempt to climb the Eiger north face. The film is about the two German climbers, Toni Kurz and Andreas Hinterstoisser, involved in a competition with an Austrian duo to be the first to scale the north face of Eiger.
The 2010 documentary Eiger: Wall of Death by Steve Robinson.
(Wikipedia)
The Mönch (German pronunciation: [ˈmœnç] German: "monk") at 4,110 metres (13,480 ft) is a mountain in the Bernese Alps, in Switzerland. Together with the Eiger and the Jungfrau, it forms a highly recognisable group of mountains, visible from far away.
The Mönch lies on the border between the cantons of Valais and Bern, and forms part of a mountain ridge between the Jungfrau and Jungfraujoch to the west, and the Eiger to the east. It is west of Mönchsjoch, a pass at 3,650 metres (11,980 ft), Mönchsjoch Hut, and north of the Jungfraufirn and Ewigschneefäld, two affluents of the Great Aletsch Glacier. The north side of the Mönch forms a step wall above the Lauterbrunnen valley.
The Jungfrau railway tunnel runs right under the summit, at an elevation of approximately 3,300 metres (10,830 ft).
The summit was first climbed on record on 15 August 1857 by Christian Almer, Christian Kaufmann (1831-1861), Ulrich Kaufmann and Sigismund Porges.
(Wikipedia)
The Jungfrau (YOONG-frow, German pronunciation: [ˈjʊŋˌfʁaʊ̯], transl. "maiden, virgin"), at 4,158 meters (13,642 ft) is one of the main summits of the Bernese Alps, located between the northern canton of Bern and the southern canton of Valais, halfway between Interlaken and Fiesch. Together with the Eiger and Mönch, the Jungfrau forms a massive wall of mountains overlooking the Bernese Oberland and the Swiss Plateau, one of the most distinctive sights of the Swiss Alps.
The summit was first reached on August 3, 1811, by the Meyer brothers of Aarau and two chamois hunters from Valais. The ascent followed a long expedition over the glaciers and high passes of the Bernese Alps. It was not until 1865 that a more direct route on the northern side was opened.
The construction of the Jungfrau Railway in the early 20th century, which connects Kleine Scheidegg to the Jungfraujoch, the saddle between the Mönch and the Jungfrau, made the area one of the most-visited places in the Alps. Along with the Aletsch Glacier to the south, the Jungfrau is part of the Jungfrau-Aletsch area, which was declared a World Heritage Site in 2001.
Etymology
The name Jungfrau ("maiden, virgin"), which refers to the highest of the three prominent mountains overlooking the Interlaken region, along with the Mönch ("monk") and the Eiger ("ogre"), is most likely derived from the name Jungfrauenberg given to Wengernalp, the alpine meadow directly facing the huge northern side of the Jungfrau, across the Trummelbach gorge. Wengernalp was so named for the nuns of Interlaken Monastery, its historical owner. Contrary to popular belief, the name did not originate from the appearance of the snow-covered mountain, the latter looking like a veiled woman.
The "virgin" peak was heavily romanticized as "goddess" or "priestess" in late 18th to 19th century Romanticism. Its summit, considered inaccessible, remained untouched until the 19th century. After the first ascent in 1811 by Swiss alpinist Johann Rudolf Meyer, the peak was jokingly referred to as "Mme Meyer" (Mrs. Meyer).
Geographic setting
Politically, the Jungfrau (and its massif) is split between the municipalities of Lauterbrunnen (Bern) and Fieschertal (Valais). It is the third-highest mountain of the Bernese Alps after the nearby Finsteraarhorn and Aletschhorn, respectively 12 and 8 km (7.5 and 5 mi) away. But from Lake Thun, and the greater part of the canton of Bern, it is the most conspicuous and the nearest of the Bernese Oberland peaks; with a height difference of 3,600 m (11,800 ft) between the summit and the town of Interlaken. This, and the extreme steepness of the north face, secured for it an early reputation for inaccessibility.
The Jungfrau is the westernmost and highest point of a gigantic 10 km (6.2 mi) wall dominating the valleys of Lauterbrunnen and Grindelwald. The wall is formed by the alignment of some of the biggest north faces in the Alps, with the Mönch (4,107 m or 13,474 ft) and Eiger (3,967 m or 13,015 ft) to the east of the Jungfrau, and overlooks the valleys to its north by a height of up to 3 km (1.9 mi). The Jungfrau is approximately 6 km (3.7 mi) from the Eiger; with the summit of the Mönch between the two mountains, 3.5 km (2.2 mi) from the Jungfrau. The Jungfraujoch is the saddle between the Jungfrau and the Mönch and the Eigerjoch is the saddle between the Mönch and the Eiger. The wall is extended to the east by the Fiescherwand and to the west by the Lauterbrunnen Wall, although it follows different directions from the Jungfrau and the Eiger.
The difference of altitude between the deep valley of Lauterbrunnen (800 m or 2,600 ft) and the summit is particularly visible from the area of Mürren. From the valley floor, west of the massif, the altitude gain is more than 3 km (1.9 mi) for a horizontal distance of 4 km (2.5 mi).
The landscapes around the Jungfrau are extremely contrasted. In contrast to the vertiginous precipices of its northwest, the mountain's southeastern side emerges from the upper snows of the Jungfraufirn, one of the main feeders of the Aletsch Glacier, at around 3,500 meters (11,500 ft). The 20-kilometer-long (12 mi) valley of Aletsch on the southeast is completely uninhabited, and is surrounded by neighboring valleys with similar landscapes. The area as a whole constitutes the largest glaciated area not just in the Alps, but in Europe as well.
Climbing history
In 1811, the brothers Johann Rudolf (1768–1825) and Hieronymus Meyer, sons of Johann Rudolf Meyer (1739–1813), the head of a rich merchant family of Aarau, along with several servants and a porter picked up at Guttannen, first reached the Valais by way of the Grimsel, and crossed the Beich Pass, a glacier pass over the Oberaletsch Glacier, to the head of the Lötschen valley. There, they added two local chamois hunters, Alois Volken and Joseph Bortis, to their party and traversed the Lötschenlücke before reaching the Aletschfirn (the west branch of the Aletsch Glacier), where they established the base camp, north of the Aletschhorn. After the Guttannen porter was sent back alone over the Lötschenlücke, the party finally reached the summit of the Jungfrau by the Rottalsattel on August 3. They then recrossed the two passes named to their point of departure in Valais, and went home again over the Grimsel.
The journey was a most extraordinary one for the time, and some persons threw doubts at its complete success. To settle these, another expedition was undertaken in 1812. In this the two sons, Rudolf (1791–1833) and Gottlieb (1793–1829), of Johann Rudolf Meyer, played the chief parts. After an unsuccessful attempt, defeated by bad weather, in the course of which the Oberaarjoch was crossed twice (this route being much more direct than the long detour through the Lötschental), Rudolf, with the two Valais hunters (Alois Volker and Joseph Bortis), a Guttannen porter named Arnold Abbühl, and a Hasle man, bivouacked on a depression on the southeast ridge of the Finsteraarhorn. Next day (August 16) the whole party attempted the ascent of the Finsteraarhorn from the Studer névé on the east by way of the southeast ridge, but Meyer, exhausted, remained behind. The following day the party crossed the Grünhornlücke to the Aletsch Glacier, but bad weather then put an end to further projects. At a bivouac, probably just opposite the present Konkordia Hut, the rest of the party, having come over the Oberaarjoch and the Grünhornlücke, joined the Finsteraarhorn party. Gottlieb, Rudolf's younger brother, had more patience than the rest and remained longer at the huts near the Märjelensee, where the adventurers had taken refuge. He could make the second ascent (September 3) of the Jungfrau, the Rottalsattel being reached from the east side as is now usual, and his companions being the two Valais hunters.
The third ascent dates from 1828, when several men from Grindelwald, headed by Peter Baumann, planted their flag upon the summit. Next came the ascent by Louis Agassiz, James David Forbes, Heath, Desor, and Duchatelier in 1841, recounted by Desor in his Excursions et Séjours dans les Glaciers. Gottlieb Samuel Studer published an account of the next ascent made by himself and Bürki in 1842.
In 1863, a party consisting of three young Oxford University graduates and three Swiss guides successfully reached the summit and returned to the base camp of the Faulberg (located near the present position of the Konkordia Hut) in less than 11 hours (see the section below, The 1863 Ascent). In the same year Mrs Stephen Winkworth became the first woman to climb the Jungfrau. She also slept overnight in the Faulberg cave prior to the ascent as there was no hut at that time.
Before the construction of the Jungfraujoch railway tunnel, the approach from the glaciers on the south side was very long. The first direct route from the valley of Lauterbrunnen was opened in 1865 by Geoffrey Winthrop Young, H. Brooke George with the guide Christian Almer. They had to carry ladders with them in order to cross the many crevasses on the north flank. Having spent the night on the rocks of the Schneehorn (3,402 m or 11,161 ft) they gained next morning the Silberlücke, the depression between the Jungfrau and Silberhorn, and thence in little more than three hours reached the summit. Descending to the Aletsch Glacier they crossed the Mönchsjoch, and passed a second night on the rocks, reaching Grindelwald next day. This route became a usual until the opening of the Jungfraujoch.
The first winter ascent was made on 23 January 1874, by Meta Brevoort and W. A. B. Coolidge with guides Christian and Ulrich Almer. They used a sled to reach the upper Aletsch Glacier, and were accompanied by Miss Brevoort's favorite dog, Tschingel.
The Jungfrau was climbed via the west side for the first time in 1885 by Fritz and Heinrich von Allmen, Ulrich Brunner, Fritz Graf, Karl Schlunegger and Johann Stäger—all from Wengen. They ascended the Rottal ridge (Innere Rottalgrat) and reached the summit on 21 September. The more difficult and dangerous northeast ridge that connects the summit from the Jungfraujoch was first climbed on 30 July 1911 by Albert Weber and Hans Schlunegger.
In July 2007, six Swiss Army recruits, part of the Mountain Specialists Division 1, died in an accident on the normal route. Although the causes of the deaths was not immediately clear, a report by the Swiss Federal Institute for Snow and Avalanche Research concluded that the avalanche risk was unusually high due to recent snowfall, and that there was "no other reasonable explanation" other than an avalanche for the incident.
The 1863 Ascent
The Führerbuch of the Alpine guide Peter Baumann records an ascent of the Jungfrau made by himself with three men from England in July 1863. The foreign climbers were long thought to have been John Tyndall, J.J. Hornby and T.H. Philpott, until in 1958 the records were checked by the Alpine Club and the following conclusion was reached:
On July 23, 1963, Phillpotts, with James Robertson and H.J. Chaytor, climbed the Jungfrau (the entry shown in A.J. 32. 227 was wrongly transcribed by Montagnier, who says ‘T.H. Philpott’ for J.S. Phillpotts). The entry in Peter Baumann’s Führerbuch (facsimile in A.C. archives) says that the trio crossed the Strahlegg Pass and the Oberaarjoch, and then climbed the Jungfrau from the Eggishorn.
Tyndall, Hornby and Philpott were well-known Alpinists, but there is no record of their having attempted the Jungfrau in 1863. Robertson, Chaytor and Phillpotts were novices; they had recently graduated from Oxford University where they had all been keen members of the Oxford University Boat Club.
William Robertson (1839–1892), the leader of the expedition (wrongly called ‘James’ in the Note quoted above), was an Australian by birth, and the first non-British national to take part in the Oxford and Cambridge Boat Race. He later became a barrister and member of parliament in Australia. He and H.J. Chaytor (possibly the father of the medievalist Henry John Chaytor) were both members of the victorious Oxford team in the 1861 Boat Race. James Surtees Phillpotts (1839–1930) was the third member of the team; he would later become headmaster of Bedford School. The trio had three Swiss guides, Peter Baumann, Peter Kaufmann ("Grabipeter", father of Peter Kaufmann the younger) and Rubi.
A description of the ascent of the Jungfrau is contained in a letter dated Sunday 26 July which Phillpotts wrote to his friend Alexander Potts (later to become the first headmaster of Fettes College). The letter is now in the possession of the Alpine Club. The following extracts are from that letter.
The Virgin certainly did not smile on the poor "fools who rushed in" on her sacred heights, i.e. in plain British, we had the treadmill slog, the biting wind, the half frost-bitten feet and the flayed faces that generally attend an Alpine ascent.
We got to the Faulberg hole about dark, and enjoyed the coffee the longman (Kauffmann) made, as one would in a hole in a rock in a cold evening. The "Faulberg Nachtlager" consists of two holes and a vestibule to the upper hole. The Upper Hole in which we lodged just contained Chay[tor], the Guv [Robertson] and myself, stretched at full length on a little hay over a hard rock mattress, convex instead of concave at the point where one likes to rest one's weight. Chaytor was in the middle, and as we were very close was warm and slept. The Guv and I courted Nature's soft nurse in vain. At two we got up and methodically put our feet into the stocks, i.e. our boots, breakfasted and shivered, then started (unwashed of course, as the cold gave us malignant hydrophobia) a little after 3:30.
