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10217 – Diagon Alley™
Ages 14+. 2,025 pieces.
US $ 149.99 CA $ 199.99 UK £ 132.75 DE 149.99 €
Expand your very own wizarding world of Harry Potter™!
No need to pass through the Leaky Cauldron. Now even Muggles can shop in Diagon Alley by building this fantastically magical set that includes 3 extensively detailed buildings and 11 minifigures! Join Harry Potter, Ron Weasley and Hermione Granger as they shop for their Hogwarts school supplies. Visit Ollivanders, Borgin and Burkes, and Gringotts Bank. Each Diagon Alley building is realistically detailed. Ollivanders offers an extensive selection of wands, storage shelves and a step ladder that allows Ollivander to gather wands from the top floor. The front desk has an “exploding” function for those inconvenient times when a spell goes awry. Borgin and Burkes includes a scary skeleton, “glow-in-the-dark” elements, a fireplace attached to the Floo Network and a Vanishing Cabinet that Dark wizards might use to sneak into Hogwarts. Gringotts Bank is an impressive two-story building with large double doors, and can be opened completely into one large building or closed to create one smaller building. The bank’s interior features a removable vault, along with the Philosopher’s Stone, a clerk’s desk, a chandelier and ‘wonky’ support pillars. Includes 11 minifigures: Harry Potter, Ron Weasley and Hermione Granger, each with magic wand; Rubeus Hagrid, equipped with his pink umbrella; Fred and George Weasley; 2 Gringotts goblins; Mr. Ollivander; Lucius Malfoy (with Death Eater disguise); Fenrir Greyback; and 4 new, decorated owls.
• Includes 11 minifigures: Harry Potter, Ron Weasley and Hermione Granger, each with magic wand; Rubeus Hagrid, equipped with his pink umbrella; Fred and George Weasley; 2 Gringotts goblins; Mr. Ollivander; Lucius Malfoy (with Death Eater disguise); Fenrir Greyback; and 4 new, decorated owls!
• Diagon Alley is made up of 3 extensively detailed buildings: Ollivanders, Borgin and Burkes and Gringotts Bank!
• Ollivanders features lots of wands, storage shelves and a step ladder that leads to the top floor!
• Front desk at Ollivanders has an “exploding” function!
• Borgin and Burkes includes a skeleton, “glow-in-the-dark” elements, fireplace attached to the Floo Network and even a Vanishing Cabinet!
• Gringotts Bank is a two-story building featuring large double doors!
• Open Gringotts Bank completely into one large building and explore inside or close it to create a smaller building!
• Gringotts Bank features a detailed interior with a removable vault, the Philosopher’s Stone, clerk’s desk, chandelier and ‘wonky’ support pillars!
• Includes 11 minifigures: Harry Potter, Ron Weasley and Hermione Granger, each with magic wand; Rubeus Hagrid, equipped with his pink umbrella; Fred and George Weasley; 2 Gringotts goblins; Mr. Ollivander; Lucius Malfoy (with Death Eater disguise); Fenrir Greyback; and 4 new, decorated owls!
• Ollivanders measures 8" (20 cm) high and 5" (13 cm) wide!
• Borgin and Burkes measures 8" (20 cm) high and 7" (18 cm) wide!
• Gringotts Bank measures 8" (21 cm) high and 4" (10 cm) wide when closed, 8" high and 9" (23 cm) wide when opened wide!
• Completed model (depending on how much space is allocated between individual parts) measures 24" (60 cm) long and 12" (30 cm) deep and 8" (21 cm) high!
Available for order directly through LEGO® beginning January 2011 via shop.LEGO.com or via phone
includes 4 zines and a shit ton of stickers made by Pacolli and I. Available for sale at High in the Bay
This site includes a very active flare stack and mini-compressors.
Photo citation: Ted Auch, FracTracker Alliance, 2021.
