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A fleeting scene that many would walk past without noticing, but I saw how everything could precisely align. One person, one shadow, perfectly framed between the buildings, the red forms, and the open sky. It’s playful, almost surreal, but rooted in something profoundly familiar: an ordinary summer day in Oostende.
What I love about shots like this is how they invite a second look. The geometry, the colour contrasts, the sense of balance all come together to make the everyday feel slightly extraordinary. Photographers often see what others overlook; we pause, notice, and wait for that split second when everything falls into place.
This image sits comfortably in both my 'One Person' and 'Urban Form' series. It’s a moment that feels spontaneous and structured, human and architectural, curious and calm. It’s about looking at the environment differently, and noticing that there’s beauty in the way shapes, architecture, colours, and people can briefly align.
I think we often only see nature on the surface where it looks tangled & disorganized which can seem just too messy & complicated for us to try to understand it or even to make any sense of it all, but if we only take a few extra moments to look closer, a little bit deeper, we will see this vast & beautiful world of creation's flowing symmetry !...I see this alot in trees & plants in the gardens, but I believe this presents itself so perfectly & vividly in frost-scapes...so small & delicate, yet strong & powerful in the most precisely balanced, most amazing tapestry of heavenly designs....yes heavenly because nothing man made could ever possibly come close to this precision of perfection....oh yes there is order...not chaos !
The birds are clearly representations of the "manutara" (the sootie tern - Onychoprion fuscatus), the species in which all Bird-Man competition is focused.
That's the cave:
PS. I will explain the Bird-man cult better when I arrive at Orongo village which is at the top of the volcano in the sequence of photographs.
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The legend of the origin of birds on Easter Island has, like all myths, part of the truth. And it is precisely that Motu Nui, together with the nearby islets Motu Iti and Motu Kao Kao, is the place chosen to nest for most of the seabirds that visit the island.
The manutara, the protagonist of our history, also nested until a few years ago on the motu or islets. This bird has been identified with two kinds of tern and specifically with the sootie tern (Onychoprion fuscatus) who came to the island every spring to lay eggs.
The manutara measures about 40 cm, has the upper part of the head black and the neck and chest white. The upper part of the wings and the body is a dark gray color by which it receives its name.
The meaning of Manutara or Manu Tara is “luck bird” in the Rapanui language. A name probably associated with its arrival coinciding with the end of winter and the beginning of a season with a greater abundance of eggs and greater fishing catches. It is possible that these reasons later made him the center of the bird-man ritual.
Unfortunately, the manutara can no longer honor its name because the bird does not visit Rapa Nui anymore due to the changes suffered in recent years in the fragile ecosystem of the island. However, as if the legend wanted to continue, the tern continues to nest in Motu Motiro Hiva, the uninhabited islet of Sala y Gómez, located 415 km northeast of the island and which is currently a protected marine reserve. Perhaps, in the near future, a new Make Make embodied in a marine biologist will introduce the species back into Rapa Nui.
The cave paintings of Ana Kai Tangata:
*Recreation of the paintings of Ana Kai Tangata | Watercolor of Melinka Pictures Hucke for the book Manu Iri:
Along with your incredible walk inside the cave, I also was able to see the rock art practiced by the natives of Rapa Nui. Yes, as you read, the island has spectacular paintings of red, white and black that adorn your wonderful walk with history and culture.
The paintings that I saw there portray the Apizarrado Tern, a bird that flew over the island for a long time and is considered sacred by the natives to this day.
The rest of the figures are related to ships and frigates that according to the researchers could represent the Europeans who landed on the island (when the Europeans first arrived on the island, they were considered gods and messengers from beyond).
The cave crisis:
Although there is no clarity of the cultural origin of this cave or of what the surprising cave paintings that I saw there mean, there is clarity of something: the seepage of seawater has caused these drawings to disappear and are in danger.
Given the above, CONAF and the government of Chile have implemented an emergency plan to maintain and restore this historical treasure. More and more care is taken with those who visit this natural wonder and there are experts working on its conservation so as not to lose this record of the Rapanui culture.
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Manutara the sacred bird that still lives in the memory of Rapa Nui.
Legend of the origin of the manutara:
Father Sebastián Englert, a Capuchin priest of German origin who lived on Easter Island for more than 30 years, studied its traditions and compiled the myths and legends that their inhabitants told him. Among them is the story of how the birds came to Rapa Nui and says:
“Formerly, when the first settlers arrived in Rapa Nui, there were no birds on the island. At that time there lived a witch or spirit called Hitu in the bay of Hanga Nui, near Tongariki. Hitu had a skull that she kept as treasure in the cavity of a rock. One day, when the sea grew, a great wave dragged the skull and carried it to the coast. Hitu threw herself into the water to retrieve it, but she could not reach it. Although she swam and swam, the skull floated among the waves and moved away.
Thus Hitu continued swimming day and night after the skull. When she was about to give up due to exhaustion, she glimpsed on the horizon the rocks of Motu Motiro Hiva (Sala y Gómez islet). When the skull reached the edge of the islet it became the creator god Make Make. Hitu reached the islet shortly after and both were welcomed by the spirit Haua who lived there because he was destined to care for the numerous seabirds that inhabited the small island.
After a few days off, Make Make ordered Haua to bring him some pairs of birds to take them to Te Pito o Te Henua (which means navel of the world, one of the names by which Easter Island is known). When Make Make arrived on the island, he went to Hanga Nui and climbed the Poike hill where he left the birds free to reproduce, and later returned to his islet.
The following year, Make Make returned to Te Pito o Te Henua to see if the birds had multiplied, but discovered that the inhabitants had eaten all the eggs. Then, furious, he picked up the birds and took them to Vaihú, where he again released them to nest there. But the same thing happened in Vaihú, and the natives ate the eggs again. The following year, Make Make, desperate, took the birds to Vai Atare, a place located on the edge of the crater of the Rano Kau volcano. There finally, the villagers left a nest with only one egg, from which the first manutara bird of the island was born.
But Make Make, to better ensure the breeding of the birds, returned again next year and left the birds on the Motu Nui islet in front of the Rano Kau volcano. There the birds multiplied in large numbers due to the difficult access of the small islet.
Later, Make Make, allowed the islanders to be able to collect the eggs of the birds in a certain period of the year, punishing those who collected them in times not allowed. In order not to provoke the wrath of God, the Ariki (king) and the priests decided to declare the eggs as Tapu (or taboo, that is, forbidden) during the closed periods. This taboo allowed the protection and development of seabirds in Rapa Nui”.
The cult of the manutara:
The importance of birds in the Rapanui culture is manifested through the numerous allusions to birds found in prints, paintings, sculptures and legends throughout its history.
This great relevance makes sense on a remote and isolated island like Rapa Nui, in which there were no large mammals or reptiles, and in which birds were the only living beings close to humans, which also provided an interesting source of protein in shape of meat and eggs, at the same time as feathers and bones to make tools and decorative objects.
Seabirds also indicate the location of shoals of fish when they fly over the surface of the sea in search of food, which was extremely useful to a people who based much of their livelihood on fishing.
It is not strange, therefore, that a religious cult arose around birds. There was a belief that the birds had a mystical relationship with the gods, and especially the seabirds that united the earth, the sea and the sky. Each year they came from “the hereafter”, an unknown land carrying messages from ancestors and spirits.
However, it is unknown exactly how the cult of the manutara was born and the bird man competition. A cult that replaced the veneration of the Moai statues with a new belief whose main ritual was carried out in spring coinciding with the migration of seabirds to nest in Motu Nui.
Floor painting at the entrance of the U-Bahn station Hauptwache. More precisely at the entrance of the MOMEM (for Museum Of Modern Electronic Music, on account of MOMA being already taken) that opened there earlier this year, replacing the Kindermuseum.
Minolta XD7 and Rokkor-HG 1:2.8 f=35mm, Agfa RSX II developped by the DM Fotoparadies and digitalized using kit zoom with macro rings.
Thank you everyone for your visits, faves and comments, they are always appreciated :)
"what matters precisely is this; the unspoken at the edge of the spoken." -virginia woolf.
happy tuesday, everyone!
March 25, 2015 - explore, #45.
Villa Victoria is a romantic French-style mansion built in 1911 and visited every summer by illustrious figures of the Spanish society, such as the famous opera singer Lucrezia Bori. It was precisely the majesty of the building what favored that during the Civil War it was used as a library. Currently a fence of meticulous work protects the inside. In the garden of palm trees, araucaria and Mediterranean shrubs, two lampposts and a classical sculpture escort the entrance to the house.
Villa Victoria es una casa palaciega romántica y afrancesada construida en 1911 y que fue visitada, verano tras verano, por ilustres personajes de la sociedad española, como la famosísima cantante de ópera Lucrecia Bori.
Fue precisamente la majestuosidad de la construcción lo que propició que durante la Guerra Civil se utilizara como biblioteca. En el jardín de palmeras, araucarias y arbustos mediterráneos, dos farolas y una escultura clásica escoltan la entrada a la casa.
Les Villes de Benicàssim
Benicàssim (Castelló de La Plana/ Spain).
Carefully carried across the ocean, precisely hung, then accidentally hit by a water-baloon!! My mosaic effort to restore it!
walet waterfall is located on Mount Salak, Bogor, West Java, Indonesia. Precisely in the area of Ciasihan Village, Pamijahan District.
Hello!!!!!
One shot from the past weekend, me and the "Gang" went to a place in Portugal called Pego do Altar more precisely at Santa Susana village, unfortunately our country is suffering from the dry weather and this is just one example of that, in this image in the very recent past it was full of water and now this is the image that you are seeing.... dry, completely dry ... that is one sad memory ... I did some Drone photoage and some film , please stay tuned to my youtube channel ( www.youtube.com/channel/UC7cq5JYZNqzAAukT1hTwfrg? ) or my web site ( www.jorgecanelas.com ) for the Vlog.
All the best, bye for now ...
Nikon D800
Nikon 16-35 mm f/4 ED VR
LEE Filter ND 0.9 HE
LEE Filter Full ND 0.9 Pro Glass
LEE Filter Field Pouch
LOWEPRO Whistler BP 450 AW
LOWEPRO Drone Guard BP 400
FLM CB30 - L3 PRO
FLM CB 43 FTR
FLM L - Bracket
Duesenberg Model J Beverly by Murphy
Due to the fact that I neglected to read the display placard in front of this fine Duesenberg, I cannot say precisely the model year: 1932, 1933, 1934, 1935 or 1936. Regardless, the model years did not vary considerably……..nor did, nor has, the original asking price or today’s “auction price”.
Many of the most beautiful bodies for Duesenberg were created not by private coachbuilders, but by Gordon Miller Buehrig, who was hired in 1929 as Duesenberg’s chief body designer. Buehrig would enjoy one of the richest and most successful careers of any American automotive designer. Following his work for Duesenberg, he would create the 1935 Auburn 851 Speedster for corporate sibling Auburn Automobile Company, as well as the mold-breaking Cord 810 and 812. His work was dashing, ahead of its time, and distinguished by beautifully tailored proportions and an eye for fine detail. He was a natural designer who truly saw cars as art, as evidenced by the title of his autobiography, Rolling Sculpture.
THE BEVERLY
One of Buehrig’s classic designs for the Model J, and among the designer’s proudest creations, was a sedan called the Beverly. Originally created for the Chicago Auto Salon of 1930, it was designed as a formal car for city use; it would have sporty, close-coupled proportions and aircraft-inspired design features, but it would also be suitable for chauffeured use. In addition, it would have a large trunk, should the owner wish to take it outside of the city for extended touring purposes.
The design’s distinguishing features were a dramatic, slanted windshield that was framed on the sides by small, triangular panes and a roofline that “dropped” in a vee between the side windows, with both serving to lighten the otherwise formal appearance of the car. Buehrig claimed that he borrowed the “drop” in the roof from the convertible tops of cars designed by Paris coachbuilders Hibbard & Darrin, but he was able to “crisp” the design by using metal frames and a fixed roof, keeping the lines well defined.
The interior was equally impressive. The rear seat was split into two cozy armchairs, by means of a fixed center armrest. “In the cabinet behind the front seat,” Buehrig noted, “we installed a radio, a glove box, and a rear seat instrument panel. Since the Duesenberg Model J was the only American car capable of 100 miles per hour, I reasoned the rear seat passenger would enjoy a speedometer.”
A total of 10 Beverlys were produced, with eight of them by the Walter M. Murphy Company, of Pasadena, California, and an additional pair by the Rollston Company, of New York City. In typical Duesenberg style, no two were alike, with each commission as unique as its fascinating original owner.
rmsothebys.com/en/auctions/ny13/new-york---art-of-the-aut...
Powertrain
Engine type ————————--————- Lycoming / Duesenberg J Straight 8
Displacement ———————————————- 6.9 l (421 ci)
Power ——————————————— 269 ps (265 bhp / 198 kw) @ 4200 rpm
Torque ———————————————— 507 Nm (374 lb-ft) @ 2000 rpm
Power / liter ——————————————————— 39 ps (38 hp)
Transmission ——————————————— Warner Gear 3 speed Manual
Layout ————————————------—— front engine, rear wheel drivePowertrain
Years —————————————----—————— 1932-1937
Body Style ——————————————————- Sedan
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The Supercharged SJ Model
The supercharged version, often referred to as "SJ", was reputed to do 104 miles per hour (167 km/h) in second and have a top speed of 135–140 mph (217–225 km/h) in third gear. Zero-to-60 mph (97 km/h) times of around eight seconds and 0–100 mph (0–161 km/h) in 17 seconds were reported for the SJ in spite of the unsynchronized transmissions, at a time when even the best cars of the era were not likely to reach 100 mph (160 km/h). Duesenberg’s generally weighed around two and a half tons; up to three tons was not unusual, considering the wide array of custom coachwork available. The wheelbase was 142.5 in (362 cm).
Source: www.rmw.lv/car/de/model-sj-beverly-by-murphy
Hope you enjoy my friends................
PS: If anyone is questioning why this picture is in the "Pursuing the Posh" Group it is because I was invited. I can tell you one thing ladies, if you were to step into this elegant classic wearing your slinky satin black evening gown, you would be "Pursuing the posh"................
Wahnbachtalsperre, Siegburg.
In summer 2008, the bigger part of the water in this reservoir was let out in order to refurbish the dam. After almost precisely 50 year, streets, bridges and remains of houses re-emerged.
Im Sommer 2008 wurde ein großer Teil des Wassers aus dieser Talsperre abgelassen, weil die Staumauer saniert werden musste. Nach fast genau 50 Jahren tauchten für einige Monate Straßen, Brücken und Häuserreste wieder auf.
The city of Petra, capital of the Nabataean Arabs, is one of the most famous archaeological sites in the world.
t is not known precisely when Petra was built, but the city began to prosper as the capital of the Nabataean Empire from the 1st century BC, which grew rich through trade in frankincense, myrrh, and spices.
Petra was later annexed to the Roman Empire and continued to thrive until a large earthquake in 363 AD destroyed much of the city in the 4th century AD.
The earthquake combined with changes in trade routes, eventually led to the downfall of the city which was ultimately abandoned.
Petra is also known as the rose-red city, a name it gets from the wonderful colour of the rock from which many of the city’s structures were carved.
The Nabataeans buried their dead in intricate tombs that were cut out of the mountain sides and the city also had temples, a theater, and following the Roman annexation and later the Byzantine influence, a colonnaded street and churches.
In addition to the magnificent remains of the Nabataean city, human settlement and land use for over 10,000 years can be traced in Petra, where great natural, cultural, archaeological and geological features merge.
On December 6, 1985, Petra was designated a World Heritage Site.
In the village of Sarnath and precisely in this stupa, Buddha preached his famous sermon:" Sermon in the deer park".
When I went to Germany and more precisely in the city of Stuttgart, I took the opportunity to discover this city that I did not know yet. Today I will introduce you to one of the main squares in Stuttgart, its finance ministry. An imposing and beautiful structure truncated in the middle of greenery. This "palace" was perfectly symmetrical, so I tried to transcribe this one as well as the imposing size of this structure.
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Canon EOS 5D Mark III
Canon EF 16-35 mm f/4.0 L IS USM
Tripod Manfrotto MT055XPRO3
Post processing Lightroom and Photoshop.
LOTD ✨
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The Hermit Card in the Tarot can be seen as Jigsaw Piece and The Hermit holds a light that can illuminate the place for this Jigsaw Piece to fit in. It maybe that The Hermit always finds a place at least a place to pause awhile before continuing. The light of the Lamp is The Star and expression of the yearning to find and the striving to fulfil self and to be the individual that we can be. Tarot Archetype and Ever Living Avatar came together to do more than putting the best foot forward. In photographing both feet on the ground the not a step further ultimate ideal was found.