The hole was about 150 feet [46 m] up one of the loose stone cliffs one now knows so well. So we groped our way down it and over the moraine – the stars still lingering, as day was just dawning. We could not start at 1:30, the proper time, as there was no moon and we wanted light as we had to tramp the glacier at once. Rubi led, and off we went, roped and in Indian file, in the old treadmill way over the slippery plowed-field-like snow that lay on the upper glacier, for a pull without a check of one or two hours.
At last we came to the region of bergschrunds and crevasses. They seemed to form at first an impassable labyrinth, but gradually the guides wound in and out between the large rifts, which were exquisitely lovely with their overhanging banks of snow and glittering icicles, and then trod as on pins and needles over a snowbridge here and there, or had to take a jump over the more feasible ones – and we found ourselves at the foot of the mountain; trudged up on the snow which ought to have been crisp but was even then more or less fresh fallen and sloppy; had to creep over about three crevasses, and after a tiresome pull, dragging one leg after another out of ankle or knee deep snow, we got on a crest of snow at right angles to the slope we had just come up. That slope with its crevasses on one side, and on the other a shorter and much steeper one which led in a few steps to a precipice.
All along this crest went a snakelike long crevasse, for which we had continually to sound, and go first one side and then the other; then we got to the foot of the saddle. Some twenty or thirty steps, some cut, some uncut, soon took us up a kind of hollow, and we got on a little sloping plateau of some six feet [1.8 m] large, where we left the grub and the knapsack, keeping my small flask of cognac only. Then up a steep ice slope, very steep I should say, down which the bits of ice cut out of the steps hopped and jumped at full gallop and then bounded over to some bottomless place which we could not see down. Their pace gave one an unpleasant idea of the possible consequence of a slip.
Here we encountered a biting bitter wind. Peter Baumann cut magnificent steps, at least he and Rubi did between them, the one improving on the other's first rough blows. After Rubi came Chaytor with Kauffmann behind him, then the Guv, and then myself, the tail of the string. Each step was a long lift from the last one, and as the snow was shallow they had to be cut in the ice which was like rock on this last slope.
Suddenly there burst upon us, on lifting our heads over the ridge, the green and cheerful valleys of Lauterbrunnen and Interlaken, of Grindelwald and a distant view of others equally beautiful stretching on for ever in one vast panorama. On the other side in grim contrast there was a wild and even awful scene. One gazed about one and tried in vain to see to the bottom of dark yawning abysses and sheer cliffs of ice or rock.
Tourism
Named after the Jungfrau, the Jungfrau Region of the Bernese Oberland is a major tourist destination in the Alps and includes a large number of railways and other facilities. While the mountain peak was once difficult to access, the Jungfrau Railway, a rack railway, now goes to the Jungfraujoch railway station at 3,454 m (11,332 ft), therefore providing an easy access to the upper Aletsch Glacier and a relatively short access to the Jungfrau itself, the height difference between the station and the summit being only 704 metres and the horizontal distance being slightly less than 2 kilometres. As a result, in the popular mind, the Jungfrau has become a mountain associated with the Bernese Oberland and Interlaken, rather than with Upper Valais and Fiesch.
In 1893, Adolf Guyer-Zeller conceived of the idea of a railway tunnel to the Jungfraujoch to make the glaciated areas on its south side more accessible. The building of the tunnel took 16 years and the summit station was not opened before 1912. The goal was in fact to reach the summit of the Jungfrau with an elevator from the highest railway station, located inside the mountain. The complete project was not realized because of the outbreak of the World War I. Nevertheless, it was at the time one of the highest railways in the world and remains today the highest in Europe and the only (non-cable) railway on Earth going well past the perennial snow-line.
The Jungfrau Railway leaves from Kleine Scheidegg, which can be reached from both sides by trains from Grindelwald, and Lauterbrunnen via Wengen. The train enters the Jungfrau Tunnel running eastward through the Eiger just above Eigergletscher, which is, since 2020, also accessible by aerial tramway from Grindelwald. Before arriving at the Jungfraujoch, it stops for a few minutes at two other stations, Eigerwand (on the north face of the Eiger) and Eismeer (on the south side), where passengers can see through the holes excavated from the mountain. The journey from Kleine Scheidegg to Jungfraujoch takes approximately 50 minutes including the stops; the downhill return journey taking only 35 minutes.
A large complex of tunnels and buildings has been constructed at the Jungfraujoch, referred to as the "Top of Europe". There are several restaurants and bars, shops, multimedia exhibitions, a post office, and a research station with dedicated accommodation facilities. An elevator enables access to the top of the Sphinx and its observatory, at 3,571 m (11,716 ft), the highest viewing platform of the area. Outside, at the level of the Jungfraujoch, there is a ski school, and the "Ice Palace", a collection of elaborate ice sculptures displayed inside the Aletsch Glacier. Another tunnel leads to the east side of the Sphinx, where one can walk on the glacier up to the Mönchsjoch Hut, the only hotel infrastructure in the area.
Apart from the Jungfraujoch, many facilities have been built in the Jungfrau Region, including numerous mountain railways. In 1908, the first public cable car in the world, the Wetterhorn Elevator, opened at the foot of the Wetterhorn, but was closed seven years later. The Schilthorn above Mürren, the Männlichen above Wengen, and the Schynige Platte above Wilderswil, offer good views of the Jungfrau and the Lauterbrunnen valley. On the south side, the Eggishorn above Fiesch also offers views of the Jungfrau, across the Aletsch Glacier.
Climbing routes
The normal route follows the traces of the first climbers, but the long approach on the Aletsch Glacier is no longer necessary. From the area of the Jungfraujoch the route to the summit takes only a few hours. Most climbers start from the Mönchsjoch Hut. After a traverse of the Jungfraufirn the route heads to the Rottalsattel (3,885 m or 12,746 ft), from where the southern ridge leads to the Jungfrau. It is not considered a very difficult climb but it can be dangerous on the upper section above the Rottalsattel, where most accidents happen. The use of the Jungfrau Railway instead of the much more gradual approach from Fiesch (or Fieschertal), via the Konkordia Hut, can cause some acclimatization troubles as the difference of altitude between the railway stations of Interlaken and Jungfraujoch is almost 3 km (1.9 mi).
(Wikipedia)
Der Eiger ist ein Berg in den Berner Alpen mit einer Höhe von 3967 m ü. M. Er ist dem Hauptkamm der Berner Alpen etwas nördlich vorgelagert und steht vollständig auf dem Territorium des Schweizer Kantons Bern. Zusammen mit Mönch und Jungfrau, deren Gipfel auf der Grenze zum Kanton Wallis liegen, dominiert der Eiger die Landschaft des zentralen Berner Oberlandes. Die etwa 3000 Meter über dem Tal aufragenden Nordflanken dieser Berge stellen die Schauseite einer der bekanntesten je als ein «Dreigestirn» bezeichneten Gipfel-Dreiergruppen in den Alpen dar.
Insbesondere die Nordwand des Eigers fasziniert sowohl Bergsteiger als auch Alpin-Laien. Durch dramatische Begehungsversuche und gelungene Begehungen dieser Wand wurde der Eiger weltweit bekannt und immer wieder ins Blickfeld der Öffentlichkeit gerückt – nicht zuletzt, da die gesamte Wand von Grindelwald und der Bahnstation Kleine Scheidegg aus einsehbar ist. Die Jungfraubahn mit ihrem Tunnel durch den Eigerfels ist seit ihrer Eröffnung im Jahr 1912 ein Touristenmagnet.
Namensherkunft
Die erste urkundliche Erwähnung des Eigers stammt aus dem Jahre 1252 – dies ist die zweitfrüheste urkundliche Erwähnung eines Schweizer Bergs nach dem Bietschhorn (1233). Am 24. Juli 1252 wurde in einer Verkaufsurkunde zwischen Ita von Wädiswyl und der Propstei Interlaken ein Grundstück mit den Worten «ad montem qui nominatur Egere» (dt.: Bis zum Berg, der Eiger genannt wird) abgegrenzt. Ein halbes Jahrhundert später wird der Eiger in einem Belehnungsbrief erstmals in deutscher Sprache erwähnt: «under Eigere».
Für die Herkunft des Namens gibt es drei gängige Erklärungen. Eine erste ist der althochdeutsche Name Agiger oder Aiger, wie der erste Siedler unterhalb des Eigers geheissen haben soll. Der Berg über dessen Weiden wurde deshalb Aigers Geissberg oder auch nur Geissberg genannt. Hieraus entwickelten sich dann im Laufe der Zeit die direkten Vorgänger der heutigen Bezeichnung. Die Herkunft des Namens könnte auch von dem lateinischen Wort acer kommen, woraus sich im Französischen aigu entwickelte. Beide Worte haben die Bedeutung scharf beziehungsweise spitz – in Anlehnung an die Form des Eigers. Die dritte Erklärung stammt von der früher gebräuchlichen Schreibweise Heiger, was sich aus dem Dialektausdruck «dr hej Ger» entwickelt haben könnte (hej bedeutet hoch, Ger war ein germanischer Wurfspiess). Wiederum wäre hier die Form des Eigers ausschlaggebend für seine Bezeichnung.
Im Zusammenhang mit dem Eiger wird auch des Öfteren die Namensähnlichkeit mit dem Oger, einem menschenähnlichen Unhold, genannt. In Anlehnung an das Dreigestirn «Eiger–Mönch–Jungfrau» gibt es die Erzählung, der Unhold Eiger wolle seine lüsternen Pranken auf die Jungfrau legen, woran er aber vom fröhlichen Mönch gehindert werde. Zu dieser Geschichte sind in Grindelwald alte Karikaturen und neuere Postkarten zu kaufen.
Lage und Umgebung
Der Eiger erhebt sich direkt südwestlich von Grindelwald (Amtsbezirk Interlaken). Die bekannte Nordwand ist genaugenommen eine Nordwestwand. Neben dieser existiert in der berühmten «Eiger-Nordansicht» auch noch die Nordostwand. Sie bildet die Basis für den scharfen Mittellegigrat, der vom Unteren Grindelwaldgletscher zum Gipfel zieht. Auf der gegenüberliegenden Seite begrenzt der Westgrat die Nordwand. Ihm folgt die Westflanke, in welcher sich der Eigergletscher und der Klein Eiger befinden. An diesen schliessen sich der Südwestgrat und noch ein Stück östlicher der Südgrat an, der wiederum die Südostwand begrenzt, welche bis zum Mittellegigrat reicht. Südöstlich des Eigers liegt der Grindelwald-Fieschergletscher.
In der Umgebung des Eigers befinden sich einige Viertausender des Aarmassivs. Im Osten ist er umgeben von Schreckhorn (4078 m ü. M.) und Lauteraarhorn (4042 m ü. M.), im Südosten vom Grossen Fiescherhorn (4049 m ü. M.), und im Südwesten ist der Mönch (4107 m ü. M.) durch das Nördliche und Südliche Eigerjoch vom Eiger getrennt. Zusammen mit dem Mönch und der Jungfrau (4158 m ü. M.) bildet der Eiger das «Dreigestirn», bei dem der Eiger den nordöstlichen und die Jungfrau den südwestlichen Endpunkt bildet. Entgegen der steil abfallenden Nordseite des Berges befindet sich im Süden des Eigers die Hochfläche und Gletscherwelt der Berner Alpen. Seit Ende 2001 gehört der Eiger zum Gebiet des UNESCO-Weltnaturerbes Schweizer Alpen Jungfrau-Aletsch.
Geologie
Der Eiger ist ein Teil des helvetischen Systems, das im Grossraum um den Thunersee die Decken des Alpennordrandes bildet. In einer späten Phase der alpidischen Gebirgsfaltung wurden die helvetischen Kalk-Sedimente von ihrer kristallinen Basis abgeschürft und in Form einer Abscherungsdecke nach Nordwesten verschoben. Während des Faltungsprozesses in der Alpenentstehung brachen die Kalkbänke auf und Kluft- sowie Faltensysteme entstanden, die später mit ausgefälltem Calcit geschlossen wurden. Wichtigste Bestandteile der Sedimente sind der Schrattenkalk der Kreidezeit und der Malmkalk. Als Füll- und Schmiermaterial dienten Mergel und Tonschiefer.
Die klar erkennbare Faltung des Helvetikums mit seinen gebänderten, plattigen Kalkschichten zeigt sich auch am Eiger. Das Massiv des Eigers besteht komplett aus Kalk der helvetischen Zone und schliesst die Flyschschichten und die Molasse des Grindelwaldbeckens steil nach Süden hin ab. Weil der Talkessel von Grindelwald so reich gegliedert ist, finden hier die verschiedensten Tiere einen Lebensraum.[6] Südlich des Eigers schliesst sich das Aarmassiv mit seinem Innertkirchner-Lauterbrunner-Kristallin an. Teilweise hat sich dieses über die Sedimente des Eiger geschoben. Im Bereich des Mönchs treffen die Sedimente auf Altkristallin. Die typischen Gesteine des helvetischen Systems im Bereich des Eigers entstanden während des Jura, dem mittleren Zeitabschnitts des Mesozoikums. Der vorherrschende Kalk ist dabei mit verschiedenen Gesteinen durchmischt. Es zeigen sich Mergel-Kalke und -Schiefer, Ton-Schiefer, Eisenoolith sowie kalkige Sandsteine.
