This wheelchair accessible walkway at Crab Cove in Alameda, California is partially submerged at high tide. The photo was taken during a king tide on February 8, 2013. Here's another photo taken at the same location, but from higher, at the time of another king tide: www.flickr.com/photos/frame_maker/8380901161/. See also www.flickr.com/photos/frame_maker/32500097432/

 

N.B. See my profile for usage guidelines.

 

To be exhibited: Art Works Downtown, San Raphael, Climate Change exhibit

1337 Fourth Street, San Raphael, CA

Exhibition Dates: January 8–February 26, 2016

Reception and Art Walk: Fri, January 8, 5-8pm:

Reception and Art Walk: Fri, February 12, 5-8pm

 

2nd Place, Pictorial, Masters level, Berkeley Camera Club, 7/2/13 [BCC_CMP:PICT 7/2/13]

2nd Place, Pictorial, Masters level, Northern California Council of Camera Clubs, 7/13

Honorable Mention, Annual Competition, Pictorial, Masters level, Berkeley Camera Club, 10/13

 

The underground tour of the White Scar Caves complex takes about 1h 20mins and is a walk of about one kilometre from the entrance to the end of the publicly accessible part of the cave complex. Parts of it are narrow and others have very low headroom but its well worth the bent knees and dripping cold water to experience the marvelous rock formations deep under the Pennine Hills. My good lady wife is seen negotiating the part of the route known as "The Squeeze" where the passageway is being narrowed by a large flowstone. All the time the noise of running water is beneath your feet as the path is elevated above an underground stream which cascades over an underground waterfall.

Rotterdam - Depot Boijmans Van Beuningen, the world’s first fully accessible art depot, will open its doors in September 2021 at Museumpark in the centre of Rotterdam. With this construction completion, now the museum and the users can start to inhabit the building and fill its spaces with priceless art. Although it will take another year before the real opening, the completion is a special moment . 7,000 lucky persons can make a safe quick visit in 3 days in September 2020.

 

The assignment for MVRDV Architects was to offer a glimpse behind the scenes of the museum world and make the whole art collection accessible to the public. The reflective round volume responds to its surroundings. The Depot features exhibition halls, a rooftop garden, and a restaurant, in addition to an enormous amount of storage space for art and design.

Depot Boijmans Van Beuningen is the first depot in the world that offers access to a complete collection. The dynamics of the depot are different from those of the museum: no exhibitions are held here, but you can - independently or with a guide - browse through 151,000 art objects. You can also take a look at, for example, conservation and restoration.. Surface 15,000 m²

 

MVRDV has completed the bowl-like Depot Boijmans Van Beuningen in Rotterdam's Museumpark, which is covered in mirrored glass and topped by a rooftop forest. The art storage facility, which will open to the public in autumn 2021, has been built to house the art collection of the Museum Boijmans Van Beuningen in one place for the first time since 1935. Depot Boijmans Van Beuningen contains a mix of storage spaces alongside areas for art maintenance, both of which will be made accessible to visitors after the artwork has been moved there. This makes the facility the first publicly accessible art depot in the world, according to MVRDV Architects, and will offer a new type of experience for museum-goers in the Netherlands.

 

The Depot Boijmans Van Beuningen measures 12 metres in height and encompasses 15,000 m2. The budget was € 55,000,000. To help reduce its visual impact, MVRDV clad the depot in 1,664 reflective glass panels so that it blends in with its surroundings in the OMA-designed Museumpark. Its bowl-shape was also developed to minimise its footprint. The rooftop features 75 birch trees. Its reflective facade wears the trappings of whatever surrounds it: people passing by, Museumpark's leafy grounds, the clouds, and Rotterdam's dynamic city skyline. Thanks to this reflection, the building is already fully integrated into its surroundings, despite its not insignificant size.

 

Inside, the building contains several storage spaces alongside studios for the curators and areas for the maintenance of the art. The storage spaces are divided into five different climate zones so that the artefacts can be stored and exhibited according to their specific temperature and humidity requirements, which can vary depending on the materials used to make them. According to MVRDV, the focal point of the depot is its central atrium, which is filled with overlapping staircases and suspended glass display cases that will eventually be filled with art chosen by the museum's curators. This atrium will connect the storage and exhibition spaces to the curators' studios, and offer visitors rare access and insights into how the museum cares and maintains its collection. Once open to the public, the Museum Boijmans Van Beuningen's artwork will be displayed throughout the entire building, including on its rooftop restaurant and sculpture garden. The rooftop forest is covered with 75 tall birch trees and was incorporated by the studio to make up for the lost green space and provide views across the city.

 

MVRDV is an architecture studio based in Rotterdam, which was founded by Winy Maas, Jacob van Rijs and Nathalie de Vries in 1991. The studio won a competition to design the Depot Boijmans Van Beuningen in 2014.

It was developed by the studio with BAM Bouw & Techniek and will be made open to the public after its interiors are completed and the artwork has been moved inside.

 

Near Middleton-in-Teesdale. Not much else to be said other than that this is a fairly accessible spot. You don't need to be John Noakes with tent, Shep and a film crew in tow to get here; a pleasant walk from Middleton will do it.

Hotel Groslot is a beautiful Neo-Renaissance mansion on the Place de l'Etape next to the cathedral in Orleans. The mansion which once hosted King Charles IX, Henri IV and Catherine de Medicis is open for visitors to admire part of the interior. It is also known as the Grande Maison de l'Etape and the Maison de Gouverneur.

 

Explore the Hôtel de Groslot

The Hotel Groslot was built for the Groslot family in the mid sixteenth century. Jaques Groslot died before the house was completed and left the house to his wife and two sons. One of the sons Jérôme Groslot became the bailif of Orleans in 1545 and in October of 1560 King Francois II came to live in the Hotel Groslot with all his court as a protest against Jéroôme Groslot who was a supporter of the Protestant Reform.

 

Whilst at the hôtel he died and the crown passed to his ten year old son Charles IX and the regency passed to his mother Catherine de Medicis. Charles and his mother finally left the Hôtel Groslot in February 1561 after the court have been staying there for 5 months!

 

In 1758 the hôtel is sold to the municipality and in 1790 it becomes the town hall. In 1981 the town hall moved to no.1 Place de l'Etape and today some rooms are open to visitors and are also used for the wedding ceremony of residents of Orleans.

 

Inside the building you can visit the sumptously furnished salon d'honneur, the council chambers and the salon des marriages where Francois II died.

 

The salon d'honneur is beautifully furnished with ornate ceilings, pannelled walls and stained glass windows. The fireplace is decorated with the story of Joan of Arc whose history is closely linked with the city of Orleans. For more information see the story of Joan of Arc.

 

The stained glass windows include portraits of famous people including Joan of Arc and CharlesVII. Opposite the fireplace is a large painting of Joan of Arc. This is a copy of a painting by Pierre-August Pichon which was offered to the city by Napoleon the 3rd and is now exhibited in the Louvre at Paris.

 

Outside in the courtyard is a large statue of Joan of Arc realised by the Princess Marie of Orleans dates from the 19th century and if you look closely you can see bullet holes from battle for the liberation of Orleans in August 1944. There is a garden behind the building that is accessible from the Rue d'Escures.

 

The Hotel de Groslot is open every day except when a marriage is taking place and is free to visit.

 

The Hotel Groslot makes a mention in literature by Honoré de Balzac in the Comedie humaine, 'Sur Catherine de Medicis'.

 

Orléans is a city in north-central France, about 120 kilometres (74 miles) southwest of Paris. It is the prefecture of the department of Loiret and of the region of Centre-Val de Loire.

 

Orléans is located on the river Loire nestled in the heart of the Loire Valley, classified as a World Heritage Site, where the river curves south towards the Massif Central. In 2020, the city had 117,026 inhabitants within its municipal boundaries Orléans is the center of Orléans Métropole that has a population of 290,346.The larger metropolitan area has a population of 454,208, the 20th largest in France.

 

The city owes its development from antiquity to the commercial exchanges resulting from the river. An important river trade port, it was the headquarters of the community of merchants frequenting the Loire. It was the capital of the Kingdom of France during the Merovingian period and played an important role in the Hundred Years' War, particularly known for the role of Joan of Arc during the siege of Orléans. Every first week of May since 1432, the city pays homage to the "Maid of Orléans" during the Johannic Holidays which has been listed in the inventory of intangible cultural heritage in France. One of Europe's oldest universities was created in 1306 by Pope Clement V and re-founded in 1966 as the University of Orléans, hosting more than 20,000 students in 2019.

 

Orléans is located in the northern bend of the Loire, which crosses from east to west. Orléans belongs to the vallée de la Loire sector between Sully-sur-Loire and Chalonnes-sur-Loire, which was in 2000 inscribed by UNESCO as a World Heritage Site. The capital of Orléanais, 120 kilometres southwest of Paris, is bordered to the north by the Beauce region, more specifically the Orléans Forest (French: forêt d'Orléans) and Orléans-la-Source neighbourhood, and the Sologne region to the south.

 

Five bridges in the city cross the Loire: Pont de l'Europe, Pont du Maréchal Joffre (also called Pont Neuf), Pont George-V (also called Pont Royal, carrying the commune tramway), Pont René-Thinat and Pont de Vierzon (rail bridge).

 

To the north of the Loire (rive droite) is to be found a small hill (102 m (335 ft) at the pont Georges-V, 110 m (360 ft) at the Place du Martroi) which gently rises to 125 m (410 ft) at la Croix Fleury, at the limits of Fleury-les-Aubrais. Conversely, the south (on the rive gauche) has a gentle depression to about 95 m (312 ft) above sea level (at Saint-Marceau) between the Loire and the Loiret, designated a "zone inondable" (flood-risk zone).

 

At the end of the 1960s, the Orléans-la-Source neighbourhood was created, 12 kilometres (7 mi)to the south of the original commune and separated from it by the Val d'Orléans and the river Loiret (whose source is in the Parc Floral de la Source). This quarter's altitude varies from about 100 to 110 m (330 to 360 ft).

 

In Orléans, the Loire is separated by a submerged dike known as the dhuis into the Grande Loire to the north, no longer navigable, and the Petite Loire to the south. This dike is just one part of a vast system of construction that previously allowed the Loire to remain navigable to this point.

 

The Loire was formerly an important navigation and trading route, and is at the heart of the city's foundation in the second century BC as a center of trade or emporium. More recently, during the 17th century, the river enabled Orleans to become a major hub for refining sugar, which was imported from the Caribbean via Nantes, and whose commerce boosted other aspects of the local economy, such as sweets, chocolate manufacturing, and paper for wrapping.[16] In the 18th century, Orleans also acquired a reputation for producing vinegar, from local vineyards as well as wine traveling up the Loire.

 

With the increase in size of ocean-going ships, large ships can now navigate the estuary only up to about Nantes.

 

Boats on the river were traditionally flat-bottomed boats, with large but foldable masts so the sails could gather wind from above the river banks, but the masts could be lowered in order to allow the boats to pass under bridges. These vessels are known as "gabarre", "futreau", and so on, and may be viewed by tourists near pont Royal.

 

The river's irregular flow strongly limits traffic on it, in particular at its ascent, though this can be overcome by boats being given a tow.

 

An Inexplosible-type paddle steamer owned by the mairie was put in place in August 2007, facing Place de la Loire and containing a bar.

 

Every two years, the Festival de Loire recalls the role played by the river in the commune's history.

 

On the river's north bank, near the town centre, is the Canal d'Orléans, which connects to the Canal du Loing and the Canal de Briare at Buges near Montargis. The canal is no longer used along its whole length. Its route within Orléans runs parallel to the river, separated from it by a wall or muret, with a promenade along the top. Its last pound was transformed into an outdoor swimming pool in the 1960s, then filled in. It was reopened in 2007 for the "fêtes de Loire." There are plans to revive use of the canal for recreation and install a pleasure-boat port there.

 

Cenabum was a Gaul stronghold, one of the principal towns of the tribe of the Carnutes where the Druids held their annual assembly. The Carnutes were massacred and the city was destroyed by Julius Caesar in 52 BC. In the late 3rd century AD, Roman Emperor Aurelian rebuilt the city and renamed it civitas Aurelianorum ("city of Aurelian") after himself. The name later evolved into Orléans.

 

In 442 Flavius Aetius, the Roman commander in Gaul, requested Goar, head of the Iranian tribe of Alans in the region to come to Orleans and control the rebellious natives and the Visigoths. Accompanying the Vandals, the Alans crossed the Loire in 408. One of their groups, under Goar, joined the Roman forces of Flavius Aetius to fight Attila when he invaded Gaul in 451, taking part in the Battle of Châlons under their king Sangiban. Goar established his capital in Orléans. His successors later took possession of the estates in the region between Orléans and Paris. Installed in Orléans and along the Loire, they were unruly (killing the town's senators when they felt they had been paid too slowly or too little) and resented by the local inhabitants. Many inhabitants around the present city have names bearing witness to the Alan presence – Allaines. Also many places in the region bear names of Alan origin.

 

Early Middle Ages

In the Merovingian era, the city was capital of the Kingdom of Orléans following Clovis I's division of the kingdom, then under the Capetians it became the capital of a county then duchy held in appanage by the house of Valois-Orléans. The Valois-Orléans family later acceded to the throne of France via Louis XII, then Francis I. In 1108, Louis VI of France became one of the few French monarchs to be crowned outside of Reims when he was crowned in Orléans cathedral by Daimbert, Archbishop of Sens.

 

High Middle Ages

The city was always a strategic point on the Loire, for it was sited at the river's most northerly point, and thus its closest point to Paris. There were few bridges over the dangerous river Loire, but Orléans had one of them, and so became – with Rouen and Paris – one of medieval France's three richest cities.

 

On the south bank the "châtelet des Tourelles" protected access to the bridge. This was the site of the battle on 8 May 1429 which allowed Joan of Arc to enter and lift the siege of the Plantagenets during the Hundred Years' War, with the help of the royal generals Dunois and Florent d'Illiers [fr]. The city's inhabitants have continued to remain faithful and grateful to her to this day, calling her "la pucelle d'Orléans" (the maid of Orléans), offering her a middle-class house in the city, and contributing to her ransom when she was taken prisoner.

 

1453 to 1699

Once the Hundred Years' War was over, the city recovered its former prosperity. The bridge brought in tolls and taxes, as did the merchants passing through the city. King Louis XI also greatly contributed to its prosperity, revitalising agriculture in the surrounding area (particularly the exceptionally fertile land around Beauce) and relaunching saffron farming at Pithiviers. Later, during the Renaissance, the city benefited from its becoming fashionable for rich châtelains to travel along the Loire valley (a fashion begun by the king himself, whose royal domains included the nearby châteaus at Chambord, Amboise, Blois, and Chenonceau).

 

The University of Orléans also contributed to the city's prestige. Specializing in law, it was highly regarded throughout Europe. John Calvin was received and accommodated there (and wrote part of his reforming theses during his stay), and in return Henry VIII of England (who had drawn on Calvin's work in his separation from Rome) offered to fund a scholarship at the university. Many other Protestants were sheltered by the city. Jean-Baptiste Poquelin, better known by his pseudonym Molière, also studied law at the University, but was expelled for attending a carnival contrary to university rules.

 

From 13 December 1560 to 31 January 1561, the French States-General after the death of Francis II of France, the eldest son of Catherine de Médicis and Henry II. He died in the Hôtel Groslot in Orléans, with his queen Mary at his side.

 

The cathedral was rebuilt several times. The present structure had its first stone laid by Henry IV, and work on it took a century. It thus is a mix of late Renaissance and early Louis XIV styles, and one of the last cathedrals to be built in France.

 

1700–1900

When France colonised America, the territory it conquered was immense, including the whole Mississippi River (whose first European name was the River Colbert), from its mouth to its source at the borders of Canada. Its capital was named la Nouvelle-Orléans in honour of Louis XV's regent, the duke of Orléans, and was settled with French inhabitants against the threat from British troops to the north-east.

 

The Dukes of Orléans hardly ever visited their city since, as brothers or cousins of the king, they took such a major role in court life that they could hardly ever leave. The duchy of Orléans was the largest of the French duchies, starting at Arpajon, continuing to Chartres, Vendôme, Blois, Vierzon, and Montargis. The duke's son bore the title duke of Chartres. Inheritances from great families and marriage alliances allowed them to accumulate huge wealth, and one of them, Philippe Égalité, is sometimes said to have been the richest man in the world at the time. His son, King Louis-Philippe I, inherited the Penthièvre and Condé family fortunes.

 

1852 saw the creation of the Compagnies ferroviaires Paris-Orléans and its famous gare d'Orsay in Paris. In the Franco-Prussian War of 1870, the city again became strategically important thanks to its geographical position, and was occupied by the Prussians on 13 October that year. The armée de la Loire was formed under the orders of General d'Aurelle de Paladines and based itself not far from Orléans at Beauce.

 

1900 to present

During the Second World War, the German army made the Orléans Fleury-les-Aubrais railway station one of their central logistical rail hubs. The Pont Georges V was renamed "pont des Tourelles". A transit camp for deportees was built at Beaune-la-Rolande. During the war, the American Air Force heavily bombed the city and the train station, causing much damage. The city was one of the first to be rebuilt after the war: the reconstruction plan and city improvement initiated by Jean Kérisel and Jean Royer was adopted as early as 1943, and work began as early as the start of 1945. This reconstruction in part identically reproduced what had been lost, such as Royale and its arcades, but also used innovative prefabrication techniques, such as îlot 4 under the direction of the architect Pol Abraham.

 

The big city of former times is today an average-sized city of 250,000 inhabitants. It is still using its strategically central position less than an hour from the French capital to attract businesses interested in reducing transport costs.

 

Heraldry

According to Victor Adolphe Malte-Brun in La France Illustrée, 1882, Orléans's arms are "gules, three caillous in cœurs de lys argent, and on a chief azure, three fleurs de lys Or." Charle Grandmaison, in the Dictionnaire Héraldique of 1861, states that it is "Or, with three hearts in gules", without the chief of France. Faulty designs sometimes describe it as "gules, three fleurs de lys argent, and on a chief azure three fleurs de lys Or."

 

The "cœurs de lys", or heart of a lily, is not a true lily, which would have 6 tepals, but a stylized or symbolic lily. Certain authors solve the problem by calling this symbol a "tiercefeuille", defined as a stemless clover leaf, with one leaf at the top and two below, thus making this coat of arms "gules, with three reversed tiercefeuilles in argent, etc".

 

Motto

"Hoc vernant lilia corde" (granted by Louis XII, then duke of Orléans), meaning "It is by this heart that lilies flourish" or "This heart makes lilies flourish", referring to the fleur de lys, symbol of the French royal family.

 

Orléans is the birthplace of:

 

Sophie Adriansen (born 1982), French writer

Patrick Barul (born 1977), football player

Joelly Belleka (born 1995), basketball player

Raoul Blanchard (1877–1965), geographer

Maxence Boitez (Ridsa) (born 1990), singer

Patrick Bornhauser (born 1957), racing driver

Raymond Brugère (1885-1966), diplomat.

Jean-Baptiste Marc Bourgery (1797–1849), anatomist

Félix Cazot (1790–1857), classical pianist and composer

Philippe Chanlot (born 1967), football player

Marion Cotillard (born 1975), actress, not born in Orléans, but grew up there

Gilles Delouche (1948–2020), linguist

Étienne Dolet (1509–1546), scholar and printer

Joël-François Durand (born 1954), composer

Jean-Louis Ferrary (1948–2020), historian

Georges Fleury (1878–1968), cyclist

Albert Gombault (1844–1904), neurologist

Guillaume Gomez (born 1969), racing driver

Jacques Guillemeau (1550–1613), physician

Albert Guyot (1881–1947), racing driver

Étienne Hubert (1567–1614), Arabist

Gaston d'Illiers (1876–1932), sculptor

Isaac Jogues (1607–1646), Jesuit missionary

Stanislas Julien (1797–1873), orientalist

Gustave Lanson (1857–1934), historian

Pierre Levesville (1570–1632), Renaissance architect

Anatole Loquin (1834–1903), writer and musicologist

Yven Moyo (born 1992), football player

Yves-Marie Pasquet (born 1947), composer

Charles Péguy (1873–1914), poet and essayist

Antoine Petit (1722–1794), physician

Lamine Sambe (born 1989), basketball player

Yacine Sene (born 1982), basketball player

Florian Thauvin (born 1993), football player

Christophe Tinseau (born 1969), racing driver

Jean Zay (1904–1944), jurist and politician

 

Historical landmarks

The Gallo-Roman town-wall on the north side of the cathedral (4th century AD) and along the rue de la Tour-Neuve

The Hôtel Groslot, built between 1550 and 1555 for Jacques Groslot, "bailli d'Orléans" by Jacques Ier Androuet du Cerceau. King François II of France died there in 1560. Kings Charles IX, Henri III of France and Henri IV of France stayed there. The "Hôtel" was restored in 1850. The building became the town Hall of Orléans in 1790 (weddings are still celebrated inside).

The hôtel de la Vieille Intendance (early 15th century) (otherwise named hôtel Brachet, formerly "The King's house"), real gothic-renaissance style château made of bricks.[27] Nowadays housing the Administrative Court of Orléans. One can admire its frontage from the entrance in the rue de la Bretonnerie. Yet, the building – which sheltered the highest figures of the kingdom passing by the city, and maybe some kings themselves (Henri IV, Louis XIII, Louis XIV of France) – can easily be observed from its gardens, opened to the public (entrance rue d'Alsace-Lorraine).

The hôtel de la Motte-Sanguin (18th century) and its gardens, manor built at the behest of Louis-Philippe, Duke of Orléans (1747–1793), cousin of the King Louis XVI. He was surnamed "Philippe Égalité" / "equality" referring to his support to the 1789 revolutionaries. Nicknamed "the richest man on earth" he voted in favour of the death penalty against his own cousin the king Louis XVI, and suffered the same fate himself. This is a classic style princely residence (and even royal, since Philippe Égalité's heir accessed the throne of France under the name of Louis-Philippe Ier). It is part of a public park opened to the public (via the Solférino street).

The school of artillery, next to the Hôtel de la Motte-Sanguin which it is often confused with, formerly housing a military school, it was built in the 19th century near the Loire.[28]

Remains of the University of Orléans (a 15th-century building housing the thesis room), founded in 1306 by pope Clement V, in which, among many other great historical figures, the Protestant John Calvin studied and taught. The University was so famous that it attracted students from all over Europe, particularly Germany. The city of Orléans is one of the cradles of Protestantism.

The House of Louis XI (end of the 15th century), on Saint-Aignan square. Built at the behest of the king, who particularly revered Saint Aignan.

The House of Joan of Arc, where she stayed during the siege of Orléans (this is actually an approximate reconstitution, the original building being bombed in 1940 during the Battle of France).

Place du Martroi, heart of the city, with the equestrian statue of Joan of Arc at its centre, made by Denis Foyatier. This statue was damaged during the Second World War, then repaired by Paul Belmondo, father of the famous 1950s to 1980s French actor.

Duke of Orléans' Chancellerie (XVIIIe), located next to the Place du Matroi, also bombed during the Second World War, only the frontage resisted.

The Bannier gate-house, discovered in 1986 under the statue of Joan of Arc (Place du Martroi). It was built in the 14th century. It can be seen through a window in the subterranean car-park under the square, or visited under certain conditions.

The rue de Bourgogne and surrounding streets, Orléans' main street since the Antiquity, it's the former Roman decumanus, crossing the city from east to west. Joan of Arc entered the city in 1429 by the "Bourgogne" gatehouse situated at its Easter end. Until today it is still giving access to the "Prefecture", where the "Prefet" (officer who represents the French State in the Region) lives, many pubs, night clubs, restaurants and shops such as the "Galeries Lafayette". It is more than a mile long. One can admire many medieval houses on its sides.