© PHH Sykes 2024
phhsykes@gmail.com
Schweiz / Berner Oberland - Eiger
seen from Fallbodensee
The Eiger (German pronunciation: [ˈaɪ̯ɡɐ]) is a 3,967-metre (13,015 ft) mountain of the Bernese Alps, overlooking Grindelwald and Lauterbrunnen in the Bernese Oberland of Switzerland, just north of the main watershed and border with Valais. It is the easternmost peak of a ridge crest that extends across the Mönch to the Jungfrau at 4,158 m (13,642 ft), constituting one of the most emblematic sights of the Swiss Alps. While the northern side of the mountain rises more than 3,000 m (10,000 ft) above the two valleys of Grindelwald and Lauterbrunnen, the southern side faces the large glaciers of the Jungfrau-Aletsch area, the most glaciated region in the Alps. The most notable feature of the Eiger is its nearly 1,800-metre-high (5,900 ft) north face of rock and ice, named Eiger-Nordwand, Eigerwand or just Nordwand, which is the biggest north face in the Alps.] This huge face towers over the resort of Kleine Scheidegg at its base, on the eponymous pass connecting the two valleys.
The first ascent of the Eiger was made by Swiss guides Christian Almer and Peter Bohren and Irishman Charles Barrington, who climbed the west flank on August 11, 1858. The north face, the "last problem" of the Alps, considered amongst the most challenging and dangerous ascents, was first climbed in 1938 by an Austrian-German expedition.The Eiger has been highly publicized for the many tragedies involving climbing expeditions. Since 1935, at least 64 climbers have died attempting the north face, earning it the German nickname Mordwand, literally "murder(ous) wall"—a pun on its correct title of Nordwand (North Wall).
Although the summit of the Eiger can be reached by experienced climbers only, a railway tunnel runs inside the mountain, and two internal stations provide easy access to viewing-windows carved into the rock face. They are both part of the Jungfrau Railway line, running from Kleine Scheidegg to the Jungfraujoch, between the Mönch and the Jungfrau, at the highest railway station in Europe. The two stations within the Eiger are Eigerwand (behind the north face) and Eismeer (behind the south face), at around 3,000 metres. The Eigerwand station has not been regularly served since 2016.
Etymology
The first mention of Eiger, appearing as "mons Egere", was found in a property sale document of 1252, but there is no clear indication of how exactly the peak gained its name. The three mountains of the ridge are commonly referred to as the Virgin (German: Jungfrau – translates to "virgin" or "maiden"), the Monk (Mönch), and the Ogre (Eiger; the standard German word for ogre is Oger). The name has been linked to the Latin term acer, meaning "sharp" or "pointed".
Geographic setting and description
The Eiger is located above the Lauterbrunnen Valley to the west and Grindelwald to the north in the Bernese Oberland region of the canton of Bern. It forms a renowned mountain range of the Bernese Alps together with its two companions: the Jungfrau (4,158 m (13,642 ft)) about 5.6 kilometres (3.5 mi) southwest of it and the Mönch (4,107 m (13,474 ft)) about in the middle of them. The nearest settlements are Grindelwald, Lauterbrunnen (795 m (2,608 ft)) and Wengen (1,274 m (4,180 ft)). The Eiger has three faces: north (or more precisely NNW), east (or more precisely ESE), and west (or more precisely WSW). The northeastern ridge from the summit to the Ostegg (lit.: eastern corner, 2,709 m (8,888 ft)), called Mittellegi, is the longest on the Eiger. The north face overlooks the gently rising Alpine meadow between Grindelwald (943 m (3,094 ft)) and Kleine Scheidegg (2,061 m (6,762 ft)), a mountain railways junction and a pass, which can be reached from both sides, Grindelwald and Lauterbrunnen/Wengen – by foot or train.
Politically, the Eiger (and its summit) belongs to the Bernese municipalities of Grindelwald and Lauterbrunnen. The Kleine Scheidegg (literally, the small parting corner) connects the Männlichen-Tschuggen range with the western ridge of the Eiger. The Eiger does not properly form part of the main chain of the Bernese Alps, which borders the canton of Valais and forms the watershed between the Rhine and the Rhône, but constitutes a huge limestone buttress, projecting from the crystalline basement of the Mönch across the Eigerjoch. Consequently, all sides of the Eiger feed finally the same river, namely the Lütschine.
Eiger's water is connected through the Weisse Lütschine (the white one) in the Lauterbrunnen Valley on the west side (southwestern face of the Eiger), and through the Schwarze Lütschine (the black one) running through Grindelwald (northwestern face), which meet each other in Zweilütschinen (lit.: the two Lütschinen) where they form the proper Lütschine. The east face is covered by the glacier called Ischmeer, (Bernese German for Ice Sea), which forms one upper part of the fast-retreating Lower Grindelwald Glacier. These glaciers' water forms a short creek, which is also confusingly called the Weisse Lütschine, but enters the black one already in Grindelwald together with the water from the Upper Grindelwald Glacier. Therefore, all the water running down the Eiger converges at the northern foot of the Männlichen (2,342 m (7,684 ft)) in Zweilütschinen (654 m (2,146 ft)), about 10 kilometres (6.2 mi) northwest of the summit, where the Lütschine begins its northern course to Lake Brienz and the Aare (564 m (1,850 ft)).
Although the north face of the Eiger is almost free of ice, significant glaciers lie at the other sides of the mountain. The Eiger Glacier flows on the southwestern side of the Eiger, from the crest connecting it to the Mönch down to 2,400 m (7,900 ft), south of Eigergletscher railway station, and feeds the Weisse Lütschine through the Trümmelbach. On the east side, the Ischmeer–well visible from the windows of Eismeer railway station–flows eastwards from the same crest then turns to the north below the impressive wide Fiescherwand, the north face of the Fiescherhörner triple summit (4,049 m (13,284 ft)) down to about 1,600 m (5,200 ft) of the Lower Grindelwald Glacier system.
The massive composition of the Eiger, Mönch, and Jungfrau constitutes an emblematic sight of the Swiss Alps and is visible from many places on the Swiss Plateau and the Jura Mountains in the northwest. The higher Finsteraarhorn (4,270 m (14,010 ft)) and Aletschhorn (4,190 m (13,750 ft)), which are located about 10 kilometres (6.2 mi) to the south, are generally less visible and situated in the middle of glaciers in less accessible areas. As opposed to the north side, the south and east sides of the range consist of large valley glaciers extending for up to 22 kilometres (14 mi), the largest (beyond the Eiger drainage basin) being those of Grand Aletsch, Fiesch, and Aar Glaciers, and is thus uninhabited. The whole area, the Jungfrau-Aletsch protected area, comprising the highest summits and largest glaciers of the Bernese Alps, was inscribed as a UNESCO World Heritage Site in 2001.
In July 2006, a piece of the Eiger, amounting to approximately 700,000 cubic metres of rock, fell from the east face. As it had been noticeably cleaving for several weeks and fell into an uninhabited area, there were no injuries and no buildings were hit.
Climbing history
While the summit was reached without much difficulty in 1858 by a complex route on the west flank, the battle to climb the north face has captivated the interest of climbers and non-climbers alike. Before it was successfully climbed, most of the attempts on the face ended tragically and the Bernese authorities even banned climbing it and threatened to fine any party that should attempt it again. But the enthusiasm which animated the young talented climbers from Austria and Germany finally vanquished its reputation of unclimbability when a party of four climbers successfully reached the summit in 1938 by what is known as the "1938" or "Heckmair" route.
The climbers that attempted the north face could be easily watched through the telescopes from the Kleine Scheidegg, a pass between Grindelwald and Lauterbrunnen, connected by rail. The contrast between the comfort and civilization of the railway station and the agonies of the young men slowly dying a short yet uncrossable distance away led to intensive coverage by the international media.
After World War II, the north face was climbed twice in 1947, first by a party of two French guides, Louis Lachenal and Lionel Terray, then by a Swiss party consisting of H. Germann, with Hans and Karl Schlunegger.
First ascent
In 1857, a first recorded attempt was made by Christian Almer, Christian Kaufmann, Ulrich Kaufmann guiding the Austrian alpinist Sigismund Porges. They did manage the first ascent of neighboring Mönch instead. Porges, however, successfully made the second ascent of the Eiger in July 1861 with the guides Christian Michel, Hans and Peter Baumann.
The first ascent was made by the western flank on August 11, 1858 by Charles Barrington with guides Christian Almer and Peter Bohren. On the previous afternoon, the party walked up to the Wengernalp hotel. From there they started the ascent of the Eiger at 3:30 a.m. Barrington describes the route much as it is followed today, staying close to the edge of the north face much of the way. They reached the summit at about noon, planted a flag, stayed for some 10 minutes and descended in about four hours. Barrington describes the reaching of the top, saying, "the two guides kindly gave me the place of first man up." After the descent, the party was escorted to the Kleine Scheidegg hotel, where their ascent was confirmed by observation of the flag left on the summit. The owner of the hotel then fired a cannon to celebrate the first ascent. According to Harrer's The White Spider, Barrington was originally planning to make the first ascent of the Matterhorn, but his finances did not allow him to travel there as he was already staying in the Eiger region.
Mittellegi ridge
Although the Mittellegi ridge had already been descended by climbers (since 1885) with the use of ropes in the difficult sections, it remained unclimbed until 1921. On the 10th of September of that year, Japanese climber Yuko Maki, along with Swiss guides Fritz Amatter, Samuel Brawand and Fritz Steuri made the first successful ascent of the ridge. The previous day, the party approached the ridge from the Eismeer railway station of the Jungfrau Railway and bivouacked for the night. They started the climb at about 6:00 a.m. and reached the summit of the Eiger at about 7:15 p.m., after an over 13 hours gruelling ascent. Shortly after, they descended the west flank. They finally reached Eigergletscher railway station at about 3:00 a.m. the next day.
Attempts on the north face
1935
In 1935, two young German climbers from Bavaria, Karl Mehringer and Max Sedlmeyer, arrived at Grindelwald to attempt the ascent of the north face. After waiting some time for the weather to improve, they set off, reaching the height of the Eigerwand station before stopping for their first bivouac. The following day, facing greater difficulties, they gained little height. On the third day, they made hardly any vertical gain. That night, the weather deteriorated, bringing snow and low cloud that shrouded the mountain from the observers below. Avalanches began to sweep the face. Two days later, the weather briefly cleared, and the two men were glimpsed a little higher and about to bivouac for the fifth night, before clouds descended again. A few days later, the weather finally cleared, revealing a completely white north face.: 225 Weeks later, the German World War I ace Ernst Udet went searching for the missing men with his aircraft, eventually spotting one of them frozen to death in what became known as the "Death Bivouac". Sedlmeyer's body was found at the foot of the face the following year by his brothers Heinrich and Martin Meier, who were part of a group looking for the victims of the 1936 climbing disaster. Mehringer's remains were found in 1962 by Swiss climbers below the "Flat Iron" (Bügeleisen) at the lefthand end of the second ice field.
1936
The next year ten young climbers from Austria and Germany came to Grindelwald and camped at the foot of the mountain. Before their attempts started one of them was killed during a training climb, and the weather was so bad during that summer that, after waiting for a change and seeing none on the way, several members of the party gave up. Of the four that remained, two were Bavarians, Andreas Hinterstoisser and Toni Kurz, and two were Austrians, Willy Angerer and Edi Rainer. When the weather improved they made a preliminary exploration of the lowest part of the face. Hinterstoisser fell 37 metres (121 ft) but was not injured. A few days later the four men finally began the ascent of the face. They climbed quickly, but on the next day, after their first bivouac, the weather changed; clouds came down and hid the group to the observers. They did not resume the climb until the following day, when, during a break, the party was seen descending, but the climbers could be seen only intermittently from the ground. The group had no choice but to retreat, since Angerer had suffered serious injuries from falling rock. The party became stuck on the face when they could not recross the difficult Hinterstoisser Traverse, from which they had taken the rope they had first used to climb it. The weather then deteriorated for two days. They were ultimately swept away by an avalanche, which only Kurz survived, hanging on a rope. Three guides started on an extremely perilous rescue attempt. They failed to reach him but came within shouting distance and learned what had happened. Kurz explained the fate of his companions: one had fallen down the face, another was frozen above him, and the third had fractured his skull in falling and was hanging dead on the rope.
In the morning the three guides came back, traversing the face from a hole near the Eigerwand station and risking their lives under incessant avalanches. Toni Kurz was still alive but almost helpless, with one hand and one arm completely frozen. Kurz hauled himself off the cliff after cutting loose the rope that bound him to his dead teammate below and climbed back onto the face. The guides were not able to pass an unclimbable overhang that separated them from Kurz. They managed to give him a rope long enough to reach them by tying two ropes together. While descending, Kurz could not get the knot to pass through his carabiner. He tried for hours to reach his rescuers who were only a few metres below him. Then he began to lose consciousness. One of the guides, climbing on another's shoulders, was able to touch the tip of Kurz's crampons with his ice-axe but could not reach higher. Kurz was unable to descend further and, completely exhausted, died slowly.
1937
An attempt was made in 1937 by Mathias Rebitsch and Ludwig Vörg. Although the attempt was unsuccessful, they were nonetheless the first climbers who returned alive from a serious attempt on the face. They started the climb on 11 August and reached a high point of a few rope lengths above Death Bivouac. A storm then broke and after three days on the wall they had to retreat. This was the first successful withdrawal from a significant height on the wall.
First ascent of the north face
The north face was first climbed on July 24, 1938 by Anderl Heckmair, Ludwig Vörg, Heinrich Harrer and Fritz Kasparek in a German–Austrian party. The party had originally consisted of two independent teams: Harrer (who did not have a pair of crampons on the climb) and Kasparek were joined on the face by Heckmair and Vörg, who had started their ascent a day later and had been helped by the fixed rope that the lead team had left across the Hinterstoisser Traverse. The two groups, led by the experienced Heckmair, decided to join their forces and roped together as a single group of four. Heckmair later wrote: "We, the sons of the older Reich, united with our companions from the Eastern Border to march together to victory."
The expedition was constantly threatened by snow avalanches and climbed as quickly as possible between the falls. On the third day a storm broke and the cold was intense. The four men were caught in an avalanche as they climbed "the Spider," the snow-filled cracks radiating from an ice-field on the upper face, but all possessed sufficient strength to resist being swept off the face. The members successfully reached the summit at four o'clock in the afternoon. They were so exhausted that they only just had the strength to descend by the normal route through a raging blizzard.
Other notable events
1864 (Jul 27): Fourth ascent, and first ascent by a woman, Lucy Walker, who was part of a group of six guides (including Christian Almer and Melchior Anderegg) and five clients, including her brother Horace Walker[
1871: First ascent by the southwest ridge, 14 July (Christian Almer, Christian Bohren, and Ulrich Almer guiding W. A. B. Coolidge and Meta Brevoort).
1890: First ascent in winter, Ulrich Kaufmann and Christian Jossi guiding C. W. Mead and G. F. Woodroffe.
1924: First ski ascent and descent via the Eiger glacier by Englishman Arnold Lunn and the Swiss Fritz Amacher, Walter Amstutz and Willy Richardet.
1932: First ascent of the northeast face ("Lauper route") by Hans Lauper, Alfred Zürcher, Alexander Graven and Josef Knubel
1970: First ski descent over the west flank, by Sylvain Saudan.
1986: Welshman Eric Jones becomes the first person to BASE jump from the Eiger.
1988: Original Route (ED2), north face, Eiger (3970m), Alps, Switzerland, first American solo (nine and a half hours) by Mark Wilford.
1991: First ascent, Metanoia Route, North Face, solo, winter, without bolts, Jeff Lowe.
1992 (18 July): Three BMG/UIAGM/IFMGA clients died in a fall down the West Flank: Willie Dunnachie; Douglas Gaines; and Phillip Davies. They had ascended the mountain via the Mittellegi Ridge.
2006 (14 June): François Bon and Antoine Montant make the first speedflying descent of the Eiger.
2006 (15 July): Approximately 700,000 cubic metres (20 million cubic feet) of rock from the east side collapses. No injuries or damage were reported.
2015 (23 July): A team of British Para-Climbers reached the summit via the West Flank Route. The team included John Churcher, the world's first blind climber to summit the Eiger, sight guided by the team leader Mark McGowan. Colin Gourlay enabled the ascent of other team members, including Al Taylor who has multiple sclerosis, and the young autistic climber Jamie Owen from North Wales. The ascent was filmed by the adventure filmmakers Euan Ryan & Willis Morris of Finalcrux Films.
Books and films
The 1959 book The White Spider by Heinrich Harrer describes the first successful ascent of the Eiger north face.
The Climb Up To Hell, 1962, by Jack Olson, an account of the ill-fated 1957 attempted climb of the north face by an Italian four-man team and the dramatic rescue of the sole survivor mounted by an international all-volunteer group of rescuers.
Eiger Direct, 1966, by Dougal Haston and Peter Gillman, London: Collins, also known as Direttissima; the Eiger Assault
The 1971 novel The Ice Mirror by Charles MacHardy describes the second attempted ascent of the Eiger north face by the main character.