Blick auf Eigergletscher und Klein Eiger
Die Kalkschichten des Eigers lagern auf Gneis und sind um 60–70° nach Norden geneigt. Geprägt wurde die heutige Form des Eigers durch die Eiszeiten. Während der Riss-Kaltzeit reichte die Vergletscherung bis an den Fuss der Nordwand. In der Würm-Kaltzeit war die Mächtigkeit des Eises um 200 Meter geringer. Durch die Bewegung der Gletscher wurde die Erdoberfläche umgestaltet. Vom Eis überlagerte Landschaften wurden abgeschliffen, wohingegen unbedeckte Bereiche durch Verwitterung und andere Formen der Erosion verändert wurden. Mit dem Rückzug des Eises änderten sich auch die Druckverhältnisse im Gestein, was sich durch Entlastungsbewegungen formgebend auswirkte. Prägend für den Eiger und seine Form war die allseitige Umlagerung von Eismassen, welche für einen recht gleichmässigen und markanten Abrieb aller Wände sorgte. Darüber hinaus war die Nordwand durch ihre Exposition den Abtragungsprozessen wie Frostverwitterung mehr ausgesetzt.
Felssturz
2006 ereignete sich am Eiger ein grosser Bergsturz, der öffentliches Interesse auf sich zog. An der Ostseite des Berges, unterhalb des Mittellegigrates, war durch Felsbewegungen ein rund 250 Meter langer Spalt entstanden, der eine Breite von etwa 7 Metern erreichte.Danach senkten sich die äusseren Teile mehrere Zentimeter pro Tag ab. Eine Ursache dieser Felsabspaltung könnte sowohl das massive Eindringen von Schmelzwasser in den Felsen gewesen sein, als auch eine Instabilität des Gesteins durch den Rückgang des Gletschers unterhalb des Felsabbruchs infolge der globalen Erwärmung. Am 13. Juli 2006 um 19:24 Uhr stürzten rund 500'000 Kubikmeter Felsbrocken auf den Unteren Grindelwaldgletscher. Über der Gemeinde Grindelwald schwebte stundenlang eine Staubwolke. Bereits am Nachmittag desselben Tages war die sogenannte «Madonna vom Eiger» zu Tal gestürzt. Hierbei handelte es sich um einen ungefähr 30 Meter hohen schlanken Felsturm mit rund 600 Kubikmeter Volumen.
Seit diesen Ereignissen wird die Felsnase (Gesamtvolumen: ungefähr eine Million Kubikmeter Gestein), aus der die Gesteinsmasse abbrach, von der Universität Lausanne beobachtet. Die Beobachtungen ergaben, dass sich die Nase von Juli 2007 bis August 2008 auf einer nach Osten geneigten Gleitfläche um 15 Meter talwärts bewegte. Zusätzlich kippte die Gesteinsmasse um zwei Grad nach Nordosten. Die Kluft zwischen Berg und Felsbrocken betrug im August 2008 50 Meter. Immer wieder brechen Gesteinsteile ab und stürzen zu Tal. Gebremst und stabilisiert wird die Masse vom Gletschereis, in das die Felsnase gleitet. Dies verhindert, dass die Nase als kompakte Masse zu Tal stürzt. So gilt es als wahrscheinlicher, dass der Gesteinsblock in sich selbst zusammenfallen wird.
(Wikipedia)
Der Mönch ist ein 4107 m ü. M. hoher Berg der Berner Alpen in der Schweiz. Zusammen mit dem Eiger und der Jungfrau bildet er eine markante, von weit her sichtbare Dreiergruppe, ein sogenanntes „Dreigestirn“.
Seine Erstbesteigung fand am 15. August 1857 durch Christian Almer, Christian Kaufmann, Ulrich Kaufmann und Sigismund Porges statt.
Südöstlich des Mönch liegt die Mönchsjochhütte, eine 3657 m ü. M. hoch gelegene Berghütte wenig oberhalb des oberen Mönchsjochs, das den Mönch vom Trugberg trennt.
Höhenbestimmung
1935 wurde die Höhe des Mönchs mit 4099 m ü. M. bestimmt. Diese Zahl ist noch heute häufig in der Literatur zu finden. 1993 ergaben jedoch Messungen per Luftfotogrammetrie eine Höhe von 4107 m ü. M.. Daraufhin wurde der Wert auf der Landeskarte der Schweiz korrigiert. Mit einer Messung per GPS ermittelte man 1997 eine Höhe von 4109,4 m ü. M.; und bei einer erneuten luftfotogrammetrischen Messung von 1999 resultierte sogar eine Höhe von 4110 m ü. M.. Diese neuen Messwerte wurden jedoch nicht auf den amtlichen Karten berücksichtigt. Für diese abweichenden Werte sind nicht nur Messfehler verantwortlich, sondern auch die Tatsache, dass der Mönch eine Kuppe aus Firn besitzt, welche in den letzten Jahren gewachsen ist.
Name
Am Fusse des Mönchs befinden sich Alpweiden, auf welchen früher Wallache, sogenannte „Münche“, gesömmert wurden. So hat man den über den Münchenalpen gelegenen Berg Münchenberg genannt und schliesslich nur noch Münch oder Mönch.
Routen
Südarm des Ostgrates (Normalroute)
Schwierigkeit: ZS-, mit II. UIAA-Grad Felskletterei
Zeitaufwand: 2½–3½ Std. von der Mönchsjochhütte, 3–4 Std. vom Jungfraujoch
Ausgangspunkt: Mönchsjochhütte (3657 m ü. M.)
Talort: Grindelwald (1034 m ü. M.)
Südwestgrat
Schwierigkeit: ZS-, mit III-. UIAA-Grad Felskletterei
Zeitaufwand: 3–4 Stunden
Ausgangspunkt: Jungfraujoch (3454 m ü. M.)
Talort: Grindelwald (1034 m ü. M.)
Nordostarm des Ostgrates
Schwierigkeit: ZS, mit III+. UIAA-Grad Felskletterei
Zeitaufwand: 4–5 Stunden
Ausgangspunkt: Mönchsjochhütte (3657 m ü. M.)
Talort: Grindelwald (1034 m ü. M.)
Nordostgrat
Schwierigkeit: ZS
Zeitaufwand: 4–5 Stunden
Ausgangspunkt: Mönchsjochhütte (3657 m ü. M.)
Talort: Grindelwald (1034 m ü. M.)
Nordwestbollwerk (Nollen)
Schwierigkeit: S
Zeitaufwand: 6–10 Stunden
Ausgangspunkt: Guggihütte (2791 m ü. M.)
Talort: Kleine Scheidegg (2061 m ü. M.)
(Wikipedia)
Die Jungfrau ist ein Berg in der Schweiz. Sie ist mit 4158 m ü. M. der dritthöchste Berg der Berner Alpen und bildet zusammen mit Eiger und Mönch eine markante Dreiergruppe, ein sogenanntes «Dreigestirn».
Am 13. Dezember 2001 wurde die Jungfrau zusammen mit südlich angrenzenden Gebieten als Schweizer Alpen Jungfrau-Aletsch in die Liste als UNESCO-Weltnaturerbe aufgenommen.
Lage und Umgebung
Über den Jungfrau-Gipfel verläuft die Grenze zwischen den Kantonen Bern und Wallis. Der Berg ist ausserordentlich vielgestaltig. Im Norden und Nordwesten, auf ihrer „weiblichen“ Schauseite (vgl. Foto) sind ihr Wengen-Jungfrau, Schneehorn, das Silberhorn, das Chly Silberhoren und der „Schwarzmönch“ vorgelagert sowie die zerrissenen Kühlauenen- und Giessengletscher. Im Westen erhebt sie sich fast eisfrei volle 3250 Meter über dem hinteren Lauterbrunnental. Es ist dies (nach dem Mont Blanc) der zweithöchste direkte Abhang in den Alpen. Ihre Südwand erhebt sich über dem versteckten Rottalgletscher und ihre Ostwand über den Firnen am Jungfraujoch.
Die Pläne, auf die Jungfrau eine Bergbahn zu bauen, wurden aufgrund finanzieller Schwierigkeiten nicht realisiert. Die ursprünglich bis unter den Gipfel geplante Jungfraubahn wurde bis 1912 mit Endstation Jungfraujoch fertiggestellt.
Auf dem untersten Absatz des Nordostgrats haben die PTT einen Funk-Umsetzer auf 3777 m ü. M. installiert.
Geologie
Die Jungfrau liegt im nördlichen Randbereich des Aarmassivs, eines der sogenannten Zentralmassive der Schweizer Alpen. Ihre höheren Lagen (Silberhorn, Wengen-Jungfrau und Hauptgipfel) sowie ihre Westflanke bis hinunter zum oberen Ende des Lauterbrunnentals sind weit überwiegend aus kristallinem Grundgebirge (prä-triassische Gneise, Glimmerschiefer u. ä.) der Helvetischen Zone aufgebaut. Die Nordwestflanke hingegen, der ganze «Vorbau» (Schwarzmönch, Rotbrett und Schneehorn) besteht aus sedimentärem, überwiegend jurassischem und kretazischem Deckgebirge des Helvetikums. Eine Besonderheit der Jungfrau ist, dass dort zwischen dem prinzipiell autochthonen Gipfel-Kristallin und dessen Deckschichten ein Überschiebungs-kontakt besteht; somit ist das Grundgebirge geringfügig auf sein Deckgebirge überschoben worden.
Name
Der Name Jungfrau dürfte sich von der Wengernalp am Fusse des Berges ableiten, die – nach den Besitzerinnen, den Nonnen vom Kloster Interlaken – früher Jungfrauenberg genannt wurde. Einer anderen Quelle zufolge leitet sich der Name vom Aussehen des Nordhanges des Berges ab, der aus der Ferne dem Schleier eines Mädchens ähneln soll.
Nach dem Berg ist die Jungfrau-Region benannt, die Tourismusorganisation der Orte Grindelwald, Wengen, Mürren und Lauterbrunnen, ausserdem die Jungfraubahn Holding AG, die neben der Jungfraubahn selbst auch die anderen Bergbahnen in der Region betreibt.
Besteigungsgeschichte
Bergsteiger auf dem Gipfel im Jahr 1878
Erstbesteiger waren Johann Rudolf Meyer und sein Bruder Hieronymus mit den Führern Joseph Bortis und Alois Volken, die am 3. August 1811 vom Lötschental her den Berg von Süden erklommen hatten. Sie folgten ungefähr der heutigen Normalroute. Der Volksmund taufte daraufhin die bis dahin unberührte Jungfrau «Madame Meyer».
1874 erfolgte die Winter-Erstbesteigung durch die Alpinistin Margaret Claudia Brevoort.
Die Jungfrau gilt, obwohl leicht erreichbar, als unfallträchtiger Berg. Bei einem der schwersten Unglücke stürzten am 12. Juli 2007 sechs Rekruten der Gebirgsspezialisten-Rekrutenschule Andermatt vom Rottalsattel 1000 Meter auf den darunterliegenden Rottalgletscher in den Tod, nachdem sie eine Lawine ausgelöst hatten. Das urteilende Militärgericht ging von einem falsch eingeschätzten, heimtückischen Lawinenrisiko aus und sprach in der Folge die verantwortlichen Bergführer frei.
Routen
Rottalsattel und Südostgrat (Normalroute)
Schwierigkeit: ZS-
Zeitaufwand: 4–5 Std. von der Mönchsjochhütte, 3½–4½ Std. vom Jungfraujoch
Ausgangspunkt: Mönchsjochhütte (3657 m)
Talort: Grindelwald (1034 m)
Innere Rottalgrat
Schwierigkeit: ZS
Zeitaufwand: 6–7 Stunden
Ausgangspunkt: Rottalhütte (2755 m)
Talort: Stechelberg (919 m)
Nordwestgrat oder „Rotbrettgrat“
Schwierigkeit: S
Zeitaufwand: 8–12 Stunden
Ausgangspunkt: Silberhornhütte (2663 m)
Talort: Stechelberg (919 m)
Nordostgrat
Schwierigkeit: S+, mit IV. UIAA-Grad Felskletterei
Zeitaufwand: 8–10 Stunden
Ausgangspunkt: Jungfraujoch (3454 m)
Talort: Grindelwald (1034 m)
Kunst
Erwähnt ist die Jungfrau unter anderem bei Friedrich Schiller, Wilhelm Tell, Vers 628 (1804). Lord Byrons Drama Manfred (1817) spielt am Fuss und auf dem Gipfel des Massivs. Ferdinand Hodler hat die Jungfrau mehrfach gemalt, darunter die perspektivisch verfremdete «Jungfrau über dem Nebelmeer». Alex Diggelmann gab 1958 eine Lithographienmappe unter dem Titel Die Jungfrau, mein Berg heraus. Stephan Bundi gestaltete 2005 eine Schweizer Gedenkmünze mit dem Bergmotiv.
Im Januar 2012 wurde zum 100-jährigen bestehen der Jungfraubahn eine übergrosse Schweizer Flagge vom Lichtkünstler Gerry Hofstetter an den Gipfel projiziert. Zeitweise waren neben dem Schweizer Kreuz auch ein Porträt des Zürcher Unternehmers Adolf Guyer-Zeller sowie ein Bild von einem der Züge zu sehen.
