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Tuesday, September 25, 2018

MOUNT WHITNEY PAINTED BY PAUL LAURITZ

https://wanderingvertexes.blogspot.com/2018/09/mount-whitney-painted-by-paul-lauritz.html

    
                                                          PAUL LAURITZ (1889–1975)
Mount Whitney  (4,421 m - 14,505 ft)
United States of America (California) 

 In The High Sierras,  oil on canvas, circa 1929 , The  Crocker Art Museum 

The mountain 
Mount Whitney (4,421 m - 14,505 ft) is the tallest mountain in California, as well as the highest summit in the contiguous United States and the Sierra Nevada.  It is in Central California, on the boundary between California's Inyo and Tulare counties. The west slope of the mountain is in Sequoia National Park and the summit is the southern terminus of the John Muir Trail which runs 211.9 mi (341.0 km) from Happy Isles in Yosemite Valley. The east slope is in the Inyo National Forest in Inyo County.
The rise is caused by a normal fault system that runs along the eastern base of the Sierra, below Mount Whitney. Thus, the granite that forms Mount Whitney is the same as the granite that forms the Alabama Hills, thousands of feet lower down.  The raising of Whitney (and the downdrop of the Owens Valley) is due to the same geological forces that cause the Basin and Range Province: the crust of much of the intermontane west is slowly being stretched.
In July 1864, the members of the California Geological Survey named the peak after Josiah Whitney, the State Geologist of California and benefactor of the survey.

The painter 
Born in a small art colony of  Norway, Lauritz was exposed to art at an early age, studying with local and foreign artists in Larvik. At age 16 he moved to eastern Canada to live with his sister and found work as a hardrock driller in a mine. Working his way west, he worked as a commercial artist in Vancouver and Portland, OR where he began painting landscapes and portraits. The meager existence in artwork led him to Alaska with the Gold Rush. Unsuccessful as a miner, he again turned to painting and became a close friend of artist Sydney Laurence. The two artists held a joint exhibition before Lauritz left Alaska. In 1919 he settled in Los Angeles and established a studio-home in the Lyceum Theatre on Spring Street. When not teaching at the Chouinard and Otis Art Institutes
or in his studio, he made painting excursions to the Sierra, up the California coast as far north as Carmel, to Mexico (1921), the Columbia River (1924), and Norway (1925).
While in his native land, he was commissioned by the King of Norway to do a painting for the royal palace. Lauritz was an involved member of the Los Angeles art community and served for six years on the Los Angeles Municipal Art Commission. A versatile painter, his diverse subjects include desert scenes, portraits, snow scenes, marines and landscapes.

2018 - Wandering Vertexes...
Un blog de Francis Rousseau, #BlogWanderingVertexes, #mountainpaintings


Friday, February 15, 2019

MOUNT WHITNEY PAINTED BY GUY ROSE




GUY ROSE  (1867-1925) 
Mount Whitney  (4,421 m - 14,505 ft)
United States of America (California) 

 In Gathering Storm, High Sierra,  oil on canvas, circa 1916 , The  Crocker Art Museum,  Sacramento

The mountain 
Mount Whitney (4,421 m - 14,505 ft) is the tallest mountain in California, as well as the highest summit in the contiguous United States and the Sierra Nevada.  It is in Central California, on the boundary between California's Inyo and Tulare counties. The west slope of the mountain is in Sequoia National Park and the summit is the southern terminus of the John Muir Trail which runs 211.9 mi (341.0 km) from Happy Isles in Yosemite Valley. The east slope is in the Inyo National Forest in Inyo County.
The rise is caused by a normal fault system that runs along the eastern base of the Sierra, below Mount Whitney. Thus, the granite that forms Mount Whitney is the same as the granite that forms the Alabama Hills, thousands of feet lower down.  The raising of Whitney (and the downdrop of the Owens Valley) is due to the same geological forces that cause the Basin and Range Province: the crust of much of the intermontane west is slowly being stretched.
In July 1864, the members of the California Geological Survey named the peak after Josiah Whitney, the State Geologist of California and benefactor of the survey.

 The painter 
The American Impressionist painter Guy Orlando Rose  was a California resident who received national recognition in the late 19th and early 20th centuries. His father was a prominent California senator. He and his wife raised their large family on an expansive Southern California ranch and vineyard – the San Gabriel Valley town of Rosemead bears the family name.
 In 1876 young Guy Rose was accidentally shot in the face during a hunting trip with his brothers. While recuperating he began to sketch and use watercolors and oil paints. He graduated from Los Angeles High School in 1884 and moved to San Francisco where he studied art between 1885 and 1888 at the School of Design with Virgil Williams, Warren E. Rollins, and the Danish-born artist Emil Carlsen.  On September 12, 1888, Rose enrolled at the Académie Julian in Paris and studied with Benjamin-Constant, Jules Lefebvre, Lucien Doucet and Jean-Paul Laurens while in Paris. In 1888-89, he won a scholarship at the Académie Delacluse and contributed religious and figural studies as well as landscapes to the Paris Salons in 1890, 1891, 1894, 1900, and 1909. He met fellow students Frank Vincent and Frederick Melville at the Académie Julian – Frank Vincent and Guy Rose were to remain lifelong friends.
Rose lived in New York, New York in the 1890s and illustrated for Harper's, Scribners, and Century. Choosing to return to France in 1899, he and his wife Ethel Rose bought a cottage at Giverny. In 1900 he resided in Paris and spent the winter in Briska, Algeria where he painted three known paintings. From 1904 to 1912 husband and wife lived in Giverny and his works from this period show the influence of "the master" Claude Monet, who became his friend and mentor.
Full wikipedia entry  =>