The 1972 novel The Eiger Sanction is an action/thriller novel by Rodney William Whitaker (writing under the pseudonym Trevanian), based around the climbing of the Eiger. This was then made into the 1975 film The Eiger Sanction starring Clint Eastwood and George Kennedy. The Eiger Sanction film crew included very experienced mountaineers (e.g., Mike Hoover, Dougal Haston, and Hamish MacInnes, see Summit, 52, Spring 2010) as consultants, to ensure accuracy in the climbing footage, equipment and techniques.
The Eiger, 1974, by Dougal Haston, London: Cassell
The 1982 book Eiger, Wall of Death by Arthur Roth is an historical account of first ascents of the north face.
The 1982 book Traverse of The Gods by Bob Langley is a World War II spy thriller where a group escaping from Nazi Germany is trapped and the only possible exit route is via the Nordwand.
Eiger, 1983, a documentary film by Leo Dickinson of Eric Jones' 1981 solo ascent of the north face.
Eiger Dreams, 1990, a collection of essays by Jon Krakauer, begins with an account of Krakauer's own attempt to climb the north face.
Eiger: The Vertical Arena (German edition, 1998; English edition, 2000), edited by Daniel Anker, a comprehensive climbing history of the north face authored by 17 climbers, with numerous photographs and illustrations.
The IMAX film The Alps features John Harlin III's climb up the north face in September 2005. Harlin's father, John Harlin II, set out 40 years earlier to attempt a direct route (the direttissima) up the 6,000-foot (1,800 m) face, the so-called "John Harlin route". At 1300 m, his rope broke, and he fell to his death. Composer James Swearingen created a piece named Eiger: Journey to the Summit in his memory.
The 2007 docu/drama film The Beckoning Silence featuring mountaineer Joe Simpson, recounting—with filmed reconstructions—the ill-fated 1936 expedition up the north face of the Eiger and how Heinrich Harrer's book The White Spider inspired him to take up climbing. The film followed Simpson's eponymous 2003 book. Those playing the parts of the original climbing team were Swiss mountain guides Roger Schäli (Toni Kurz), Simon Anthamatten (Andreas Hinterstoisser), Dres Abegglen (Willy Angerer) and Cyrille Berthod (Edi Rainer). The documentary won an Emmy Award the subsequent year.
The 2008 German historical fiction film Nordwand is based on the 1936 attempt to climb the Eiger north face. The film is about the two German climbers, Toni Kurz and Andreas Hinterstoisser, involved in a competition with an Austrian duo to be the first to scale the north face of Eiger.
The 2010 documentary Eiger: Wall of Death by Steve Robinson.
(Wikipedia)
Der Eiger ist ein Berg in den Berner Alpen mit einer Höhe von 3967 m ü. M. Er ist dem Hauptkamm der Berner Alpen etwas nördlich vorgelagert und steht vollständig auf dem Territorium des Schweizer Kantons Bern. Zusammen mit Mönch und Jungfrau, deren Gipfel auf der Grenze zum Kanton Wallis liegen, dominiert der Eiger die Landschaft des zentralen Berner Oberlandes. Die etwa 3000 Meter über dem Tal aufragenden Nordflanken dieser Berge stellen die Schauseite einer der bekanntesten je als ein «Dreigestirn» bezeichneten Gipfel-Dreiergruppen in den Alpen dar.
Insbesondere die Nordwand des Eigers fasziniert sowohl Bergsteiger als auch Alpin-Laien. Durch dramatische Begehungsversuche und gelungene Begehungen dieser Wand wurde der Eiger weltweit bekannt und immer wieder ins Blickfeld der Öffentlichkeit gerückt – nicht zuletzt, da die gesamte Wand von Grindelwald und der Bahnstation Kleine Scheidegg aus einsehbar ist. Die Jungfraubahn mit ihrem Tunnel durch den Eigerfels ist seit ihrer Eröffnung im Jahr 1912 ein Touristenmagnet.
Namensherkunft
Die erste urkundliche Erwähnung des Eigers stammt aus dem Jahre 1252 – dies ist die zweitfrüheste urkundliche Erwähnung eines Schweizer Bergs nach dem Bietschhorn (1233). Am 24. Juli 1252 wurde in einer Verkaufsurkunde zwischen Ita von Wädiswyl und der Propstei Interlaken ein Grundstück mit den Worten «ad montem qui nominatur Egere» (dt.: Bis zum Berg, der Eiger genannt wird) abgegrenzt. Ein halbes Jahrhundert später wird der Eiger in einem Belehnungsbrief erstmals in deutscher Sprache erwähnt: «under Eigere».
Für die Herkunft des Namens gibt es drei gängige Erklärungen. Eine erste ist der althochdeutsche Name Agiger oder Aiger, wie der erste Siedler unterhalb des Eigers geheissen haben soll. Der Berg über dessen Weiden wurde deshalb Aigers Geissberg oder auch nur Geissberg genannt. Hieraus entwickelten sich dann im Laufe der Zeit die direkten Vorgänger der heutigen Bezeichnung. Die Herkunft des Namens könnte auch von dem lateinischen Wort acer kommen, woraus sich im Französischen aigu entwickelte. Beide Worte haben die Bedeutung scharf beziehungsweise spitz – in Anlehnung an die Form des Eigers. Die dritte Erklärung stammt von der früher gebräuchlichen Schreibweise Heiger, was sich aus dem Dialektausdruck «dr hej Ger» entwickelt haben könnte (hej bedeutet hoch, Ger war ein germanischer Wurfspiess). Wiederum wäre hier die Form des Eigers ausschlaggebend für seine Bezeichnung.
Im Zusammenhang mit dem Eiger wird auch des Öfteren die Namensähnlichkeit mit dem Oger, einem menschenähnlichen Unhold, genannt. In Anlehnung an das Dreigestirn «Eiger–Mönch–Jungfrau» gibt es die Erzählung, der Unhold Eiger wolle seine lüsternen Pranken auf die Jungfrau legen, woran er aber vom fröhlichen Mönch gehindert werde. Zu dieser Geschichte sind in Grindelwald alte Karikaturen und neuere Postkarten zu kaufen.
Lage und Umgebung
Der Eiger erhebt sich direkt südwestlich von Grindelwald (Amtsbezirk Interlaken). Die bekannte Nordwand ist genaugenommen eine Nordwestwand. Neben dieser existiert in der berühmten «Eiger-Nordansicht» auch noch die Nordostwand. Sie bildet die Basis für den scharfen Mittellegigrat, der vom Unteren Grindelwaldgletscher zum Gipfel zieht. Auf der gegenüberliegenden Seite begrenzt der Westgrat die Nordwand. Ihm folgt die Westflanke, in welcher sich der Eigergletscher und der Klein Eiger befinden. An diesen schliessen sich der Südwestgrat und noch ein Stück östlicher der Südgrat an, der wiederum die Südostwand begrenzt, welche bis zum Mittellegigrat reicht. Südöstlich des Eigers liegt der Grindelwald-Fieschergletscher.
In der Umgebung des Eigers befinden sich einige Viertausender des Aarmassivs. Im Osten ist er umgeben von Schreckhorn (4078 m ü. M.) und Lauteraarhorn (4042 m ü. M.), im Südosten vom Grossen Fiescherhorn (4049 m ü. M.), und im Südwesten ist der Mönch (4107 m ü. M.) durch das Nördliche und Südliche Eigerjoch vom Eiger getrennt. Zusammen mit dem Mönch und der Jungfrau (4158 m ü. M.) bildet der Eiger das «Dreigestirn», bei dem der Eiger den nordöstlichen und die Jungfrau den südwestlichen Endpunkt bildet. Entgegen der steil abfallenden Nordseite des Berges befindet sich im Süden des Eigers die Hochfläche und Gletscherwelt der Berner Alpen. Seit Ende 2001 gehört der Eiger zum Gebiet des UNESCO-Weltnaturerbes Schweizer Alpen Jungfrau-Aletsch.
Geologie
Der Eiger ist ein Teil des helvetischen Systems, das im Grossraum um den Thunersee die Decken des Alpennordrandes bildet. In einer späten Phase der alpidischen Gebirgsfaltung wurden die helvetischen Kalk-Sedimente von ihrer kristallinen Basis abgeschürft und in Form einer Abscherungsdecke nach Nordwesten verschoben. Während des Faltungsprozesses in der Alpenentstehung brachen die Kalkbänke auf und Kluft- sowie Faltensysteme entstanden, die später mit ausgefälltem Calcit geschlossen wurden. Wichtigste Bestandteile der Sedimente sind der Schrattenkalk der Kreidezeit und der Malmkalk. Als Füll- und Schmiermaterial dienten Mergel und Tonschiefer.
Die klar erkennbare Faltung des Helvetikums mit seinen gebänderten, plattigen Kalkschichten zeigt sich auch am Eiger. Das Massiv des Eigers besteht komplett aus Kalk der helvetischen Zone und schliesst die Flyschschichten und die Molasse des Grindelwaldbeckens steil nach Süden hin ab. Weil der Talkessel von Grindelwald so reich gegliedert ist, finden hier die verschiedensten Tiere einen Lebensraum.[6] Südlich des Eigers schliesst sich das Aarmassiv mit seinem Innertkirchner-Lauterbrunner-Kristallin an. Teilweise hat sich dieses über die Sedimente des Eiger geschoben. Im Bereich des Mönchs treffen die Sedimente auf Altkristallin. Die typischen Gesteine des helvetischen Systems im Bereich des Eigers entstanden während des Jura, dem mittleren Zeitabschnitts des Mesozoikums. Der vorherrschende Kalk ist dabei mit verschiedenen Gesteinen durchmischt. Es zeigen sich Mergel-Kalke und -Schiefer, Ton-Schiefer, Eisenoolith sowie kalkige Sandsteine.
Die Kalkschichten des Eigers lagern auf Gneis und sind um 60–70° nach Norden geneigt. Geprägt wurde die heutige Form des Eigers durch die Eiszeiten. Während der Riss-Kaltzeit reichte die Vergletscherung bis an den Fuss der Nordwand. In der Würm-Kaltzeit war die Mächtigkeit des Eises um 200 Meter geringer. Durch die Bewegung der Gletscher wurde die Erdoberfläche umgestaltet. Vom Eis überlagerte Landschaften wurden abgeschliffen, wohingegen unbedeckte Bereiche durch Verwitterung und andere Formen der Erosion verändert wurden. Mit dem Rückzug des Eises änderten sich auch die Druckverhältnisse im Gestein, was sich durch Entlastungsbewegungen formgebend auswirkte. Prägend für den Eiger und seine Form war die allseitige Umlagerung von Eismassen, welche für einen recht gleichmässigen und markanten Abrieb aller Wände sorgte. Darüber hinaus war die Nordwand durch ihre Exposition den Abtragungsprozessen wie Frostverwitterung mehr ausgesetzt.
Felssturz
2006 ereignete sich am Eiger ein grosser Bergsturz, der öffentliches Interesse auf sich zog. An der Ostseite des Berges, unterhalb des Mittellegigrates, war durch Felsbewegungen ein rund 250 Meter langer Spalt entstanden, der eine Breite von etwa 7 Metern erreichte.Danach senkten sich die äusseren Teile mehrere Zentimeter pro Tag ab. Eine Ursache dieser Felsabspaltung könnte sowohl das massive Eindringen von Schmelzwasser in den Felsen gewesen sein, als auch eine Instabilität des Gesteins durch den Rückgang des Gletschers unterhalb des Felsabbruchs infolge der globalen Erwärmung. Am 13. Juli 2006 um 19:24 Uhr stürzten rund 500'000 Kubikmeter Felsbrocken auf den Unteren Grindelwaldgletscher. Über der Gemeinde Grindelwald schwebte stundenlang eine Staubwolke. Bereits am Nachmittag desselben Tages war die sogenannte «Madonna vom Eiger» zu Tal gestürzt. Hierbei handelte es sich um einen ungefähr 30 Meter hohen schlanken Felsturm mit rund 600 Kubikmeter Volumen.
Seit diesen Ereignissen wird die Felsnase (Gesamtvolumen: ungefähr eine Million Kubikmeter Gestein), aus der die Gesteinsmasse abbrach, von der Universität Lausanne beobachtet. Die Beobachtungen ergaben, dass sich die Nase von Juli 2007 bis August 2008 auf einer nach Osten geneigten Gleitfläche um 15 Meter talwärts bewegte. Zusätzlich kippte die Gesteinsmasse um zwei Grad nach Nordosten. Die Kluft zwischen Berg und Felsbrocken betrug im August 2008 50 Meter. Immer wieder brechen Gesteinsteile ab und stürzen zu Tal. Gebremst und stabilisiert wird die Masse vom Gletschereis, in das die Felsnase gleitet. Dies verhindert, dass die Nase als kompakte Masse zu Tal stürzt. So gilt es als wahrscheinlicher, dass der Gesteinsblock in sich selbst zusammenfallen wird.
(Wikipedia)
The Laponian area is a large mountainous wildlife area in the Lapland province in northern Sweden, more precisely in Gällivare Municipality, Arjeplog Municipality and Jokkmokk Municipality. It was made a UNESCO World Heritage Site in 1996; the bulk of it had enjoyed protected status since the early 20th century.
The total area is about 9,400 square kilometres (3,600 sq mi), making it the world's largest unmodified nature area to be still cultured by natives—the natives in this case being the reindeer herding Sami people also known as Lapps (though this term is considered derogatory). Only parts of the area is actually used for pasture by them. With such a large space, the geography of the area varies greatly; it is dominated by mountains, rivers and lakes. Each nature reserve and national park has its distinctive features. The amount of snow in winter and rain in summer is considerable.
95% of the area is protected as national parks or nature reserves. It consists of the national parks Muddus, Sarek, Padjelanta and Stora Sjöfallet, and the nature reserves Sjaunja and Stubba. The remaining 5% are located in the areas of Sulitelma, Tjuoltadalen, and Rapadalen (part of which is in the Sarek park). The village of Porjus is a natural point of entry to the Laponian area and has recently opened an information center.
The Laponia area also contains three major hydropower stations with belonging basins and a big expansion of 100 wind power stations inside the world heritage area is planned.
The highest mountain of the area is Sarektjåhkkå, at 2,089 metres (6,854 ft).
Saint. Petersberg, Russia
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The name of the church comes from the fact that it was built precisely on the spot where Alexander II was murdered.
www.creativesuite.com/architecture-design/the-church-of-t...
Ercole de 'Roberti, also known as Ercole da Ferrara (Ferrara, 1451-1456 - Ferrara, 1496) - Face of weeping Magdalene (1478-1486) fresco detached from the Garganelli Chapel in the Cathedral of San Pietro in Bologna 24.5 x 28, 5 cm - Pinacoteca Nazionale di Bologna
Questo piccolo dipinto di straordinaria intensità emotiva, con il volto di Maria Maddalena piangente è l’unico frammento superstite della decorazione ad affresco eseguita da Ercole Roberti insieme a Francesco del Cossa, altro autorevole rappresentante della pittura ferrarese, sulle pareti della Cappella Garganelli nella cattedrale di San Pietro a Bologna.
Il crollo parziale della chiesa, avvenuto nel 1599, comportò la distruzione degli affreschi, ma le fonti storiche e alcune copie consentono di ricostruire l'intero programma figurativo della cappella, talmente nota e celebrata da essere definita da Michelangelo “una mezza Roma di bontà”. Ed è, appunto, da una copia con la Crocifissione, che possiamo rilevare la posizione esatta che occupava il frammento all’interno del ciclo.
Il volto della Maria Maddalena testimonia la straordinaria qualità dei perduti dipinti e una potenza espressiva che richiama la drammaticità dei volti delle Marie del gruppo scultoreo con il Compianto sul Cristo morto di Niccolò dell’Arca conservato nella chiesa bolognese di Santa Maria della Vita.
La descrizione meticolosa di ogni più piccolo dettaglio realizzato nello stile calligrafico di Ercole Roberti mostra la conoscenza della contemporanea pittura fiamminga, conosciuta direttamente a Ferrara nelle collezioni estensi.
La pelle arrossata dal pianto, le palpebre socchiuse, i denti visibili nella bocca spalancata, i capelli delineati uno a uno, sino all’eccellenza esecutiva delle lacrime cristalline sono particolari davvero strabilianti, soprattutto se si considera la rapidissima esecuzione obbligata dalla tecnica dell’affresco.
This small painting of extraordinary emotional intensity, with the face of Mary Magdalene weeping, is the only surviving fragment of the fresco decoration executed by Ercole Roberti together with Francesco del Cossa, another authoritative representative of Ferrara painting, on the walls of the Garganelli Chapel in the cathedral of San Pietro in Bologna.
The partial collapse of the church, which took place in 1599, led to the destruction of the frescoes, but historical sources and some copies make it possible to reconstruct the entire figurative program of the chapel, so well known and celebrated that it was defined by Michelangelo as "a half Rome of goodness" . And it is precisely from a copy with the Crucifixion that we can detect the exact position that the fragment occupied within the cycle.
The face of Mary Magdalene testifies to the extraordinary quality of the lost paintings and an expressive power that recalls the drama of the faces of the Marys of the sculptural group with the Lamentation over the Dead Christ by Niccolò dell’Arca preserved in the Bolognese church of Santa Maria della Vita.