The Tour Blanche / White Tower, it is one of the only medieval defensive towers remaining in the city (still in use at the time of the siege of Orléans). It nowadays houses the city's archaeological department.

The Docks, (Port of Orléans) once the most important inland port of France (18th century). While boats could not sail on the river Seine because of the windings, they could sail to Orléans on the river Loire with the wind in their back. Then the merchandise was brought to Paris by roadways. Wine, and sugar from the colonies, were shipped to Orléans where they were stored and refined. Vinegar is still a city speciality due to the lapsing of wine stocks during the shipment. One can admire the old pavement of the docks (18th and 19th centuries) on the north bank of the river in the city and on the island in the middle, that was used to channel the water

The Hôpital Madeleine (former hospital), built by King Louis XIV (18th century) and his successors (notably an important part of the 18th century).

Saint-Charles chapel, located within the grounds of the Madeleine Hospital, it was built in 1713 by Jacques V Gabriel, one of Louis XIV's architects.

The Hôtel Cabu, otherwise named house of Diane de Poitiers, built at the behest of Philippe Cabu, barrister, in 1547, famous architect Jacques Ier Androuet du Cerceau providing the plans.

The Hôtel Hatte, 16th century. Today's Charles-Péguy Center.

The Hôtel Toutin, 16th century

The Hôtel Pommeret d'Orléans, 16th century

The Hôtel Ducerceau, 16th century

The maison de la coquille, 16th century

The Hôtel des Créneaux, former city hall, flanked by its bell tower (15th century). It nowadays houses the city's school of music. This is a magnificent piece of late gothic secular architecture (15th century) that calls to mind the famous and much more recent Parisian city hall.

The House of Jean Dalibert, 16th century

The Study of Jacques Bouchet (16th century), which can be admired from the public square "Jacques Bouchet"

The mansions, rue d'Escure (17th and 18th centuries)

The "Préfecture" : former Benedictine monastery, built in 1670 and housing the "Préfecture du Loiret" since 1800.

The Pont de l'Europe, designed by Santiago Calatrava, is an inclined bow-string ark bridge particularly original.

The Pont Royal / George V Royal bridge, the oldest bridge of the city. Built between 1751 and 1760, at the request of Daniel-Charles Trudaine, administrator and civil engineer. It was renamed in honour of King George V after the World War I out of respect of Britain's role in the war.

The Pont des Tourelles, built in 1140 and demolished in 1760, was the first stone-made bridge of Orléans. When the river Loire is low, one can see remains of it in the water

The Palais épiscopal d'Orléans, former Bishop's Palace. It was built between 1635 and 1641. Napoléon stayed there. It is nowadays housing the international centre for research, part of University of Orléans.

The courthouse (18th to 20th centuries)

The "salle de l'Institut", located on the "place Sainte Croix", is a small concert hall which can be converted into a ballroom. Its acoustics are remarkable.

Mansions, rue de la Bretonnerie. This street concentrates many particular mansions, of all styles and ages (15th to 20th centuries). High society members, politicians, barristers, doctors... continue to live there.

Mansions, rue d'Alsace-Lorraine, 19th-century bourgeoisie style houses.

Statue La Baigneuse by Paul Belmondo, aside the rue Royale (1955).

Statue of Calvin, by Daniel Leclercq, facing the Calvinist temple (2009).

The FRAC Centre building named "Les turbulences", an advanced piece of architecture covered with L.E.Ds.

Memorial Museum to the Children of Vel d'Hiv at the Centre d'étude et de recherche sur les camps d'internement du Loiret (Study and Research Centre on the Internment Camps in Loiret), commemorating over 4,000 Jewish children who were concentrated at the Vélodrome d´Hiver cycling arena in Paris in July 1942, after which they were interned at either Pithiviers or Beaune-la-Rolande, and eventually deported to the Auschwitz extermination camp.

Many historical houses and mansions (hundreds) can still be admired in the city centre, which is one of the largest in France due to the great importance of the city until the 20th century. The historical centre dating back to the 15th century extends far beyond the limits of the pedestrian sector that has been extensively restored in the past few years. In fact it corresponds to the portion of the modern city which is enclosed by the Boulevards. Many historical monuments remain in the non-pedestrian sectors of the city (for example, at rue Notre-Dame-de-Recouvrance, at rue des Carmes, at rue de la Bretonnerie, at Square Saint-Aignan).

  

Snowdonia, or Eryri is a mountainous region and national park in North Wales. It contains all 15 mountains in Wales over 3000 feet high, including the country's highest, Snowdon (Yr Wyddfa), which is 1,085 metres (3,560 ft) tall. These peaks are all part of the Snowdon, Glyderau, and Carneddau ranges in the north of the region. The shorter Moelwynion and Moel Hebog ranges lie immediately to the south.

 

The national park has an area of 823 square miles (2,130 km2) (the fourth-largest in the UK), and covers most of central and southern Gwynedd and the western part of Conwy County Borough. This is much larger than the area traditionally considered Snowdonia, and in addition to the five ranges above includes the Rhinogydd, Cadair Idris, and Aran ranges and the Dyfi Hills. It also includes most of the coast between Porthmadog and Aberdyfi. The park was the first of the three national parks of Wales to be designated, in October 1951, and the third in the UK after the Peak District and Lake District, which were established in April and May 1951 respectively. The park received 3.89 million visitors in 2015.

 

The name Snowdon means 'snow hill' and is derived from the Old English elements snāw and dūn, the latter meaning 'hill'. Snowdonia is simply taken from the name of the mountain.

 

The origins of Eryri are less clear. Two popular interpretations are that the name is related to eryr, 'eagle', and that it means 'highlands' and is related to the Latin oriri ('to rise'). Although eryri is not any direct form of the word eryr in the meaning 'eagle', it is a plural form of eryr in the meaning 'upland'.

 

Before the boundaries of the national park were designated, "Snowdonia" was generally used to refer to a smaller upland area of northern Gwynedd centred on the Snowdon massif. The national park covers an area more than twice that size, extending south into the Meirionnydd area.

 

This difference is apparent in books published before 1951. In George Borrow's 1907 Wild Wales he states that "Snowdon or Eryri is no single hill, but a mountainous region, the loftiest part of which is called Y Wyddfa", making a distinction between the summit of the mountain and the surrounding massif. The Mountains of Snowdonia by H. Carr & G. Lister (1925) defines "Eryri" as "composed of the two cantrefs of Arfon and Arllechwedd, and the two commotes of Nant Conwy and Eifionydd", which corresponds to Caernarfonshire with the exception of southwest Llŷn and the Creuddyn Peninsula. In Snowdonia: The National Park of North Wales (1949), F. J. North states that "When the Committee delineated provisional boundaries, they included areas some distance beyond Snowdonia proper".

 

Snowdonia National Park, also known as Eryri National Park in English and Parc Cenedlaethol Eryri in Welsh, was established in October 1951. It was the third national park in the United Kingdom, following the Peak District and Lake District in April and May of the same year. It covers 827 square miles (2,140 km2) in the counties of Gwynedd and Conwy, and has 37 miles (60 km) of coastline.

 

The park is governed by the Snowdonia National Park Authority, which has 18 members: 9 appointed by Gwynedd, 3 by Conwy, and 6 by the Welsh Government to represent the national interest. The authority's main offices are at Penrhyndeudraeth.

 

The park authority used Snowdonia and Snowdon when referring to the national park and mountain in English until February 2023, when it resolved to primarily use the Welsh names, Eryri and Yr Wyddfa. There will be a transitional period of approximately two years in which the authority will continue to use the English names in parentheses — for example "Yr Wyddfa (Snowdon)" — where the context requires.

 

Unlike national parks in other countries, national parks in the UK are made up of both public and private lands under a central planning authority. The makeup of land ownership in the national park is as follows:

 

More than 26,000 people live within the park, of whom 58.6% could speak Welsh in 2011. While most of the land is either open or mountainous land, there is a significant amount of agricultural activity within the park.

 

The national park does not include the town of Blaenau Ffestiniog, which forms a unique non-designated enclave within the park boundaries. The town was deliberately excluded from the park when it was established because of its slate quarrying industry. The boundaries of the Peak District National Park exclude the town of Buxton and its adjacent limestone quarries for a similar reason.

 

The geology of Snowdonia is key to the area's character. Glaciation during a succession of ice ages, has carved from a heavily faulted and folded succession of sedimentary and igneous rocks, a distinctive rocky landscape. The last ice age ended only just over 11,500 years ago, leaving a legacy of features attractive to visitors but which have also played a part in the development of geological science and continue to provide a focus for educational visits. Visiting Cwm Idwal in 1841 Charles Darwin realised that the landscape was the product of glaciation. The bedrock dates largely from the Cambrian and Ordovician periods with intrusions of Ordovician and Silurian age associated with the Caledonian Orogeny. There are smaller areas of Silurian age sedimentary rocks in the south and northeast and of Cenozoic era strata on the Cardigan Bay coast though the latter are concealed by more recent deposits. Low grade metamorphism of Cambrian and Ordovician mudstones has resulted in the slates, the extraction of which once formed the mainstay of the area's economy.

 

The principal ranges of the traditional Snowdonia are the Snowdon massif itself, the Glyderau, the Carneddau, the Moelwynion and the Moel Hebog range. All of Wales' 3000ft mountains are to be found within the first three of these massifs and are most popular with visitors. To their south within the wider national park are the Rhinogydd and the Cadair Idris and Aran Fawddwy ranges. Besides these well-defined areas are a host of mountains which are less readily grouped though various guidebook writers have assigned them into groups such as the 'Arenigs', the 'Tarrens' and the 'Dyfi hills'.

 

Snowdon's summit at 1085 metres (3560 feet) is the highest in Wales and the highest in Britain south of the Scottish Highlands. At 905 metres (2970 feet) Aran Fawddwy is the highest in Wales outside of northern Snowdonia; Cadair Idris, at 893 metres (2930 feet), is next in line.

 

Rivers draining the area empty directly into Cardigan Bay are typically short and steep. From north to south they include the Glaslyn and Dwyryd which share a common estuary, the Mawddach and its tributaries the Wnion and the Eden, the smaller Dysynni and on the park's southern margin the Dyfi. A series of rivers drain to the north coast. Largest of these is the Conwy on the park's eastern margin which along with the Ogwen drains into Conwy Bay. Further west the Seiont and Gwyrfai empty into the western end of the Menai Strait. A part of the east of the national park is within the upper Dee (Dyfrydwy) catchment and includes Bala Lake, the largest natural waterbody in Wales. A fuller list of the rivers and tributaries within the area is found at List of rivers of Wales.

 

There are few natural waterbodies of any size in Wales; Snowdonia is home to most. Besides Bala Lake, a few lakes occupy glacial troughs including Llyn Padarn and Llyn Peris at Llanberis and Tal-y-llyn Lake south of Cadair Idris. Llyn Dinas, Llyn Gwynant, and Llyn Cwellyn to the south and west of Snowdon feature in this category as do Llyn Cowlyd and Llyn Ogwen on the margins of the Carneddau. There are numerous small lakes occupying glacial cirques owing to the former intensity of glacial action in Snowdonia. Known generically as tarns, examples include Llyn Llydaw, Glaslyn and Llyn Du'r Arddu on Snowdon, Llyn Idwal within the Glyderau and Llyn Cau on Cadair Idris.

 

There are two large wholly man-made bodies of water in the area, Llyn Celyn and Llyn Trawsfynydd whilst numerous of the natural lakes have had their levels artificially raised to different degrees. Marchlyn Mawr reservoir and Ffestiniog Power Station's Llyn Stwlan are two cases where natural tarns have been dammed as part of pumped storage hydro-electric schemes. A fuller list of the lakes within the area is found at List of lakes of Wales. In 2023, the park standardised its Welsh language lake names, to be also used in English.

 

The national park meets the Irish Sea coast within Cardigan Bay between the Dovey estuary in the south and the Dwyryd estuary. The larger part of that frontage is characterised by dune systems, the largest of which are Morfa Dyffryn and Morfa Harlech. These two locations have two of the largest sand/shingle spits in Wales. The major indentations of the Dovey, the Mawddach and Dwyryd estuaries, have large expanses of intertidal sands and coastal marsh which are especially important for wildlife: see #Natural history. The northern tip of the national park extends to the north coast of Wales at Penmaen-bach Point, west of Conwy, where precipitous cliffs have led to the road and railway negotiating the spot in tunnels.

 

There are only three towns within the park boundary, though there are several more immediately beyond it. Dolgellau is the most populous followed by Bala on the eastern boundary and then Harlech overlooking Tremadog Bay. More populous than these is the town of Blaenau Ffestiniog, which is within an exclave, that is to say it is surrounded by the national park but excluded from it, whilst the towns of Tywyn and Barmouth on the Cardigan Bay coast are within coastal exclaves. Llanrwst in the east, Machynlleth in the south and Porthmadog and Penrhyndeudraeth in the west are immediately beyond the boundary but still identified with the park; indeed the last of these hosts the headquarters of the Snowdonia National Park Authority. Similarly the local economies of the towns of Conwy, Bethesda, and Llanberis in the north are inseparably linked to the national park as they provide multiple visitor services. The lower terminus of the Snowdon Mountain Railway is at Llanberis. Though adjacent to it, Llanfairfechan and Penmaenmawr are less obviously linked to the park.

 

There are numerous smaller settlements within the national park: prominent amongst these are the eastern 'gateway' village of Betws-y-Coed, Aberdyfi on the Dovey (Dyfi) estuary and the small village of Beddgelert each of which attract large numbers of visitors. Other sizeable villages are Llanuwchllyn at the southwest end of Bala Lake (Llyn Tegid), Dyffryn Ardudwy, Corris, Trawsfynydd, Llanbedr, Trefriw and Dolwyddelan.

 

Six primary routes serve Snowdonia, the busiest of which is the A55, a dual carriageway which runs along the north coast and provides strategic road access to the northern part of the national park. The most important north–south route within the park is the A470 running from the A55 south past Betws-y-Coed to Blaenau Ffestiniog to Dolgellau. It exits the park a few miles to the southeast near Mallwyd. From Dolgellau, the A494 runs to Bala whilst the A487 connects with Machynlleth. The A487 loops around the northwest of the park from Bangor via Caernarfon to Porthmadog before turning in land to meet the A470 east of Maentwrog. The A5 was built as a mail coach road by Thomas Telford between London and Holyhead; it enters the park near Pentrefoelas and leaves it near Bethesda. Other A class roads provide more local links; the A493 down the Dovey valley from Machynlleth and up the coast to Tywyn then back up the Mawddach valley to Dolgellau, the A496 from Dolgellau down the north side of the Mawddach to Barmouth then north up the coast via Harlech to Maentwrog. The A4212 connecting Bala with Trawsfynydd is relatively modern having been laid out in the 1960s in connection with the construction of Llyn Celyn. Three further roads thread their often twisting and narrow way through the northern mountains; A4085 links Penrhyndeudraeth with Caernarfon, the A4086 links Capel Curig with Caernarfon via Llanberis and the A498 links Tremadog with the A4086 at Pen-y-Gwryd. Other roads of note include that from Llanuwchllyn up Cwm Cynllwyd to Dinas Mawddwy via the 545 metre (1788') high pass of Bwlch y Groes, the second highest tarmacked public road in Wales and the minor road running northwest and west from Llanuwchllyn towards Bronaber via the 531 metre (1742') high pass of Bwlch Pen-feidiog.

 

The double track North Wales Coast Line passes along the northern boundary of the park between Conwy and Bangor briefly entering it at Penmaen-bach Point where it is in tunnel. Stations serve the communities of Conwy, Penmaenmawr, Llanfairfechan and Bangor. The single-track Conwy Valley Line runs south from Llandudno Junction, entering the park north of Betws-y-coed which is served by a station then west up the Lledr valley by way of further stations at Pont-y-pant, Dolwyddelan and Roman Bridge. After passing through a tunnel the passenger line now terminates at Blaenau Ffestiniog railway station. Prior to 1961 the route continued as the Bala and Ffestiniog Railway via Trawsfynydd to Bala joining another former route along the Dee valley which ran southwest via Dolgellau to join the still extant coastal Cambrian Line south of Barmouth. The Pwllheli branch of the Cambrian Line splits from the Aberystwyth branch at Dovey Junction and continues via stations at Aberdovey, Tywyn, Tonfanau, Llwyngwril, Fairbourne and Morfa Mawddach to Barmouth where it crosses the Mawddach estuary by the Grade II* listed wooden Barmouth Bridge, a structure which also provides for walkers and cyclists. Further stations serve Llanaber, Tal-y-bont, Dyffryn Ardudwy, Llanbedr, Pensarn and Llandanwg before reaching Harlech. Tygwyn, Talsarnau and Llandecwyn stations are the last before the line exits the park as it crosses the Dwyryd estuary via Pont Briwet and turns westwards bound for Pwllheli via Penrhyndeudraeth, Porthmadog and Criccieth.

 

Many sections of dismantled railway are now used by walking and cycling routes and are described elsewhere. The Bala Lake Railway is a heritage railway which has been established along a section of the former mainline route between Bala and Llanuwchllyn. Other heritage railways occupy sections of former mineral lines, often narrow gauge and are described in a separate section.

 

The national park is served by a growing bus network, branded Sherpa'r Wyddfa (formerly Snowdon Sherpa). Together with the TrawsCymru network of buses this provides a car-free option to tourists and locals wishing to travel across the National Park.

 

The network was relaunched in July 2022 with a new brand, Sherpa'r Wyddfa, to reflect the National Park's new push for the promotion of Welsh place names. As such the publicity and websites for the newly branded service only use these Welsh names, even for English language users.

 

Snowdonia is one of the wettest parts of the United Kingdom; Crib Goch in Snowdonia is the wettest spot in the United Kingdom, with an average rainfall of 4,473 millimetres (176.1 in) a year over the 30-year period prior to the mid-2000s. (There is a rainfall gauge at 713 metres, 2340' on the slopes below Crib Goch.)

 

The earliest evidence for human occupation of the area dates from around 4000–3000 BCE with extensive traces of prehistoric field systems evident in the landscape. Within these are traces of irregular enclosures and hut circles. There are burial chambers of Neolithic and Bronze Age such as Bryn Cader Faner and Iron Age hillforts such as Bryn y Castell near Ffestiniog.

 

The region was finally conquered by the Romans by AD 77–78. Remains of Roman marching camps and practice camps are evident. There was a Roman fort and amphitheatre at Tomen y Mur. Roads are known to have connected with Segontium (Caernarfon) and Deva Victrix (Chester) and include the northern reaches of Sarn Helen.

 

There are numerous memorial stones of Early Christian affinity dating from the post-Roman period. The post-Roman hillfort of Dinas Emrys also dates to this time. Churches were introduced to the region in the 5th and 6th centuries. Llywelyn the Great and Llywelyn ap Gruffudd had various stone castles constructed to protect their borders and trade routes. Edward I built several castles around the margins including those at Harlech and Conwy for military and administrative reasons. Most are now protected within a World Heritage Site. Some of Snowdonia's many stone walls date back to this period too. In the Middle Ages, the title Prince of Wales and Lord of Snowdonia (Tywysog Cymru ac Arglwydd Eryri) was used by Llywelyn ap Gruffudd; his grandfather Llywelyn Fawr used the title Prince of north Wales and Lord of Snowdonia.

 

The 18th century saw the start of industrial exploitation of the area's resources, assisted by the appearance in the late part of the century of turnpike trusts making it more accessible. The engineer Thomas Telford left a legacy of road and railway construction in and around Snowdonia. A new harbour at Porthmadog linked to slate quarries at Ffestiniog via a narrow gauge railway. At its peak in the 19th century the slate industry employed around 12,000 men. A further 1000 were employed in stone quarrying at Graiglwyd and Penmaenmawr. Mining for copper, iron and gold was undertaken during the 18th and 19th centuries, leaving a legacy of mine and mill ruins today. Ruins of the gold industry are found at Cefn Coch on the Dolmelynllyn estate.

 

The Snowdonia Society is a registered charity formed in 1967; it is a voluntary group of people with an interest in the area and its protection.

 

Amory Lovins led the successful 1970s opposition to stop Rio Tinto digging up the area for a massive mine.

 

The park's entire coastline is a Special Area of Conservation, which runs from the Llŷn Peninsula down the mid-Wales coast, the latter containing valuable sand dune systems.

 

The park's natural forests are of the mixed deciduous type, the commonest tree being the Welsh oak. Birch, ash, mountain-ash and hazel are also common. The park also contains some large (planted) coniferous forested areas such as Gwydir Forest near Betws-y-Coed, although some areas, once harvested, are now increasingly being allowed to regrow naturally.

 

Northern Snowdonia is the only place in Britain where the Snowdon lily (Gagea serotina), an arctic–alpine plant, is found and the only place in the world where the Snowdonia hawkweed Hieracium snowdoniense grows.

 

One of the major problems facing the park in recent years has been the growth of Rhododendron ponticum. This fast-growing invasive species has a tendency to take over and stifle native species. It can form massive towering growths and has a companion fungus that grows on its roots producing toxins that are poisonous to any local flora and fauna for a seven-year period after the Rhododendron infestations have been eradicated. As a result, there are a number of desolate landscapes.

 

Mammals in the park include otters, polecats, feral goats, and pine martens. Birds include raven, red-billed chough, peregrine, osprey, merlin and the red kite. The rainbow-coloured Snowdon beetle (Chrysolina cerealis) is only found in northern Snowdonia.

 

Snowdonia has a particularly high number of protected sites in respect of its diverse ecology; nearly 20% of its total area is protected by UK and European law. Half of that area was set aside by the government under the European Habitats Directive as a Special Area of Conservation. There are a large number of Sites of special scientific interest (or 'SSSIs'), designated both for fauna and flora but also in some cases for geology. Nineteen of these sites are managed as national nature reserves by Natural Resources Wales. The park also contains twelve Special Areas of Conservation (or 'SACs'), three Special Protection Areas (or 'SPAs') and three Ramsar sites. Some are wholly within the park boundaries, others straddle it to various degrees.

 

There are numerous SSSIs within the park, the most extensive of which are Snowdonia, Migneint-Arenig-Dduallt, Morfa Harlech, Rhinog, Berwyn, Cadair Idris, Llyn Tegid, Aber Mawddach / Mawddach Estuary, Dyfi, Morfa Dyffryn, Moel Hebog, Coedydd Dyffryn Ffestiniog and Coedydd Nanmor.

 

The following NNRs are either wholly or partly within the park: Allt y Benglog, Y Berwyn (in multiple parts), Cader Idris, Ceunant Llennyrch, Coed Camlyn, Coed Cymerau, Coed Dolgarrog, Coed Ganllwyd, Coed Gorswen, Coed Tremadog, Coedydd Aber, Coedydd Maentwrog (in 2 parts), Coed y Rhygen, Cwm Glas Crafnant, Cwm Idwal, Hafod Garregog, Morfa Harlech, Rhinog and Snowdon.

 

The twelve SACs are as follows: Snowdonia SAC which covers much of the Carneddau, Glyderau, and the Snowdon massif, Afon Gwyrfai a Llyn Cwellyn, Corsydd Eifionydd / Eifionydd Fens (north of Garndolbenmaen), the Coedydd Derw a Safleoedd Ystlumod Meirion / Meirionydd Oakwoods and Bat Sites - a series of sites between Tremadog, Trawsfynydd, and Ffestiniog and Beddgelert and extending up the Gwynant. It also includes many of the oakwoods of the Mawddach and its tributaries. Afon Eden – Cors Goch Trawsfynydd, Rhinog, Cadair Idris (in 2 parts), Migneint-Arenig-Dduallt, River Dee and Afon Dyfrdwy a Llyn Tegid (Wales), Mwyngloddiau Fforest Gwydir / Gwydyr Forest Mines (north of Betws-y-Coed) and a part of the Berwyn a Mynyddoedd De Clwyd / Berwyn and South Clwyd Mountains SAC. The Pen Llyn a'r Sarnau / Lleyn Peninsula and the Sarnau SAC covers the entire Cardigan Bay coastline of the park and the sea area and extends above the high water mark at Morfa Harlech, Mochras and around the Dovey and Mawddach estuaries.

