VESUVIUS ERUPTION BY GEORGE-JULIUS POULETT SCROPE

 GEORGE-JULIUS POULETT SCROPE (1797-1876)

 Mount Vesuvius(1,281 m- 4,203 ft at present) 

 Italy

In  The Eruption of Vesuvius as seen from Naples, October 1822,   

Historical drawing from George Julius Poulett Scrope

The mountain 

Mount Vesuvius (1,281 meters- 4,203 ft at present) is one of those legendary and mythic mountains the Earth paid regularly tribute. Monte Vesuvio in Italian modern langage or Mons Vesuvius in antique Latin langage is a stratovolcano in the Gulf of Naples (Italy) about 9 km (5.6 mi) east of Naples and a short distance from the shore. 

It is one of several volcanoes which form the Campanian volcanic arc. Vesuvius consists of a large cone partially encircled by the steep rim of a summit caldera caused by the collapse of an earlier and originally much higher structure.

Mount Vesuvius is best known for its eruption in AD 79 that led to the burying and destruction of the Roman antique cities of Pompeii, Herculaneum, and several other settlements. That eruption ejected a cloud of stones, ash, and fumes to a height of 33 km (20.5 mi), spewing molten rock and pulverized pumice at the rate of 1.5 million tons per second, ultimately releasing a hundred thousand times the thermal energy released by the Hiroshima bombing. At least 1,000 people died in the eruption. The only surviving eyewitness account of the event consists of two letters by Pliny the Younger to the historian Tacitus.

Vesuvius has erupted many times since and is the only volcano on the European mainland to have erupted within the last hundred years. Nowadays, it is regarded as one of the most dangerous volcanoes in the world because of the population of 3,000,000 people living nearby and its tendency towards explosive eruptions (said Plinian eruptions). It is the most densely populated volcanic region in the world.

Vesuvius was formed as a result of the collision of two tectonic plates, the African and the Eurasian. The former was subducted beneath the latter, deeper into the earth. As the water-saturated sediments of the oceanic African plate were pushed to hotter depths in the earth, the water boiled off and caused the melting point of the upper mantle to drop enough to create partial melting of the rocks. Because magma is less dense than the solid rock around it, it was pushed upward. Finding a weak place at the Earth's surface it broke through, producing the volcano.

he area around Vesuvius was officially declared a national park on June 5, 1995. The summit of Vesuvius is open to visitors and there is a small network of paths around the mountain that are maintained by the park authorities on weekends.

There is access by road to within 200 metres (660 ft) of the summit (measured vertically), but thereafter access is on foot only. There is a spiral walkway around the mountain from the road to the crater.

The first funicular cable car on Mount Vesuvius opened in 1880. It was later destroyed by the 1944 eruption. "Funiculì, Funiculà", a famous Neapolitan song with lyrics by journalist Peppino Turco set to music by composer Luigi Denza, commemorates its opening.

The artist
George Julius Poulett Scrope (1797- 1876) was an English geologist and political economist as well as a magistrate for Stroud in Gloucestershire. He was educated at Harrow, and for a short time at Pembroke College, Oxford, but in 1816 he entered St John's College, Cambridge, graduating BA in 1821.  Through the influence of Edward Clarke and Adam Sedgwick he became interested in mineralogy and geology.
During the winter of 1816–1817 he was at Naples, and was so keenly interested in Vesuvius that he renewed his studies of the volcano in 1818; and in the following year visited Etna and the Lipari Islands. In 1821 he married the daughter and heiress of William Scrope of Castle Combe, Wiltshire, and assumed her name; and he entered the House of Commons of the United Kingdom in 1833 as MP for Stroud, retaining his seat until 1868.
Meanwhile he began to study the volcanic regions of central France in 1821, and visited the Eifel district in 1823. In 1825 he published Considerations on Volcanos, leading to the establishment of a new theory of the Earth, and in the following year was elected FRS. This earlier work was subsequently amplified and issued under the title of Volcanos (1862); an authoritative text-book of which a second edition was published ten years later.
In 1827 he issued his classic Memoir on the Geology of Central France, including the Volcanic formations of Auvergne, the Velay and the Vivarais, a quarto volume illustrated by maps and plates. The substance of this was reproduced in a revised and somewhat more popular form in The Geology and extinct Volcanos of Central France (1858). These books were the first widely published descriptions of the Chaîne des Puys, a chain of over 70 small volcanoes in the Massif Central.
Scrope was awarded the Wollaston Medal by the Geological Society of London in 1867. Among his other works was the History of the Manor and Ancient Barony of Castle Combe (printed for private circulation, 1852).
He died at Fairlawn near Cobham, Surrey on 19 January 1876.

