LE MONT RAINIER PEINT PAR ALBERT BIERSTADT

ALBERT BIERSTADT (1830-1902)
Mont Rainier (4.932m)
Etats-Unis (Etat de Washington)

In Mount Rainier, 1876, oil on canvas, Smithsonian American Art Museum.

 

Le volcan
Le mont Rainier (4.932m) est un volcan situé dans l'État de Washington, aux États-Unis. Il constitue le point culminant de l'État et de la chaîne des Cascades. Il est recouvert par une importante calotte glaciaire. C'est un stratovolcan actif de l'arc volcanique des Cascades, dont la dernière éruption remonterait à la fin du 19e siècle. Situé à une centaine de kilomètres au sud-sud-est de l'agglomération de Seattle, il présente des risques pour les populations et les infrastructures environnantes, notamment en raison des potentiels lahars. Découvert par les premiers Européens en 1792 lors d'un voyage d'exploration mené par George Vancouver, le volcan tire son nom de son ami, le contre-amiral dans la Royal Navy Peter Rainier. Sa première ascension remonte à 1870. Dans les années 1890, la nécessité de protéger ses ressources naturelles et économiques est démontrée ; il est ainsi intégré au Parc national du mont Rainier, qui attire depuis une foule de visiteurs en quête de nature et d'alpinistes à la recherche de sommets. Son ascension présente des difficultés liées à la météorologie et à l'évolution en milieu glaciaire.
Le sommet du mont Rainier possède trois cimes : la plus élevée se nomme Columbia Crest ; la deuxième est Point Success (4 315 mètres), une cime secondaire au sud-ouest, et la troisième Liberty Cap (4 303 mètres et 151 mètres de proéminence) au nord-ouest. Sur le flanc oriental se trouve également le pic Little Tahoma à 3 394 mètres, qui est un vestige érodé du mont Rainier lorsqu'il était encore plus élevé ; avec 256 mètres de proéminence et en dehors des voies principales vers le sommet du mont Rainier, il peut être considéré comme un sommet distinct et, le cas échéant, le troisième plus élevé de l'État de Washington après le mont Adams.

Le peintre
Albert Bierstadt est un peintre allemand naturalisé américain. Connu pour ses paysages de l'Ouest americain Bierstadt faisait partie de l’Hudson River School, un groupe informel de peintres du xixe siècle pratiquant une peinture romantique, baignée d’une lumière radieuse qui lui valu taussi l'appellation de Luminisme. Albert Bierstadt est né à Solingen en province de Rhénanie. Sa famille émigre à New Bedford en 1833. Il étudie la peinture avec des membres de l’École de peinture de Düsseldorf de 1853 à 1857 et voyage sur le continent européen avec ses amis, les peintres Sanford Robinson Gifford et Worthington Whittredge. De retour aux États-Unis, il enseigne un temps le dessin à New Bedford avant de se consacrer entièrement à son art. En 1859, il entreprend un voyage vers l’Ouest jusqu'aux montagnes Rocheuses, en compagnie d’un arpenteur du gouvernement américain. Il retourne dans l’Ouest en 1863 avec l’écrivain Fitz Hugh Ludlow, dont la femme devint plus tard son épouse. En 1863, Albert Bierstadt demande à William Byers, fondateur du journal de Denver, le Rocky Mountain News, de lui servir de guide pour une expédition d'Idaho Springs, vers le sommet du Mont Evans, qui sera d'abord appelé Mont Bierstadt, puis Mont Rosalie.
Dans les années 1870, il vit à San Francisco. En 1876, sa femme est diagnostiquée tuberculeuse, aussi le couple passe-t-il plusieurs mois par année à Nassau aux Bahamas jusqu'au décès de la malade en 1893. Pendant cette période, le peintre voyage également, en solitaire, au Canada. En 1882, plusieurs de ses œuvres sont détruites dans l'incendie de son atelier, situé dans le comté de Westchester en banlieue de New York.
Pendant sa longue carrière, Bierstadt a produit plus de 500 toiles.

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2024 - Gravir les montagnes en peinture
Un blog de Francis Rousseau   

LE MONT SHASTA /UYTAAHKOO PEINT PAR FRANK TENNEY JOHNSON

 

FRANK TENNEY JOHNSON (1874-1939)
Mont Shasta / Uytaahkoo (4,317m )
Etats -Unis d'Amérique (Californie)

In Cowboys roping the bear, huile su toile, 71 x 91 cm, Collection privée (Christie's)

La montagne
Le mont Shasta / Uytaahkoo (4,317m) appelé Mount Sisson jusqu'en 1922, est un stratovolcan de l'État de Californie, à l'ouest des États-Unis, le deuxième plus haut sommet de la chaîne des Cascades. Le mont Shasta présente la particularité d'être à 3 000 mètres au-dessus de la plaine alentour. Sa première ascension s'est faite en 1854 par E.D. Pearce. Le mont Shasta est constitué de quatre cônes séparés, ensevelis les uns sur les autres. Le Shastina (3 749 mètres) est le cône le plus visible et constitue un sommet secondaire. Au sommet de ce dernier, on peut trouver un cratère totalement intact, ce qui prouve que Shastina fut formée après le dernier âge glaciaire. Le reste des pentes de Shasta montre relativement peu de traces d'érosion. Paradoxalement, la seule exception se situe au sud, où la Sargents Ridge est parallèle au U-shaped Avalanch Gulch (la plus grande vallée glaciaire sur le volcan, bien qu'il n'y ait plus de glacier). Il y a cinq petits glaciers sur le flanc nord de la montagne. Il existe de nombreux promontoires glaciaires qui furent créés durant les périodes de glaciation de la glaciation de Würm. La plupart ont été remplis par de la lave andésitique, des coulées pyroclastiques et les talus des dômes de lave .Au cours des derniers 10 000 ans, le mont Shasta est entré en éruption en moyenne tous les 800 ans, mais sur les derniers 4 500 ans, la période entre deux éruptions est de 600 ans. La dernière éruption d'importance se serait produite il y a 200 ans. Le mont Shasta en Californie a fait l'objet d'un nombre inhabituellement élevé de mythes et de légendes. En particulier, on dit souvent qu'il cache une ville secrète sous ses sommets. Les Amérindiens de la tribu Iore, qui habitaient la région, pensaient que le mont Shasta était habité par l'esprit du chef Skell, qui était descendu du paradis vers le sommet de la montagne. Depuis lors, de nombreux autres cultes ont été attirés par le Mont Shasta. Pour les Acumawis, une source de la montagne serait formée des larmes de tous les daims pour leur éviter de pleurer lorsqu'ils sont tués par un chasseur. Le mont Shasta est aussi le lieu d'un monastère bouddhiste, Shasta Abbey, fondé par Houn Jiyu-Kennett en 1971.Le mont Shasta est longuement et rigoureusement décrit par John Muir dans le chapitre « Tempête de neige sur le mont Shasta » (« Snow-Storm on Mount Shasta » - première édition septembre 1877) du recueil de certains de ses textes Forêts dans la tempête et autres colères de la nature. Le mont Shasta est cité au début du recueil de nouvelles de Jack Kerouac La grande traversée de l'Ouest en bus.


