KILAUEA BY EDUARDO LEFEBVRE SCOVELL

EDUARDO  LEVEBRE SCOVELL (1864-1918)

 Kilauea  (1,247 m - 4,091 ft) 

 United States of America  (Hawaii)




1. Kilauea caldera in 1908, oil on canvas, Bernice P. Bishop Museum, Honolulu. 

2. Kilauea in 1890, oil on canvas,  Bernice P. Bishop Museum, Honolulu.

The mountain 

Kīlauea (1,247 m-4,091 ft) is a currently active shield volcano in the Hawaiian Islands, and the most active of the five volcanoes that together form the island of Hawaiʻi. Located along the southern shore of the island, the volcano is between 300,000 and 600,000 years old and emerged above sea level about 100,000 years ago. It is the second youngest product of the Hawaiian hotspot and the current eruptive center of the Hawaiian–Emperor seamount chain. Structurally, Kīlauea has a large, fairly recently formed caldera at its summit and two active rift zones, one extending 125 km (78 mi) east and the other 35 km (22 mi) west, as an active fault of unknown depth moving vertically an average of 2 to 20 mm (0.1 to 0.8 in) per year.

Kīlauea's eruptive history has been a long and active one; its name means "spewing" or "much spreading" in the Hawaiian language, referring to its frequent outpouring of lava. The earliest lavas from the volcano date back to its submarine preshield stage, samples having been recovered by remotely operated underwater vehicles from its submerged slopes; samples of other flows have been recovered as core samples. Lavas younger than 1,000 years cover 90 percent of the volcano's surface. The oldest exposed lavas date back 2,800 years. The first well-documented eruption of Kīlauea occurred in 1823 (Western contact and written history began in 1778), and since that time the volcano has erupted repeatedly. Most historical eruptions have occurred at the volcano's summit or its eastern rift zone, and are prolonged and effusive in character. The geological record shows, however, that violent explosive activity predating European contact was extremely common, and in 1790 one such eruption killed over 80 warriors; should explosive activity start anew the volcano would become much more of a danger to humans. Kīlauea's current eruption dates back to January 3, 1983, and is by far its longest-duration historical period of activity, as well as one of the longest-duration eruptions in the world; as of January 2011, the eruption has produced 3.5 km3 (1 cu mi) of lava and resurfaced 123.2 km2 (48 sq mi) of land.

Kīlauea's high state of activity has a major impact on its mountainside ecology where plant growth is often interrupted by fresh tephra and drifting volcanic sulfur dioxide, producing acid rains particularly in a barren area south of its southwestern rift zone known as the Kaʻū Desert. Nonetheless, wildlife flourishes where left undisturbed elsewhere on the volcano and is highly endemic thanks to Kīlauea's (and the island of Hawaiʻi's) isolation from the nearest landmass. Historically, the five volcanoes on the island were considered sacred by the Hawaiian people, and in Hawaiian mythology Kīlauea's Halemaumau Crater served as the body and home of Pele, goddess of fire, lightning, wind, and volcanoes. William Ellis, a missionary from England, gave the first modern account of Kīlauea and spent two weeks traveling along the volcano; since its foundation by Thomas Jaggar in 1912, the Hawaiian Volcano Observatory, located on the rim of Kilauea caldera, has served as the principal investigative and scientific body on the volcano and the island in general. In 1916 a bill forming the Hawaii Volcanoes National Park was signed into law by President Woodrow Wilson; since then the park has become a World Heritage Site and a major tourist destination, attracting roughly 2.6 million people annually.

In 2018, Kilauea enters in a new important phase of eruptions.

The painter 

Eduardo Lefebvre Scovell  was a British artist, one of the so called Volcano School, a group of non-native artists who painted dramatic nocturnal scenes of Hawaii's erupting volcanoes. Following his education at Eton College and the University of Cambridge, Scovell studied art in Paris. He then traveled extensively, including one year in Rome and Florence. Several years were spent in India, China and Japan. He visited Brazil and spent eight years in Hawaii where he specialized in volcano scenes. He was in San Francisco during the earthquake and fire of 1906 and then settled in Los Angeles. Scovell was a resident there until his death on 23 September 1918.
Scovell's paintings Kilauea several times between 1890 and 1908 (see above) ;  those paintings are in the Bernice P. Bishop Museum in Honolulu.

KILAUEA PAINTED BY JULES TAVERNIER

JULES TAVERNIER (1844-1889)

  Kilauea  (1,247 m - 4,091 ft) 

 United states of America  (Hawaii)

1. Kilauea Caldera,  San Diego Museum of Art

2. Kilauea Volcano at Night (1885-86), Honolulu Museum of Art

3. Kilauea at night (1880) Honolulu Museum of Art

The mountain 

Kīlauea (1,247 m-4,091 ft) is a currently active shield volcano in the Hawaiian Islands, and the most active of the five volcanoes that together form the island of Hawaiʻi. Located along the southern shore of the island, the volcano is between 300,000 and 600,000 years old and emerged above sea level about 100,000 years ago. It is the second youngest product of the Hawaiian hotspot and the current eruptive center of the Hawaiian–Emperor seamount chain. Because it lacks topographic prominence and its activities historically coincided with those of Mauna Loa, Kīlauea was once thought to be a satellite of its much larger neighbor. Structurally, Kīlauea has a large, fairly recently formed caldera at its summit and two active rift zones, one extending 125 km (78 mi) east and the other 35 km (22 mi) west, as an active fault of unknown depth moving vertically an average of 2 to 20 mm (0.1 to 0.8 in) per year.
Kīlauea's eruptive history has been a long and active one; its name means "spewing" or "much spreading" in the Hawaiian language, referring to its frequent outpouring of lava. The earliest lavas from the volcano date back to its submarine preshield stage, samples having been recovered by remotely operated underwater vehicles from its submerged slopes; samples of other flows have been recovered as core samples. Lavas younger than 1,000 years cover 90 percent of the volcano's surface. The oldest exposed lavas date back 2,800 years. The first well-documented eruption of Kīlauea occurred in 1823 (Western contact and written history began in 1778), and since that time the volcano has erupted repeatedly. Most historical eruptions have occurred at the volcano's summit or its eastern rift zone, and are prolonged and effusive in character. The geological record shows, however, that violent explosive activity predating European contact was extremely common, and in 1790 one such eruption killed over 80 warriors; should explosive activity start anew the volcano would become much more of a danger to humans. Kīlauea's current eruption dates back to January 3, 1983, and is by far its longest-duration historical period of activity, as well as one of the longest-duration eruptions in the world; as of January 2011, the eruption has produced 3.5 km3 (1 cu mi) of lava and resurfaced 123.2 km2 (48 sq mi) of land.
Kīlauea's high state of activity has a major impact on its mountainside ecology where plant growth is often interrupted by fresh tephra and drifting volcanic sulfur dioxide, producing acid rains particularly in a barren area south of its southwestern rift zone known as the Kaʻū Desert. Nonetheless, wildlife flourishes where left undisturbed elsewhere on the volcano and is highly endemic thanks to Kīlauea's (and the island of Hawaiʻi's) isolation from the nearest landmass. Historically, the five volcanoes on the island were considered sacred by the Hawaiian people, and in Hawaiian mythology Kīlauea's Halemaumau Crater served as the body and home of Pele, goddess of fire, lightning, wind, and volcanoes. William Ellis, a missionary from England, gave the first modern account of Kīlauea and spent two weeks traveling along the volcano; since its foundation by Thomas Jaggar in 1912, the Hawaiian Volcano Observatory, located on the rim of Kilauea caldera, has served as the principal investigative and scientific body on the volcano and the island in general. In 1916 a bill forming the Hawaii Volcanoes National Park was signed into law by President Woodrow Wilson; since then the park has become a World Heritage Site and a major tourist destination, attracting roughly 2.6 million people annually.