The meticulous description of every smallest detail made in Ercole Roberti's calligraphic style shows the knowledge of contemporary Flemish painting, known directly in Ferrara in the Este collections.
The skin reddened by tears, the half-closed eyelids, the teeth visible in the wide open mouth, the hair outlined one by one, up to the executive excellence of the crystalline tears are truly amazing details, especially if we consider the very rapid execution required by the fresco technique.
As you can easily guess from the name "Little Kozjak Waterfall", it is located not far from the waterfall I showed two days ago. More precisely, it is a few hundred meters downstream from this one.
Although the waterfall was very easy to access, it was arguably the most difficult of those I explored from a photographic point of view.
It started with the fact that I couldn't find him. So I knew where he was, he was loud enough. I also saw where the water disappears down (because that was right next to the trail) and where it comes out at the end of a little maze of rocks (it was, where I made yesterdays photo). But no matter where I climbed, I just didn't see the waterfall itself. Shortly before I was about to give up, I found my way here thanks to some footprints in the mud.
The second challenge was that the water in this chimney was constantly spraying in all directions, including mine. I was thus constantly busy drying my lens while searching for a suitable composition, again with the fear of accidentally knocking my camera into the river.
Taking photos is really exciting.
However, when I look at the result now, I'm happy to say that it all paid off.
Wie man aus dem Namen "Kleiner Kozjak Wasserfall" leicht schließen kann, ist dieser unweit von dem Wasserfall gelegen, den ich vor zwei Tagen gezeigt habe. Genauer gesagt liegt er ein paar hundert Meter stromabwärts von diesem.
Obwohl der Wasserfall sehr einfach zu erreichen war, war er aus fotografischer Sicht wohl der schwierigste von denen, die ich erkundet habe.
Das ging schon damit los, dass ich ihn nicht finden konnte. Also ich wusste wo er ist, er war ja laut genug. Ich hab auch gesehen, wo das Wasser nach unten verschwindet (das war nämlich direkt neben dem Wanderweg) und wo es am Ende eines kleinen Labyrints aus Felsen wieder austritt (das war da, wo ich das gestrige Foto gemacht habe) . Doch ganz gleich wo ich hin geklettert bin, den Wasserfall selbst hab ich einfach nicht gesehen. Kurz bevor ich schon aufgeben wollte, hab ich dann, dank einiger Fußspuren im Matsch hier her gefunden.
Die zweite Herausforderung war, dass das Wasser in diesem Kamin permanent in alle Richtungen spritzte, also auch in meine. Ich war somit ununterbrochen damit beschäftgt meine Linse zu trocknen während ich nach einer geeigneten Komposition gesucht habe, und das erneut mit der Angst dabei versehentlich meine Kamera in den Fluß zu stoßen.
Fotografieren ist schon echt aufregend.
Wenn ich mir jetzt das Ergebnis anschaue stelle ich jedoch mit Freuden fest, dass sich das alles ausgezahlt hat.
more of this on my website at: www,shoot-to-catch.de
Pretty Dora Falls in Leggett, 50 ft. high precisely. I think this was my favorite of the falls I saw last weekend. I was not expecting such a pretty waterfall here.
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The general term ice age or, more precisely, "glacial age" denotes a geological period of long-term reduction in the temperature of the Earth's surface and atmosphere, resulting in an expansion of continental ice sheets, polar ice sheets and alpine glaciers. There have been at least four major ice ages in the Earth's past. Outside these periods, the Earth seems to have been ice-free even in high latitudes. There is evidence that greenhouse gas levels fell at the start of ice ages and rose during the retreat of the ice sheets, but it is difficult to establish cause and effect (see the notes above on the role of weathering). Greenhouse gas levels may also have been affected by other factors which have been proposed as causes of ice ages, such as the movement of continents and vulcanism. Although the last glacial period ended more than 8,000 years ago, its effects can still be felt today. For example, the moving ice carved out landscape in Canada, Greenland, northern Eurasia and Antarctica. The erratic boulders, till, drumlins, eskers, fjords, kettle lakes, moraines, cirques, horns, etc., are typical features left behind by the glaciers.
This is the Marken lighthouse, given its name due to its shape ('paard' means 'horse' in dutch). The original was built in 1700, then reconstructed on top of the early foundations in 1839. It's still in use today.
Photo of hummocks taken at the lighthouse of Marken. A red airplane flew pretty low around the lighthouse to enjoy the view of the sea of ice. A hummock is a boss or rounded knoll of ice rising above the general level of an ice-field, Hummocky ice is caused by slow and unequal pressure in the main body of the packed ice, and by unequal structure and temperature at a later period.
Een ijstijd of glaciatie is een geologisch tijdvak waarin ijskappen voorkomen. In het Engels wordt dit een periode van ice-house genoemd, als tegenhanger van een ijskaploze periode, de greenhouse ("broeikas"). Aangezien er gletsjers liggen op bijvoorbeeld Groenland of Antarctica, leven we tegenwoordig in een ijstijd. Men neemt aan dat dit in de gehele geologische geschiedenis van de Aarde minstens vijfmaal het geval is geweest, waarvan eenmaal zelfs zo sterk dat de ijskappen van de polen vrijwel tot aan de evenaar waren opgerukt. Ook zijn er periodes dat er aanzienlijke opwarming optrad waarbij die ijskappen grotendeels waren weggesmolten. Het klimaat op Aarde wordt beïnvloed door vele factoren, zoals de intensiteit van de zonnestraling, de ligging van de continenten, de continentverplaatsingen, vulkanisme, de zeestromen, de bedekking van het land door vegetatie, het weerkaatsingsvermogen van het aardoppervlak en vele kleine andere factoren. Met behulp van klimaatmodellen wordt door wetenschappers een reconstructie van het klimaat en de klimaatveranderingen in het verleden gemaakt. Alhoewel er een zekere consensus bestaat onder wetenschappers, zijn er nog vele onzekerheden en tegenstrijdigheden in dit onderzoek.
Hierboven een foto van kruiend ijs. Zoetwatermeren kunnen spectaculair bevriezen. Grotere meren zoals het IJsselmeer (IJmeer) hierboven hebben bijna altijd wel golven, en dit werkt directe bevriezing van het wateroppervlak tegen. Eerst vormen zich kleine ijsschotsen, die naar de kust drijven onder invloed van de wind. Deze schotsen vormen zo een ijsveld op het water dat de golven dempt, en uiteindelijk vriezen alle schotsen aan elkaar vast tot een massa. Voordat dit gebeurt schuren de schotsen voortdurend langs elkaar heen en schrapen zo stukjes ijs van elkaar af; elke schots krijgt zo een witte rand. Zulk ijs is dus totaal niet geschikt om op te schaatsen. Wanneer grotere delen van het meer bevriezen beginnen de platen, die soms een paar vierkante kilometer groot zijn, langzaam tegen elkaar te bewegen onder invloed van de wind en stroming. Dit heeft kruiend ijs tot gevolg: de ijsschotsen worden met kracht gebroken en op elkaar gestapeld langs de dijken langs het meer. Dit hoeft niet alleen bij dun ijs te gebeuren; soms kruit het ijs bij een dikte van meer dan 20 cm. De stapels ijs worden dan hoog, en het geluid is oorverdovend. Het Paard van Marken is een vuurtoren van Marken. De vuurtoren is gebouwd in 1839 en staat op de oostelijke punt van het eiland. De toren heeft een hoogte van 16 meter en een lichtbereik van 16,7 km.
Aigle ibérique
Águila imperial ibérica
Much better pictures of this amazing raptor can be found on Flickr but for the most part, they are taken from expensive hides where raptors are lured with dead rabbits. I refuse to play this game as, to me, the whole point of wildlife photography is precisely to capture animals in the wild, without any human intervention.
This one was seen gliding over our group of birdwatchers led by a guide of the SEO Birdlife (Sociedad Española de Ornitologia)
In July of 1988 my brother and I happened upon this recently destroyed stone house in Creek Hills. We talked to a neighbor who told us that the folks who were renting it got mad at the landlord and decided to burn the place down.
I had seen the house before but never realized it was built of stone because it had been painted white. It was of unusual construction because the stones were so large and so precisely cut, arranged in rows almost like they were cement blocks. Usually the stone houses in the area were a combination of squared off corner quoins for stability and randomly shaped, flat faced stones for the body. It was also quite large. The stones soon disappeared and we were told they had been salvaged for reuse.
Scanned from a film print
Su una ripidissima e imponente rupe che si eleva a 130 m sopra lo specchio del lago (di origine glaciale), si erge il simbolo di Bled e della Slovenia – il Castello di Bled
La storia del castello risale nell'anno 1004, quando l'imperatore germanico Enrico II donò i possedimenti di Bled ad Albuino, vescovo di Bressanone. In quel periodo al posto del castello si erigeva solamente una torre romanica, protetta da una cinta muraria. Il primo castello fu costruito intorno all'anno 1011, ma i vescovi di Bressanone non ci abitavano mai. Proprio per questo all'interno non ci sono sale sontuose, venne, infatti, data molta più importanza al sistema di difesa.
On a steep and imposing cliff that rises 130 m above the surface of the lake (glacial), stands the symbol of Bled and Slovenia - Bled Castle
The history of the castle dates back in 1004, when the Holy Roman Emperor Henry II donated the Bled estate to Albuino, bishop of Bressanone. At that time, instead of the castle is erected only a Romanesque tower, protected by walls. The first castle was built around the year 1011, but the bishops of Brixen never lived there. Precisely for this reason there is no salt in sumptuous, was, in fact, given much more importance to the defense system.
beauty of nature
Nature. The most beautiful thing in the world is, precisely, the conjunction of learning and inspiration. Oh, the passion for research and the joy of discovery!
A human being is a part of the whole called by us universe, a part limited in time and space. He experiences himself, his thoughts and feeling as something separated from the rest, a kind of optical delusion of his consciousness. This delusion is a kind of prison for us, restricting us to our personal desires and to affection for a few persons nearest to us. Our task must be to free ourselves from this prison by widening our circle of compassion to embrace all living creatures and the whole of nature in its beauty.
In the afternoon at my favorite bridge, Germany 31/03/2018 at 04:55 pm.
About the series (to which the Photo above belongs)
My dear Flickr-Friends, my dear unknown Flickr-User,
First, I would like to mention: “Mettwurst is a strongly flavoured German sausage, made from raw minced pork which is preserved by curing and smoking, often with garlic. The southern German variety is soft and similar to Teewurst.” (Source: en.wikipedia.org/wiki/Mettwurst)
Second, I want to amplify: During the last years I had my camera very often with me. An immense amount of photos have been shot, most of them rather unplanned on walks through my hometown. With the series I would like to present a few of my personal favorites (most of them are less than one year old). As the subtitle promises: the Photos show undoubtedly/exclusively trivial things.
Fuck you reality, fuck you so much, I want to be cheated!
About the post-processing
For editing I've used the Lightromm plug-in "Silver Efex Pro 2". More precisely: Preset "Film Noir 3" as a basis (nr. 32), but with some modifications. Apart from other small corrections (eg in contrast or exposure) I removed the artificial grain and the frame of the preset and I added a blue toning for all the photos of the series. And: For almost all photos I used a green or blue color filter.
Isn't this a duck pose everyone shoots? Of course it is...since it's about the most interesting thing a duck does when it is on the water. Of course, with a hundred bazillion photos uploaded to Flickr...EVERYTHING is a cliche, so that does sort of negate it a bit.
This is another photo from the first outing with the new camera and long lens. The day was totally grey and colorless, and birds weren't flying, First test had to settle for ducks on the water. And not particularly close to shore.
If you watch duck behavior, you know precisely when this is going to happen, and it is easy to be ready for it, The raw (not RAW) file is virtually colorless, though nicely sharp. A bit of processing, and visual interest is restored. Hope you like it.
The Villa Poppaea is an ancient Roman seaside villa (villa maritima) situated between Naples and Sorrento, in southern Italy. It is also referred to as the Villa Oplontis, or more precisely as Villa A by modern archaeologists.The villa itself is a large structure situated in the ancient Roman town of Oplontis (the modern Torre Annunziata), about ten meters below the modern ground level. Evidence suggests that it was owned by the Emperor Nero, and believed to have been used by his second and rather notorious wife, Poppaea Sabina, as her main residence when she was not in Rome.
Like many of the frescoes that were preserved due to the eruption of Mount Vesuvius, those decorating the walls of the Villa Poppaea are striking both in form and in color. Many of the frescoes are in the “Second Style” (also called the Architectural Style) of ancient Roman painting, dating to ca. 90-25 BCE as classified in 1899 by August Mau. Details include feigned architectural features such as trompe-l'œil windows, doors, and painted columns.
Frescoes in the caldarium depicting Hercules in the Garden of the Hesperides are painted in the "Third Style" (also called the Ornate Style) dating to ca. 25 BCE-40 CE according to Mau. Attention to realistic perspective is abandoned in favor of flatness and elongated architectural forms which “form a kind of shrine" around a central scene, which is often mythological.
Immediately to the west of the triclinium is a large oecus, which was the main living room of a Roman house. Like the caldarium frescoes, the room is also painted in the Second Style. The east wall includes some wonderful details such as a theatre mask and peacock.
Much attention has been paid to the allusions to stage painting (scenae frons) in the Villa Poppaea frescoes, particularly those in Room 23.
The full Moon looms large in this Picture of the Week, framing ESO’s Extremely Large Telescope (ELT). Taken at precisely the moment that the rising Moon appears to perch atop Cerro Armazones, this perfectly timed photo captures the striking halo created around the ELT’s ongoing construction.
On either side of the telescope’s structure we can see the outlines of gigantic cranes, hard at work shaping what will become the world’s largest optical and infrared telescope. The construction team, led by the company Cimolai, has partially covered the ELT dome with insulating cladding, captured here shining as the sun sets, that will protect the telescope from sunlight and the harsh environment of the Atacama desert. Through an opening in this dome, we can also peek at the telescope’s main structure, which will hold the ELT’s five mirrors. Right now, one of the two sliding doors that will cover this opening is being installed.
This stunning image was taken on 13 March by our colleague Juan Beltrán, who works at ESO’s Paranal Observatory, not far from the ELT. And as you can tell from the images linked below, other photographers joined in to capture this unique alignment. As work continues on the ELT, we’re watching it grow before our very eyes — and look forward to sharing more inspiring shots like this one.
Credit: J. Beltrán/ESO
More precisely, young Africans (on road to Senerengeti NP) performing as Masai warriors for money. Of course, I don't really understand their situation.
White Storks
I watched this pair of white storks for some time and their mating ritual was always the same, so I was able to set the distance and detail precisely and focus on the right moment to trigger the camera ...
First, the male leaves the nest and flies into the nearby forest. It collects branches for nest building. Then it flies back to the nest and is already expected and welcomed. Then it gets nagged and finally mates - always the same for more than half an hour. You could have filmed it, but since I'm more of a photographer, I decided to do a little series here.
Have fun watching these wonderful birds.
Ich habe dieses Weißstorchenpaar einige Zeit beobachtet und ihr Paarungsritual spielte sich immer wieder gleich ab und so konnte ich die Entfernung und den Ausschnitt präzise manuell einstellen und mich auf den richtigen Moment für die Auslösung der Kamera konzentrieren...
Zunächst verlässt das Männchen das Nest und fliegt in den nahen Wald. Es sammelt Zweige für den Nestbau. Dann fliegt es zurück ins Nest und wird schon erwartet und begrüßt. Dann wird geschnäbelt und letztendlich paaren sie sich - immer der gleiche Ablauf für mehr als eine halbe Stunde. Man hätte es sicherlich filmen können, doch da ich nun mal eher Fotograf bin, habe ich mich hier für eine kleine Serie entschieden.
Viel Spaß beim Betrachten dieser wunderbaren Vögel.
"Nothing terrifies me as much as staying precisely the same. This cannot be as far as I get to go, there is so much more to become."
~Tyler Knott Gregson
Pittamiglio Castle is a building located in the city of Montevideo ( Uruguay ), more precisely the street Francisco Vidal, between September 21 and the Rambla de Montevideo , at Punta Trouville in Punta Carretas neighborhood. The facade facing the promenade shows a replica of the Victory of Samothrace , representing "the victory of life", which makes the building emblematic of the coast of Montevideo.
It was residence of the architect Humberto Pittamiglio from 1911 to 1966 , who maintained it in permanent construction with the premise that its construction never finished. In the castle are alchemical, Christian , Templar , Rosicrucian and Masonic symbolism , among others. Inside the building there are numerous narrow corridors, doors that lead to nothing, blind windows and rooms with strange shapes. The history of the castle is surrounded by myths and legends, including those that affirm that it housed the Holy Grail between 1944 and 1956, that satanic orgies and rituals were realized there or that its owner left at night to Walk along the boulevard wrapped in a red cape.
