MOUNT COLEMAN PAINTED BY ARTHUR P. COLEMAN

 

ARTHUR P. COLEMAN (1852-1939)
Mount Coleman (3,135 m-10,285 ft)
Canada (Alberta) 

 In  "Mountain un the Canadian rockies"

The mountain
Mount Coleman (3,135 m-10,285 ft) mountain summit located in the upper North Saskatchewan River valley in Banff National Park, in the Canadian Rockies of Alberta, Canada. Its nearest higher peak is Cirrus Mountain, 4.46 km (2.77 mi) to the north.  Mount Coleman is situated along the east side the Icefields Parkway midway between Saskatchewan Crossing and Sunwapta Pass.
Mount Coleman was named in 1898 after Arthur Philemon Coleman (1852-1939), a Canadian geologist and among the first white men to explore the area that is now Jasper National Park.(see below). Like other mountains in Banff Park, Mount Coleman is composed of sedimentary rock laid down from the Precambrian to Jurassic periods. Formed in shallow seas, this sedimentary rock was pushed east and over the top of younger rock during the Laramide orogeny.  Based on the Köppen climate classification, Mount Coleman is located in a subarctic climate with cold, snowy winters, and mild summers.  Temperatures can drop below -20 °C with wind chill factors below -30 °C. Precipitation runoff from Mount Coleman drains into tributaries of the North Saskatchewan River.

The painter
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 is named in his honor. He was awarded the Penrose Medal in 1936.
He planned to climb "his" mountain, "Mount Coleman"'in the Albertan Rockies, and had also prepared a trip to British Guiana, but death intervened.
He was author of:
- Reports on the Economic Geology of Ontario (1903)
- Lake Ojibway; Last of the Great Glacial Lakes (1909)
- The Canadian Rockies: New and Old Trails (1911)
- Ice Ages, Recent and Ancient (1926), and was co-author of Elementary Geology (1922).
- The Last Million Years (1941) edited by George F. Kay

__________________________________________
2022 - Wandering Vertexes...
by Francis Rousseau

CLYDE PEAK PAINTED BY ARTHUR P. COLEMAN

 

ARTHUR P. COLEMAN (1852-1939)
Clyde Peak (2,624 m - 8,610 ft)
United States of America (Montana)

In Mountain South Clide, watercolor on paper, 1895 A.P Coleman Funds.

The mountain
Clyde Peak 2,624 m- is an 8,610 ft) is  located in Glacier National Park in the U.S. state of Montana. The mountain straddles the border shared by Flathead County and Glacier County. It is situated on the Continental Divide so precipitation runoff from the west side of the mountain drains into Thompson Creek which is part of the Middle Fork Flathead Riverwatershed, and the east side drains into headwaters of Red Eagle Creek, which flows to Red Eagle Lake, thence Saint Mary Lake. It is set in the Lewis Range, and the nearest higher neighbor is Mount Logan 1.44 mile to the northwest. Topographic relief is significant as the southwest aspect rises approximately 4,000 feet (1,220 meters) in one mile.
The mountain's name commemorates Norman Clyde (1885–1972), who made the first ascent of this peak on July 23, 1923.  Clyde is credited with 130 first ascents, most of which were in the Sierra Nevada of California.[ In 1923 he spent 36 days in Glacier National Park, Montana, where he climbed 36 mountains, including 11 first ascents.

The painter
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 is named in his honor. He was awarded the Penrose Medal in 1936.
He planned to climb "his" mountain, "Mount Coleman"'in the Albertan Rockies, and had also prepared a trip to British Guiana, but death intervened.
He was author of:
- Reports on the Economic Geology of Ontario (1903)
- Lake Ojibway; Last of the Great Glacial Lakes (1909)
- The Canadian Rockies: New and Old Trails (1911)
- Ice Ages, Recent and Ancient (1926), and was co-author of Elementary Geology (1922).
- The Last Million Years (1941) edited by George F. Kay

 
___________________________________________
2021 - Wandering Vertexes...
by Francis Rousseau

MOUNT BRAZEAU BY ARTHUR. P. COLEMAN

ARTHUR P. COLEMAN (1852-1939)