The painter 
Jules Tavernier was a French painter, illustrator, and an important member of Hawaii’s Volcano School.  He studied with the French painter, Félix Joseph Barrias (1822–1907). he left France in the 1870s and never  return. Tavernier was employed as an illustrator by Harper's Magazine, which sent him, along with Paul Frenzeny, on a year-long coast-to-coast sketching tour in 1873.
 Eventually, he continued westward to Hawaii, where he became quite famous as a landscape painter. He was fascinated by Hawaii’s erupting volcanoes—a subject that pre-occupied him for the rest of his life, which was spent in Hawaii, Canada and the western United States. Tavernier died on 18 May 1889 in Honolulu, Hawaii. He painted several version of the Kilauea erupting between 1880 and the end of his life.
Among the public collections holding paintings by Jules Tavernier are the Brigham Young University Museum of Art (Provo, UT), the Colorado Springs Fine Arts Center (Colorado Springs, CO), the Crocker Art Museum (Sacramento), the Gilcrease Museum (Tulsa, OK), Hearst Art Gallery (Saint Mary's College of California, Moraga, CA), the Honolulu Museum of Art, the Museum of Nebraska Art (Kearney, NE), the Oakland Museum of California, the San Diego Museum of Art, the Stark Museum of Art (Orange, TX), the Society of California Pioneers (San Francisco, CA), the Washington County Museum of Fine Arts (Hagerstown, MD) and the Yosemite Museum (Yosemite National Park).

After his death his art lived on in the hearts and homes of Hawaiians, and many more artists picked up on the volcano landscape theme he started. His Western art was mostly forgotten. Fifty years after his death the Honolulu Advertiser remembered Jules Tavernier in December 1940 with the comment: “...to the generation which knew King Kalakaua, Tavernier recalls to mind some of the greatest paintings ever made of Hawaii volcanoes.” At the beginning of the twenty-first century interest has reawakened in Tavernier's Western landscape art; museums are purchasing his pictures and prices for his oil paintings are increasing. His students included D. Howard Hitchcock (1861–1943), Amédée Joullin (1862–1917), Charles Rollo Peters (1862–1917) and Manuel Valencia (1856–1935).

KILAUEA PAINTED BY AMBROSE PATTERSON

AMBROSE MC CARTHY PATTERSON (1877-1966) 

Mount Kilauea  (1,247 m - 4,091 ft) 

United States of America (Hawaï)  

In Mount Kilauea,  the house of Everlasting Fire, 1917 oil on canvas, Honolulu Museum of Art  

The mountain 
Kilauea (1,247 m - 4,091 ft) is a currently active shield volcano in the Hawaiian Islands, and the most active of the five volcanoes that together form the island of Hawaiʻi. Located along the southern shore of the island, the volcano is between 300,000 and 600,000 years old and emerged above sea level about 100,000 years ago. It is the second youngest product of the Hawaiian hotspot and the current eruptive center of the Hawaiian–Emperor seamount chain. Because it lacks topographic prominence and its activities historically coincided with those of Mauna Loa, Kīlauea was once thought to be a satellite of its much larger neighbor. Structurally, Kīlauea has a large, fairly recently formed caldera at its summit and two active rift zones, one extending 125 km (78 mi) east and the other 35 km (22 mi) west, as an active fault of unknown depth moving vertically an average of 2 to 20 mm (0.1 to 0.8 in) per year.
Kīlauea's eruptive history has been a long and active one; its name means "spewing" or "much spreading" in the Hawaiian language, referring to its frequent outpouring of lava. The earliest lavas from the volcano date back to its submarine preshield stage, samples having been recovered by remotely operated underwater vehicles from its submerged slopes; samples of other flows have been recovered as core samples. Lavas younger than 1,000 years cover 90 percent of the volcano's surface. The oldest exposed lavas date back 2,800 years. The first well-documented eruption of Kīlauea occurred in 1823 (Western contact and written history began in 1778), and since that time the volcano has erupted repeatedly. Most historical eruptions have occurred at the volcano's summit or its eastern rift zone, and are prolonged and effusive in character. The geological record shows, however, that violent explosive activity predating European contact was extremely common, and in 1790 one such eruption killed over 80 warriors; should explosive activity start anew the volcano would become much more of a danger to humans. Kīlauea's current eruption dates back to January 3, 1983, and is by far its longest-duration historical period of activity, as well as one of the longest-duration eruptions in the world; as of January 2011, the eruption has produced 3.5 km3 (1 cu mi) of lava and resurfaced 123.2 km2 (48 sq mi) of land.
Kīlauea's high state of activity has a major impact on its mountainside ecology where plant growth is often interrupted by fresh tephra and drifting volcanic sulfur dioxide, producing acid rains particularly in a barren area south of its southwestern rift zone known as the Kaʻū Desert. Nonetheless, wildlife flourishes where left undisturbed elsewhere on the volcano and is highly endemic thanks to Kīlauea's (and the island of Hawaiʻi's) isolation from the nearest landmass. Historically, the five volcanoes on the island were considered sacred by the Hawaiian people, and in Hawaiian mythology Kīlauea's Halemaumau Crater served as the body and home of Pele, goddess of fire, lightning, wind, and volcanoes. William Ellis, a missionary from England, gave the first modern account of Kīlauea and spent two weeks traveling along the volcano; since its foundation by Thomas Jaggar in 1912, the Hawaiian Volcano Observatory, located on the rim of Kilauea caldera, has served as the principal investigative and scientific body on the volcano and the island in general. In 1916 a bill forming the Hawaii Volcanoes National Park was signed into law by President Woodrow Wilson; since then the park has become a World Heritage Site and a major tourist destination, attracting roughly 2.6 million people annually.