EXPLORE: Feb 13/12 #336
There are situations where time anchors us and other situations where time tests us. Make time your friend. You might as well. And it will keep your molecules vibrating at precisely the right speed. And it will give you little glimpses through the peep-holes you punch through it once in a while.
from my finally finished book, After the Interlude
They are blooming now in the forest :)
Bilberry (Vaccinium myrtillus) is a species of shrub with edible fruit of blue color, more precisely called common bilberry or blue whortleberry. It is found natively in Europe, northern Asia, Greenland, Iceland, Western Canada, and the Western United States. It occurs in the wild on heathlands and acidic soils. Its berry has been long consumed in the Old World. It is related to the widely cultivated North American blueberry. The bilberry fruit is smaller than that of the blueberry and similar in taste. Bilberries are darker in colour, and usually appear near black with a slight shade of blue. While the blueberry's fruit pulp is light green, the bilberry's is red or purple, heavily staining the fingers and lips of consumers eating the raw fruit. Vaccinium myrtillus fruits has been used for nearly 1,000 years in traditional European medicine for treatment of disorders of the gastrointestinal tract and diabetes. In cooking, the bilberry fruit is commonly used for the same purposes as the American blueberry such as pies, cakes, jams, muffins, cookies, sauces, syrups, juices, and candies.
Our Daily Challenge - theme: "Everything that blooms"
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Kwitnące jagody pstryknięte w lesie :)
Borówka czarna (Vaccinium myrtillus) – gatunek rośliny wieloletniej z rodziny wrzosowatych. Ma wiele nazw zwyczajowych, m.in. jagoda, czarna jagoda, czernica. Roślina jest szeroko rozprzestrzeniona w Azji, Europie i Ameryce Północnej na obszarach o klimacie umiarkowanym i arktycznym. W Polsce jest pospolita zarówno na nizinach, jak i w górach. Jest wykorzystywana szeroko jako roślina jadalna i lecznicza. Znaczenie gospodarcze borówki czarnej pozostaje wysokie mimo silnej konkurencji znacznie bardziej plennych borówek północnoamerykańskich, których owoce mają uboższy skład chemiczny od czernicy. Owoce borówki czarnej były od dawna bardzo istotne dla Słowian i ludów północnej Europy. Używano jej owoców jako lekarstwa przy biegunkach i krwawej dyzenterii. Zastosowanie takie utrzymało się w lecznictwie ludowym, przy czym często zalecano je także w większych dawkach przeciw owsikom. Ponadto owoce borówki czarnej oferowane i spożywane są w postaci świeżej, suszonej, mrożonej oraz jako składnik przetworów takich jak dżemy, ciasta, soki oraz ciekłe lub sproszkowane koncentraty, będące suplementem diety. Przetwory z jagód wyróżniają się długą trwałością.
Schweiz / Wallis - Matterhorn
seen on the way from Riffelsee to Riffelalp
gesehen auf dem Weg vom Riffelsee zur Riffelalp
The Matterhorn (/ˈmætərhɔːrn/, German: [ˈmatɐˌhɔʁn]; Italian: Cervino, [tʃerˈviːno]; French: Cervin, [sɛʁvɛ̃]; Romansh: Mont(e) Cervin(u)) is a mountain of the Alps, straddling the main watershed and border between Switzerland and Italy. It is a large, near-symmetric pyramidal peak in the extended Monte Rosa area of the Pennine Alps, whose summit is 4,478 metres (14,692 ft) high, making it one of the highest summits in the Alps and Europe. The four steep faces, rising above the surrounding glaciers, face the four compass points and are split by the Hörnli, Furggen, Leone/Lion, and Zmutt ridges. The mountain overlooks the Swiss town of Zermatt, in the canton of Valais, to the northeast; and the Italian town of Breuil-Cervinia in the Aosta Valley to the south. Just east of the Matterhorn is Theodul Pass, the main passage between the two valleys on its north and south sides, which has been a trade route since the Roman Era.
The Matterhorn was studied by Horace-Bénédict de Saussure in the late eighteenth century, and was followed by other renowned naturalists and artists, such as John Ruskin, in the 19th century. It remained unclimbed after most of the other great Alpine peaks had been attained and became the subject of an international competition for the summit. The first ascent of the Matterhorn was in 1865 from Zermatt by a party led by Edward Whymper, but during the descent, a sudden fall claimed the lives of four of the seven climbers. This disaster, later portrayed in several films, marked the end of the golden age of alpinism. The north face was not climbed until 1931 and is among the three biggest north faces of the Alps, known as "The Trilogy". The west face, the highest of the Matterhorn's four faces, was completely climbed only in 1962. It is estimated that over 500 alpinists have died on the Matterhorn, making it one of the deadliest peaks in the world.
The Matterhorn is mainly composed of gneisses (originally fragments of the African Plate before the Alpine orogeny) from the Dent Blanche nappe, lying over ophiolites and sedimentary rocks of the Penninic nappes. The mountain's current shape is the result of cirque erosion due to multiple glaciers diverging from the peak, such as the Matterhorn Glacier at the base of the north face. Sometimes referred to as the Mountain of Mountains (German: Berg der Berge), it has become an indelible emblem of the Alps in general. Since the end of the 19th century, when railways were built in the area, the mountain has attracted increasing numbers of visitors and climbers. Each year, numerous mountaineers try to climb the Matterhorn from the Hörnli Hut via the northeast Hörnli ridge, the most popular route to the summit. Many trekkers also undertake the 10-day-long circuit around the mountain. The Matterhorn has been part of the Swiss Federal Inventory of Natural Monuments since 1983.
Names
The name Matterhorn derives from the German words Matte ("meadow") and Horn ("horn"), and is often translated as "the peak of the meadows".
In the Schalbetter map, printed by Sebastian Münster in 1545, the valley is labelled Mattertal, but the mountain has the Latin name Mons Silvius as well as the German name Augstalberg, in concord with the Aosta Valley (German Augstal). The 1548 map by Johannes Stumpf gives only Mons Silvius.
The French name Cervin, from which the Italian term Cervino derives, stems from the Latin Mons Silvanus (or Mons Sylvanus), where silva means "forest"; this was corrupted to Selvin and then Servin. The change of the first letter "s" to "c" is attributed to Horace Bénédict de Saussure, who thought the word was related to "deer" (French: cerf and Italian: cervo).
Josias Simler hypothesized in De Alpibus Commentarius (1574) that the name Mons Silvius was readopted by T. G. Farinetti: "Silvius was probably a Roman leader who sojourned with his legions in the land of the Salassi and the Seduni, and perhaps crossed the Theodul Pass between these two places. This Silvius may have been that same Servius Galba whom Caesar charged with the opening up of the Alpine passes, which from that time onward traders have been wanting to cross with great danger and grave difficulty. Servius Galba, in order to carry out Caesar's orders, came with his legions from Allobroges (Savoy) to Octodurum (Martigny) in the Valais, and pitched his camp there. The passes which he had orders to open from there could be no other than the St. Bernard, the Simplon, the Theodul, and the Moro; it therefore seems likely that the name of Servius, whence Silvius and later Servin, or Cervin, was given in his honour to the famous pyramid." It is unknown when the new name of Servin, or Cervin, replaced the old, from which it seems to be derived.
The Matterhorn is also named Gran Bècca ("big mountain") by the Valdôtains and Horu by the local Walliser German speaking people.
Because of its recognizable shape, many other similar mountains around the world were named or nicknamed the 'Matterhorn' of their respective countries or mountain ranges.
Height
The Matterhorn has two distinct summits, situated at either end of a 100-metre-long (330 ft) exposed rocky crest which forms the Italian/Swiss border. In August 1792, the Genevan geologist and explorer Horace Bénédict de Saussure made the first measurement of the Matterhorn's height, using a sextant and a 50-foot-long (15 m) chain spread out on the Theodul glacier. He calculated its height as 4,501.7 m (14,769 ft). In 1868 the Italian engineer Felice Giordano measured a height of 4,505 m (14,780 ft) by means of a mercury barometer, which he had taken to the summit. The Dufour map, which was afterwards followed by the Italian surveyors, gave 4,482 m (14,705 ft) as the height of the Swiss summit.
In 1999, the summit height was precisely determined to be at 4,477.54 m (14,690 ft) above sea level by using Global Positioning System technology as part of the TOWER Project (Top of the World Elevations Remeasurement) and to an accuracy of less than one centimetre, which allows future changes to be tracked.
The topographic prominence of the Matterhorn is 1,042 metres (3,419 ft) as the ridge connecting it with a higher summit (in this case the Weisshorn, which is the culminating point of the range west of the Mattertal valley) sinks to a height of 3,436 m (11,273 ft) at the Col Durand, a saddle between the Pointe de Zinal and the Mont Durand. The topographic isolation is 13.9 km (8.6 mi), as the nearest point of higher elevation is the one-metre (3 ft 3 in) higher Western Liskamm
Considering mountains with a topographic prominence of at least 300 m (980 ft), the Matterhorn is the sixth-highest summit in the Alps and Europe outside the Caucasus Mountains. It is the fifth-highest summit of Valais and Switzerland and the third highest summit of the Aosta Valley and Italy. Locally, it is the third-highest summit in the municipality of Zermatt and the highest summit in the municipality of Valtournenche. On the official International Climbing and Mountaineering Federation list of Alpine four-thousanders, which also includes subsidiary summits of higher mountains such as the nearby Monte Rosa, the Matterhorn is the 12th highest summit in the Alps.
Geography
The Matterhorn has a pyramidal shape with four faces nearly facing the four compass points. Three of them (north, east and west) are on the Swiss side of the border and watershed (Mattertal valley) and one of them (south) is on the Italian side of the border (Valtournenche valley). The north face overlooks the Ober Gabelhorn (7 km away) across the Zmutt Glacier and valley (above Zermatt), the east face overlooks the Gorner Glacier system between the Gornergrat and Monte Rosa (respectively 10 and 17 km away) across the Theodul Pass, the west face overlooks the upper basin of the Zmutt Glacier between the Dent Blanche and the Dent d'Hérens (respectively 7 and 4 km away) and the south face fronts the resort town of Breuil-Cervinia and overlooks a good portion of the Valtournenche. The Matterhorn does not form a perfect square pyramid, as the north and south faces are wider than the west and east faces. Moreover, the latter faces do not actually meet on the summit but are connected by a 100-metre-long horizontal west–east ridge between the north and south faces.
The Matterhorn's faces are steep, and only small patches of snow and ice cling to them; regular avalanches send the snow down to accumulate on the glaciers at the base of each face, the largest of which are the Tiefmattengletscher to the west, part of the Zmutt Glacier, and the Matterhorn Glacier to the north. Smaller glaciers lie at the base of the south face (the Lower Matterhorn Glacier) and the east face (unnamed). In this area, the border between Switzerland and Italy coincides with the main Alpine watershed, separating the drainage basin of the Rhone on the north (Mediterranean Sea) and that of the Po on the south (Adriatic Sea). The north side is drained by the Zmuttbach (west and north faces) and the Gornera through the Furggbach (east face), tributaries of the Rhone through the (Matter) Vispa. The south side and face is drained by the Marmore torrent, a tributary of the Po through the Dora Baltea (or Doire baltée). The Theodul Pass, located on the watershed between the Matterhorn and the Breithorn, at 3,295 metres, is the easiest passage between the two valleys and countries (the slightly lower Furggjoch not being used as a pass). The pass was used as a crossover and trade route for the Romans and the Romanised Celtic population Salassi between 100 BCE and 400 CE. The area is now heavily glaciated and covered on the north side by the Theodul Glacier.
Well-known faces are the east and north, visible from the area of Zermatt, although mostly hidden from the Mattertal by the chain of the Weisshorn. The east face is 1,000 metres high and, because it is "a long, monotonous slope of rotten rocks", presents a high risk of rockfall, making its ascent dangerous. The north face is 1,200 metres high and is one of the most dangerous north faces in the Alps, in particular for its risk of rockfall and storms. The south face, well visible from the Valtournenche, is 1,350 metres high and offers many different routes. The west face, the highest at 1,400 metres, has the fewest ascent routes and lies in a more remote area than the other faces.
The four main ridges separating the four faces are the main climbing routes. The least difficult technical climb and the usual climbing route, the Hörnli ridge (Hörnligrat), lies between the east and north faces and is aligned towards the Oberrothorn above Zermatt. To its west lies the Zmutt ridge (Zmuttgrat), between the north and west faces and aligned towards the Wandfluehorn; this is, according to Collomb, "the classic route up the mountain, its longest ridge, also the most disjointed." The Lion ridge (Cresta del Leone / Arête du lion), lying between the south and west faces and aligned towards the Dent d'Hérens is the Italian normal route and goes across Pic Tyndall; Collomb comments, "A superb rock ridge, the shortest on the mountain, now draped with many fixed ropes, but a far superior climb compared with the Hörnli." Finally the south side is separated from the east side by the Furggen ridge (Furggengrat), which is aligned towards the Klein Matterhorn. It is, according to Collomb, "the hardest of the ridges [...] the ridge still has an awesome reputation but is not too difficult in good conditions by the indirect finish".
While the Matterhorn is the culminating point of the Valtournenche on the south, it is only one of the many 4000 metres summits of the Mattertal valley on the north. Its height is exceeded by four major summits: the Weisshorn (4,505 m), the Dom (4,545 m), the Liskamm (4,527 m) and the second-highest in the Alps, Monte Rosa (4,634 m). This section of the Pennine Alps, including the Matterhorn, the Zinalrothorn, the Dent Blanche, the Dent d'Hérens, the Breithorn, the Strahlhorn, the Rimpfischhorn and the Alphubel, concentrates most of western Europe's highest mountains and forms a crown of peaks around Zermatt. The deeply glaciated region between the Matterhorn and Monte Rosa (named Dent Blanche-Matterhorn-Monte Rosa) is listed in the Federal Inventory of Landscapes and Natural Monuments since 1983.
Weather
The Matterhorn is an isolated mountain. Because of its position on the main Alpine watershed and its great height, the Matterhorn is exposed to rapid weather changes. In addition, the steep faces of the mountain and its isolated location make it prone to banner clouds formation, with the air flowing around the mountain producing condensation of the air on the lee side and also creating vortices.
Geology
The Matterhorn's pyramid is composed of Paleozoic rocks, which were thrusted over the Matterhorn's Mesozoic base during the Cenozoic. Quaternary glaciation and weathering give the mountain its current shape.
Apart from the base of the mountain, the Matterhorn is composed of gneiss belonging to the Dent Blanche klippe, an isolated part of the Austroalpine nappes, lying over the Penninic nappes. The Austroalpine nappes are part of the Apulian plate, a small continent that broke up from Africa before the Alpine orogeny. For this reason, the Matterhorn has been popularized as an African mountain. The Austroalpine nappes are mostly common in the Eastern Alps.
The Swiss explorer and geologist Horace-Bénédict de Saussure, inspired by the view of the Matterhorn, anticipated modern theories of geology:
What power must have been required to shatter and to sweep away the missing parts of this pyramid; for we do not see it surrounded by heaps of fragments; one only sees other peaks - themselves rooted to the ground - whose sides, equally rent, indicate an immense mass of débris, of which we do not see any trace in the neighbourhood. Doubtless, this is that débris which, in the form of pebbles, boulders, and sand, fills our valleys and our plains.
Formation
The formation of the Matterhorn (and the whole Alpine range) started with the break-up of the Pangaea continent 200 million years ago into Laurasia (containing Europe) and Gondwana (containing Africa). While the rocks constituting the nearby Monte Rosa remained in Laurasia, the rocks constituting the Matterhorn found themselves in Gondwana, separated by the newly formed Tethys Ocean.
100 million years ago the extension of the Tethys Ocean stopped and the Apulian plate broke from Gondwana and moved toward the European continent. This resulted in the closure of the western Tethys by subduction under the Apulian plate (with the Piemont-Liguria Ocean first and Valais Ocean later). The subduction of the oceanic crust left traces still visible today at the base of the Matterhorn (accretionary prism). The orogeny itself began after the end of the oceanic subduction when the European continental crust collided with the Apulian continent, resulting in the formation of nappes.
The Matterhorn acquired its characteristic pyramidal shape in much more recent times as it was caused by natural erosion over the past million years. At the beginning of alpine orogeny, the Matterhorn was only a rounded mountain like a hill. Because its height is above the snowline, its flanks are covered by ice, resulting from the accumulation and compaction of snow. During the warmer period of summer, part of the ice melts and seeps into the bedrock. When it freezes again, it fractures pieces of rock because of its dilatation (freeze-thaw), forming a cirque. Four cirques led to the shape of the mountain.
Rocks
Most of the base of the mountain lies in the Tsaté nappe, a remnant of the Piedmont-Liguria oceanic crust (ophiolites) and its sedimentary rocks. Up to 3,400 metres the mountain is composed of successive layers of ophiolites and sedimentary rocks. From 3,400 metres to the top, the rocks are gneisses from the Dent Blanche nappe (Austroalpine nappes). They are divided into the Arolla series (below 4,200 m) and the Valpelline zone (the summit). Other mountains in the region (Weisshorn, Zinalrothorn, Dent Blanche, Mont Collon) also belong to the Dent Blanche nappe.