(Wikipedia)
Digitised image from the Town Hall Photographer's Collection - GB127.M850
The Town Hall Photographer’s Collection is a large photographic collection held in Manchester City Council’s Central Library archives, ranging in date from 1956 to 2007.
The collection consists of tens of thousands of images, covering the varied areas of work of Manchester Corporation and latterly, Manchester City Council.
The photographs were taken by staff photographers, who were tasked to document the work of Corporation/Council departments and, in doing so, captured many aspects of Manchester life and history, including significant changes to the Manchester landscape.
The collection includes many different formats from glass negatives, to slides, prints, CDs and even a couple of cine films.
What is especially exciting is that the majority of these images have never before been available in a digital format and therefore have only ever been seen by a handful of people.
A team of dedicated Staff and Volunteers are currently working on the systematic digitisation of the negatives held within the collection.
This album represents the result of their work to date.
More from the Historic Masters Festival, Brands Hatch. Inside the Druids Hairpin is a great place to practice your panning
New York City Mayor Bill de Blasio announced that the proposed budget for 2018 would include an unprecedented commitment to Vision Zero improvements in the City. Improvements will include additional NYPD Crossing Guards, lighting, street safety redesign, and increased Vision Zero law enforcement. Brooklyn, NY. Wednesday, January 25th, 2017.
Edwin J. Torres/ Mayoral Photography Office.
ROCKTROPOLIS is a progressive rock band that is like a volcano ready to explode upon your ears. Members include guitarist ROCKTROPOLIS, Bassist and Keyboardist Sam Metropoulos and Drummer Marc Stemmler. Influences are Dream Theater, Rush, Yngwie, Yes, Deep Purple and Iron Maiden to name a few. Guitarist ROCKTROPOLIS has worked with The Process, Gabe Gonzalez (George Clinton) and former drummer John Macaluso (Yngwie Malmsteen, ARK and VOX). Multi instrumentalist Sam Metropoulos has collaborated on several albums with The Process, played with John Macaluso and has opened for Yngwie Malmsteen. Akin to the pillars of the great Parthenon, drummer Marc Stemmler provides the foundation for which ROCKTROPOLIS bridges the hemispheres between classical and progressive rock music. ROCKTROPOLIS is a Nominee of the 2013 Detroit Music Awards.
ROCKTROPOLIS is represented by Howard Hertz/Joseph Bellanca (Hertz Schram, p.c.) Mr. Hertz’s impressive roster includes George Clinton, Sippie Wallace, The Romantics, The Bass Brothers, Eminem, Marilyn Manson, Russell Simmons, O-Town, Pantera, Marcus Belgrave, The GO, Mike Posner, Elmore Leonard, Warner Tamerlane and Atlantic Records.
ROCKTROPOLIS is currently recording/producing their debut album, with Chris Lewis as their recording engineer (Fire Hyena Studio). Projected release date is summer 2013. Be prepared to own a collection of brilliant compositions that are melodic, epic and infectious to the soul.
www.RocktropolisMusic.com (c) 2012
The facade include, like the other churches of Malta, two clocks : one which shows the real time, and another one which exhibits a wrong time : it is to cheat the devil who, wanting to divert the faithful during the offices, doesn't know exactly what time is it.
Maltese people are catholic and practice at 98% : the religious presence is seen everywhere : on the front of the houses, in the form of statuettes of the Virgin, in the names given to the houses, on the posters and religious texts placed in the buses.
Roundhill Furniture 5-Piece Wood and Metal Dining Room Set, Includes Table with 4 Chairs via Smart Furniture Shop ift.tt/1C5kngY
Ars Electronica Home Delivery is a weekly program that includes guided tours of Ars Electronica's exhibitions, excursions to Ars Electronica Labs, visits to the Machine Learning Studio, concerts with real-time visualizations, deep space LIVE sessions, workshops with engineers and talks with artists and scientists from around the world, as well as programs for schools, universities and companies.
In order to make these streams happen, a lot of work has to be done as the light has to be porperly set up, the sound and cameras have to be adjusted, stage directions have to be given, the set has to be re-arranged, ...
Find out more about Ars Electronica Home Delivery:
ars.electronica.art/homedelivery/en/
Credit: Ars Electronica - Robert Bauernhansl
Provincetown, Massachusetts, 34th annual Carnival Parade "A Space Odyssey" August 16th 2012
Every year Ptown hosts Carnival week, with the highlight being the mardi gras style parade down Commercial Street, with lots of beads and happy faces of all ages. Each year a theme is selected, such themes include "Viva Las Vegas" 2013, "A Space Odyssey" 2012, "Can't Stop the Music" 2011, "Jungle Fantasy" 2010, "Peace Love and Go-Go Boots" 2009. Homes and business's get in on the fun and the entire town is decorated for the fans of the event that travel from miles away to attend.
Provincetown, which is sometimes called "P-town" is a New England town located at the extreme tip of Cape Cod in Barnstable County, Massachusetts, United States.
For more about Provincetown, Massachusetts, Carnival Parade visit
Photo
Provincetown, Massachusetts USA
08-16-2012
Motorbike action on the hillclimb at the Goodwood Festival of Speed. Stunt master Mattie Griffin on his BMW F800R
Hagerstown, Indiana (September 10, 2012) The new Model T Ford Museum is slated to hold its grand opening during Richmond’s Octoberfest on September 28 at 6 p.m. The museum which was previously located in Centerville, Indiana near the Warm Glow Candle Factory for 5 years moved just a few miles east to Richmond, Indiana’s Historical Depot District this past spring.
Since the move to Richmond volunteers have been steadily preparing the museum’s new home, displays and vehicles for the event.
Today, a photo shoot for the Model T Museum’s newly acquired 1930 Pietenpol Sky Scout was held at the Hagerstown Airport.
The plan arrived at the airport around 10:00 a.m. this morning and was assembled by Model T enthusiasts and many of them brought their own Model Ts to use during the photo shoot.
One of the people there today was Mr. Jay Klehfoth who is the CEO and publisher of the Vintage Ford Magazine.
Jay is a walking encyclopedia when it comes to all things Model T. I was to learn he’s pretty knowledgeable in a lot of areas too. During our walk around of the plane Jay pointed out one of the parts for the engine had been made by a former factory in Richmond of all places. And there are many other special things about this airplane I’m sure he’ll be writing about in the next issue of the the Vintage Ford Magazine. He not only knew a lot about the Pietenpol Sky Scout plane that was being photographed for the magazine cover. He’s pretty sharp when it comes to airports too. He said that the Hagerstown airport were today’s photo shoot was done has the longest grass landing strip in the United States which to me made it the perfect place for today’s event.
This Pietenpol that will be on display at the museum is powered by a 20 HP Model T engine which was modified to include dual-ignition which is used in aviation. According to an article in the AntiqueAirfield.com website from September 10, 2012 there was only one original Pietenpol Sky Scout built by Bernard Pietenpol himself, and just two replicas. The article also said that all 3 were still flying.
The new Model T Ford Museum is going to be an exciting addition to what is one of Indiana’s grandest historical areas and a must in this part of the Midwest.
Richmond is a perfect place for any day trip. But, if you want to see all that Richmond has to offer you’ll need to plan on staying several days.
The Model T Ford Museum is located in Richmond’s Historic Depot District at 309 N 8th St, Richmond, IN 47374 - 765-488-0026.
Model T Ford Museum website: www.mtfca.com/clubpages/museum.htm
Additional Information:
The Model T Ford Club of America has nearly 8,000 families worldwide. Members are from all 50 states and 41 other countries.
The Vintage Ford Magazine is published bimonthly by the Model T Ford Club of America, 119 W. Main Street, Centerville, Indiana and is mailed to all members. Subscription rates are $35.00 per year (six issues) in the United States ($42.00 Canada and $44.00 elsewhere) and include member ship in the club.
All correspondence should be ad dressed to:
THE MODEL T FORD CLUB
OF AMERICA
P.O. Box 126
Centerville, IN 47330-0126
765-855-5248 fax 765-855-3428
e-mail: admin@mtfca.com
Raw Video: Prepping Pietenpol Sky Scout For Photo Shoot youtu.be/7_JnszAF8GA
Video: Pietenpol Sky Scout Photo Shoot youtu.be/h3m6ZWgNJMg
Video: Model T Ford Museum Grand Opening Set youtu.be/OwIiE5O1UQk
Graffitiwear - Complete outfit includes the dress, sleeves, panties, and shoes. Comes with a HUD of 8 dresses & sleeves, 8 panties, and 8 shoes*. 4 design themes available.
> Maitreya & Petite
> LaraX & Petite
> Legacy & Perky
> Reborn & Waifu
> Prima Busty & Petite
marketplace.secondlife.com/p/Graffitiwear-Celebrate-DEMO/...
Solar Flair, L&C's 2017 Summer Garden Show, is a celebration of light, energy, lunar cycles and how plants connect with the cosmos. This year’s theme is influenced by the solar system and culminates with the unique experience of a total solar eclipse that will be visible along a narrow track that runs diagonally from the northwest to southeast coasts across the continental U.S. — with St. Louis very close to the path of totality – on Monday, Aug. 21. It will be the first total solar eclipse to touch the continental U.S. since 1979, and the first to cross from coast to coast since 1918.
This year’s garden show experience will also include a curated art exhibition by Michiko Itatani, which will be free and open to the public from Aug. 22-Sept. 22.
Photo by S. Paige Allen, L&C media specialist/photographer
For almost 60 years drummer Louis Hayes has backed and played with some of the most prolific jazz musicians in the music’s short history. The Detroit, Michigan native comes from a great musical class which includes: Dr. Barry Harris, Yusef Lateef, Curtis Fuller, Kenny Burrell, and Ron Carter; musicians he began playing with professionally while still in his teens. Louis knew from an early age that he was destined to become a great musician and his parents encouraged him and geared towards that.
By the time he was 19 Louis was recruited by pianist Horace Silver to join his unit and sent for him to come to New York City in 1956 where he’s been a resident ever since. For three years he was part of Horace’s historic quintet he started after his stint with Art Blakey. But is was another musician that was also making waves on the jazz scene that on his way out and was about to form his own group. Julian “Cannonball” Adderley was playing with the Miles Davis Quintet which featured the legendary John Coltrane on tenor saxophone. By the end of Miles’s critically acclaimed “Kind of Blue” recording peaked jazz heads as well as gain new listeners, both Trane and Adderley would leave Miles and forge their own history in jazz music.
On a recommendation from bassist Sam Jones, Louis would be asked by Cannonball to join his quintet that would become legendary in their own right. The group would include: Cannonball on alto saxophone; Nat Adderley on coronet; Louis Hayes on drums; Yusef Lateef on reeds; Joe Zawinul on piano; and Sam Jones on bass. This unit would become one of the most influential groups in modern jazz and serve as springboard for many new jazz groups to come.
After a fruitful six year run with the Adderley’s, he then joined the legendary Oscar Peterson Trio for two years. Throughout his career he’s also played with Junior Cook, James Spaulding, Woody Shaw, and McCoy Tyner.
Louis continues to carry Cannonball’s legacy with the Louis Hayes Cannonball Legacy Band featuring Vincent Herring on alto sax; Jeremy Pelt on trumpet; Rick Germanson on piano; and Richie Goods on bass. Louis tours all over the world playing Cannonball’s songbook like: “Work Song,” “Hi-Fly,” “Tradition,” and “Jive Samba.”
Watch this video on Vimeo. Video created by Brian Pace.
When couples dream of their perfect wedding destination abroad, their vision often includes escaping to a far-away place that offers all of the charms one could possibly desire for their Religious or Civil Ceremony. So, if you're looking at celebrating your wedding in Sicily, Taormina is a good choice.Taormina's beauty is uncontested. Some cities are known for their art treasures, others for their natural beauties; only a few, like Taormina, own both.Visitors to this magical yet relatively undiscovered island, leave with its images of sheer beauty, its cultural simplicity, the passion and warmth of the people and historical delights etched permanently in their memories.Within its ancient stone gates, the old town has fascinating archeological monuments and medieval homes. Magnificent views of the sea complete the picture.The city is located on a cliff top overlooking the deep blue of the never ending horizon reflected in a clear turquoise sea which surrounds the bays and beaches.In fact it is Sicily's number one tourist resort, boasting magnificent scenery, architecture and great local cuisine. It's no wonder tourists flock to Taormina every year Its rich culture and crystal clear sea and views of Mount Etna create a magical atmosphere. Taormina has endlessly winding medieval streets and tiny passages, each with its own secrets.Some of these intriguing places are secluded gardens hidden by stone walls; others are set on terraces overlooking the coast or in more public but equally pleasant squares.Taormina is beautiful by day but in the evenings its atmosphere is simply enchanting, whether you stroll the illuminated streets or indulge in the view of the coast over an authentic Sicilian dinner. Taormina's ancient Greek splendor, medieval charm and unique views will leave you with a lasting impression of Sicily.The climate is mild even in the winter, where it feels like eternal spring time. Its air is filled with the scent of orange and lemon blossoms. Steal away on an island retreat in beautiful Sicily, as it offers a taste of the traditional with a delicate touch of the exotic.There are several charming churches here in which to have a Catholic wedding, as well as Palazzo Santo Stefano for civil weddings, which takes an exquisitely charming medieval mood. Taormina's regal Norman Byzantine, Romanesque and Baroque churches offer a beautiful venue for a religious wedding.Couples may choose to exchange their wedding vows in any of these spectacular locations!The whole Taormina experience leaves visitors breathless and enthusiastic to plan their dream wedding here.