Le peintre
Frank Tenney Johnson fut et reste le plus grand peintre, avec Frederic Remington, du Far West. Il a largement popularisé un style de peinture de cow-boys, devenu célèbre sous l'appellation de "The Johnson Moonlight Technique". Somewhere on the Range est un exemple de cette technique "au clair de lune" de Johnson. Pour peindre ses tableaux, il utilisait des couteaux, des pinceaux et ses doigts. Frank Tenney Johnson a grandi dans la ferme de sa famille dans l'ancien Overland Trail, près de Big Grove, Iowa (aujourd'hui connu sous le nom d' Oakland, Iowa ) dans la région de Council Bluffs, où son père élevait du bétail. Les premiers ancêtres américains de Johnson seraeent originaires à la fois d'Angleterre, d'Irlande, du Pays de Galles, du Danemark et de Suède. Ses ancêtres Bascom étaient basques français. Lorsque sa mère de Johnson est décédée en 1886, la famille a déménagé dans la région de Milwaukee, Wisconsin. Il a alors fréquenté le lycée Oconomowoc à Oconomowoc  En 1893, il s'inscrit à la Milwaukee School of Art (absorbée par la Milwaukee State Normal School en 1913), où il étudie avec Richard Lorenz, un peintre  connu pour ses paysages. En 1895, Johnson déménage à New York, où il a étudie avec le grand peintre paysagiste et pédagogue américain John Henry Twachtman à l' Art Students League de New York.  

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2023 - Gravir les Montagnes en peinture
Un blog de Francis Rousseau

MOUNT TACOMA / MOUNT RAINIER BY CHARLES HAMILTON SMITH

CHARLES HAMILTON SMITH (1776-1859)

Mount Tacoma / Mont Rainier (4,392 m -14,411 ft)

United States of America (Washington)

In Mount Rainier from the South Part of Admiralty Inlet, Watercolor and graphite from Views of Polar region, Yale Center for British arts, Connectitcut USA.

The mountain
Mount Rainier, Mount Tacoma, or Mount Tahoma (4,392 m-14,411 ft) is the highest mountain of the Cascade Range of the Pacific Northwest, and the highest mountain in the U.S. state of Washington. It is a large active stratovolcano located 54 miles (87 km) south-southeast of Seattle. It is the most topographically prominent mountain in the contiguous United States and the Cascade Volcanic Arc.
Mount Rainier was first known by the Native Americans as Talol, or Tacoma or Tahoma.
The current name was given by George Vancouver, who named it in honor of his friend, Rear Admiral Peter Rainier. The map of the Lewis and Clark expedition of 1804-1806 refers to it as "Mt. Regniere". Mount Rainier is ranked third of the 128 ultra-prominent mountain peaks of the United States.
With 26 major glaciers and 36 sq mi (93 km2) of permanent snowfields and glaciers, Mount Rainier is the most heavily glaciated peak in the lower 48 states. The summit is topped by two volcanic craters, each more than 1,000 ft (300 m) in diameter, with the larger east crater overlapping the west crater. Geothermal heat from the volcano keeps areas of both crater rims free of snow and ice, and has formed the world's largest volcanic glacier cave network within the ice-filled craters, with nearly 2 mi (3.2 km) of passages. The Carbon, Puyallup, Mowich, Nisqually, and Cowlitz Rivers begin at eponymous glaciers of Mount Rainier. The sources of the White River are Winthrop, Emmons, and Fryingpan Glaciers. The White, Carbon, and Mowich join the Puyallup River, which discharges into Commencement Bay at Tacoma; the Nisqually empties into Puget Sound east of Lacey; and the Cowlitz joins the Columbia River between Kelso and Longview.

The artist
Lieutenant-Colonel Charles Hamilton Smith, was an English artist, naturalist, antiquary, illustrator, soldier, and... spy as well !. His military career began in 1787, when he studied at the Austrian academy for artillery and engineers at Mechelen and Leuven in Belgium (his native country). Although his military service, which ended in 1820 and included the Napoleonic Wars, saw him travel extensively (including the West Indies, Canada, United States, Southern and Northern Europe and ...Antarctica).
As a prolific self-taught illustrator (over 38,000 drawings!) He left quite an important number of books of beautifully watercolored landscapes taken all around the world. those nooks of watercolors are nowadays in the collections of the Yale Center From British Art. Among them :
- Views of France, Volume I (81 watercolors), Views of France, Volume II (93 watercolors),
- Views of England and Wales, Volume I (82 watercolors), Views of England and Wales, Volume II (74 watercolors),
- Views of Northern Europe, Volume I (68watercolors) , Views of Northern Europe, Volume II (78) watercolors),
- Views of Polar Regions (75 watercolors) (see above)
- Views of Spain, Volume I (69 watercolors), Views of Spain, Volume II (72 watercolors), But one of his noteworthy achievements was an 1800 experiment to determine which color should be used for military uniforms. He is also known in military history circles for Costume of the Army of the British Empire, produced towards the end of the Napoleonic Wars and an accurate depiction of contemporary British uniform.
As an antiquarian, he also produced, in collaboration with Samuel Rush Meyrick, Costume of the Original Inhabitants of the British Islands, 1815, and The Ancient Costume of England, with historical illustrations of medieval knights, ladies, shipsm and battles.
He also wrote on the history of the Seven Years' War and TheNatural history of dogs.
Quite a productive fellow !

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2020 - Wandering Vertexes...
by Francis Rousseau

MOUNT TACOMA / RAINIER BY HIROSHI YOSHIDA / 吉田 博

HIROSHI YOSHIDA / 吉田 博 (1876-1950)

Mount Tacoma also called Mont Rainier (4,392 m -14,411 ft) 

United States of America (Washington)

In Mt. Rainier USA- Woodblock print - 1925

The mountain
Mount Rainier, Mount Tacoma, or Mount Tahoma (4,392 m-14,411 ft) is the highest mountain of the Cascade Range of the Pacific Northwest, and the highest mountain in the U.S. state of Washington. It is a large active stratovolcano located 54 miles (87 km) south-southeast of Seattle. It is the most topographically prominent mountain in the contiguous United States and the Cascade Volcanic Arc.
Mount Rainier was first known by the Native Americans as Talol, or Tacoma or Tahoma. One hypothesis of the word origin is ("mother of waters"), in the Lushootseed language spoken by the Puyallup people. Another hypothesis is that "Tacoma" means "larger than Mount Baker" in Lushootseed: "Ta", larger, plus "Koma", Mount Baker. Other names originally used include Tahoma, Tacobeh, and Pooskaus.
The current name was given by George Vancouver, who named it in honor of his friend, Rear Admiral Peter Rainier. The map of the Lewis and Clark expedition of 1804-1806 refers to it as "Mt. Regniere".
This peak is located just east of Eatonville and just southeast of Seattle and Tacoma. Mount Rainier is ranked third of the 128 ultra-prominent mountain peaks of the United States.

