CATHEDRAL ROCK, EL CAPITAN, SENTINEL DOME AND HALF DOME BY DAVID HOCKNEY

 

DAVID HOCKNEY (bn. 1937)

Middle Cathedral Rock (2,026 m - 6,648 ft)

El Capitan (2,309 m - 7,573 ft)

Sentinel Dome (2,477 m - 8,127 ft)

Half Dome (2, 695 m - 8,844  ft)

United States of America (California)

In Yosemite I, October 16, 2011, 

iPad drawing printed on four sheets of paper, mounted on four sheets of Dibond, Private collection

Mountains of Yosemite Valley
The Middle Cathedral Rock (2,026 m- 6,648 ft)  (on right in the painting above with the cascades) is a prominent rock face on the south side of Yosemite Valley, California.
El Capitan (2,309m - 7,573 ft) (on left in the painting above) is a vertical rock formation in Yosemite National Park, located on the north side of Yosemite Valley, near its western end. The granite monolith extends about 3,000 feet (900 m) from base to summit along its tallest face and is one of the world's favorite challenges for rock climbers. The formation was named "El Capitan" by the Mariposa Battalion when it explored the valley in 1851. El Capitan ("the captain", "the chief") was taken to be a loose Spanish translation of the local Native American name for the cliff, variously transcribed as "To-to-kon oo-lah" or "To-tock-ah-noo-lah". It is unclear if the Native American name referred to a specific tribal chief or simply meant "the chief" or "rock chief". In modern times, the formation's name is often contracted to "El Cap", especially among rock climbers and BASE jumpers. 
Sentinel Dome (2,477m - 8,127ft)  (behind Cathedral rock in the painting above) is a granite dome in Yosemite National Park, United States. It lies on the south wall of Yosemite Valley, 0.8 miles (1.3 km) southwest of Glacier Point and 1.4 miles (2.3 km) northeast of Profile Cliff. Sentinel Dome is known for a Jeffrey Pine that grew from its peak (see photograph above). The pine was photographed as early as 1867 by Carleton Watkins, and was the subject of the well-known photograph by Ansel Adams. The pine died during the drought of 1976, but remained standing until August 2003. The original Native American name of Sentinel Dome, in the Southern Sierra Miwok language, was "Sakkaduch". The Bunnell survey named it "South Dome", but the Whitney survey renamed it Sentinel Dome (from its likeness to a watch-tower). The view from the top offers a 360 degree view of Yosemite Valley and surroundings. One can see Half Dome,Yosemite Falls, El Capitan, North Dome, Basket Dome, and much more.
Half Dome (2, 695 m - 8,844 ft) (behind Sentienl Dome in the painting above) is a granite dome at the eastern end of Yosemite Valley in Yosemite National Park, California, part of the Sierra Nevada Range. It is a well-known rock formation in the park, named for its distinct shape; One side is a sheer face while the other three sides are smooth and round, making it appear like a dome cut in half.  The impression from the valley floor that this is a round dome that has lost its northwest half is an illusion. From Washburn Point, Half Dome can be seen as a thin ridge of rock, an arête, that is oriented northeast-southwest, with its southeast side almost as steep as its northwest side except for the very top. Although the trend of this ridge, as well as that of Tenaya Canyon, is probably controlled by master joints, 80 percent of the northwest "half" of the original dome may well still be there. As late as the 1870s, Half Dome was described as "perfectly inaccessible" by Josiah Whitney of the California Geological Survey. The summit was finally conquered by George G. Anderson in October 1875, via a route constructed by drilling and placing iron eyebolts into the smooth granite.

The artist
David Hockney (born 9 July 1937) is an English painter, draughtsman, printmaker, stage designer and photographer. An important contributor to the pop art movement of the 1960s, he is considered one of the most influential British artists of the 20th century.
At the Royal College of Art, Hockney featured in the exhibition Young Contemporaries—alongside Peter Blake—that announced the arrival of British Pop art. He was associated with the movement, but his early works display expressionist elements, similar to some works by Francis Bacon. When the RCA said it would not let him graduate in 1962, Hockney drew the sketch The Diploma in protest. He had refused to write an essay required for the final examination, saying he should be assessed solely on his artworks. Recognising his talent and growing reputation, the RCA changed its regulations and awarded the diploma. After leaving the RCA, he taught at Maidstone College of Art for a short time. A visit to California, where he subsequently lived for many years, inspired him to make a series of paintings of swimming pools in the comparatively new acrylic medium rendered in a highly realistic style using vibrant colours. The artist moved to Los Angeles in 1964, returned to London in 1968, and from 1973 to 1975 lived in Paris.
Hockney has a home and studio in Kensington, London and two residences in California, where he has lived on and off for over 30 years: one in Nichols Canyon, Los Angeles, and an office and archives on Santa Monica Boulevard in West Hollywood, California.
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2020 - Wandering Vertexes...
by Francis Rousseau

MOUNTAINS OF YOSEMITE VALLEY PAINTED BY THOMAS HILL

 

THOMAS HILL (1829-1908)  

Middle Cathedral Rock (2,026 m - 6,648 ft)

El Capitan (2,309 m - 7,573 ft)

Sentinel Dome (2,477 m - 8,127 ft)

Half Dome (2, 695 m - 8,844  ft)

United States of America (California)

In View of Yosemite Valley oil on canvas, 1885, (92.1 x 137.8 cm), Metropolitan Museum of Art, New York, NY (not on view)



Mountains of Yosemite Valley
The Middle Cathedral Rock (2,026 m- 6,648 ft)  (on right in the painting above with the cascades) is a prominent rock face on the south side of Yosemite Valley, California.
El Capitan (2,309m - 7,573 ft) (on left in the painting above) is a vertical rock formation in Yosemite National Park, located on the north side of Yosemite Valley, near its western end. The granite monolith extends about 3,000 feet (900 m) from base to summit along its tallest face and is one of the world's favorite challenges for rock climbers. The formation was named "El Capitan" by the Mariposa Battalion when it explored the valley in 1851. El Capitan ("the captain", "the chief") was taken to be a loose Spanish translation of the local Native American name for the cliff, variously transcribed as "To-to-kon oo-lah" or "To-tock-ah-noo-lah". It is unclear if the Native American name referred to a specific tribal chief or simply meant "the chief" or "rock chief". In modern times, the formation's name is often contracted to "El Cap", especially among rock climbers and BASE jumpers.
Sentinel Dome (2,477m - 8,127ft) (behind Cathedral rock in the painting above) is a granite dome in Yosemite National Park, United States. It lies on the south wall of Yosemite Valley, 0.8 miles (1.3 km) southwest of Glacier Point and 1.4 miles (2.3 km) northeast of Profile Cliff. Sentinel Dome is known for a Jeffrey Pine that grew from its peak (see photograph above). The pine was photographed as early as 1867 by Carleton Watkins, and was the subject of the well-known photograph by Ansel Adams. The pine died during the drought of 1976, but remained standing until August 2003. The original Native American name of Sentinel Dome, in the Southern Sierra Miwok language, was "Sakkaduch". The Bunnell survey named it "South Dome", but the Whitney survey renamed it Sentinel Dome (from its likeness to a watch-tower). The view from the top offers a 360 degree view of Yosemite Valley and surroundings. One can see Half Dome,Yosemite Falls, El Capitan, North Dome, Basket Dome, and much more.
Half Dome (2, 695 m - 8,844 ft) (behind Sentinel Dome in the painting above) is a granite dome at the eastern end of Yosemite Valley in Yosemite National Park, California, part of the Sierra Nevada Range. It is a well-known rock formation in the park, named for its distinct shape; One side is a sheer face while the other three sides are smooth and round, making it appear like a dome cut in half. The impression from the valley floor that this is a round dome that has lost its northwest half is an illusion. From Washburn Point, Half Dome can be seen as a thin ridge of rock, an arête, that is oriented northeast-southwest, with its southeast side almost as steep as its northwest side except for the very top. Although the trend of this ridge, as well as that of Tenaya Canyon, is probably controlled by master joints, 80 percent of the northwest "half" of the original dome may well still be there. As late as the 1870s, Half Dome was described as "perfectly inaccessible" by Josiah Whitney of the California Geological Survey. The summit was finally conquered by George G. Anderson in October 1875, via a route constructed by drilling and placing iron eyebolts into the smooth granite.