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Death Valley National Park is an American national park that straddles the California–Nevada border, east of the Sierra Nevada. The park boundaries include Death Valley, the northern section of Panamint Valley, the southern section of Eureka Valley, and most of Saline Valley. The park occupies an interface zone between the arid Great Basin and Mojave deserts, protecting the northwest corner of the Mojave Desert and its diverse environment of salt-flats, sand dunes, badlands, valleys, canyons, and mountains. Death Valley is the largest national park in the contiguous United States, and the hottest, driest and lowest of all the national parks in the United States. The second-lowest point in the Western Hemisphere is in Badwater Basin, which is 282 feet (86 m) below sea level. Approximately 91% of the park is a designated wilderness area. The park is home to many species of plants and animals that have adapted to this harsh desert environment. Some examples include creosote bush, bighorn sheep, coyote, and the Death Valley pupfish, a survivor from much wetter times. UNESCO included Death Valley as the principal feature of its Mojave and Colorado Deserts Biosphere Reserve in 1984.
A series of Native American groups inhabited the area from as early as 7000 BC, most recently the Timbisha around 1000 AD who migrated between winter camps in the valleys and summer grounds in the mountains. A group of European Americans, trapped in the valley in 1849 while looking for a shortcut to the gold fields of California, gave the valley its name, even though only one of their group died there. Several short-lived boom towns sprang up during the late 19th and early 20th centuries to mine gold and silver. The only long-term profitable ore to be mined was borax, which was transported out of the valley with twenty-mule teams. The valley later became the subject of books, radio programs, television series, and movies. Tourism expanded in the 1920s when resorts were built around Stovepipe Wells and Furnace Creek. Death Valley National Monument was declared in 1933 and the park was substantially expanded and became a national park in 1994.
The natural environment of the area has been shaped largely by its geology. The valley is actually a graben with the oldest rocks being extensively metamorphosed and at least 1.7 billion years old. Ancient, warm, shallow seas deposited marine sediments until rifting opened the Pacific Ocean. Additional sedimentation occurred until a subduction zone formed off the coast. The subduction uplifted the region out of the sea and created a line of volcanoes. Later the crust started to pull apart, creating the current Basin and Range landform. Valleys filled with sediment and, during the wet times of glacial periods, with lakes, such as Lake Manly.
Source: Wikipedia
The BLM manages about 864,000 acres in its Medford district and some of that land includes portions of the famous Pacific Crest Trail, or PCT.
The 43-mile stretch of PCT in southern Oregon includes countless scenic views and well-known recreation points: Mount Shasta; Pilot Rock, Hyatt Lake; Soda Mountain Wilderness; and the Cascade-Siskiyou National Monument, to name a few.
Hikers will also be able to experience a variety of natural environments, from wildflower meadows to old growth forests and rocky bluffs.
This photo was captured in the summer of 2015.
How to access the PCT on southern Oregon public lands managed by the BLM: www.blm.gov/or/resources/recreation/csnm/csnm-pct.php
We have expanded the color range of PRECIOSA Rocailles for you to include new natural colors!
We offer you the PRECIOSA Traditional Czech Beads™ rocaille range in newly developed and unique shades of light lilac and pink. This involves an exceptional change in our standard extensive color range after many years.
Don't miss the opportunity to get your hands on the seed beads in these delicate tones. They are excellent in children's costume jewelry collections, hair decorations or various tassels. The time of brides is also fast approaching. Decorate and adorn your unforgettable day with seed beads in the new glass colors!
The shades of delicate pink and lilac in opaque colors and transparent lilac can also be beautified with the sfinx and rainbow surface finishes. See for yourself.
You will love the unique extended color range of these glass seed beads!
TECHNICAL DATA:
PRECIOSA Rocailles
Article number: 311 19 001
Size: 1/0, 6/0, 8/0, 10/0, 11/0 (opaque pink 73420 and opaque lilac 23420)
Size: 1/0, 6/0, 8/0 (transparent lilac 20420)
Article number: 331 19 001
Size: 6/0 (the sfinx and rainbow finishes)
The Sfinx Finish
78420 (on opaque pink)
28420 (on opaque lilac)
28420 (on opaque lilac)
The Rainbow Finish
74420 (on opaque pink)
24420 (on opaque lilac)
21420 (on transparent lilac)
Visit our website for more information about the PRECIOSA New Seed Beads Colors
Harajuku is an area between Shinjuku and Shibuya. Local landmarks include the headquarters of NHK, Meiji Shrine, and Yoyogi Park.