The painter 
Ambrose McCarthy Patterson  was a painter and printmaker, born in Daylesford, Victoria (Australia). He studied at the Melbourne Art School under E. Phillips Fox and Tudor St George Tucker, at the National Gallery Art School in Melbourne and continued his studies in Paris at the Académie Colarossi and the Académie Julian under Lucien Simon, André Lhote and Maxime Maufra. In Paris he became a friend of compatriot Nellie Melba, the famous soprano; Patterson's brother, Tom, was married to Melba's sister, Belle. Through Melba's influence, he was able to continue his studies with John Singer Sargent. He became part of the Paris arts scene and exhibited at the first Salon d'Automne exhibitions. He had five paintings at the 1905 Paris Salon at which Henri Matisse and the fauves stunned the art world.
He arrived in Hawaii in 1916 on a stopover from Sidney to New York, and decided to stay with a Parisian friend living in Honolulu. During the next 18 months, Patterson made block prints and paintings with particular interest in Kilauea. His art was included in the Hawaiian Society of Artists Annual in 1917. He left for California in 1918 and settled in Seattle. At the 1918 Spring Annual of the San Francisco Art Association (SFAA) his wood block prints were said to be "especially fine in color." That summer his art was given a one-man exhibition at the SFAA galleries and he contributed three color prints (The Steeple Chase, The Bull Fight, and The Long Beach) to the Seventh Annual of the California Society of Etchers.
By September 1918 Patterson had moved to Seattle to work as a freelance artist, perhaps being the first modern artist in that city, and that fall his art was given a solo show at the Seattle Fine Arts Society, the first of many exhibitions in Washington State. In 1919 he established the University of Washington School of Painting and Design. Patterson married painter and former student Viola Hansen in 1922, and the two became major figures of the arts in the Pacific Northwest region. Patterson taught until his retirement in 1947. He died in Seattle in 1966 leaving behind an impressive record of awards received and exhibitions across the United States, including the: Art Institute of Chicago, Museum of Modern Art in New York City, National Gallery of Art in Washington, D.C., and the World’s Fairs in San Francisco and New York City.
The Art Gallery of New South Wales (Sydney, Australia), the Honolulu Museum of Art, the National Portrait Gallery (Australia) (Canberra), the Philadelphia Museum of Art, the Seattle Art Museum and the Tacoma Art Museum are among the public collections holding works by Ambrose McCarthy Patterson.

KILAUEA VOLCANO PAINTED BY CHARLES FURNEAUX

CHARLES FURNEAUX (1835-1913)
Kilauea (1,247 m - 4,091 ft) 
United States of America (Hawaii)

 

The mountain 

Kīlauea (1,247 m-4,091 ft) is a currently active shield volcano in the Hawaiian Islands, and the most active of the five volcanoes that together form the island of Hawaiʻi. Located along the southern shore of the island, the volcano is between 300,000 and 600,000 years old and emerged above sea level about 100,000 years ago. It is the second youngest product of the Hawaiian hotspot and the current eruptive center of the Hawaiian–Emperor seamount chain. Structurally, Kīlauea has a large, fairly recently formed caldera at its summit and two active rift zones, one extending 125 km (78 mi) east and the other 35 km (22 mi) west, as an active fault of unknown depth moving vertically an average of 2 to 20 mm (0.1 to 0.8 in) per year.

Kīlauea's eruptive history has been a long and active one; its name means "spewing" or "much spreading" in the Hawaiian language, referring to its frequent outpouring of lava. The earliest lavas from the volcano date back to its submarine preshield stage, samples having been recovered by remotely operated underwater vehicles from its submerged slopes; samples of other flows have been recovered as core samples. Lavas younger than 1,000 years cover 90 percent of the volcano's surface. The oldest exposed lavas date back 2,800 years. The first well-documented eruption of Kīlauea occurred in 1823 (Western contact and written history began in 1778), and since that time the volcano has erupted repeatedly. Most historical eruptions have occurred at the volcano's summit or its eastern rift zone, and are prolonged and effusive in character. The geological record shows, however, that violent explosive activity predating European contact was extremely common, and in 1790 one such eruption killed over 80 warriors; should explosive activity start anew the volcano would become much more of a danger to humans. Kīlauea's current eruption dates back to January 3, 1983, and is by far its longest-duration historical period of activity, as well as one of the longest-duration eruptions in the world; as of January 2011, the eruption has produced 3.5 km3 (1 cu mi) of lava and resurfaced 123.2 km2 (48 sq mi) of land.

In 2018, Kilauea enters in a new important phase of eruptions.

 

The painter 
Charles Furneaux was born in Boston and became a drawing instructor in that area. For many years he lived in the town of Melrose, Massachusetts. In 1880, Furneaux moved to Hawaii, where he cultivated the friendship of King Kalakaua and other members of the Hawaiian royal family, from whom he later received several commissions. In the late 1880s, he was commissioned in Honolulu by Alexander Joy Cartwright, widely credited as the "father of baseball" and another dear friend of King Kalakaua, to paint the only oil portrait of his 72-year life. While living in Honolulu he taught at the private schools Punahou and St. Albans (now known as Iolani School). In 1885, he received the order of Chevalier of Kapiolani from King Kalakaua in 'recognition of his services in advancing Hawaiian art'. He died in Hawaii in 1913.
His reputation is mainly based on the paintings he executed in Hawaii, especially those of erupting volcanoes. The Bishop Museum (Honolulu), the Brooklyn Museum, the Honolulu Museum of Art, Iolani Palace (Honolulu) and Mount Holyoke College Art Museum (South Hadley, Massachusetts) are among the public collections holding works by Charles Furneaux.

 

___________________________________
2022 - Wandering Vertexes
A blog by Francis Rousseau
 

KILAUEA BY CONSTANCE GORDON-CUMMING

 

CONSTANCE GORDON-CUMMING (1837–1924)

 Kilauea  (1,247 m - 4,091 ft) 

 United States of America  (Hawaii)

 In Kilauea Temporary Chimneys and Fire Fountains, watercolor, c.1880

The volcano

Kīlauea (1,247 m-4,091 ft) is a currently active shield volcano in the Hawaiian Islands, and the most active of the five volcanoes that together form the island of Hawaiʻi. Located along the southern shore of the island, the volcano is between 300,000 and 600,000 years old and emerged above sea level about 100,000 years ago. It is the second youngest product of the Hawaiian hotspot and the current eruptive center of the Hawaiian–Emperor seamount chain. Structurally, Kīlauea has a large, fairly recently formed caldera at its summit and two active rift zones, one extending 125 km (78 mi) east and the other 35 km (22 mi) west, as an active fault of unknown depth moving vertically an average of 2 to 20 mm (0.1 to 0.8 in) per year.