Make the dream come true for you...
www.facebook.com/pages/Weddinginsicily-Taormina/475641052...
The Postcard
A postally unused postcard that was published prior to June 1918 by Stengel & Co. Ltd., Post Card Publishers, of London N. The card, which has a divided back, was printed in Saxony.
Queen's College Oxford
Queen's College Oxford (on the right of the photograph) was founded in 1341 by Robert de Eglesfield in honour of Queen Philippa of Hainaut (wife of King Edward III of England). The college is distinguished by its predominantly neoclassical architecture, which includes buildings designed by Sir Christopher Wren and Nicholas Hawksmoor.
In 2015, the college had an endowment of £265 million, making it the fifth wealthiest college (after St. John's, Christ Church, All Souls and Merton).
In April 2012, as part of the celebrations of the Diamond Jubilee of Elizabeth II, a series of commemorative stamps were released featuring A-Z pictures of famous British landmarks. Queen's College's front quad was used on the Q stamp, alongside other landmarks such as the Angel of the North on A and the Old Bailey on O.
The most famous feast of the College is the Boar's Head Gaudy, which originally was the Christmas Dinner for members of the College who were unable to return home over the Christmas break between terms, but is now a feast for old members of the College on the Saturday before Christmas.
Queen's College Alumni
Alumni of Queen's include:
- Tony Abbott, 28th Prime Minister of Australia
- Rowan Atkinson, actor and comedian, known for Blackadder and Mr. Bean
- Jeremy Bentham, English philosopher, and legal and social reformer
- Tim Berners-Lee, inventor of the World Wide Web
- Cory Booker, United States Senator from New Jersey
- Eric Garcetti, Mayor of Los Angeles
- Leonard Hoffmann, Baron Hoffmann, English jurist and judge
- Edmund Halley, English astronomer
- King Henry V of England
- Edwin Powell Hubble, American astronomer
- Sir John Peel, gynaecologist to H.M. Queen Elizabeth II
- Leopold Stokowski, conductor.
'Oxford in War-Time'
During the Great War, a man named W. Snow was inspired to write a poem called 'Oxford in War-Time'.
Snow prefaces his poem with the following:
'The Boat Race will not be held this year (1915).
The whole of last year's Oxford eight and the
great majority of the cricket and football teams
are serving the King'.
The poem is as follows:
'Under the tow-path past the barges
Never an eight goes flashing by;
Never a blatant coach on the marge is
Urging his crew to do or die;
Never the critic we knew enlarges,
Fluent, on How and Why!
Once by the Iffley Road November
Welcomed the Football men aglow,
Covered with mud, as you'll remember,
Eager to vanquish Oxford's foe.
Where are the teams of last December?
Gone - where they had to go!
Where are her sons who waged at cricket
Warfare against the foeman-friend?
Far from the Parks, on a harder wicket,
Still they attack and still defend;
Playing a greater game, they'll stick it,
Fearless until the end!
Oxford's goodliest children leave her,
Hastily thrusting books aside;
Still the hurrying weeks bereave her,
Filling her heart with joy and pride;
Only the thought of you can grieve her,
You who have fought and died'.
Sir Tim Berners-Lee
Sir Timothy John Berners-Lee OM KBE FRS RDI FRSA DFBCS FREng was born on the 8th. June 1955. Also known as TimBL, he is an English computer scientist, best known as the inventor of the World Wide Web, the HTML markup language, the URL system, and HTTP.
He is a professorial research fellow at the University of Oxford, and a professor emeritus at the Massachusetts Institute of Technology (MIT).
Berners-Lee proposed an information management system on the 12th. March 1989, and implemented the first successful communication between a Hypertext Transfer Protocol (HTTP) client and server via the Internet in mid-November.
He devised and implemented the first Web browser and Web server, and helped foster the Web's subsequent explosive development. He is the founder and director of the World Wide Web Consortium (W3C), which oversees the continued development of the Web.
Tim co-founded (with Rosemary Leith) the World Wide Web Foundation. In April 2009, he was elected as Foreign Associate of the National Academy of Sciences.
Berners-Lee is a senior researcher and holder of the 3Com founder's chair at the MIT Computer Science and Artificial Intelligence Laboratory (CSAIL). He is a director of the Web Science Research Initiative (WSRI), and a member of the advisory board of the MIT Center for Collective Intelligence.
In 2011, he was named as a member of the board of trustees of the Ford Foundation. He is a founder and president of the Open Data Institute, and is currently an advisor at social network MeWe.
In 2004, Berners-Lee was knighted by Queen Elizabeth II for his pioneering work. He received the 2016 Turing Award:
"... for inventing the World Wide Web, the first
web browser, and the fundamental protocols
and algorithms allowing the Web to scale".
He was named in Time magazine's list of the 100 Most Important People of the 20th. century, and has received many other accolades for his invention.
-- Tim Berners-Lee - The Early Years
Tim Berners-Lee was born in London, the son of mathematicians and computer scientists Mary Lee Woods (1924–2017) and Conway Berners-Lee (1921–2019). His parents were both from Birmingham, and worked on the Ferranti Mark 1, the first commercially-built computer.
He has three younger siblings; his brother, Mike, is a professor of ecology and climate change management.
Berners-Lee attended Sheen Mount Primary School, then attended Emanuel School (a direct grant grammar school at the time) from 1969 to 1973. A keen trainspotter as a child, he learnt about electronics from tinkering with a model railway.
From 1973 to 1976, he studied at The Queen's College, Oxford, where he received a first-class BA in physics. While there, he made a computer out of an old television set he had purchased from a repair shop.
-- Tim Berners-Lee's Career and Research
After graduation, Berners-Lee worked as an engineer at the telecommunications company Plessey in Poole, Dorset.
In 1978, he joined D. G. Nash in Ferndown, Dorset, where he helped create typesetting software for printers.
Berners-Lee worked as an independent contractor at CERN from June to December 1980. While in Geneva, he proposed a project based on the concept of hypertext, to facilitate sharing and updating information among researchers.
To demonstrate it, he built a prototype system named ENQUIRE.
After leaving CERN in late 1980, Tim went to work at John Poole's Image Computer Systems Ltd. in Bournemouth, Dorset, where he ran the company's technical side for three years.
The project he worked on was a "real-time remote procedure call" which gave him experience in computer networking. In 1984, he returned to CERN as a fellow.
In 1989, CERN was the largest Internet node in Europe, and Berners-Lee saw an opportunity to join hypertext with the Internet:
"I just had to take the hypertext idea and
connect it to the TCP and DNS ideas and—
ta-da!—the World Wide Web."
Tim also recalled:
"Creating the web was really an act of desperation,
because the situation without it was very difficult
when I was working at CERN later.
Most of the technology involved in the web, like the
hypertext, like the Internet, multifont text objects,
had all been designed already.
I just had to put them together. It was a step of
generalising, going to a higher level of abstraction,
thinking about all the documentation systems out
there as being possibly part of a larger imaginary
documentation system."
Berners-Lee wrote his proposal in March 1989 and, in 1990, redistributed it. It was accepted by his manager, Mike Sendall, who called his proposals:
"Vague, but exciting."
Robert Cailliau had independently proposed a project to develop a hypertext system at CERN, and joined Berners-Lee as a partner in his efforts to get the web off the ground. They used similar ideas to those underlying the ENQUIRE system to create the World Wide Web, for which Berners-Lee designed and built the first web browser.
Tim's software also functioned as an editor (called WorldWideWeb, running on the NeXTSTEP operating system), and the first Web server, CERN HTTPd (short for Hypertext Transfer Protocol daemon).
Berners-Lee published the first web site, which described the project itself, on the 20th. December 1990; it was available to the Internet from the CERN network.
The site provided an explanation of what the World Wide Web was, and how people could use a browser and set up a web server, as well as how to get started with your own website.
On the 6th. August 1991, Berners-Lee first posted, on Usenet, a public invitation for collaboration with the WorldWideWeb project.
In a list of 80 cultural moments that shaped the world, chosen by a panel of 25 eminent scientists, academics, writers and world leaders, the invention of the World Wide Web was ranked number one, with the entry stating:
"The fastest growing communications medium
of all time, the Internet has changed the shape
of modern life forever. We can connect with
each other instantly, all over the world."
In 1994, Berners-Lee founded the W3C at the Massachusetts Institute of Technology. It comprised various companies that were willing to create standards and recommendations to improve the quality of the Web.
Berners-Lee made his idea available freely, with no patent and no royalties due. The World Wide Web Consortium decided that its standards should be based on royalty-free technology, so that they easily could be adopted by anyone.
In 2001, Berners-Lee became a patron of the East Dorset Heritage Trust, having previously lived in Colehill in Wimborne, East Dorset. In December 2004, he accepted a chair in computer science at the School of Electronics and Computer Science, University of Southampton, Hampshire, to work on the Semantic Web.
In a Times article in October 2009, Berners-Lee admitted that the initial pair of slashes ("//") in a web address were "unnecessary". He told the newspaper that he easily could have designed web addresses without the slashes. In his lighthearted apology he said:
"There you go, it seemed like
a good idea at the time."
-- Tim Berners-Lee's Policy Work
In June 2009, then-British prime minister Gordon Brown announced that Berners-Lee would work with the UK government in order to help make data more open and accessible on the Web, building on the work of the Power of Information Task Force.
Berners-Lee and Professor Nigel Shadbolt are the two key figures behind data.gov.uk, a UK government project to open up almost all data acquired for official purposes for free re-use.
Commenting on the opening up of Ordnance Survey data in April 2010, Berners-Lee said:
"The changes signal a wider cultural change
in government, based on an assumption that
information should be in the public domain
unless there is a good reason not to — not
the other way around."
He went on to say:
"Greater openness, accountability and
transparency in Government will give
people greater choice and make it
easier for individuals to get more
directly involved in issues that matter
to them."
In November 2009, Berners-Lee launched the World Wide Web Foundation (WWWF) in order to campaign:
"To advance the Web to empower humanity
by launching transformative programs that
build local capacity to leverage the Web as
a medium for positive change".
Berners-Lee is one of the pioneer voices in favour of net neutrality, and has expressed the view that:
"ISPs should supply connectivity with no strings
attached, and should neither control nor monitor
the browsing activities of customers without their
expressed consent."
Tim advocates the idea that net neutrality is a kind of human network right:
"Threats to the Internet, such as companies
or governments that interfere with or snoop
on Internet traffic, compromise basic human
network rights."
As of May 2012, Tim is president of the Open Data Institute, which he co-founded with Nigel Shadbolt in 2012.
The Alliance for Affordable Internet (A4AI) was launched in October 2013, and Berners-Lee is leading the coalition of public and private organisations that includes Google, Facebook, Intel and Microsoft.
The A4AI seeks to make Internet access more affordable, so that access is broadened in the developing world, where only 31% of people are online. Berners-Lee is working with those aiming to decrease Internet access prices so that they fall below the UN Broadband Commission's worldwide target of 5% of monthly income.
Berners-Lee holds the founders chair in Computer Science at the Massachusetts Institute of Technology, where he heads the Decentralized Information Group and is leading Solid, a joint project with the Qatar Computing Research Institute that aims to radically change the way Web applications work today, resulting in true data ownership as well as improved privacy.
In October 2016, he joined the Department of Computer Science at Oxford University as a professorial research fellow, and as a fellow of Christ Church, one of the Oxford colleges.
From the mid-2010's Berners-Lee initially remained neutral on the emerging Encrypted Media Extensions (EME) proposal with its controversial digital rights management (DRM) implications.
In March 2017 he felt he had to take a position which was to support the EME proposal. He reasoned EME's virtues whilst noting DRM was inevitable. As W3C director, he went on to approve the finalised specification in July 2017.
Tim's stance was opposed by some, including Electronic Frontier Foundation (EFF), the anti-DRM campaign, Defective by Design, and the Free Software Foundation. Varied concerns raised included being not supportive of the Internet's open philosophy against commercial interests, and risks of users being forced to use a particular web browser to view specific DRM content.
The EFF raised a formal appeal which did not succeed, and the EME specification became a formal W3C recommendation in September 2017.
On the 30th. September 2018, Berners-Lee announced his new open-source startup Inrupt to fuel a commercial ecosystem around the Solid project, which aims to give users more control over their personal data and lets them choose where the data goes, who's allowed to see certain elements and which apps are allowed to see that data.
In November 2019 at the Internet Governance Forum in Berlin Berners-Lee and the WWWF launched Contract for the Web, a campaign initiative to persuade governments, companies and citizens to commit to nine principles to stop "misuse", with the warning that:
"Ff we don't act now – and act together –
to prevent the web being misused by
those who want to exploit, divide and
undermine, we are at risk of squandering
its potential for good."
