google.com, pub-0288379932320714, DIRECT, f08c47fec0942fa0 GRAVIR LES MONTAGNES... EN PEINTURE: APENNINES
Showing posts with label APENNINES. Show all posts
Showing posts with label APENNINES. Show all posts

Saturday, August 19, 2023

LE VÉSUVE DÉSSINÉ PÄR JOHN AULDJO


JOHN AULDJO ( 1805-1886) Le Vésuve (1,281 mètres actuellment) Italie   In " Auldjo in the white pants, leaning on a rock and contemplating a spewing lava dome ", watercolor,  Linda Hall Library


JOHN AULDJO ( 1805-1886)
Le Vésuve (1,281 mètres actuellement)
Italie

In " Auldjo in the white pants, leaning on a rock and contemplating a spewing lava dome ", watercolor,  Linda Hall Library


Le peintre
John Richardson Auldjo était un voyageur, géologue, écrivain et artiste canado-britannique. Il était consul britannique à Genève. John Auldjo est né dans une grande famille de marchands et d'hommes politiques de Montréal. En 1822, Auldjo entra au Trinity College de Cambridge . Avant de se lancer dans son Grand Tour, il s'est assuré une place au Lincoln's Inn, à Londres. En 1827, au début de sa tournée, il décide de monter au sommet du Mont Blanc accompagné de six guides. Au sommet, il partage une bouteille de vin avec les guides, puis s'assoid pour écrire une courte lettre à sa sœur. La lettre, encore conservée aujourd'hui et signée au dos par les six guides, est l'un des éléments les plus pittoresques des Archives du Club Alpin. Le récit de l'ascension, qu'il écrivit en 1828 augmenté de ses propres illustrations, fut un succès immédiat et connut trois éditions successives.
En 1830, il prend la décision de rester en Europe en donnant procuration sur ses propriétés canadiennes à son avocat, Thomas Kirkpatrick. A partir de ce moment là , Auldjo a vécu à Naples et devint l'un des piliers du cercle de Sir William Gell. Ce cercle très fermé comprenait Sir William Drummond, Keppel Richard Craven Lady Blessington Sir Walter Scott et Edward Bulwer-Lytton, qui était l'ami particulièrement proche d'Auldjo. Lord Byron, un autre invité fréquent à Naples, lui était également bien connu. En 1831, Auldjo entreprend de grimper sur le Vésuve alors que celui ci connait une période d'activité intense. Il publie à son retour un livre rempli de lithographies coloriées à la main du volcan en pleine éruption.Ses recherches sur le Vésuve ont ensuite été récompensées par des bourses à la Royal Society et à la Royal Geographical Society.
En 1833, il se rend Constantinople et dans les îles grecques et publie un récit de son séjour. Franc-maçon actif, il est nommé en 1837, grand maître du Haut-Canada et, à ce titre, à la fin de l'été de cette année-là, il s'y rendit. Entre-temps, son frère, qui séjournait avec lui à Naples , mourut.Il retourna à Londres et fut noté pour la dernière fois dans les archives des francs-maçons comme assistant à une réunion en 1841–2. On perd ensuie totalement sa trace avant qu'il ne réeapparaisse à Genève en 1870, à l'occasion d'un entretien avec son avocat, Sir George Airey Kirkpatrick, au sujet de la propriété canadienne. Il a occupé le poste non rémunéré de consul britannique à Genève de 1872 jusqu'à sa mort en 1886. Il y est enterré au cimetière de la Châtelaine.


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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2023 - Gravir les montagnes en peinture...
Un blog de Francis Rousseau



Sunday, November 20, 2022

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

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

Friday, April 29, 2022

MOUNT VESUVIUS SEEN FROM SORRENTE BY ALFRED DE CURZON


ALFRED DE CURZON (1820-1895) Mount Vesuvius (1,281 m- 4,203 ft at present) Italy  In "Sorrente, devant la mer de Naples ", 1851 Huile sur papier marouflé sur toile 24,5 x 33 cm, Collection privée, courtesy Galerie d'Athènes, Paris

 

ALFRED DE CURZON (1820-1895)
Mount Vesuvius (1,281 m- 4,203 ft at present)
Italy

In "Sorrente, devant la mer de Naples ", 1851, huile sur papier marouflé sur toile 24,5 x 33 cm,
Collection privée, courtesy Galerie d'Athènes, Paris