The painter
Thomas Hill produced many fine paintings of the California landscape, in particular of the Yosemite Valley, as well as the White Mountains of New Hampshire. Hill’s work was often driven by a vision resulting from his experiences with nature.
Hill was loosely associated with the Hudson River School of painters. The Hudson River School celebrated nature with a sense of awe for its natural resources, which brought them a feeling of enthusiasm when thinking of the potential it held. Mainly the earlier members of the Hudson River School, around the 1850-60’s, displayed man as in unison with nature in their landscape paintings by often painting men on a very small scale compared to the vast landscape. Thomas Hill often brought this technique into his own paintings in for example in his painting, Yosemite Valley, 1889.
He made early trips to the White Mountains with his friend Benjamin Champney and painted White Mountain subjects throughout his career. An example of his White Mountain subjects is Mount Lafayette in his Mount Lafayette in Winter.
Hill acquired the technique of painting en plein air. These paintings in the field later served as the basis for larger finished works.
Hill’s move to California in 1861 brought him new material for his paintings. He chose monumental vistas, like Yosemite. During his lifetime, Hill’s paintings were popular in California, costing as much as $10,000. Hill's best works are considered to be these monumental subjects, including Great Canyon of the Sierra, Yosemite, Vernal Falls and Yosemite Valley.

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2020 - Wandering Vertexes...
by Francis Rousseau

HALF DOME PHOTOGRAPHED BY ANSEL ADAMS

ANSEL ADAMS (1902-1984)

Half Dome (2, 695 m - 8,844 ft)  

United States of America (California) 

In  Moon and Half Dome, Yosemite National Park, 1960 

The mountain
Half Dome (2, 695 m - 8,844 ft)   is a granite dome at the eastern end of Yosemite Valley in Yosemite National Park, California, part of the Sierra Nevada Range. It is a well-known rock formation in the park, named for its distinct shape; One side is a sheer face while the other three sides are smooth and round, making it appear like a dome cut in half. The granite crest rises more than 4,737 ft (1,444 m) above the valley floor. The impression from the valley floor that this is a round dome that has lost its northwest half is an illusion. From Washburn Point, Half Dome can be seen as a thin ridge of rock, an arête, that is oriented northeast-southwest, with its southeast side almost as steep as its northwest side except for the very top. Although the trend of this ridge, as well as that of Tenaya Canyon, is probably controlled by master joints, 80 percent of the northwest "half" of the original dome may well still be there. As late as the 1870s, Half Dome was described as "perfectly inaccessible" by Josiah Whitney of the California Geological Survey. The summit was finally conquered by George G. Anderson in October 1875, via a route constructed by drilling and placing iron eyebolts into the smooth granite.
Today, Half Dome may now be ascended in several different ways. Thousands of hikers reach the top each year by following an 8.5 mi (13.7 km) trail from the valley floor. After a rigorous 2 mi (3.2 km) approach, including several hundred feet of granite stairs, the final pitch up the peak's steep but somewhat rounded east face is ascended with the aid of a pair of post-mounted braided steel cables originally constructed close to the Anderson route in 1919.
Alternatively, over a dozen rock climbing routes lead from the valley up Half Dome's vertical northwest face. The first technical ascent was in 1957 via a route pioneered by Royal Robbins, Mike Sherrick, and Jerry Gallwas, today known as the Regular Northwest Face. Their five-day epic was the first Grade VI climb in the United States. Their route has now been free soloed several times in a few hours' time. Other technical routes ascend the south face and the west shoulder.

 The photographer
Ansel Easton Adams was an American photographer and environmentalist.
His black-and-white landscape photographs of the American West, especially Yosemite National Park, have been widely reproduced on calendars, posters, books, and the internet. Adams and Fred Archer developed the Zone System as a way to determine proper exposure and adjust the contrast of the final print. The resulting clarity and depth characterized his photographs. He primarily used large-format cameras because their high resolution helped ensure sharpness in his images. Adams founded the photography group known as Group f/64, along with fellow photographers Willard Van Dyke and Edward Weston and Imogen Cunningham.
In September 1941, Adams contracted with the Department of the Interior to make photographs of National Parks, Indian reservations, and other locations for use as mural-sized prints for decoration of the Department's new building. Part of his understanding with the Department was that he might also make photographs for his own use, using his own film and processing.
Full entry Wanderingvertexes

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2019 - Wandering Vertexes...
by Francis Rousseau 

HALF DOME PAINTED BY THOMAS HILL

 THOMAS HILL (1829-1908),

Half Dome (2, 695 m - 8,844 ft)

United States of America (California)

In Royal Arches And Half Dome, Yosemite National Park, Private collection

The mountain
Half Dome (2, 695 m - 8,844 ft) is a granite dome at the eastern end of Yosemite Valley in Yosemite National Park, California, part of the Sierra Nevada Range. It is a well-known rock formation in the park, named for its distinct shape; One side is a sheer face while the other three sides are smooth and round, making it appear like a dome cut in half. The granite crest rises more than 4,737 ft (1,444 m) above the valley floor. The impression from the valley floor that this is a round dome that has lost its northwest half is an illusion. From Washburn Point, Half Dome can be seen as a thin ridge of rock, an arête, that is oriented northeast-southwest, with its southeast side almost as steep as its northwest side except for the very top. Although the trend of this ridge, as well as that of Tenaya Canyon, is probably controlled by master joints, 80 percent of the northwest "half" of the original dome may well still be there. As late as the 1870s, Half Dome was described as "perfectly inaccessible" by Josiah Whitney of the California Geological Survey. The summit was finally conquered by George G. Anderson in October 1875, via a route constructed by drilling and placing iron eyebolts into the smooth granite.
Today, Half Dome may now be ascended in several different ways. Thousands of hikers reach the top each year by following an 8.5 mi (13.7 km) trail from the valley floor. After a rigorous 2 mi (3.2 km) approach, including several hundred feet of granite stairs, the final pitch up the peak's steep but somewhat rounded east face is ascended with the aid of a pair of post-mounted braided steel cables originally constructed close to the Anderson route in 1919.
Alternatively, over a dozen rock climbing routes lead from the valley up Half Dome's vertical northwest face. The first technical ascent was in 1957 via a route pioneered by Royal Robbins, Mike Sherrick, and Jerry Gallwas, today known as the Regular Northwest Face. Their five-day epic was the first Grade VI climb in the United States. Their route has now been free soloed several times in a few hours' time. Other technical routes ascend the south face and the west shoulder.

The painter
Thomas Hill was an American artist of the 19th century. He produced many fine paintings of the California landscape, in particular of the Yosemite Valley, as well as the White Mountains of New Hampshire. Hill’s work was often driven by a vision resulting from his experiences with nature. For Thomas Hill, Yosemite Valley and the White Mountains of New Hampshire were his sources of inspiration to begin painting and captured his direct response to nature.
Hill was loosely associated with the Hudson River School of painters. The Hudson River School celebrated nature with a sense of awe for its natural resources, which brought them a feeling of enthusiasm when thinking of the potential it held. Mainly the earlier members of the Hudson River School, around the 1850-60’s, displayed man as in unison with nature in their landscape paintings by often painting men on a very small scale compared to the vast landscape. Thomas Hill often brought this technique into his own paintings in for example in his painting, Yosemite Valley, 1889.
He made early trips to the White Mountains with his friend Benjamin Champney and painted White Mountain subjects throughout his career. An example of his White Mountain subjects is Mount Lafayette in his Mount Lafayette in Winter.
Hill acquired the technique of painting en plein air. These paintings in the field later served as the basis for larger finished works. In plein air means to “paint outdoors and directly from the landscape”,[ which Hill incorporated into many of his paintings. Hill’s landscape paintings demonstrate how he combined his powers of observation with powerful motifs in each painting.
Hill’s move to California in 1861 brought him new material for his paintings. He chose monumental vistas, like Yosemite. During his lifetime, Hill’s paintings were popular in California, costing as much as $10,000. Hill's best works are considered to be these monumental subjects, including Great Canyon of the Sierra, Yosemite, Vernal Falls and Yosemite Valley.