_______________________________
2019 - Wandering Vertexes...
by Francis Rousseau 

MOUNT VESUVIUS PAINTED BY BYJEAN-DOMINIQUE INGRES

JEAN-DOMINIQUE INGRES (1780-1867) 

Mount Vesuvius (1, 281m - 4,203 ft current)

Italy

In  Caroline Murat, reine de Naples, 1814 oil on canvas 92 × 60 cm) Private owner 

The painting  
The portrait shows Queen Caroline Murat, wife of Joachim Murat and sister of Napoleon Ist, shortly before the fall of the kingdom led by her husband then King of Naples. She is shown "en pieds ", the body in profile, and wearing a black dress. She is holding a notebook on a table covered with green, and looks at the viewer. She is represented in the large cabinet of the Royal, Palace furnished in the antique style, framed by the large draped curtains. Behind her, a gold and crimson armchair. A large bay window faces the Bay of Naples, where Vesuvius can be seen from afar, from which a plume of smoke escapes. The portrait is signed lower left: Ingres Pxit Roma 18141.
Ingres left Rome in February 1814 to go to Naples, where he remained for three months. He works on the portrait of Queen Caroline Murat in July, as evidenced by a correspondence to Marcotte d'Argenteuil dated July 7, 1814: "I work in this moment-cy for the Queen of Naples. I just finished a little portrait of her ". 
The work painted in 1814, is part of the series of portraits painted by Ingres in Italy, and mainly in Rome, from 1807, representing the models detached on a landscape background
Ingres began by drawing several preparatory studies, including a drawing of the face (Museum Ingres de Montauban), three studies for the dress and the hand, and several drawings of draperies, furniture, and a view of the Bay of Naples and Vesuvius (Ingres Museum).

The painter
Jean-Auguste-Dominique Ingres was a French Neoclassical painter.
 Ingres was profoundly influenced by past artistic traditions and aspired to become the guardian of academic orthodoxy against the ascendant Romantic style. Although he considered himself a painter of history in the tradition of Nicolas Poussin and Jacques-Louis David, it is his portraits, both painted and drawn, that are recognized as his greatest legacy. His expressive distortions of form and space made him an important precursor of modern art, influencing Picasso, Matisse and other modernists.
Born into a modest family in Montauban, he travelled to Paris to study in the studio of David.
In 1802 he made his Salon debut, and won the Prix de Rome for his painting The Ambassadors of Agamemnon in the tent of Achilles. By the time he departed in 1806 for his residency in Rome, his style—revealing his close study of Italian and Flemish Renaissance masters—was fully developed, and would change little for the rest of his life. While working in Rome and subsequently Florence from 1806 to 1824, he regularly sent paintings to the Paris Salon, where they were faulted by critics who found his style bizarre and archaic. He received few commissions during this period for the history paintings he aspired to paint, but was able to support himself and his wife as a portrait painter and draughtsman.
He was finally recognized at the Salon in 1824, when his Raphaelesque painting of the Vow of Louis XIII was met with acclaim, and Ingres was acknowledged as the leader of the Neoclassical school in France. Although the income from commissions for history paintings allowed him to paint fewer portraits, his Portrait of Monsieur Bertin marked his next popular success in 1833. The following year, his indignation at the harsh criticism of his ambitious composition The Martyrdom of Saint Symphorian caused him to return to Italy, where he assumed directorship of the French Academy in Rome in 1835. He returned to Paris for good in 1841. In his later years he painted new versions of many of his earlier compositions, a series of designs for stained glass windows, several important portraits of women, and The Turkish Bath, the last of his several Orientalist paintings of the female nude, which he finished at the age of 83.