More about Kilauea

The painter
Constance Frederica “Eka” Gordon-Cumming was a noted Scottish travel writer and painter. Born in a wealthy family, she travelled around the world and painted described scenes and life as she saw them. Constance Gordon-Cumming was a prolific landscape painter, mostly in Asia and the Pacific. She painted over a thousand watercolors and worked with a motto to ‘never a day without at least one careful-coloured sketch’ starting her day at 5 am while in India. Places she visited include Australia, New Zealand, America, China, and Japan.
She arrived in Hilo, Hawaii in October 1879, and was among the first artists to paint the active volcanoes. Her Hawaii travelogue, Fire Fountains: The Kingdom of Hawaii, was published in Edinburgh in 1883. She had several dangerous moments but her travel ended in 1880 when the Montana that she was on ran into rocks at Holyhead. While most of the passengers took the lifeboat, she stayed on last along with the captain to save her paintings and was rescued many hours later. She returned to live at Crieff with her widowed sister Eleanor and continued to write books.
Her best known books are At Home in Fiji and A Lady's Cruise on a French Man-of-War. The latter book resulted from an invitation to join a French ship put into service for the Bishop of Samoa so that he could visit remote parts of his far-flung diocese.
Miss Gordon-Cumming received much criticism from male writers of the era, perhaps because she did not fit in the traditional Victorian role of women, as she often traveled alone and unaided.
In any case, her landscape drawings and watercolors seem to be universally admired.

_________________________________________
2019 - Wandering Vertexes...
by Francis Rousseau

MAUNA LOA PAINTED BY JULES TAVERNIER

JULES TAVERNIER (1844-1889) 

Mauna Loa volcano  (4,170m - 13, 680 ft)

 United States of America  (Hawai'i)

 In  Mokuaweoweo at the top of Mauna Loa, oil on canvas, Honolulu Museum of Arts  

The volcano 

Mauna Loa  (4,170m - 13, 680ft)  which means Long Mountain in Hawaiian, is one of five volcanoes that form the Island of Hawaii in the U.S. state of Hawaiʻi in the Pacific Ocean. The largest subaerial volcano in both mass and volume, Mauna Loa has historically been considered the largest volcano on Earth. It is an active shield volcano with relatively gentle slopes, with a volume estimated at approximately 18,000 cubic miles (75,000 km3), although its peak is about 120 feet (37 m) lower than that of its neighbor, Mauna Kea. Lava eruptions from Mauna Loa are silica-poor and very fluid, and they tend to be non-explosive.

Mauna Loa has probably been erupting for at least 700,000 years, and may have emerged above sea level about 400,000 years ago. The oldest-known dated rocks are not older than 200,000 years. The volcano's magma comes from the Hawaii hotspot, which has been responsible for the creation of the Hawaiian island chain over tens of millions of years. The slow drift of the Pacific Plate will eventually carry Mauna Loa away from the hotspot within 500,000 to one million years from now, at which point it will become extinct.

Mauna Loa's most recent eruption occurred from March 24 to April 15, 1984. No recent eruptions of the volcano have caused fatalities, but eruptions in 1926 and 1950 destroyed villages, and the city of Hilo is partly built on lava flows from the late 19th century. Because of the potential hazards it poses to population centers, Mauna Loa is part of the Decade Volcanoes program, which encourages studies of the world's most dangerous volcanoes. Mauna Loa has been monitored intensively by the Hawaiian Volcano Observatory since 1912. Observations of the atmosphere are undertaken at the Mauna Loa Observatory, and of the Sun at the Mauna Loa Solar Observatory, both located near the mountain's summit. Hawaii Volcanoes National Park covers the summit and the southeastern flank of the volcano, and also incorporates Kilauea, a separate volcano.

Source: 

- Hawaii Center for Volcanology

The painter 
Jules Tavernier was a French painter, illustrator, and an important member of Hawaii’s Volcano School.  He studied with the French painter, Félix Joseph Barrias (1822–1907). he left France in the 1870s and never  return. Tavernier was employed as an illustrator by Harper's Magazine, which sent him, along with Paul Frenzeny, on a year-long coast-to-coast sketching tour in 1873.
 Eventually, he continued westward to Hawaii, where he became quite famous as a landscape painter. He was fascinated by Hawaii’s erupting volcanoes—a subject that pre-occupied him for the rest of his life, which was spent in Hawaii, Canada and the western United States. Tavernier died on 18 May 1889 in Honolulu, Hawaii. He painted several version of the Kilauea erupting between 1880 and the end of his life.
Among the public collections holding paintings by Jules Tavernier are the Brigham Young University Museum of Art (Provo, UT), the Colorado Springs Fine Arts Center (Colorado Springs, CO), the Crocker Art Museum (Sacramento), the Gilcrease Museum (Tulsa, OK), Hearst Art Gallery (Saint Mary's College of California, Moraga, CA), the Honolulu Museum of Art, the Museum of Nebraska Art (Kearney, NE), the Oakland Museum of California, the San Diego Museum of Art, the Stark Museum of Art (Orange, TX), the Society of California Pioneers (San Francisco, CA), the Washington County Museum of Fine Arts (Hagerstown, MD) and the Yosemite Museum (Yosemite National Park).
After his death his art lived on in the hearts and homes of Hawaiians, and many more artists picked up on the volcano landscape theme he started. His Western art was mostly forgotten.
Fifty years after his death the Honolulu Advertiser remembered Jules Tavernier in December 1940 with the comment: “...to the generation which knew King Kalakaua, Tavernier recalls to mind some of the greatest paintings ever made of Hawaii volcanoes.”
At the beginning of the twenty-first century interest has reawakened in Tavernier's Western landscape art; museums are purchasing his pictures and prices for his oil paintings are increasing.
His students included D. Howard Hitchcock (1861–1943), Amédée Joullin (1862–1917), Charles Rollo Peters (1862–1917) and Manuel Valencia (1856–1935).
Source:
- Tigertail Virtual Museum 

MAUNA LOA PAINTED BY JULES TAVERNIER

JULES TAVERNIER (1844-1889) 

Mauna Loa volcano  (4,170m - 13, 680 ft)

 United States of America  (Hawai'i)

 In Wailuku Falls, Hilo, Snow on the Mauna Loa, c. 1886,  oil on canvas 
Honolulu Museum of Arts  

The volcano 

Mauna Loa  (4,170m - 13, 680ft)  which means Long Mountain in Hawaiian, is one of five volcanoes that form the Island of Hawaii in the U.S. state of Hawaiʻi in the Pacific Ocean. The largest subaerial volcano in both mass and volume, Mauna Loa has historically been considered the largest volcano on Earth. It is an active shield volcano with relatively gentle slopes, with a volume estimated at approximately 18,000 cubic miles (75,000 km3), although its peak is about 120 feet (37 m) lower than that of its neighbor, Mauna Kea. Lava eruptions from Mauna Loa are silica-poor and very fluid, and they tend to be non-explosive.