___________________________________________

2020 - Wandering Vertexes...
by Francis Rousseau

HALF DOME / TIS-SA-ACK PAR ANSEL ADAMS

ANSEL ADAMS (1902-1984)
Half Dome / Tis-sa-ack (2, 695 m - 8,844 ft)
Etats-Unis d'Amérique (Californie)

 

In Moon and Half Dome, Yosemite National Park, California 1960, printed 1974 Gelatin silver print
The MET, New York

Le photographe
Ansel Easton Adams est un photographe et écologiste américain, connu pour ses photographies en noir et blanc de l'Ouest américain, notamment dans la Sierra Nevada, et plus particulièrement du parc national de Yosemite. Une de ses plus célèbres photographies s'intitule Moonrise, Hernandez, Nouveau-Mexique. En collaboration avec Fred Archer, Adams développa le zone system, procédé qui permet de déterminer l'exposition correcte ainsi que l'ajustement du contraste sur le tirage final. La profondeur et la clarté qui en résultent sont la marque de fabrique des photographies d'Ansel Adams et de ceux à qui il a enseigné la technique. Dans un premier temps, Adams utilisera des appareils photographiques grand format (plus que 4 × 5 pouces), qui malgré leur taille, leur poids, le temps de mise en place et le prix des films sont un bon moyen, de par leur résolution élevée, de s'assurer du piqué de l'image. Adams fonda le Groupe f/64 avec ses amis photographes Edward Weston et Imogen Cunningham, qui à leur tour, mettront en place le département de la photographie au sein du Museum of Modern Art. Les photographies intemporelles et visuellement saisissantes d'Ansel Adams sont de nos jours encore reproduites sur une grande variété de supports : calendriers, posters, livres, faisant de ses clichés des images célèbres et reconnaissables. Une réserve de nature sauvage porte désormais son nom, au sud du parc national de Yosemite, en Californie.

La montagne
Half Dome / Tis-sa-ack (2, 695 m - 8,844 ft) « Demi Dôme » en anglais, " roche fendue » en langage amérindien, est un dôme granitique situé à l’extrémité est de la vallée de Yosemite, sans doute l’élément le plus célèbre de la vallée. Le sommet se situe à plus de 1 440 mètres au-dessus du niveau de la vallée. Half Dome est un excellent exemple de dôme d'exfoliation. Il ne fut probablement jamais un dôme complet et rond. Quand le Half Dome s’est formé, il avait déjà des fractures dans le granite. L’eau s’infiltra dans les fractures et gela, cassant la roche. Des glaciers érodèrent la base du dôme. Finalement, environ 20 % du dôme fut emporté par le glacier Tenaya, laissant derrière lui une paroi presque verticale.
Jusque dans les années 1870, on considérait que le Half Dome ne pouvait être grimpé. De nos jours, des milliers de randonneurs atteignent le sommet chaque année par la « voie normale avec les câbles ». Un itinéraire qui part du fond de la vallée et fait 13,5 kilomètres (8,5 miles) pour 1 500 mètres de dénivelé positif, avec une difficulté de « randonnée alpine » (T4). Les derniers 200 mètres d'ascension sont une dalle très inclinée (30°) équipée de câbles métalliques (posés en 1919).
D’autre part, il existe une douzaine de voies d’escalade qui mènent de la vallée au sommet à travers la face verticale nord-ouest du Half Dome. D’autres itinéraires escaladent la paroi sur la face sud et la paroi ouest. La première voie ouverte était la voie Regular Northwest Face (voie normale de la face nord-ouest), grimpée pour la première fois en 1957 par Royal Robbins, Mike Sherrick et Jerry Gallwas. Cette ascension dura 5 jours et fut la première voie de niveau VI aux États-Unis. Depuis, cette montagne f  a été le témoin d'un autre grand exploit sportif. Le 6 septembre 2007, la jeune figure montante de l'escalade en solo, Alex Honnold, a grimpé le Regular Northwest Face (voie de plus de 700 mètres (23 longueurs de corde) cotée 5.12a) sans aucune protection en seulement 2 heures et 50 minutes.
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2023 - Wandering Vertexes ....
            Errant au-dessus des Sommets Silencieux...
            Un blog de Francis Rousseau

THE HALF DOME PAINTED BY ARTHUR P. COLEMAN

ARTHUR P. COLEMAN (1852-1939)

Half Dome (2, 695 m - 8,844 ft)  

United States of America (California) 

The mountain

Half Dome (2, 695 m - 8,844 ft)   is a granite dome at the eastern end of Yosemite Valley in Yosemite National Park, California, part of the Sierra Nevada Range. It is a well-known rock formation in the park, named for its distinct shape; One side is a sheer face while the other three sides are smooth and round, making it appear like a dome cut in half. The granite crest rises more than 4,737 ft (1,444 m) above the valley floor. The impression from the valley floor that this is a round dome that has lost its northwest half is an illusion. From Washburn Point, Half Dome can be seen as a thin ridge of rock, an arête, that is oriented northeast-southwest, with its southeast side almost as steep as its northwest side except for the very top. Although the trend of this ridge, as well as that of Tenaya Canyon, is probably controlled by master joints, 80 percent of the northwest "half" of the original dome may well still be there.

As late as the 1870s, Half Dome was described as "perfectly inaccessible" by Josiah Whitney of the California Geological Survey. The summit was finally conquered by George G. Anderson in October 1875, via a route constructed by drilling and placing iron eyebolts into the smooth granite.

Today, Half Dome may now be ascended in several different ways. Thousands of hikers reach the top each year by following an 8.5 mi (13.7 km) trail from the valley floor. After a rigorous 2 mi (3.2 km) approach, including several hundred feet of granite stairs, the final pitch up the peak's steep but somewhat rounded east face is ascended with the aid of a pair of post-mounted braided steel cables originally constructed close to the Anderson route in 1919.

Alternatively, over a dozen rock climbing routes lead from the valley up Half Dome's vertical northwest face. The first technical ascent was in 1957 via a route pioneered by Royal Robbins, Mike Sherrick, and Jerry Gallwas, today known as the Regular Northwest Face. Their five-day epic was the first Grade VI climb in the United States. Their route has now been free soloed several times in a few hours' time. Other technical routes ascend the south face and the west shoulder.

The artist 

Arthur Philemon Coleman was a Canadian a geologist, professor, minerals prospector, artist, Rockies explorer, backwoods canoeist, world traveller, scientist, popular lecturer, museum administrator, memoirist and...  one of Canada’s most beloved scientist. 

Arthur Coleman is a fine example of that rare bird, a polished amateur artist whose drawings and paintings stand comfortably beside those of many professionals. He was active during the time when sketching and painting was ceding to photography the task of recording the visible world. Although he was also a photographer, painting was, for him, both a poetic and a descriptive pursuit, a way of wrapping an artistic expression around a phenomenon he was interested in or moved by. Thus motivated, Coleman's paintings give much joy and command a good deal of respect. The more surprising, perhaps given that he used to introduced himself more as a geologist than a painter.

Coleman travelled throughout the United States for professional conferences as well as geological field work.  He visited many of the major American mountain ranges including: the American Cordillera Mountains (Washington, Oregon and California); the Sierra Nevada Mountains (California and Nevada); Yellowstone National Park (Wyoming, Montana and Idaho); and the Appalachian Mountains (eastern United States). Pleistocene glaciation had extended in Northern Europe as far south as Berlin and London and covered an area of two million square miles. Coleman also visited such countries as India, Australia, Brazil, Argentina, Scandinavia, Bolivia, New Zealand, South Africa and Uruguay. In his final years he made two expeditions to the Andes in Colombia, to mountains in Southern Mexico and to two mountains in Central America.  He achieved the first ascent of Castle Mountain in 1884, and in 1907, he was the first white man to attempt to climb Mount Robson. He made a total of eight exploratory trips to the Canadian Rockies, wholly four of them looking for the mythical giants of Hooker and Brown. 