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2019 - Wandering Vertexes...
by Francis Rousseau 

Thursday, June 25, 2020

MOUNT WHITNEY PAINTED BY FRANZ BISHOFF






 
FRANZ BISHOFF (1864-1929)
Mount Whitney  (4,421 m - 14,505 ft)
United States of America (California)

The mountain
Mount Whitney (4,421 m - 14,505 ft) is the tallest mountain in California, as well as the highest summit in the contiguous United States and the Sierra Nevada. It is in Central California, on the boundary between California's Inyo and Tulare counties. The west slope of the mountain is in Sequoia National Park and the summit is the southern terminus of the John Muir Trail which runs 211.9 mi (341.0 km) from Happy Isles in Yosemite Valley. The east slope is in the Inyo National Forest in Inyo County.
The rise is caused by a normal fault system that runs along the eastern base of the Sierra, below Mount Whitney. Thus, the granite that forms Mount Whitney is the same as the granite that forms the Alabama Hills, thousands of feet lower down. The raising of Whitney (and the downdrop of the Owens Valley) is due to the same geological forces that cause the Basin and Range Province: the crust of much of the intermontane west is slowly being stretched.
In July 1864, the members of the California Geological Survey named the peak after Josiah Whitney, the State Geologist of California and benefactor of the survey.

The painter
Franz Albert Bischoff was an American artist known primarily for his China painting, floral paintings and California landscapes. He was born in Steinschцnau, Austria (now in Czech Republic).He immigrated to the United States as a teenager where he became a naturalized citizen. While in Europe, his early training was focused upon applied design, watercolor and ceramic decorations. After arriving in the United States, Bischoff worked in New York, Fostoria, Ohio, Detroit, Michigan and Dearborn, Michigan. While in Detroit and Dearborn, he gained success as a porcelain painter, and as a teacher of the techniques, as well as a manufacturer of ceramic glazes as well as a teacher of watercolor painting.Franz Bischoff decided to visit California in 1900 and ultimately chose to settle in the Los Angeles area in 1906. Shortly after arriving, he started making arrangements to design and build a large Italian Renaissance style home in Pasadena that also became his studio. This landmark home was completed in 1908. Bischoff was one of the earliest members of the California Art Club, and the group's second meeting was held at his studio on February 5, 1910. Also present at that meeting were Carl Oscar Borg and William Wendt.Inspired by the California countryside, Bischoff attempted to capture the area's brilliant light and diverse landscapes. Spending less time with ceramic painting following the start of World War I, Bischoff took up canvas painting. He painted local farms, fishing wharfs, coastal landscapes and scenes of the Sierra Nevada and the mountains of Utah, including Zion National Park. Recognized during his career for use of color and vivid composition, his paintings always displayed reverence for nature. One critic commented that some of his later works flirted with Expressionism and his use of colors were reminiscent of Fauvism. Franz Bischoff died of heart failure at home in his adopted city of South Pasadena, California on February 5, 1929.

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2020 - Wandering Vertexes...
by Francis Rousseau

Sunday, October 16, 2016

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 ArcThe 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 ShastaOkwanuchuModocAchomawiAtsugewiKarukKlamathWintu, 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 MuirJosiah WhitneyClarence 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:

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

Monday, December 25, 2017

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 CountyCalifornia. Mount Shasta  is the most voluminous stratovolcano in the Cascade Volcanic ArcThe 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 ShastaOkwanuchuModocAchomawiAtsugewiKarukKlamathWintu, 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 (WhitneyBolamHotlum, 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 WatkinsKonwakiton, 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.