More about Mont Tacoma /Rainier 

The painter
Hiroshi Yoshida (not to be confused with Toshi Yoshida) was born in 1876. He began his artistic training with his adoptive father in Kurume, Fukuoka prefecture. Around the age of twenty, he left Kurume to study with Soritsu Tamura in Kyoto, subsequently moving to Tokyo and the tutelage of Shotaro Koyama. Yoshida studied Western-style painting, winning many exhibition prizes and making several trips to the United States, Europe and North Africa selling his watercolors and oil paintings. In 1902, he played a leading role in the organization of the Meiji Fine Arts Society into the Pacific Painting Association. His work was featured in the exhibitions of the state-sponsored Bunten and Teiten. While highly successful as an oil painter and watercolor artist, Yoshida turned to printmaking upon learning of the Western world’s infatuation with ukiyo-e.
Following the Great Kanto Earthquake of 1923, Yoshida embarked on a tour of the United States and Europe, painting and selling his work. When he returned to Japan in 1925, he started his own workshop, specializing in landscapes inspired both by his native country and his travels abroad. Yoshida often worked through the entire process himself: designing the print, carving his own blocks, and printing his work. His career was temporarily interrupted by his sojourn as a war correspondent in Manchuria during the Pacific War. Although he designed his last print in 1946, Yoshida continued to paint with oils and watercolors up until his death in 1950.
Yoshida was widely traveled and knowledgeable of Western aesthetics, yet maintained an allegiance to traditional Japanese techniques and traditions. Attracted by the calmer moments of nature, his prints breathe coolness, invite meditation, and set a soft, peaceful mood. All of his lifetime prints are signed “Hiroshi Yoshida” in pencil and marked with a jizuri (self-printed) seal outside of the margin. Within the image, most prints are signed “Yoshida” with brush and ink beside a red “Hiroshi” seal.

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2019 - Wandering Vertexes...
by Francis Rousseau

MOUNT TACOMA / MOUNT RAINIER BY ELIZA BARCHUS

ELIZA BARCHUS (1857-1959)

Mount Tacoma / Mont Rainier (4,392 m -14,411 ft) 

United States of America (Washington)

The mountain
Mount Rainier, Mount Tacoma, or Mount Tahoma (4,392 m-14,411 ft) is the highest mountain of the Cascade Range of the Pacific Northwest, and the highest mountain in the U.S. state of Washington. It is a large active stratovolcano located 54 miles (87 km) south-southeast of Seattle. It is the most topographically prominent mountain in the contiguous United States and the Cascade Volcanic Arc.
Mount Rainier was first known by the Native Americans as Talol, or Tacoma or Tahoma.
The current name was given by George Vancouver, who named it in honor of his friend, Rear Admiral Peter Rainier. The map of the Lewis and Clark expedition of 1804-1806 refers to it as "Mt. Regniere".
Mount Rainier is ranked third of the 128 ultra-prominent mountain peaks of the United States. Mount Rainier has a topographic prominence of 13,210 ft (4,026 m), which is greater than that of K2, the world's second-tallest mountain, at 13,189 ft (4,020 m). On days of exceptional clarity, it can also be seen from as far away as Corvallis, Oregon (at Marys Peak) and Victoria, British Columbia.
With 26 major glaciers and 36 sq mi (93 km2) of permanent snowfields and glaciers, Mount Rainier is the most heavily glaciated peak in the lower 48 states. The summit is topped by two volcanic craters, each more than 1,000 ft (300 m) in diameter, with the larger east crater overlapping the west crater. Geothermal heat from the volcano keeps areas of both crater rims free of snow and ice, and has formed the world's largest volcanic glacier cave network within the ice-filled craters, with nearly 2 mi (3.2 km) of passages. 

The Carbon, Puyallup, Mowich, Nisqually, and Cowlitz Rivers begin at eponymous glaciers of Mount Rainier. 

The sources of the White River are Winthrop, Emmons, and Fryingpan Glaciers. The White, Carbon, and Mowich join the Puyallup River, which discharges into Commencement Bay at Tacoma; the Nisqually empties into Puget Sound east of Lacey; and the Cowlitz joins the Columbia River between Kelso and Longview.

The painter
Eliza Barchus was an American landscape painter who lived in Portland for most of her life.
After taking art lessons from another landscape painter, Will S. Parrott, Barchus sold her first painting in 1885. Between then and 1935, she produced thousands of oil paintings and reproductions of subjects such as Mount Hood, Yellowstone Falls, Muir Glacier, and San Francisco Bay.
Barchus, who had won medals at Mechanics Fairs in Portland in the late 1880s, drew national attention in 1890, when one of her large canvases of Mount Hood was displayed at the National Academy of Design exhibition in New York City. In 1901, several of her works were shown at the Pan-American Exposition in Buffalo, New York, and in 1905 she won a gold medal at the Lewis and Clark Centennial Exposition in Portland for oil paintings of Pacific coast scenery.
Widowed in 1899, Barchus supported herself and her family for decades largely by selling or trading her art. Several years after her death at age 102, the Oregon Legislative Assembly named her "The Oregon Artist". Many art collections in Portland and elsewhere include examples of her work.

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2019 - Wandering Vertexes...

by Francis Rousseau 

MOUNT TACOMA/ MOUNT RAINIER BY ABBY WILLIAMS HILL

ABBY WILLIAMS HILL (1861-1943) 

Mount Tacoma / Mount Rainier (4,392 m-14,411 ft)

United States of America  (Washington State)

In Mount Rainier from Eunice Lake, 1904, University of Puget Sound 

The mountain
Mount Rainier,  Mount Tacoma, or Mount Tahoma (4,392 m-14,411 ft) is the highest mountain of the Cascade Range of the Pacific Northwest, and the highest mountain in the U.S. state of Washington. It is a large active stratovolcano located 54 miles (87 km) south-southeast of Seattle. It is the most topographically prominent mountain in the contiguous United States and the Cascade Volcanic Arc.
Mount Rainier was first known by the Native Americans as Talol, or Tacoma or Tahoma. One hypothesis of the word origin is  ("mother of waters"), in the Lushootseed language spoken by the Puyallup people. Another hypothesis is that "Tacoma" means "larger than Mount Baker" in Lushootseed: "Ta", larger, plus "Koma", Mount Baker. Other names originally used include Tahoma, Tacobeh, and Pooskaus.
The current name was given by George Vancouver, who named it in honor of his friend, Rear Admiral Peter Rainier. The map of the Lewis and Clark expedition of 1804-1806 refers to it as "Mt. Regniere".
With 26 major glaciers and 36 sq mi (93 km2) of permanent snowfields and glaciers, Mount Rainier is the most heavily glaciated peak in the lower 48 states. The summit is topped by two volcanic craters, each more than 1,000 ft (300 m) in diameter, with the larger east crater overlapping the west crater. Geothermal heat from the volcano keeps areas of both crater rims free of snow and ice, and has formed the world's largest volcanic glacier cave network within the ice-filled craters, with nearly 2 mi (3.2 km) of passages. A small crater lake about 130 by 30 ft (39.6 by 9.1 m) in size and 16 ft (5 m) deep, the highest in North America with a surface elevation of 14,203 ft (4,329 m), occupies the lowest portion of the west crater below more than 100 ft (30 m) of ice and is accessible only via the caves. The Carbon, Puyallup, Mowich, Nisqually, and Cowlitz Rivers begin at eponymous glaciers of Mount Rainier. The sources of the White River are Winthrop, Emmons, and Fryingpan Glaciers. The White, Carbon, and Mowich join the Puyallup River, which discharges into Commencement Bay at Tacoma; the Nisqually empties into Puget Sound east of Lacey; and the Cowlitz joins the Columbia River between Kelso and Longview.