Tourism and trekking
Since the eighteenth century, the Alps have attracted more and more people and fascinated generations of explorers and climbers. The Matterhorn remained relatively little known until 1865, but the successful ascent followed by the tragic accident of the expedition led by Edward Whymper caused a rush on the mountains surrounding Zermatt.
The construction of the railway linking the village of Zermatt from the town of Visp started in 1888. The first train reached Zermatt on 18 July 1891 and the entire line was electrified in 1930. Since 1930 the village is directly connected to St. Moritz by the Glacier Express panoramic train. However, there is no connection with the village of Breuil-Cervinia on the Italian side. Travellers have to hire mountain guides to cross the 3,300-metre-high glaciated Theodul Pass, separating the two resorts. The town of Zermatt remains almost completely free of internal combustion vehicles and can be reached by train only. (Apart from the local police service which uses a Volkswagen car, and the refuse collection lorry, only electric vehicles are used locally).
Rail and cable-car facilities have been built to make some of the summits in the area more accessible. The Gornergrat railway, reaching a record altitude of 3,100 metres, was inaugurated in 1898. Areas served by cable car are the Unterrothorn and the Klein Matterhorn (Little Matterhorn) (3,883 m, highest transportation system in Europe). The Hörnli Hut (3,260 m), which is the start of the normal route via the Hörnli ridge, is easily accessible from Schwarzsee (2,600 m) and is also frequented by hikers. The Zermatt and Breuil-Cervinia resorts function as separate ski resort all year round and are connected by skilifts over the Theodul Pass. In 2015 it was expected that there would be constructed a cable car link between Testa Grigia (or Tête grise) and Klein Matterhorn. It will finally provide a link between the Swiss and Italian side of the Matterhorn.
The Matterhorn Museum (Zermatt) relates the general history of the region from alpinism to tourism. In the museum, which is in the form of a reconstituted mountain village, the visitors can relive the first and tragic ascent of the Matterhorn and see the objects that belonged to the protagonists.
The Tour of the Matterhorn can be effected by trekkers in about 10 days. Considered by some as one of the most beautiful treks in the Alps, it follows many ancient trails that have linked the Swiss and Italian valleys for centuries. The circuit includes alpine meadows, balcony trails, larch forests and glacial crossings. It connects six valleys embracing three different cultures: the German-speaking high Valais, the French-speaking central Valais and the bilingual French/Italian-speaking Aosta Valley. Good conditions are necessary to circumnavigate the peak. After reaching Zinal from Zermatt by the Augstbord and Meiden passes, the trekker crosses the Col de Sorebois and the Col de Torrent before arriving at Arolla. Then the Arolla Glacier and the Col Collon must be crossed on the way to Prarayer, followed by the Col de Valcournera to Breuil-Cervinia. In the last and highest section, the Theodul Pass must be crossed before returning to Zermatt. In total, seven passes between 2,800 and 3,300 metres must be crossed on relatively difficult terrain.
As of 2015, almost two million visitors arrive at Zermatt annually. An average of around twelve people per year have died on Matterhorn in the ten years from 2005 to 2015.
Climbing history
The Matterhorn was one of the last of the main Alpine mountains to be ascended, not because of its technical difficulty, but because of the fear it inspired in early mountaineers. The first serious attempts were all from the Italian side, although, despite appearances, the southern routes are technically harder. The main figures were Jean-Antoine Carrel and his uncle Jean-Jacques Carrel, from the Valtournenche area, who made the first attempts in 1857 and 1858, reaching 3,800 m (12,500 ft) on the latter occasion. In July 1860, three brothers from Liverpool attempted the mountain, Alfred, Charles and Sandbach Parker, but they turned back at about 3,500 m (11,500 ft). In August of the same year, Jean-Jacques Carrel returned to guide, with Johann Joseph Bennen , Vaughan Hawkins and John Tyndall to about 3,960 m (12,990 ft) before turning back. In 1861 the Carrels managed to reach the Crête du Coq at 4,032 m (13,228 ft). In July 1862, Jean-Antoine, together with César Carrel, accompanied as porters (sic) John Tyndall, Anton Walters and J.J. Bennen to Matterhorn's Shoulder at 4,248 m (13,937 ft), which was subsequently named Pic Tyndall in honor of the client.
Edward Whymper joined the efforts in August 1861, but in his first 7 attempts with a variety of companions could only reach a maximum height of 4,100 m (13,500 ft). However, on 14 July 1865, in what is considered the last ascent of the golden age of alpinism, he was able to reach the summit by an ascent of the Hörnli ridge in Switzerland, guided by the famed French mountaineer Michel Croz and the Swiss father and son Peter Taugwalder Sr. and Jr., and accompanied by the British gentlemen Charles Hudson, Lord Francis Douglas, Douglas Robert Hadow. Upon descent, Hadow, Croz, Hudson and Douglas fell to their deaths on the Matterhorn Glacier, and all but Douglas (whose body was never found) are buried in the Zermatt churchyard.
Just three days later, on 17 July 1865, Jean-Antoine Carrel and Jean-Baptiste Bich reached the summit from the Italian side.
Before the first ascent
In the summer of 1860, Edward Whymper came across the Matterhorn for the first time. He was an English artist and engraver who had been hired by a London publisher to make sketches of the mountains in the region of Zermatt. Although the unclimbed Matterhorn had a mixed reputation among British mountaineers, it fascinated Whymper. Whymper's first attempt was in August 1861, from the village of Breuil on the south side. In Châtillon he hired a Swiss guide, who remained anonymous in his accounts, and in Valtournanche he almost hired Jean-Antoine Carrel as well, but, disliking the looks of Carrel's uncle, he changed his mind. The Carrels decided to give Matterhorn a try by themselves again, and caught up with Whymper at nightfall. Whymper now had "a strong inclination to engage the pair; but, finally, decided against it" and the Carrels went alone to reach a new high on Matterhorn of 4,032 m (13,228 ft) the next day. Whymper and his guide camped one more night on the Col du lion (= Col Tournanche) 3,479 m (11,414 ft) and were forced to turn around only an hour above this pass the day after.
In 1862 Whymper made further attempts, still from the south side, on the Lion ridge (or Italian ridge), where the route seemed easier than the Hörnli ridge (the normal route today). On his own, he reached above 4,000 metres, but was injured on his way down to Breuil. In July John Tyndall with Johann Joseph Bennen and another guide overcame most of the difficulties of the ridge that seemed so formidable from below and successfully reached the main shoulder; but at a point not very far below the summit they were stopped by a deep cleft that defied their utmost efforts. The Matterhorn remained unclimbed.
Whymper returned to Breuil in 1863, persuading Carrel to join forces with him and try the mountain once more via the Italian ridge. On this attempt, however, a storm soon developed and they were stuck halfway to the summit. They remained there for 26 hours in their tent before giving up. Whymper did not make another attempt for two years.
In the decisive year 1865, Whymper returned with new plans, deciding to attack the Matterhorn via its south face instead of the Italian ridge. On 21 June, Whymper began his ascent with Swiss guides, but halfway up they experienced severe rockfall; although nobody was injured, they decided to give up the ascent. This was Whymper's seventh attempt.
During the following weeks, Whymper spent his time climbing other mountains in the area with his guides, before going back to Breuil on 7 July. Meanwhile, the Italian Alpine Club was founded and its leaders, Felice Giordano and Quintino Sella, established plans to conquer the Matterhorn before any non-Italian could succeed. Felice Giordano hired Carrel as a guide. He feared the arrival of Whymper, now a rival, and wrote to Quintino Sella
I have tried to keep everything secret, but that fellow whose life seems to depend on the Matterhorn is here, suspiciously prying into everything. I have taken all the best men away from him; and yet he is so enamored of the mountain that he may go with others...He is here in the hotel and I try to avoid speaking to him.
Just as he did two years before, Whymper asked Carrel to be his guide, but Carrel declined; Whymper was also unsuccessful in hiring other local guides from Breuil. When Whymper discovered Giordano and Carrel's plan, he left Breuil and crossed the Theodul Pass to Zermatt to hire local guides. He encountered Lord Francis Douglas, a Scottish mountaineer, who also wanted to climb the Matterhorn. They arrived later in Zermatt in the Monte Rosa Hotel, where they met two other British climbers — the Reverend Charles Hudson and his young and inexperienced companion, Douglas Robert Hadow — who had hired the French guide Michel Croz to try to make the first ascent. These two groups decided to join forces and try the ascent of the Hörnli ridge. They hired another two local guides, a father and son, both named Peter Taugwalder.
First ascent
Whymper and party left Zermatt early in the morning of 13 July 1865, heading to the foot of the Hörnli ridge, which they reached 6 hours later (approximately where the Hörnli Hut is situated today). Meanwhile, Carrel and six other Italian guides also began their ascent of the Italian ridge.
Despite its appearance, Whymper wrote that the Hörnli ridge was much easier to climb than the Italian ridge:
We were now fairly upon the mountain, and were astonished to find that places which from the Riffel, or even from the Furggen Glacier, looked entirely impracticable, were so easy that we could run about.
After camping for the night, Whymper and party started on the ridge. According to Whymper:
The whole of this great slope was now revealed, rising for 3,000 feet like a huge natural staircase. Some parts were more, and others were less, easy; but we were not once brought to a halt by any serious impediment, for when an obstruction was met in front it could always be turned to the right or left. For the greater part of the way there was, indeed, no occasion for the rope, and sometimes Hudson led, sometimes myself. At 6.20 we had attained a height of 12,800 feet and halted for half an hour; we then continued the ascent without a break until 9.55, when we stopped for fifty minutes, at a height of 14,000 feet.
When the party came close to the summit, they had to leave the ridge for the north face because "[the ridge] was usually more rotten and steep, and always more difficult than the face". At this point of the ascent Whymper wrote that the less experienced Hadow "required continual assistance". Having overcome these difficulties the group finally arrived in the summit area, with Croz and Whymper reaching the top first.
The slope eased off, and Croz and I, dashing away, ran a neck-and-neck race, which ended in a dead heat. At 1.40 p.m. the world was at our feet, and the Matterhorn was conquered. Hurrah! Not a footstep could be seen.
Precisely at this moment, Carrel and party were approximatively 400 metres below, still dealing with the most difficult parts of the Italian ridge. When seeing his rival on the summit, Carrel and party gave up on their attempt and went back to Breuil.
After building a cairn, Whymper and party stayed an hour on the summit. Then they began their descent of the Hörnli ridge. Croz descended first, then Hadow, Hudson and Douglas, the elder Taugwalder, Whymper, with the younger Taugwalder coming last. They climbed down with great care, only one man moving at a time. Whymper wrote:
As far as I know, at the moment of the accident no one was actually moving. I cannot speak with certainty, neither can the Taugwalders, because the two leading men were partially hidden from our sight by an intervening mass of rock. Poor Croz had laid aside his axe, and in order to give Mr. Hadow greater security was absolutely taking hold of his legs and putting his feet, one by one, into their proper positions. From the movements of their shoulders it is my belief that Croz, having done as I have said, was in the act of turning round to go down a step or two himself; at this moment Mr. Hadow slipped, fell on him, and knocked him over.
The weight of the falling men pulled Hudson and Douglas from their holds and dragged them down the north face. The Taugwalders and Whymper were left alive when the rope linking Douglas to the elder Taugwalder broke. They were stunned by the accident and for a time could not move until the younger Taugwalder descended to enable them to advance. When they were together Whymper asked to see the broken rope and saw that it had been employed by mistake as it was the weakest and oldest of the three ropes they had brought. They frantically looked, but in vain, for traces of their fallen companions. They continued their descent, including an hour in the dark, until 9.30 p.m. when a resting place was found. The descent was resumed at daybreak and the group finally reached Zermatt, where a search of the victims was quickly organized. The bodies of Croz, Hadow and Hudson were found on the Matterhorn Glacier, but the body of Douglas was never found. Although the elder Taugwalder was accused of cutting the rope to save himself and his son, the official inquest found no proof of this.
Second ascent
On 16 July, two days after the first ascent and the catastrophe, Jean-Antoine Carrel set out to crown Whymper's victory by proving that the Italian side was not unconquerable. He was accompanied by Amé Gorret, a priest who had shared with him the first attempt on the mountain back in 1857. Jean-Baptiste Bich and Jean-Augustin Meynet completed the party. Giordano would have joined them, but Carrel refused absolutely to take him with them; he said he would not have the strength to guide a traveller, and could neither answer for the result nor for any one's life. After hearing Sunday mass at the chapel of Breuil, the party started. Amé Gorret has described this ascent with enthusiasm: "At last we crossed the Col du Lion and set foot upon the pyramid of the Matterhorn!" On the following day, the 17th, they continued the ascent and reached Tyndall's flagstaff. "We were about to enter unknown country," wrote Gorret, "for no man had gone beyond this point." Here opinions were divided; Gorret suggested ascending by the ridge and scaling the last tower straight up. Carrel was inclined to traverse to the west of the peak, and thence go up on the Zmutt side. Naturally the wish of Carrel prevailed, for he was the leader and had not lost the habit of command, notwithstanding his recent defeat.
They made the passage of the enjambée, and traversed the west face to reach the Zmutt ridge. A false step made by one of the party and a fall of icicles from above warned them to return to the direct line of ascent, and the traverse back to the Lion ridge was one of the greatest difficulty. A falling stone injured Gorret in the arm.
At last they reached the base of the final tower. "We stood," wrote Gorret, "in a place that was almost comfortable. Although it was not more than two yards wide, and the slope was one of 75 percent, we gave it all kinds of pleasant names : the corridor, the gallery, the railroad, &c., &c." They imagined all difficulties were at an end; but a rock couloir, which they had hitherto not observed, lay between them and the final bit of ridge, where progress would be perfectly easy. It would have been unwise for all four to descend into the couloir, because they did not know where to fix the rope that would be needed on their return. Time pressed: it was necessary to reduce the numbers of the party; Gorret sacrificed himself, and Meynet stopped with him. Very soon afterwards Carrel and Bich were finally on the top. Meanwhile, Giordano at Breuil was writing in his diary as follows: "Splendid weather; at 9.30 saw Carrel and his men on the Shoulder, after that saw nothing more of them. Then much mist about the summit. Lifted a bit about 3.30, and we saw our flag on the western summit of the Matterhorn."
Other ascents
Ridges
The first direct ascent of the Italian (south-west) ridge as it is climbed today was by J. J. and J. P. Maquignaz on 13 September 1867.Julius Elliott made the second ascent via the Hörnli (north-east) ridge in 1868, and later that year the party of John Tyndall, J. J. and J. P. Maquignaz was the first to traverse the summit by way of the Hörnli and Italian ridges. On 22 August 1871, while wearing a white print dress, Lucy Walker became the first woman to reach the summit of the Matterhorn, followed a few weeks later by her rival Meta Brevoort. The first winter ascent of the Hörnli ridge was by Vittorio Sella with guides J. A. Carrel, J. B. Carrel and L. Carrel on 17 March 1882, and its first solo ascent was made by W. Paulcke in 1898. The first winter solo ascent of the Hörnli ridge was by G. Gervasutti in 1936.
The Zmutt (north-west) ridge was first climbed by Albert F. Mummery, Alexander Burgener, J. Petrus and A. Gentinetta on 3 September 1879. Its first solo ascent was made by Hans Pfann in 1906, and the first winter ascent was made by H. Masson and E. Petrig on 25 March 1948.
The last of the Matterhorn's four ridges to be ascended was the Furggen (south-east) ridge. M. Piacenza with guides J. J. Carrel and J. Gaspard on 9 September 1911, climbed most of the ridge but bypassed the overhangs near the top to the south. Not until 23 September 1942, during the Second World War, did Alfredo Perino, along with guides Louis Carrel (nicknamed "The Little Carrel") and Giacomo Chiara, climb the complete ridge and the overhangs directly.
In 1966, René Arnold and Joseph Graven made the first solo enchainement of the four Matterhorn ridges in 19.5 hours. Beginning at the 3,300m Bossi Bivouac hut, the pair followed the normal route up the Furggen Ridge and then descended the Hornli Ridge. After crossing the Matterhorn Glacier at the base of the north face, they ascended the Zmutt Ridge and then descended the Italian (Lion) Ridge to the village of Breuil. In 1985, Marco Barmasse repeated their achievement, but this time his route included the first solo ascent of the Furggen overhangs. He completed the enchainement, reaching the Abruzzi Hut after 15 hours.
On 20 August 1992, Italian alpinist Hans Kammerlander and Swiss alpine guide Diego Wellig climbed the Matterhorn four times in just 23 hours and 26 minutes. The route they followed was: Zmutt ridge–summit–Hörnli ridge (descent)–Furggen ridge–summit–Lion ridge (descent)–Lion ridge–summit–Hörnli ridge (descent)–Hörnli ridge–summit–Hörnli Hut (descent). However the Italian route (Lion Ridge), was not climbed from Duca degli Abruzzi Refuge at 2802 m, but from Carrel Hut, at 3830 m, both uphill and downhill.