The mountain 
Mount Vesuvius (1,281 meters- 4,203 ft current) is one of those legendary and mythic mountains  the Earth paid regularly tribute. Monte Vesuvio in Italian modern langage or Mons Vesuvius in antique Latin langage is a stratovolcano in the Gulf of Naples (Italy) about 9 km (5.6 mi) east of Naples and a short distance from the shore.
It is one of several volcanoes which form the Campanian volcanic arc. Vesuvius consists of a large cone partially encircled by the steep rim of a summit caldera caused by the collapse of an earlier and originally much higher structure.
Mount Vesuvius is best known for its eruption in AD 79 that led to the burying and destruction of the Roman antique cities of Pompeii, Herculaneum, and several other settlements. That eruption ejected a cloud of stones, ash, and fumes to a height of 33 km (20.5 mi), spewing molten rock and pulverized pumice at the rate of 1.5 million tons per second, ultimately releasing a hundred thousand times the thermal energy released by the Hiroshima bombing. At least 1,000 people died in the eruption. The only surviving eyewitness account of the event consists of two letters by Pliny the Younger to the historian Tacitus.
Vesuvius has erupted many times since and is the only volcano on the European mainland to have erupted within the last hundred years. Nowadays, it is regarded as one of the most dangerous volcanoes in the world because of the population of 3,000,000 people living nearby and its tendency towards explosive eruptions (said Plinian eruptions). It is the most densely populated volcanic region in the world.
Vesuvius was formed as a result of the collision of two tectonic plates, the African and the Eurasian. The former was subducted beneath the latter, deeper into the earth. As the water-saturated sediments of the oceanic African plate were pushed to hotter depths in the earth, the water boiled off and caused the melting point of the upper mantle to drop enough to create partial melting of the rocks. Because magma is less dense than the solid rock around it, it was pushed upward. Finding a weak place at the Earth's surface it broke through, producing the volcano.
The area around Vesuvius was officially declared a national park on June 5, 1995. The summit of Vesuvius is open to visitors and there is a small network of paths around the mountain that are maintained by the park authorities on weekends.
There is access by road to within 200 metres (660 ft) of the summit (measured vertically), but thereafter access is on foot only. There is a spiral walkway around the mountain from the road to the crater.
The first funicular cable car on Mount Vesuvius opened in 1880. It was later destroyed by the 1944 eruption. "Funiculì, Funiculà", a famous Neapolitan song with lyrics by journalist Peppino Turco set to music by composer Luigi Denza, commemorates its opening.

_______________________________
2018 - Wandering Vertexes...
by Francis Rousseau 

MOUNT VESUVIUS PAINTED BY ALBERT MARQUET

ALBERT MARQUET (1875–1947), 

 Mount Vesuvius (1,281 m- 4,203 ft at present) 

 Italy

In La baie de  Naples et le Vésuve, 81 x 69 cm, oil on canvas 1909,   Pushkin museum, Moscow

The mountain 

Mount Vesuvius (1,281 m - 4,203 ft at present) is one of those legendary and mythic mountains  the Earth  paid regularly tribute. Monte Vesuvio in Italian modern langage or Mons Vesuvius in antique Latin langage is a stratovolcano in the Gulf of Naples (Italy) about 9 km (5.6 mi) east of Naples and a short distance from the shore. 

It is one of several volcanoes which form the Campanian volcanic arc. Vesuvius consists of a large cone partially encircled by the steep rim of a summit caldera caused by the collapse of an earlier and originally much higher structure.

Mount Vesuvius is best known for its eruption in AD 79 that led to the burying and destruction of the Roman antique cities of Pompeii, Herculaneum, and several other settlements. That eruption ejected a cloud of stones, ash, and fumes to a height of 33 km (20.5 mi), spewing molten rock and pulverized pumice at the rate of 1.5 million tons per second, ultimately releasing a hundred thousand times the thermal energy released by the Hiroshima bombing. At least 1,000 people died in the eruption. The only surviving eyewitness account of the event consists of two letters by Pliny the Younger to the historian Tacitus.

Vesuvius has erupted many times since and is the only volcano on the European mainland to have erupted within the last hundred years. Nowadays, it is regarded as one of the most dangerous volcanoes in the world because of the population of 3,000,000 people living nearby and its tendency towards explosive eruptions (said Plinian eruptions). It is the most densely populated volcanic region in the world.

Vesuvius was formed as a result of the collision of two tectonic plates, the African and the Eurasian. The former was subducted beneath the latter, deeper into the earth. As the water-saturated sediments of the oceanic African plate were pushed to hotter depths in the earth, the water boiled off and caused the melting point of the upper mantle to drop enough to create partial melting of the rocks. Because magma is less dense than the solid rock around it, it was pushed upward. Finding a weak place at the Earth's surface it broke through, producing the volcano.