The Painter 
Abby Williams Hill was an American plein-air painter most known for her landscapes of the American West. Hill also advocated for children's rights, attended the 1905 Congress of Mothers in Washington, D.C., and founded the Washington (state) Parent-Teacher Association.
In the early 1900s, the Great Northern Railway and the Northern Pacific Railway commissioned Hill to paint landscapes of the northwestern United States to promote tourism. The commission required that Hill produce 22 paintings in just 18 weeks, and that she produce them en plein air.  Accompanied by her four children, Abby Hill took prolonged camping trips for the purpose of painting scenery in places such as Yosemite National Park and Yellowstone National Park.  Her works were exhibited at the 1904 World's Fair in St. Louis and the 1905 Lewis & Clark Centennial Exposition in Portland. Over the course of her career, Hill achieved her goal of painting in every national park in the Western United States.
Her husband became incapacitated by psychotic depression in 1911, so the family moved to the small isolated community of Laguna Beach, California, for the benefit of the mild, sunny climate.
Abby Hill was one of several early-20th-century American artists who built studios in Laguna Beach and transformed it into an artist community. She became a founding member of the Laguna Beach Art Association.
Following the death of her husband in 1938, Abby Hill became bedridden. She died in Laguna Beach in 1943.
A permanent collection of her works and papers is held by the University of Puget Sound.

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2019 - Wandering Vertexes...
by Francis Rousseau 

MOUNT ADAMS PAINTED BY CHILDE HASSAM

CHILDE HASSAM (1859-1935)
Mount Adams or Patho or Klikitat (3, 473m - 12, 281ft) 

United States of America (Washington State) 

In  Looking towards Mount Adams from Mount Hood, watercolor, 1904

The mountain

Mount Adams or Patho or Klikitat (3, 473m - 12, 281ft)  is a potentially active stratovolcano in the Cascade Range, USA. Although Adams has not erupted in more than 1,000 years, it is not considered extinct. It is the second-highest mountain in the U.S. state of Washington, after Mount Rainier/Tacoma. Mount Adams is a member of the Cascade Volcanic Arc, and is one of the arc's largest volcanoes, located in a remote wilderness approximately 34 miles (55 km) east of Mount St. Helens. The Mount Adams Wilderness consists of the upper and western part of the volcano's cone. The eastern side of the mountain is designated as part of the territory of the Yakama Nation.

Adams' asymmetrical and broad body rises 1.5 miles (2.4 km) above the Cascade crest. Its nearly flat summit was formed as a result of cone-building eruptions from separated vents. A false summit, Pikers Peak, rises 11,657 feet (3,553 m) on the south side of the nearly half-mile (800 m) wide summit area. The true summit is about 600 feet (180 m) higher on the gently sloping north side. A small lava and scoria cone marks the highest point. Suksdorf Ridge is a long buttress descending from the false summit down to an elevation of 8,000 feet (2,000 m). This structure was built by repeated lava flows in the late Pleistocene. 

Air travelers flying the busy routes above the area sometimes confuse Mount Adams with nearby Mount Rainier/Tacoma, which has a similar flat-topped shape.

The Pacific Crest Trail traverses the western flank of the mountain.

In the early 21st century, glaciers cover a total of 2.5% of Adams' surface. During the last ice age about 90% of the mountain was glaciated. Mount Adams has 209 perennial snow and ice features and 12 officially named glaciers : Adams Glacier, Pinnacle Glacier, White Salmon Glacier,  Avalanche Glacier, Mazama Glacier, Klickitat Glacier, Rusk Glacier, Wilson Glacier, Gotchen Glacier, Crescent Glacier and Lava Glacier.

The painter
Frederick Childe Hassam was an American Impressionist painter, noted for his urban and coastal scenes. Along with Mary Cassatt and John Henry Twachtman, Hassam was instrumental in promulgating Impressionism to American collectors, dealers, and museums. He produced over 3,000 paintings, oils, watercolors, etchings, and lithographs over the course of his career, and was an influential American artist of the early 20th century.
In 1904 and 1908, he traveled to Oregon and was stimulated by new subjects and diverse views, frequently working out-of-doors with friend, lawyer and amateur painter Colonel C. E. S. Wood.
He produced over 100 paintings, pastels, and watercolors of the High Desert, the rugged coast, the Cascades, scenes of Portland.  As usual, he adapted his style and colors to the subject at hand and the mood of place, but always in the Impressionist vein. With the art market now eagerly accepting his work, by 1909 Hassam was enjoying great success, earning as much as $6,000 per painting. His close friend and fellow artist J. Alden Weir commented to another artist : "Our mutual friend Hassam has been in the greatest of luck and merited success. He sold his apartment studio and has sold more pictures this winter, I think, than ever before and is really on the crest of the wave. So he goes around with a crisp, cheerful air."

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2019 - Wandering Vertexes...
by Francis Rousseau 

MOUNT HOOD / WY'EAST BY ALBERT BIERSTADT

ALBERT BIERSTADT (1830-1902)

Mount Hood  / Wy 'east (3,429m - 11, 249ft)
United States of America (Oregon) 

 In Mount Hood, 1869, oil on canvas,  Portland Art Museum

About this Painting

In Mount Hood, Bierstadt characteristically exaggerates the height of the mountain and includes several landscape elements that could not be viewed from a single site along the Columbia River Gorge. For example, Mount Hood is painted as though seen from the northern shore of the Columbia River and Multnomah Falls, but the profile of the mountain is actually the one seen from Portland, and featured in a Childe Hassam painting nearby. The drama and monumentality of the far West, as a metaphor, was more important to Bierstadt than geographic accuracy.

In Notice from he Portland Art Museum 

The mountain 

 Mount Hood (3,429m - 11, 249ft) called Wy'east by the Multnomah tribe, is a potentially active stratovolcano in the Cascade Volcanic Arc of northern Oregon. It was formed by a subduction zone on the Pacific coast and rests in the Pacific Northwest region of the United States. It is located about 50 miles (80 km) east-southeast of Portland, on the border between Clackamas and Hood River counties. In addition to being Oregon's highest mountain, it is one of the loftiest mountains in the nation based on its prominence.

The height assigned to Mount Hood's snow-covered peak has varied over its history. Modern sources point to three different heights: 11,249 feet (3,429 m), a 1991 adjustment of a 1986 measurement by the U.S. National Geodetic Survey,  11,240 feet (3,426 m) based on a 1993 scientific expedition,and 11,239 feet (3,425.6 m) of slightly older origin. 

The peak is home to 12 named glaciers and snowfields. It is the highest point in Oregon and the fourth highest in the Cascade Range. Mount Hood is considered the Oregon volcano most likely to erupt, though based on its history, an explosive eruption is unlikely. Still, the odds of an eruption in the next 30 years are estimated at between 3 and 7 %, so the U.S. Geological Survey (USGS) characterizes it as "potentially active", but the mountain is informally considered dormant.