From 1901 to 1922, he was a Professor of Geology at the University of Toronto and was Dean of the Faculty of Arts from 1919 to 1922. From 1931 to 1934, he was a geologist with the Department of Mines of the Government of Ontario. He was elected a Fellow of the Royal Society of Canada in 1900 and was its President in 1921. In 1929, he was appointed Honorary Vice-President of the Royal Canadian Geographical Society.

 "Mount Coleman" and "Coleman Glacier" in Banff National Park are named in his honor. 

 He was awarded the Penrose Medal in 1936.

He planned to climb "hi" mountain, "Mount Coleman"'in the Albertan Rockies, and had also prepared a trip to British Guiana, but death intervened.

HALF DOME PEINT PAR WAYNE THIEBAUD

 

WAYNE THIEBAUD (1920-2021)
Half Dome (2, 695 m - 8,844 ft)
United States of America (California)

In Yosemite Rock Formation, Memory Mountains  huile sur toile 80,x 60 cm, 2012

A propos de la série Memory Mountains
Memory Mountains, se compose de 31 peintures et 17 œuvres sur papier qui occupe les deux étages de la Galerie Paul Thiebaud. à San Fransisco. A propos de la peinture de montagnes Watne Thiebaud au Hufftington Post :  " Un jour je me suis demandé ce qui se passerait si on essayait de voir les montagnes sous un autre angle que l'angle habituel.   En effet, en peinture,  nous les voyons le plus souvent  de loin, à moins que nous ne les escaladions. Face à cette tendance à toujours représenter les montagnes vues de loin, j'ai pris le parti dans ma série Memory Mountains,  de m'en rapprocher le plus possible pour les peindre. "

 

La montagne
Half Dome (2 695 m - 8 844 pieds) est un dôme de granit situé à l'extrémité est de la vallée de Yosemite dans le parc national de Yosemite, en Californie, qui fait partie de la chaîne de montagnes de la Sierra Nevada. C'est une formation rocheuse bien connue dans le parc, nommée pour sa forme particulière la faisant apparaître comme un dôme coupé en deux. La crête de granit s'élève à plus de 4 737 pieds (1 444 m) au-dessus du fond de la vallée. L'impression ressentie du fond de la vallée qu'il s'agit d'un dôme rond qui a perdu sa moitié nord-ouest est une illusion. De Washburn Point, Half Dome peut être vu comme une mince crête de roche, une arête orientée nord-est-sud-ouest, avec son côté sud-est presque aussi raide que son côté nord-ouest à l'exception du sommet. Jusque dans les années 1870, Half Dome était décrit comme "parfaitement inaccessible" par Josiah Whitney du California Geological Survey. Le sommet a finalement été conquis par George G. Anderson en octobre 1875, via un itinéraire élaboé en forant et en plaçant des boulons en fer dans le granit lisse.
Aujourd'hui, Half Dome peut  être escaladé de plusieurs manières différentes. Des milliers de randonneurs atteignent le sommet chaque année en suivant un sentier de 13,7 km depuis le fond de la vallée. Après une approche rigoureuse de 3,2 km (2 mi), comprenant plusieurs centaines de pieds d'escaliers en granit, la pente finale de la face est escarpée mais quelque peu arrondie du pic est montée à l'aide d'une paire de câbles en acier tressé montés sur poteau construits à l'origine près de la route Anderson en 1919.
Plus d'une douzaine de voies d'escalade mènent de la vallée à la face verticale nord-ouest du Half Dome. La première ascension technique a eu lieu en 1957 via un itinéraire lancé par Royal Robbins, Mike Sherrick et Jerry Gallwas, aujourd'hui connu sous le nom de Regular Northwest Face. Leur épopée de cinq jours a été la première ascension de grade VI aux États-Unis. Leur route a maintenant été parcourue en solo plusieurs fois en quelques heures.

 Le peintre
Morton Wayne Thiebaud était un peintre américain connu pour ses œuvres colorées représentant des objets du quotidien  - tartes, rouges à lèvres, pots de peinture, cornets de crème glacée, pâtisseries et hot-dogs - ainsi que pour ses paysages et ses peintures de personnages. Thiebaud est associé au mouvement pop art en raison de son intérêt pour les objets de la culture de masse, bien que ses premières œuvres, exécutées dans les années cinquante et soixante, soient antérieures aux œuvres des artistes pop classiques. Thiebaud a utilisé des pigments lourds et des couleurs exagérées pour représenter ses sujets, et les ombres bien définies caractéristiques des publicités sont presque toujours incluses dans son travail.
Thiebaud était opposé aux étiquettes telles que « beaux-arts » par opposition à « art commercial » et se décrivait comme « juste un peintre à l'ancienne ». Il n'aimait pas les peintures "plates" et "mécaniques" d'Andy Warhol et ne se considérait pas comme un artiste pop.
En plus des pâtisseries, Thiebaud a peint des personnages tels que Mickey Mouse ainsi que des paysages, des paysages de rue et des paysages urbains, qui ont été influencés par le travail de Richard Diebenkorn. Ses peintures telles que Sunset Streets (1985) et Flatland River (1997) sont réputées pour leur hyper réalisme et ont été comparées au travail d'Edward Hopper, un autre artiste fasciné par les scènes banales de la vie quotidienne américaine.
En 1962, le travail de Thiebaud a été inclus, avec Roy Lichtenstein, Andy Warhol, Jim Dine et Robert Dowd, dans la "Nouvelle peinture d'objets communs" historiquement importante et révolutionnaire organisée au Pasadena Art Museum. Cette exposition est considérée comme l'une des premières expositions de Pop Art aux États-Unis. Ces peintres faisaient partie d'un nouveau mouvement, à une époque de troubles sociaux, qui a choqué les États-Unis et le monde de l'art.

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2023 - Wandering Vertexes ....
Errant au-dessus des Sommets Silencieux...
Un blog de Francis Rousseau   

SENTINEL DOME & JEFFREY PINE BY ANSEL ADAMS

ANSEL ADAMS (1902-1984) 

Sentinel Dome  (2,477m - 8,127ft)

United States of America (California)  

In Jeffrey Pine, Sentinel Dome, Yosemite National Park, 1940

The mountain  and the pine 

Sentinel Dome  (2,477m - 8,127ft) is a granite dome in Yosemite National Park, United States. It lies on the south wall of Yosemite Valley, 0.8 miles (1.3 km) southwest of Glacier Point and 1.4 miles (2.3 km) northeast of Profile Cliff.

Sentinel Dome is known for a Jeffrey Pine that grew from its peak (see photograph above). The pine was photographed as early as 1867 by Carleton Watkins, and was the subject of the well-known photograph above  by Ansel Adams. The pine died during the drought of 1976, but remained standing until August 2003.

The original Native American name of Sentinel Dome, in the Southern Sierra Miwok language, was "Sakkaduch". The Bunnell survey named it "South Dome", but the Whitney survey renamed it Sentinel Dome (from its likeness to a watch-tower). The view from the top offers a 360 degree view of Yosemite Valley and surroundings. One can see Half Dome,Yosemite Falls, El Capitan,  North Dome, Basket Dome, and much more. 

The trail to the base of Sentinel Dome is a relatively easy 1.1-mile (1.8 km) hike. The trailhead, the same as the Taft Point trailhead, is located 6 miles (9.7 km) from Bridalveil Creek on the Glacier Point road. Once at the base, hikers traverse the less imposing northeast granite slope to the summit.In winter, Sentinel Dome can be reached from Badger Pass by a 10-miles ski tour.