The area around Vesuvius was officially declared a national park on June 5, 1995. The summit of Vesuvius is open to visitors and there is a small network of paths around the mountain that are maintained by the park authorities on weekends.

The painter 
Albert Marquet was a French painter, associated with the Fauvist movement. He initially became one of the Fauve painters and a lifelong friend of Henri Matisse. In 1890 Marquet moved to Paris to attend the Ecole des Arts Decoratifs, where he met Henri Matisse. They were roommates for a time, and they influenced each other's work. Marquet began studies in 1892 at the École des Beaux-Arts de Paris under Gustave Moreau, the famous symbolist artist. In 1905 he exhibited at the Salon d'Automne. Dismayed by the intense coloration in these paintings, critics reacted by naming the artists the "Fauves", i.e. the wild beasts. Although Marquet painted with the fauves for years, he used less bright and violent colours than the others, and emphasized less intense tones made by mixing complementaries, thus always as colors and never as grays.
From 1907 to his death, Marquet alternated between working in his studio in Paris (a city he painted a lot of times) and many parts of the European coast and in North Africa. He was most involved with Algeria and Algiers and Tunisia. He remained also impressed particularly with Naples and Venice where he painted the sea and boats, accenting the light over water.  During his voyages to Germany and Sweden he painted the subjects he usually preferred: river and sea views, ports and ships, but also cityscapes.

Matisse said ; "When I look at Hokusai, I think of Marquet—and vice versa ... I don't mean imitation of Hokusai, I mean similarity with him".

___________________________________________
2019 - Wandering Vertexes...
by Francis Rousseau 

VESUVIUS PAINTED BY JOSEPH REBELL

JOSEPH REBELL (1787-1828) 

Mount Vesuvius (1,281m - 4,203ft)

Italy

In Vesuvio in 1813-15, oil on canvas, Staatliche Kunsthalle Karlsruhe.

The mountain 

Mount Vesuvius (1,281 meters- 4,203 ft at present) is one of those legendary and mythic mountains the Earth paid regularly tribute. Monte Vesuvio in Italian modern langage or Mons Vesuvius in antique Latin langage is a stratovolcano in the Gulf of Naples (Italy) about 9 km (5.6 mi) east of Naples and a short distance from the shore.
It is one of several volcanoes which form the Campanian volcanic arc. Vesuvius consists of a large cone partially encircled by the steep rim of a summit caldera caused by the collapse of an earlier and originally much higher structure.
Mount Vesuvius is best known for its eruption in AD 79 that led to the burying and destruction of the Roman antique cities of Pompeii, Herculaneum, and several other settlements. That eruption ejected a cloud of stones, ash, and fumes to a height of 33 km (20.5 mi), spewing molten rock and pulverized pumice at the rate of 1.5 million tons per second, ultimately releasing a hundred thousand times the thermal energy released by the Hiroshima bombing. At least 1,000 people died in the eruption. The only surviving eyewitness account of the event consists of two letters by Pliny the Younger to the historian Tacitus.

More about Vesuvius ...

The painter
Joseph Rebell is an Austrian landscape painter.
After studying at the Academy of Fine Arts in Vienna, he stayed in Berne in Switzerland in 1809 and in Milan between 1810 and 1812 at the court of Eugene de Beauharnais and Naples between 1813 and 1815, including the court of Joachim Murat. He then moved to Rome between 1816 and 1824. On this date, he was called to Vienna by Francis I of Austria to run the Belvedere Gallery, where he remained until his death from illness in 1828, when a trip to Dresden.

__________________________________________________
2019 - Wandering Vertexes...
by Francis Rousseau

VESUVIUS PAINTED BY GUSTAVE CAILLEBOTTE

GUSTAVE CAILLEBOTTE  (1848-1894) 

Vesuvius  (1,281m - 4,203ft)

Italy

In Sur une route à Naples (c. 1872), Oil on canvas, 60 x 40 cm. Private Collection

About the painting

The mountain was not, strictly speaking, Caillebotte's main subject of interest ! He painted very little, (not to say) no mountains! The canvas above is his only known example and still represents a mountain (the Vesuvius) seized as by accident while he wants especially to paint the horse-drawn car which led him in this  Neapolitan  campaign to observe this most famous volcano under a nes angle. The result is a masterwork  with this unexpected view of the volcano ! 