Mount Brazeau (3, 500 m - 11, 483 ft) 

Canada (Alberta) 

 In The Brazeau from camp 17, 1892 watercolor 

The mountain 

Mount Brazeau  (3, 470m - 11, 380ft)  is a mountain in  Canada (Alberta),  located in the upper Coronet Creek Valley of Jasper National Park. It stands west of the Coronet Glacier and south of Maligne Lake. The mountain was named in 1902 by Arthur P. Coleman (who painted the mountain as well) after Joseph Edward Brazeau, who had provided his translation skills to the Palliser Expedition. The name Brazeau was originally applied to the Brazeau River by Sir James Hector ( the most important members of the Palliser Expedition, becoming the first to travel through much of the Canadian Rockies.) 

Mount Brazeau is an impressive mountain with several striking and formidable faces falling down to Maligne Lake and Coronet Creek in southern Jasper National Park. The West Face is massive and near vertical, rising nearly 1,000 metres (3,280 ft.) from Coronet Creek to the summit plateau, which is draped in the glacial mass of the Brazeau Icefield. The south and southwest slopes, topped with the Brazeau Icefield, are low angle and gentle, but are riddled with a minefield of hidden crevasses. 

Mount Brazeau is high on the list of Canadian Rockies 11,000 footers, depending on your perspective, either the thirteenth, seventeenth or twenty first highest mountain in the Canadian Rockies; 21 th on the generally accepted list of 54 summits. 

Jasper National Park  (11,228 square kilometres -4,335 square miles) is the largest of Canada's Rocky Mountain Parks and part of a UNESCO World Heritage Site. 

The painter 
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 is 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.
He was author of:
- Reports on the Economic Geology of Ontario (1903)
- Lake Ojibway; Last of the Great Glacial Lakes (1909)
- The Canadian Rockies: New and Old Trails (1911)
- Ice Ages, Recent and Ancient (1926), and was co-author of Elementary Geology (1922).
- The Last Million Years (1941) edited by George F. Kay

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.

ROCHE MIETTE PAINTED BY ARTHUR P. COLEMAN

ARTHUR P. COLEMAN (1852-1939)

 Roche Miette (2,316m - 7,600 ft) 

Canada

The mountain 

Roche Miette mountain  (2,316m - 7,600 ft) is part Miette Range (in the Canadian Rockies) located in the Athabasca River Valley southwest of Mountain Creek and northeast of Rocky River.  Roche Miette dominates the entrance to the Canadian Rockies. Ben Gadd, author of “Handbook of the Canadian Rockies” feels that the name "Miette" is derived from the Cree word "Myat," which means "bighorn sheep." He thinks that this makes a lot of sense, considering that sheep frequented the lower slopes of the mountain. According to Don Beers, author of “Jasper-Robson –A Taste of Heaven” the name was first recorded as Roche Miette in a journal written by Gabriel Franchere. However Don feels that the mountain was likely named after a voyageur named Baptiste Millette, who worked in the fur trade in the Athabasca River area during 1812 and 1813.  "Roche" is the French word for "rock"  and "Miette" means "crumb". Roche Miette is the official name but an other name is  often given : Millet's Rock. 

In their book, "The Northwest Passage by Land" (1865) William Fitzwilliam (Viscount Milton) and Walter Cheadle describe the northern cliffs of the mountain as they approached from the east as, "a cleft in the range, cut clean as with a knife" and that showed, "what we supposed to be the opening of the gorge through which we were to pass."

When James Hector visited the area in 1859 he wrote that, "Miette's Rock is a bold object, bounding the valley of the Athabasca to the south, and resembling the "Devil's Head which lies to the north of the Bow River". He tried to climb the mountain with Moberly, reaching a sharp peak high above any vegetation but the great cubical block still towered above them and they could go no higher.