The painter 

Albert Bierstadt was a German-born American painter. He was brought to the United States at the age of one by his parents. He later returned to study painting for several years in Düsseldorf. At an early age Bierstadt developed a taste for art and made clever crayon sketches in his youth. 

In 1851, he began to paint in oils. He became part of the Hudson River School in New York, an informal group of like-minded painters who started painting along this scenic river. Their style was based on carefully detailed paintings with romantic, almost glowing lighting, sometimes called luminism. An important interpreter of the western landscape, Bierstadt, along with Thomas Moran, is also grouped with the Rocky Mountain School.

Despite his popular success, Bierstadt was criticized by some contemporaries for the romanticism evident in his choices of subject and his use of light was felt to be excessive. 

In 1882 Bierstadt's studio at Irvington, New York, was destroyed by fire, resulting in the loss of many of his paintings. By the time of his death on February 18, 1902, the taste for epic landscape painting had long since subsided. Bierstadt was then largely forgotten. He was buried at the Rural Cemetery in New Bedford, Massachusetts.

Interest in his work was renewed in the 1960s, with the exhibition of his small oil studies. The subsequent reassessment of Bierstadt's work has placed it in a favorable context.

Bierstadt's theatrical art, fervent sociability, international outlook, and unquenchable personal energy reflected the epic expansion in every facet of western civilization during the second half of the nineteenth century.

Bierstadt was a prolific artist, having completed over 500 paintings during his lifetime. Many of these are held by museums across the United States.

MOUNT RAINIER OR TACOMA BY SANFORD ROBINSON GIFFORD (

SANFORD ROBINSON GIFFORD (1823-1880)

Mount Rainier  also called MontTacoma (4,392 m -14,411 ft) 

United States of America  (Washington)

In Mount Rainier from the Bay of Tacoma, oil on canvas,  1875,  Tacoma Art Museum

The mountain

Mount Rainier,  Mount Tacoma, or Mount Tahoma (4,392 m-14,411 ft) is the highest mountain of the Cascade Range of the Pacific Northwest, and the highest mountain in the U.S. state of Washington. It is a large active stratovolcano located 54 miles (87 km) south-southeast of Seattle. It is the most topographically prominent mountain in the contiguous United States and the Cascade Volcanic Arc.

Mount Rainier was first known by the Native Americans as Talol, or Tacoma or Tahoma. 

One hypothesis of the word origin is  ("mother of waters"), in the Lushootseed language spoken by the Puyallup people. Another hypothesis is that "Tacoma" means "larger than Mount Baker" in Lushootseed: "Ta", larger, plus "Koma", Mount Baker. Other names originally used include Tahoma, Tacobeh, and Pooskaus. The current name was given by George Vancouver, who named it in honor of his friend, Rear Admiral Peter Rainier. The map of the Lewis and Clark expedition of 1804-1806 refers to it as "Mt. Regniere". Mount Rainier has a topographic prominence of 13,210 ft (4,026 m), which is greater than that of K2, the world's second-tallest mountain, at 13,189 ft (4,020 m). On clear days it dominates the southeastern horizon in most of the Seattle-Tacoma metropolitan area to such an extent that locals sometimes refer to it simply as "the Mountain." 

With 26 major glaciers and 36 sq mi (93 km2) of permanent snowfields and glaciers, Mount Rainier is the most heavily glaciated peak in the lower 48 states. The summit is topped by two volcanic craters, each more than 1,000 ft (300 m) in diameter, with the larger east crater overlapping the west crater. 

Mountain climbing on Mount Rainier is difficult, involving traversing the largest glaciers in the U.S. south of Alaska. Most climbers require two to three days to reach the summit. Climbing teams demand experience in glacier travel, self-rescue, and wilderness travel. 

The worst mountaineering accident on Mount Rainier occurred in 1981, when eleven people lost their lives in an ice fall on the Ingraham Glacier. This was the largest number of fatalities on Mount Rainier in a single incident since 32 people were killed in a 1946 plane crash on the South Tahoma Glacier.

The painter 

Sanford Robinson Gifford was born in Greenfield, New York and spent his childhood in Hudson, New York, the son of an iron foundry owner. He attended Brown University 1842-44, before leaving to study art in New York City in 1845. He studied drawing, perspective and anatomy under the direction of the British watercolorist and drawing-master, John Rubens Smith.  He also studied the human figure in anatomy classes at the Crosby Street Medical college and took drawing classes at the National Academy of Design.  By 1847 he was sufficiently skilled at painting to exhibit his first landscape at the National Academy and was elected an associate in 1851, an academician in 1854. Thereafter Gifford devoted himself to landscape painting, becoming one of the finest artists of the early Hudson River School.

Like most Hudson River School artists, Gifford traveled extensively to find scenic landscapes to sketch and paint. In addition to exploring New England, upstate New York and New Jersey, Gifford made extensive trips abroad. He first traveled to Europe from 1855 to 1857, to study European art and sketch subjects for future paintings. During this trip Gifford also met Albert Bierstadt and Worthington Whittredge.

In 1858, he traveled to Vermont, "apparently" with his friend and fellow painter Jerome Thompson. Details of their visit were carried in the contemporary Home Journal. Both artists submitted paintings of Mount Mansfield, Vermont's tallest peak, to the National Academy of Design's annual show in 1859. Thompson's work, "Belated Party on Mansfield Mountain" is now owned by the MET in New York, according to the report.

Thereafter, he served in the Union Army as a corporal in the 7th Regiment of the New York Militia upon the outbreak of the Civil War. A few of his canvases belonging to New York City's Seventh Regiment and the Union League Club of New York are testament to that troubled time.

During the summer of 1867, Gifford spent most of his time painting on the New Jersey coast, specifically at Sandy Hook and Long Branch, according to an auction Web site.

Another journey, this time with Jervis McEntee and his wife, took him across Europe in 1868. Leaving the McEntees behind, Gifford traveled to the Middle East, including Egypt in 1869. Then in the summer of 1870 Gifford ventured to the Rocky Mountains in the western United States, this time with Worthington Whittredge and John Frederick Kensett. At least part of the 1870 travels were as part of a Hayden Expedition, led by Ferdinand Vandeveer Hayden.

Returning to his studio in New York City, Gifford painted numerous major landscapes from scenes he recorded on his travels. Gifford's method of creating a work of art was similar to other Hudson River School artists. He would first sketch rough, small works in oil paint from his sketchbook pencil drawings. Those scenes he most favored he then developed into small, finished paintings, then into larger, finished paintings.

Gifford referred to the best of his landscapes as his "chief pictures". Many of his chief pictures are characterized by a hazy atmosphere with soft, suffuse sunlight. Gifford often painted a large body of water in the foreground or middle distance (see above) in which the distant landscape would be gently reflected. Examples of Gifford's "chief pictures" in museum collections today include: Lake Nemi (1856–57), Toledo Museum of Art, Toledo, Ohio ; The Wilderness (1861), Toledo Museum of Art, Toledo, Ohio ;  A Passing Storm (1866), Wadsworth Atheneum, Hartford, Connecticut ;  Ruins of the Parthenon (1880), Corcoran Gallery of Art, Washington, D.C. On August 29, 1880, Gifford died in New York City, having been diagnosed with malarial fever. The MET in New York City celebrated his life that autumn with a memorial exhibition of 160 paintings. A catalog of his work published shortly after his death recorded in excess of 700 paintings during his career.