 

The three SPAs are Dovey Estuary / Aber Dyfi (of which a part is within the park), Berwyn (of which a part is within the park) and Migneint-Arenig-Dduallt.

 

The three designated Ramsar sites are the Dyfi Biosphere (Cors Fochno and Dyfi), Cwm Idwal and Llyn Tegid (Bala Lake).

 

The area's economy was traditionally centred upon farming and from the early 19th century increasingly on mining and quarrying. Tourism has become an increasingly significant part of Snowdonia's economy during the 20th and 21st centuries.

 

The extensive farming of sheep remains central to Snowdonia's farming economy.

 

Significant sections of the park were afforested during the 20th century for timber production. Major conifer plantations include Dyfi Forest, Coed y Brenin Forest between Dolgellau and Trawsfynydd, Penllyn Forest south of Bala, Beddgelert Forest and Gwydyr (or Gwydir) Forest near Betws-y-Coed which is managed as a forest park by Natural Resources Wales.

 

The region was once the most important producer of slate in the world. Some production continues but at a much reduced level from its peak. The park boundaries are drawn such that much of the landscape affected by slate quarrying and mining lies immediately outside of the designated area.

 

Construction of a nuclear power station beside Llyn Trawsfynydd began in 1959 with the first power produced in 1965. The site was operational until 1991 though it continues as an employer during its decommissioning phase. Pumped storage hydroelectric schemes are in operation at Llanberis and Ffestiniog.

 

Research indicates that there were 3.67 million visitors to Snowdonia National Park in 2013, with approximately 9.74 million tourist days spent in the park during that year. Total tourist expenditure was £433.6 million in 2013.

 

Many of the hikers in the area concentrate on Snowdon itself. It is regarded as a fine mountain, but at times gets very crowded; in addition the Snowdon Mountain Railway runs to the summit.

 

The other high mountains with their boulder-strewn summits as well as Tryfan, one of the few mountains in the UK south of Scotland whose ascent needs hands as well as feet are also very popular. However, there are also some spectacular walks in Snowdonia on the lower mountains, and they tend to be relatively unfrequented. Among hikers' favourites are Y Garn (east of Llanberis) along the ridge to Elidir Fawr; Mynydd Tal-y-Mignedd (west of Snowdon) along the Nantlle Ridge to Mynydd Drws-y-Coed; Moelwyn Mawr (west of Blaenau Ffestiniog); and Pen Llithrig y Wrach north of Capel Curig. Further south are Y Llethr in the Rhinogydd, and Cadair Idris near Dolgellau.

 

The park has 1,479 miles (2,380 km) of public footpaths, 164 miles (264 km) of public bridleways, and 46 miles (74 km) of other public rights of way. A large part of the park is also covered by right to roam laws.

 

The Wales Coast Path runs within the park between Machynlleth and Penrhyndeudraeth, save for short sections of coast in the vicinity of Tywyn and Barmouth which are excluded from the park. It touches the park boundary again at Penmaen-bach Point on the north coast. An inland alternative exists between Llanfairfechan and Conwy, wholly within the park. The North Wales Path, which predates the WCP, enters the park north of Bethesda and follows a route broadly parallel to the north coast visiting Aber Falls and the Sychnant Pass before exiting the park on the descent from Conwy Mountain. The Cambrian Way is a long-distance trail between Cardiff and Conwy that stays almost entirely within the national park from Mallwyd northwards. It was officially recognised in 2019, and is now depicted on Ordnance Survey maps.

 

The use of the English names for the area has been divisive, with an increase in protests against their use since 2020; these led to the national park authority deciding to use Welsh names as far as legally possible in November 2022. An early example of pressure to deprecate Snowdon and Snowdonia was a 2003 campaign by Cymuned, inspired by campaigns to refer to Ayers Rock as Uluru and Mount Everest as Qomolangma.

 

In 2020 an e-petition calling for the removal of the English names was put forward to the Senedd, but rejected as responsibility lies with the national park authority. In 2021 an e-petition on the same topic attracted more than 5,300 signatures and was presented to the national park authority.

 

On 28 April 2021 Gwynedd councillor John Pughe Roberts put forward a motion to use the Welsh names exclusively, calling this a "question of respect for the Welsh language". The motion was not considered and delayed, as the national park authority already appointed a "Welsh Place Names Task and Finish Group" to investigate the issue. The park authority however cannot compel other bodies and/or individuals to stop using the English names, with the proposals facing some criticism.

 

In May 2021, following the dismissal of the motion, YouGov conducted a poll on Snowdon's name. 60% of Welsh adults supported the English name Snowdon, compared to 30% wanting the Welsh name Yr Wyddfa. Separating by language, 59% of Welsh speakers preferred the Welsh name, but 37% of these still wanted Snowdon to be used as well. 69% of non-Welsh speakers firmly supported Snowdon as the Mountain's name. The proposals to rename Snowdon are usually accompanied with proposals to rename Snowdonia.

 

On 16 November 2022, Members of the Snowdonia National Park Authority committee voted to use the Welsh names Yr Wyddfa and Eryri to refer to the mountain and the national park, rather than the English names, in materials produced by the authority. The national park authority described the decision as "decisive action" and the authority's head of culture heritage stated that Welsh place names were part of the area's "special qualities" and that other public bodies, English-language press and filming companies have used the Welsh-language names. Before the decision the park had already prioritised the Welsh names by using them first and giving the English names in parentheses. The name "Snowdonia" cannot be abandoned entirely, as it is set in law and so must be used in statutory documents. The authority announced a review of the authority's branding in 2023 to adapt to the new approach to Welsh place names.

 

Gwynedd is a county in the north-west of Wales. It borders Anglesey across the Menai Strait to the north, Conwy, Denbighshire, and Powys to the east, Ceredigion over the Dyfi estuary to the south, and the Irish Sea to the west. The city of Bangor is the largest settlement, and the administrative centre is Caernarfon. The preserved county of Gwynedd, which is used for ceremonial purposes, includes the Isle of Anglesey.

 

Gwynedd is the second largest county in Wales but sparsely populated, with an area of 979 square miles (2,540 km2) and a population of 117,400. After Bangor (18,322), the largest settlements are Caernarfon (9,852), Bethesda (4,735), and Pwllheli (4,076). The county has the highest percentage of Welsh speakers in Wales, at 64.4%, and is considered a heartland of the language.

 

The geography of Gwynedd is mountainous, with a long coastline to the west. Much of the county is covered by Snowdonia National Park (Eryri), which contains Wales's highest mountain, Snowdon (Yr Wyddfa; 3,560 feet, 1,090 m). To the west, the Llŷn Peninsula is flatter and renowned for its scenic coastline, part of which is protected by the Llŷn AONB. Gwynedd also contains several of Wales's largest lakes and reservoirs, including the largest, Bala Lake (Llyn Tegid).

 

The area which is now the county has played a prominent part in the history of Wales. It formed part of the core of the Kingdom of Gwynedd and the native Principality of Wales, which under the House of Aberffraw remained independent from the Kingdom of England until Edward I's conquest between 1277 and 1283. Edward built the castles at Caernarfon and Harlech, which form part of the Castles and Town Walls of King Edward in Gwynedd World Heritage Site. During the Industrial Revolution the slate industry rapidly developed; in the late nineteenth century the neighbouring Penrhyn and Dinorwic quarries were the largest in the world, and the Slate Landscape of Northwest Wales is now a World Heritage Site. Gwynedd covers the majority of the historic counties of Caernarfonshire and Merionethshire.

 

In the past, historians such as J. E. Lloyd assumed that the Celtic source of the word Gwynedd meant 'collection of tribes' – the same root as the Irish fine, meaning 'tribe'. Further, a connection is recognised between the name and the Irish Féni, an early ethnonym for the Irish themselves, related to fían, 'company of hunting and fighting men, company of warriors under a leader'. Perhaps *u̯en-, u̯enə ('strive, hope, wish') is the Indo-European stem. The Irish settled in NW Wales, and in Dyfed, at the end of the Roman era. Venedotia was the Latin form, and in Penmachno there is a memorial stone from c. AD 500 which reads: Cantiori Hic Iacit Venedotis ('Here lies Cantiorix, citizen of Gwynedd'). The name was retained by the Brythons when the kingdom of Gwynedd was formed in the 5th century, and it remained until the invasion of Edward I. This historical name was revived when the new county was formed in 1974.

 

Gwynedd was an independent kingdom from the end of the Roman period until the 13th century, when it was conquered by England. The modern Gwynedd was one of eight Welsh counties created on 1 April 1974 under the Local Government Act 1972. It covered the entirety of the historic counties of Anglesey and Caernarfonshire, and all of Merionethshire apart from Edeirnion Rural District (which went to Clwyd); and also a few parishes of Denbighshire: Llanrwst, Llansanffraid Glan Conwy, Eglwysbach, Llanddoged, Llanrwst and Tir Ifan.

 

The county was divided into five districts: Aberconwy, Arfon, Dwyfor, Meirionnydd and Anglesey.

 

The Local Government (Wales) Act 1994 abolished the 1974 county (and the five districts) on 1 April 1996, and its area was divided: the Isle of Anglesey became an independent unitary authority, and Aberconwy (which included the former Denbighshire parishes) passed to the new Conwy County Borough. The remainder of the county was constituted as a principal area, with the name Caernarfonshire and Merionethshire, as it covers most of the areas of those two historic counties. As one of its first actions, the Council renamed itself Gwynedd on 2 April 1996. The present Gwynedd local government area is governed by Gwynedd Council. As a unitary authority, the modern entity no longer has any districts, but Arfon, Dwyfor and Meirionnydd remain as area committees.

 

The pre-1996 boundaries were retained as a preserved county for a few purposes such as the Lieutenancy. In 2003, the boundary with Clwyd was adjusted to match the modern local government boundary, so that the preserved county now covers the two local government areas of Gwynedd and Anglesey. Conwy county borough is now entirely within Clwyd.

 

A Gwynedd Constabulary was formed in 1950 by the merger of the Anglesey, Caernarfonshire and Merionethshire forces. A further amalgamation took place in the 1960s when Gwynedd Constabulary was merged with the Flintshire and Denbighshire county forces, retaining the name Gwynedd. In one proposal for local government reform in Wales, Gwynedd had been proposed as a name for a local authority covering all of north Wales, but the scheme as enacted divided this area between Gwynedd and Clwyd. To prevent confusion, the Gwynedd Constabulary was therefore renamed the North Wales Police.

 

The Snowdonia National Park was formed in 1951. After the 1974 local authority reorganisation, the park fell entirely within the boundaries of Gwynedd, and was run as a department of Gwynedd County Council. After the 1996 local government reorganisation, part of the park fell under Conwy County Borough, and the park's administration separated from the Gwynedd council. Gwynedd Council still appoints nine of the eighteen members of the Snowdonia National Park Authority; Conwy County Borough Council appoints three; and the Welsh Government appoints the remaining six.

 

There has been considerable inwards migration to Gwynedd, particularly from England. According to the 2021 census, 66.6% of residents had been born in Wales whilst 27.1% were born in England.

 

The county has a mixed economy. An important part of the economy is based on tourism: many visitors are attracted by the many beaches and the mountains. A significant part of the county lies within the Snowdonia National Park, which extends from the north coast down to the district of Meirionnydd in the south. But tourism provides seasonal employment and thus there is a shortage of jobs in the winter.

 

Agriculture is less important than in the past, especially in terms of the number of people who earn their living on the land, but it remains an important element of the economy.

 

The most important of the traditional industries is the slate industry, but these days only a small percentage of workers earn their living in the slate quarries.

 

Industries which have developed more recently include TV and sound studios: the record company Sain has its HQ in the county.

 

The education sector is also very important for the local economy, including Bangor University and Further Education colleges, Coleg Meirion-Dwyfor and Coleg Menai, both now part of Grŵp Llandrillo Menai.

 

The proportion of respondents in the 2011 census who said they could speak Welsh.

Gwynedd has the highest proportion of people in Wales who can speak Welsh. According to the 2021 census, 64.4% of the population aged three and over stated that they could speak Welsh,[7] while 64.4% noted that they could speak Welsh in the 2011 census.

 

It is estimated that 83% of the county's Welsh-speakers are fluent, the highest percentage of all counties in Wales.[9] The age group with the highest proportion of Welsh speakers in Gwynedd were those between ages 5–15, of whom 92.3% stated that they could speak Welsh in 2011.

 

The proportion of Welsh speakers in Gwynedd declined between 1991 and 2001,[10] from 72.1% to 68.7%, even though the proportion of Welsh speakers in Wales as a whole increased during that decade to 20.5%.

 

The Annual Population Survey estimated that as of March 2023, 77.0% of those in Gwynedd aged three years and above could speak Welsh.

 

Notable people

Leslie Bonnet (1902–1985), RAF officer, writer; originated the Welsh Harlequin duck in Criccieth

Sir Dave Brailsford (born 1964), cycling coach; grew up in Deiniolen, near Caernarfon

Duffy (born 1984), singer, songwriter and actress; born in Bangor, Gwynedd

Edward II of England (1284–1327), born in Caernarfon Castle

Elin Fflur (born 1984), singer-songwriter, TV and radio presenter; went to Bangor University

Bryn Fôn (born 1954), actor and singer-songwriter; born in Llanllyfni, Caernarfonshire.

Wayne Hennessey (born 1987), football goalkeeper with 108 caps for Wales; born in Bangor, Gwynedd

John Jones (c. 1530 – 1598), a Franciscan friar, Roman Catholic priest and martyr; born at Clynnog

Sir Love Jones-Parry, 1st Baronet (1832–1891), landowner and politician, co-founder of the Y Wladfa settlement in Patagonia

T. E. Lawrence (1888–1935), archaeologist, army officer and inspiration for Lawrence of Arabia, born in Tremadog

David Lloyd George (1863–1945), statesman and Prime Minister; lived in Llanystumdwy from infancy

Sasha (born 1969), disc jockey, born in Bangor, Gwynedd

Sir Bryn Terfel (born 1965), bass-baritone opera and concert singer from Pant Glas

Sir Clough Williams-Ellis (1883–1978), architect of Portmeirion

Owain Fôn Williams, (born 1987), footballer with 443 club caps; born and raised in Penygroes, Gwynedd.

Hedd Wyn (1887–1917), poet from the village of Trawsfynydd; killed in WWI

Shaoguan Train Station, Guangdong, China

Forest path, wheel chair accessible, in western Norway. Also of note: the path was constructed by volunteers.

A Mirror Image (in a plane mirror) is a reflected duplication of an object that appears almost identical, but is reversed in the direction perpendicular to the mirror surface. As an optical effect it results from reflection off from substances such as a mirror or water. It is also a concept in geometry and can be used as a conceptualization process for 3-D structures. Two-dimensional mirror images can be seen in the reflections of mirrors or other reflecting surfaces, or on a printed surface seen inside-out.

 

If we first look at an object that is effectively two-dimensional (such as the writing on a card) and then turn the card to face a mirror, the object turns through an angle of 180° and we see a left-right reversal in the mirror. In this example, it is the change in orientation rather than the mirror itself that causes the observed reversal. Another example is when we stand with our backs to the mirror and face an object that's in front of the mirror. Then we compare the object with its reflection by turning ourselves 180°, towards the mirror. Again we perceive a left-right reversal due to a change in our orientation. So, in these examples the mirror does not actually cause the observed reversals.

 

The palace was constructed on a monumental scale that was intended to reflect the might and power of Imperial Russia. From the palace, the Tsar ruled over 22,400,000 square kilometers (8,600,000 sq mi) (almost 1/6 of the Earth's landmass) and over 125 million subjects by the end of the 19th century. It was designed by many architects, most notably Bartolomeo Rastrelli, in what came to be known as the Elizabethan Baroque style. The green-and-white palace has the shape of an elongated rectangle, and its principal façade is 215 metres (705 ft) long and 30 m (98 ft) high. The Winter Palace has been calculated to contain 1,886 doors, 1,945 windows, 1,500 rooms and 117 staircases. Following a serious fire, the palace's rebuilding of 1837 left the exterior unchanged, but large parts of the interior were redesigned in a variety of tastes and styles, leading the palace to be described as a "19th-century palace inspired by a model in Rococo style".

 

The State Hermitage Museum is a museum of art and culture in Saint Petersburg. The second-largest art museum in the world, it was founded in 1764 when Empress Catherine the Great acquired an impressive collection of paintings from the Berlin merchant Johann Ernst Gotzkowsky. The museum celebrates the anniversary of its founding each year on 7 December, Saint Catherine's Day. It has been open to the public since 1852. It attracted 4,956,524 visitors in 2019, ranking it eighth among the most visited art museums in the world. Of the six buildings in the main museum complex, five—namely the Winter Palace, Small Hermitage, Old Hermitage, New Hermitage, and Hermitage Theatre—are open to the public. The entrance ticket for foreign tourists costs more than the fee paid by citizens of Russia and Belarus. However, entrance is free of charge the third Thursday of every month for all visitors, and free daily for students and children. The museum is closed on Mondays. The entrance for individual visitors is located in the Winter Palace, accessible from the Courtyard.

Source: en.wikipedia.org/wiki/Arizona

 

Arizona is a state in the Southwestern region of the United States, sharing the Four Corners region of the western United States with Colorado, New Mexico, and Utah. Its other neighboring states are Nevada to the northwest and California to the west. It also shares an international border with the Mexican states of Sonora and Baja California to the south and southwest. It is the 6th-largest and the 14th-most-populous of the 50 states. Its capital and largest city is Phoenix, which is the most populous state capital in the United States.

 

Arizona is the 48th state and last of the contiguous states to be admitted to the Union, achieving statehood on February 14, 1912. Historically part of the territory of Alta California and Nuevo México in New Spain, it became part of independent Mexico in 1821. After being defeated in the Mexican–American War, Mexico ceded much of this territory to the United States in 1848, where the area became part of the territory of New Mexico. The southernmost portion of the state was acquired in 1853 through the Gadsden Purchase.

 

Southern Arizona is known for its desert climate, with extremely hot summers and mild winters. Northern Arizona features forests of pine, Douglas fir, and spruce trees; the Colorado Plateau; mountain ranges (such as the San Francisco Mountains); as well as large, deep canyons, with much more moderate summer temperatures and significant winter snowfalls. There are ski resorts in the areas of Flagstaff, Sunrise, and Tucson. In addition to the internationally known Grand Canyon National Park, which is one of the world's seven natural wonders, there are several national forests, national parks, and national monuments.

 

Arizona is home to a diverse population. About one-quarter of the state is made up of Indian reservations that serve as the home of 27 federally recognized Native American tribes, including the Navajo Nation, the largest in the state and the country, with more than 300,000 citizens. Since the 1980s, the proportion of Hispanics has grown significantly owing to migration from Mexico and Central America. A substantial portion of the population are followers of the Roman Catholic Church and the Church of Jesus Christ of Latter-day Saints. Arizona's population and economy have grown dramatically since the 1950s because of inward migration, and the state is now a major hub of the Sun Belt. Cities such as Phoenix and Tucson have developed large, sprawling suburban areas. Many large companies, such as PetSmart and Circle K, have headquarters in the state, and Arizona is home to major universities, including the University of Arizona, Arizona State University, and Northern Arizona University. The state is known for a history of conservative politicians such as Barry Goldwater and John McCain, though it has become a swing state in recent years.

 

Source: en.wikipedia.org/wiki/Antelope_Canyon

 

Navajo Upper Antelope Canyon is a slot canyon in the American Southwest, on Navajo land east of Lechee, Arizona. It includes six separate, scenic slot canyon sections on the Navajo Reservation, referred to as Upper Antelope Canyon (or The Crack), Rattle Snake Canyon, Owl Canyon, Mountain Sheep Canyon, Canyon X and Lower Antelope Canyon (or The Corkscrew). It is the primary attraction of Lake Powell Navajo Tribal Park, along with a hiking trail to Rainbow Bridge National Monument.

 

The Navajo name for Upper Antelope Canyon is Tsé bighánílíní, which means 'the place where water runs through the (Slot Canyon) rocks'. Lower Antelope Canyon is Hazdistazí (called "Hasdestwazi" by the Navajo Parks and Recreation Department), or 'spiral rock arches'. Both are in the LeChee Chapter of the Navajo Nation. They are accessible by Navajo guided tour only.

 

Additional Foreign Language Tags:

 

(United States) "الولايات المتحدة" "Vereinigte Staaten" "アメリカ" "米国" "美国" "미국" "Estados Unidos" "États-Unis" "ארצות הברית" "संयुक्त राज्य" "США"

 

(Arizona) "أريزونا" "亚利桑那州" "אריזונה" "एरिजोना" "アリゾナ州" "애리조나" "Аризона"

The location of Big Ed Hurley from the TV series Twin Peaks, in Preston, Washington, USA.

 

Named after railway official William T. Preston, it is a historic mill town on the northeast edge of the large Tiger Mountain State Forest and is located within commuting distance of Seattle and Bellevue.

 

The local Raging River feeds into the Snoqualmie River at Fall City and offers recreational activities like fly-fishing and swimming. Eastside Fire & Rescue has an all-volunteer fire station, Station 74, staffed by residents of Preston and nearby communities, which serves the Preston area.

 

The Preston Community Club is a volunteer organization that was created to unite and protect the historic Preston community by organizing town events and acting as liaisons to local and state government.

 

Several small stores have popped up as the area has grown, such as the Preston General store, Indoor Garden & Lighting, Coffee Too!, Subway, and the Preston Post Office. Several larger companies have taken advantage of Preston's accessibility, such as bottled water company Talking Rain, SanMar, and Platt.

 

Information Sources:

en.wikipedia.org/wiki/Preston,_Washington

www.twinpeaksblog.com/2018/05/15/setting-the-stage-big-ed...

www.cntraveler.com/galleries/2015-03-16/10-real-life-twin...

 

Dudiptsar lake or Dudipat Lake is a beautiful lake encircled by snow clad peaks. The lake lies in the extreme north of Kaghan Valley at N35.0185 E74.0895 and is about a four hours drive from the chief town Naran. The road is not entirely accessible for cars, even Jeeps. From Besal onwards the visitors have to trek about 6-8 hours in vast alpine meadows to reach the lake.

 

Trek consists of at sometimes steep climb while at other places walk through huge flat valleys, but at all the time filled with amazing sights.

 

Its water is a beautiful greenish blue and very cold too. Dudipatsar is also close to another major Lake Lulusar which is the main contributory to the Kunhar river that runs through Kaghan valley. At a distance from the lake lies the Babusar Top or the Babusar Pass which is the end of 150 km long Kaghan valley.

 

The whole area is accessible for four months every year from June-September after which it is closed to snow.

 

It is highly not advised to track it in snow, as there is a high probability of avalanches in the area. The lake used to have abundance of trout, but illegal fishing using dynamite and nets has resulted in a sharp decline.

 

The word "dudi" means white and "sar" means lake. This name has been given to the lake because of the white color of snow at surrounding peaks. In summer the water of the lake reflects like a mirror. Getting to the lake takes four to six hours of tough hiking and trekking.