The area has two main shopping streets, Omotesando and Takeshita Street (Takeshita-dori). The latter caters to youth fashions and has many small stores selling Gothic Lolita, visual kei, rockabilly, hip hop, and punk outfits, in addition to fast food outlets and so forth.
Omotesando has recently seen a rise in openings of up-scale fashion shops such as Louis Vuitton, Chanel, and Prada. The avenue is sometimes referred to as the Champs-Élysées of Tokyo. Until 2004, one side of the avenue was occupied by the Dojunkai Aoyama apato, Bauhaus-inspired apartments built in 1927 after the 1923 Kanto earthquake. In 2006 the buildings were controversially destroyed by Mori Building and replaced with the "Omotesando Hills" shopping mall, designed by Tadao Ando. The area known as "Ura-Hara", back streets of Harajuku, is a center of Japanese fashion for younger people—brands such as A Bathing Ape and Undercover have shops in the area.
From "all but 4 wheels", the theme for the May Goodwood Breakfast Club. This BMW Isetta 3-wheeler looked very cosy for two.
Includes a episode of the hit series A Pup Named Scooby Doo from 1988 and a behind the sceens look at this film
Lime Rock Park Weathertech IMSA weekend July 2018. Classes include IMSA WeatherTech and the Continental Tire Sportscar Challenge.
Includes wing quivering or trembling ( possible submissive courtship behaviour0. Strathspey, Scotland in bird cherry. Bird song audible includes wrem.
Action from the Animal WD40 Action Sports Tour at the Paddle Round the Pier event in Brighton. Hot and sunny - so the event and the beach was packed. Excellent skills from the cyclists and the parkour gymnast
The Baker City Memory Cruise includes a show and shine at Baker City’s Geiser Pollman Park, a cruise through historic downtown Baker City and ends with the cars on display at Quail Ridge Golf Course during the Annual Durkee Steak Feed
For more information about the Baker City Memory Cruise, Quail Ridge Golf Course or the Durkee Steak Feed, visit the Baker County Tourism website www.basecampbaker.com/ or become a fan at www.facebook.com/basecampbaker
Our mural includes a depiction of 4 distinct female mermaid characters. They appear in progressive stages from resting, to sitting, to rising, to the more adventurous action of swimming off to explore the deep. the composition of the figures wraps around the wall from narrow to full wall height as a representation of shallow to deep water. The mural will contain elements of sea and underwater life, such as fish, kelp and skulls. Our mural strongly depicts female collaboration through our combined approach of working background elements, as well as the interaction between our mermaid characters. Through the progression of colour scheme, shallow to deep water, and the actions of the mermaids, we intend to work within a theme of transformation, as well as an awareness for the ocean and our Pacific West Coast.
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
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.[
is not only all that is visible to the eye.. it also includes the inner pictures of the soul.
Edvard Munch
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)
More from the Historic Masters Festival, Brands Hatch. Inside the Druids Hairpin is a great place to practice your panning
The Kerala backwaters are a chain of brackish lagoons and lakes lying parallel to the Arabian Sea coast (known as the Malabar Coast) of Kerala state in southern India. The network includes five large lakes linked by canals, both manmade and natural, fed by 38 rivers, and extending virtually half the length of Kerala state. The backwaters were formed by the action of waves and shore currents creating low barrier islands across the mouths of the many rivers flowing down from the Western Ghats range.
The Kerala Backwaters are a network of interconnected canals, rivers, lakes and inlets, a labyrinthine system formed by more than 900 km of waterways, and sometimes compared to the American Bayou. In the midst of this landscape there are a number of towns and cities, which serve as the starting and end points of backwater cruises. National Waterway No. 3 from Kollam to Kottapuram, covers a distance of 205 km and runs almost parallel to the coast line of southern Kerala facilitating both cargo movement and backwater tourism.
The backwaters have a unique ecosystem - freshwater from the rivers meets the seawater from the Arabian Sea. In certain areas, such as the Vembanad Kayal, where a barrage has been built near Kumarakom, salt water from the sea is prevented from entering the deep inside, keeping the fresh water intact. Such fresh water is extensively used for irrigation purposes.
Many unique species of aquatic life including crabs, frogs and mudskippers, water birds such as terns, kingfishers, darters and cormorants, and animals such as otters and turtles live in and alongside the backwaters. Palm trees, pandanus shrubs, various leafy plants and bushes grow alongside the backwaters, providing a green hue to the surrounding landscape.