In 1995, Bruno Brunod climbed Matterhorn from the village Breuil-Cervinia in 2 h 10 min. and from Breuil-Cervinia to Matterhorn and back, in 3:14:44
On 21 August 2013, the Spanish mountain runner Kilian Jornet broke Brunod's record as it took him 1 hour, 56 min to the top from Breuil-Cervinia - a round-trip time of 2 hours 52 minutes to return to his starting point.
Faces
William Penhall and guides made the first (partial) ascent of the west face, the Matterhorn's most hidden and unknown, one hour after Mummery and party's first ascent of the Zmutt ridge on 3 September 1879. It was not until 1962 that the west face was completely climbed. The ascent was made on 13 August by Renato Daguin and Giovanni Ottin. In January 1978 seven Italian alpine guides made a successful winter climb of Daguin and Ottin's highly direct, and previously unrepeated, 1962 route. But a storm came during their ascent, bringing two metres of snow to Breuil-Cervinia and Zermatt, and their accomplishment turned bitter when one of the climbers died during the descent.
The north face, before it was climbed in 1931, was one of the last great big wall problems in the Alps. To succeed on the north face, good climbing and ice-climbing technique and route-finding ability were required. Unexpectedly it was first climbed by the brothers Franz and Toni Schmid on 31 July – 1 August 1931. They reached the summit at the end of the second day, after a night of bivouac. Because they had kept their plans secret, their ascent was a complete surprise. In addition, the two brothers had travelled by bicycle from Munich and after their successful ascent they cycled back home again. The first winter ascent of the north face was made by Hilti von Allmen and Paul Etter on 3-4 February 1962. Its first solo ascent was made in five hours by Dieter Marchart on 22 July 1959. Walter Bonatti climbed the "North Face Direct" solo on 18-22 February 1965. The same year, Yvette Vaucher became the first woman to climb the north face. Bonatti's direct route was not repeated solo until 29 years later, in winter 1994 by Catherine Destivelle.
Ueli Steck set the record time in climbing the north face (Schmid route) of Matterhorn in 2009 with a time of 1 hour 56 minutes.
After Bonatti's climb, the best alpinists were still preoccupied with one last great problem: the "Zmutt Nose", an overhang lying on the right-hand side of the north face. In July 1969 two Italians, Alessandro Gogna and Leo Cerruti, attempted to solve the problem. It took them four days to figure out the unusual overhangs, avoiding however its steepest part. In July 1981 the Swiss Michel Piola and Pierre-Alain Steiner surmounted the Zmutt Nose by following a direct route, the Piola-Steiner.
The first ascent of the south face was made by Enzo Benedetti with guides Louis Carrel and Maurice Bich on 15 October 1931, and the first complete ascent of the east face was made by Enzo Benedetti and G. Mazzotti with guides Louis and Lucien Carrel, Maurice Bich and Antoine Gaspard on 18-19 September 1932.
Casualties on the Matterhorn
The four men lost in 1865 have not been the only fatalities on the Matterhorn. In fact, several climbers die each year due to a number of factors including the scale of the climb and its inherent dangers, inexperience, falling rocks, and overcrowded routes. The Matterhorn is thus amongst the deadliest mountains in the world. By the late 1980s, it was estimated that over 500 people have died whilst attempting its summit since the 1865 ascent, with an average of about 12 deaths each year.
In the 2000s, there was a trend of fewer people dying each year on the mountain. This has been attributed partly to a greater awareness of the risks, and also due to the fact that a majority of climbers now use local guides. However, in the summer of 2018, at least ten people died on the mountain.
Here is a list of people who died on the mountain whose bodies were not recovered until later:
1954 French skier Henri le Masne went missing on the Matterhorn. In 2005 remains were found, identified as le Masne in 2018
1970 Two Japanese climbers missing; remains found after 45 years in 2015
1979 British climber missing; remains found after 34 years in 2014
2014 Japanese hiker missing; remains found 2018
2016 Two British climbers missing; remains found 2016
Legacy: beginning of mountain culture
The first ascent of the Matterhorn changed mountain culture. Whymper’s book about his first ascent, Scrambles Amongst the Alps, published in 1871, was a worldwide bestseller. Tourists began to visit Switzerland in the summer to see the Alps and often hired locals as guides. With the beginning of alpine skiing in the early 20th century, tourists began traveling to Switzerland in winter also. Mountaineering, in part, helped transform Switzerland’s mountain regions from poor rural areas to tourist destinations. This combination of mountain climbing, skiing and tourism, was used in the western United States, creating Sun Valley, Vail, Jackson Hole, and other mountain towns around the world.
Climbing routes
Today, all ridges and faces of the Matterhorn have been ascended in all seasons, and mountain guides take a large number of people up the northeast Hörnli route each summer. In total, up to 150 climbers attempt the Matterhorn each day during summer. By modern standards, the climb is fairly difficult (AD Difficulty rating), but not hard for skilled mountaineers according to French climbing grades. There are fixed ropes on parts of the route to help. Still, it should be remembered that several climbers may die on the mountain each year.
The usual pattern of ascent is to take the Schwarzsee cable car up from Zermatt, hike up to the Hörnli Hut elev. 3,260 m (10,700 ft), a large stone building at the base of the main ridge, and spend the night. The next day, climbers rise at 3:30 am so as to reach the summit and descend before the regular afternoon clouds and storms come in. The Solvay Hut located on the ridge at 4,003 m (13,133 ft) can be used only in a case of emergency.
Other popular routes on the mountain include the Italian (Lion) ridge (AD+ Difficulty rating) and the Zmutt ridge (D Difficulty rating). The four faces, as well as the Furggen ridge, constitute the most challenging routes to the summit. The north face is amongst the six most difficult faces of the Alps, as well as ‘The Trilogy’, the three hardest of the six, along with the north faces of the Eiger and the Grandes Jorasses (TD+ Difficulty rating).
Overcrowding on the several routes have become an issue and guides and local authorities have struggled with how to regulate the numbers. In 2015 the Hörnli hut became the first mountain shelter in Europe to limit beds.
History
Aegidius Tschudi, one of the earliest Alpine topographers and historians, was the first to mention the region around the Matterhorn in his work, De Prisca ac Vera Alpina Raethi, published in Basel in 1538. He approached the Matterhorn as a student when in his Alpine travels he reached the summit of the Theodul Pass but he does not seem to have paid any particular attention to the mountain itself.
The Matterhorn remained unstudied for more than two centuries, until a geologist from Geneva, Horace Benedict de Saussure, travelled to the mountain, which filled him with admiration. However, de Saussure was not moved to climb the mountain, and had no hope of measuring its altitude by taking a barometer to its summit. "Its precipitous sides," he wrote, "which give no hold to the very snows, are such as to afford no means of access." Yet his scientific interest was kindled by "the proud peak which rises to so vast an altitude, like a triangular obelisk, that seems to be carved by a chisel." His mind intuitively grasped the causes which gave the peak its present precipitous form: the Matterhorn was not like a perfected crystal; the centuries had laboured to destroy a great part of an ancient and much larger mountain. On his first journey de Saussure had come from Ayas to the Col des Cimes Blanches, from where the Matterhorn first comes into view; descending to Breuil, he ascended to the Theodul Pass. On his second journey, in 1792, he came to the Valtournanche, studying and describing it; he ascended to the Theodul Pass, where he spent three days, analysing the structure of the Matterhorn, whose height he was the first to measure, and collecting stones, plants and insects. He made careful observations, from the sparse lichen that clung to the rocks to the tiny but vigorous glacier fly that fluttered over the snows and whose existence at such heights was mysterious. At night he took refuge under the tent erected near the ruins of an old fort at the top of the pass. During these days he climbed the Klein Matterhorn (3,883 metres), which he named the Cime Brune du Breithorn.
The first inquirers began to come to the Matterhorn. There is a record of a party of Englishmen who in the summer of 1800 crossed the Great St. Bernard Pass, a few months after the passage of Bonaparte; they came to Aosta and thence to Valtournenche, slept at the chalets of Breuil, and traversed the Theodul Pass, which they called Monte Rosa. The Matterhorn was to them an object of the most intense and continuous admiration.
The Matterhorn is mentioned in a guide-book to Switzerland by Johann Gottfried Ebel, which was published in Zürich towards the end of the eighteenth century, and translated into English in 1818. The mountain appeared in it under the three names of Silvius, Matterhorn, and Mont Cervin, and was briefly described as one of the most splendid and wonderful obelisks in the Alps. On Zermatt there was a note: "A place which may, perhaps, interest the tourist is the valley of Praborgne (Zermatt); it is bounded by huge glaciers which come right down into the valley; the village of Praborgne is fairly high, and stands at a great height above the glaciers; its climate is almost as warm as that of Italy, and plants belonging to hot countries are to be found there at considerable altitudes, above the ice."
William Brockedon, who came to the region in 1825, considered the crossing of the Theodul Pass from Breuil to Zermatt a difficult undertaking. He gave, however, expression to his enthusiasm on the summit. When he arrived exhausted on the top of the pass, he gazed "on the beautiful pyramid of the Cervin, more wonderful than aught else in sight, rising from its bed of ice to a height of 5,000 feet, a spectacle of indescribable grandeur." In this "immense natural amphitheatre, enclosed from time immemorial by snow-clad mountains and glaciers ever white, in the presence of these grand walls the mind is overwhelmed, not indeed that it is unable to contemplate the scene, but it staggers under the immensity of those objects which it contemplates."
Those who made their way up through the Valtournanche to the foot of the mountain were few in number. W. A. B. Coolidge, a diligent collector of old and new stories of the Alps, mentions that during those years, besides Brockedon, only Hirzel-Escher of Zürich, who crossed the Theodul Pass in 1822, starting from Breuil, accompanied by a local guide. The greater number came from the Valais up the Visp valley to Zermatt. In 1813, a Frenchman, Henri Maynard, climbed to the Theodul Pass and made the first ascent of the Breithorn; he was accompanied by numerous guides, among them J. M. Couttet of Chamonix, the same man who had gone with de Saussure to the top of the Klein Matterhorn in 1792. The writings of these pioneers make much mention of the Matterhorn; the bare and inert rock is gradually quickened into life by men's enthusiasm. "Stronger minds," remarked Edward Whymper, "felt the influence of the wonderful form, and men who ordinarily spoke or wrote like rational beings, when they came under its power seemed to quit their senses, and ranted and rhapsodised, losing for a time all common forms of speech."
Among the poets of the Matterhorn during these years (1834 to 1840) were Elie de Beaumont, a famous French geologist; Pierre Jean Édouard Desor, a naturalist of Neuchâtel, who went up there with a party of friends, two of whom were Louis Agassiz and Bernhard Studer. Christian Moritz Engelhardt, who was so filled with admiration for Zermatt and its neighbourhood that he returned there at least ten times (from 1835 to 1855), described these places in two valuable volumes, drew panoramas and maps, and collected the most minute notes on the mineralogy and botany of the region. Zermatt was at that time a quiet little village, and travellers found hospitality at the parish priest's, or at the village doctor's.
In 1841 James David Forbes, professor of natural philosophy at the University of Edinburgh, came to see the Matterhorn. A philosopher and geologist, and an observant traveller, he continued the work of De Saussure in his journeys and his writings. He was full of admiration for the Matterhorn, calling it the most wonderful peak in the Alps, unsealed and unscalable. These words, pronounced by a man noted among all his contemporaries for his thorough knowledge of mountains, show what men's feelings then were towards the Matterhorn, and how at a time when the idea of Alpine exploration was gaining ground in their minds, the Matterhorn stood by itself as a mountain apart, of whose conquest it was vain even to dream. And such it remained till long after this; as such it was described by John Ball twenty years later in his celebrated guide-book. Forbes ascended the Theodul Pass in 1842, climbed the Breithorn, and came down to Breuil; as he descended from the savage scenery of the Matterhorn, the Italian landscapes of the Valtournanche seemed to him like paradise. Meanwhile, Gottlieb Samuel Studer, the geographer, together with Melchior Ulrich, was describing and mapping the topographical features of the Zermatt peaks.
Rodolphe Töpffer, who first accompanied and guided youth to the Alps for purposes of education and amusement, began his journeys in 1832, but it is only in 1840 that he mentions the Matterhorn. Two years later Töpffer and his pupils came to Zermatt. He has described this journey of his in a chapter entitled Voyage autour du Mont Blanc jusqu'à Zermatt, here he sings a hymn of praise to the Matterhorn, comparing its form with a "huge crystal of a hundred facets, flashing varied hues, that softly reflects the light, unshaded, from the uttermost depths of the heavens". Töpffer's book was illustrated by Alexandre Calame, his master and friend, with drawings of the Matterhorn, executed in the romantic style of the period. It is an artificial mountain, a picture corresponding rather with the exaggerated effect it produces on the astonished mind of the artist, than with the real form of the mountain.
About this time there came a man who studied the Matterhorn in its structure and form, and who sketched it and described it in all its parts with the curiosity of the artist and the insight of the scientist. This was John Ruskin, a new and original type of philosopher and geologist, painter and poet, whom England was enabled to create during that period of radical intellectual reforms, which led the way for the highest development of her civilisation. Ruskin was the Matterhorn's poet par excellence. He went to Zermatt in 1844, and it is to be noticed as a curious fact, that the first time he saw the Matterhorn it did not please him. The mountain on its lofty pedestal in the very heart of the Alps was, perhaps, too far removed from the ideal he had formed of the mountains; but he returned, studied and dreamt for long at its feet, and at length he pronounced it "the most noble cliff in Europe." Ruskin was no mountaineer, nor a great friend to mountaineering; he drew sketches of the mountains merely as an illustration of his teaching of the beauty of natural forms, which was the object of his whole life. In his work on Modern Painters he makes continual use of the mountains as an example of beauty and an incentive to morality. The publication of Ruskin's work certainly produced a great impression at the time on educated people in England, and a widespread desire to see the mountains.
It is a fragment of some size; a group of broken walls, one of them overhanging; crowned with a cornice, nodding some hundred and fifty feet over its massive flank, three thousand above its glacier base, and fourteen thousand above the sea, — a wall truly of some majesty, at once the most precipitous and the strongest mass in the whole chain of the Alps, the Mont Cervin.
Other men of high attainments followed, but in the years 1850 scientists and artists were about to be succeeded by real climbers and the passes and peaks around Zermatt were explored little by little. In the preface to the first volume of the Alpine Journal, which appeared in 1863, the editor Hereford Brooke George wrote that: "While even if all other objects of interest in Switzerland should be exhausted, the Matterhorn remains (who shall say for how long?) unconquered and apparently invincible." Whymper successfully reached the summit in 1865, but four men perished on the descent. The English papers discussed it with bitter words of blame; a German newspaper published an article in which Whymper was accused of cutting the rope between Douglas and Taugwalder, at the critical moment, to save his own life.
In 1890 the Federal Government was asked simultaneously by the same contractor for a concession for the Zermatt-Gornergrat railway, and for a Zermatt-Matterhorn one. The Gornergrat railway was constructed in 1896-1898 and has been working since August 1898, but there has been no more talk of the other. The project essentially consisted of a line which went up to the Hörnli, and continued thence in a rectilinear tunnel about two kilometres long, built under the ridge, and issuing near the summit on the Zmutt side. Sixty years later in 1950, Italian engineer Count Dino Lora Totino planned a cable car on the Italian side from Breuil-Cervinia to the summit. But the Alpine Museum of Zermatt sent a protest letter with 90,000 signatures to the Italian government. The latter declared the Matterhorn a natural wonder worthy of protection and refused the concession to the engineer.
2015 marked the 150th anniversary of the first ascent. Events and festivities were held throughout the year. A completely renewed Hörnli Hut opened the same year in the month of July.
In 2020, during the COVID-19 pandemic, light artist Gerry Hofstetter started projecting country flags and messages of endurance onto the mountain peak as part of a nightly series designed to show support and spread hope for everyone suffering and those fighting the pandemic.
Other mountains
Hundreds of other mountains have been compared with the Matterhorn, either for their resemblance to it or because of their apparent inaccessibility.
Mountains named after the Matterhorn
Little Matterhorn (1,480 m), Australia
Matterhorn (1,600 m), in Antarctica
Matterhorn (3,305 m), in Nevada
Matterhorn Peak (3,744 m), in California
Matterhorn Peak (4,144 m), in Colorado
Matterhorn Peak (2,636 m), in British Columbia
Neny Matterhorn (1,125 m), Antarctica
In culture
During the 20th century, the Matterhorn and the story of the first ascent in particular, inspired various artists and film producers such as Luis Trenker and Walt Disney. Large-scale replicas can be found at Disneyland and Window of the World. In 2021, a Matterhorn-related attraction opened in the Swiss Museum of Transport, enabling visitors to climb it virtually from the Solvay Hut to the summit.