 

The word "sar" is used with the name of each lake in the area meaning lake. In the summer when the water of the lake reflects like a mirror a large number of visitors from different areas of the country come to watch the enchanting views of these lake.

 

The whole area is private property but declared national park by Government of Pakistan.

 

The deep blue Dudipat Sar, at 3,800 meters, is surrounded by green hills at about 4,800 meters, with snow patches in the shady hollows. This lake is very little visited by people and its natural beauty is still very much protected. October 8, 2005's earthquake in North Pakistan has made it more difficult to be accessed.

 

Seonjeongneung in Gangnam is home to three royal tombs. Also referred to as Seolleung, Jeongneung, or Samneung, but officially known as Seonjeongneung. Here there are the tombs of King Seongjong (the 9th king of the Joseon Dynasty), Queen Jeonghyeon (the second wife of King Seongjong) and King Jungjong (a son of the two). The tombs are set in a beautiful parkland setting with a mix of grassland and woods to explore and learn about the historic setting, or just to enjoy some nature in the bustling Gangnam district.

 

Accessible from:

Seolleung Station, Line 2 or the Bundang Line, exit 8.

 

Near the Massa Martana train station, in a place remained unchanged and easily accessible on foot, is a completely intact Roman bridge built with perfectly squared massive blocks of travertine in a single arch. It granted passage on the ancient Via Flaminia over the Fonnaia river. The Fonnaia bridge hasn’t changed since the restoration of the Augustan period (27 AD), is 15 m long, 8 m high, with a single circular arch of 3.5, has a lower slanting surface so that the road above can maintain its geometric axis. On the inner surface of the arch the blocks are disposed in even rows, and marked by letters and numbers that indicate the quarry.

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Locandina:

 

stanzedicinema.com/wp-content/uploads/2009/12/children-lo...

 

www.imdb.com/it/title/tt0206634/

 

www.imdb.com/it/video/vi3459826457/?playlistId=tt0206634&...

 

Gianluca Gotto

 

youtu.be/ESmJKPZtZw4

 

www.mondadori.it/content/uploads/2021/02/978880472904HIG-...

 

www.facebook.com/watch/?v=706199753402023

 

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or…. Press the “L” button to zoom in the image;

 

clicca sulla piccola icona per attivare lo slideshow: sulla facciata principale del photostream, in alto a destra c'è un piccolo rettangolo (rappresenta il monitor) con dentro un piccolo triangolo nero;

oppure…. premi il tasto “L” per ingrandire l'immagine;

 

Qi Bo's photos on Fluidr

  

Qi Bo's photos on Flickriver

  

www.worldphoto.org/sony-world-photography-awards/winners-...

  

www.fotografidigitali.it/gallery/2726/opere-italiane-segn...

 

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I describe this photographic series (with some “poetic license” on the theme of “beach photography”) by quoting an introduction I wrote some time ago, for a photographic series of mine having the same theme today. I would like to focus on two photos from the current series, on how, from a particular situation, in this case photographic, others can arise, I would like to share this with those who are not too bored reading this story: I photographed a young girl while she was reading a book, she was sitting inside one of the many lava formations present along the shore of Naxos (near Taormina), dug with a perfectly rounded shape (this suggests that their origin is man-made, I will not dwell on the hypothesis that attempts to explain these ancient formations), the little water collected inside these "pools" certainly gave a little refreshment to the unaware "reader", once at home, curiosity pushed me to investigate what she was reading, the high resolution of the photos allowed me to easily read the two pages of the book she was holding in her hand, and it was a kind of revelation, some paragraphs of the book, and I was more and more intrigued, about what the book was and its Author, a A quick Google search, and I found what I was looking for. The book is titled "Something Wonderful Always Happens." Its author is Gianluca Gotto. I didn't know him, but I was able to watch and listen to him on YouTube. I found it extremely interesting. I've already ordered the book on Amazon. I'll just quote a short excerpt from the page the reader was reading. It's brief, as I don't want to infringe on any copyright: "(...) do you know what the three poisons of man are according to Buddhism?" I shook my head. "Greed, or the desire to always have more when each of us already has everything we need; ignorance, or the lack of awareness: believing that life is different from what it is here and now; and finally, anger, a condition contrary to any form of happiness."

Beach holidays were born in the 1700s in Great Britain, this social phenomenon was born in which bathers for the first time go to the beaches, certainly not as sunny as those bathed by the Mediterranean Sea, they are fully dressed; this "new fashion" is also encouraged by the belief of English doctors since the beginning of the eighteenth century (starting around 1720), that breathing the brackish sea air and bathing in cold sea water is healthy, invigorates the body and cure lung diseases (conviction even more strengthened by the discovery of oxygen by Antoine Lavoisier in 1778, which led to the greater diffusion and conviction of the theories on the health benefits of sea air, which was thought to be more oxygenated and pure), these theories push many people from Northern Europe suffering from severe lung diseases to spend long periods in southern Europe, often in the south of Italy, this explains why characters with extraordinary qualities come to Taormina to cure their tuberculosis. The photographer baron Wilhelm von Gloeden and the English lady Florence Trevelyan Trevelyan had the seawater brought with their mules from Isola Bella, but while W. Von Gloeden heated the sea water, the English noblewoman Lady Trevelian did not heat it, mindful of the teachings of the English medical school, this will cause her death from bronchopneumonia on 4 October 1907 (see my previous "photographic stories" about Taormina). In fact, "thalassotherapy" was born in Great Britain, together with the social and cultural phenomenon of frequenting bathing beaches (before the beginning of the 18th century, the sea and its beaches were lived, except for reasons of trade and fishing, in a dark and negative way, from the sea often came very serious dangers such as the sudden landings of ferocious pirates, or foreigners carrying very serious diseases could land). Thus the fashion of spending holidays by the sea was born in the English aristocracy and high bourgeoisie of the time, subsequently the habit of going to the sea spread to all levels of society, the railways that were built throughout Great Britain to 'beginning of the nineteenth century, made travel to the ocean accessible even to the lower classes, they too will frequent the seaside resorts, Blackpool becomes the first seaside resort in Great Britain completely frequented by the working classes thanks to the presence of low-cost bathing establishments; the great and definitive boom in seaside tourism will then take place in the 1950s and 1960s. This being the case, it should not be surprising to know that in Great Britain the beaches are more frequented than one might instinctively think due to a climate very different from the Mediterranean one, and that this socio-cultural phenomenon has been investigated at the photographic by photographers of the same Great Britain, of these I mention four names. An important photographer, who probably inspired subsequent photographers, was Tony Ray-Jones, who died prematurely in 1972, at the young age of 30, who was trying to create a “photographic memory” of the stereotypes of the English people; the famous photojournalist Martin Parr, who, although inspired by the previous one, differs from it for his way of doing “social satire” with his goal; finally, I would like to mention David Hurn and Simon Roberts, the latter with wider-ranging photographs, with photographs more detached from the individual. In Italy there are numerous photographers (I will mention only a few) who have made in their long career images captured in seaside resorts (generally we speaking of "beach photography" similar to "street photography"), photographs that are often unique in their style, such as that adopted by Franco Fontana, I mention Mimmo Jodice, Ferdinando Scianna (of whom I am honored to have known him personally), and Massimo Vitali, famous photographer (understood by some as "the photographer of the beaches"), especially for his beautiful photographs taken on the beaches (but not only), thanks to the presence of elevated fixed structures as a kind of mezzanine, built specifically in the bathing beaches for the realization of his photographs. This is my introduction to talk about the theme proposed here, that of “beach photography” (with some exceptions for “narrative” reasons), with a series of photographs taken on the beaches surrounding Taormina (Sicily). ……………………………………………………………

 

Descrivo questa serie fotografica (con qualche “licenza poetica” sul tema della “beach photography”) riportando una mia introduzione scritta po’ di tempo fa, per una mia serie fotografica avente lo stesso tema odierno. Desidero soffermarmi su due foto dell’attuale serie, di come, da una particolare situazione, in questo caso fotografica, ne possano scaturire altre, desidero condividere ciò con chi non si annoia troppo a leggere questo racconto: ho fotografato una giovane ragazza mentre stava leggendo un libro, era seduta all’interno di una delle tante formazioni laviche presenti lungo il bagnasciuga di Naxos (vicino Taormina), scavate con forma perfettamente rotondeggiante (questo fa pensare che la loro origine sia manufatta, non mi dilungo sulla ipotesi che tenta di spiegare queste antiche formazioni), la poca acqua raccolta all’interno di queste “vasche” davano certamente un po’ di refrigerio alla inconsapevole “lettrice” , una volta a casa, la curiosità mi ha spinto ad indagare su cosa stesse leggendo, l’elevata risoluzione delle foto mi ha consentito di leggere con facilità le due pagine del libro da lei tenuto in mano, ed è stata una specie di rivelazione, qualche trafiletto del libro, ed ero sempre più incuriosito, su quale fosse il libro ed il suo Autore, una breve ricerca su Google, ed ho trovato quanto cercavo, il libro si intitola “Succede sempre qualcosa di meraviglioso”, il suo Autore è Gianluca Gotto, non lo conoscevo, su You Tube ho potuto vederlo ed ascoltarlo, l’ho trovato estremamente interessante, il libro l’ho già ordinato su Amazon; riporterò qui solo un breve trafiletto preso dalla pagina che stava leggendo la lettrice, breve, non vorrei incorrere in qualche violazione sui diritti d’Autore: “ (…) sai quali sono i tre veleni dell’uomo secondo il Buddhismo ?” Scossi la testa. “La cupidigia, ovvero il desiderio di avere sempre di più quando ognuno di noi ha già tutto ciò che gli serve; l’ignoranza, ovvero la mancanza di consapevolezza: credere che la vita sia diversa da ciò che è qui e ora; infine la rabbia, una condizione contraria a ogni forma di felicità.”

  

Le vacanze al mare nascono nel ‘700 in Gran Bretagna, nasce questo fenomeno sociale nel quale i bagnanti per la prima volta si recano sulle spiagge, non certo assolate come quelle bagnate dal mar Mediterraneo, sono completamente vestiti; questa “nuova moda” è anche incoraggiata dalla convinzione dei medici inglesi fin dall’inizio del ‘700 (a partire dal 1720 circa), che respirare l’aria salmastra del mare e fare il bagno nell’acqua marina fredda sia salutare, rinvigorisca il corpo e curi le malattie polmonari (convinzione ancor più rafforzata dalla scoperta dell’ossigeno da parte di Antoine Lavoisier nel 1778, che portò alla maggiore diffusione e convinzione delle teorie sui benefici per la salute dell’aria di mare, che si pensava essere più ossigenata e pura), queste teorie spingono molte persone del Nord Europa affette da gravi malattie polmonari a trascorrere dei lunghi periodi nel sud Europa, spesso nel meridione d’Italia, questo spiega perché a Taormina giungono personaggi dalle qualità straordinarie per curare il proprio “mal sottile”, il barone fotografo Wilhelm von Gloeden e la lady inglese Florence Trevelyan Trevelyan si facevano portare coi muli l’acqua di mare proveniente dall’Isola Bella, però mentre W. Von Gloeden riscaldava l’acqua marina, la nobildonna inglese lady Trevelian non la riscaldava, memore degli insegnamenti della scuola medica inglese, questo causerà la sua morte per broncopolmonite il 4 ottobre del 1907 (vedi i miei precedenti “racconti fotografici” su Taormina). Infatti la “talassoterapia” nasce in Gran Bretagna, insieme al fenomeno sociale e culturale della frequentazione dei lidi balneari (prima dell’inizio del ‘700, il mare e le sue spiagge erano vissuti, tranne che per motivi di commercio e di pesca, in maniera oscura e negativa, dal mare spesso provenivano gravissimi pericoli come gli sbarchi improvvisi di feroci pirati, oppure potevano sbarcare stranieri portatori di gravissime malattie). Nell’aristocrazia e nell’alta borghesia inglese di allora nasce così la moda di trascorrere le vacanze al mare, successivamente l’abitudine di andare al mare si diffonde a tutti i livelli della società, le ferrovie che furono costruite in tutta la Gran Bretagna all’inizio dell’Ottocento, resero i viaggi verso l’oceano accessibili anche per i ceti più bassi, quelli più popolari e meno agiati, anch’essi frequenteranno le località balneari, Blackpool diviene la prima località balneare della Gran Bretagna completamente frequentata dalle classi popolari grazie alla presenza di stabilimenti balneari a basso costo; il grande e definitivo boom del turismo balneare si avrà poi negli anni ’50 e ’60. Stando così le cose, non ci si deve meravigliare nel sapere che in Gran Bretagna le spiagge sono più frequentate di quanto istintivamente si possa pensare a causa di un clima ben diverso da quello Mediterraneo, e che questo fenomeno socio-culturale sia stato indagato a livello fotografico da parte di fotografi della stessa Gran Bretagna, di questi cito quattro nomi. Un importante fotografo, che probabilmente ispirò i successivi fotografi, fu Tony Ray-Jones, scomparso prematuramente nel 1972, alla giovane età di 30 anni, il quale cercava di realizzare una “memoria fotografica” degli stereotipi del popolo inglese; il famoso fotoreporter Martin Parr, il quale pur ispirandosi al precedente, se ne differenzia per il suo modo di fare “satira sociale” col suo obiettivo; infine desidero menzionare David Hurn e Simon Roberts, quest’ultimo con fotografie di più ampio respiro, con fotografie più distaccate dal singolo individuo. In Italia numerosi sono i fotografi (ne cito solo qualcuno) che hanno realizzato nella loro lunga carriera immagini colte in località balneari (genericamente si parla di “beach photography” affine alla “street photography”), fotografie spesso uniche nel loro stile, come quello adottato da Franco Fontana, menziono Mimmo Jodice, Ferdinando Scianna (del quale mi onoro di averlo conosciuto personalmente), e Massimo Vitali, famoso fotografo (da alcuni inteso come “il fotografo delle spiagge”), soprattutto per le sue bellissime fotografie realizzate sui lidi (ma non solo), grazie alla presenza di strutture fisse sopraelevate a mò di soppalco, costruite appositamente nei lidi balneari per la realizzazione delle sue fotografie. Questo mio incipit, per introdurre il tema da me affrontato, quello della “beach photography” (con qualche eccezione per motivi ”narrativi”), con una serie di fotografie realizzate sulle spiagge circostanti Taormina (Sicilia).

 

...........................................................................

 

Near Wajurda Point, Nelson's Beach, Mimosa Rocks National Park, NSW AUS. This beach is accessible by dirt road and popular with surfers.

From City of St.Catharines Guide to Accessible information & Communication training. December 5, 2011

 

Regardless of their disabilities, all Ontarians have the same rights to communicate as individuals without a disability; rights that are protected by the Ontario Human Rights Code.

 

Organizations must be prepared to provide alternative formats of traditional communication tools. This includes written documents, reports, brochures, and forms and also extends to multi-media tools, such as videos and website.

 

Must provide accessible formats

Upon Request

In a Timely Manner

At NO extra cost!

 

The Information and Communications Standard section under the Integrated Accessibility Regulation provides guidance for providing accessible communication.

Not just the law but good customer service, too

 

StatsCan estimates that by 2026 one of every five people living in Canada will be a senior. As people age, they have greater incidences of hearing loss, low vision, cognitive impairments and lessened mobility and dexterity.

 

Approximately 836,000 Canadians identified themselves as having a seeing disability in a 2007 StatsCan study, while approximately 10 per cent of Canada’s population suffers from some form of hearing lost.

 

Add to this the 10 per cent of Canadians who have a learning disability and it is easy to see that in the future increasing numbers of residents and customers will require some kind of alternative format to access information from the City.

 

By providing accessible communications, we will increase the number of people who can access information, reaching a greater number of our residents.

 

And that is good customer service.

 

Use Plain Language

 

Plain Language is text that the reader can read and understand the first time.

 

It sounds easy enough, but text is often cluttered with acronyms, jargon and complex sentence structure.

 

Text that is clear and easy to read benefits customers with learning disabilities and low literacy skills. It improves comprehension for all users and allows for easy adaptation to other formats.

 

When writing plain language, remember to:

•Keep your intended audience in mind

•Use an active voice

•Shorten sentences

•Use everyday words

•Eliminate jargon

•Use simple sentence structure and grammar

 

Other notes:

 

Align Left (justified text causes problems)

Watch Font size (no less than 12 point font)

Use styles / style sheets for formatting

Use Tables for data not formatting

Provide alternative text for charts and pictures

Caption videos

  

SCRTD was the nation's leader in requiring its buses to be wheelchair accessible.

New campus of the University of Economics and Business in Vienna. The nickname of this faculty building D4 by Architects of Estudio Carme Pinós S.L. from Barcelona, Spain, is Tetris Building. See www.wu.ac.at/campus/architecture/en/

 

The Department building D4 was designed by Barcelona's Estudio Carme Pinós S. L. It is located directly across from the AD administration building and forms the northernmost border of the campus to the exhibition grounds Messe Wien.

 

The geometric façade features a playful arrangement of parallelograms with dynamically placed windows, also based on a pattern of intersecting parallelograms. Folding aluminum shutters provide protection from direct sun and give the façade an ever-changing appearance. While spacious and rambling, the building has a well-defined central point, from which various connections branch off.

 

The entry area is the main hub for accessing the offices, the café, and the Library for Social Sciences located on the ground floor of the building. The front offices of three Departments as well as five Research Institutes on four upper levels are also accessible from this central core. Additional Department offices are distributed over two stories of the building, connected by internal staircases. Seminar and project rooms are located in separate, slightly raised elements on the ground floor, as are the self-study zones. The interior design is based on the same parallelogram pattern as the façade, creating hallways, additional functional areas, and storage space.

Schweiz / Wallis - Aletschgletscher

 

The Aletsch Glacier (German: Aletschgletscher, German pronunciation: [ˈalɛtʃˌɡlɛtʃɐ]) or Great Aletsch Glacier (Grosser Aletschgletscher) is the largest glacier in the Alps. It has a length of about 23 km (14 mi) (2014), has about a volume of 15.4 km3 (3.7 cu mi) (2011), and covers about 81.7 km2 (31.5 square miles) (2011) in the eastern Bernese Alps in the Swiss canton of Valais. The Aletsch Glacier is composed of four smaller glaciers converging at Konkordiaplatz, where its thickness was measured by the ETH to be still near 1 km (3,300 ft). It then continues towards the Rhône valley before giving birth to the Massa. The Aletsch Glacier is – like most glaciers in the world today – a retreating glacier. As of 2016, since 1980 it lost 1.3 kilometres (0.81 mi) of its length, since 1870 3.2 kilometres (2.0 mi), and lost also more than 300 metres (980 ft) of its thickness.

 

The whole area, including other glaciers is part of the Jungfrau-Aletsch Protected Area, which was declared a UNESCO World Heritage Site in 2001.

 

Geography

 

The Aletsch Glacier is one of the many glaciers located between the cantons of Bern and Valais on the Bernese Alps located east of the Gemmi Pass. The whole area is considered to be the largest glaciated area in western Eurasia. The Fiescher and Aar Glaciers lying on the east have similar extensions.

 

Except the Finsteraarhorn, all the highest summits of the Bernese Alps are located within the drainage basin of the glacier. The Jungfrau and Mönch constitute the northern boundary; the Gross Fiescherhorn and Gross Wannenhorn lie on its east side; finally the culminating point, the Aletschhorn (4,193 m (13,757 ft)) is located on the west side.

 

Before reaching the maximum flow, four smaller glaciers converge at Konkordiaplatz:

 

From the western mouth flows the Grosser Aletschfirn, which runs along the northern foot of the Aletschhorn and Dreieckhorn. The Grosser Aletschfirn is supplied from the north by three notable firns: the Äbeni Flue-Firn, the Gletscherhornfirn, and the Kranzbergfirn. All of these firns have their starting points at around 3,800 m (12,500 ft). From the Äbeni Flue-Firn to the Konkordiaplatz, the Grosser Aletschfirn is 9 km (5.6 mi) long and is on average about 1.5 km (0.93 mi) wide. On the west, the Grosser Aletschfirn connects with the Langgletscher over the 3,158 m (10,361 ft) high glacier pass, the Lötschenlücke, into the Lötschental.

 

From the northwestern mouth flows the Jungfraufirn. This firn in fact represents the straight continuation of the Aletsch Glacier, yet is the shortest of the four tributary glaciers. It has its origin on the southern flank of the Mönch and at the eastern flank of the Jungfrau with the Jungfraujoch in-between. Up to the Konkordiaplatz, the Jungfraufirn is a scarce 7 km (4.3 mi) long, and returns to flank the Kranzberg in the west and the Trugberg in the east. At its highest point, it is 2 km (1.2 mi) wide, and further down it is still a good 1 km (0.62 mi) wide.

From the northern mouth flows the Ewigschneefäld ("Eternal snow field"), where its starting point takes the east flank of the Mönch. In an elbow, it flanks from Trugberg in the west and the Gross Fiescherhorn and Grünhorn in the east, flowing on to the Konkordiaplatz. Up to here, it is about 8 km (5.0 mi) long and averages about 1.2 km (0.75 mi) wide.

 

The mouth at the Konkordiaplatz it follows over a rise with a descent from 25 to 30 percent; here, the glacier is sharply split. Against the north is the Ewigschneefäld over the snow-covered pass of the Unners Mönchsjoch (3,518 m (11,542 ft)), connected with the catchment area of the Ischmeer (Wallis German for "Ice Sea"). Through the Obere Mönchsjoch (3,624 m (11,890 ft)) between the Mönch and the Trugberg stands a connection to the Jungfraufirn.

 

From the east, the smallest firn arrives at the Konkordiaplatz: the Grüneggfirn. Its northern arm begins below the Grünegghorn (3,860 m (12,660 ft)). The southern arm collects its snow and ice in the pot flanked by the Wyssnollen, Fiescher Gabelhorn (3,866 m (12,684 ft)), and the Chamm. Between the peaks Wyssnollen and Grünhörnli another glacier pass, the Grünhornlücke (3,279 m (10,758 ft)), connects to the Fieschergletscher. The Grüneggfirn enters the Konkordiaplatz in a gap between the mountainsides Grünegg to the north and the Fülberg to the south. On the western side of the Fülberg the Konkordia hut (mountain hut) overlooks the whole Konkordiaplatz at an altitude of 2,850 m (9,350 ft).

 

South of Konkordiaplatz, the glacier runs towards the valley of the Oberwallis (Upper Valais); on the east side, near Bettmeralp, lies a small glacier lake, Märjelensee (2,301 m (7,549 feet)); from the western side used to enter the Mittelaletschgletscher, but since the end of the 20th century the connection with the Aletsch Glacier has been lost. Further down, until about 1880, the Oberaletschgletscher did also enter the Aletsch Glacier at its mouth. But since then both glaciers have been retreating so far that they do not connect anymore (the Upper Aletsch Glacier did retreat about 1.3 km (0.81 mi) from its connecting point with the Aletsch Glacier), but both serve now only as the source of the river Massa. The river flows through the Lake Gibidum (a reservoir, and coincidentally representing the glacier's mouth region in the 19th century, which is a retreat of more than 4 km (2.5 mi)) and a gorge of the same name before reaching the Rhône near Brig.

 

Tourism

 

The area of the Aletsch Glacier and some surrounding valleys is on the UNESCO World Heritage list, thus it is protected and the facilities are mostly restricted to the external zones. The region between Belalp, Riederalp and Bettmeralp (which is called Aletsch Region) in Valais gives access to the lower part of the glacier. The Bettmerhorn and Eggishorn are popular view points and are accessible by cable car. The Massa river can be crossed since 2008 by a suspension bridge, thus allowing hikes between the left and the right part of the glacier.