Vembanad Kayal is the largest of the lakes, covering an area of 200 km², and bordered by Alappuzha (Alleppey), Kottayam, and Ernakulam districts. The port of Kochi (Cochin) is located at the lake's outlet to the Arabian Sea. Alleppey, "Venice of the East", has a large network of canals that meander through the town. Vembanad is India’s longest lake.
HOUSE BOATS
The kettuvallams (Kerala houseboats) in the backwaters are one of the prominent tourist attractions in Kerala. More than 2000 kettuvallams ply the backwaters, 120 of them in Alappuzha. Kerala government has classified the tourist houseboats as Platinum, Gold and silver.
The kettuvallams were traditionally used as grain barges, to transport the rice harvested in the fertile fields alongside the backwaters. Thatched roof covers over wooden hulls, 30 m in length, provided protection from the elements. At some point in time the boats were used as living quarters by the royalty. Converted to accommodate tourists, the houseboats have become floating cottages having a sleeping area, with western-style toilets, a dining area and a sit out on the deck. Most tourists spend the night on a house boat. Food is cooked on board by the accompanying staff – mostly having a flavour of Kerala. The houseboats are of various patterns and can be hired as per the size of the family or visiting group. The living-dining room is usually open on at least three sides providing a grand view of the surroundings, including other boats, throughout the day when it is on the move. It is brought to a standstill at times of taking food and at night. After sunset, the boat crew provide burning coils to drive away mosquitoes. Ketuvallams are motorised but generally proceed at a slow speed for smooth travel. All ketuvallams have a generator and most bedrooms are air-conditioned. At times, as per demand of customers, electricity is switched off and lanterns are provided to create a rural setting.
While many ketuvalloms take tourists from a particular point and bring them back to around the same point next morning there are some specific cruises mostly in the Alappuzha area, such as the one night cruise from Alappuzha to Thotapally via Punnamada Lake two nights cruise from Alappuzha to Alumkavadi,[8] one night cruise from Alappuzha to Kidangara, and one night cruise from Alappuzha to Mankotta. There are numerous such cruises.
Beypore, located 10 km south of Kozhikode at the mouth of the Chaliyar River, is a famous fishing harbour, port and boat building centre. Beypore has a 1,500 year-tradition of boatbuilding. The skill of the local shipwrights and boat builders are widely sought after. There is a houseboat-building yard at Alumkadavu, in Ashtamudi Kayal near Kollam.
FERRY SERVICES
Regular ferry services connect most locations on both banks of the backwaters. The Kerala State Water Transport Department operates ferries for passengers as well as tourists. It is the cheapest mode of transport through the backwaters.
ECONOMIC SIGNIFICANCE
Connected by artificial canals, the backwaters form an economical means of transport, and a large local trade is carried on by inland navigation. Fishing, along with fish curing is an important industry.
Kerala backwaters have been used for centuries by the local people for transportation, fishing and agriculture. It has supported the efforts of the local people to earn a livelihood. In more recent times, agricultural efforts have been strengthened with reclamation of some backwater lands for rice growing, particularly in the Kuttanad area. Boat making has been a traditional craft, so has been the coir industry.
Kuttanad is crisscrossed with waterways that run alongside extensive paddy fields, as well as fields of cassava, banana and yam. A unique feature of Kuttanad is that many of these fields are below sea level and are surrounded by earthen embankments. The crops are grown on the low-lying ground and irrigated with fresh water from canal and waterways connected to Vembanad lake. The area is similar to the dikes of the Netherlands where land has been reclaimed from the sea and crops are grown.
WIKIPEDIA
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 Alpine Accentor is one of the few song birds still found at altitudes higher than 5000m in the Himalaya.
For any form of publication, please include the link to this page: www.grida.no/resources/4142
This photo has been graciously provided to be used in the GRID-Arendal resources library by: Wenzel Prokosch
The Dallas Arts District's "Spotlight Sunday" on October 18
Festivities to celebrate the opening of the new AT&T Performing Arts Center include a day of free admission and extended hours. Enjoy performances in the exhibition All the World’s a Stage, tours family experiences, and much more.