In his book, "The Glittering Mountains of Canada" J. Monroe Thorington mentions that Dr. Hector (James Hector of the Palliser Expedition who travelled up the Athabasca Valley during the winter in early 1859) always enjoyed a mountain-scramble and wrote, "I started with Moberly to ascend the Roche Miette... After a long and steep climb, we reached a sharp peak far above any vegetation, and which, as measured by the aneroid, is 3500 feet above the valley. The great cubical block which forms the top of this mountain, still towered above us for 2000 feet, and is quite inaccessible from this side, and is said to have been only once ascended from the south side by a hunter named Miette, after whom it was named."

Legend has it that Bonhomme Miette was a French-Canadian voyageur who made the first ascent, climbing it from its south side. He became a well-known figure in French Canadian folklore and was said to have been a gifted fiddler and storyteller. When he reached the top, the story goes, he sat down, dangling his feet over the precipice, smoked his pipe, and as Miette himself put it "I been have de nice smoke up dere wit St. Peter on de gate." During the 1830's it is known that a man named Miette did live in the Athabasca Valley where he was a "company servant" who hauled coal from the area of Roche Miette to Jasper House as well as to Henry House at the mouth of the Miette River. Ben Gadd believes that Bonhomme Miette was a “legendary” voyageur as no one by that name worked for either the Hudson Bay Company or the Northwest Company during the years prior to 1814. 

Many early travelers wrote of Roche Miette with admiration but their enthusiasm was tempered by the barrier it presented. Roche Miette slopes steeply into the Athabasca and posed a serious obstacle to those travelling up the south bank of the river. Steep, downward sloping slabs of slippery rock often sent horses sliding down into the river at what became known as "Disaster Point." Early travelers attempted to negotiate a dangerous trail that climbed some 395 metres above the river. One referred to, "a very narrow pathway, with a perpendicular wall of rock on one side, and a steep declivity down to the edge of a precipice several hundred feel high on the other." The dangerous "nose" of Roche Miette remained an obstacle until it was blasted away by the railway builders in the early 1900's.

Arthur Coleman (painting above) exited the Canadian Rockies via the Athabasca Valley in 1907, describing Roche Miette as, "The most impressive bit of architecture along the Athabasca, pushing its bold front out into the valley like a commanding fort with unscalable walls three thousand feet high, and a flat top somewhat parapeted and loop-holed."

Climbing

North Face IV 5.8 A3

This climb takes on the impressive N face. An alpine rock route that starts off at a moderate standard (5.6-5.8) and ends up with some A3 thrown in near the end for a complete Rockies rock experience. The rock is excellent throughout, belays are good and the pitches are generally full 50 m affairs. Originally climbed with a bivi but this no doubt was a result of a 4 pm alpine start! It could be climbed in a day, though you will have to be slick to complete a round trip road to road in this time. 

The painter 

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 is 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.

He was author of:

- Reports on the Economic Geology of Ontario (1903)

- Lake Ojibway; Last of the Great Glacial Lakes (1909) 

- The Canadian Rockies: New and Old Trails (1911)

- Ice Ages, Recent and Ancient (1926), and was co-author of Elementary Geology (1922).

- The Last Million Years (1941) edited by George F. Kay

ATITLAN & TOLIMAN VOLCANOS BY ARTHUR P. COLEMAN (1852-1939)

ARTHUR P. COLEMAN (1852-1939)

  Atitlбn (3,535 m -11,598ft) & Tolimбn  (3,158 m -10,361ft) 