Mauna Loa has probably been erupting for at least 700,000 years, and may have emerged above sea level about 400,000 years ago. The oldest-known dated rocks are not older than 200,000 years. The volcano's magma comes from the Hawaii hotspot, which has been responsible for the creation of the Hawaiian island chain over tens of millions of years. The slow drift of the Pacific Plate will eventually carry Mauna Loa away from the hotspot within 500,000 to one million years from now, at which point it will become extinct.

Mauna Loa's most recent eruption occurred from March 24 to April 15, 1984. No recent eruptions of the volcano have caused fatalities, but eruptions in 1926 and 1950 destroyed villages, and the city of Hilo is partly built on lava flows from the late 19th century. Because of the potential hazards it poses to population centers, Mauna Loa is part of the Decade Volcanoes program, which encourages studies of the world's most dangerous volcanoes. Mauna Loa has been monitored intensively by the Hawaiian Volcano Observatory since 1912. Observations of the atmosphere are undertaken at the Mauna Loa Observatory, and of the Sun at the Mauna Loa Solar Observatory, both located near the mountain's summit. Hawaii Volcanoes National Park covers the summit and the southeastern flank of the volcano, and also incorporates Kilauea, a separate volcano.

The painter 
Jules Tavernier was a French painter, illustrator, and an important member of Hawaii’s Volcano School.  He studied with the French painter, Félix Joseph Barrias (1822–1907). he left France in the 1870s and never  return. Tavernier was employed as an illustrator by Harper's Magazine, which sent him, along with Paul Frenzeny, on a year-long coast-to-coast sketching tour in 1873.
 Eventually, he continued westward to Hawaii, where he became quite famous as a landscape painter. He was fascinated by Hawaii’s erupting volcanoes—a subject that pre-occupied him for the rest of his life, which was spent in Hawaii, Canada and the western United States. Tavernier died on 18 May 1889 in Honolulu, Hawaii. He painted several version of the Kilauea erupting between 1880 and the end of his life.
Among the public collections holding paintings by Jules Tavernier are the Brigham Young University Museum of Art (Provo, UT), the Colorado Springs Fine Arts Center (Colorado Springs, CO), the Crocker Art Museum (Sacramento), the Gilcrease Museum (Tulsa, OK), Hearst Art Gallery (Saint Mary's College of California, Moraga, CA), the Honolulu Museum of Art, the Museum of Nebraska Art (Kearney, NE), the Oakland Museum of California, the San Diego Museum of Art, the Stark Museum of Art (Orange, TX), the Society of California Pioneers (San Francisco, CA), the Washington County Museum of Fine Arts (Hagerstown, MD) and the Yosemite Museum (Yosemite National Park).
After his death his art lived on in the hearts and homes of Hawaiians, and many more artists picked up on the volcano landscape theme he started. His Western art was mostly forgotten.
Fifty years after his death the Honolulu Advertiser remembered Jules Tavernier in December 1940 with the comment: “...to the generation which knew King Kalakaua, Tavernier recalls to mind some of the greatest paintings ever made of Hawaii volcanoes.”
At the beginning of the twenty-first century interest has reawakened in Tavernier's Western landscape art; museums are purchasing his pictures and prices for his oil paintings are increasing.
His students included D. Howard Hitchcock (1861–1943), Amédée Joullin (1862–1917), Charles Rollo Peters (1862–1917) and Manuel Valencia (1856–1935).

EL CAPITAN PAINTED BY JULES TAVERNIER

JULES TAVERNIER (1844-1889) 

El Capitan (2,309m - 7,573 ft) 

United States of America 

The mountain 

El Capitan 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.

The top of El Capitan can be reached by hiking out of Yosemite Valley on the trail next to Yosemite Falls, then proceeding west. For climbers, the challenge is to climb up the sheer granite face. There are many named climbing routes, all of them arduous, including Iron Hawk and Sea of Dreams, for example.

Climbing

The Nose was first climbed in 1958 by Warren Harding, Wayne Merry and George Whitmore in 47 days using "siege" tactics: climbing in an expedition style using fixed ropes along the length of the route, linking established camps along the way. 

The second ascent of The Nose was in 1960 by Royal Robbins, Joe Fitschen, Chuck Pratt and Tom Frost, who took seven days in the first continuous climb of the route without siege tactics. 

The first solo climb of The Nose was done by Tom Bauman in 1969. 

The first ascent of The Nose in one day was accomplished in 1975 by John Long, Jim Bridwell and Billy Westbay. Today, The Nose typically takes fit climbers 4–5 days of full climbing, and has a success rate of around 60%.

Beverly Johnson was the first woman to successfully ascend El Capitan, via the Nose route, with Dan Asay in June 1973. In September 1973, Beverly Johnson and Sibylle Hechtel were the first team of women to ascend El Capitan via the Triple Direct route, which takes the first ten pitches of the Salathe Wall, then continues up the middle portion of El Capitan via the Muir Wall, and finishes on the upper pitches of the Nose route.  In 1977, Molly Higgins and Barb Eastman climbed the Nose, to become the second party of women to climb El Capitan and the first to climb it via the Nose. In 1978, Bev Johnson was the first woman to solo El Capitan by climbing the Dihedral Wall.  Hazel Findlay has made three free ascents of El Capitan, including the first female ascent of Golden Gate in 2011, the first female ascent of Pre-Muir Wall in 2012, and a three-day ascent of Freerider in 2013.

Reference:

- El Capitan in web Stanford edu page 
- El Capitan in Wikipedia page 

The painter 
Jules Tavernier was a French painter, illustrator, and an important member of Hawaii’s Volcano School.  He studied with the French painter, Félix Joseph Barrias (1822–1907). he left France in the 1870s and never  return. Tavernier was employed as an illustrator by Harper's Magazine, which sent him, along with Paul Frenzeny, on a year-long coast-to-coast sketching tour in 1873.
 Eventually, he continued westward to Hawaii, where he became quite famous as a landscape painter. He was fascinated by Hawaii’s erupting volcanoes—a subject that pre-occupied him for the rest of his life, which was spent in Hawaii, Canada and the western United States. Tavernier died on 18 May 1889 in Honolulu, Hawaii. He painted several version of the Kilauea erupting between 1880 and the end of his life.
Among the public collections holding paintings by Jules Tavernier are the Brigham Young University Museum of Art (Provo, UT), the Colorado Springs Fine Arts Center (Colorado Springs, CO), the Crocker Art Museum (Sacramento), the Gilcrease Museum (Tulsa, OK), Hearst Art Gallery (Saint Mary's College of California, Moraga, CA), the Honolulu Museum of Art, the Museum of Nebraska Art (Kearney, NE), the Oakland Museum of California, the San Diego Museum of Art, the Stark Museum of Art (Orange, TX), the Society of California Pioneers (San Francisco, CA), the Washington County Museum of Fine Arts (Hagerstown, MD) and the Yosemite Museum (Yosemite National Park).