The mountain 

Mount Vesuvius (1,281 meters- 4,203 ft at present) is one of those legendary and mythic mountains the Earth paid regularly tribute. Monte Vesuvio in Italian modern langage or Mons Vesuvius in antique Latin langage is a stratovolcano in the Gulf of Naples (Italy) about 9 km (5.6 mi) east of Naples and a short distance from the shore. 

It is one of several volcanoes which form the Campanian volcanic arc. Vesuvius consists of a large cone partially encircled by the steep rim of a summit caldera caused by the collapse of an earlier and originally much higher structure.

Mount Vesuvius is best known for its eruption in AD 79 that led to the burying and destruction of the Roman antique cities of Pompeii, Herculaneum, and several other settlements. That eruption ejected a cloud of stones, ash, and fumes to a height of 33 km (20.5 mi), spewing molten rock and pulverized pumice at the rate of 1.5 million tons per second, ultimately releasing a hundred thousand times the thermal energy released by the Hiroshima bombing. At least 1,000 people died in the eruption. The only surviving eyewitness account of the event consists of two letters by Pliny the Younger to the historian Tacitus.

Vesuvius has erupted many times since and is the only volcano on the European mainland to have erupted within the last hundred years. Nowadays, it is regarded as one of the most dangerous volcanoes in the world because of the population of 3,000,000 people living nearby and its tendency towards explosive eruptions (said Plinian eruptions). It is the most densely populated volcanic region in the world.

Vesuvius was formed as a result of the collision of two tectonic plates, the African and the Eurasian. The former was subducted beneath the latter, deeper into the earth. As the water-saturated sediments of the oceanic African plate were pushed to hotter depths in the earth, the water boiled off and caused the melting point of the upper mantle to drop enough to create partial melting of the rocks. Because magma is less dense than the solid rock around it, it was pushed upward. Finding a weak place at the Earth's surface it broke through, producing the volcano.

he area around Vesuvius was officially declared a national park on June 5, 1995. The summit of Vesuvius is open to visitors and there is a small network of paths around the mountain that are maintained by the park authorities on weekends.

There is access by road to within 200 metres (660 ft) of the summit (measured vertically), but thereafter access is on foot only. There is a spiral walkway around the mountain from the road to the crater.

The first funicular cable car on Mount Vesuvius opened in 1880. It was later destroyed by the 1944 eruption. "Funiculì, Funiculà", a famous Neapolitan song with lyrics by journalist Peppino Turco set to music by composer Luigi Denza, commemorates its opening.

The painter
The very important french painter Gustave Caillebotte, (known in US more than his own country) was a member and patron of the artists known as Impressionists,(or independents) although he painted in a more realistic manner than many others in the group. Caillebotte was noted for his early interest in photography as an art form.
With regard to the composition and painting style of his works, Caillebotte may be considered part of the first movement after Impressionism: Neo-Impressionism. The second period of Pointillism, whose main representative was Georges Seurat, announced its influence in the late works that Caillebotte painted at his country house in Petit Gennevilliers. 

Caillebotte's style belongs to the School of Realism but was strongly influenced by his Impressionist associates. In common with his precursors Jean-François Millet and Gustave Courbet, as well his contemporary Degas, Caillebotte aimed to paint reality as it existed and as he saw it, hoping to reduce the inherent theatricality of painting. Perhaps because of his close relationship with so many of his peers, his style and technique vary considerably among his works, as if "borrowing" and experimenting, but not really sticking to any one style. At times, he seems very much in the Edgar Degas camp of rich-colored realism (especially his interior scenes); at other times, he shares the Impressionist commitment to "optical truth" and employs an impressionistic pastel-softness and loose brush strokes most similar to Renoir and Pissarro, although with a less vibrant palette.
The tilted ground common to these paintings is very characteristic of Caillebotte's work, which may have been strongly influenced by Japanese prints and the new technology of photography, although evidence of his use of photography is lacking. Cropping and "zooming-in", techniques that commonly are found in Caillebotte's oeuvre, may also be the result of his interest in photography, but may just as likely be derived from his intense interest in perspective effects. A large number of Caillebotte's works also employ a very high vantage point, including View of Rooftops - Snow (Vue de toits (Effet de neige) 1878, Boulevard Seen from Above (Boulevard vu d'en haut) 1880, and A Traffic Island (Un refuge, boulevard Haussmann), 1880.
Caillebotte is best known for his paintings of  still life , water sports and urban Paris, The latter is almost unique among his works for its particularly flat colors and photo-realistic effect, which give the painting its distinctive and modern look, almost akin to American Realists such as Edward Hopper.