-- Tim Berners-Lee's Awards and Honours
Tim Berners-Lee's entry in Time magazine's list of the 100 Most Important People of the 20th century (March 1999) reads as follows:
"He wove the World Wide Web and created a mass
medium for the 21st century. The World Wide Web
is Berners-Lee's alone. He designed it. He loosed it
on the world. And he more than anyone else has
fought to keep it open, nonproprietary and free."
Berners-Lee has received many awards and honours. He was knighted by Queen Elizabeth II in the 2004 New Year Honours:
"For services to the global development
of the Internet."
On the 13th. June 2007, he was appointed to the Order of Merit (OM), an order restricted to 24 living members, plus any honorary members. Bestowing membership of the Order of Merit is within the personal purview of the Sovereign, and does not require recommendation by ministers or the Prime Minister.
Tim was elected a Fellow of the Royal Society (FRS) in 2001. He was also elected as a member of the American Philosophical Society in 2004 and the National Academy of Engineering in 2007.
He has been conferred honorary degrees from a number of universities around the world, including Manchester (his parents worked on the Manchester Mark 1 in the 1940's), Harvard and Yale.
In 2012, Berners-Lee was among the British cultural icons selected by artist Sir Peter Blake to appear in a new version of his most famous artwork – the Beatles' Sgt. Pepper's Lonely Hearts Club Band album cover – to celebrate the British cultural figures of his life that he most admires to mark his 80th. birthday.
In 2013, he was awarded the inaugural Queen Elizabeth Prize for Engineering. On the 4th. April 2017, Tim received the 2016 Association for Computing Machinery's Turing Award for his invention of the World Wide Web, the first web browser, and their fundamental protocols and algorithms.
-- Tim Berners-Lee's Personal Life
Berners-Lee has said
"I like to keep work and
personal life separate."
Berners-Lee married Nancy Carlson, an American computer programmer, in 1990. She was also working in Switzerland at the World Health Organization. They had two children and divorced in 2011.
In 2014, he married Rosemary Leith at the Chapel Royal, St. James's Palace in London. Leith is a Canadian Internet and banking entrepreneur, and a founding director of Berners-Lee's World Wide Web Foundation. The couple also collaborate on venture capital to support artificial intelligence companies.
Berners-Lee was raised as an Anglican, but he turned away from religion in his youth. After he became a parent, he became a Unitarian Universalist (UU). When asked whether he believes in God, he stated:
"Not in the sense of most people, I'm
atheist and Unitarian Universalist."
The web's source code was auctioned by Sotheby's in London in 2021, as a non-fungible token (NFT) by TimBL. Selling for US$5,434,500, it was reported the proceeds would be used to fund initiatives by TimBL and Leith.
The Wieliczka Salt Mine located in the town of Wieliczka in southern Poland, lies within the Kraków metropolitan area. The mine, built in the 13th century, produced table salt continuously until 2007, as one of the world's oldest salt mines still in operation. Mining was discontinued in 1996 due to low salt prices and mine flooding.
The mine's attractions include dozens of statues, three chapels and an entire cathedral that has been carved out of the rock salt by the miners. The oldest sculptures are augmented by the new carvings by contemporary artists. About 1.2 million people visit the Wieliczka Salt Mine annually.
(Photo: Christopher Meyers) Gary’s population has fallen to around 80,000 from nearly 180,000 in the 1960s, leaving at least 12,000 abandoned buildings; some must certainly come down but the Gary Heat, Light & Water warehouse shouldn’t be one of them. The utility company—a U.S. Steel subsidiary—commissioned the noted Chicago firm George W. Maher & Son, to design the building. The steel-framed, precast concrete structure shows U.S. Steel did not skimp during the prosperous 1920s. Exterior ornament includes pilaster capitals, cartouches, spandrel panels, dentils, and massive exterior lantern-like light fixtures. The structurally sound building retains original terrazzo floors, plaster details, wood moldings, and a semi-elliptical staircase. The city’s general services department occupied the building for many years but abandoned it more than a decade ago. In 2012 the city declared the building blighted, and targeted it for demolition, but it’s sturdy and adaptable to new uses.
With the exception of the West Wall, the interior of St Martin is a little, OK, a lot disappointing, then the fabric of the church, best seen from outside reveals a mix of Kentish flint and Roman bricks, so I include the next shots, unedited of the exterior of the church, showing the mix of materials.
--------------------------------------------------------
There is old, and there is really old. Well, in this case, ancient.
I must admit that I have not visited many churches in Canterbury: this is not helped by the fact when I go to try to get inside, I find that they are always locked. There is the heritage day, of course, but then there are so many churches to visit on that day, that it is impossible to get round all churches I would like to see.
I first heard about St Martin when researching the history of Canterbury Cathedral and St Augustine's Abbey, and I suppose that without this existing church in the midst of time, the home of the Anglican church, and Christianity could be somewhere else other than Canterbury.
Christianity did survive after the Romans left these shores, it seems likely that the original dedication of this was St Martin of Tours, so when Queen Bertha married Ethelbert, she was already Christian, and it seems used the existing church, dedicated to a saint from her hometown in France.
St Martin lies outside the old City walls, but adjoining the huge St Augustine Abbey site. It is invisible from the main road which runs from the city centre to Sandwich, but there is a simple signpost pointing to the church. However, there is little parking near the church and on the main road, so a 5 minute walk from the city centre is the best way to arrive to the church.
You approach the church up a narrow lane, with just the lychgate in view, and the churchyard rising behind it.
Once through the lychgate, the church is on a slight rise to your right, a short walk up three sets of steps. The entrance is set in the base of the low tower.
I will let John describe the interior, which I concour with, a church with so much history, and so little of interest to see. However, walk round the exterior, and you will see many, many Roman bricks Incorporated into the fabric of the church.
----------------------------------------------------------
Historically, this is the most important church in Kent. St Martin's is the building in which Queen Bertha and St Augustine worshipped together in the closing years of the sixth century, making it the oldest parish church in England that is still in use. Furthermore it is built of large quantities of Roman tile mixed with local flint and ragstone. The exterior shows typical Saxon buttresses and long and short work, but there are no Saxon window openings still in use. However, the west wall inside has been stripped of plaster which allows us to see very early blocked windows. Apart from the great age of the walls there is little of visual interest - with a fourteenth-century tower at the west end and a rather severe atmosphere resulting from the drastic nineteenth-century restoration that saw the insertion of dreadful 'catalogue' stained glass. Were it not for the early history of this church the font would be its outstanding feature. It is of Norman date and is carved from a large block of Caen stone. Tall, solid, and eminently decorative it has intersecting circlets in two lower levels, and arcading of Romanesque arches above, topped by a rim of rolling swags. As a complete contrast to these earl treasures the churchyard contains the grave of Mary Tourtel, creator of Rupert Bear.
www.kentchurches.info/church.asp?p=Canterbury+7
-------------------------------------------------
St Martin’s is the oldest church in continuous use in the English-speaking world. Click here to see the Timeline of St. Martin's
The oldest part of St Martin’s church was built during the Roman occupation of Britain. It is uncertain whether at first the building was a church, a mausoleum, or something else.
Bertha was a Christian princess from Tours, in France. About AD 580 she married Ethelbert of Kent, who was a pagan Anglo-Saxon. Ethelbert restored St Martin’s for her, and she prayed here regularly. Ethelbert became king of Kent and ‘over-king’ of all the kingdoms northwards to the River Humber (200 miles to the north).
Augustine was a Benedictine monk in Rome. He arrived here in AD 597 with 40 companions, including Roman monks and Frankish interpreters, to preach the good news of Jesus Christ. St Martin’s was Augustine’s first base for his mission. “Here they first began to assemble, to sing the psalms, to pray, to celebrate mass, to preach and to baptize, until the king was converted to the faith and gave them greater freedom to preach and to build and restore churches everywhere.” (Bede’s Ecclesiastical History, AD 731).
Bede writes of the enormous impact made by the message of Jesus, by the holy lives of the monks, and by miracles which confirmed the message. “Great numbers gathered each day to hear the word of God, forsaking their heathen rites and entering the unity of Christ’s holy church as believers.” Pope Gregory, who had sent Augustine from Rome, wrote to Augustine telling him not to become swollen-headed because of the extraordinary things that God had chosen to do through him.
Needing more space, they extended St Martin’s to nearly its present size, using Roman building methods and reusing some Roman bricks. The largest part of the building (the nave) was the first Anglo Saxon structure made of mortared brick and stone instead of wood. Ethelbert soon granted Augustine more land in Canterbury, where he founded the Abbey and the Cathedral. Augustine became the first Archbishop of Canterbury. He died in AD 604 and was buried in the Abbey.
The east end of St Martin’s church was extended in the 12-13th centuries and substantially altered in the 19th century. The church tower was added in the 14th century. It has three bells, the largest of which was made in 1393.
St Martin’s remains in use for Christian worship, prayer and mission, as it has done ever since Augustine arrived in the 6th century.
www.martinpaul.org/storyofstmartins.htm
-------------------------------------------------------
The Church of St Martin in Canterbury, England, situated slightly beyond the city centre, is the first church founded in England, the oldest parish church in continuous use and the oldest church in the entire English-speaking world. As such, it is recognised, along with Canterbury Cathedral and St Augustine's Abbey, as part of a World Heritage Site. Since 1668 the church has been part of the benefice of St Martin and St Paul Canterbury. Both St Martin's and nearby St Paul's churches are used for weekly services. The current rector of the parish is the Revd Canon Noelle Hall.
St Martin's was the private chapel of Queen Bertha of Kent in the 6th century before Augustine arrived from Rome. Queen Bertha was a Christian Frankish princess who arrived in England with her Chaplain, Bishop Liudhard. King Æthelberht of Kent, her pagan husband, allowed her to continue to practise her religion by renovating (ca. AD 580) an existing church which the Venerable Bede says had been in use in the late Roman period but had fallen into disuse. As Bede specifically names it, this church was dedicated to Saint Martin of Tours, a city located near where Bertha grew up.
Upon Augustine's arrival he used St Martin's as his mission headquarters, immediately enlarging it (AD 597), and King Æthelberht was soon baptised here. With the quickly subsequent establishments of Canterbury Cathedral and St Augustine's Abbey, St Martin's lost prestige but retains its priority and historical importance.
Shortly before 1844, a hoard of gold coins which may date from the late 6th century was found in the churchyard, one of which is the Liudhard medalet, which bears an image of a diademed figure with a legend referring to Liudhard.
Local finds prove that Christianity did exist in this area of the city at the time, and the church contains many reused Roman bricks or spolia, as well as complete sections of walls of Roman tiles. At the core of the church the brick remains of a Roman tomb were integrated into the structure[3] Several sections of walls are clearly very early, and it is possible that a blocked square-headed doorway in the chancel was the entrance to Bertha's church, while other sections of wall come from the period after the Gregorian mission in the 7th or 8th centuries, including most of the nave. The apse that was originally at the east end has been removed.[4] The tower is much later, in Perpendicular style. The church is a Grade I listed building.
I'll include nearly all the photos of this one, many of which are duds with only a tiny bit in focus. I think it is one that we have found before (at Dip Falls last time) that we (Tony) thought may be a newbie Acanthuchus. Unfortunately it was very adept at getting between the waratah leaves.
The monument includes a late 16th century artillery fort, superseded by and partially incorporated into a mid 17th century bastioned artillery defence, called the Citadel, with associated outworks. The monument also includes a series of alterations and additions made to the Citadel during subsequent centuries, and a statue of George II erected in 1728. The monument is situated on the eastern part of Plymouth Hoe, a limestone cliff overlooking the strategically important entrance to the Cattewater in Plymouth Sound on the south west coast of Devon.
Historical sources provide the context for the construction of the late 16th century artillery fort between 1592-1598 in response to a perceived threat of attack by sea from the Spanish. Although the Armada had been defeated in 1588, fears that Spain would attempt to invade England again led to a strengthening of English defences. The construction of the fort at Plymouth was part of these works. Situated at the east end of the Hoe, it protected the entrance to the important sheltered anchorage of the Cattewater and the harbour in Sutton Pool. Contemporary plans show this fort consisted of two parts: a roughly triangular fort with two bastions pointing to the north and west to defend against landward attack from the Hoe, and the lower fort containing the main armament in ramparts of earth and stone, called bulwarks, along the shore. The stone walls of this fort were about 4m high, and 1.4m thick at the base, accompanied by an outer ditch 6m wide. Guns were mounted on timber staging on earth platforms. The main fort contained the captain's lodgings, barracks, a storehouse, stables, guardhouse, powderhouse and the medieval Chapel of St Katherine on the Hoe, an important landmark for shipping. Parts of this fort have been revealed by partial excavation.
The late 16th century artillery fort was partially incorporated into the mid 17th century Citadel. Although much of the walling around the main area of the earlier fort was demolished as the Citadel was constructed, the lower fort, at the south eastern end of the main 16th century fort was retained. Within the Citadel, the south curtain wall from and including the Cumberland Battery to Prince Henry's Demi-Bastion follows the line of the dividing wall between the 16th century main fort and its lower fort. The Citadel's curtain wall between Prince Edward's Bastion and Prince Henry's Demi-Bastion may also preserve the line of the earlier main fort's east wall. The base of the point of Prince Henry's Demi-Bastion and the sides of Piper's Platform contain some original 16th century stonework and the wall running south east from Piper's Platform towards Fisher's Nose continues the line of the 16th century lower fort wall. Beyond this monument, further walling of the 16th century lower fort is likely to survive along the coastal margin by the blockhouse at Fisher's Nose.