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The Dallas Arts District
2200 Ross Ave
Dallas, TX 75201
(214) 744-6642
The Dallas Arts District is a unique, 68-acre, 19-block neighborhood in the heart of the city. A rare jewel that is the centerpiece of the region’s cultural life, the District is home to some of the finest architecture in the world. Enhancing the downtown Dallas skyline are buildings by Pritzker Prize winners I.M. Pei, Renzo Piano, Norman Foster, Rem Koolhaas and AIA “Gold Medal” recipient Edward Larrabee Barnes.
Our neighborhood is a center for innovative architecture, world-class exhibits, exemplary cultural programming and much more. We are restaurants, hotels, churches, residences and even the world headquarters of 7-Eleven.
This website is designed to help you explore the many facets of the district. And whether you are coming from around the corner or from around the world, we hope you will find your trip enjoyable and your experience unparalleled.
We look forward to sharing with you the works of art, the performances, the cuisine and the vibrancy of the Dallas Arts District.
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Dallas Museum of Art
The Dallas Museum of Art ranks among leading art institutions in the country and is distinguished by its innovative exhibitions and groundbreaking educational programs.
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Nasher Sculpture Center
The Nasher Sculpture Center opened in 2003 as the first institution in the world dedicated exclusively to the exhibition of modern and contemporary sculpture with a collection of global significance at its foundation.
www.nashersculpturecenter.org/
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Trammell Crow Center and Crow Collection of Asian Art
The Trammell and Margaret Crow Collection of Asian Art is nestled like a small jewel in Dallas’ Arts District, offering visitors a glimpse of a world possessing serene beauty and spirituality in the heart of a bustling city.
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Belo Mansion
The current home of the Dallas Bar Association, the Belo Mansion was built c. 1890 by Coleonel A. H. Belo, founder of the Dallas Morning News.
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Cathedral Shrine of the Virgin of Guadalupe
The city’s oldest Catholic parish, this High Victorian Gothic cathedral is the second busiest Catholic cathedral in the nation.
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Morton H. Meyerson Symphony Center
Since its grand opening celebration, the legendary rich sound of the Meyerson’s Eugene McDermott Concert Hall has made it a premier destination for the world’s finest soloists and conductors.
www.dallasculture.org/meyersonSymphonyCenter/
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AT&T Performing Arts Center Margot and Bill Winspear Opera House
With transparent, soaring 60-foot glass walls revealing views of the Grand Lobby and a café open throughout the day, the Winspear Opera House is a destination for all.
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AT&T Performing Arts Center Dee and Charles Wyly Theatre
The world’s only vertical theatre, the innovative design of the Wyly Theatre creates ultimate performance flexibility.
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Booker T. Washington High School for the Visual and Performing Arts
The school’s dual emphasis on arts and academics has produced a stellar list of famous graduates including Grammy Award®-winners Norah Jones, Erykah Badu and jazz trumpeter Roy Hargrove.
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St. Paul United Methodist Church
St. Paul United Methodist Church was founded in 1873 by freed slaves from Mississippi, Louisiana and Texas.
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One Arts Plaza
One Arts Plaza is a multiuse structure comprised of residences, corporate offices and retail, the first of three buildings on over 10 acres at the eastern edge of the Dallas Arts District.
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Dallas Black Dance Theatre
Dallas Black Dance Theatre is the city’s oldest continuously operating dance company.
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AT&T Performing Arts Center Elaine D. and Charles A. Sammons Park
Weaving together the Winspear Opera House, Wyly Theatre, Strauss Square and City Performance Hall, the ten-acre park stretches from Woodall Rodgers Freeway to Ross Avenue, and is the first public park in the Dallas Arts District.
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Sarajevo is the capital and largest city of Bosnia and Herzegovina, with a population of 275,524 in its administrative limits. The Sarajevo metropolitan area including Sarajevo Canton, Istočno Sarajevo and nearby municipalities is home to 555,210 inhabitants. Located within the greater Sarajevo valley of Bosnia, it is surrounded by the Dinaric Alps and situated along the Miljacka River in the heart of the Balkans, a region of Southeastern Europe.