Guatemala 

In Atitlan and Tolimon seen from Lake Atitlan, 1937, watercolor, 

The mountains

Atitlбn volcano  (3,535 m - 11,598 ft)  is a large, conical, active stratovolcano adjacent to the caldera of Lake Atitlбn in the Guatemalan Highlands of the Sierra Madre de Chiapas range. It is within the Sololб Department, northern Guatemala. The volcano has been quite active historically, with more than a dozen eruptions recorded between 1469 and 1853, the date of its most recent eruption. Atitlбn is part of the Central American Volcanic Arc. The arc is a chain of volcanoes stretching along Central America formed by subduction of the Cocos Plate underneath the Caribbean Plate. This volcano is part of the Ring of Fire around the Pacific Ocean. Atitlбn is home to two particularly rare and beautiful birds that are endemic to the cloud forests of this region. The horned guan (Oreophasis derbianus) is a Pleistocene relic of the Cracidae family that persists today only in small fragments of its previous range. Its habitat is limited to cloud forests above approximately 1,650 metres (5,410 ft). This bird is the size of a turkey and the adult male has a one-inch scarlet-colored "horn" projecting straight up from the top of its head. The Cabanis's or azure-rumped tanager (Tangara cabanisi) is probably the most restricted-range species in the region. It occurs only at mid-elevations within the Sierra Madre del Sur of Chiapas, Mexico and western Guatemala. Atitlбn lies on the southern rim of the caldera, while Volcano San Pedro and Volcano Tolimбn lie within the caldera. San Pedro is the oldest of the three and seems to have stopped erupting about 40,000 years ago. Tolimбn began growing after San Pedro stopped erupting, and probably remains active, although it has not erupted in historic times. Atitlбn has developed almost entirely in the last 10,000 years and remains active, with its most recent eruption having occurred in 1853.




Tolimбn volcano  (3,158 m -10,361 ft) is located on the southern shores of Lago de Atitlбn. The volcano  was formed near the southern margin of the Pleistocene Atitlбn III caldera. The top of the volcano has a shallow crater and its flanks are covered with the thick remains of ancient lava flows that emerged from vents in the volcano's flanks. A parasitic lava dome, known as Cerro de Oro, was formed on the volcano's northern flank, which may have erupted a few thousand years ago.




San Pedro volcano  (3,020m -9,908 ft) (also named Las Yeguas) represented in the foggy background of in the Coleman painting, is the third stratovolcano on the shores of Lago de Atitlбn, in the Solol Department of northern Guatemala. At its base is the village of San Pedro La Laguna.




The first volcanic activity in the region occurred about 11 million years ago, and since then the region has seen four separate episodes of volcanic growth and caldera collapse, the most recent of which began about 1.8 million years ago and culminated in the formation of the present caldera. The lake now fills a large part of the caldera, reaching depths of up to 600 metres.

The caldera-forming eruption is known as Los Chocoyos eruption and ejected up to 300 km3 (72 cu mi) of tephra. The enormous eruption dispersed ash over an area of some 6 million kmІ: it has been detected from Florida to Ecuador, and can be used as a stratigraphic marker in both the Pacific and Atlantic oceans (known as Y-8 ash in marine deposits). A chocoyo is a type of bird which is often found nesting in the relatively soft ash layer.

On February 4, 1976, a massive earthquake (magnitude 7.5) struck Guatemala, killing more than 26,000 people. The earthquake fractured the lake bed and caused subsurface drainage from the lake, allowing the water level to drop two meters within one month

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 is 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.

He was author of:

- Reports on the Economic Geology of Ontario (1903)

- Lake Ojibway; Last of the Great Glacial Lakes (1909) 

- The Canadian Rockies: New and Old Trails (1911)

- Ice Ages, Recent and Ancient (1926), and was co-author of Elementary Geology (1922).

- The Last Million Years (1941) edited by George F. Kay

MOUNT BALL PAINTED BY ARTHUR P. COLEMAN

ARTHUR P. COLEMAN (1852-1939)

Mount Ball  (3,311 m - 10,863 ft) 

Canada (Alberta)

The mountain 
Mount Ball is a mountain located on the Continental Divide, on the borders of Banff and Kootenay national parks in Canada. Mt. Ball is the highest peak of the Ball Range in the Canadian Rockies.
The mountain was named in 1858 by James Hector after John Ball, a politician who helped secure funding for the Palliser Expedition.  Mount Ball was first climbed in 1904 by J.D. Patterson, guided by Christian & Hans Kaufmann. The name was officially adopted in 1924 based on Palliser's 1863 map of British North America. Mt. Ball can be ascended from a scrambling route by late summer but involves remote bushwhacking, which limits the number of attempts per year. The trailhead is located at the Marble Canyon Campground in Kootenay National Park.

The painter 
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.
 "Mount Coleman" and "Coleman Glacier" in Banff National Park are named in his honor. 
He was awarded the Penrose Medal in 1936.

