ATITLAN VOLCANO BY ALFRED MAUDSLAY

ALFRED MAUDSLAY (1850-1931) 

Atitlбn (3,535 m -11,598ft) 

Guatemala

 In Lake and volcano of Atitlan, gelatine print, 1898 

The mountain
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.

The photographer 
The  British diplomat, explorer and archaeologist Alfred Percival Maudslay  was also a photographer... and rather a good one according to the numerous photographs on dry plate he left.   He was one of the first Europeans to study Maya ruins.
After leaving Medical School, he moved to Trinidad, becoming private secretary to Governor William Cairns, and transferred with Cairns to Queensland. He subsequently moved to Fiji to work with Sir Arthur Gordon, its governor.  Later he served as British consul in Tonga and Samoa. In February 1880, Maudslay resigned from the colonial service to pursue his own interests, having spent six years in the British Pacific colonies. He then joined his siblings in Calcutta during their round-the-world trip, returned to Britain in December, and then set out for Guatemala via British Honduras.
In Guatemala, Maudslay began the major archaeological work for which he is now best remembered. He started at the Maya ruins of Quirigua and Copan where, with the help of Frank Sarg, he hired labourers to help clear and survey the remaining structures and artefacts. Sarg also introduced Maudslay to the newly found ruins in Tikal and to a reliable guide Gorgonio López. Maudslay was the first to describe the site of Yaxchilán. With Teobert Maler, Alfred Maudslay explored Chichén in the 1880s and both spent several weeks at the site and took extensive photographs. Maudslay published the first long-form description of Chichen Itza in his book, "Biologia Centrali-Americana".
In the course of his surveys, Maudslay pioneered many of the later archaeological techniques. He hired Italian expert Lorenzo Giuntini and technicians to make plaster casts of the carvings, while Gorgonio López made casts of papier-mâché. Artist Annie Hunter drew impressions of the casts before they were shipped to museums in England and the United States. Maudslay also took numerous detailed photographs – dry plate photography was then a new technique – and made copies of the inscriptions.
All told, Maudslay made a total of six expeditions to Maya ruins. After 13 years of preparation, he published his findings in 1902 as a 5-volume compendium entitled Biologia Centrali-Americana, which contained numerous excellent drawings and photographs of Maya ruins, Maudslay's commentary, and an appendix on archaic calendars by Joseph Thompson Goodman.
In 1907 the Maudslays moved permanently back to Britain. Maudslay become a President of the Royal Anthropological Institute 1911–12. He also chaired the 18th International Congress of Americanists in London in 1912.

______________________________
2019 - Wandering Vertexes...
by Francis Rousseau 

SANTA MARIA VOLCANO PHOTOGRAPHED BY TEMPEST ANDERSON

TEMPEST ANDERSON (1846-1913)

Santa María Volcano (3,772m- 12, 375ft)

Guatemala

In Santa Maria Volcano crater of 1902,  photographed in 1907, black and white glass lantern slide 

The mountain 
Santa María Volcano (3,772m- 12, 375ft)  is a large active volcano in the western highlands of Guatemala, in the Quetzaltenango Department near the city of Quetzaltenango.
The volcano was known as Gagxanul in the local K'iche' language, before the 16th century Spanish Conquest of the region.
The VEI 6 eruption of Santa María Volcano in 1902 was one of the  largest eruptions of the 20th century and one of the five biggest eruptions of the past 200 (and most likely 300) years.
Santa María Volcano is part of the Sierra Madre range of volcanoes, which extends along the western edge of Guatemala, separated from the Pacific Ocean by a broad plain. The volcanoes are formed by the subduction of the Cocos Plate under the Caribbean Plate, which led to the formation of the Central America Volcanic Arc.
Eruptions at Santa María are estimated to have begun about 30,000 years ago but the The VEI 6 eruption of october 1902 is the first eruption in recorded history. Before 1902 the volcano had been dormant for at least 500 years and possibly several thousand years, but its awakening was clearly indicated by a seismic swarm in the region starting in January 1902, which included a major earthquake in April 1902. The eruption began on 24 October, and the largest explosions occurred over the following two days, ejecting an estimated 5.5 cubic kilometres (1.3 cu mi) of magma. The eruption was one of the largest of the 20th century, only slightly less in magnitude to that of  NObaruptia in 1912 and Mount Pinatubo in 1991. The eruption had a VEI of 6, thus being 'Colossal'.
The pumice formed in the climactic eruption fell over an area of about 273,000 square kilometres (105,000 sq mi), and volcanic ash as far away as San Francisco, 4,000 kilometres (2,500 mi) away. The eruption tore away much of the south-western flank of the volcano, leaving a crater about 1 kilometre (0.6 mi) in diameter and about 300 metres (980 ft) deep, stretching from just below the summit to an elevation of about 2,300 metres (7,500 ft). The first evidence of the eruption was a sprinkling of sand on Quezaltenango. The wind then changed from the south to the east and ashes began to fall at Helvetia, a coffee plantation six miles to the South-West. Because of the lack of recorded eruptive activity at Santa María, local people did not recognise the preceding seismicity as warning signs of an eruption. At least 5,000 people died as a result of the eruption itself, and a subsequent outbreak of malaria killed many more.

The photographer
Tempest Anderson  was an ophthalmic surgeon at York County Hospital in the United Kingdom, and an expert amateur photographer and vulcanologist. He was a member of the Royal Society Commission which was appointed to investigate the aftermath of the eruptions of Soufriere volcano, St Vincent and Mont Pelee, Martinique, West Indies which both erupted in May 1902. Some of his photographs of these eruptions were subsequently published in his book, Volcanic Studies in Many Lands.
Tempest Anderson spent nine months in Mexico, Guatemala and the West Indies in 1906/1907. He travelled to Mexico to attend the 10th Congres Geologique International before sailing by mail steamer to Guatemala to study the effects of the 1902 earthquake. During the trip he observed and photographed Cerro Quemado, Santa Maria, and Atitlan. During this trip he collected first hand accounts of the 1902 eruption of the Santa Maria and the immediate aftermath. Captain Saunders of the Pacific Mail Steamer S.S. Newport observed the eruption cloud which rose to a great height. The Captain measured it using a sextant and recorded it as reaching 17 to 18 miles. The sounds accompanying the eruption were loud and were heard even louder at more distant places than close to the mountain. The eruption was heard as far away as Guatemala City, the noises so strong, they were assumed to come from neighbouring volcanoes.

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