Sarajevo is the political, financial, social, and cultural center of Bosnia and Herzegovina and a prominent center of culture in the Balkans. It exerts region-wide influence in entertainment, media, fashion, and the arts. Due to its long history of religious and cultural diversity, Sarajevo is sometimes called the "Jerusalem of Europe" or "Jerusalem of the Balkans". It is one of a few major European cities to have a mosque, Catholic church, Eastern Orthodox church, and synagogue within the same neighborhood. It is also home to the former Yugoslavia's first institution of tertiary education in the form of an Islamic polytechnic, today part of the University of Sarajevo.
Although there is evidence of human settlement in the area since prehistoric times, the modern city arose in the 15th century as an Ottoman stronghold when the Ottoman empire extended into Europe. Sarajevo has gained international renown several times throughout its history. In 1885, it was the first city in Europe and the second city in the world to have a full-time electric tram network running through the city, following San Francisco.
In 1914, Sarajevo was the site of the assassination of Archduke Franz Ferdinand by a local Young Bosnia activist Gavrilo Princip, a murder that sparked World War I. This resulted in the end of Austro-Hungarian rule in Bosnia and the creation of the multicultural Kingdom of Yugoslavia in the Balkan region. Later, after World War II, the area was designated the capital of the communist Socialist Republic of Bosnia and Herzegovina within the Socialist Federal Republic of Yugoslavia, leading to rapid expansion of its population and businesses with investment in infrastructure and economic development.
In 1984, Sarajevo hosted the 1984 Winter Olympics, which marked a prosperous era for the city. However, after the start of the Yugoslav Wars, the city suffered the longest siege of a capital city in the history of modern warfare, for a total of 1,425 days, from April 1992 to February 1996, during the Bosnian War.
With continued post-war reconstruction in the aftermath, Sarajevo is the fastest growing city in Bosnia and Herzegovina. The travel guide series Lonely Planet ranked Sarajevo as the 43rd best city in the world. In December 2009, it recommended Sarajevo as one of the top ten cities to visit in 2010.
In 2011, Sarajevo was nominated as the 2014 European Capital of Culture. It was selected to host the European Youth Olympic Festival. In addition, in October 2019, Sarajevo was designated as a UNESCO Creative City for having placed culture at the center of its development strategies. It is also ranked as one of the world's eighteen Cities of Film.
Irton with Santon is a civil parish in Cumberland, Cumbria, England, which includes the village of Santon Bridge. It has a parish council. It had a population of 373 in 2001, decreasing to 316 at the 2011 Census.
The parish is bordered by the parishes of Gosforth to the north west and west, Eskdale to the east, Muncaster to the south east, and Drigg and Carleton to the south west. Irton Pike is a hill of 751 feet (229 m) included in Wainwright's book The Outlying Fells of Lakeland, and the River Irt flows through the parish, bridged at Santon Bridge. The parish lies within the Lake District National Park, and the only major road is a short stretch of the A595 along the western edge, passing through Holmrook (a village divided between this parish and Drigg and Carleton).
There are 17 listed buildings or structures in the parish. The Church of St Paul and the medieval tower incorporated into Irton Hall are at grade II* and the rest at grade II.
St Paul's church stands in an isolated position roughly midway between Holmrook and Santon Bridge. It is part of the benefice of Eskdale, Irton, Muncaster and Waberthwaite in the Diocese of Carlisle, and services are held twice a month. The Anglo-Saxon Irton Cross stands in its graveyard; there is a reproduction of it in the Cast Courts of the Victoria and Albert Museum, commissioned by the museum in 1882. A plaque by the font is in memorial to Robert Wilfred Skeffington-Lutwidge who was a commissioner in lunacy. The plaque tells the tragic tale of how he died after being hit on the head by a lunatic.[citation needed] The church was rebuilt in 1857 on the site of an earlier church, by Miles Thompson of Kendal (who also designed Arnside Church) and includes glass by Morris & Co.
The Keighley Library staff members' Christmas Party in December 1961. The party was held in the lecture hall, part of the new extension that was opened at the Library in March 1961. Those present include Betty Cardwell, Sarah Hudson, Stewart Cardwell, Joan Wooller, Doreen Nolan and Barbara Watson (serving). From a slide taken by John Normington.
The item is part of the John Normington Collection, donated to Keighley and District Local History Society by John's daughter Liz Hornby in September 2021.