_______________________________

 

2018 - Wandering Vertexes...

by Francis Rousseau 

SURPRISE MOUNTAIN BY ARTHUR. P. COLEMAN

ARTHUR P. COLEMAN (1852-1939)

Surprise Mountain  (1,929m - 63,30ft) 

United States of America (Washington State) 

In Surprize Mountain, Showing Thalkessel, left side in shade, watercolor 

The mountain 
Surprise Mountain  (1,929m - 63,30ft) is an alpine peak nestled in the middle of the Alpine Lakes Wilderness of Washington State. Perhaps appropriately, several alpine lakes are found near the mountain. The Deception Lakes are located at the south end of the mountain, and Glacier Lake and Surprise Lake are located northeast of the mountain. Views of surrounding peaks and valleys from the mountain are also far-reaching, including Mount Daniel and Glacier Peak. Surprise Mountain is located southeast of Spark Plug Mountain and southwest of Thunder Mountain.
In 1932, the U.S. Forest Service built a L-4 cab fire lookout on the summit of Surprise Mountain, due to its wide views of the Central Cascade Mountains. The U.S. Forest Service then decommissioned and destroyed the fire lookout during the 1950s. The only remnant of the lookout that remains today is a tall metallic pole at the mountain summit.

The painter 
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.
 "Mount Coleman" and "Coleman Glacier" in Banff National Park are named in his honor.
He was awarded the Penrose Medal in 1936.

_______________________________

2019 - Wandering Vertexes...

by Francis Rousseau 

MOUNT CAUBVICK/ MONT D'IBERVILLE PAINTED BY ARTHUR P. COLEMAN

 

 

ARTHUR P. COLEMAN (1852-1939)

Mount Caubvick / Mont D'Iberville (1,652 m -5,420 ft) 

Canada (Labrador /Quebec border) 

In Mountains South of Nakvak, Labrador; oil on canvas, 1910, Private collection

The mountain 
Mount Caubvick / Mont D'Iberville (1,652 m -5,420 ft)  is a mountain located in Canada on the border between Labrador and Quebec in the Selamiut Range of the Torngat Mountains. Mount Caubvick is the highest point in mainland Canada east of the Rockies. The mountain contains a massive peak that rises sharply from nearby sea level. Craggy ridges, steep cirques and glaciers are prominent features of the peak.
The alp was named Mont d'Iberville by the Quebec government in 1971. It remained nameless on the Labrador side for several years; it became known unofficially as L1, L for Labrador and 1 for highest. In 1981, at the suggestion of Dr. Peter Neary, the provincial government named the mountain after Caubvick, one of the five Inuit who accompanied George Cartwright to England in 1772.
Mount Caubvick also hosts the highest point in both the province of Newfoundland and Labrador and Quebec, although the summit itself lies about 10 metres (33 ft) northeast of the Quebec provincial border and is entirely within Labrador.

The painter
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.
"Mount Coleman" and "Coleman Glacier" in Banff National Park are named in his honor.
He was awarded the Penrose Medal in 1936.

_______________________________

2020 - Wandering Vertexes...
by Francis Rousseau

MOUNT ROBSON BY ARTHUR P. COLEMAN

ARTHUR P. COLEMAN (1852-1939)
Mount Robson (3,954 m - 12, 972 ft) 

Canada (British Columbia)

  In Mount Robson glacier -cutting steps, oil on canvas

The mountain 

Mount Robson (3,954 m - 12, 972 ft) is the most prominent mountain in North America's Rocky Mountain range; it is also the highest point in the Canadian Rockies. The mountain is located entirely within Mount Robson Provincial Park of British Columbia, and is part of the Rainbow Range. Mount Robson is the second highest peak entirely in British Columbia, behind Mount Waddington in the Coast Range. The south face of Mount Robson is clearly visible from the Yellowhead Highway (Highway 16), and is commonly photographed along this route.