 

The Jungfraujoch railway station (3,450 m) gives a direct access to the upper Aletsch Glacier as well as the normal route to the Jungfrau. It can be reached only from Interlaken in the canton Bern. Hiking paths pass the Konkordia Hut or the Hollandia Hut, eventually reaching other glaciers in the massif.

 

On the Riederfurka, at 2,065 metres between Riederalp and the glacier, is located the historic Villa Cassel, former summer residence of many famous and influential guests from the worlds of politics and finance. The house is now one of the centers of the environmental organization Pro Natura, which hosts a permanent exhibition about the site.

 

Panorama

 

Also at the mouth of the Konkordiaplatz from the east is the small but important Grüneggfirn (3 km long and averaging 600 m wide). This firn is connected in the over the glacier pass Grünhornlücke (3280 m high) to the Fiescher Glacier in the east.

 

From the Konkordiaplatz, the Aletsch Glacier has a width of approximately 1.5 km and moves at a rate of 180 m per year to the southeast on course with the Rhône valley, bordering the Dreieckhorn in the west and the great Wannenhorn in the east. It then takes a great right turn and bends ever closer to the southwest, running through the edge of the Eggishorn and Bettmerhorn of the Rhône valley. The lowest part of the great Aletsch Glacier is largely covered with detritus of the lateral and medial moraines. The glacier's toe currently lies about 1560 m high, far beneath the local tree line. From it springs the Massa stream, which flows through the Massa Canyon and is used to generate hydroelectric power. It continues through the upper half of the Brig, eventually entering into the Rhône.

 

The great Aletsch Glacier shows considerable ice cover. At the Konkordiaplatz, it has an ice cover of more than 900 m, but as it moves to the south, the greater part of the ice melts, gradually decreasing the cover to around 150 m.

 

The characteristically dark medial moraine, situated almost in the middle of the glacier, runs protracted in two bands from the Konkordiaplatz along the whole length to the glacier's toe-zone. This medial moraine is collected from the ice of three large ice fields, which all run together. The westernmost medial moraine has been named the Kranzbergmoräne, and the easternmost carries the name Trugbergmoräne.

 

Formation and evolution

 

The Aletsch Glacier resulted from the accumulation and compaction of snow. Glaciers generally form where snow and ice accumulation exceed snow and ice melt. As the snow and ice thicken it reaches a point where it begins to move due to a combination of gravity and pressure of the overlying snow and ice.

 

During the last glacial periods, the Aletsch Glacier was much larger than now. 18,000 years ago the lower part of the ridge, between Riederalp and the glacier, was completely covered by ice. Only the summits of the Bettmerhorn, Eggishorn and the Fusshörner were above the glacier. After an important retreat, the glacier again advanced 11,000 years ago during the last glacial period. The glacier reached the Rhône valley, and its ice the Riederfurka. Remaining moraines are still visible in the Aletsch Forest.

 

Since the last glaciation, the glacier generally retreated. However slight climatic changes happened and, in 1860, the glacier was 3 km longer and the ice level 200 m higher.

 

As for many other glaciers, records show a major longer-term retreat trend. The Aletsch Glacier receded by 3.2 km (2.0 mi) since 1870, including 1.3 km (0.81 mi) since 1980.[6] A record retreat of 114.6 metres (376 ft) happened in 2006 alone.

 

Since the end of the Little Ice Age in 1850 the glacier has lost 20 percent of its ice mass, considerably less than other glaciers in Switzerland, which have lost up to 50 percent. This is explained with the large size of the Aletsch Glacier, which reacts much slower to climate change than smaller glaciers. It is however estimated that, by 2100, the glacier will have only one tenth of its 2018 ice mass.

 

Photo opportunity

 

On August 18, 2007, photographer Spencer Tunick used hundreds of naked people in a "living sculpture" on the Aletsch Glacier in a photo shoot which he said was intended to draw attention to global warming and the shrinking of the world's glaciers. The temperature was about 10 °C (50 °F) at the time of the photo shoot. The 600 participants on the shrinking glacier said that they had volunteered for Tunick (a collaboration with Greenpeace) to let the world know about the effects of global warming on the melting Swiss glaciers.

 

(Wikipedia)

 

Der Grosse Aletschgletscher ist der flächenmässig grösste und längste Gletscher der Alpen. Er befindet sich auf der Südabdachung der Berner Alpen im Schweizer Kanton Wallis. Die Länge des Gletschers beträgt 22,6 km, die Fläche wird mit 78,49 km² angegeben. Der Aletschgletscher entwässert über die Massa in die Rhone. Die Fläche des gesamten Einzugsgebiets der Massa beträgt 195 km², wovon 1973 etwa zwei Drittel vergletschert waren. Oft werden bei der Flächenangabe der Ober- und Mittelaletschgletscher einbezogen, da diese früher mit dem Grossen Aletschgletscher verbunden waren. Die gesamte vergletscherte Fläche einschliesslich dieser Gletscher betrug 1973 etwa 128 km², für das Jahr 1863 wird eine Fläche von 163 km² angenommen.

 

Ursprung am Konkordiaplatz

 

Der Ursprung des Grossen Aletschgletschers liegt in der rund 3800 m hoch gelegenen Jungfrau-Region. Am Konkordiaplatz (♁645905 / 150101), einer 6 km² grossen und nur wenig geneigten Eisfläche, fliessen drei mächtige Firnströme zusammen:

 

Von Westen mündet der Grosse Aletschfirn, der entlang dem Nordfuss von Aletschhorn und Dreieckhorn fliesst. Der Grosse Aletschfirn wird von Norden her durch drei weitere bedeutende Firne gespeist, nämlich durch den Ebnefluhfirn, den Gletscherhornfirn und den Kranzbergfirn. Alle diese Firne nehmen ihren Ausgangspunkt auf rund 3800 m ü. M. Einschliesslich des Ebnefluhfirns hat der Grosse Aletschfirn bis zum Konkordiaplatz eine Länge von 9 km und ist durchschnittlich fast 1,5 km breit. Gegen Westen ist der Grosse Aletschfirn über den 3173 m ü. M. hohen Gletscherpass der Lötschenlücke mit dem Langgletscher verbunden, der ins Lötschental abfliesst.

 

Von Nordwesten mündet der Jungfraufirn, der zwar die gerade Fortsetzung des Aletschgletschers darstellt, jedoch der kürzeste der drei Tributärgletscher ist. Er hat seinen Ursprung an der Südflanke des Mönchs, am Jungfraujoch und an der Ostflanke der Jungfrau. Bis zum Konkordiaplatz legt der Jungfraufirn eine Wegstrecke von knapp 7 km zurück und wird dabei im Westen vom Kranzberg, im Osten vom Trugberg flankiert. Er ist in seinem oberen Teil 2 km, weiter unten noch gut 1 km breit.

 

Von Norden mündet das Ewigschneefeld, das seinen Ausgangspunkt an der Ostflanke des Mönchs nimmt und in einem Bogen, flankiert vom Trugberg im Westen sowie dem Gross Fiescherhorn und dem Grünhorn im Osten, zum Konkordiaplatz fliesst. Bis hierher ist es ungefähr 8 km lang und durchschnittlich 1,2 km breit. Die Mündung in den Konkordiaplatz erfolgt über einen Steilhang mit einem Gefälle von 25 bis 30 %; der Gletscher ist hier stark zerklüftet. Gegen Norden ist das Ewigschneefeld über den firnbedeckten Pass des Unteren Mönchsjochs (3529 m ü. M.) mit dem Einzugsgebiet des Unteren Grindelwaldgletschers verbunden. Durch das Obere Mönchsjoch (3627 m ü. M.) zwischen dem Mönch und dem Trugberg besteht eine Verbindung zum Jungfraufirn. Ferner mündet am Konkordiaplatz von Osten noch der wesentlich kleinere Grüneggfirn (3 km lang und durchschnittlich 600 m breit). Dieser ist nach Osten über den Gletscherpass der Grünhornlücke (3280 m ü. M.) mit dem Fieschergletscher verbunden.

 

Weiterer Verlauf

 

Vom Konkordiaplatz aus bewegt sich der Eisstrom mit einer Breite von ungefähr 1,5 km und mit einer Geschwindigkeit von bis zu 180 Metern pro Jahr nach Südosten in Richtung Rhonetal, gesäumt vom Dreieckhorn im Westen und dem Gross Wannenhorn im Osten. Er zeichnet dann eine grosse Rechtskurve und biegt immer mehr nach Südwesten ab, nun durch den Grat des Eggishorns und Bettmerhorns vom Rhonetal getrennt. Der unterste Teil des Grossen Aletschgletschers ist weitgehend durch das Geschiebematerial von Seiten- und Mittelmoränen bedeckt. Die Gletscherzunge liegt derzeit auf rund 1'560 Meter Höhe, weit unterhalb der lokalen Waldgrenze. Aus ihr entspringt der Bach Massa, welcher nach der Massaschlucht und einer Nutzung in einem Wasserkraftwerk, in Bitsch, oberhalb von Naters, in die Rhone (Rotten) fliesst.

 

Der Grosse Aletschgletscher weist beachtliche Eisdicken auf. Am Konkordiaplatz hat der Gletscher eine Eisdicke von mehr als 900 Metern, gegen Süden nimmt die Mächtigkeit des Eises allmählich auf rund 150 m ab. Charakteristisch sind die beiden dunklen, fast in der Mitte des Aletschgletschers gelegenen Moränenspuren, welche sich ab dem Konkordiaplatz auf der gesamten Länge bis in den Zungenbereich hinziehen. Es sind die Mittelmoränen, die das Eis der drei Hauptfirne voneinander trennen. Die westliche Mittelmoräne wird auch Kranzbergmoräne genannt, die östliche trägt den Namen Trugbergmoräne.

 

Gletscherschwankungen

 

In seinem Hochstadium während der Kleinen Eiszeit um die Mitte des 19. Jahrhunderts erstreckte sich der Grosse Aletschgletscher noch rund 2,5 km weiter talabwärts. Aufgrund der allgemeinen Erwärmung seit etwa 1870 hat er besonders unterhalb des Konkordiaplatzes massiv an Volumen eingebüsst und sowohl an den Seiten als auch im Zungenbereich Flächen von mehreren Quadratkilometern freigegeben. Der einstmalige, in der Neuzeit höchste Gletscherstand kann gut an den noch fast vegetationslosen Seitenmoränen abgeschätzt werden. Seit 1850 hat die Eisdicke um teilweise über 100 m abgenommen. Früher waren auch die Eisströme des Oberaletschgletschers und des Mittelaletschgletschers direkt mit dem Grossen Aletschgletscher verbunden.

 

In der Senke zwischen dem Strahlhorn und dem Eggishorn liegt der Märjelensee, der im 19. Jahrhundert beim Gletscherhochstand zu einem Gletscherrandsee aufgestaut wurde. Seine wiederholten plötzlichen Ausbrüche durch Gletscherspalten verursachten immer wieder starke Schadenshochwasser der Massa hin zum Rhonetal.

 

Gegen kurzfristige Klimaschwankungen ist der Gletscher aufgrund seiner grossen Masse relativ immun. Während viele andere Gletscher Ende der 1970er Jahre bis Anfang der 1980er Jahre vorstiessen, reagierte der Aletschgletscher auf die vorübergehende Abkühlung kaum – ebenso wenig wie auf die warmen Jahre seit 1983. Aufgrund der zunehmend extremen Hitze der letzten Jahre zieht er sich aber nun doch – wie alle übrigen Alpengletscher – deutlich verstärkt zurück.

 

Die relative Trägheit in seinen Reaktionen auf Klimaschwankungen macht den Aletschgletscher auch zu einem idealen Untersuchungsobjekt zur Erforschung der Klimaentwicklung im Alpenraum. Die Längenschwankungen des Aletschgletschers in der Vergangenheit dürften sogar eine Rekonstruktion aller grösseren Klimaveränderungen der letzten 3200 Jahre erlauben. Die Bestimmung der verschiedenen Längenstadien des Aletschgletschers in der Vergangenheit erfolgt durch die Radiokohlenstoffdatierung fossiler Baumstämme, die der Gletscher bei einem früheren Vorstoss einmal überfahren haben muss und nun während seines aktuellen Rückzuges wieder freigibt. Der Befund fossiler Böden und von Wurzelwerk garantiert dabei, dass es sich bei dem Fundort auch um den Wuchsstandort des fossilen Baumes handelt. Durch Zählung der Jahresringe der geborgenen Stämme kann sogar der Zeitraum bestimmt werden, während dessen der Aletschgletscher den Fundort nicht erreicht hat. Mit dieser Methode wurde festgestellt, dass der Aletschgletscher bis etwa 1200 v. Chr. um einiges kleiner gewesen sein muss als gegen Ende des 20. Jahrhunderts. Für die Jahre etwa von 1200 bis 1110 v. Chr., 850 bis 750 v. Chr. und 350 bis 250 v. Chr. sind Vorstösse festgestellt worden. Dabei ist der Aletschgletscher von 900 bis 400 v. Chr. jedoch kleiner gewesen als am Ende des 20. Jahrhunderts, genauso wie von etwa 100 v. Chr. bis ins Jahr 250. Um das Jahr 300 ist eine Gletscherlänge vergleichbar der des Höchststandes im 19. Jahrhundert festzustellen.

 

Laut der letzten Studie der Universität Erlangen-Nürnberg (Juni 2020) schmolz die Oberfläche des Grossen Aletschgletscher zwischen den Jahren 2001 und 2014 um mehr als fünf Meter pro Jahr in den unteren Lagen.

 

Tourismus

 

Der Aletschgletscher galt schon früh als besondere Sehenswürdigkeit für Reisende und als willkommenes Untersuchungsobjekt für Forschende. Forschungsstationen gibt es seit 1937 auf dem Jungfraujoch und seit 1976 auf der Riederfurka oberhalb der Riederalp. Durch zahlreiche Luftseilbahnen besonders gut erschlossen ist der Berggrat zwischen dem Riederhorn und dem Eggishorn, der sehr schöne Einblicke in den Zungenbereich und den unteren Teil des Gletschers gewährt. Mit dem Bau der Jungfraubahn auf das Jungfraujoch (auf der Sphinx 3571 m ü. M.) wurde 1912 auch für nicht berggewohnte Leute ein Blick in den oberen Teil des Gletschers ermöglicht.

 

Am Felshang des Faulbergs östlich des Konkordiaplatzes stehen auf 2850 m ü. M. die Konkordiahütten des Schweizer Alpen-Clubs SAC. Sie dienen als wichtiger Etappenort auf der hochalpinen Gletscherroute vom Jungfraujoch oder vom Lötschental in das Gebiet des Grimselpasses.

 

UNESCO-Weltnaturerbe

 

Das Gebiet des Grossen Aletschgletschers ist zusammen mit dem einzigartigen Aletschwald und den umliegenden Regionen seit dem 13. Dezember 2001 Bestandteil des UNESCO-Weltnaturerbes Schweizer Alpen Jungfrau-Aletsch.

 

(Wikipedia)

Lost Creek Campground is a fully accessible campground allowing anyone access to campsites, fishing and a paved nature trail that meanders through the area. The campground is also near the Wild and Scenic Sandy River and not far from the popular Ramona Falls Trailhead. Mt. Hood is just southeast of the campground and is close enough for visitors to enjoy a day trip and sightseeing. (www.recreation.gov/camping/lost-creek/r/campgroundDetails...)

Paved, accessible trail in the Lava Lands Trail of Molten Lands in Newberry Volcano National Monument

Vieux Port | Quai des Belges 20/07/2013 09h53

Together with the new refurnished and paved square in front of the Vieux Port Marseille is together with the region Provence the Cultural European Capital of 2013.

On 23/04/2013 the huge inverted mirror has been inaugurated; l'Ombrière. Designer is Norman Foster . In total 158 mirrors are placed and the shade house has a surface of 1080 square meters. In fact it is a mirrored sunshade and events pavilion in the Vieux Port. A polished steel canopy reflects visitors walking underneath, nothing more nothing less.

Supported by eight slender columns, the stainless-steel structure stretches over the paving to create a sheltered events space in the city's Old Port. The roof features sharply tapered edges, creating the impression of a paper-like thickness.

"The new pavilion is quite literally a reflection of its surroundings," explained head of design Spencer de Grey. "Its lightweight steel structure is a minimal intervention and appears as a simple silver line on the horizon."

The Vieux Port pavilion forms part of a masterplan of public realm projects that Foster + Partners has been working on along the seafront of the French city to tie in with its role as European Capital of Culture 2013. Other improvements includes new surfaces, wider pavements and a series of nautical pavilions.

"Our aim has been to make the Vieux Port accessible to all," said De Grey. "The project is an invitation to the people of Marseille to enjoy and use this grand space for events, markets and celebrations once again."

[ On the many sources: www.dezeen.com/2013/03/06/vieux-port-pavilion-by-foster-p... ]

Children with additional support needs will have improved access to nursery education thanks to £2 million announced by First Minister Nicola Sturgeon today.

 

The money will fund specialist training and equipment to ensure all nurseries offering the free early learning and childcare (ELC) entitlement are equipped to care for children with additional support needs

 

The First Minister and Mark McDonald, Minister for Childcare and Early Years announced the funding while visiting Smile Childcare Early Years Centre in Wester Hailes, Edinburgh.

The only fully low floor bus in Sydney, prototype Scania N310UA Volgren CR228L 2112 sits at Sydenham between 430s.

 

2112 was a trial bus for the STA, testing fully low floor layouts. 2112s engine is mounted vertically at the rear of the bus allowing for step and ramp free access down the length of the bus.

Emerald Lake is located in Yoho National Park, British Columbia, Canada.It is the largest of Yoho's 61 lakes and ponds, as well as one of the park's premier tourist attractions. Emerald Lake Lodge, a high-end lodge perched on the edge of the lake, provides local accommodation. A 5.2 km (3.2 mi) hiking trail circuits the lake, the first half of which is accessible to wheelchairs and strollers. During the summer months, canoe rentals are available; in the winter, the lake is a popular cross country skiing destination. .

【★ Reference By Wikipedia】

@ Yahoo!

 

accessibility.yahoo.com/

Copyright - All Rights Reserved - Black Diamond Images

 

Wallis Island European chateau-style mansion, Chateau Le Marais, is accessible only by boat or a helicopter. The 104 hectare property boasts a 990 square metre five-bedroom, six-bathroom house that overlooks Wallis Lake, and includes 1.5 kilometres of lake frontage, an orchard, lagoons, fishing wetlands and its own botanical gardens.

Woollahra, Sydney, antique dealer Andre Fink and his wife Cecile bought the Wallis Island property in 1996 for around $290,000. They proceeded to commission a luxurious mansion worthy of holding their unique 18th-century antique collection.

Chateau Le Marais was built by master stonemasons in a grand French chateau style with its decor and skilled labour sourced from around the world. Featuring several French fireplaces, Sphinx-like sculptures guarding the entrance, chandeliers, oak parquetry floors and ornate carvings on the gable completed the buildings impressive façade.

 

appear to have offered the mansion for sale without furniture.

 

Chateau Le Marais had been the Fink's labour of love for 15 years, the building taking some "inspiration from Le Chateau du Marias, the late 18th-century French castle that replaced the Huraults’ castle, of which nothing remains but the moats and the dungeon on the Marais. Henri Hurault was count of Cheverny and the military treasurer of King Louis XI." Reference

 

With his Woollahra Antique business going through hard times due to the GFC in 2011, the Finks tried to sell the property. Although incomplete, Chateau Le Marais was reported to have been initially marketed for $20 million then $18 million, and then $16 million.

 

When the property failed to sell it was withdrawn from the market in 2013 and the Finks ultimately defaulted on their loans to the ANZ bank. Subsequently the bank assumed control of the property in 2014. In early 2015, a court ruled that an amount of $3.4 million of the loans were valid and binding, rejecting the Fink's assertion that the bank had taken an “unconscientious advantage of its superior bargaining position”.

 

In January 2018, Cubecorp Realty was reportedly marketing the property with a guide of about $10 million.

 

Sydney developer Adam Dai then purchased the property for an undisclosed sum and completed much of the unfinished work on the building for an amount reported to be in the vicinity of several million dollars. Mr Dai had used the property to host family and business guests, but due to a busy work schedule in Sydney, had decided to sell.

In 2019 the asking price at auction was reportedly around $6 million, however, although several buyers were interested, that asking price failed to attract a buyer and in early 2022, as far as I understand, the property remains in the hands of Adam Dai.

 

Reference - www.domain.com.au/news/nothing-similar-the-wallis-island-...

 

I will do a bit of homework and see if I can add some details of ownership prior to the Finks purchasing the property in 1996.

 

Image taken from the Free Spirit Cruise Boat.

 

one more then... I have more pics and have plans for a near future, but those won't be public accessible. Need to find out how to change the settings.

The Eiffel Tower (French: La Tour Eiffel, nickname La dame de fer, the iron lady) is an iron lattice tower located on the Champ de Mars in Paris, named after the engineer Gustave Eiffel, whose company designed and built the tower. Erected in 1889 as the entrance arch to the 1889 World's Fair, it has become both a global cultural icon of France and one of the most recognizable structures in the world. The tower is the tallest structure in Paris and the most-visited paid monument in the world; 7.1 million people ascended it in 2011. The third level observatory's upper platform is at 279.11 m the highest accessible to public in the European Union and the highest in Europe as long as the platform of the Ostankino Tower, at 360 m, remains closed as a result of the fire of August 2000. The tower received its 250 millionth visitor in 2010.

The tower stands 320 metres (1,050 ft) tall, about the same height as an 81-storey building. During its construction, the Eiffel Tower surpassed the Washington Monument to assume the title of the tallest man-made structure in the world, a title it held for 41 years, until the Chrysler Building in New York City was built in 1930. However, because of the addition, in 1957, of the antenna atop the Eiffel Tower, it is now taller than the Chrysler Building. Not including broadcast antennas, it is the second-tallest structure in France, after the Millau Viaduct.

The tower has three levels for visitors. Tickets can be purchased to ascend, by stairs or lift (elevator), to the first and second levels. The walk from ground level to the first level is over 300 steps, as is the walk from the first to the second level. The third and highest level is accessible only by lift - stairs exist but they are not usually open for public use. Both the first and second levels feature restaurants.

The tower has become the most prominent symbol of both Paris and France, often in the establishing shot of films set in the city.

 

History

 

Origin

  

First drawing of the Eiffel Tower by Maurice Koechlin

The design of the Eiffel Tower was originated by Maurice Koechlin and Émile Nouguier, two senior engineers who worked for the Compagnie des Establissments Eiffel after discussion about a suitable centrepiece for the proposed 1889 Exposition Universelle, a World's Fair which would celebrate the centennial of the French Revolution. In May 1884 Koechlin, working at his home, made an outline drawing of their scheme, described by him as "a great pylon, consisting of four lattice girders standing apart at the base and coming together at the top, joined together by metal trusses at regular intervals". Initially Eiffel himself showed little enthusiasm, but he did sanction further study of the project, and the two engineers then asked Stephen Sauvestre, the head of company's architectural department, to contribute to the design. Sauvestre added decorative arches to the base, a glass pavilion to the first level and other embellishments. This enhanced version gained Eiffel's support, and he bought the rights to the patent on the design which Koechlin, Nougier and Sauvestre had taken out, and the design was exhibited at the Exhibition of Decorative Arts in the autumn of 1884 under the company name. On 30 March 1885 Eiffel read a paper on the project to the Société des Ingiénieurs Civils: after discussing the technical problems and emphasising the practical uses of the tower, he finished his talk by saying that the tower would symbolise "not only the art of the modern engineer, but also the century of Industry and Science in which we are living, and for which the way was prepared by the great scientific movement of the eighteenth century and by the Revolution of 1789, to which this monument will be built as an expression of France's gratitude."