The mid 17th century Citadel was constructed between 1665-1675 in response to another perceived threat of war, this time with the Dutch, rivals for overseas trade with the colonies. Charles II wished to secure Plymouth as a naval base, whose town and hinterland was large enough to victual a large number of ships, and which had a large sheltered anchorage. The Citadel was situated at the east of the Hoe on the site of the late 16th century fortress, retaining the earlier lower fort at its south east end. Designed by Sir Bernard de Gomme, the King's Engineer General, the original plan had been for a regular five bastioned fort to the west of the Elizabethan fort, but was adapted to incorporate as much as possible of the earlier fort and to maintain defence of the Cattewater while it was being built. The resulting Citadel was constructed as a six bastioned walled fortification. The wall was backed by an earth rampart. Beyond the wall was a broad flat-bottomed ditch except on the south east side where it was adjoined by the lower fort. The surface against the outer side of the ditch was levelled to create a covered way, protected by a raised outer lip from which a long outer slope, called a glacis, descended to the surrounding ground surface. Within the ditch, a triangular outwork, called a ravelin, protected the main entrance to the north; the covered way outside the ditch was enlarged on the east and west to create two assembly points for troops, called place d'armes. Beyond this monument, a small rock cut harbour was constructed to the south of the lower fort to supply ships under cover of the Citadel.
By the end of 1667 most of the defensive works had been completed, as had the impressive main gateway, though the interior still required the completion of the ramparts and construction of the buildings needed to house the garrison. Work finished on the Citadel in 1675.
The walls of the Citadel enclose an area approximately 280m east-west by 270m north-south, and survive as an almost complete circuit meeting either side of the northern main entrance. The walls are constructed of limestone quarried from the ditch supplemented by limestone from the two nearby quarries of Lambhay and Tinside. Dartmoor granite was used for the quoins on the corners of the bastions, for the sides of the gun ports, called embrasures, and for the cordon, a rounded horizontal moulding running around the exterior face of the Citadel just below the embrasures. There were also granite corbels or moulded supports for sentry boxes close to the top of the bastions, one of which survives on the north east point of Prince of Wales' Bastion. Originally there were stone sentry boxes on the top of the walls at various points around the Citadel. The only portion of wall which has not survived to its original height is along Prince of Wales' Curtain where it was lowered in the 1890s. The walls are capped with turf, except between Bath's Bastion and Prince Henry's Demi-Bastion where it is capped with asphalt above the later casemates.
The walls form six bastions and one demi-bastion linked by sections of curtain wall; of these only Prince George's Bastion to the north west and King Charles' Bastion to the south west are of regular design. Prince of Wales' Bastion to the north east is truncated because of the steep slope of the ground to the east. Bath's Bastion is extended to link with the line of the earlier fort. The curtain wall from Prince Edward's Bastion towards Prince Henry's Demi-Bastion also links with or possibly follows the line of the earlier fort. The other bastion and the demi-bastion follow the line of the earlier fort. There are several large water tanks, now disused, within Prince George's and King Charles' Curtain walls. Originally there were probably five entrance ways, called sallyports, through the walls. The sallyports have granite doorways or lintels, decorated in each corner above their arched entrance. One sallyport is in the west wall facing the Hoe with a plain arched entrance; another to the south west has a later doorway; one faces south into the lower fort, now facing the Queen's Battery, and another faces south east to Piper's Platform. There was probably a sallyport facing north east before the Prince of Wales' Curtain was taken down. The Queens Battery is a tenaille, a low wall enclosing the area between Cumberland Battery and Prince Henry's Demi-Bastion in front of the curtain wall, it was constructed to provide extra cover for the curtain wall above the lower fort and also gave access to the lower fort.
The ramparts were constructed of earth and stone immediately behind the inner face of the walls and provided platforms for the guns for the defence of the Citadel. The ramparts survive as steep turfed banks and are approximately 8m to 12m thick and 4m to 5m high. Gently sloping inclines or paths up the ramparts' inner faces provided access for the guns and gun carriages; these are now tarmacked but were originally cobbled, as survives in a small area on one incline. Four inclines survive in all: to the west of the main entrance, to King Charles' Bastion, to Bath's Bastion and to Prince Edward's Bastion. Originally there was an incline east of the main entrance and two more between King Charles' Bastion and Prince George's Bastion. The north side of the incline to Prince Edward's Bastion forms three wide shallow steps.
On the ramparts, the gun ports, called embrasures, are backed by granite paved gun platforms, a rectangular area paved with large granite blocks, on which a gun on its carriage would stand. There were embrasures around King Charles' Bastion to the south west, Prince George's Bastion to the north west, Prince Edward's Bastion to the south east and Prince of Wales' Bastion to the north east, and along the west curtain. On the wall facing the ramparts between Cumberland Battery and Prince Henry's Demi-Bastion is a rectangular stone plaque which was probably a name plate for the battery or curtain wall. On King Charles' Bastion four traversing guns were positioned, their metal racers surviving. Similar racers for another traversing gun survive on Prince Henry's Demi-Bastion. Both Bath's Bastion and Queen's Battery have grooves in the granite where the racers for a traversing gun have been. The full length of Cumberland Battery is paved with granite forming interlocking wedge shapes, reflecting its use also as a saluting battery. The positions of former merlons (the solid part of a parapet, between two embrasures) can be seen where the parapet has been made good upon their removal. The brick sills of the former embrasures remain, well weathered, each opposite the earlier phase of wedge shaped granite platforms. Remains of paved gun platforms also survive on the Queen's Battery.
There are four surviving magazine stores on the inner edge of the ramparts, a short length of high wall against which ammunition may have been stored. However the lengths of these walls and the fixing positions for lean to roofs and racking suggest that these may have been side-arms sheds, or stores for ramrods, sponges, traversing staves and ropes. The one along Prince Edward's Bastion is wider than the other three, which are between Prince George's Bastion and King Charles' Bastion. The only section of the ramparts which has been removed, during the 1890s, is along Prince of Wales' Bastion and Curtain wall. The ramparts between Bath's Bastion and Prince Henry's Demi-Bastion were not completed in 1665-1670, when only some masonry arches and piers were built.
The main entrance to the Citadel is in the north wall. It was designed by Sir Thomas Fitch or Fitz, an associate of Sir Christopher Wren. Flanking the arch are paired Ionic pilasters with carved motifs between them. The keystone is adorned with the coat of arms of John Grenville, Earl of Bath. Above the arch is a large niche which probably displayed a statue of Charles II until the early 19th century, when it appears to have fallen and never been replaced; the niche now contains a small pile of four cast-iron spherical mortar bombs. Above the niche is the date 1670 and to either side, a Corinthian column and carved motifs of trophies of arms. The pediment bears the royal coat of arms in relief. Between the large niche and the royal arms is a rectangular stone tablet inscribed `Carolus secundus dei gratia magnae brittaniae franciae et hiberniae'. Originally a guardroom occupied the floor over the arch, later taken down, leaving the decoration above the arch fronting a facade. The interior face of the entrance displays the royal coat of arms above the archway.
EH Listing
At Pevensey Castle
Pevensey Castle: a Saxon Shore fort, Norman defences, a medieval enclosure castle, and later associated remains
The monument includes Anderita Saxon Shore fort, traces of later, Norman defences, an enclosure castle, a 16th century gun emplacement and World War II defences situated on a low spur of sand and clay which now lies around 2km north west of the present East Sussex coastline at Pevensey. During the Roman and medieval periods the spur formed a peninsula projecting into a tidal lagoon and marshland, but coastal deposition and land reclamation have gradually built up the ground around it so that it is now completely land-locked. The roughly oval, north east-south west aligned Roman fort is the earliest of the structures which make up the monument and has been dated to the first half of the fourth century AD. Covering almost 4ha, the fort survives in the form of substantial ruins and buried remains. It is enclosed by a massive defensive wall with a flint and sandstone rubble core faced by coursed greensand and ironstone blocks, interspersed with red tile bonding courses. The whole is up to 3.7m thick and survives to a height of up to 8.1m. The wall was originally topped by a wall walk and parapet. Part excavation in 1906-8 showed that the wall was constructed on footings of rammed chalk and flints underpinned by oak piles and held together by a framework of wooden beams. Investigation of the internal face indicated that this was stepped upwards from a wide base so as to provide extra strength and support. Despite these precautions, a landslip on the south eastern side of the fort has resulted in the destruction of a c.180m length of the perimeter walls and, although fragments of the fallen masonry do survive, most have been removed over the years. Smaller sections of wall have also collapsed along the north western and eastern stretches. The defensive strength provided by the perimeter wall was enhanced by irregularly-spaced, externally projecting semicircular bastions with diameters of around 5m. There were originally at least 15 of these, of which 10 survive today. The fort was entered from its south western, landward approach by way of the main gateway. In front of this a protective ditch 5.5m wide was dug, and, although this became infilled over the years, a 40m stretch located towards its south eastern end has been recut and exposed. The ditch would have been spanned originally by a wooden bridge, although this no longer survives. The main gateway takes the form of a rectangular gatehouse set back between two solid semicircular bastions 8m apart. The 2.7m wide, originally arched entrance is flanked by two oblong guardrooms and the whole gateway structure projects beyond the inner face of the perimeter wall into the fort and is thought to have been originally two or even three storeys high. On the eastern side of the fort is a more simply designed subsidiary gateway, originally a 3m wide archway entrance, giving access to part of the adjacent Roman harbour, now overlain by Pevensey village. The extant archway is a modern reconstruction of the Norman rebuilding of the original entrance. Traces of a wooden causeway which led from it into the fort have been found during partial excavation. Midway along the north western stretch of perimeter wall is a now ruined postern c.2m wide, approached by a curved passage set within the wall. Part excavation between 1906-1908 indicated that the internal buildings which housed the garrison of up to 1,000 men, along with their livestock and supplies, were constructed of timber infilled with wattle and daub. A c.1m sq timber-lined Roman well was found in the south western sector of the fort, at the bottom of which were the remains of the wooden bucket with rope still attached. The well was found to have been filled with rubbish in Roman times and the presence of the bones of cattle, sheep, red deer, wild boar, wild birds, domestic dogs and cats, along with sea shells, gives some indication of the diet and lifestyle of the fort's original inhabitants. Anderita is thought to have been abandoned by its garrison by the latter half of the 4th century AD, and although little is known of its subsequent history until the 11th century, the Anglo-Saxon Chronicle records a massacre of Britons by the invading Saxons at the fort in AD 491. The Bayeux Tapestry states that William the Conquerer landed at Pevensey in 1066, and the Norman army are believed to have made use of the Roman fort as one of their first armed camps. The defences at Pevensey and the surrounding land were granted to King William's half-brother Robert, Count of Mortain. The medieval defences then went through at least 300 years of development, culminating in the construction of a stone built enclosure castle within the largely intact walls of the earlier Roman fort. It is thought that the first Norman defences took the form of a wooden palisade surrounded by a bank and ditch, and a c.40m length of partially infilled ditch up to 9m wide which survives across the north eastern sector of the earlier fort may indicate their original extent. Limited excavations in 1993-94 showed that the ground surface in the south eastern sector of the fort, in the vicinity of the later stone-built keep, was artificially raised some time before 1200, suggesting that a motte may also have been constructed. The original Roman gateways were rebuilt and a new ditch dug in front of the south western gate. Most of the Norman defences and interior wooden buildings will now survive in buried form beneath the later medieval castle, although herringbone-pattern repairs to the Roman masonry, by then serving as the outer bailey of the medieval defences, also date from this time. Around 1100 the defences were strengthened and the accommodation improved by the addition of a masonry keep in the south eastern sector of the earlier fort. The subject of a complex history of alteration, collapse and repair, the keep utilises part of the earlier, Roman perimeter wall and bastions. It takes the form of a rectangular block measuring c.16.8m by c.9m internally, reinforced by apsidal projections on all sides. Now surviving in ruined form up to first floor level, the keep originally took the form of a tall tower with an entrance on the first floor. A rectangular building measuring 7.6m by 6m was later constructed in the south eastern angle between the keep and the Roman wall. At around 1200 work began on the construction of a smaller, stone-built inner bailey in the south eastern sector of the earlier fort. An L-shaped ditch around 20m wide was dug to define the new enclosure, and this retains water in its northern arm. The material excavated from the ditch and from the destruction of the earlier bank was spread over much of the outer bailey to a depth of up to 1.5m. The ditch was recut during extensive renovations carried out during the early 20th century. The first structure to be built in this phase was the gatehouse to the south west which has an arched entrance between twin, semicircular external towers, now ruined. The basement chambers beneath each tower have ashlar-faced walls and barrel-vaulted ceilings, the southern chamber being entered by way of a newel staircase, the northern by a trapdoor. Both were used to house prisoners. Many subsequent alterations included the replacement, during the 15th century, of the wooden bridge over the outer ditch by a stone causeway. The originally embattled curtain wall enclosing the inner bailey was built within the ditch and inner berm around 1250. This survives almost to its full original height and is faced with coursed Greensand ashlar. Three semicircular external towers provided flanking cover from the narrow embrasures which pierce their walls. Each has a narrow staircase to a basement, a branch staircase off it into the ditch and a room and garderobe, or latrine, at ground floor level. Upper rooms were entered by way of the wall walk and were heated by fireplaces. The basement of the northernmost tower has two rib-vaulted bays, the keeled ribs resting on stiff-leaf corbels. The interior castle buildings continued to be built mainly of wood and these will survive in buried form, although the stone foundations of a chapel were exposed during partial excavation of the northern sector of the inner bailey. Around 20m south east of the chapel is a large stone-lined well at least 15.5m deep, and near this is a pile of medieval stone missile-balls, a selection of those recovered from the ditch. These were thrown from trebuchets during the four sieges of the castle. William, Count of Mortain forfeited Pevensey after an unsuccessful rebellion against Henry I in 1101 and the castle, which remained in the royal gift until the later Middle Ages, passed into the hands of the de Aquila family. The most famous siege took place in 1264-65 when the supporters of Henry III, fleeing from their defeat by the Barons at Lewes, took refuge in the castle. In 1372 the castle was given to John of Gaunt, and during his period of office was used to imprison James I, King of Scotland, who had been seized in 1406, and Joan, Queen of Navarre, accused of witchcraft by her stepson, Henry V. By 1300, the sea had gradually begun to recede from around the castle and its military importance declined as a result. Contemporary records show that the castle walls were constantly in need of expensive repair and by the end of the 14th century were not being properly maintained, although the roof leads were kept intact until the middle of the 15th century. By 1500 the castle had ceased to be inhabited and fell rapidly into decay. The threat of the Spanish Armada led to some renewed interest in the defensive value of the site, and a survey of 1587 records that the castle housed two demi-culverins, or heavy guns. These were sited on the contemporary, south east orientated, M-shaped earthen gun emplacement situated in the outer bailey around 90m north east of the main Roman gateway. This takes the form of a raised level platform c.20m long bounded on the seaward side by a slight bank c.0.4m high and around 3m wide. One of the cast iron guns, manufactured in the East Sussex Weald, is now housed within the inner bailey on a modern replica carriage. From the 17th century the castle passed through the hands of various private owners. Valued as a picturesque ruin during the 18th and 19th centuries, it features in many contemporary engravings and illustrations. In 1925 the Duke of Devonshire presented the monument to the state, and extensive repairs began with a view to opening the monument to the public. These were interrupted by the outbreak of World War II, when the castle resumed its original military purpose of protecting the south coast. The castle was refortified in May 1940 as an observation and command post. It was continuously occupied by regular troops, including Canadian forces and the United States Army Air Corps, who used it as a radio direction centre, and by the Home Guard until 1944. The World War II defences include two pillboxes and three machine gun posts of concrete faced with rubble and flints, carefully concealed and camouflaged within the earlier Roman and medieval fabric. An internal tower was built just to the south of the Roman east gateway and a blockhouse housing anti-tank weapons was built in front of the main Roman gateway. The blockhouse no longer survives. Modifications carried out to the medieval mural towers included lining the interiors with brick and inserting wooden floors. In 1945 the monument was returned to peaceful use and is now in the guardianship of the Secretary of State and open to the public.