_______________________________

2018 - Wandering Vertexes...
by Francis Rousseau 

MOUNT SHASTA IN VINTAGE POSTCARD 1966

VINTAGE POSTCARD 1966

Mount Shasta (4,322 m - 14,179 ft)

United Sates of America  (California)

The mountain 

Mount Shasta (4,322 m- 14,179 ft) named after a tribe of native american the Shasta, is also called "Uytaahkoo" (in Karuk) or "White Mountain". It  is a potentially active volcano (last known eruption in 1786) at the southern end of the Cascade Range in Siskiyou County, California. Mount Shasta  is the most voluminous stratovolcano in the Cascade Volcanic Arc. The mountain and its surrounding area are managed by the U.S. Forest Service as part of the Shasta-Trinity National Forest. Mount Shasta was declared a National Natural Landmark in December 1976.

In his Picturesque California in 1888, John Muir  described Mount Shasta and its area  "The Shasta region is still a fresh unspoiled wilderness, accessible and available for travelers of every kind and degree. Would it not be a fine thing to set it apart like the Yellowstone and Yosemite as a National Park for the welfare and benefit of all mankind, preserving its fountains and forests and all its glad life in primeval beauty?"

At the time of Euro-American contact in the 1820s, the Native American tribes who lived within view of Mount Shasta included: the Shasta, Okwanuchu, Modoc, Achomawi, Atsugewi, Karuk, Klamath, Wintu, and Yana tribes. 

The historic eruption of Mount Shasta in 1786 may have been observed by the french explorer Lapérouse. Although perhaps first seen by Spanish explorers, the first reliably reported land sighting of Mount Shasta by a European or American was by Peter Skene Ogden (a leader of a Hudson's Bay Company trapping brigade) in 1826. In 1827, the name "Sasty" or "Sastise" was given to nearby Mount McLoughlin by Ogden. The name was transferred to present-day Mount Shasta in 1841, partly as a result of work by the United States Exploring Expedition.

The lore of some of the Klamath Tribes in the area held that Mount Shasta is inhabited by the Spirit of the Above-World, , who descended from heaven to the mountain's summit at the request of a Klamath chief. Skell fought with Spirit of the Below-World, Llao, who resided at Mount Mazama by throwing hot rocks and lava, probably representing the volcanic eruptions at both mountains.

 A group of Native Americans from the McCloud River area practice rituals on the mountain.

Mount Shasta has also been a focus for non-Native American legends, centered on a hidden city of advanced beings from the lost continent of Lemuria. The legend grew from an offhand mention of Lemuria in the 1880s, to a description of a hidden Lemurian village in 1925. In 1931, Wisar Spenle Cerve wrote Lemuria: the lost continent of the Pacific, published by the Rosicrucians, about the hidden Lemurians of Mount Shasta that cemented the legend in many readers' minds.

In August 1987, believers in the spiritual significance of the Harmonic Convergence described Mount Shasta as one of a small number of global "power centers". Mount Shasta remains a focus of "New Age" attention.

Mount Shasta is connected to nearby Shastina, and they dominate the northern California landscape. 

The mountain consists of four overlapping volcanic cones that have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft (3,760 m) Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mount Rainier, Rainier's Liberty Cap, and Mount Shasta itself).

Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft (3,000 m) primarily on the north and east sides. The Whitney Glacier is the longest, and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft (3,400 m) on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek glaciers.

Vintage postcards
Postcards became popular at the turn of the 20th century, especially for sending short messages to friends and relatives. They were collected right from the start, and are still sought after today by collectors of pop culture, photography, advertising, wartime memorabilia, local history, and many other categories. Postcards were an international craze, published all over the world. The Detroit Publishing Co. and Teich & Co. were two of the major publishers in the U.S, and sometimes individuals printed their own postcards as well. Yvon were the most famous in France. Many individual or anonymous publishers did exist around the world and especially in Africa and  Asia (Japan, Thailand, Nepal, China, Java) between 1920 and 1955. These photographer were mostly local notables, soldiers, official guides belonging to the colonial armies (british french, belgium...) who sometimes had rather sophisticated equipment and readily produced colored photograms or explorers, navigators, climbers (Vittorio Sella and the Archiduke of Abruzzi future king of Italy remains the most famous of them).
There are many types of collectible vintage postcards.
Hold-to-light postcards were made with tissue paper surrounded by two pieces of regular paper, so light would shine through. Fold-out postcards, popular in the 1950s, had multiple postcards attached in a long strip. Real photograph postcards (RPPCs) are photographs with a postcard backing.
Novelty postcards were made using wood, aluminum, copper, and cork. Silk postcards–often embroidered over a printed image–were wrapped around cardboard and sent in see-through glassine paper envelopes; they were especially popular during World War I.
In the 1930s and 1940s, postcards were printed on brightly colored paper designed to look like linen.

Most vintage postcard collectors focus on themes, like Christmas, Halloween, portraits of movie stars, European royalty and U.S. presidents, wartime imagery, and photos of natural disasters or natural wonders. Not to mention cards featuring colorful pictures by famous artists like Alphonse Mucha, Harrison Fisher, Ellen Clapsaddle, and Frances Brundage.

MOUNT ADAMS PAINTED BY ALVAN FISCHER

ALVAN FISCHER (1792-1863)
Mount Adams or Patho or Klikitat (3, 473m - 12, 281ft) 

United States of America (Washington State) 

In Mount Adams from the Peabody, 1857, oil on canvas

The mountain

Mount Adams or Patho or Klikitat (3, 473m - 12, 281ft)  is a potentially active stratovolcano in the Cascade Range, USA. Although Adams has not erupted in more than 1,000 years, it is not considered extinct. It is the second-highest mountain in the U.S. state of Washington, after Mount Rainier/Tacoma. Mount Adams is a member of the Cascade Volcanic Arc, and is one of the arc's largest volcanoes, located in a remote wilderness approximately 34 miles (55 km) east of Mount St. Helens. The Mount Adams Wilderness consists of the upper and western part of the volcano's cone. The eastern side of the mountain is designated as part of the territory of the Yakama Nation.

Adams' asymmetrical and broad body rises 1.5 miles (2.4 km) above the Cascade crest. Its nearly flat summit was formed as a result of cone-building eruptions from separated vents. A false summit, Pikers Peak, rises 11,657 feet (3,553 m) on the south side of the nearly half-mile (800 m) wide summit area. The true summit is about 600 feet (180 m) higher on the gently sloping north side. A small lava and scoria cone marks the highest point. Suksdorf Ridge is a long buttress descending from the false summit down to an elevation of 8,000 feet (2,000 m). This structure was built by repeated lava flows in the late Pleistocene. 

Air travelers flying the busy routes above the area sometimes confuse Mount Adams with nearby Mount Rainier/Tacoma, which has a similar flat-topped shape.

The Pacific Crest Trail traverses the western flank of the mountain.