After his death his art lived on in the hearts and homes of Hawaiians, and many more artists picked up on the volcano landscape theme he started. His Western art was mostly forgotten. Fifty years after his death the Honolulu Advertiser remembered Jules Tavernier in December 1940 with the comment: “...to the generation which knew King Kalakaua, Tavernier recalls to mind some of the greatest paintings ever made of Hawaii volcanoes.” At the beginning of the twenty-first century interest has reawakened in Tavernier's Western landscape art; museums are purchasing his pictures and prices for his oil paintings are increasing. His students included D. Howard Hitchcock (1861–1943), Amédée Joullin (1862–1917), Charles Rollo Peters (1862–1917) and Manuel Valencia (1856–1935). Reference   - Biography of  Jules Tavernier in Tigertail Virtual Museum

MAUNA LOA PAINTED BY CHARLES FURNEAUX

CHARLES FURNEAUX (1835-1913)

Mauna Loa volcano  (4,170m - 13, 680 ft)

 United States of America  (Hawai'i)

In Eruption of Mauna Loa in 1889, oil on canvas, Bernice Pauahi Bishop Museum Honolulu 

The volcano 

Mauna Loa  (4,170m - 13, 680ft)  which means Long Mountain in Hawaiian, is one of five volcanoes that form the Island of Hawaii in the U.S. state of Hawaiʻi in the Pacific Ocean. The largest subaerial volcano in both mass and volume, Mauna Loa has historically been considered the largest volcano on Earth. It is an active shield volcano with relatively gentle slopes, with a volume estimated at approximately 18,000 cubic miles (75,000 km3), although its peak is about 120 feet (37 m) lower than that of its neighbor, Mauna Kea. Lava eruptions from Mauna Loa are silica-poor and very fluid, and they tend to be non-explosive.

Mauna Loa has probably been erupting for at least 700,000 years, and may have emerged above sea level about 400,000 years ago. The oldest-known dated rocks are not older than 200,000 years. The volcano's magma comes from the Hawaii hotspot, which has been responsible for the creation of the Hawaiian island chain over tens of millions of years. The slow drift of the Pacific Plate will eventually carry Mauna Loa away from the hotspot within 500,000 to one million years from now, at which point it will become extinct.

Mauna Loa's most recent eruption occurred from March 24 to April 15, 1984. No recent eruptions of the volcano have caused fatalities, but eruptions in 1926 and 1950 destroyed villages, and the city of Hilo is partly built on lava flows from the late 19th century. Because of the potential hazards it poses to population centers, Mauna Loa is part of the Decade Volcanoes program, which encourages studies of the world's most dangerous volcanoes. Mauna Loa has been monitored intensively by the Hawaiian Volcano Observatory since 1912. Observations of the atmosphere are undertaken at the Mauna Loa Observatory, and of the Sun at the Mauna Loa Solar Observatory, both located near the mountain's summit. Hawaii Volcanoes National Park covers the summit and the southeastern flank of the volcano, and also incorporates Kilauea, a separate volcano.

The painter 
Charles Furneaux was born in Boston and became a drawing instructor in that area. For many years he lived in the town of Melrose, Massachusetts. In 1880, Furneaux moved to Hawaii, where he cultivated the friendship of King Kalakaua and other members of the Hawaiian royal family, from whom he later received several commissions. In the late 1880s, he was commissioned in Honolulu by Alexander Joy Cartwright, widely credited as the "father of baseball" and another dear friend of King Kalakaua, to paint the only oil portrait of his 72-year life. While living in Honolulu he taught at the private schools Punahou and St. Albans (now known as Iolani School). In 1885, he received the order of Chevalier of Kapiolani from King Kalakaua in 'recognition of his services in advancing Hawaiian art'. He died in Hawaii in 1913.
His reputation is mainly based on the paintings he executed in Hawaii, especially those of erupting volcanoes. The Bishop Museum (Honolulu), the Brooklyn Museum, the Honolulu Museum of Art, Iolani Palace (Honolulu) and Mount Holyoke College Art Museum (South Hadley, Massachusetts) are among the public collections holding works by Charles Furneaux.

HALEMA'UMA 'U CRATER PAINTED BY DAVID HOWARD HITCHCOCK

 

DAVID HOWARD HITCHCOCK (1861-1943),

Halemaʻumaʻu Crater / Kilauea (1,247 m - 4,091 ft) 

United states of America (Hawaii) 

In Halemaumau, lake of fire, oil on board,  1888

The volcano

Halemaʻumaʻu Crater (six syllables: HAH-lay-MAH-oo-MAH-oo) is a pit crater within the much larger summit caldera of Kīlauea in Hawaii Volcanoes National Park. The roughly circular crater was 770 meters (2,530 ft) x 900 m (2,950 ft) before collapses that roughly doubled the size of the crater after May 3, 2018. Halemaʻumaʻu is home to Pele, goddess of fire and volcanoes, according to the traditions of Hawaiian religion. Halemaʻumaʻu means "house of the ʻāmaʻu fern".

Halemaʻumaʻu contained an active lava lake for much of the time before 1924, and was the site of several eruptions during the 20th century. The crater again contained an active lava lake between 2008 and 2018, usually fluctuating between 20 to 150 meters below Halemaʻumaʻu's crater floor, though at times the lava lake rose high enough to spill onto crater floor.

As new volcanic vents opened in lower Puna in May 2018, the level of the lava lake began to drop in early May 2018, eventually to the point where the lava lake was no longer visible. The subsidence of the lava lake was accompanied by a period of explosions, earthquakes, large clouds of ash and toxic gas, and finally a gradual collapse of the summit caldera around Halemaʻumaʻu Crater, resulting in the closure of the Hawaii Volcanoes National Park from May 10 to September 22, 2018. The collapse events ceased abruptly on August 2, 2018.

In the summer of 2019, for the first time in recorded history, a water pond appeared in Halemaʻumaʻu. The greenish pond has deepened and enlarged since first being observed.