___________________________________________

2019 - Wandering Vertexes...

by Francis Rousseau 

VESUVIUS PAINTED BY ALBERT MARQUET

 

ALBERT MARQUET (1875–1947)

Mount Vesuvius (1,281m - 4,203ft)

Italy

 In La baie de  Naples et le Vésuve, 1909, Oil on canvas, 62x 80 cm  

Ermitage Museum, Sankt-Petersburg, Russia

The mountain
Mount Vesuvius (1,281 meters- 4,203 ft at present) is one of those legendary and mythic mountains the Earth paid regularly tribute. Monte Vesuvio in Italian modern langage or Mons Vesuvius in antique Latin langage is a stratovolcano in the Gulf of Naples (Italy) about 9 km (5.6 mi) east of Naples and a short distance from the shore.
It is one of several volcanoes which form the Campanian volcanic arc. Vesuvius consists of a large cone partially encircled by the steep rim of a summit caldera caused by the collapse of an earlier and originally much higher structure.
Mount Vesuvius is best known for its eruption in AD 79 that led to the burying and destruction of the Roman antique cities of Pompeii, Herculaneum, and several other settlements. That eruption ejected a cloud of stones, ash, and fumes to a height of 33 km (20.5 mi), spewing molten rock and pulverized pumice at the rate of 1.5 million tons per second, ultimately releasing a hundred thousand times the thermal energy released by the Hiroshima bombing. At least 1,000 people died in the eruption. The only surviving eyewitness account of the event consists of two letters by Pliny the Younger to the historian Tacitus.
More about Vesuvius ...


The painter
Albert Marquet was a French painter, associated with the Fauvist movement. He initially became one of the Fauve painters and a lifelong friend of Henri Matisse. In 1890 Marquet moved to Paris to attend the Ecole des Arts Decoratifs, where he met Henri Matisse. They were roommates for a time, and they influenced each other's work. Marquet began studies in 1892 at the École des Beaux-Arts de Paris under Gustave Moreau, the famous symbolist artist. In 1905 he exhibited at the Salon d'Automne. Dismayed by the intense coloration in these paintings, critics reacted by naming the artists the "Fauves", i.e. the wild beasts. Although Marquet painted with the fauves for years, he used less bright and violent colours than the others, and emphasized less intense tones made by mixing complementaries, thus always as colors and never as grays.
Marquet subsequently painted in a more naturalistic style, primarily landscapes, but also several portraits and, between 1910 and 1914, several female nude paintings.
From 1907 to his death, Marquet alternated between working in his studio in Paris (a city he painted a lot of times) and many parts of the European coast and in North Africa. He was most involved with Algeria and Algiers and with Tunisia. He remained also impressed particularly with Naples (see above) and Venice where he painted the sea and boats, accenting the light over water. During his voyages to Germany and Sweden he painted the subjects he usually preferred: river and sea views, ports and ships, but also cityscapes.
Marquet was particularly revered by the American painters Leland Bell and his wife Louisa Matthiasdottir. He was also revered by Bell's contemporaries Al Kresch and Gabriel Laderman. Since both Bell and Laderman were teachers in several American art schools, they have had an influence on younger American figurative artists and their appreciation of Marquet.
Matisse said ; "When I look at Hokusai, I think of Marquet—and vice versa ... I don't mean imitation of Hokusai, I mean similarity with him".

_____________________________

2020 - Wandering Vertexes...
by Francis Rousseau

LE VESUVE PEINT PAR ROBERT SCOTT DUNCANSON

 

ROBERT SCOTT DUNCANSON (1821-1872)
Le Vésuve (1,281m)
Italie

In Mount Vesuvius and Pompei ruins, 1879, Huile sur toile, 25.4 x 39.7 cm.
Smithsonian American Art Museum, Washington DC