In the early 21st century, glaciers cover a total of 2.5% of Adams' surface. During the last ice age about 90% of the mountain was glaciated. Mount Adams has 209 perennial snow and ice features and 12 officially named glaciers : Adams Glacier, Pinnacle Glacier, White Salmon Glacier,  Avalanche Glacier, Mazama Glacier, Klickitat Glacier, Rusk Glacier, Wilson Glacier, Gotchen Glacier, Crescent Glacier and Lava Glacier.

The painter 
Alvan Fisher  was one of the United States's pioneers in landscape painting and genre works.
Fisher traveled throughout the northeastern United States searching out sites of landscape beauty such as the views of Springfield, Hartford, and Providence and the spectacular scenery of the White Mountains of New Hampshire. He sketched outdoors and began to compose pastoral scenes in his studio before Thomas Cole or others of the Hudson River School gave serious attention to nature. The Watering Place, 1816, now in the collection of Fruitlands Museum, Harvard, Massachusetts, is his earliest extant pure landscape. His paintings of Niagara Falls, commissioned by Judge Daniel Appleton White of Salem, Massachusetts, were completed following his visit there in 1820.
In April, 1825, Fisher sailed for a tour of the great art centers of Europe. He was the first important American landscapist to make such a tour. He visited England, France, Italy and Switzerland, countries considered important for any artist's professional stature and artistic maturation. In London he visited private collections and was inspired by the composition and subject matter of landscapes by Claude Lorrain. In Paris he studied drawing and made copies of works by the Old Masters at the Louvre. He had evidently met General Lafayette in 1824 when Lafayette stopped at Dedham during his triumphal tour of the United States. Fisher was granted permission to complete paintings of Chateau La Grange, Lafayette's estate outside Paris. His four views of La Grange were then drawn on lithographic stones in France by the noted lithographer Isadore Deroy, and brought back for printing on one of the first lithographic presses used in the United States. Portfolios of these prints were sold as souvenirs building on the popularity of General Lafayette.
Perhaps the greatest recognition of his skill as a landscape artist came one hundred years his death  later when First Lady Jacqueline Kennedy chose his painting, The Remnant of the Tribe, to hang in the Green Room of the White House. The Dedham Historical Society has a collection of his paintings, sketches and biographical material. 

MOUNT ADAMS / PAHTO PAINTED BY ALBERT BIERSTADT

ALBERT BIERSTADT  (1830-1902) 

Mount Adams or Patho or Klikitat (3, 473m - 12, 281ft) 

United States of America (Washington State) 

In Mount Adams , 1875, oil on canvas, Princeton University Art Museum, USA

The mountain

Mount Adams or Patho or Klikitat (3, 473m - 12, 281ft)  is a potentially active stratovolcano in the Cascade Range, USA. Although Adams has not erupted in more than 1,000 years, it is not considered extinct. It is the second-highest mountain in the U.S. state of Washington, after Mount Rainier/Tacoma. Mount Adams is a member of the Cascade Volcanic Arc, and is one of the arc's largest volcanoes, located in a remote wilderness approximately 34 miles (55 km) east of Mount St. Helens. The Mount Adams Wilderness consists of the upper and western part of the volcano's cone. The eastern side of the mountain is designated as part of the territory of the Yakama Nation.

Adams' asymmetrical and broad body rises 1.5 miles (2.4 km) above the Cascade crest. Its nearly flat summit was formed as a result of cone-building eruptions from separated vents. A false summit, Pikers Peak, rises 11,657 feet (3,553 m) on the south side of the nearly half-mile (800 m) wide summit area. The true summit is about 600 feet (180 m) higher on the gently sloping north side. A small lava and scoria cone marks the highest point. Suksdorf Ridge is a long buttress descending from the false summit down to an elevation of 8,000 feet (2,000 m). This structure was built by repeated lava flows in the late Pleistocene. 

Air travelers flying the busy routes above the area sometimes confuse Mount Adams with nearby Mount Rainier/Tacoma, which has a similar flat-topped shape.

The Pacific Crest Trail traverses the western flank of the mountain.

In the early 21st century, glaciers cover a total of 2.5% of Adams' surface. During the last ice age about 90% of the mountain was glaciated. Mount Adams has 209 perennial snow and ice features and 12 officially named glaciers : Adams Glacier, Pinnacle Glacier, White Salmon Glacier,  Avalanche Glacier, Mazama Glacier, Klickitat Glacier, Rusk Glacier, Wilson Glacier, Gotchen Glacier, Crescent Glacier and Lava Glacier.

 The Painter 
Albert Bierstadt was a German-born American painter.At an early age Bierstadt developed a taste for art and made clever crayon sketches in his youth. In 1851, he began to paint in oils. He became part of the Hudson River School in New York, an informal group of like-minded painters who started painting along this scenic river. Their style was based on carefully detailed paintings with romantic, almost glowing lighting, sometimes called Luminism. An important interpreter of the western landscape, Bierstadt, along with Thomas Moran, is also grouped with the Rocky Mountain School.
In 1858 he exhibited a large painting of a Swiss landscape at the National Academy of Design, which gained him positive critical reception and honorary membership in the Academy.  At this time Bierstadt began painting scenes in New England and upstate New York, including in the Hudson River valley. A group of artists known as the Hudson River School portrayed its majestic landscapes and craggy areas, as well as the light affected by the changing waters.
In 1859, Bierstadt traveled westward in the company of Frederick W. Lander, a land surveyor for the U.S. government, to see those landscapes.  He continued to visit the American West throughout his career....
 - More on Albert Bierstadt 's life and works

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 SHASTA BY HENRY JOSEPH BREUER

HENRY JOSEPH BREUER  (1860-1932) 

Mount Shasta (4,322 m - 14,179 ft)

United Sates of America  (California)

oil on canvas,1903

The mountain 

Mount Shasta (4,322 m- 14,179 ft) named after a tribe of native american the Shasta, is also called "Uytaahkoo" (in Karuk) or "White Mountain". It  is a potentially active volcano (last known eruption in 1786) at the southern end of the Cascade Range in Siskiyou County, California. Mount Shasta  is the most voluminous stratovolcano in the Cascade Volcanic Arc. The mountain and its surrounding area are managed by the U.S. Forest Service as part of the Shasta-Trinity National Forest. Mount Shasta was declared a National Natural Landmark in December 1976.

In his Picturesque California in 1888, John Muir  described Mount Shasta and its area  "The Shasta region is still a fresh unspoiled wilderness, accessible and available for travelers of every kind and degree. Would it not be a fine thing to set it apart like the Yellowstone and Yosemite as a National Park for the welfare and benefit of all mankind, preserving its fountains and forests and all its glad life in primeval beauty?"

At the time of Euro-American contact in the 1820s, the Native American tribes who lived within view of Mount Shasta included: the Shasta, Okwanuchu, Modoc, Achomawi, Atsugewi, Karuk, Klamath, Wintu, and Yana tribes. 

The historic eruption of Mount Shasta in 1786 may have been observed by the french explorer Lapérouse. Although perhaps first seen by Spanish explorers, the first reliably reported land sighting of Mount Shasta by a European or American was by Peter Skene Ogden (a leader of a Hudson's Bay Company trapping brigade) in 1826. In 1827, the name "Sasty" or "Sastise" was given to nearby Mount McLoughlin by Ogden. The name was transferred to present-day Mount Shasta in 1841, partly as a result of work by the United States Exploring Expedition.