Mount Robson was likely named after Colin Robertson, who worked for both the North West Company and the Hudson’s Bay Company at various times in the early 19th century, though there was confusion over the name as many assumed it to have been named for John Robson, an early premier of British Columbia. The Texqakallt, a Secwepemc people and the earliest inhabitants of the area, call it Yuh-hai-has-kun (The Mountain of the Spiral Road). Other unofficial names include Cloud Cap Mountain.

In 1893, five years after the expedition of A.P. Coleman to Athabasca Pass and the final settling of the mistaken elevations of Mt. Hooker and Mt. Brown, Mt. Robson was first surveyed by James McEvoy and determined to be the highest peak in the Canadian Rockies. The first documented ascent of Mount Robson, led by the young guide Conrad Kain, at its time the hardest ice face to be climbed on the continent, was achieved during the 1913 annual expedition organized by a large party of Alpine Club of Canada members who made use of the newly completed Grand Trunk Pacific railway to access the area. Prior to 1913, it had been necessary to approach the mountain by pack train from Edmonton or Laggan via Jasper and Lucerne, so only few intrepid explorers had made previous attempts at exploring the mountain. The most famous early ascensionist was the Reverend George Kinney, a founding member of the Alpine Club, who on his twelfth attempt in August 1909 claimed to have reached the summit with local outfitter Donald "Curly" Phillips. A major controversy over this claim and over the implausible nature of his unlikely and dangerous route dominated the discourse within the Alpine Club elite, and he is now generally presumed to have reached the high summit ridge before being turned back at the final ice dome of the peak. Kinney Lake, below the south face, is named in his honour.

The north face of Mount Robson is heavily glaciated and 800 m (2,600 ft) of ice extends from the summit to Berg Glacier. The Berg glacier calves directly into the lake. The Robson Glacier, which fills the cirque and valley between Mount Robson and Mount Resplendent, in the early 1900s fed directly into both Berg lake and Adolphus lake, straddling the Continental Divide and draining thus to both the Arctic and Pacific oceans via the Smoky and Robson Rivers, respectively. It since has receded more than 2 kilometres and is the source of the Robson River only.

The painter 
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.
 "Mount Coleman" and "Coleman Glacier" in Banff National Park are named in his honor.
He was awarded the Penrose Medal in 1936.

_______________________________

2019 - Wandering Vertexes...

by Francis Rousseau 

CASTLE MOUNTAIN IN VINTAGE POSTCARD 1947

VINTAGE POSTCARD  1947

Castle Mountain or  Mount Eisenhower   (2,766m - 9,075ft)