Little happened until the beginning of 1886, when Jules Grévy was re-elected as President and Édouard Lockroy was appointed as Minister for Trade. A budget for the Exposition was passed and on 1 May Lockroy announced an alteration to the terms of the open competition which was being held for a centerpiece for the exposition, which effectively made the choice of Eiffel's design a foregone conclusion: all entries had to include a study for a 300 m (980 ft) four-sided metal tower on the Champ de Mars. On 12 May a commission was set up to examine Eiffel's scheme and its rivals and on 12 June it presented its decision, which was that all the proposals except Eiffel's were either impractical or insufficiently worked out. After some debate about the exact site for the tower, a contract was finally signed on 8 January 1887. This was signed by Eiffel acting in his own capacity rather than as the representative of his company, and granted him one and a half million francs toward the construction costs: less than a quarter of the estimated cost of six and a half million francs. Eiffel was to receive all income from the commercial exploitation of the tower during the exhibition and for the following twenty years. Eiffel later established a separate company to manage the tower, putting up half the necessary capital himself.

 

The "Artists Protest"

 

Caricature of Gustave Eiffel comparing the Eiffel tower to the Pyramids.

The projected tower had been a subject of some controversy, attracting criticism both from those who did not believe that it was feasible and also from those who objected on artistic grounds. Their objections were an expression of a longstanding debate about relationship between architecture and engineering. This came to a head as work began at the Champ de Mars: A "Committee of Three Hundred" (one member for each metre of the tower's height) was formed, led by the prominent architect Charles Garnier and including some of the most important figures of the French arts establishment, including Adolphe Bouguereau, Guy de Maupassant, Charles Gounod and Jules Massenet: a petition was sent to Charles Alphand, the Minister of Works and Commissioner for the Exposition, and was published by Le Temps.

"We, writers, painters, sculptors, architects and passionate devotees of the hitherto untouched beauty of Paris, protest with all our strength, with all our indignation in the name of slighted French taste, against the erection…of this useless and monstrous Eiffel Tower … To bring our arguments home, imagine for a moment a giddy, ridiculous tower dominating Paris like a gigantic black smokestack, crushing under its barbaric bulk Notre Dame, the Tour Saint-Jacques, the Louvre, the Dome of les Invalides, the Arc de Triomphe, all of our humiliated monuments will disappear in this ghastly dream. And for twenty years … we shall see stretching like a blot of ink the hateful shadow of the hateful column of bolted sheet metal"

Gustave Eiffel responded to these criticisms by comparing his tower to the Egyptian Pyramids : "My tower will be the tallest edifice ever erected by man. Will it not also be grandiose in its way ? And why would something admirable in Egypt become hideous and ridiculous in Paris ?" These criticisms were also masterfully dealt with by Édouard Lockroy in a letter of support written to Alphand, ironically saying "Judging by the stately swell of the rhythms, the beauty of the metaphors, the elegance of its delicate and precise style, one can tell that …this protest is the result of collaboration of the most famous writers and poets of our time", and going on to point out that the protest was irrelevant since the project had been decided upon months before and was already under construction. Indeed, Garnier had been a member of the Tower Commission that had assessed the various proposals, and had raised no objection. Eiffel was similarly unworried, pointing out to a journalist that it was premature to judge the effect of the tower solely on the basis of the drawings, that the Champ de Mars was distant enough from the monuments mentioned in the protest for there to be little risk of the tower overwhelming them, and putting the aesthetic argument for the Tower: "Do not the laws of natural forces always conform to the secret laws of harmony?"

Some of the protestors were to change their minds when the tower was built: others remained unconvinced. Guy de Maupassant[20] supposedly ate lunch in the Tower's restaurant every day. When asked why, he answered that it was the one place in Paris where one could not see the structure. Today, the Tower is widely considered to be a striking piece of structural art.

  

Construction

 

Foundations of the Eiffel Tower

  

Eiffel Tower under construction between 1887 and 1889

Work on the foundations started in January 1887. Those for the east and south legs were straightforward, each leg resting on four 2 m (6.6 ft) concrete slabs, one for each of the principal girders of each leg but the other two, being closer to the river Seine were more complicated: each slab needed two piles installed by using compressed-air caissons 15 m (49 ft) long and 6 m (20 ft) in diameter driven to a depth of 22 m (72 ft)[21] to support the concrete slabs, which were 6 m (20 ft) thick. Each of these slabs supported a block built of limestone each with an inclined top to bear a supporting shoe for the ironwork. Each shoe was anchored into the stonework by a pair of bolts 10 cm (4 in) in diameter and 7.5 m (25 ft) long. The foundations were complete by 30 June and the erection of the ironwork began. The very visible work on-site was complemented by the enormous amount of exacting preparatory work that was entailed: the drawing office produced 1,700 general drawings and 3,629 detailed drawings of the 18,038 different parts needed:

The task of drawing the components was complicated by the complex angles involved in the design and the degree of precision required: the position of rivet holes was specified to within 0.1 mm (0.04 in) and angles worked out to one second of arc. The finished components, some already riveted together into sub-assemblies, arrived on horse-drawn carts from the factory in the nearby Parisian suburb of Levallois-Perret and were first bolted together, the bolts being replaced by rivets as construction progressed. No drilling or shaping was done on site: if any part did not fit it was sent back to the factory for alteration. In all there were 18,038 pieces of puddle iron using two and a half million rivets.

At first the legs were constructed as cantilevers but about halfway to the first level construction was paused in order to construct a substantial timber scaffold. This caused a renewal of the concerns about the structural soundness of the project, and sensational headlines such as "Eiffel Suicide!" and "Gustave Eiffel has gone mad: he has been confined in an Asylum" appeared in the popular press. At this stage a small "creeper" crane was installed in each leg, designed to move up the tower as construction progressed and making use of the guides for the lifts which were to be fitted in each leg. The critical stage of joining the four legs at the first level was complete by March 1888. Although the metalwork had been prepared with the utmost precision, provision had been made to carry out small adjustments in order to precisely align the legs: hydraulic jacks were fitted to the shoes at the base of each leg, each capable of exerting a force of 800 tonnes, and in addition the legs had been intentionally constructed at a slightly steeper angle than necessary, being supported by sandboxes on the scaffold.

No more than three hundred workers were employed on site, and because Eiffel took safety precautions, including the use of movable stagings, guard-rails and screens, only one man died during construction.

  

Inauguration and the 1889 Exposition

 

The 1889 Exposition Universelle for which the Eiffel Tower was built

The main structural work was completed at the end of March 1889 and on the 31st Eiffel celebrated this by leading a group of government officials, accompanied by representatives of the press, to the top of the tower. Since the lifts were not yet in operation, the ascent was made by foot, and took over an hour, Eiffel frequently stopping to make explanations of various features. Most of the party chose to stop at the lower levels, but a few, including Nouguier, Compagnon, the President of the City Council and reporters from Le Figaro and Le Monde Illustré completed the climb. At 2.35 Eiffel hoisted a large tricolore, to the accompaniment of a 25-gun salute fired from the lower level. There was still work to be done, particularly on the lifts and the fitting out of the facilities for visitors, and the tower was not opened to the public until nine days after the opening of the Exposition on 6 May, and even then the lifts had not been completed.

The tower was an immediate success with the public, and lengthy queues formed to make the ascent. Tickets cost 2 francs for the first level, 3 for the second and 5 for the top, with half-price admission on Sundays, and by the end of the exhibition there had been nearly two million visitors.

Eiffel had a permit for the tower to stand for 20 years; it was to be dismantled in 1909, when its ownership would revert to the City of Paris. The City had planned to tear it down (part of the original contest rules for designing a tower was that it could be easily demolished) but as the tower proved valuable for communication purposes, it was allowed to remain after the expiry of the permit. In the opening weeks of the First World War the powerful radio transmitters using the tower were used to jam German communications, seriously hindering their advance on Paris and contributing to the Allied victory at the First Battle of the Marne.

 

Subsequent events

 

10 September 1889 Thomas Edison visited the tower. He signed the guestbook with the following message— To M Eiffel the Engineer the brave builder of so gigantic and original specimen of modern Engineering from one who has the greatest respect and admiration for all Engineers including the Great Engineer the Bon Dieu, Thomas Edison.

 

19 October 1901 Alberto Santos-Dumont in his Dirigible No.6 won a 10,000-franc prize offered by Henri Deutsch de la Meurthe for the first person to make a flight from St Cloud to the Eiffel tower and back in less than half an hour.

 

1910 Father Theodor Wulf measured radiant energy at the top and bottom of the tower. He found more at the top than expected, incidentally discovering what are today known as cosmic rays.[28]

 

4 February 1912 Austrian tailor Franz Reichelt died after jumping 60 metres from the first deck of Eiffel tower with his home-made parachute.

 

1914 A radio transmitter located in the tower jammed German radio communications during the lead-up to the First Battle of the Marne.

 

1925 The con artist Victor Lustig "sold" the tower for scrap metal on two separate, but related occasions.

 

1930 The tower lost the title of the world's tallest structure when the Chrysler Building was completed in New York City.

 

1925 to 1934 Illuminated signs for Citroën adorned three of the tower's four sides, making it the tallest advertising space in the world at the time.

 

1940–1944 Upon the German occupation of Paris in 1940, the lift cables were cut by the French so that Adolf Hitler would have to climb the steps to the summit. The parts to repair them were allegedly impossible to obtain because of the war. In 1940 German soldiers had to climb to the top to hoist the swastika[citation needed], but the flag was so large it blew away just a few hours later, and was replaced by a smaller one. When visiting Paris, Hitler chose to stay on the ground. It was said that Hitler conquered France, but did not conquer the Eiffel Tower. A Frenchman scaled the tower during the German occupation to hang the French flag. In August 1944, when the Allies were nearing Paris, Hitler ordered General Dietrich von Choltitz, the military governor of Paris, to demolish the tower along with the rest of the city. Von Choltitz disobeyed the order. Some say Hitler was later persuaded to keep the tower intact so it could later be used for communications. The lifts of the Tower were working normally within hours of the Liberation of Paris.

 

3 January 1956 A fire damaged the top of the tower.

 

1957 The present radio antenna was added to the top.

 

1980s A restaurant and its supporting iron scaffolding midway up the tower was dismantled; it was purchased and reconstructed on St. Charles Avenue and Josephine Street in the Garden District of New Orleans, Louisiana, by entrepreneurs John Onorio and Daniel Bonnot, originally as the Tour Eiffel Restaurant, later as the Red Room and now as the Cricket Club (owned by the New Orleans Culinary Institute). The restaurant was re-assembled from 11,000 pieces that crossed the Atlantic in a 40-foot (12 m) cargo container.

 

31 March 1984 Robert Moriarty flew a Beechcraft Bonanza through the arches of the tower.

 

1987 A.J. Hackett made one of his first bungee jumps from the top of the Eiffel Tower, using a special cord he had helped develop. Hackett was arrested by the Paris police upon reaching the ground.

 

27 October 1991 Thierry Devaux, along with mountain guide Hervé Calvayrac, performed a series of acrobatic figures of bungee jumping (not allowed) from the second floor of the Tower. Facing the Champ de Mars, Thierry Devaux was using an electric winch between each figure to go back up. When firemen arrived, he stopped after the sixth bungee jump.

 

New Year's Eve 1999 The Eiffel Tower played host to Paris's Millennium Celebration. On this occasion, flashing lights and four high-power searchlights were installed on the tower, and fireworks were set off all over it. An exhibition above a cafeteria on the first floor commemorates this event. Since then, the light show has become a nightly event. The searchlights on top of the tower make it a beacon in Paris's night sky, and the 20,000 flash bulbs give the tower a sparkly appearance every hour on the hour.

 

28 November 2002 The tower received its 200,000,000th guest.

 

2004 The Eiffel Tower began hosting an ice skating rink on the first floor each winter.

 

Design of the tower

 

Material

  

The Eiffel Tower from below

 

The puddle iron structure of the Eiffel Tower weighs 7,300 tonnes, while the entire structure, including non-metal components, is approximately 10,000 tonnes. As a demonstration of the economy of design, if the 7,300 tonnes of the metal structure were melted down it would fill the 125-metre-square base to a depth of only 6 cm (2.36 in), assuming the density of the metal to be 7.8 tonnes per cubic metre. Depending on the ambient temperature, the top of the tower may shift away from the sun by up to 18 cm (7.1 in) because of thermal expansion of the metal on the side facing the sun.

 

Wind considerations

 

At the time the tower was built many people were shocked by its daring shape. Eiffel was criticised for the design and accused of trying to create something artistic, or inartistic according to the viewer, without regard to engineering. Eiffel and his engineers, however, as experienced bridge builders, understood the importance of wind forces and knew that if they were going to build the tallest structure in the world they had to be certain it would withstand the wind. In an interview reported in the newspaper Le Temps, Eiffel said:

Now to what phenomenon did I give primary concern in designing the Tower? It was wind resistance. Well then! I hold that the curvature of the monument's four outer edges, which is as mathematical calculation dictated it should be […] will give a great impression of strength and beauty, for it will reveal to the eyes of the observer the boldness of the design as a whole.[37]

Researchers have found that Eiffel used empirical and graphical methods accounting for the effects of wind rather than a specific mathematical formula. Careful examination of the tower shows a basically exponential shape; actually two different exponentials, the lower section overdesigned to ensure resistance to wind forces. Several mathematical explanations have been proposed over the years for the success of the design; the most recent is described as a nonlinear integral equation based on counterbalancing the wind pressure on any point on the tower with the tension between the construction elements at that point. As a demonstration of the tower's effectiveness in wind resistance, it sways only 6–7 cm (2–3 in) in the wind.

 

Accommodation

 

When built, the first level contained two restaurants: an "Anglo-American Bar", and a 250 seat theatre. A 2.6 m (8 ft 6 in) promenade ran around the outside.

On the second level, the French newspaper Le Figaro had an office and a printing press, where a special souvenir edition, Le Figaro de la Tour, was produced. There was also a pâtisserie.

On the third level were laboratories for various experiments and a small apartment reserved for Gustave Eiffel to entertain guests. This is now open to the public, complete with period decorations and lifelike models of Gustave and some guests.

 

Engraved names

 

Gustave Eiffel engraved on the tower seventy-two names of French scientists, engineers and other notable people. This engraving was painted over at the beginning of the twentieth century but restored in 1986–1987 by the Société Nouvelle d'exploitation de la Tour Eiffel, a company contracted to operate business related to the Tower.

 

Maintenance

 

Maintenance of the tower includes applying 50 to 60 tonnes of paint every seven years to protect it from rust. The height of the Eiffel Tower varies by 15 cm due to temperature.

 

Aesthetic considerations

 

In order to enhance the impression of height, three separate colours of paint are used on the tower, with the darkest on the bottom and the lightest at the top. On occasion the colour of the paint is changed; the tower is currently painted a shade of bronze. On the first floor there are interactive consoles hosting a poll for the colour to use for a future session of painting.

The only non-structural elements are the four decorative grillwork arches, added in Stephen Sauvestre's sketches, which served to reassure visitors that the structure was safe, and to frame views of other nearby architecture.

One of the great Hollywood movie clichés is that the view from a Parisian window always includes the tower. In reality, since zoning restrictions limit the height of most buildings in Paris to 7 storeys, only a very few of the taller buildings have a clear view of the tower.

 

Popularity

 

More than 200,000,000 people have visited the tower since its construction in 1889, including 6,719,200 in 2006. The tower is the most-visited paid monument in the world.

 

Passenger lifts

 

Ground to the second level

The original lifts (elevators) to the first and second floors were provided by two companies. Both companies had to overcome many technical obstacles as neither company (or indeed any company) had experience with installing lifts climbing to such heights with large loads. The slanting tracks with changing angles further complicated the problems. The East and West lifts were supplied by the French company Roux Combaluzier Lepape, using hydraulically powered chains and rollers. The North and South lifts were provided by the American company Otis using car designs similar to the original installation but using an improved hydraulic and cable scheme. The French lifts had a very poor performance and were replaced with the current installations in 1897 (West Pillar) and 1899 (East Pillar) by Fives-Lille using an improved hydraulic and rope scheme. Both of the original installations operated broadly on the principle of the Fives-Lille lifts.

The Fives-Lille lifts from ground level to the first and second levels are operated by cables and pulleys driven by massive water-powered pistons. The hydraulic scheme was somewhat unusual for the time in that it included three large counterweights of 200 tonnes each sitting on top of hydraulic rams which doubled up as accumulators for the water. As the lifts ascend the inclined arc of the pillars, the angle of ascent changes. The two lift cabs are kept more or less level and indeed are level at the landings. The cab floors do take on a slight angle at times between landings.

The principle behind the lifts is similar to the operation of a block and tackle but in reverse. Two large hydraulic rams (over 1 metre diameter) with a 16 metre travel are mounted horizontally in the base of the pillar which pushes a carriage (the French word for it translates as chariot and this term will be used henceforth to distinguish it from the lift carriage) with 16 large triple sheaves mounted on it. There are 14 similar sheaves mounted statically. Six wire ropes are rove back and forth between the sheaves such that each rope passes between the 2 sets of sheaves 7 times. The ropes then leave the final sheaves on the chariot and pass up through a series of guiding sheaves to above the second floor and then through a pair of triple sheaves back down to the lift carriage again passing guiding sheaves.

This arrangement means that the lift carriage, complete with its cars and passengers, travels 8 times the distance that the rams move the chariot, the 128 metres from the ground to the second floor. The force exerted by the rams also has to be 8 times the total weight of the lift carriage, cars and passengers, plus extra to account for various losses such as friction. The hydraulic fluid was water, normally stored in three accumulators, complete with counterbalance weights. To make the lift ascend, water was pumped using an electrically driven pump from the accumulators to the two rams. Since the counterbalance weights provided much of the pressure required, the pump only had to provide the extra effort. For the descent, it was only necessary to allow the water to flow back to the accumulators using a control valve. The lifts were operated by an operator perched precariously underneath the lift cars. His position (with a dummy operator) can still be seen on the lifts today.

The Fives-Lille lifts were completely upgraded in 1986 to meet modern safety requirements and to make the lifts easier to operate. A new computer-controlled system was installed which completely automated the operation. One of the three counterbalances was taken out of use, and the cars were replaced with a more modern and lighter structure. Most importantly, the main driving force was removed from the original water pump such that the water hydraulic system provided only a counterbalancing function. The main driving force was transferred to a 320 kW electrically driven oil hydraulic pump which drives a pair of hydraulic motors on the chariot itself, thus providing the motive power. The new lift cars complete with their carriage and a full 92 passenger load weigh 22 tonnes.

Owing to elasticity in the ropes and the time taken to get the cars level with the landings, each lift in normal service takes an average of 8 minutes and 50 seconds to do the round trip, spending an average of 1 minute and 15 seconds at each floor. The average journey time between floors is just 1 minute.

The original Otis lifts in the North and South pillars in their turn proved to be inferior to the new (in 1899) French lifts and were scrapped from the South pillar in 1900 and from the North pillar in 1913 after failed attempts to repower them with an electric motor. The North and South pillars were to remain without lifts until 1965 when increasing visitor numbers persuaded the operators to install a relatively standard and modern cable hoisted system in the north pillar using a cable-hauled counterbalance weight, but hoisted by a block and tackle system to reduce its travel to one third of the lift travel. The counterbalance is clearly visible within the structure of the North pillar. This latter lift was upgraded in 1995 with new cars and computer controls.

The South pillar acquired a completely new fairly standard electrically driven lift in 1983 to serve the Jules Verne restaurant. This was also supplied by Otis. A further four-ton service lift was added to the South pillar in 1989 by Otis to relieve the main lifts when moving relatively small loads or even just maintenance personnel.

The East and West hydraulic (water) lift works are on display and, at least in theory, are open to the public in a small museum located in base of the East and West tower, which is somewhat hidden from public view. Because the massive mechanism requires frequent lubrication and attention, public access is often restricted. However, when open, the wait times are much less than the other, more popular, attractions. The rope mechanism of the North tower is visible to visitors as they exit from the lift.

 

Second to the third level

 

The original spiral stairs to the third floor which were only 80 centimetres wide. Note also the small service lift in the background.

The original lifts from the second to the third floor were also of a water-powered hydraulic design supplied by Léon Edoux. Instead of using a separate counterbalance, the two lift cars counterbalanced each other. A pair of 81-metre-long hydraulic rams were mounted on the second level reaching nearly halfway up to the third level. A lift car was mounted on top of the rams. Ropes ran from the top of this car up to a sheave on the third level and back down to a second car. The result of this arrangement was that each car only travelled half the distance between the second and third levels and passengers were required to change lifts halfway walking between the cars along a narrow gangway with a very impressive and relatively unobstructed downward view. The ten-ton cars held 65 passengers each or up to four tons.

One interesting feature of the original installation was that the hoisting rope ran through guides to retain it on windy days to prevent it flapping and becoming damaged. The guides were mechanically moved out of the way of the ascending car by the movement of the car itself. In spite of some antifreeze being added to the water that operated this system, it nevertheless had to close to the public from November to March each year.

The original lifts complete with their hydraulic mechanism were completely scrapped in 1982 after 97 years of service. They were replaced with two pairs of relatively standard rope hoisted cars which were able to operate all the year round. The cars operate in pairs with one providing the counterbalance for the other. Neither car can move unless both sets of doors are closed and both operators have given a start command. The commands from the cars to the hoisting mechanism are by radio obviating the necessity of a control cable. The replacement installation also has the advantage that the ascent can be made without changing cars and has reduced the ascent time from 8 minutes (including change) to 1 minute and 40 seconds. This installation also has guides for the hoisting ropes but they are electrically operated. The guide once it has moved out of the way as the car ascends automatically reverses when the car has passed to prevent the mechanism becoming snagged on the car on the downward journey in the event it has failed to completely clear the car. Unfortunately these lifts do not have the capacity to move as many people as the three public lower lifts and long lines to ascend to the third level are common. Most of the intermediate level structure present on the tower today was installed when the lifts were replaced and allows maintenance workers to take the lift halfway.

The replacement of these lifts allowed the restructuring of the criss-cross beams in upper part of the tower and further allowed the installation of two emergency staircases. These replaced the dangerous winding stairs that were installed when the tower was constructed.

Restaurants

The tower has two restaurants: Le 58 tour Eiffel, on the first floor 311 ft (95 m) above sea level; and the Le Jules Verne, a gastronomical restaurant on the second floor, with a private lift. This restaurant has one star in the Michelin Red Guide. In January 2007, the multi-Michelin star chef Alain Ducasse was brought in to run Jules Verne.

 

Attempted relocation

 

According to interviews given in the early 1980s, Montreal Mayor Jean Drapeau negotiated a secret agreement with French President Charles de Gaulle for the tower to be dismantled and temporarily relocated to Montreal to serve as a landmark and tourist attraction during Expo 67. The plan was allegedly vetoed by the company which operated the tower out of fear that the French government could refuse permission for the tower to be restored to its original location.

 

Economics

 

The American TV show Pricing the Priceless speculates that in 2011 the tower would cost about $480,000,000 to build, that the land under the tower is worth $350,000,000, and that the scrap value of the tower is worth $3,500,000. The TV show estimates the tower makes a profit of about $29,000,000 per year, though it is unlikely that the Eiffel Tower is managed so as to maximize profit.

It costs $5,300,000 to repaint the tower, which is done once every seven years. The electric bill is $400,000 per year for 7.5 million kilowatt-hours.

The Tokyo Tower in Japan is a very similar structure of very similar size. It was finished in 1958 at a final cost of ¥2.8 billion ($8.4 million in 1958).