The lore of some of the Klamath Tribes in the area held that Mount Shasta is inhabited by the Spirit of the Above-World, , who descended from heaven to the mountain's summit at the request of a Klamath chief. Skell fought with Spirit of the Below-World, Llao, who resided at Mount Mazama by throwing hot rocks and lava, probably representing the volcanic eruptions at both mountains.

 A group of Native Americans from the McCloud River area practice rituals on the mountain.

Mount Shasta has also been a focus for non-Native American legends, centered on a hidden city of advanced beings from the lost continent of Lemuria. The legend grew from an offhand mention of Lemuria in the 1880s, to a description of a hidden Lemurian village in 1925. In 1931, Wisar Spenle Cerve wrote Lemuria: the lost continent of the Pacific, published by the Rosicrucians, about the hidden Lemurians of Mount Shasta that cemented the legend in many readers' minds.

In August 1987, believers in the spiritual significance of the Harmonic Convergence described Mount Shasta as one of a small number of global "power centers". Mount Shasta remains a focus of "New Age" attention.

Mount Shasta is connected to nearby Shastina, and they dominate the northern California landscape. 

The mountain consists of four overlapping volcanic cones that have built a complex shape, including the main summit and the prominent satellite cone of 12,330 ft (3,760 m) Shastina, which has a visibly conical form. If Shastina were a separate mountain, it would rank as the fourth-highest peak of the Cascade Range (after Mount Rainier, Rainier's Liberty Cap, and Mount Shasta itself).

Mount Shasta's surface is relatively free of deep glacial erosion except, paradoxically, for its south side where Sargents Ridge runs parallel to the U-shaped Avalanche Gulch. This is the largest glacial valley on the volcano, although it does not presently have a glacier in it. There are seven named glaciers on Mount Shasta, with the four largest (Whitney, Bolam, Hotlum, and Wintun) radiating down from high on the main summit cone to below 10,000 ft (3,000 m) primarily on the north and east sides. The Whitney Glacier is the longest, and the Hotlum is the most voluminous glacier in the state of California. Three of the smaller named glaciers occupy cirques near and above 11,000 ft (3,400 m) on the south and southeast sides, including the Watkins, Konwakiton, and Mud Creek glaciers.

Climbing Mount Shasta

The first recorded ascent of Mount Shasta occurred in 1854 (by Elias Pearce), after several earlier failed attempts. In 1856, the first women (Harriette Eddy, Mary Campbell McCloud, and their party) reached the summit. By the 1860s and 1870s, Mount Shasta was the subject of scientific and literary interest. A book by California pioneer and entrepreneur James Hutchings, titled Scenes of Wonder and Curiosity in California, contained an account of an early summit trip in 1855. The summit was achieved (or nearly achieved) by John Muir, Josiah Whitney, Clarence King, and John Wesley Powell. In 1877, Muir wrote a dramatic popular article about his surviving an overnight blizzard on Mount Shasta by lying in the hot sulfur springs near the summit. This experience was inspiration to Kim Stanley Robinson's short story "Muir on Shasta".

The 1887 completion of the Central Pacific Railroad, built along the line of the Siskiyou Trail between California and Oregon, brought a substantial increase in tourism, lumbering, and population into the area around Mount Shasta. Early resorts and hotels, such as Shasta Springs and Upper Soda Springs, grew up along the Siskiyou Trail around Mount Shasta, catering to these early adventuresome tourists and mountaineers.

Many climbers attempt the summit of Mount Shasta. The summer climbing season runs from late April until October, although many attempts are made in the winter. Avalanches and rapidly changing weather conditions make winter climbs more dangerous, however rock fall is a threat year round. Visit the Shasta-Trinity National Forest  web-site for more general information regarding other activites and safety information for The Shasta-Trinity National Forest.

Mount Shasta is also a popular destination for backcountry skiing. Many of the climbing routes can be descended by experienced skiers, and there are numerous lower-angled areas around the base of the mountain.

The most popular route on Mount Shasta is Avalanche Gulch route, which begins at the Bunny Flat Trailhead and gains about 7,300 feet (2,200 m) of elevation in approximately 11.5 miles (18.5 km) round trip. The crux of this route is considered to be to climb from Lake Helen, at approximately 10,443 feet (3,183 m), to the top of Red Banks. The Red Banks are the most technical portion of the climb, as they are usually full of snow/ice, are very steep, and top out at around 13,000 feet (4,000 m) before the route heads to Misery Hill. The Casaval Ridge route is a steeper, more technical route on the mountain's southwest ridge best climbed when there's a lot of snow pack. This route tops out to the left (north) of the Red Banks, directly west of Misery Hill. So the final sections involve a trudge up Misery Hill to the summit plateau, similar to the Avalanche Gulch route.^] Mount Shasta's west face as seen from Hidden Valley high on the mountain. The west face gulley is an alternate climbing route to the summit.

No quota system currently exists for climbing Mount Shasta, and reservations are not required. However, climbers must obtain a summit pass and a wilderness permit to climb the mountain. Permits and passes are available at the ranger station in Mount Shasta and the ranger station in McCloud, or climbers can obtain self-issue permits and passes at any of the trailheads 24 hours a day.

Sources:

- Mount Shasta in Summitpost.org

- Mount Shasta by College of the Siskiyous

- Mount Shasta Wikipedia Page

The painter 

Not to be  confused with the austrian physician, Joseph Breuer, Henry Joseph Breuer, born in Philadelphia, Pennsylvania,  in 1860 is a american painter who earned a reputation as a well-known "painter of poetic landscapes."  He studied art during the 1870s in Buffalo, New York, and then worked as a designer-decorator for the Rockwood Pottery Company in Cincinnati where he also attended the Art Academy. He worked for five years as a lithographer in New York City. 

In 1888, he settled in San Francisco where he became art editor for the San Francisco Chronicle and Californian magazine. Then he went to France for art study and was influenced by the Barbizon School of impressionist painters of rural landscapes. 

Living out of a horse-drawn wagon, he traveled extensively along the western coast of California and Oregon, painting and earning a national reputation for his landscapes. He also painted in Arizona including Canyon de Chelly in Navajo country and did commissioned views of the San Gabriel Valley for the St. Louis Exposition in 1904.


In 1903 he spent two weeks in  Mount Shasta which had a great impact on him. In the Cincinatti  Time Stars he wrote: 

" I board a train to some station somewhere near Mount Shasta,and this into the woods. I man a one- man camp every night for two weeks.  It was cold and sometimes miserable in the thick, wet, cold mist of the mountain side, but the days were grand before that high, white altar, Shasta! I shall feel for all my life that I was a true pilgrim, and for the sake of days like that, I am happy to be what I am, a landscape painter..."

Sources:  - Edan Hughes, Artists in California, 1786-1940 - Peggy and Harold Samuels, The Illustrated Biographical Encyclopedia of Artists of the American West - Breuer biography in Califonia Art Auction website - Breuer  biography in Rehs Gallery