L'artiste
Robert Scott Duncanson,  est le premier artiste afro-américain qui ait été reconnu de son vivant. Selon Joseph D. Ketner, conservateur de la galerie d'art de l'université d'État de Washington, il peint dans la tradition de l'Ecole de l'Hudson River. Il a été souvent inspiré par la littérature romantique anglaise. C'est un artiste peintre assez peu connu aujourd'hui, tant pour ses portraits que ses paysages beaux et sereins, marqués par les espaces encore sauvages de l'Amérique du Nord.
À son retour au domicile de sa mère, Duncanson aurait dit, « je reviens pour être artiste ». Il déménagea à Cincinnati. À cette époque, Cincinnati était connue comme « l'Athènes de l'Occident ». Duncanson possédait le dynamisme et la volonté de devenir artiste, mais il n'avait reçu aucune formation technique. Autodidacte, il apprit en copiant des portraits et des images imprimées. Sa détermination lui permit de voyager dans le monde et de poursuivre une longue carrière, jusqu'à sa mort en 1872. Il peignit plusieurs fois le Vésuve dans une période calme  relatif comme on peut le voir,  mais  il ne le peignit qu'une seule fois en insérant un tableau dans le tableau comme ici avec ce fragment de mur peint dont il est  plutôt difficile d'identifier le sujet.

Le volcan
Le Vésuve (1,281 mètres actuellement) fait partie de ces montagnes légendaires qui se rappelle régulièrement à l'attention des terriens. Monte Vesuvius ou Vesuvio en italien moderne ou Mons Vesuvius en latin antique est un stratovolcan située dans le golfe de Naples (Italie) à environ 9 km (5,6 mi) à l'est de Naples et à une courte distance du rivage. C'est l'un des nombreux volcans qui forment l'Arc Campanien. Il s'est formé à la suite de la collision de deux plaques tectoniques, l'africaine et l'eurasienne. Le Vésuve se compose d'un grand cône partiellement encerclé par le bord escarpé d'une caldeira sommitale causée par l'effondrement d'une structure antérieure et à l'origine beaucoup plus élevée.
Le mont Vésuve est surtout connu pour sa grande  éruption en 79 après JC qui a conduit à l'enterrement et à la destruction des villes antiques romaines de Pompéi, d'Herculanum et de plusieurs autres petits villages. Cette éruption a éjecté un nuage de pierres, de cendres et de fumées à une hauteur de 33 km (20,5 mi), crachant de la roche en fusion et de la pierre ponce pulvérisée à raison de 1,5 million de tonnes par seconde, libérant finalement cent mille fois l'énergie thermique libérée par l'attentat d'Hiroshima. Au moins 1 000 personnes sont mortes dans l'éruption. Le seul récit de témoin oculaire survivant de l'événement consiste en deux lettres de Pline le Jeune à l'historien Tacite. Depuis l'an 79, le Vésuve est entré en éruption environ trois douzaines de fois.
En 203, du vivant de l'historien Cassius Dio.
En 472, il a éjecté un tel volume de cendres que des chutes de cendres ont été signalées jusqu'à Constantinople à 1 220 km) de là.
Les éruptions de 512 ont été si graves que les habitants des pentes du Vésuve ont été exonérés d'impôts par Théodoric le Grand, alors le roi d'Italie.
D'autres éruptions ont été enregistrées en 787, 968, 991, 999, 1007 et 1036 avec les premières coulées de lave enregistrées. Le volcan s'est calmé à la fin du XIIIe siècle et dans les années suivantes, il s'est à nouveau couvert de jardins et de vignes comme autrefois. Même l'intérieur du cratère était rempli d'arbustes.
Le Vésuve est entré dans une nouvelle phase en décembre 1631, lorsqu'une éruption majeure a enseveli de nombreux villages sous des coulées de lave, tuant environ 3 000 personnes. Des torrents de lahar ont  ajouté à la dévastation. L'activité est ensuite devenue presque continue, avec des éruptions relativement graves se produisant en 1660, 1682, 1694, 1698, 1707, 1737, 1760, 1767, 1779, 1794, 1822, 1834, 1839, 1850, 1855, 1861, 1868, 1872, 1906 1926, 1929 et 1944. De nos jours, il est considéré comme l'un des volcans les plus dangereux au monde en raison de la population de 3 000 000 de personnes vivant à proximité et de sa tendance aux éruptions explosives (dites éruptions pliniennes). C'est la région volcanique la plus densément peuplée au monde.

La zone autour du Vésuve a été officiellement déclarée parc national le 5 juin 1995. Le sommet du Vésuve est ouvert aux visiteurs et il existe un petit réseau de sentiers autour de la montagne

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2022 - Wandering Vertexes ....
            Errant au-dessus des Sommets Silencieux...
            Un blog de Francis Rousseau