Thursday, January 24, 2019

MOUNT MASSIVE BY WILLIAM HENRY JACKSON


WILLIAM HENRY JACKSON (1843-1942)
Mount Massive  (4,398 m - 14, 428 ft)
United States of America 

In  Mount Massive From Iron Hill, 1870, collodion  photography, Fogg Museum 

The mountain 
Mount Massive (4,398 m - 14, 428 ft) is the second-highest summit of the Rocky Mountains of North America and the U.S. state of Colorado. This prominent fourteener of the Sawatch Range is located in the Mount Massive Wilderness of San Isabel National Forest, 10.6 miles (17.1 km) west-southwest (bearing 247°) of the City of Leadville in Lake County, Colorado, United States.
Mount Massive edges out the third-highest summit of the Rockies, Mount Harvard, by 7 feet (2.1 m), but falls short of Mount Elbert by 12 feet (3.7 m). It ranks as the third-highest peak in the contiguous United States after Mount Whitney and Mount Elbert.
Mount Massive was first surveyed and climbed in 1873 during the Hayden Survey of the American West. Survey member Henry Gannett is credited with the first ascent. Its name comes from its elongated shape: it has five summits, all above 14,000 ft (4,300 m), and a summit ridge over 3 mi (4.8 km) long, resulting in more area above 14,000 ft (4,300 m) than any other mountain in the 48 contiguous states, narrowly edging Mount Rainier in that category. Mount Elbert (14,440 ft (4,400 m)) is Mount Massive's nearest neighbor among the fourteeners; it lies about 5 mi (8.0 km) south-southeast of the peaks.
There are several glacial lakes in the wilderness area. The lower slopes of the mountain are covered in lodgepole pine forests, which gradually yield to Engelmann Spruce and Fir. Treeline is just below 12,000 feet. Among the mountain's fauna are the American pika, the mountain goat, elk, mule deer, moose, gray jay, martin, and the yellow-bellied marmot.

The artist
William Henry Jackson  was an American painter, Civil War veteran, geological survey photographer and an explorer famous for his images of the American West. He was a great-great nephew of Samuel Wilson, the progenitor of America's national symbol Uncle Sam.
In 1869 Jackson won a commission from the Union Pacific to document the scenery along the various railroad routes for promotional purposes. When his work was discovered by Ferdinand Hayden, who was organizing a geologic survey to explore the Yellowstone River region, he was asked to join the expedition.
The following year, he got a last-minute invitation to join the 1870 U.S. government survey (predecessor of U.S. Geological Survey) of the Yellowstone River and Rocky Mountains led by Ferdinand Hayden. He also was a member of the Hayden Geological Survey of 1871[6] which led to the creation of Yellowstone National Park. Painter Thomas Moran was also part of the expedition, and the two artists worked closely together to document the Yellowstone region. Hayden's surveys (usually accompanied by a small detachment of the U.S. Cavalry) were annual multidisciplinary expeditions meant to chart the largely unexplored west, observe flora (plants), fauna (animals), and geological conditions (geology), and identify likely navigational routes, so as official photographer for the survey, Jackson was in a position to capture the first photographs of legendary landmarks of the West. These photographs played an important role in convincing Congress in 1872 to establish Yellowstone National Park, the first national park of the U.S. His involvement with Hayden's survey established his reputation as one of the most accomplished explorers of the American continent. Among Hayden's party were Jackson, Moran, geologist George Allen, mineralogist Albert Peale, topographical artist Henry Elliot, botanists, and other scientists who collected numerous wildlife specimens and other natural data.
Jackson worked in multiple camera and plate sizes, under conditions that were often incredibly difficult.  His photography was based on the collodion process invented in 1848 and published in 1851 by Frederick Scott Archer.  Jackson produced more than 900 photographs for the commission, which are now part of a collection on display at the Library of congress.

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2019 - Wandering Vertexes...
by Francis Rousseau 

Wednesday, November 29, 2017

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.

Thursday, April 2, 2020

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.

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2020 - Wandering Vertexes...
by Francis Rousseau






Wednesday, January 25, 2023

LE MONT WILLIAMSON PAR ANSEL ADAMS


ANSEL ADAMS  (1902-1984) Mont Williamson (4,383m) Etats-Unis d'Amérique (Californie)  In Mount Williamson Sierra Nevada, 1944, photographie


ANSEL ADAMS  (1902-1984)
Mont Williamson (4,383m)
Etats-Unis d'Amérique (Californie)

In Mount Williamson Sierra Nevada, 1944, photographie


La montagne
Le mont Williamson (4 383 mètres) culmine au centre de la Californie, dans l'Ouest des États-Unis. Il fait partie de la Sierra Nevada et se situe à moins de dix kilomètres du mont Whitney, le point culminant du massif et le plus haut sommet du pays en dehors de l'Alaska. Il est constitué de granite. Gravi pour la première fois en 1884, il reste difficile d'accès et peu fréquenté. La montagne est protégée intégralement par la réserve intégrale John Muir et la forêt nationale d'Inyo, ainsi que par la California Bighorn Sheep Zoological Area destinée à protéger une sous-espèce menacée de mouflon endémique de la Sierra Nevada.

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.

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



 

Sunday, September 3, 2023

LE MONT SHASTA /UYTAAHKOO PEINT PAR FRANK TENNEY JOHNSON

 

FRANK TENNEY JOHNSON T1874-1939) Mont Whitney / Tumanguya ( 4,417 m) Etats -Unis d'Amérique (Californie)  In Cowboys roping the bear, huile su toile, Collection privée (Christie's)


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

Monday, February 24, 2020

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

Friday, March 22, 2019

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