The photographer 
Ansel Easton Adams was an American photographer and environmentalist.
His black-and-white landscape photographs of the American West, especially Yosemite National Park, have been widely reproduced on calendars, posters, books, and the internet. Adams and Fred Archer developed the Zone System as a way to determine proper exposure and adjust the contrast of the final print. The resulting clarity and depth characterized his photographs. He primarily used large-format cameras because their high resolution helped ensure sharpness in his images. Adams founded the photography group known as Group f/64, along with fellow photographers Willard Van Dyke and Edward Weston and Imogen Cunningham.
In September 1941, Adams contracted with the Department of the Interior to make photographs of National Parks, Indian reservations, and other locations for use as mural-sized prints for decoration of the Department's new building. Part of his understanding with the Department was that he might also make photographs for his own use, using his own film and processing. Although Adams kept meticulous records of his travel and expenses, he was less disciplined about recording the dates of his images, and neglected to note the date of Moonrise, so it was not clear whether it belonged to Adams or to the U.S. Government. But the position of the moon allowed the image to eventually be dated from astronomical calculations, and it was determined that Moonrise was made on November 1, 1941, a day for which he had not billed the Department, so the image belonged to Adams. The same was not true for many of his other negatives, including The Tetons and the Snake River, which, having been made for the Mural Project, became the property of the U.S. Government.
When Edward Steichen formed his Naval Aviation Photographic Unit in early 1942, he wanted Adams to be a member, to build and direct a state-of-the-art darkroom and laboratory in Washington, D.C. In February 1942, Steichen asked Adams to join. Adams agreed, with two conditions: He wanted to be commissioned as an officer, and he also told Steichen he would not be available until July 1. Steichen, who wanted the team assembled as quickly as possible, passed Adams by, and had his other photographers ready to go by early April.
Adams was distressed by the Japanese American Internment that occurred after the Pearl Harbor attack. He requested permission to visit the Manzanar War Relocation Center in the Owens Valley, at the foot of Mount Williamson. The resulting photo-essay first appeared in a Museum of Modern Art exhibit, and later was published as Born Free and Equal: The Story of Loyal Japanese-Americans. He also contributed to the war effort by doing many photographic assignments for the military, including making prints of secret Japanese installations in the Aleutians. " It was met with some distressing resistance and was rejected by many as disloyal." Adams was the recipient of three Guggenheim fellowships during his career, the first in 1946 to photograph every National Park. This series of photographs produced memorable images of Old Faithful Geyser, Grand Teton (above), and Mount McKinley....
Full entry Wanderingvertexes

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2019 - Wandering Vertexes...
by Francis Rousseau 

MOUNT ST HELENS BY EMMET GOWIN

EMMET GOWIN (bn. 1941) 

Mount St. Helens or Louwala-Clough (2, 549 m - 8, 363 ft) 

United States of America (Washington State)

1. Debris flow at the northern base of Mounts Helens, 1980

2. Ash over new snow on the  South flank of Mount St Helens, 1982

3. Ashes after Mount St Helens 1980 Plinian eruption, 1982 

The mountain 
Mount St. Helens ( 2, 549m- 8,363 ft )  or Louwala-Clough (known as Lawetlat'la to the Cowlitz people, and Loowit to the Klickitat people) is an active stratovolcano located in Skamania County, Washington, in the Pacific Northwest region of the United States. It is 96 miles (154 km) south of Seattle, Washington, and 50 miles (80 km) northeast of Portland, Oregon. Mount St. Helens takes its English name from the British diplomat Lord St Helens, a friend of explorer George Vancouver who made a survey of the area in the late 18th century.The volcano is located in the Cascade Range and is part of the Cascade Volcanic Arc, a segment of the Pacific Ring of Fire that includes over 160 active volcanoes. This volcano is well known for its ash explosions and pyroclastic flows.
Mount St. Helens is most notorious for its major 1980 eruption, the deadliest and most economically destructive volcanic event in the history of the United States. The magma in St. Helens burst forth into a large-scale pyroclastic flow that flattened vegetation and buildings over 230 square miles (600 km2). More than 1.5 million metric tons of sulfur dioxide were released into the atmosphere. On the Volcanic Explosivity Index scale, the eruption was rated a five (a Plinian eruption). Fifty-seven people were killed; 250 homes, 47 bridges, 15 miles (24 km) of railways, and 185 miles (298 km) of highway were destroyed. A massive debris avalanche triggered by an earthquake measuring 5.1 on the Richter scale caused an eruption that reduced the elevation of the mountain's summit from 9,677 ft (2,950 m) to 8,363 ft (2,549 m), leaving a 1 mile (1.6 km) wide horseshoe-shaped crater. The debris avalanche was up to 0.7 cubic miles (2.9 km3) in volume. For more than nine hours, a vigorous plume of ash erupted, eventually reaching 12 to 16 miles (20 to 27 km) above sea level.  The plume moved eastward at an average speed of 60 miles per hour (100 km/h) with ash reaching Idaho by noon. Ashes from the eruption were found collecting on top of cars and roofs next morning, as far as the city of Edmonton in Alberta, Canada. The Mount St. Helens National Volcanic Monument was created to preserve the volcano and allow for its aftermath to be scientifically studied.
As with most other volcanoes in the Cascade Range, Mount St. Helens is a large eruptive cone consisting of lava rock interlayered with ash, pumice, and other deposits. The mountain includes layers of basalt and andesite through which several domes of dacite lava have erupted. The largest of the dacite domes formed the previous summit, and off its northern flank sat the smaller Goat Rocks dome. Both were destroyed in the 1980 eruption.
Between 1980 and 1986, activity continued at Mount St. Helens, with a new lava dome forming in the crater. Numerous small explosions and dome-building eruptions occurred. From December 7, 1989, to January 6, 1990, and from November 5, 1990, to February 14, 1991, the mountain erupted with sometimes huge clouds of ash.
Magma reached the surface of the volcano about October 11, 2004, resulting in the building of a new lava dome on the existing dome's south side. This new dome continued to grow throughout 2005 and into 2006. Several transient features were observed, such as a lava spine nicknamed the "whaleback," which comprised long shafts of solidified magma being extruded by the pressure of magma beneath. These features were fragile and broke down soon after they were formed. On July 2, 2005, the tip of the whaleback broke off, causing a rockfall that sent ash and dust several hundred meters into the air.
Mount St. Helens showed significant activity on March 8, 2005, when a 36,000-foot (11,000 m) plume of steam and ash emerged—visible from Seattle. This relatively minor eruption was a release of pressure consistent with ongoing dome building. The release was accompanied by a magnitude 2.5 earthquake. Another feature to emerge from the dome was called the "fin" or "slab." Approximately half the size of a football field, the large, cooled volcanic rock was being forced upward as quickly as 6 ft (2 m) per day.
In mid-June 2006, the slab was crumbling in frequent rockfalls, although it was still being extruded. The height of the dome was 7,550 feet (2,300 m), still below the height reached in July 2005 when the whaleback collapsed. On October 22, 2006, the collapse and avalanche of the lava dome sent an ash plume 2,000 feet (600 m) over the western rim of the crater; the ash plume then rapidly dissipated. On December 19, 2006, a large white plume of condensing steam was observed, leading some media people to assume there had been a small eruption. However, the Cascades Volcano Observatory of the USGS did not mention any significant ash plume.  The volcano was in continuous eruption from October 2004, but this eruption consisted in large part of a gradual extrusion of lava forming a dome in the crater.
On January 16, 2008, steam began seeping from a fracture on top of the lava dome. Associated seismic activity was the most noteworthy since 2004. Scientists suspended activities in the crater and the mountain flanks, but the risk of a major eruption was deemed low.] By the end of January, the eruption paused; no more lava was being extruded from the lava dome.
On July 10, 2008, it was determined that the eruption had ended, after more than six months of no volcanic activity.
Source:
 - Wikipedia 