Designed in 1908 by Emil Cardinaux, a leading poster artist of the time, the Matterhorn poster for the Zermatt tourist office is often considered the first modern poster. It has been described as a striking example of a marriage of tourism, patriotism and popular art. It served as decoration in many Swiss military hospices during the war in addition to be found in countless middle-class living rooms. Another affiche depicting the Matterhorn was created by Cardinaux for the chocolate brand Toblerone in the 1920s. The image of the Matterhorn first appeared on Toblerone chocolate bars in 1960. Since then, the Matterhorn has become a reference that still inspires graphic artists today and has been used extensively for all sort of publicity and advertising.
Paintings
The Matterhorn (1849), John Ruskin
The Matterhorn (1867), Albert Bierstadt
Matterhorn (1879), Edward Theodore Compton
Le Cervin (1892), Félix Vallotton
Filmography
Struggle for the Matterhorn (1928)
The Mountain Calls (1938)
The Challenge (1938)
Climbing the Matterhorn (1947)
Third Man on the Mountain (1959)
Im Banne des Berges (2015)[90]
Soarin' Around the World/Soaring Over the Horizon (2016)
The Horn (2016) - Documentary series following the mountain rescue teams in the Swiss Alps.
(Wikipedia)
Das Matterhorn (italienisch Monte Cervino oder Cervino, französisch Mont Cervin oder Le Cervin, walliserdeutsch Hore oder Horu) ist mit 4478 m ü. M. einer der höchsten Berge der Alpen. Wegen seiner markanten Gestalt und seiner Besteigungsgeschichte ist das Matterhorn einer der bekanntesten Berge der Welt. Für die Schweiz ist es ein Wahrzeichen und eine der meistfotografierten Touristenattraktionen.
Der Berg steht in den Walliser Alpen zwischen Zermatt und Breuil-Cervinia. Ost-, Nord- und Westwand liegen auf schweizerischem, die Südwand auf italienischem Staatsgebiet.
Wissenswertes über das Matterhorn vermittelt das Matterhorn Museum in Zermatt.
Geschichte des Namens
Im Allgemeinen kamen im Gebirge die Bergspitzen erst spät zu ihren Namen, die daruntergelegenen Passübergänge und Alpen jedoch meist früher. So nannte Johannes Schalbetter 1545 den heutigen Theodulpass als «Mons Siluius» (deutsch übersetzt Salasser-berg) oder deutsch Augsttalberg. Mit Augsttal ist dabei das Tal von Aosta (lateinisch Augusta Praetoria Salassorum) gemeint, das Aostatal.
«Siluius» wurde dann sehr wahrscheinlich volksetymologisch falsch interpretiert über vermeintlich lateinisch «silvius» und «silvanus» zu französisch und italienisch «Cervin/Cervin(i)». 1581 wurde das Matterhorn erstmals als Mont Cervin erwähnt, wie später Mons Silvanus und Mons Silvius. Im Jahr 1682 nannte Anton Lambien das heutige Matterhorn Matter Dioldin h[orn] (Matterhornspitze) zur Abgrenzung vom gleichnamigen Pass, der bis Mitte des 19. Jahrhunderts (beispielsweise auf der Dufourkarte) noch «Matterjoch» genannt wurde.
In der Lokalbevölkerung wird der Berg auch einfach ds Hore («das Horn», Zermatter Dialekt) oder ds Horu («das Horn», Oberwalliser Dialekt) genannt.
Geologie
Das Matterhorn ist ein Karling, und seine charakteristische Form entstand durch Erosion und Gletscherschliff in den Eiszeiten. Das Matterhorn ist Teil der Dent-Blanche-Decke des Unter-Ostalpins, also eines weit nach Westen auf die penninischen Decken der Westalpen aufgeschobenen Trümmerstücks eines ostalpinen Deckgesteins. Die untere Gesteinsschicht des Matterhorns, die bis zur Höhe der Hörnlihütte reicht, ist penninisch, also westalpin. Das im Vergleich dazu kleine Horn selbst sitzt auf dieser Basis auf und gehört zur Dent-Blanche-Decke, und zwar der untere Teil bis zur «Schulter» zur Arolla-Serie aus Orthogneisen und Metagabbros und der oberste Teil zur Valpelline-Serie aus hochmetamorphen Paragneisen der Dent-Blanche-Decke. Einfach ausgedrückt, besteht das Matterhorn aus zwei verschiedenen, schräg aufeinanderliegenden Gesteinspaketen. Der heutige Matterhorngletscher entstand erst wieder im Pessimum der Völkerwanderungszeit nach dem Optimum der Römerzeit.
Eine Besonderheit ist die charakteristische «Matterhorn-Wolke». Sie ist ein herausragendes Beispiel für einen Wolkentyp, den Meteorologen als Bannerwolke bezeichnen: Wie eine mächtige Fahne bildet sich die Wolke auf der windabgewandten Seite (Lee-Seite) des Gipfels als fast ständiger Begleiter des Berges. Die plausibelste Erklärung für ihr Entstehen ist die folgende: Das Matterhorn überragt das umgebende Gebirge wie ein Turm, so dass sich an ihm Leewirbel bilden, die feuchte Luft aus dem Tal nach oben führen, wo es zur Kondensation und Wolkenbildung kommt. Ist das Gipfelniveau erreicht, so wird die Wolke von einem waagerechten Ast des Leewirbels erfasst, der zu der typischen Fahnen-Form führt (Leewirbel-Hypothese).
Erstbesteigungen
Seit 1857 wurden mehrere erfolglose Versuche unternommen, das Matterhorn zu besteigen, zumeist von der italienischen Seite her. 1862 erstieg John Tyndall mit den Führern Johann Josef Benet, Anton Walter, Jean-Jacques und Jean-Antoine Carrel erstmals die Südwestschulter, den heutigen Pic Tyndall. Die Fortsetzung des Aufstiegs entlang des Liongrates erschien ihnen unmöglich.
Dem Erstbesteiger des Matterhorns, Edward Whymper, erschien der Liongrat weiterhin als nicht machbar. Insgesamt war er bereits sieben Mal gescheitert und überlebte u. a. einen Sturz über 60 Meter. Whymper versuchte daher, seinen Freund Jean-Antoine Carrel zu einer Besteigung von der Zermatter Seite zu überreden. Carrel beharrte darauf, von Italien her aufzusteigen.
Im Juli 1865 erfuhr Whymper zufällig von einem Gastwirt in Breuil-Cervinia, dass Carrel sich – ohne Whymper zu benachrichtigen – wieder zum Liongrat aufgemacht hatte. Whymper fühlte sich getäuscht und eilte nach Zermatt, um dort eine Gruppe für einen sofortigen Versuch über den Hörnligrat zusammenzustellen. Am 14. Juli 1865 gelang der 7er-Seilschaft Whympers die Erstbesteigung. Die Gruppe stieg über den Hörnligrat auf die Schulter; weiter oben, im Bereich der heutigen Fixseile, wich sie in die Nordwand aus. Edward Whymper erreichte als erster den Gipfel, weil er sich vor dem Gipfel vom Seil losschnitt und vorauslief. Ihm folgten der Bergführer Michel Croz (aus Chamonix), Reverend Charles Hudson, Lord Francis Douglas, D. Robert Hadow (alle aus England) sowie die Zermatter Bergführer Peter Taugwalder Vater und Peter Taugwalder Sohn. Sie sahen Carrel und seine Gruppe weit unterhalb am Pic Tyndall.
Beim Abstieg der Erstbesteiger stürzten die vorderen vier der Seilschaft (Croz, Hadow, Hudson und Douglas) noch oberhalb der «Schulter» über die Nordwand tödlich ab. Josef Marie Lochmatter brach ab dem 15. Juli 1865 mehrmals mit Rettungsmannschaften auf, um den vier Abgestürzten Erste Hilfe zu leisten. Am 19. Juli barg ein Bergungstrupp die Leichen von Croz, Hadow und Hudson auf dem Matterhorngletscher. Douglas' Leiche wurde nie gefunden.
Am 17. Juli gelang auch Carrel zusammen mit Jean-Baptiste Bich und Amé Gorret der Aufstieg über den Liongrat bis zum Gipfel. Die drei traversierten vom Nordende der italienischen Schulter durch die oberste Westwand auf den Zmuttgrat (sog. Galleria Carrel) und schlossen die Besteigung über diesen ab.
Runde Jahrestage der Erstbesteigung des Matterhorns sind feierlich begangen worden. So zeigte das Schweizer Fernsehen zum 100. Jahrestag am 14. Juli 1965 eine internationale Live-Sendung einer Matterhornbesteigung mit Beteiligung von Berg-Reportern der BBC und der RAI. Am 30. Juni 1965 zeigte das Schweizer Fernsehen den eigens produzierten Dokumentarfilm Bitterer Sieg: Die Matterhorn Story (Regie: Gaudenz Meili). Anlässlich des 150. Jahrestages wurde am 14. Juli 2015 auf dem Bahnhofplatz in Zermatt eine Countdown-Uhr aufgebaut, im Dezember 2014 wurde im Zentrum der Stadt («Matterhorn Plaza») ein Treffpunkt für das Jubiläumsjahr ins Leben gerufen.
Am 22. Juli 1871, sechs Jahre nach Whymper, bestieg die britische Alpinistin Lucy Walker als erste Frau das Matterhorn. 1869 hatten Isabella Straton und Emmeline Lewis Lloyd als reine Frauenseilschaft die Besteigung versucht; sie scheiterten kurz vor dem Gipfel. 1871 bestieg auch Anna Voigt aus Frankfurt das Matterhorn; sie war damals eine der ersten Frauen in der Sektion Frankfurt am Main des Deutschen Alpenvereins. Yvette Vaucher (* 1929) ist die erste Frau, die die Nordwand des Matterhorns bestiegen hat.
Routen
Der am weitaus häufigsten begangene Aufstiegsweg ist der Hörnligrat von Zermatt aus über die Hörnlihütte (Nordostgrat, ZS+). Er stellt den sogenannten Normalweg, also den leichtesten Aufstieg, dar. Auf 4003 Metern Höhe, nordöstlich unterhalb des Gipfels, gibt es als Biwak für Notfälle, wie Wettersturz und Zeitverzug, die von der Hörnlihütte aus betreute Solvayhütte mit zehn Notlagern. Weitere Aufstiegsrouten gibt es am Südwestgrat über den kirchendachartigen Pic Tyndall (auch Liongrat oder Italienerweg genannt, ZS+), am Nordwestgrat (Zmuttgrat, S) und am Südostgrat (Furggengrat, SS, wenig begangen). Auch durch die abweisende Nordwand verläuft eine Aufstiegsroute, die hin und wieder von Spezialisten, z. B. Walter Bonatti, gewählt wird.
(Wikipedia)
I'm an ordinary man,
Who desires nothing more than an ordinary chance,
to live exactly as he likes, and do precisely what he wants...
An average man am I, of no eccentric whim,
Who likes to live his life, free of strife,
doing whatever he thinks is best, for him,
Well... just an ordinary man...
le ore della Luna...
In the early hours of the Morning when the Light of day still did not show the silhouette of a male specimen of Alpine Chamois - Rupicapra rupicapra - attracted my attention because it stood out in the huge full Moon.
We are in the Heart of the Gran Paradiso National Park at 2,800 m (this year it will turn 100 years old and it is the oldest park in Italy) and precisely in the Cogne Valley...
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Dietro ogni scatto ci sono sempre fatiche e attese!
Zaino carico e pesante (quasi sempre) e, quando trasporti la Fotocamera con obiettivo, la Sera avverti un dolore al collo...
Ma le Passioni, è noto, comportano sempre sacrifici!
In Natura non esistono malintesi esistono solo in ciò che l'uomo chiama ragione!
ProteggiAMO tutto questo!
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La Vallée d'Aoste à ma guise - La Valle d'Aosta a modo mio - Aosta Valley in my own way
Vivre en Montagne, au quotidien, pour satisfaire la Curiosité de la Photographie de la Nature...
Valle d'Aosta - Vallée d'Aoste
(Une Montagne d'émotions...)
Clickalps Photography - Troise Carmine - Washi
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Fotocamere:
Canon 5D Mark lV
Obiettivi:
Canon EF 100-400mm f/4.5-5.6 L IS USM II
Canon EF 24-105mm f/4L IS USM II
Canon EF 16-35mm f/4L IS USM
Canon EF 50mm f/1.4 USM
Canon EF 100mm f/2.8 Macro USM
Treppiede Manfrotto 190 X Prob
Testa Manfrotto a sfera compact nera con attacco rapido 496RC2 con frizione
Piastra a sgancio rapido 200PL
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in Ombra insieme al Branco...
Raccolgo solo candide e pure Emozioni!
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Dietro ogni scatto ci sono sempre fatiche e attese!
Zaino carico e pesante (quasi sempre) e, quando trasporti la Fotocamera con obiettivo, la Sera avverti un dolore al collo...
Ma le Passioni, è noto, comportano sempre sacrifici!
In Natura non esistono malintesi esistono solo in ciò che l'uomo chiama ragione!
ProteggiAMO tutto questo!
PreoccupiAMOci della Natura il nostro futuro dipende da essa!
Osservare tutto questo è un dono, innAMÒRarsene una ricchezza!
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Inn AMÒR ati della NATURA anche tu!
Il mio tempo in Montagna!
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La Vallée d'Aoste à ma guise - La Valle d'Aosta a modo mio - Aosta Valley in my own way
Vivre en Montagne, au quotidien, pour satisfaire la Curiosité de la Photographie de la Nature...
Valle d'Aosta - Vallée d'Aoste
(Une Montagne d'émotions...)
Clickalps Photography - Troise Carmine - Washi
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Fotocamere:
Canon 5D Mark lV
Obiettivi:
Canon EF 100-400mm f/4.5-5.6 L IS USM II
Canon EF 24-105mm f/4L IS USM II
Canon EF 16-35mm f/4L IS USM
Canon EF 50mm f/1.4 USM
Canon EF 100mm f/2.8 Macro USM
Treppiede Manfrotto 190 X Prob
Testa Manfrotto a sfera compact nera con attacco rapido 496RC2 con frizione
Piastra a sgancio rapido 200PL
Telecomando infrarossi Canon RC-6
Telecomando Rollei Schermo LCD e Retroilluminazione
These are clam shells — marine bivalve mollusk shells. More precisely, they look like single valves from two different clam species, not two halves of the same animal. Bivalves include clams, oysters, mussels, and scallops, and are defined by having paired shell valves joined at a hinge.
Left shell
Likely hard clam / quahog type — Mercenaria sp., possibly Mercenaria mercenaria
Confidence: moderate
The left shell is thick, rounded-triangular to oval, dark gray-brown, and marked mostly by concentric growth bands rather than strong radial ribs. That fits the general look of a hard clam/quahog-type shell. NOAA describes northern hard clams as having thick gray-to-white shells with outer concentric growth rings; other references describe Mercenaria mercenaria as broadly triangular-oval with distinct growth lines.
What prevents a firm species ID: the interior, hinge teeth, pallial sinus, and exact locality are not visible. Those features matter for separating similar clams.
Right shell
Likely a Venus clam-type bivalve, possibly a cross-barred Venus group — Chione sp. / related Veneridae
Confidence: low to moderate
The right shell has a warm orange-brown/cream pattern and a strong crosshatched surface: concentric ridges crossed by finer radial ribs. That points toward the Venus clam family, Veneridae, especially shells with cancellate or cross-barred sculpture. The Florida Cross-barred Venus, Chione elevata, is described as having concentric ridges intercepted by denser radial ribs; the broader Veneridae family includes shells with commarginal, radial, or cancellated sculpture.
Not a firm species ID from this view alone. It could be a related Venus clam rather than Chione elevata, especially if the shell is larger than typical Chione specimens or came from outside the Florida/Caribbean/Gulf region.
Description
The image shows two contrasting clam valves on a white background:
Left: darker, smoother, more subdued; brown, gray, black, and tan horizontal banding; worn surface; low, rounded dome.
Right: larger-looking, brighter, more decorative; orange, rust, cream, and brown color zones; strong ridged texture; pronounced growth bands; more inflated and sculptural.
The pairing works visually because the shells share the same basic bivalve form but contrast strongly in color, texture, and age/wear. The left shell feels weathered and muted; the right shell feels fresher, warmer, and more patterned.
The church of San Cristobal was erected on the grounds of the first Inca Qollqanpata Palace, which belonged precisely to the first Inca “Manco Capac”, who according to the theory came from the highlands, along with his “Coya” known as “Mama Ocllo” with the mission to found the Empire of the Incas.
Cusco, often spelled Cuzco, is a city in southeastern Peru, near the Urubamba Valley of the Andes mountain range. It is the capital of the Cusco Region and of the Cusco Province.
Peru is a country in western South America. It is bordered in the north by Ecuador and Colombia, in the east by Brazil, in the southeast by Bolivia, in the south by Chile, and in the west by the Pacific Ocean.
Peru is a magical destination, abundant with ancient ruins dating back to the Incas.
Peru is the third largest country in South America, after Brazil and Argentina.