 

Source Wikipedia

   

Mariner's Warning. The remains of the shipwreck Peter Iredale and the warm glow of two fishing vessels working beyond the horizon are juxtaposed beneath a Pacific winter squall converging on the Oregon coast at midnight. Once a two-thousand ton four-masted steel barque, this bow section is all that remains of the sailing vessel that ran aground on 25 October 1906. Nikon D700, Nikon AF Nikkor 20-35 f/2.8D.

"For my part I know nothing with any certainty, but the sight of the stars makes me dream" - Van Gogh

 

Via Lactea.

 

I felt a bit down today, but I was happy that the sky was clear. I had a feeling this night would be the perfect moment to capture the thing that eluded me last year - the Milky Way. Seeing this, after 3 hours of being out in the cold (-5C), was one of the most amazing moments I've had.

 

Anyway, I packed two of my DSLRs (Nikon D7000 and the D800), along with two tripods. The lenses of choice were the 24-70mm for the D800, and the 18-105mm for the D7000. I was mostly using the D7000 to record timelapse via the intervalometer and a few creative shots. This was shot in near pitch black conditions- though, still with the presence of slight light pollution. GPS data + constellation maps + weather data really helped!

 

It was still a bit hard to discern the presence of the Milky Way due to slight light pollution, but these were the best conditions I have seen during winter. Accessibility as well, since it was close, and most of the light pollution from the city is being blocked by mountains.

 

Now, I can relax a bit, knowing it is possible to capture it (:

Accessible by boat or canoe on the Pieman River.

At the port of Messina (immediately adjacent to Messina Centrale station), all railway traffic to and from Sicily is embarked or disembarked from a fleet of train ferries that are accessible to non-railway traffic as well (cars and foot passengers). Hence the possibility to shoot this shot. A number of covered goods vans is embarked on M/F «Villa». The set of points in the foreground is actually on the deck of the ship (to my knowledge, that is fairly unique, however all Strait of Messina vessels seem to be equipped this way), whereas the other tracks converge to the edge of the deck but the three-way points are located on the access ramp (visible here and here). Messina Marittima, 06-06-2009.

In downtown Inverness, Cooter Pond Park provides a boardwalk over its namesake pond for birding and wildlife watching, plus a great photo op with a stack of oversized turtles near one of the park entrances. Across the pond, the Withlacoochee State Trail slips into Inverness and is accessible from the north end of this park.

Schweiz / Berner Oberland - Jungfraujoch

 

Aletsch Glacier seen from Sphinx Observatory.

 

Aletschgletscher gesehen vom Sphinx-Observatorium.

 

The Jungfraujoch (German: lit. "maiden saddle") is a saddle connecting two major 4000ers of the Bernese Alps: the Jungfrau and the Mönch. It lies at an elevation of 3,463 metres (11,362 ft) above sea level and is directly overlooked by the rocky prominence of the Sphinx. The Jungfraujoch is a glacier saddle, on the upper snows of the Aletsch Glacier, and part of the Jungfrau-Aletsch area, situated on the boundary between the cantons of Bern and Valais, halfway between Interlaken and Fiesch.

 

Since 1912, the Jungfraujoch has been accessible to tourists by the Jungfrau line, a railway from Interlaken and Kleine Scheidegg, running partly underground through a tunnel through the Eiger and Mönch. The Jungfraujoch railway station, at an elevation of 3,454 metres (11,332 ft) is the highest in Europe. It lies east of the saddle, below the Sphinx station, and is connected to the Top of Europe building, which includes several panoramic restaurants, shops, exhibitions, and a post office. Several tunnels lead outside, where secured hiking trails on the crevassed glacier can be followed, in particular to the Mönchsjoch Hut. The normal route to the Jungfrau and Mönch starts from there.

 

The Sphinx Observatory, one of the highest astronomical observatories in the world, provides an additional viewing platform at a height of 3,572 metres (11,719 ft), the second-highest in Switzerland. It can be reached by an elevator from the Jungfraujoch. The observatory houses one of the Global Atmosphere Watch's atmospheric research stations. The Jungfraujoch radio relay station, which is not accessible to the public, is installed west of the Jungfraujoch, on the Jungfrau ridge. It is Europe's highest radio relay station.

 

Etymology

 

Swiss and Austro-Bavarian German Joch (lit. 'yoke') is a term for 'ridge between two higher peaks' recorded in the 14th century (Grimm, Deutsches Wörterbuch "bereits im 14. jahrh. als ortsname: des gotzhus zwing und ban vahet an Rotenhalden und denne die roten bachtalen uf unz an den grat, und den grat obnan hin ob Grüblen hin iemerme, unz an Joch. und ab Joch unz an Stoerben. weisth. 1, 4 (Zürich)").

 

The name Jungfrau ('maiden, virgin'), which refers to the highest mountain overlooking the Jungfraujoch, is most likely derived from the name Jungfrauenberg given to Wengernalp, so named for the nuns of Interlaken Monastery, its historical owner. However, the "virgin" peak was heavily romanticized as a "goddess" or "priestess" only in late 18th- to 19th-century Romanticism. 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

 

The Jungfraujoch is a snow saddle located directly between the summits of Mathildespitze (west) and Sphinx (east). It is, however, most notably the lowest point between the Jungfrau and the Mönch, respectively third and fourth highest mountains in the Bernese Alps, and the key col of the former. The south side (canton of Valais), almost flat, is constituted by the Jungfraufirn, one of the branches of the Aletsch Glacier, the longest in the Alps. From the south, the Jungfraujoch can be relatively easily accessed by mountaineers in two days from the region of Fiesch, via the Konkordia Hut. The north side (canton of Bern) is almost vertical with a difference of height of nearly 3,000 metres from the bottom of the valley at Interlaken, with no easy natural access. For those reasons, the only easy and quick access to the Jungfraujoch is through the 7 kilometre-long tunnel of the Jungfrau Railway, accessed via Kleine Scheidegg on the north side, the railway pass between Lauterbrunnen and Grindelwald.

 

Administrativelly, the Jungfraujoch is split between the territories of the municipalities of Lauterbrunnen and Fieschertal. Nearly all built infrastructure, including the Jungfraujoch railway station, Top of Europe complex and the Sphinx Observatory, are on the Valais side of the border, therefore in the municipality of Fieschertal. The ridge between the Jungfrau and the Mönch is a major European watershed as well. The north side is drained by the Weisse Lütschine, the Aare and the Rhine. The south side is drained by the Massa and the Rhone.

 

First crossing

 

There is a tradition in the Bernese Oberland, supported by some documentary evidence, that a pass existed between Grindelwald and Fiesch in Valais in the late medieval period, later lost to the advancing glaciers. With the early development of tourism in Switzerland and the exploration of the High Alps in the 19th century, there were once again attempts to traverse the great ridge that encloses the head of the Aletsch Glacier, and connecting Fiesch with Grindelwald and Wengernalp. Four such routes were found, with the Jungfraujoch and the Eigerjoch being among the most difficult passes in the Alps, despite the former having a relatively easy southern approach on the Aletsch Glacier.

 

The first ascent of the north side of the Jungfraujoch succeeded in July 1862, by a party of six English climbers and six Swiss guides: Leslie Stephen, F. J. Hardy, H. B. George, Living, Moore, and Morgan, with Christian Almer, Christian and Peter Michel, Ulrich Kauffmann, P. Baumann, and C. Bohren as guides. The time of ascent from Wengernalp was nine hours.

 

The party turned back on the first day at a bergschrund, returning on the following day with a ladder 25 ft (7.6 m) in length, carried by Peter Rubi, a porter from Grindelwald. The way lay at first by the rocky buttress of the Mönch, separating the Eiger and Guggi glaciers. From the buttress the route descended a short distance in order to reach the Guggi Glacier, which could be ascended to a plateau. This halting place was reached in about three hours.

 

Above the bergschrund was a second and smaller plateau which was situated immediately under the long slopes of broken neve that lay below the saddle. The final and very arduous stage in the ascent was a single patch of dark rocks jutted out from the snow in the ridge connecting the Jungfrau with the Mönch. After more than an hour of climbing, a great wall of ice, whose projecting cornice of snow was fringed by long icicles, had to be avoided bearing left in the direction of the Mönch, along the base of the wall by a slippery pathway of ice formed from the dripping from the icicles above. At a point where the pathway thinned out nearly to a point, and was cut across by a transverse crevasse, the wall became low enough to be scaled by the ladder. This was the last serious obstacle: a moderate slope of névé, unbroken by crevasses, then led up to the summit of the saddle.

 

After reaching the first patch of rocks, a short way below the saddle on the south side, the party divided: George and Moore, with C. Almer and U. Kaufmann went down to the Eggishorn and Fiesch, therefore completing the first crossing of the Jungfraujoch, while the remainder of the party returned to Grindelwald by the Mönchsjoch.

 

Jungfrau Railway

 

History

 

Adolf Guyer-Zeller first thought of the idea of a tunnel in 1893, and at that point, he had planned to have seven stations inside the tunnel before reaching the peak of the Sphinx. The building of the tunnel started on July 27, 1896 and took 16 years to complete.[6] The construction phase was troubled by many problems including monetary shortages, inclement weather and mounting deaths due to construction accidents. The worst accident occurred in 1908, when 30 tons of dynamite accidentally exploded.

 

When construction finally finished, the railway reached only to the height of the Jungfraujoch saddle, rather than the summit of the Sphinx, and had only two intermediate stations. However, even in its current state, the Jungfraubahn is a significant achievement in engineering and construction, still holding the title for highest railway in Europe.

 

Railway

 

The train into the mountain leaves from Kleine Scheidegg, which can be reached by trains from Grindelwald and Lauterbrunnen. The train enters the tunnel running eastward through the Eiger shortly after leaving Kleine Scheidegg.

 

It runs close behind the Eiger's north face, stopping at Eigerwand, where there is a window about 8 m long and a metre high, halfway up the face. The windows have been placed in holes used to remove excavated rock from the tunnel during construction, and are also occasionally used as access points, by climbers, and also rescue parties. This window was used for one of the final scenes of a Clint Eastwood spy movie, The Eiger Sanction. There one can get off the train to admire the view before the train continues five minutes later. The tunnel then turns west, heading towards the Jungfrau. There is a second stop at a window looking out on the Eismeer ("Sea of Ice") before the train continues to the Jungfraujoch. The tunnel was constructed between 1898 and 1912; it is about 7 kilometers (4.3 mi) long, with gradients of up to 25%. The journey from Kleine Scheidegg to Jungfraujoch takes approximately 50 minutes including the stops at Eigerwand and Eismeer; the downhill return journey taking only 35 minutes.

 

The Jungfraujoch complex plays an important role in John Christopher's The Tripods novels.

 

Climate

 

Located above the permanent snow line, the Jungfraujoch is officially the coldest place in Switzerland, although other higher locations with no weather station, for example the top of the nearby Jungfrau and Finsteraarhorn, probably experience a more extreme climate. According to Köppen climate classification, the Jungfraujoch has an alpine climate on the border between tundra climate (ET) and ice cap climate (EF) with long, cold winters lasting most of the year and a brief period during summer where the average daily highs rise above freezing.

 

(Wikipedia)

 

The Aletsch Glacier (German: Aletschgletscher, German pronunciation: [ˈalɛtʃˌɡlɛtʃɐ]) or Great Aletsch Glacier (Grosser Aletschgletscher) is the largest glacier in the Alps. It has a length of about 23 km (14 mi) (2014), has about a volume of 15.4 km3 (3.7 cu mi) (2011), and covers about 81.7 km2 (31.5 square miles) (2011) in the eastern Bernese Alps in the Swiss canton of Valais. The Aletsch Glacier is composed of four smaller glaciers converging at Konkordiaplatz, where its thickness was measured by the ETH to be still near 1 km (3,300 ft). It then continues towards the Rhône valley before giving birth to the Massa. The Aletsch Glacier is – like most glaciers in the world today – a retreating glacier. As of 2016, since 1980 it lost 1.3 kilometres (0.81 mi) of its length, since 1870 3.2 kilometres (2.0 mi), and lost also more than 300 metres (980 ft) of its thickness.

 

The whole area, including other glaciers is part of the Jungfrau-Aletsch Protected Area, which was declared a UNESCO World Heritage Site in 2001.

 

Geography

 

The Aletsch Glacier is one of the many glaciers located between the cantons of Bern and Valais on the Bernese Alps located east of the Gemmi Pass. The whole area is considered to be the largest glaciated area in western Eurasia. The Fiescher and Aar Glaciers lying on the east have similar extensions.

 

Except the Finsteraarhorn, all the highest summits of the Bernese Alps are located within the drainage basin of the glacier. The Jungfrau and Mönch constitute the northern boundary; the Gross Fiescherhorn and Gross Wannenhorn lie on its east side; finally the culminating point, the Aletschhorn (4,193 m (13,757 ft)) is located on the west side.

 

Before reaching the maximum flow, four smaller glaciers converge at Konkordiaplatz:

 

From the western mouth flows the Grosser Aletschfirn, which runs along the northern foot of the Aletschhorn and Dreieckhorn. The Grosser Aletschfirn is supplied from the north by three notable firns: the Äbeni Flue-Firn, the Gletscherhornfirn, and the Kranzbergfirn. All of these firns have their starting points at around 3,800 m (12,500 ft). From the Äbeni Flue-Firn to the Konkordiaplatz, the Grosser Aletschfirn is 9 km (5.6 mi) long and is on average about 1.5 km (0.93 mi) wide. On the west, the Grosser Aletschfirn connects with the Langgletscher over the 3,158 m (10,361 ft) high glacier pass, the Lötschenlücke, into the Lötschental.

 

From the northwestern mouth flows the Jungfraufirn. This firn in fact represents the straight continuation of the Aletsch Glacier, yet is the shortest of the four tributary glaciers. It has its origin on the southern flank of the Mönch and at the eastern flank of the Jungfrau with the Jungfraujoch in-between. Up to the Konkordiaplatz, the Jungfraufirn is a scarce 7 km (4.3 mi) long, and returns to flank the Kranzberg in the west and the Trugberg in the east. At its highest point, it is 2 km (1.2 mi) wide, and further down it is still a good 1 km (0.62 mi) wide.

From the northern mouth flows the Ewigschneefäld ("Eternal snow field"), where its starting point takes the east flank of the Mönch. In an elbow, it flanks from Trugberg in the west and the Gross Fiescherhorn and Grünhorn in the east, flowing on to the Konkordiaplatz. Up to here, it is about 8 km (5.0 mi) long and averages about 1.2 km (0.75 mi) wide.

 

The mouth at the Konkordiaplatz it follows over a rise with a descent from 25 to 30 percent; here, the glacier is sharply split. Against the north is the Ewigschneefäld over the snow-covered pass of the Unners Mönchsjoch (3,518 m (11,542 ft)), connected with the catchment area of the Ischmeer (Wallis German for "Ice Sea"). Through the Obere Mönchsjoch (3,624 m (11,890 ft)) between the Mönch and the Trugberg stands a connection to the Jungfraufirn.

 

From the east, the smallest firn arrives at the Konkordiaplatz: the Grüneggfirn. Its northern arm begins below the Grünegghorn (3,860 m (12,660 ft)). The southern arm collects its snow and ice in the pot flanked by the Wyssnollen, Fiescher Gabelhorn (3,866 m (12,684 ft)), and the Chamm. Between the peaks Wyssnollen and Grünhörnli another glacier pass, the Grünhornlücke (3,279 m (10,758 ft)), connects to the Fieschergletscher. The Grüneggfirn enters the Konkordiaplatz in a gap between the mountainsides Grünegg to the north and the Fülberg to the south. On the western side of the Fülberg the Konkordia hut (mountain hut) overlooks the whole Konkordiaplatz at an altitude of 2,850 m (9,350 ft).

 

South of Konkordiaplatz, the glacier runs towards the valley of the Oberwallis (Upper Valais); on the east side, near Bettmeralp, lies a small glacier lake, Märjelensee (2,301 m (7,549 feet)); from the western side used to enter the Mittelaletschgletscher, but since the end of the 20th century the connection with the Aletsch Glacier has been lost. Further down, until about 1880, the Oberaletschgletscher did also enter the Aletsch Glacier at its mouth. But since then both glaciers have been retreating so far that they do not connect anymore (the Upper Aletsch Glacier did retreat about 1.3 km (0.81 mi) from its connecting point with the Aletsch Glacier), but both serve now only as the source of the river Massa. The river flows through the Lake Gibidum (a reservoir, and coincidentally representing the glacier's mouth region in the 19th century, which is a retreat of more than 4 km (2.5 mi)) and a gorge of the same name before reaching the Rhône near Brig.

 

Tourism

 

The area of the Aletsch Glacier and some surrounding valleys is on the UNESCO World Heritage list, thus it is protected and the facilities are mostly restricted to the external zones. The region between Belalp, Riederalp and Bettmeralp (which is called Aletsch Region) in Valais gives access to the lower part of the glacier. The Bettmerhorn and Eggishorn are popular view points and are accessible by cable car. The Massa river can be crossed since 2008 by a suspension bridge, thus allowing hikes between the left and the right part of the glacier.

 

The Jungfraujoch railway station (3,450 m) gives a direct access to the upper Aletsch Glacier as well as the normal route to the Jungfrau. It can be reached only from Interlaken in the canton Bern. Hiking paths pass the Konkordia Hut or the Hollandia Hut, eventually reaching other glaciers in the massif.

 

On the Riederfurka, at 2,065 metres between Riederalp and the glacier, is located the historic Villa Cassel, former summer residence of many famous and influential guests from the worlds of politics and finance. The house is now one of the centers of the environmental organization Pro Natura, which hosts a permanent exhibition about the site.

 

Panorama

 

Also at the mouth of the Konkordiaplatz from the east is the small but important Grüneggfirn (3 km long and averaging 600 m wide). This firn is connected in the over the glacier pass Grünhornlücke (3280 m high) to the Fiescher Glacier in the east.

 

From the Konkordiaplatz, the Aletsch Glacier has a width of approximately 1.5 km and moves at a rate of 180 m per year to the southeast on course with the Rhône valley, bordering the Dreieckhorn in the west and the great Wannenhorn in the east. It then takes a great right turn and bends ever closer to the southwest, running through the edge of the Eggishorn and Bettmerhorn of the Rhône valley. The lowest part of the great Aletsch Glacier is largely covered with detritus of the lateral and medial moraines. The glacier's toe currently lies about 1560 m high, far beneath the local tree line. From it springs the Massa stream, which flows through the Massa Canyon and is used to generate hydroelectric power. It continues through the upper half of the Brig, eventually entering into the Rhône.

 

The great Aletsch Glacier shows considerable ice cover. At the Konkordiaplatz, it has an ice cover of more than 900 m, but as it moves to the south, the greater part of the ice melts, gradually decreasing the cover to around 150 m.

 

The characteristically dark medial moraine, situated almost in the middle of the glacier, runs protracted in two bands from the Konkordiaplatz along the whole length to the glacier's toe-zone. This medial moraine is collected from the ice of three large ice fields, which all run together. The westernmost medial moraine has been named the Kranzbergmoräne, and the easternmost carries the name Trugbergmoräne.

 

Formation and evolution

 

The Aletsch Glacier resulted from the accumulation and compaction of snow. Glaciers generally form where snow and ice accumulation exceed snow and ice melt. As the snow and ice thicken it reaches a point where it begins to move due to a combination of gravity and pressure of the overlying snow and ice.

 

During the last glacial periods, the Aletsch Glacier was much larger than now. 18,000 years ago the lower part of the ridge, between Riederalp and the glacier, was completely covered by ice. Only the summits of the Bettmerhorn, Eggishorn and the Fusshörner were above the glacier. After an important retreat, the glacier again advanced 11,000 years ago during the last glacial period. The glacier reached the Rhône valley, and its ice the Riederfurka. Remaining moraines are still visible in the Aletsch Forest.

 

Since the last glaciation, the glacier generally retreated. However slight climatic changes happened and, in 1860, the glacier was 3 km longer and the ice level 200 m higher.

 

As for many other glaciers, records show a major longer-term retreat trend. The Aletsch Glacier receded by 3.2 km (2.0 mi) since 1870, including 1.3 km (0.81 mi) since 1980.[6] A record retreat of 114.6 metres (376 ft) happened in 2006 alone.

 

Since the end of the Little Ice Age in 1850 the glacier has lost 20 percent of its ice mass, considerably less than other glaciers in Switzerland, which have lost up to 50 percent. This is explained with the large size of the Aletsch Glacier, which reacts much slower to climate change than smaller glaciers. It is however estimated that, by 2100, the glacier will have only one tenth of its 2018 ice mass.

 

Photo opportunity

 

On August 18, 2007, photographer Spencer Tunick used hundreds of naked people in a "living sculpture" on the Aletsch Glacier in a photo shoot which he said was intended to draw attention to global warming and the shrinking of the world's glaciers. The temperature was about 10 °C (50 °F) at the time of the photo shoot. The 600 participants on the shrinking glacier said that they had volunteered for Tunick (a collaboration with Greenpeace) to let the world know about the effects of global warming on the melting Swiss glaciers.

 

(Wikipedia)

 

Das Jungfraujoch ist mit 3466 m ü. M. der tiefste Punkt im Verbindungsgrat zwischen dem Mönch und der Jungfrau in den Berner Alpen, auf der Grenze zwischen den Kantonen Bern und Wallis. Das Joch ist weit und stark überfirnt. Aufgrund der auch dort stattfindenden Gletscherschmelze sinkt es jedes Jahr im Schnitt einige Dezimeter ab. Es gehört zu den bedeutendsten Reisezielen in der Schweiz. Etwa 1 Million Touristen (Stand 2018) fahren jährlich zum höchstgelegenen Bahnhof Europas.

 

Umgebung

 

In der Umgebung des Jungfraujochs befinden sich einige Viertausender der Berner Alpen. Im Nordosten befinden sich der Mönch (4107 m ü. M.) sowie der Eiger (3967 m ü. M.) und im Südwesten die Jungfrau (4158 m ü. M.). Im Süden des Jungfraujochs ist hinter dem Konkordiaplatz das Aletschhorn zu sehen. 200 Meter westlich befindet sich auf dem Grat zur Jungfrau die 3557 Meter hohe Mathildespitze, etwa 600 Meter östlich des Jochs erhebt sich die Sphinx, eine markante kleine Spitze mit einer Höhe von 3571 Metern. Sie trägt eine Aussichtsplattform und ein wissenschaftliches Observatorium (Sphinx-Observatorium). In ihrem Innern befindet sich auf 3454 Metern Höhe die Endstation der Jungfraubahn. Diese Station ist der höchstgelegene Bahnhof Europas (daher der Beiname Top of Europe). Durch einen Stollen gelangt man von hier aus auf die Walliser Seite und zum Aletschgletscher. Der schnellste Aufzug der Schweiz führt auf den Gipfel der Sphinx. Ein im Sommer üblicherweise für Spaziergänger präparierter Weg führt vom Jungfraujoch zur Mönchsjochhütte. Beim Jungfraujoch selbst gibt es für Besucher keine Übernachtungsmöglichkeit. Die Stollen werden nachts verschlossen, so dass auch freies Biwakieren nicht möglich ist.

 

Passübergang

 

Als Übergang für Fuss- oder Skitouristen vom Berner Oberland ins Wallis oder umgekehrt besitzt das Jungfraujoch praktisch keine Bedeutung. Der Weg vom Wallis über den Aletschgletscher hinauf ist – von der Spaltengefahr im Jungfraufirn abgesehen – leicht. Der Aufstieg vom Berner Oberland her ist jedoch eine beschwerliche Hochtour (Steileis, G 5-6, zeitweise unmöglich).