The photographer 
Emmet Gowin (born 1941 in Danville, Virginia) is an American photographer. He first gained attention in the 1970s with his intimate portraits of his wife, Edith, and her family. Later he turned his attention to the landscapes of the American West, taking aerial photographs of places that had been changed by humans or nature, including the Hanford Site, Mount St. Helens(see below), and the Nevada Test Site. Gowin taught at Princeton University for 25 years.
After graduating from high school he attended the Richmond Professional Institute (now Virginia Commonwealth University). During his first year in college he saw a catalog of the Family of Man exhibit and was particularly inspired by the works of Robert Frank and Henri Cartier-Bresson.
In 1970 his work was shown at the George Eastman House and a year later at the Museum of Modern Art. About this same time he was introduced to the photographer Frederick Sommer, who became his lifelong mentor and friend. Gowin received a Guggenheim Fellowship in 1974, which allowed him to travel throughout Europe. He was also awarded a National Endowment for the Arts Fellowship in 1979 and a Pew Fellowship in the Arts in 1994.
In 1980 Gowin received a scholarship from the Seattle Arts Commission which provided funding for him to travel in Washington and the Pacific Northwest. Beginning with a trip to Mount St. Helens soon after it erupted, Gowin began taking aerial photographs (see below). For the next twenty years, Gowin captured strip mining sites, nuclear testing fields, large-scale agricultural fields and other scars in the natural landscape.
In 1982 the Gowins were invited by Queen Noor of Jordan, who had studied with Gowin at Princeton, to photograph historic places in her country. He traveled there over the next three years and took a series of photographs of the archaeological site at Petra. The prints he made of these images were the first time he introduced photographic print toning in his work.
Gowin retired from teaching at Princeton University at the end of 2009  and lives in Pennsylvania with his wife Edith.
Gowin once said that : "The coincidence of the many things that fit together to make a picture is singular. They occur only once. The never occur for you in quite the same way that they occur for someone else, so that in the tiny differences between them you can reemploy a model or strategy that someone else has used and still reproduce an original picture. Those things that do have a distinct life of their own strike me as being things coming to you out of life itself."
In an essay for the catalog for an exhibition of his work at Yale University, writer Terry Tempest Williams said "Emmet Gowin has captured on film the state of our creation and, conversely, the beauty of our losses. And it is full of revelations."

MOUNT TARAWERA (2) PAINTED BY CHARLES BLOMFIELD

 

CHARLES BLOMFIELD (1848-1926)

Mount Tarawera (1, 111m - 3,645ft) 

New Zealand (North Island)

  In  White Terraces, oil on canvas, 1882, Museum of New Zeland Te Papa Tongarewa 

The full extraordinsary story  of this unbelievable volcano  in paintings is HERE

 

The mountain 
Mount Tarawera (1, 111m - 3,645ft) is the volcano responsible for one of New Zealand's largest historic eruptions. Located 24 kilometres southeast of Rotorua in the North Island, it consists of a series of rhyolitic lava domes that were fissured down the middle by an explosive basaltic eruption in 1886, which killed an estimated 120 people. These fissures run for about 17 kilometres northeast-southwest.
The volcano's component domes include Ruawahia Dome, Tarawera Dome and Wahanga Dome. It is surrounded by several lakes, most of which were created or drastically altered by the 1886 eruption. These lakes include Lakes Tarawera, Rotomahana, Rerewhakaaitu, Okataina, Okareka, Tikitapu (Blue Lake) and Rotokakahi (Green Lake). The Tarawera River runs northeastwards across the northern flank of the mountain from Lake Tarawera.
Main eruptions 
- 1315 : Mount Tarawera erupted for the fist time on modern history. The ash thrown from this event may have affected temperatures around the globe and precipitated the Great Famine of 1315–17 in Europe.
- 1886 : Shortly after midnight on the morning of 10 June 1886, a series of more than 30 increasingly strong earthquakes were felt in the Rotorua area and an unusual sheet lightning display was observed from the direction of Tarawera. At around 2:00 am a larger earthquake was felt and followed by the sound of an explosion. By 2:30 am Mount Tarawera's three peaks had erupted, blasting three distinct columns of smoke and ash thousands of metres into the sky (see painting above). At around 3.30 am, the largest phase of the eruption commenced; vents at Rotomahana produced a pyroclastic surge that destroyed several villages within a 6 kilometre radius, and the Pink and White Terraces appeared to be obliterated.
The eruption was heard clearly as far away as Blenheim and the effects of the ash in the air were observed as far south as Christchurch, over 800 km away. In Auckland the sound of the eruption and the flashing sky was thought by some to be an attack by Russian warships.
Although the official contemporary death toll was 153, exhaustive research by physicist Ron Keam only identified 108 people killed by the eruption. Much of the discrepancy was due to misspelled names and other duplications. Allowing for some unnamed and unknown victims, he estimated that the true death toll was 120 at most.  Some people claim that many more people died.
The eruption also buried many Māori villages, including Te Wairoa which has now become a tourist attraction (Buried Village of Te Wairoa) and the world-famous Pink and White Terraces were lost. A small portion of the Pink Terraces was rediscovered under Lake Rotomahana 125 years later. Approximately 2 cubic kilometres of tephra was erupted, more than Mount St. Helens ejected in 1980. Many of the lakes surrounding the mountain had their shapes and areas dramatically altered, especially the eventual enlargement of Lake Rotomahana, the largest crater involved in the eruption, as it re-filled with water.
Legend
One legend surrounding the 1886 eruption is that of the phantom canoe. Eleven days before the eruption, a boat full of tourists returning from the Terraces saw what appeared to be a war canoe approach their boat, only to disappear in the mist half a mile from them. One of the witnesses was a clergyman, a local Maori man from the Te Arawa iwi. Nobody around the lake owned such a war canoe, and nothing like it had been seen on the lake for many years. It is possible that the rise and fall of the lake level caused by pre eruption fissures had freed a burial waka (canoe) from its resting place. Traditionally dead chiefs were tied in an upright position. A number of letters have been published from the tourists who experienced the event.
Though skeptics maintained that it was a freak reflection seen on the mist, tribal elders at Te Wairoa claimed that it was a waka wairua (spirit canoe) and was a portent of doom. It has been suggested that the waka was actually a freak wave on the water, caused by seismic activity below the lake, but locals believe that a future eruption will be signaled by the reappearance of the canoe.

The painter 

 Charles Blomfield  was a New Zealand decorator, artist and music teacher born in London, England.

A widow, Blomfield's mother brought her family to New Zealand in the 1860's intending to settle in Northland as part of a settlement called Albertland. On arrival in Auckland they decided not to proceed on Northland to become farmers but to pursue urban trades in Auckland. The family remained in Auckland after that and many of the descendants of the various children still reside in the Auckland area.

Charles Blomfield lived in Freeman's Bay - 40 Wood Street, in a house built by his brother and allegedly made out of the timber from one large Kauri tree. As well as an exhibiting easel painter Blomfield worked as a sign-writer and interior decorator; for this trade he maintained studios in shops at various times. These were usually on Karangahape Road, one of these was shared with his daughter who made a living painting floral pieces which she also exhibited at the Auckland Society of Arts.

Blomfield travelled throughout the centre of the North Island on several occasions in the 1870s and 80s creating many landscape paintings of the New Zealand countryside, often for sale to visitors to New Zealand. He was fortunate to view the famed Pink and White Terraces several times and paint them before they were destroyed by the eruption of Tarawera in 1886. His meticulous sketches and finished paintings are some of the main records of them (see above).  For the remainder of his life he was probably able to rely on new versions of his classic views of them to supplement his income.

His paintings are widely regarded as the epitome of 19th century New Zealand landscape art, although his work, like many of his contemporaries, fell out of fashion during the 20th century, only to be re-evaluated in the 1970s. He was unable to come to terms with developments in art and remained staunchly conservative and hostile to 'modern art'. In his later years he found himself increasingly sidelined by the artistic circles in Auckland which he had previously shone in and was probably embittered by this.

Blomfield died at his residence in Wood Street in 1926. He was survived by several children. One of his brothers, William, was a noted newspaper cartoonist.