The painter
David Howard Hitchcock  was an American painter of the  so called Volcano School, known for his depictions of Hawaii.  Born in Hilo, Hawaii, Hitchcock attended Oberlin College in Ohio, where he saw his first art exhibition. Back in Hawaii, he wandered the volcano wilderness with a sketch pad and watercolors. French artist Jules Tavernier, painting in Hawaii, saw Hitchcock's sketches and convinced him to study art seriously.
After Tavernier's death in 1889 Hitchcock studied painting at the National Academy of Design in New York City and from 1891 to 1893 at the Académie Julian in Paris under Aldolphe Bourguereau and Gabriel Joseph Ferrier. His work was accepted at the Paris Salon of 1893. He returned to Hawaii in 1893.
In 1894, Hitchcock became one of the founders of the Kilohana Art League, an active art program in Honolulu at the turn of the century, exhibiting at least twice a year.
During extensive travels in the 1900s, Hitchcock explored the volcanic regions of the island of Hawaii, and in July 1907 he made his first visit to the island of Kauaʻi, where he painted Waimea Canyon. He toured and painted the island of Maui in 1915 and 1916. He was a leading member of Hawaii's Volcano School, and his most important paintings date from about 1905 to 1930.
His canvases were displayed in 1924 at the First Hawaiian and South Seas Exhibition in the Los Angeles Museum in Exposition Park. In 1927, he exhibited several paintings at the opening of the Honolulu Museum of Art, where he had a retrospective exhibition in 1936. In 1939 he exhibited in the Golden Gate International Exposition in San Francisco and at the 1939 New York World's Fair.

_______________________________

2019 - Wandering Vertexes...
by Francis Rousseau

ASCRAEUS MONS SEEN BY NASA MARS RECONNAISSANCE ORBITER

NASA MARS RECONNAISSANCE ORBITER (2005-2015) 

Ascraeus mons (18, 225m / 18, 1 kms- 50, 793 ft / 11, 1mi) 

Planet Mars

1.  In Ascraeus mons, HiRISE camera ,Mars Reconnaissance Orbiter (MRO); November 2010

2.  In  Colorized MOLA topography of Ascraeus Mons, 2006   

The mountain 
Ascraeus mons (18, 225m / 18kms- 50, 793 ft / 11, 1mi)  is a large shield volcano located in the Tharsis region of the planet Mars. It is the northernmost and tallest of three shield volcanoes collectively known as the Tharsis Montes. The volcano's location corresponds to the classical albedo feature Ascraeus Lacus.
Ascraeus Mons was discovered by the Mariner 9 spacecraft in 1971. The volcano was originally called North Spot because it was the northernmost of only four spots visible on the surface due to a global dust storm that was then enshrouding the planet. As the dust cleared, the spots were revealed to be extremely tall volcanoes whose summits had projected above the dust-laden, lower atmosphere.
The volcano is located in the southeast-central portion of the Tharsis quadrangle at 11.8°N, 255.5°E in Mars' western hemisphere.  Ascraeus Mons is roughly 480 km in diameter and is the second highest mountain on Mars, with a summit elevation of 18.1 km ! The volcano has a very low profile with an average flank slope of 7°. Slopes are steepest in the middle portion of the flanks, flattening out toward the base and near the top where a broad summit plateau and caldera (collapse crater) complex are located.
Volcanic vents, located on the northeastern and southwestern edges of the volcano, are sources for broad lava aprons, or fans, that bury nearby portions of the volcano and extend over 100 km out into the surrounding plains.  The southwest-northeast orientation of the aprons matches the orientation of the Tharsis Montes, suggesting that a major fissure or rift in the Martian crust is responsible for the orientation of both the aprons and the Tharsis Montes chain. The presence of the lava aprons causes some disagreement in the actual dimensions of the volcano.
Like most of the Tharsis region, Ascraeus Mons has a high albedo (reflectivity) and low thermal inertia, indicating that the volcano and surrounding areas are covered with large amounts of fine dust.  The dust forms a mantle over the surface that obscures or mutes much of the fine-scale topography and geology of the region. Tharsis is probably dusty because of its high elevations. The atmospheric density is too low to mobilize and remove dust once it is deposited.
Ascraeus Mons is surrounded by lava flow plains that are mid to late Amazonian in age. The elevation of the plains averages about 3 km above datum (Martian "sea" level), giving the volcano an average vertical relief of 15 km.  However, the elevation of the plains varies considerably. The plains northwest of the volcano are less than 2 km in elevation. The plains are highest (>3 km) southeast of the volcano.
The lava plains northwest of Ascraeus Mons are notable for having two dark collapse pits photographed by the HiRISE camera on the Mars Reconnaissance Orbiter (MRO) in November 2010 (image above) . The pits resemble those imaged around Arsia Mons by the Mars Odyssey spacecraft. The two pits measure about 180 and 310 m wide, and the larger pit is approximately 180 meters deep. The eastern walls of the pits consist of steep, overhanging ledges. The bottoms of both pits contain sediments and large boulders.  These rimless pit craters are believed to form by collapse of surface material into a subsurface void created either by a dike or lava tube. They are analogous to volcanic pit craters on Earth, such as the Devil's Throat crater on the upper east rift zone of Kilauea Volcano, Hawaii.  In some cases, they may mark skylights/entrances to subsurface lava caves.