Canada

 In Castle Mountain in Banff National Park, 1947, Hand-tinted photograph  

The mountain 

Castle Mountain (2,766m - 9,075ft) also named Mount Eisenhower between 1946 and 1979, is a mountain located within Banff National Park in the Canadian Rockies, approximately halfway between Banff and Lake Louise. It is the easternmost mountain of the Main Ranges in the Bow Valley and sits astride the Castle Mountain Fault which has thrust older sedimentary and metamorphic rocks forming the upper part of the mountain over the younger rocks forming its base. The mountain's castellated, or castle-like, appearance is a result of erosive processes acting at different rates on the peak's alternating layers of softer shale and harder limestone, dolomite and quartzite.
The mountain was named in 1858 by James Hector for its castle-like appearance. From 1946 to 1979 it was known as Mount Eisenhower in honour of the World War II general Dwight D. Eisenhower. Public pressure caused its original name to be restored, but a pinnacle on the southeastern side of the mountain was named Eisenhower Tower. Located nearby are the remains of Silver City, a 19th-century mining settlement, and the Castle Mountain Internment Camp in which persons deemed enemy aliens and suspected enemy sympathizers were confined during World War I.
While looking nearly inaccesible from the Trans-Canada Highway, the peak can be ascended from the backside on the northeastern slopes. The trail to Rockbound Lake leads hikers around the eastern side. The massif contains several high points including Helena Ridge (2,862 m - 9,390 ft), Stuart Knob (2,850 m - 9,350 ft) and Television Peak (2,970 m - 9,744 ft), the latter being named for the TV repeater located on top. Technicians use a helicopter rather than hiking the long ascent to the top.
James Hector, who accompanied the Palliser Expedition, encountered Castle Mountain in August 1858 while leading a side expedition to find the headwaters of the Bow River. He noted that it "...looks exactly like a gigantic castle" and named it Castle Mountain.  He also made the first recorded ascent of its slopes, but is not believed to have reached its summit.
The first climber to reach the top of Castle Mountain was Arthur P. Coleman, a professor at the University of Toronto, in 1884. Lawrence Grassi and P. Cerutti, both from Canmore, were the first to climb Eisenhower Tower in 1926.
In 1881, Joe Healy received some ore in trade from a First Nations person which was discovered to contain a relatively high silver content. The following year he settled at Castle Mountain as a prospector. News of Healy's ore soon spread; others began to arrive and the settlement of Silver City, situated near Castle Mountain, quickly developed. It was already thriving when the Canadian Pacific transcontinental railroad was built through the area in 1884.  Over three thousand people lived there at its height, but it was almost entirely abandoned in 1885 because the mines failed to yield a significant profit.
Situated nearby is Castle Mountain Internment Camp, a First World War internment camp where Ukrainian immigrants to Canada were confined. Life in the camps was often described as 'grim'; with its isolated location far from the roads of the time, the Castle Mountain camp was an ideal place to confine 'enemy aliens' and 'suspected enemy sympathisers'. The forced labour of these men helped build much of the infrastructure of Banff National Park. Internees were held at the Cave & Basin site during the winter months.
Construction began in 1910 at Castle Junction on a highway connecting British Columbia to Calgary that would, upon its completion in the early 1920s, make Castle Mountain more accessible to climbers, hikers and other tourists.


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 ATHABASCA PAINTED BY ARTHUR P. COLEMAN

ARTHUR P. COLEMAN (1852-1939)

Mount Athabasca  (3,491m - 11,453ft)

Canada

1. In Athabasca near Wicox pass, 1807, watercolour, Private coll.

2.  In Athabasca near Wilcox Pass between Saskatchewan & Athabasca,watercolour, Private coll.  

3.  In  Up the Athabasca from Junction of Sunwapta, 1893, drawing, Private coll. 

The mountain 

Mount Athabasca (3,491m - 11,453ft) or Athabaska, is located in the Columbia Icefield of  Jasper National Park  in Canada. Athabasca is the Cree Indian name for "where there are reeds" which originally referred to Lake Athabasca.The first known Europeans to discover this peak in 1896 were Walter Wilcox, Robert Barrett and their two guides. They made an attempt to climb the peak but were unsuccessful.The mountain was named in 1898 by J. Norman Collie and ,Herman Woolley who made the first ascent on August 18 of that year. This climb of the mountain was the result of nineteen days of travel and searching on horseback and on foot, beginning in Lake Louise. It is a lot easier today.

After Mount Robson and Mount Temple, Mt. Athabasca may be the most well-known peak in the Canadian Rockies. It was my first Canadian alpine ascent and the same goes for many. The surrounding area include, Mt Andreomeda, Snow Dome, Mt. Kitchener, Mt Wilcox and Nigel Peak.

Definitely a main climbing and tourist attraction in the area.


Climbing 

There are several climbing routes, including:  North Glacier (Normal Route), Silverhorn, AA Col II, Regular North Face III 5.8, North Ridge III 5.5, The Hourglass 300m, III, AI3-4. One of the most prominent features of Mount Athabasca is a horned-shaped tip near the top called the "Silverhorn". The Silverhorn is one of the easier routes to the summit but requires more caution and ability than the normal route because of Blue ice and falling ice from other parties. Although not apparent from the typical roadside view of the mountain, the south side of Silverhorn actually contains a scrambling route but one must still cross the north glacier to get to it. From the top of the Silverhorn, the summit is a rather easy 15-minute plod in good summer weather over the narrow snow-covered summit ridge.

Sources: 

- Mount Athabaska page in summit post.org 

- The Alpine Club of Canada 

- Parks Canada

The artist 

Arthur Philemon Coleman Biography in this blog