 

Erschliessung

 

Seit dem 1. August 1912 ist das Jungfraujoch durch die Jungfraubahn erschlossen. Von Grindelwald oder Lauterbrunnen erreicht man mit der Wengernalpbahn die Station Kleine Scheidegg. Diese Station auf 2061 m ü. M. ist die „Talstation“ der Jungfraubahn. Von hier aus muss die Jungfraubahn 9,34 Kilometer bezwingen, davon verlaufen die letzten 7,32 km unterirdisch, bis sie am Jungfraujoch ankommt. Die unterirdische Endstation auf 3454 m ü. M. ist der höchste Bahnhof Europas. Auf ihrem Weg hält die Bahn an zwei Stationen: Eigergletscher (2320 m) und Eismeer (3158 m). Seit dem 11. Dezember 2016 wird die Station Eigerwand (2864 m) nicht mehr bedient.

 

Bauten und Anlagen

 

Seit 1912, mit der Eröffnung der Jungfraubahn, wird für das Wohlergehen der Besucher auf dem Jungfraujoch gesorgt. Mehrere Restaurants, aber auch spezielle Aussichtsplattformen und Erlebnisse wurden eigens dafür geplant und realisiert.

 

Restaurants

 

Bereits bei der Eröffnung weihte man das provisorische „Touristenhaus“ mit dem höchstgelegenen Restaurant Europas ein. Mit seiner Eröffnung in 1924 ergänzte das neue „Berghaus Jungfraujoch“ – mit Giebeldach und in die Felswand gebaut – dieses Touristenhaus. Es wurde als „Das Haus über den Wolken“ bekannt. Im Erdgeschoss befanden sich eine geräumige Wartehalle mit geheiztem Fussboden, Bahn- und Postschaltern und ein Bazar. Besonders ins Auge stach die „Walliserstube“, die mit der Arvenholztäfelung und Anwendung von Naturstein eine besondere Charakteristik erhielt. Gäste aus aller Welt übernachteten in einem der 18 gemütlichen, holzgetäfelten Schlafzimmer mit Waschbecken und Krügen auf dem Nachttisch. Auf der Aussichtslaube stand man am Ursprung des längsten und grössten zusammenhängenden Gletschers der Alpen, dem Aletschgletscher. 1972 wütete im Berghaus ein Feuer mit erheblichen Folgen: Lediglich das Bahnbüro, die Perronanlage in der rückwärtigen Felsenkaverne sowie die Forschungsstation konnten vor dem Feuer geschützt werden. Nach dem Unglück lud die Jungfraubahn Architekten zu einem Wettbewerb ein, ein neues Gebäude zu entwerfen. Der Gewinner war Ernst E. Anderegg mit dem im Hang eingefügten „Top of Europe“, das 1987 eingeweiht wurde.

 

Sphinx-Observatorium und Forschungsstation

 

Bereits vor Baubeginn der Jungfraubahn war die Einrichtung eines Observatoriums und einer meteorologischen Forschungsstation vom Gründer der Bahn, Adolf Guyer-Zeller, geplant. 1931 konnten die Laboratorien für Meteorologie, Glaziologie, Strahlungsforschung, Astronomie, Physiologie und Medizin auf (3571 m ü. M.) mit einem Felsenheim für 13 Forscher eingeweiht werden. 1937 wurde das Sphinx-Observatorium bezogen. 1950 wurde dem Observatorium die Kuppel für astronomische Beobachtungen aufgesetzt, die seither immer wieder den modernsten Erfordernissen der Wissenschaft angepasst wird. Das Forschungsgebäude selbst ist nicht zu besichtigen.

 

Unterhalb des Sphinx-Observatoriums und östlich des Bahnhofs und der Restaurants befindet sich die Hochalpine Forschungsstation, eine an die Universität Bern angegliederte Forschungseinrichtung der International Foundation High Altitude Research Stations Jungfraujoch and Gornergrat. Die Gästezimmer der Forschungsstation sind die einzige Übernachtungsmöglichkeit auf dem Jungfraujoch, aber nur Wissenschaftlern und den Betreuern vorbehalten.

 

Das Observatorium ist mit einem 111,4 Meter langen Lift erschlossen. Die Aussichtsplattform bietet den Besuchern bei schönem Wetter einen Ausblick bis in die Nachbarländer Frankreich, Deutschland und Italien. 1993 wurde die Sphinx für die Besucher renoviert. Drei Jahre waren nötig, um sie gemeinsam mit der schnellsten Liftanlage der Schweiz, der verglasten Aussichtshalle und der rund um das Gebäude verlaufenden Terrasse fertigzustellen.

 

Eispalast

 

Zwei Bergführer begannen in den 30er Jahren eine gewaltige Halle aus dem Gletschereis zu schneiden. In Handarbeit, mit Eispickel und Säge, entstand ein 1'000 Quadratmeter grosses Labyrinth – der Eispalast. Das 1934 begonnene Werk ist nie vollendet worden. Durch die Ausdünstung der tausenden Besucher muss die Grotte auf minus drei Grad künstlich klimatisiert werden. Die Decken und das Gewölbe der Gänge müssen regelmässig nachgehauen werden. 1992 bekam der Eispalast einen neuen Zugang und ist seit 2002 durch den Ice-Gateway erreichbar.

 

Post

 

Auf dem Jungfraujoch liegt auch das höchstgelegene Postbüro Europas mit der eigenen Postleitzahl 3801. Obwohl die Postleitzahl gemäss Schweizerischer Post dem Kanton Wallis zugewiesen ist, so befindet sie sich dennoch im Zahlengebiet 38xx der im Tal liegenden Gemeinden des Kantons Bern.

 

Richtstrahlstation Ostgrat

 

Am Ostgrat der Jungfrau auf nicht ganz 3700 Meter Höhe befand sich die 2011 abgebaute Richtstrahlstation Ostgrat. Vom Jungfraujoch führen eine teilweise durch den Gletscher geführte Stollenbahn sowie eine einspurige Standseilbahn zur Anlage. In der Mitte der Standseilbahnstrecke befindet sich eine Zwischenstation, welche für Forschungszwecke genutzt wird. Es existieren dort Photovoltaik-Testanlagen.

 

Versorgung

 

Die intensive Sonnenstrahlung bietet sich zur Energienutzung an. So wird die tagsüber einfallende Wärme für die Nacht gespeichert. Aber auch die zahlreichen sonst kaum beachteten Wärmequellen – von Lampen über Elektrogeräte bis zur Körperwärme der anwesenden Personen – werden in die Regulierung der Raumtemperatur einbezogen. So gibt es im gesamten Berghaus keinen Heizkörper. Sogar wenn die Sonne nicht scheint und die Aussentemperatur bei minus 30 °C liegt, kann tagsüber auf zusätzliche Heizungen verzichtet werden. Nur nachts wird über die Lüftungsanlage mit elektrischer Energie so viel Wärme zugeführt, dass eine Raumtemperatur von mindestens 18 °C erhalten bleibt.

 

Brauchwasser wird aus Schnee gewonnen und aufbereitet. In Trockenperioden muss es nach wie vor mit Zisternenwagen auf der Schiene von der Kleinen Scheidegg heraufgebracht werden. Für das Jahr 2012 ist ein neues Projekt geplant, bei dem das Wasser durch Leitungen von der Kleinen Scheidegg mit Druckluft hinauf auf das Jungfraujoch gepumpt wird. Somit können die Zisternentransporte reduziert werden.

 

Das Abwasser lässt sich nicht mehr in den Gletscherschrund einleiten. Deshalb wurde eine 9,4 Kilometer lange Abwasserleitung ins Tal installiert. Sämtliche Abwässer aus Küchen, Unterkünften und Toiletten können auf diese Weise umweltfreundlich entsorgt werden.

 

Klima

 

Auf dem Jungfraujoch herrschen extreme Klimabedingungen. Die mittlere Jahrestemperatur beträgt −6,7 °C mit Schwankungen von −37 °C bis +13 °C. Die Windgeschwindigkeit kann bis zu 260 km/h betragen. Die Sonne scheint jährlich durchschnittlich 1773 Stunden. Zu jeder Jahreszeit muss mit starken Vereisungen, Schneefall und Lawinen gerechnet werden. Die Messstation von MeteoSchweiz liegt auf einer Höhe von 3571 m ü. M.

 

Tiere

 

Bis zum Jahr 2009 waren auf dem Gletscher täglich 25 Polarhunde im Einsatz. Auf einer präparierten Piste (rund 500 Meter lang) zogen die Hunde Schlitten mit Besuchern, waren aber auch für Postsendungen und Lebensmitteltransporte von Wengen zum Eigergletscher im Einsatz. Das Rudel galt als das meistfotografierte Motiv auf dem Jungfraujoch.

 

Für Ornithologen ist die Hochgebirgsregion interessant, da verschiedene Vogelarten zum Teil auch überwintern. Der Schneefink beispielsweise nistet und schläft in den schroffen Felswänden und findet bei den Behausungen der Forscher Futter.

 

(Wikipedia)

 

Der Grosse Aletschgletscher ist der flächenmässig grösste und längste Gletscher der Alpen. Er befindet sich auf der Südabdachung der Berner Alpen im Schweizer Kanton Wallis. Die Länge des Gletschers beträgt 22,6 km, die Fläche wird mit 78,49 km² angegeben. Der Aletschgletscher entwässert über die Massa in die Rhone. Die Fläche des gesamten Einzugsgebiets der Massa beträgt 195 km², wovon 1973 etwa zwei Drittel vergletschert waren. Oft werden bei der Flächenangabe der Ober- und Mittelaletschgletscher einbezogen, da diese früher mit dem Grossen Aletschgletscher verbunden waren. Die gesamte vergletscherte Fläche einschliesslich dieser Gletscher betrug 1973 etwa 128 km², für das Jahr 1863 wird eine Fläche von 163 km² angenommen.

 

Ursprung am Konkordiaplatz

 

Der Ursprung des Grossen Aletschgletschers liegt in der rund 3800 m hoch gelegenen Jungfrau-Region. Am Konkordiaplatz (♁645905 / 150101), einer 6 km² grossen und nur wenig geneigten Eisfläche, fliessen drei mächtige Firnströme zusammen:

 

Von Westen mündet der Grosse Aletschfirn, der entlang dem Nordfuss von Aletschhorn und Dreieckhorn fliesst. Der Grosse Aletschfirn wird von Norden her durch drei weitere bedeutende Firne gespeist, nämlich durch den Ebnefluhfirn, den Gletscherhornfirn und den Kranzbergfirn. Alle diese Firne nehmen ihren Ausgangspunkt auf rund 3800 m ü. M. Einschliesslich des Ebnefluhfirns hat der Grosse Aletschfirn bis zum Konkordiaplatz eine Länge von 9 km und ist durchschnittlich fast 1,5 km breit. Gegen Westen ist der Grosse Aletschfirn über den 3173 m ü. M. hohen Gletscherpass der Lötschenlücke mit dem Langgletscher verbunden, der ins Lötschental abfliesst.

 

Von Nordwesten mündet der Jungfraufirn, der zwar die gerade Fortsetzung des Aletschgletschers darstellt, jedoch der kürzeste der drei Tributärgletscher ist. Er hat seinen Ursprung an der Südflanke des Mönchs, am Jungfraujoch und an der Ostflanke der Jungfrau. Bis zum Konkordiaplatz legt der Jungfraufirn eine Wegstrecke von knapp 7 km zurück und wird dabei im Westen vom Kranzberg, im Osten vom Trugberg flankiert. Er ist in seinem oberen Teil 2 km, weiter unten noch gut 1 km breit.

 

Von Norden mündet das Ewigschneefeld, das seinen Ausgangspunkt an der Ostflanke des Mönchs nimmt und in einem Bogen, flankiert vom Trugberg im Westen sowie dem Gross Fiescherhorn und dem Grünhorn im Osten, zum Konkordiaplatz fliesst. Bis hierher ist es ungefähr 8 km lang und durchschnittlich 1,2 km breit. Die Mündung in den Konkordiaplatz erfolgt über einen Steilhang mit einem Gefälle von 25 bis 30 %; der Gletscher ist hier stark zerklüftet. Gegen Norden ist das Ewigschneefeld über den firnbedeckten Pass des Unteren Mönchsjochs (3529 m ü. M.) mit dem Einzugsgebiet des Unteren Grindelwaldgletschers verbunden. Durch das Obere Mönchsjoch (3627 m ü. M.) zwischen dem Mönch und dem Trugberg besteht eine Verbindung zum Jungfraufirn. Ferner mündet am Konkordiaplatz von Osten noch der wesentlich kleinere Grüneggfirn (3 km lang und durchschnittlich 600 m breit). Dieser ist nach Osten über den Gletscherpass der Grünhornlücke (3280 m ü. M.) mit dem Fieschergletscher verbunden.

 

Weiterer Verlauf

 

Vom Konkordiaplatz aus bewegt sich der Eisstrom mit einer Breite von ungefähr 1,5 km und mit einer Geschwindigkeit von bis zu 180 Metern pro Jahr nach Südosten in Richtung Rhonetal, gesäumt vom Dreieckhorn im Westen und dem Gross Wannenhorn im Osten. Er zeichnet dann eine grosse Rechtskurve und biegt immer mehr nach Südwesten ab, nun durch den Grat des Eggishorns und Bettmerhorns vom Rhonetal getrennt. Der unterste Teil des Grossen Aletschgletschers ist weitgehend durch das Geschiebematerial von Seiten- und Mittelmoränen bedeckt. Die Gletscherzunge liegt derzeit auf rund 1'560 Meter Höhe, weit unterhalb der lokalen Waldgrenze. Aus ihr entspringt der Bach Massa, welcher nach der Massaschlucht und einer Nutzung in einem Wasserkraftwerk, in Bitsch, oberhalb von Naters, in die Rhone (Rotten) fliesst.

 

Der Grosse Aletschgletscher weist beachtliche Eisdicken auf. Am Konkordiaplatz hat der Gletscher eine Eisdicke von mehr als 900 Metern, gegen Süden nimmt die Mächtigkeit des Eises allmählich auf rund 150 m ab. Charakteristisch sind die beiden dunklen, fast in der Mitte des Aletschgletschers gelegenen Moränenspuren, welche sich ab dem Konkordiaplatz auf der gesamten Länge bis in den Zungenbereich hinziehen. Es sind die Mittelmoränen, die das Eis der drei Hauptfirne voneinander trennen. Die westliche Mittelmoräne wird auch Kranzbergmoräne genannt, die östliche trägt den Namen Trugbergmoräne.

 

Gletscherschwankungen

 

In seinem Hochstadium während der Kleinen Eiszeit um die Mitte des 19. Jahrhunderts erstreckte sich der Grosse Aletschgletscher noch rund 2,5 km weiter talabwärts. Aufgrund der allgemeinen Erwärmung seit etwa 1870 hat er besonders unterhalb des Konkordiaplatzes massiv an Volumen eingebüsst und sowohl an den Seiten als auch im Zungenbereich Flächen von mehreren Quadratkilometern freigegeben. Der einstmalige, in der Neuzeit höchste Gletscherstand kann gut an den noch fast vegetationslosen Seitenmoränen abgeschätzt werden. Seit 1850 hat die Eisdicke um teilweise über 100 m abgenommen. Früher waren auch die Eisströme des Oberaletschgletschers und des Mittelaletschgletschers direkt mit dem Grossen Aletschgletscher verbunden.

 

In der Senke zwischen dem Strahlhorn und dem Eggishorn liegt der Märjelensee, der im 19. Jahrhundert beim Gletscherhochstand zu einem Gletscherrandsee aufgestaut wurde. Seine wiederholten plötzlichen Ausbrüche durch Gletscherspalten verursachten immer wieder starke Schadenshochwasser der Massa hin zum Rhonetal.

 

Gegen kurzfristige Klimaschwankungen ist der Gletscher aufgrund seiner grossen Masse relativ immun. Während viele andere Gletscher Ende der 1970er Jahre bis Anfang der 1980er Jahre vorstiessen, reagierte der Aletschgletscher auf die vorübergehende Abkühlung kaum – ebenso wenig wie auf die warmen Jahre seit 1983. Aufgrund der zunehmend extremen Hitze der letzten Jahre zieht er sich aber nun doch – wie alle übrigen Alpengletscher – deutlich verstärkt zurück.

 

Die relative Trägheit in seinen Reaktionen auf Klimaschwankungen macht den Aletschgletscher auch zu einem idealen Untersuchungsobjekt zur Erforschung der Klimaentwicklung im Alpenraum. Die Längenschwankungen des Aletschgletschers in der Vergangenheit dürften sogar eine Rekonstruktion aller grösseren Klimaveränderungen der letzten 3200 Jahre erlauben. Die Bestimmung der verschiedenen Längenstadien des Aletschgletschers in der Vergangenheit erfolgt durch die Radiokohlenstoffdatierung fossiler Baumstämme, die der Gletscher bei einem früheren Vorstoss einmal überfahren haben muss und nun während seines aktuellen Rückzuges wieder freigibt. Der Befund fossiler Böden und von Wurzelwerk garantiert dabei, dass es sich bei dem Fundort auch um den Wuchsstandort des fossilen Baumes handelt. Durch Zählung der Jahresringe der geborgenen Stämme kann sogar der Zeitraum bestimmt werden, während dessen der Aletschgletscher den Fundort nicht erreicht hat. Mit dieser Methode wurde festgestellt, dass der Aletschgletscher bis etwa 1200 v. Chr. um einiges kleiner gewesen sein muss als gegen Ende des 20. Jahrhunderts. Für die Jahre etwa von 1200 bis 1110 v. Chr., 850 bis 750 v. Chr. und 350 bis 250 v. Chr. sind Vorstösse festgestellt worden. Dabei ist der Aletschgletscher von 900 bis 400 v. Chr. jedoch kleiner gewesen als am Ende des 20. Jahrhunderts, genauso wie von etwa 100 v. Chr. bis ins Jahr 250. Um das Jahr 300 ist eine Gletscherlänge vergleichbar der des Höchststandes im 19. Jahrhundert festzustellen.

 

Laut der letzten Studie der Universität Erlangen-Nürnberg (Juni 2020) schmolz die Oberfläche des Grossen Aletschgletscher zwischen den Jahren 2001 und 2014 um mehr als fünf Meter pro Jahr in den unteren Lagen.

 

Tourismus

 

Der Aletschgletscher galt schon früh als besondere Sehenswürdigkeit für Reisende und als willkommenes Untersuchungsobjekt für Forschende. Forschungsstationen gibt es seit 1937 auf dem Jungfraujoch und seit 1976 auf der Riederfurka oberhalb der Riederalp. Durch zahlreiche Luftseilbahnen besonders gut erschlossen ist der Berggrat zwischen dem Riederhorn und dem Eggishorn, der sehr schöne Einblicke in den Zungenbereich und den unteren Teil des Gletschers gewährt. Mit dem Bau der Jungfraubahn auf das Jungfraujoch (auf der Sphinx 3571 m ü. M.) wurde 1912 auch für nicht berggewohnte Leute ein Blick in den oberen Teil des Gletschers ermöglicht.

 

Am Felshang des Faulbergs östlich des Konkordiaplatzes stehen auf 2850 m ü. M. die Konkordiahütten des Schweizer Alpen-Clubs SAC. Sie dienen als wichtiger Etappenort auf der hochalpinen Gletscherroute vom Jungfraujoch oder vom Lötschental in das Gebiet des Grimselpasses.

 

UNESCO-Weltnaturerbe

 

Das Gebiet des Grossen Aletschgletschers ist zusammen mit dem einzigartigen Aletschwald und den umliegenden Regionen seit dem 13. Dezember 2001 Bestandteil des UNESCO-Weltnaturerbes Schweizer Alpen Jungfrau-Aletsch.

 

(Wikipedia)

Jordan Kay at Twitter tweeted to say that "when Apple sends out their standard 'Make Your App Accessible' email", they link to my blog post on accessibility.

 

I asked him to forward me a copy, and sure enough, they do!

 

The full content of the email is quoted below.

 

==============

 

We are excited to hear about your interest in expanding your app's marketability by addressing the needs of individuals with disabilities. There are benefits for developers who choose to enhance their apps to take advantage of accessibility APIs that drive the VoiceOver feature in iOS including....

 

* Make your app stand out from the crowd

* Expand your user base (approximately 1 in 6 individuals in the US have some type of disability, but that doesn't preclude them from wanting to use your app. Even those that don’t identify themselves as disabled can also benefit from accessibility features)

* Improve User Interface testing through automation

* Easy to implement using Apple's developer tools

* Appropriate for almost every app

 

Read Matt Legend Gemmell’s blog post about his experience writing apps that support the visually impaired: Accessibility for iPhone and iPad apps

 

Here are some great resources to help you make your app more accessible. Please note many of these pages require an iDP developer account to access them.

 

1) The best place to start is with our iOS Accessibility page: developer.apple.com/technologies/ios/accessibility.html

 

2) Another great place to learn more about how to program your app for Accessibility is the Accessibility Programming Guide for iOS.

 

3) You can download the WWDC 2011 Session Videos for free by logging into WWDC 2011 Videos using your Apple ID and password. There you will find a few accessibility sessions which include podcasts and a copy of the presentation slides, but additionally, we would like to highlight the one below for iOS:

 

iOS Accessibility

Description: iOS devices are incredibly popular for blind and low vision users, and those with other disabilities. Learn how to make your apps accessible to everyone, as well as how to make apps that are tailored expressly for users with disabilities. This talk will cover new and existing UIAccessibility APIs, and it will provide tips and tricks for making all apps more usable by everyone.

 

4) On our public Apple website, we have a dedicated page discussing our commitment to Accessibility: www.apple.com/accessibility/

 

5) Finally, here are some great examples of apps that take advantage of VoiceOver:

* Science360 for iPad

* NYTimes (iPhone Edition)

* Shazam

* itunes.apple.com/us/app/dictionary.com-dictionary/id36474...

* Inkling

* Urbanspoon for iPad

MTA Chief Accessibility Officer and Senior Advisor Quemuel Arroyo Tours OMNY Call Center on Friday, November 4, 2022

 

MTA

Being the kind of nerd I am, I had to analyse this button panel in the elevator at ARoS art museum in Aarhus, Denmark. I think I was overwhelmed at all the options at first.

 

The typography was hard to read - tiny black letters on the matte steel.

Kudos to all the Braille.

 

But... why were there "close doors" and "open doors" buttons in two spots? I wonder if the lower set was for someone in a wheelchair or someone who was unable to reach the higher buttons? I didn't think about that at the time that I photographed this panel. That could explain it. But that makes the lower buttons look built-in and not built-in. We know what that means. Not designed for inclusion from the beginning!

 

Kudos, too, to the museum for having signs outside the elevator encouraging people who did not have any special needs (wheelchairs, canes, etc.) to use the stairs and leave the elevator to those who really needed it.

Accessible PowerScape 3D play system with shade structures, adaptive whirl and swings, musical instruments, motion activities and much more.

MTA Chair & CEO Janno Lieber, Chief Accessibility Officer Quemuel Arroyo, NYC DOT Commissioner Ydanis Rodriguez, and State Senator Brad Hoylman-Sigal commemorate Disability Pride Month at 66 St-Lincoln Center on Tuesday, Jul 18, 2023 by announcing the rollout of accessibility features at stations around the west side.

 

(Marc A. Hermann / MTA)

Syracuse Village, affordable housing: flats from $100s, this building appears to be eight apartments. (Model homes had those American flags out front.) Note the subtle ramps on the side; even though everything appeared to be slab on grade, some of the market-rate homes seemed to thwart accessibility with weird stairs. link to Stapleton houses for sale page

A MindMap on Web Accessibility

new logo Accessibility

Londrina - Paraná - Brazil