The camera
The image above, has been captured by the HiRISE  (High Resolution Imaging Science Experiment) camera aboard NASA’s Mars Reconnaissance Orbiter. The 65 kg (143 lb), $40 million USD instrument was built under the direction of the University of Arizona's Lunar and Planetary Laboratory by Ball Aerospace & Technologies Corp. It consists of a 0.5 m (19.7 in) aperture reflecting telescope, the largest so far of any deep space mission, which allows it to take pictures of Mars with resolutions of 0.3 m/pixel (about 1 foot), resolving objects below a meter across.
HiRISE has imaged Mars landers on the surface, including the ongoing Curiosity and Opportunity rover missions.
HiRISE was designed to be a High Resolution camera from the beginning. It consists of a large mirror, as well as a large CCD camera. Because of this, it achieves a resolution of 1 microradian, or 0.3 meter at a height of 300 km. (For comparison purposes, satellite images on Google Mars are available to 1 meter). It can image in three color bands, 400–600 nm (blue-green or B-G), 550–850 nm (red) and 800–1,000 nm (near infrared or NIR).
HiRISE incorporates a 0.5-meter primary mirror, the largest optical telescope ever sent beyond Earth's orbit. The mass of the instrument is 64.2 kg.
Red color images are at 20,048 pixels wide (6 km in a 300 km orbit), and Green-Blue and NIR are at 4,048 pixels wide (1.2 km). These are gathered by 14 CCD sensors, 2048 x 128 pixels. HiRISE's onboard computer reads out these lines in time with the orbiter's ground speed, meaning the images are potentially unlimited in height. Practically this is limited by the onboard computer's 28 Gbit (3.5 GByte) memory capacity. The nominal maximum size of red images (compressed to 8 bits per pixel) is about 20,000 × 126,000 pixels, or 2520 megapixels and 4,000 × 126,000 pixels (504 megapixels) for the narrower images of the B-G and NIR bands. A single uncompressed image uses up to 28 Gbit. However, these images are transmitted compressed, with a typical max size of 11.2 Gigabits. These images are released to the general public on the HiRISE website via a new format called JPEG 2000.
To facilitate the mapping of potential landing sites, HiRISE can produce stereo pairs of images from which the topography can be measured to an accuracy of 0.25 meter.
The HiRISE camera is designed to view surface features of Mars in greater detail than has previously been possible. It has provided a closer look at fresh martian craters, revealing alluvial fans, viscous flow features and ponded regions of pitted materials containing breccia clast.  This allows for the study of the age of Martian features, looking for landing sites for future Mars landers, and in general, seeing the Martian surface in far greater detail than has previously been done from orbit. By doing so, it is allowing better studies of Martian channels and valleys, volcanic landforms, possible former lakes and oceans, and other surface landforms as they exist on the Martian surface.
The general public is allowed to request sites for the HiRISE camera to capture (see HiWish). For this reason, and due to the unprecedented access of pictures to the general public, shortly after they have been received and processed, the camera has been termed "The People's Camera".
 The pictures can be viewed online, downloaded, or with the free HiView software.

PITON DE LA FOURNAISE BY J- B. BORY DE SAINT VINCENT

JEAN-BAPTISTE BORY DE SAINT VINCENT  (1778-1846)

Le Piton de la Fournaise  (2,632 m -8,635 ft)

 France  (Ile de la Réunion)

 Drawing view"as the crow flies" of the peak of the Furnace after the eruption of 1801

The mountain 

Piton de la Fournaise (Peak of the Furnace) is a shield volcano on the eastern side of Réunion island (a French department) in the Indian Ocean. It is currently one of the most active volcanoes in the world, along with Kilauea in the Hawaiian Islands (Pacific Ocean), Stromboli, Etna (Italy) and Mount Erebus in Antarctica. A previous eruption began in August 2006 and ended in January 2007. The volcano erupted again in February 2007, on 21 September 2008, on 9 December 2010, which lasted for two days and on 1 August 2015 A. An other one on 26 May 2016 ... the very last eruption just begun yesterday,  11 Septembre 2016. 

The volcano is located within Réunion National Park, a World Heritage site.

Piton de la Fournaise is often known locally as le Volcan (The Volcano); it is a major tourist attraction on Réunion island.  Due to his activity, the Piton de la Fournaise is constantly monitored by geophysical sensors (tiltmeters, extensometers, differential GPS receivers, etc.).  The data from those various sensors is sent to the Piton de la Fournaise Volcano Observatory, located in Bourg-Murat, northwest of the volcano.  The observatory, founded in 1978 following the Piton-Sainte-Rose flow, is operated by the Institut de Physique du Globe de Paris (Global Geophysics Institute of Paris), in association with CNRS ( National Institute of Scientific Resarch)  and the University of Réunion. The OVPF often publishes reports on Piton de la Fournaise's current activity via their website in French. RIGIC (the Réunion Island Geological Information Center) takes this information and translates it into English for distribution to the English-speaking scientific.

Climbing

A high quality forestry road, followed by a track (with lots of bumps), connects the highway of the plains in Bourg-Murat to the Pas de Bellecombe (Bellecombe Pass), where a parking lot and a snack bar are available to visitors.  The Pas de Bellecombe is situated over the caldera rim cliffs and offers a good point of view over the northeast part of the caldera.

A good stairway path descends from the pass to the caldera floor.  This path is closed for safety reasons during seismic events that may precede eruptions and during eruptions. White paint marks over rocks delimit a number of footpaths ascending the lava shield inside the caldera.  Visitors exploring the caldera should be in good physical condition, with hiking shoes and a supply of drinking water and food. They must be prepared to exercise caution, for the weather can change very quickly, moving from bright sunlight and heat (with risks of heatstroke) to dense fog with cold and rain. In dense fog, straying from paths is very risky. Visitors are advised to take the necessary precautions for sun, heat, cold and rain and not to stray from marked paths.  An excellent, albeit expensive, way to get a good sight of the volcano is to ride in the tourist helicopter flights offered by commercial companies on the island The lower parts of the Grand Brûlé can be visited from the N2 highway.  Lava flows that have crossed the road are indicated by signs.

Completely free access during eruptions was permitted until 1998; access has been limited since that date, being virtually banned at present.

The painter  

Jean-Baptiste Genevieve Marcellin Bory de Saint-Vincent is a French officer, naturalist and geographer, who was mainly interested in volcanology, botany and systematic.

During the las years of the 18th century (particularly agitated in France) , he learned the departure of a scientific expedition organized by the government and gets the job of chief zoologist aboard a participating corvettes then met Bernard Germain de Lacépède. Thus, after leaving the army, Jean Baptiste Bory de Saint-Vincent left Paris on September 30, arrived in Le Havre on 2 October and leaves town aboard one of the ships that captain Nicolas Baudin took  around the world from 1800 to 1804.  He stopped in Mauritius in March 1801.  From there, he reached l'Ile de la Réunion (ex Bourbon Island) where he performed in October and November 1801 ( "An X" in the Revolutionary Calendar)  the rise and the first general scientific description of the Piton de la Fournaise, the active volcano of the island.  It gives the name of the scientist Dolomieu he just learned the death to  one of the craters he describes as a nipple. It gives its own name to the  crater of the summit.  Back in France in 1802, he published Voyage dans les îles d'Afrique (Travel in african Islands). He continued his scientific career in parallel to a military career: he was elected correspondent of the Museum in August 1803 and the "correspond of  first class" of the Institute de France in the spring of 1808. In 1804, he published  Essais sur les iles fortunées  (Essay on the wealthy islands) et Voyage dans les quatre principales îles des mers d'Afrique (Travel in the four main islands of the African seas). The articles, written by international scientific luminaries, were illustrated by  lithographs printed by Duval Mercourt then Marcellin Jobard.  In 1828, he was appointed to head the commission scientific exploration of Morea, held in 1829-1830. In 1830 he appeared in an election to become a member of the Institute after the death of Lamarck. He died in 1846 а Paris and was buried in Père Lachaise Cemetery (49th division).