 Source : 

- Museum of New Zeland Te Papa Tongarewa

 

 _____________________________________
2022 - Wandering Vertexes...
Un blog de Francis Rousseau 

MOUNT TARAWERA / PINK TERRACES BY JOHN BARR CLARK HOYTE

JOHN BARR CLARK HOYTE (1835-1913)

Mount Tarawera (1, 111m - 3,645ft) 

 New Zealand

In The pink terraces, Mount Tarawera, oil on canvas

The mountain 
Mount Tarawera (1, 111m - 3,645ft) is the volcano responsible for one of New Zealand's largest historic eruptions. Located 24 kilometres southeast of Rotorua in the North Island, it consists of a series of rhyolitic lava domes that were fissured down the middle by an explosive basaltic eruption in 1886, which killed an estimated 120 people. These fissures run for about 17 kilometres northeast-southwest.
The volcano's component domes include Ruawahia Dome, Tarawera Dome and Wahanga Dome. It is surrounded by several lakes, most of which were created or drastically altered by the 1886 eruption. These lakes include Lakes Tarawera, Rotomahana, Rerewhakaaitu, Okataina, Okareka, Tikitapu (Blue Lake) and Rotokakahi (Green Lake). The Tarawera River runs northeastwards across the northern flank of the mountain from Lake Tarawera.
Main eruptions 
- 1315 : Mount Tarawera erupted for the fist time on modern history. The ash thrown from this event may have affected temperatures around the globe and precipitated the Great Famine of 1315–17 in Europe.
- 1886 : Shortly after midnight on the morning of 10 June 1886, a series of more than 30 increasingly strong earthquakes were felt in the Rotorua area and an unusual sheet lightning display was observed from the direction of Tarawera. At around 2:00 am a larger earthquake was felt and followed by the sound of an explosion. By 2:30 am Mount Tarawera's three peaks had erupted, blasting three distinct columns of smoke and ash thousands of metres into the sky (see painting above). At around 3.30 am, the largest phase of the eruption commenced; vents at Rotomahana produced a pyroclastic surge that destroyed several villages within a 6 kilometre radius, and the Pink and White Terraces appeared to be obliterated.
The eruption was heard clearly as far away as Blenheim and the effects of the ash in the air were observed as far south as Christchurch, over 800 km away. In Auckland the sound of the eruption and the flashing sky was thought by some to be an attack by Russian warships.
Although the official contemporary death toll was 153, exhaustive research by physicist Ron Keam only identified 108 people killed by the eruption. Much of the discrepancy was due to misspelled names and other duplications. Allowing for some unnamed and unknown victims, he estimated that the true death toll was 120 at most.  Some people claim that many more people died.
The eruption also buried many Māori villages, including Te Wairoa which has now become a tourist attraction (Buried Village of Te Wairoa) and the world-famous Pink and White Terraces were lost. A small portion of the Pink Terraces was rediscovered under Lake Rotomahana 125 years later. Approximately 2 cubic kilometres of tephra was erupted, more than Mount St. Helens ejected in 1980. Many of the lakes surrounding the mountain had their shapes and areas dramatically altered, especially the eventual enlargement of Lake Rotomahana, the largest crater involved in the eruption, as it re-filled with water.
Legend
One legend surrounding the 1886 eruption is that of the phantom canoe. Eleven days before the eruption, a boat full of tourists returning from the Terraces saw what appeared to be a war canoe approach their boat, only to disappear in the mist half a mile from them. One of the witnesses was a clergyman, a local Maori man from the Te Arawa iwi. Nobody around the lake owned such a war canoe, and nothing like it had been seen on the lake for many years. It is possible that the rise and fall of the lake level caused by pre eruption fissures had freed a burial waka (canoe) from its resting place. Traditionally dead chiefs were tied in an upright position. A number of letters have been published from the tourists who experienced the event.
Though skeptics maintained that it was a freak reflection seen on the mist, tribal elders at Te Wairoa claimed that it was a waka wairua (spirit canoe) and was a portent of doom. It has been suggested that the waka was actually a freak wave on the water, caused by seismic activity below the lake, but locals believe that a future eruption will be signaled by the reappearance of the canoe.

The Painter 
John Barr Clark Hoyte was born in England, probably in London,  Nothing is known of Hoyte's education and artistic training and we are reduced to the obvious deduction that he was heir to the English tradition of topographic draughtsmanship and watercolour painting. Firm drawing underlies his landscapes, making it appropriate to group him with colonial surveyor–architect artists such as Edward Ashworth, Edmund Norman and George O'Brien.
During his years in New Zealand John Hoyte travelled assiduously in search of new scenes to exploit.   His pictorial exploration of the colony's principal dramatic landscapes was completed when he took a cruise circumnavigating the South Island in early 1877, exploring the coast of Fiordland with particular attention. New Zealand subjects would continue to inspire his production long after he had settled in Australia, where they shared his attention with coastal and mountain views drawn chiefly from the neighbourhood of Sydney.
Despite his apparent commercial success, however, Hoyte's standing, like that of George O'Brien, waned in the 1870s: a decade which marked a major shift in New Zealand colonial taste as the Turnerian Romantics such as Gully, J. C. Richmond and W. M. Hodgkins moved into greater prominence. They and their style were to dominate the following decades.

2019 - Wandering Vertexes...

by Francis Rousseau 

MOUNT TARAWERA AND TERRACES BY JOHN HOYTE

JOHN HOYTE (1835-1913) 

Mount Tarawera (1, 111m - 3,645ft)

New Zealand

1.  In  White Terraces, Tepapa, oil on canvas, 1875,

The mountain 
Mount Tarawera (1, 111m - 3,645ft) is the volcano responsible for one of New Zealand's largest historic eruptions. Located 24 kilometres southeast of Rotorua in the North Island, it consists of a series of rhyolitic lava domes that were fissured down the middle by an explosive basaltic eruption in 1886, which killed an estimated 120 people. These fissures run for about 17 kilometres northeast-southwest.
The volcano's component domes include Ruawahia Dome, Tarawera Dome and Wahanga Dome. It is surrounded by several lakes, most of which were created or drastically altered by the 1886 eruption. These lakes include Lakes Tarawera, Rotomahana, Rerewhakaaitu, Okataina, Okareka, Tikitapu (Blue Lake) and Rotokakahi (Green Lake). The Tarawera River runs northeastwards across the northern flank of the mountain from Lake Tarawera.
Main eruptions 
- 1315 : Mount Tarawera erupted for the fist time on modern history. The ash thrown from this event may have affected temperatures around the globe and precipitated the Great Famine of 1315–17 in Europe.
- 1886 : Shortly after midnight on the morning of 10 June 1886, a series of more than 30 increasingly strong earthquakes were felt in the Rotorua area and an unusual sheet lightning display was observed from the direction of Tarawera. At around 2:00 am a larger earthquake was felt and followed by the sound of an explosion. By 2:30 am Mount Tarawera's three peaks had erupted, blasting three distinct columns of smoke and ash thousands of metres into the sky (see painting above). At around 3.30 am, the largest phase of the eruption commenced; vents at Rotomahana produced a pyroclastic surge that destroyed several villages within a 6 kilometre radius, and the Pink and White Terraces appeared to be obliterated.
The eruption was heard clearly as far away as Blenheim and the effects of the ash in the air were observed as far south as Christchurch, over 800 km away. In Auckland the sound of the eruption and the flashing sky was thought by some to be an attack by Russian warships.
Although the official contemporary death toll was 153, exhaustive research by physicist Ron Keam only identified 108 people killed by the eruption. Much of the discrepancy was due to misspelled names and other duplications. Allowing for some unnamed and unknown victims, he estimated that the true death toll was 120 at most.  Some people claim that many more people died.
The eruption also buried many Māori villages, including Te Wairoa which has now become a tourist attraction (Buried Village of Te Wairoa) and the world-famous Pink and White Terraces were lost. A small portion of the Pink Terraces was rediscovered under Lake Rotomahana 125 years later. Approximately 2 cubic kilometres of tephra was erupted, more than Mount St. Helens ejected in 1980. Many of the lakes surrounding the mountain had their shapes and areas dramatically altered, especially the eventual enlargement of Lake Rotomahana, the largest crater involved in the eruption, as it re-filled with water.
Legend
One legend surrounding the 1886 eruption is that of the phantom canoe. Eleven days before the eruption, a boat full of tourists returning from the Terraces saw what appeared to be a war canoe approach their boat, only to disappear in the mist half a mile from them. One of the witnesses was a clergyman, a local Maori man from the Te Arawa iwi. Nobody around the lake owned such a war canoe, and nothing like it had been seen on the lake for many years. It is possible that the rise and fall of the lake level caused by pre eruption fissures had freed a burial waka (canoe) from its resting place. Traditionally dead chiefs were tied in an upright position. A number of letters have been published from the tourists who experienced the event.
Though skeptics maintained that it was a freak reflection seen on the mist, tribal elders at Te Wairoa claimed that it was a waka wairua (spirit canoe) and was a portent of doom. It has been suggested that the waka was actually a freak wave on the water, caused by seismic activity below the lake, but locals believe that a future eruption will be signaled by the reappearance of the canoe.