John Normington was born in Keighley on 26th May 1929 and grew up in the Exley Head area of the town. He was joined by younger brother William five years later. John attended Ingrow Primary School and later won a scholarship for Keighley Boys’ Grammar School. His interest in music started with playing the drums at the age of six, then swapping to take up the piano.
His first job was at Keighley Library, where he remained (except for a break for National Service in 1947-49) until taking early retirement in March 1984. He was made Chief Assistant (Deputy) in 1953 having studied at the Leeds School of Librarianship. He ultimately became a lecturer himself in Cataloguing and Classification. He worked alongside local historian Ian Dewhirst for many years. Six months after he retired from Keighley Library in 1984, he took up the part-time role of Library Assistant at South Craven School.
One of his passions beyond the library was his music, and in performing. In the 1940s and 1950s he both acted with and played the drums for the Ingrow St. John’s Parish Church Players. Later he played the piano (and occasionally the drums) for Keighley Amateurs (of which he was a member for 72 years). Utilising his musical skills, he joined the Good Time Jazz Band in 1978. Another passion was potholing, having been introduced to it in the late 1940s, and he joined the Craven Pothole Club in 1952. He served as President of the Club in 1982 and as treasurer from 1984 to 1992. He was also a member of the 40 Club, the Grafton Club and Haworth Round Table. John died on 11th January 2020 at the age of 90.
Motorbike action on the hillclimb at the Goodwood Festival of Speed. Stunt master Mattie Griffin on his BMW F800R
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.
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marketplace.secondlife.com/p/Graffitiwear-Celebrate-DEMO/...
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.
This is a photograph from the Forest Marathon festival 2013 which was held in the beautiful Coillte forest of Portumna in Co. Galway, Ireland on Saturday 15th June 2013. The event includes a 10k, a full marathon, a half marathon and two ultra-running events - a 50k and 100k race. The races started at 08:00 with the 100KM, the 50KM at 10:00, and subsequent races at two hour intervals onwards. All events started and finished within the forest with the exception of the half marathon and marathon which started outside of the forest. All events see participants complete 5KM loops of the forest which start and end at the car-park/amenity end of the forest. There is an official Refreshment/Handling Zones at this point on the loop.
The event was organised by international coach Sebastien Locteau from SportsIreland.ie and his fantastic team of volunteers from Galway and beyond. Congratulations to Seb on organising a very professionally run event and an event which is growing bigger and more prestigious with each passing year. There was an incredible atmosphere amongst the runners, the spectators, and the organisers. Hats off to everyone involved.
The marathon, 50KM, and 100KM events are sanctioned by Athletics Ireland and AIMS (the Association of International Marathons and Distance Races). The event has also achieved IAU (International Association of Ultrarunners) Bronze Label status for 2013.
Electronic timing was provided by RedTagTiming: www.redtagtiming.com/
Energy Bars, Gels, Drinks etc were provided by Fuel4Sport: www.fuel4sport.ie/
This is a set of photographs taken at various points on the 5KM loop in the Forest and contains photographs of competitors from all of the events except the 10KM race.
Viewing this on a smartphone device?
If you are viewing this Flickr set on a smartphone and you want to see the larger version(s) of this photograph then: scroll down to the bottom of this description under the photograph and click the "View info about this photo..." link. You will be brought to a new page and you should click the link "View All Sizes".
Overall Race Summary
Participants: Approximately 600 people took part across all of the events which were staged: 10km, half marathon, marathon, 50km, and 100KM.
Weather: The weather was unfortunately not what a summer's day in June should be like - there was rain, some breeze, but mild temperatures.
Course: This is a fast flat course depending on your event. The course is left handed around the Forest and roughly looks like a figure of 8 in terms of routing.
Location Map: Start/finish area on Google StreetView [goo.gl/maps/WWTgD] are inside the parklands and trails
Refreshments: There are no specific refreshments but the race organizers provide very adequate supplies for all participants.