[Historic England]
At Pevensey Castle
Pevensey Castle: a Saxon Shore fort, Norman defences, a medieval enclosure castle, and later associated remains
The monument includes Anderita Saxon Shore fort, traces of later, Norman defences, an enclosure castle, a 16th century gun emplacement and World War II defences situated on a low spur of sand and clay which now lies around 2km north west of the present East Sussex coastline at Pevensey. During the Roman and medieval periods the spur formed a peninsula projecting into a tidal lagoon and marshland, but coastal deposition and land reclamation have gradually built up the ground around it so that it is now completely land-locked. The roughly oval, north east-south west aligned Roman fort is the earliest of the structures which make up the monument and has been dated to the first half of the fourth century AD. Covering almost 4ha, the fort survives in the form of substantial ruins and buried remains. It is enclosed by a massive defensive wall with a flint and sandstone rubble core faced by coursed greensand and ironstone blocks, interspersed with red tile bonding courses. The whole is up to 3.7m thick and survives to a height of up to 8.1m. The wall was originally topped by a wall walk and parapet. Part excavation in 1906-8 showed that the wall was constructed on footings of rammed chalk and flints underpinned by oak piles and held together by a framework of wooden beams. Investigation of the internal face indicated that this was stepped upwards from a wide base so as to provide extra strength and support. Despite these precautions, a landslip on the south eastern side of the fort has resulted in the destruction of a c.180m length of the perimeter walls and, although fragments of the fallen masonry do survive, most have been removed over the years. Smaller sections of wall have also collapsed along the north western and eastern stretches. The defensive strength provided by the perimeter wall was enhanced by irregularly-spaced, externally projecting semicircular bastions with diameters of around 5m. There were originally at least 15 of these, of which 10 survive today. The fort was entered from its south western, landward approach by way of the main gateway. In front of this a protective ditch 5.5m wide was dug, and, although this became infilled over the years, a 40m stretch located towards its south eastern end has been recut and exposed. The ditch would have been spanned originally by a wooden bridge, although this no longer survives. The main gateway takes the form of a rectangular gatehouse set back between two solid semicircular bastions 8m apart. The 2.7m wide, originally arched entrance is flanked by two oblong guardrooms and the whole gateway structure projects beyond the inner face of the perimeter wall into the fort and is thought to have been originally two or even three storeys high. On the eastern side of the fort is a more simply designed subsidiary gateway, originally a 3m wide archway entrance, giving access to part of the adjacent Roman harbour, now overlain by Pevensey village. The extant archway is a modern reconstruction of the Norman rebuilding of the original entrance. Traces of a wooden causeway which led from it into the fort have been found during partial excavation. Midway along the north western stretch of perimeter wall is a now ruined postern c.2m wide, approached by a curved passage set within the wall. Part excavation between 1906-1908 indicated that the internal buildings which housed the garrison of up to 1,000 men, along with their livestock and supplies, were constructed of timber infilled with wattle and daub. A c.1m sq timber-lined Roman well was found in the south western sector of the fort, at the bottom of which were the remains of the wooden bucket with rope still attached. The well was found to have been filled with rubbish in Roman times and the presence of the bones of cattle, sheep, red deer, wild boar, wild birds, domestic dogs and cats, along with sea shells, gives some indication of the diet and lifestyle of the fort's original inhabitants. Anderita is thought to have been abandoned by its garrison by the latter half of the 4th century AD, and although little is known of its subsequent history until the 11th century, the Anglo-Saxon Chronicle records a massacre of Britons by the invading Saxons at the fort in AD 491. The Bayeux Tapestry states that William the Conquerer landed at Pevensey in 1066, and the Norman army are believed to have made use of the Roman fort as one of their first armed camps. The defences at Pevensey and the surrounding land were granted to King William's half-brother Robert, Count of Mortain. The medieval defences then went through at least 300 years of development, culminating in the construction of a stone built enclosure castle within the largely intact walls of the earlier Roman fort. It is thought that the first Norman defences took the form of a wooden palisade surrounded by a bank and ditch, and a c.40m length of partially infilled ditch up to 9m wide which survives across the north eastern sector of the earlier fort may indicate their original extent. Limited excavations in 1993-94 showed that the ground surface in the south eastern sector of the fort, in the vicinity of the later stone-built keep, was artificially raised some time before 1200, suggesting that a motte may also have been constructed. The original Roman gateways were rebuilt and a new ditch dug in front of the south western gate. Most of the Norman defences and interior wooden buildings will now survive in buried form beneath the later medieval castle, although herringbone-pattern repairs to the Roman masonry, by then serving as the outer bailey of the medieval defences, also date from this time. Around 1100 the defences were strengthened and the accommodation improved by the addition of a masonry keep in the south eastern sector of the earlier fort. The subject of a complex history of alteration, collapse and repair, the keep utilises part of the earlier, Roman perimeter wall and bastions. It takes the form of a rectangular block measuring c.16.8m by c.9m internally, reinforced by apsidal projections on all sides. Now surviving in ruined form up to first floor level, the keep originally took the form of a tall tower with an entrance on the first floor. A rectangular building measuring 7.6m by 6m was later constructed in the south eastern angle between the keep and the Roman wall. At around 1200 work began on the construction of a smaller, stone-built inner bailey in the south eastern sector of the earlier fort. An L-shaped ditch around 20m wide was dug to define the new enclosure, and this retains water in its northern arm. The material excavated from the ditch and from the destruction of the earlier bank was spread over much of the outer bailey to a depth of up to 1.5m. The ditch was recut during extensive renovations carried out during the early 20th century. The first structure to be built in this phase was the gatehouse to the south west which has an arched entrance between twin, semicircular external towers, now ruined. The basement chambers beneath each tower have ashlar-faced walls and barrel-vaulted ceilings, the southern chamber being entered by way of a newel staircase, the northern by a trapdoor. Both were used to house prisoners. Many subsequent alterations included the replacement, during the 15th century, of the wooden bridge over the outer ditch by a stone causeway. The originally embattled curtain wall enclosing the inner bailey was built within the ditch and inner berm around 1250. This survives almost to its full original height and is faced with coursed Greensand ashlar. Three semicircular external towers provided flanking cover from the narrow embrasures which pierce their walls. Each has a narrow staircase to a basement, a branch staircase off it into the ditch and a room and garderobe, or latrine, at ground floor level. Upper rooms were entered by way of the wall walk and were heated by fireplaces. The basement of the northernmost tower has two rib-vaulted bays, the keeled ribs resting on stiff-leaf corbels. The interior castle buildings continued to be built mainly of wood and these will survive in buried form, although the stone foundations of a chapel were exposed during partial excavation of the northern sector of the inner bailey. Around 20m south east of the chapel is a large stone-lined well at least 15.5m deep, and near this is a pile of medieval stone missile-balls, a selection of those recovered from the ditch. These were thrown from trebuchets during the four sieges of the castle. William, Count of Mortain forfeited Pevensey after an unsuccessful rebellion against Henry I in 1101 and the castle, which remained in the royal gift until the later Middle Ages, passed into the hands of the de Aquila family. The most famous siege took place in 1264-65 when the supporters of Henry III, fleeing from their defeat by the Barons at Lewes, took refuge in the castle. In 1372 the castle was given to John of Gaunt, and during his period of office was used to imprison James I, King of Scotland, who had been seized in 1406, and Joan, Queen of Navarre, accused of witchcraft by her stepson, Henry V. By 1300, the sea had gradually begun to recede from around the castle and its military importance declined as a result. Contemporary records show that the castle walls were constantly in need of expensive repair and by the end of the 14th century were not being properly maintained, although the roof leads were kept intact until the middle of the 15th century. By 1500 the castle had ceased to be inhabited and fell rapidly into decay. The threat of the Spanish Armada led to some renewed interest in the defensive value of the site, and a survey of 1587 records that the castle housed two demi-culverins, or heavy guns. These were sited on the contemporary, south east orientated, M-shaped earthen gun emplacement situated in the outer bailey around 90m north east of the main Roman gateway. This takes the form of a raised level platform c.20m long bounded on the seaward side by a slight bank c.0.4m high and around 3m wide. One of the cast iron guns, manufactured in the East Sussex Weald, is now housed within the inner bailey on a modern replica carriage. From the 17th century the castle passed through the hands of various private owners. Valued as a picturesque ruin during the 18th and 19th centuries, it features in many contemporary engravings and illustrations. In 1925 the Duke of Devonshire presented the monument to the state, and extensive repairs began with a view to opening the monument to the public. These were interrupted by the outbreak of World War II, when the castle resumed its original military purpose of protecting the south coast. The castle was refortified in May 1940 as an observation and command post. It was continuously occupied by regular troops, including Canadian forces and the United States Army Air Corps, who used it as a radio direction centre, and by the Home Guard until 1944. The World War II defences include two pillboxes and three machine gun posts of concrete faced with rubble and flints, carefully concealed and camouflaged within the earlier Roman and medieval fabric. An internal tower was built just to the south of the Roman east gateway and a blockhouse housing anti-tank weapons was built in front of the main Roman gateway. The blockhouse no longer survives. Modifications carried out to the medieval mural towers included lining the interiors with brick and inserting wooden floors. In 1945 the monument was returned to peaceful use and is now in the guardianship of the Secretary of State and open to the public.
[Historic England]
View includes The Lake and Jacqueline Kennedy Onassis Reservoir in Central Park, the Metropolitan Museum of Art, the Hilton New York hotel, Financial Times Building and Burlington House on Avenue of the Americas, the 'Black Rock' CBS Building on West 52nd Street, the Solow Building on West 57th Street, the General Motors Building and Trump Tower on Fifth Avenue, and 712 Fifth Avenue.
Taken from the Top of the Rock observation deck at the top of the GE Building. The views are awesome and much better than those from the Empire State Building.
PC180169