 The artist 
John Barr Clark Hoyte (1835 –1913) was a New Zealand artist and teacher. He was born in London, England. During his years in New Zealand John Hoyte travelled assiduously in search of new scenes to exploit. In January 1866 he exhibited views from Whangarei, Coromandel, Auckland, Waikato, the Wellington region and Nelson, although some of these pictures were not painted from the subject. In the 1870s he travelled each summer, progressively adding the thermal region, Taranaki, Nelson, Christchurch, Arthur's Pass, Banks Peninsula and Otago to his repertoire between 1872 and 1876. His pictorial exploration of the colony's principal dramatic landscapes was completed when he took a cruise circumnavigating the South Island in early 1877, exploring the coast of Fiordland with particular attention. New Zealand subjects would continue to inspire his production long after he had settled in Australia, where they shared his attention with coastal and mountain views drawn chiefly from the neighbourhood of Sydney.
Hoyte brought a professional determination to his career. He exhibited paintings whenever and wherever he could, in his home and studio, at fêtes and fairs and in many formal art exhibitions in both New Zealand and Australia. He was tireless in his support of formal structures for the embryonic antipodean art world.

MOUNT TARAWERA AND THE TERRACES BY CHARLES BLOMFIELD

CHARLES BLOMFIELD (1848-1926)

Mount Tarawera (1, 111m - 3,645ft) 

New Zealand (North Island)

1. In White Terraces,  Lake Rotomahana, 1885, oil on canvas,  Auckland Art Gallery Toi O Tamaki 

2. In  The Terraces, 1886, oil on canvas, Museum of New Zeland Te Papa Tongarewa

3. In Mount Tarawera in eruption on June 1886,  Museum of New Zeland Te Papa Tongarewa

4. In Mount Tarawera after eruption,1900 oil on canvas, Private collection 

The mountain 
Mount Tarawera (1, 111m - 3,645ft) is the volcano responsible for one of New Zealand's largest historic eruptions. Located 24 kilometres southeast of Rotorua in the North Island, it consists of a series of rhyolitic lava domes that were fissured down the middle by an explosive basaltic eruption in 1886, which killed an estimated 120 people. These fissures run for about 17 kilometres northeast-southwest.
The volcano's component domes include Ruawahia Dome, Tarawera Dome and Wahanga Dome. It is surrounded by several lakes, most of which were created or drastically altered by the 1886 eruption. These lakes include Lakes Tarawera, Rotomahana, Rerewhakaaitu, Okataina, Okareka, Tikitapu (Blue Lake) and Rotokakahi (Green Lake). The Tarawera River runs northeastwards across the northern flank of the mountain from Lake Tarawera.
Main eruptions 
- 1315 : Mount Tarawera erupted for the fist time on modern history. The ash thrown from this event may have affected temperatures around the globe and precipitated the Great Famine of 1315–17 in Europe.
- 1886 : Shortly after midnight on the morning of 10 June 1886, a series of more than 30 increasingly strong earthquakes were felt in the Rotorua area and an unusual sheet lightning display was observed from the direction of Tarawera. At around 2:00 am a larger earthquake was felt and followed by the sound of an explosion. By 2:30 am Mount Tarawera's three peaks had erupted, blasting three distinct columns of smoke and ash thousands of metres into the sky (see painting above). At around 3.30 am, the largest phase of the eruption commenced; vents at Rotomahana produced a pyroclastic surge that destroyed several villages within a 6 kilometre radius, and the Pink and White Terraces appeared to be obliterated.
The eruption was heard clearly as far away as Blenheim and the effects of the ash in the air were observed as far south as Christchurch, over 800 km away. In Auckland the sound of the eruption and the flashing sky was thought by some to be an attack by Russian warships.
Although the official contemporary death toll was 153, exhaustive research by physicist Ron Keam only identified 108 people killed by the eruption. Much of the discrepancy was due to misspelled names and other duplications. Allowing for some unnamed and unknown victims, he estimated that the true death toll was 120 at most.  Some people claim that many more people died.
The eruption also buried many Māori villages, including Te Wairoa which has now become a tourist attraction (Buried Village of Te Wairoa) and the world-famous Pink and White Terraces were lost. A small portion of the Pink Terraces was rediscovered under Lake Rotomahana 125 years later. Approximately 2 cubic kilometres of tephra was erupted, more than Mount St. Helens ejected in 1980. Many of the lakes surrounding the mountain had their shapes and areas dramatically altered, especially the eventual enlargement of Lake Rotomahana, the largest crater involved in the eruption, as it re-filled with water.
Legend
One legend surrounding the 1886 eruption is that of the phantom canoe. Eleven days before the eruption, a boat full of tourists returning from the Terraces saw what appeared to be a war canoe approach their boat, only to disappear in the mist half a mile from them. One of the witnesses was a clergyman, a local Maori man from the Te Arawa iwi. Nobody around the lake owned such a war canoe, and nothing like it had been seen on the lake for many years. It is possible that the rise and fall of the lake level caused by pre eruption fissures had freed a burial waka (canoe) from its resting place. Traditionally dead chiefs were tied in an upright position. A number of letters have been published from the tourists who experienced the event.
Though skeptics maintained that it was a freak reflection seen on the mist, tribal elders at Te Wairoa claimed that it was a waka wairua (spirit canoe) and was a portent of doom. It has been suggested that the waka was actually a freak wave on the water, caused by seismic activity below the lake, but locals believe that a future eruption will be signaled by the reappearance of the canoe.
Source: 
 - National Museum of Natural History

The painter 

 Charles Blomfield  was a New Zealand decorator, artist and music teacher born in London, England.

A widow, Blomfield's mother brought her family to New Zealand in the 1860's intending to settle in Northland as part of a settlement called Albertland. On arrival in Auckland they decided not to proceed on Northland to become farmers but to pursue urban trades in Auckland. The family remained in Auckland after that and many of the descendants of the various children still reside in the Auckland area.

Charles Blomfield lived in Freeman's Bay - 40 Wood Street, in a house built by his brother and allegedly made out of the timber from one large Kauri tree. As well as an exhibiting easel painter Blomfield worked as a sign-writer and interior decorator; for this trade he maintained studios in shops at various times. These were usually on Karangahape Road, one of these was shared with his daughter who made a living painting floral pieces which she also exhibited at the Auckland Society of Arts.

Blomfield travelled throughout the centre of the North Island on several occasions in the 1870s and 80s creating many landscape paintings of the New Zealand countryside, often for sale to visitors to New Zealand. He was fortunate to view the famed Pink and White Terraces several times and paint them before they were destroyed by the eruption of Tarawera in 1886. His meticulous sketches and finished paintings are some of the main records of them (see above).  For the remainder of his life he was probably able to rely on new versions of his classic views of them to supplement his income.

His paintings are widely regarded as the epitome of 19th century New Zealand landscape art, although his work, like many of his contemporaries, fell out of fashion during the 20th century, only to be re-evaluated in the 1970s. He was unable to come to terms with developments in art and remained staunchly conservative and hostile to 'modern art'. In his later years he found himself increasingly sidelined by the artistic circles in Auckland which he had previously shone in and was probably embittered by this.

Blomfield died at his residence in Wood Street in 1926. He was survived by several children. One of his brothers, William, was a noted newspaper cartoonist.

 Source : 

- Museum of New Zeland Te Papa Tongarewa