Some Useful Links
Official Race Event Website: www.forestmarathon.com/
The Boards.ie Athletics Forum Thread for the 2013 Event: www.boards.ie/vbulletin/showthread.php?t=2056874371
A GPS Garmin Trace of the Course Profile (from the 50KM event) connect.garmin.com/activity/189495781
Our Flickr Photographs from the 2012 Events: www.flickr.com/photos/peterm7/sets/72157630146344494/
Our Flickr Photographs from the 2011 Events: www.flickr.com/photos/peterm7/sets/72157626865466587/
Title Sponsors Sports Ireland Website: sites.google.com/a/sportsireland.ie/welcome-sports-irelan...
A VIDEO of the Course: www.youtube.com/watch?feature=player_embedded&v=2FLxE...
Google StreetView of the Entrance to Portuma Forest: goo.gl/maps/MX62O
Wikipedia: Read about Portumna and Portumna Forest Park: en.wikipedia.org/wiki/Portumna#Portumna_Forest_Park
Coilte Ourdoors Website: www.coillteoutdoors.ie/?id=53&rec_site=115
Portumna Forest on EveryTrails: www.everytrail.com/guide/portumna-forest-park-woodland-tr...
More about the IAU Bronze Label: www.iau-ultramarathon.org/index.asp?menucode=h07&tmp=...
How can I get a full resolution copy of these photographs?
All of the photographs here on this Flickr set have a visible watermark embedded in them. All of the photographs posted here on this Flickr set are available offline, free, at no cost, at full image resolution WITHOUT watermark. We take these photographs as a hobby and as a contribution to the running community in Ireland. Our only "cost" is our request that if you are using these images: (1) on social media sites such as Facebook, Tumblr, Pinterest, Twitter,LinkedIn, Google+, etc or (2) other websites, web multimedia, commercial/promotional material that you provide a link back to our Flickr page to attribute us. This also extends the use of these images for Facebook profile pictures. In these cases please make a separate wall or blog post with a link to our Flickr page. If you do not know how this should be done for Facebook or other social media please email us and we will be happy to help suggest how to link to us.
Please email petermooney78 AT gmail DOT com with the links to the photographs you would like to obtain a full resolution copy of. We also ask race organisers, media, etc to ask for permission before use of our images for flyers, posters, etc. We reserve the right to refuse a request.
In summary please remember - all we ask is for you to link back to our Flickr set or Flickr pages. Taking the photographs and preparing them for online posting does take a significant effort. We are not posting photographs to Flickr for commercial reasons. If you really like what we do please spread the link around your social media, send us an email, leave a comment beside the photographs, send us a Flickr email, etc.
If you would like to contribute something for your photograph(s)?
Many people offer payment for our photographs. As stated above we do not charge for these photographs. We take these photographs as our contribution to the running community in Ireland. If you feel that the photograph(s) you request are good enough that you would consider paying for their purchase from other photographic providers we would suggest that you can provide a donation to any of the great charities in Ireland who do work for Cancer Care or Cancer Research in Ireland.
I ran in the race - but my photograph doesn't appear here in your Flickr set! What gives?
As mentioned above we take these photographs as a hobby and as a voluntary contribution to the running community in Ireland. Very often we have actually ran in the same race and then switched to photographer mode after we finished the race. Consequently, we feel that we have no obligations to capture a photograph of every participant in the race. However, we do try our very best to capture as many participants as possible. But this is sometimes not possible for a variety of reasons:
►You were hidden behind another participant as you passed our camera
►Weather or lighting conditions meant that we had some photographs with blurry content which we did not upload to our Flickr set
►There were too many people - some races attract thousands of participants and as amateur photographs we cannot hope to capture photographs of everyone
►We simply missed you - sorry about that - we did our best!
You can email us petermooney78 AT gmail DOT com to enquire if we have a photograph of you which didn't make the final Flickr selection for the race. But we cannot promise that there will be photograph there. As alternatives we advise you to contact the race organisers to enquire if there were (1) other photographs taking photographs at the race event or if (2) there were professional commercial sports photographers taking photographs which might have some photographs of you available for purchase. You might find some links for further information above.
Don't like your photograph here?
That's OK! We understand!
If, for any reason, you are not happy or comfortable with your picture appearing here in this photoset on Flickr then please email us at petermooney78 AT gmail DOT com and we will remove it as soon as possible. We give careful consideration to each photograph before uploading.
I want to tell people about these great photographs!
Great! Thank you! The best link to spread the word around is probably www.flickr.com/peterm7/sets
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
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