The painter
Alfred de Curzon is a French painter, grandson of Joseph-Emmanuel-Auguste-François de Lambertye and brother of Emmanuel Parent de Curzon. Alfred de Curzon's family is part of the aristocracy of western France. While he was a student, the painting Médée furieuse by Eugène Delacroix, exhibited at the Salon of 1838, made a strong impression on him. He tries his hand at pastel and decides to become a painter. He entered the 1 April 1840 at the School of Fine Arts in Paris in the studio of Michel Martin Drolling. On the advice of one of his classmates from the school, Louis Georges Brillouin (1817-1893), he changed studio to follow the lessons of Louis Cabat from 1845.
In 1849 he painted La Mort de Milon de Crotone. At the request of the Academy, he obtained from the minister the enjoyment of the pension of Rome for two years. There he met Alexandre Cabanel, Jean-Achille Benouville, François-Léon Benouville, Louis Français and Charles Busson who remained his friend. He travel to Greece in 1852 with the writer Edmond About and the architect Charles Garnier. Greek antiquity then strongly impregnated him and is found in many of his paintings.
He began at the Salon of 1843 with a painting entitled Landscape. He obtained a 2nd class medal in 1857, followed by recalls in 1859, 1861 and 1863. He was awarded a 3rd class medal at the Universal Exhibition of 1867.
Charles Baudelaire notes, in his Salon of 1845: "A serenade in a boat, - is one of the most distinguished things of the Salon. - The arrangement of all these figures is very happily conceived; the old man at the end of the boat, lying in the middle of the garlands, is a very pretty idea. - The compositions of M. Brillouin and that of M. Curzon have some analogy; they have this above all in common, that they are well drawn - and drawn with spirit."
Alfred de Curzon practiced all genres, but it was his landscapes that made him famous. Many drawings can be seen at the Sainte-Croix museum in Poitiers (France).

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.
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.
 
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2022 - Wandering Vertexes / Mountain painting
By Francis Rousseau

Saturday, May 1, 2021

MOUNT VESUVIUS PAINTED BY CHARLES-FRANÇOIS DE LA CROIX DE MARSEILLE

CHARLES-FRANÇOIS DE LA CROIX DE MARSEILLE (1700-1782) Mount Vesuvius (1,281m - 4,203ft) Italy  In Eruption du Vésuve en 1770, oil on canvas, Private collection

CHARLES-FRANÇOIS DE LA CROIX DE MARSEILLE (1700-1782)
Mount Vesuvius (1,281m - 4,203ft)
Italy

In Eruption du Vésuve en 1770, oil on canvas, Private collection
 


The volcano
Mount Vesuvius (1,281 meters- 4,203 ft at present) is one of those legendary and mythic mountains the Earth paid regularly tribute. Monte Vesuvius or 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.  Since the eruption of AD 79, Vesuvius has erupted around three dozen times.
It erupted again in 203, during the lifetime of the historian Cassius Dio.
In 472, it ejected such a volume of ash that ashfalls were reported as far away as Constantinople (760 mi.; 1,220 kms).
The eruptions of 512 were so severe that those inhabiting the slopes of Vesuvius were granted exemption from taxes by Theodoric the Great, the Gothicking of Italy.
Further eruptions were recorded in 787, 968, 991, 999, 1007 and 1036 with the first recorded lava flows. The volcano became quiescent at the end of the 13th century and in the following years it again became covered with gardens and vineyards as of old. Even the inside of the crater was moderately filled with shrubbery.
Vesuvius entered a new phase in December 1631, when a major eruption buried many villages under lava flows, killing around 3,000 people. Torrents of lahar were also created, adding to the devastation. Activity thereafter became almost continuous, with relatively severe eruptions occurring in 1660, 1682, 1694, 1698, 1707, 1737, 1760, 1767, 1779, 1794, 1822, 1834, 1839, 1850, 1855, 1861, 1868, 1872, 1906, 1926, 1929, and 1944.  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 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

Charles François Grenier de Lacroix, called Charles Francois Lacroix de Marseille, was a French painter
reknown for his landscapes and marines, in the style of Claude Joseph Vernet, Jean-Joseph Kapeller and Henry of Arles. He was a pupil and imitator of Joseph Vernet, and stayed in Rome in 1754. From 1776, he exhibited with great success and spent a good part of his life between Italy and Provence. In 1780, he published an ad to welcome students in his studio in Paris. Jean-Jacques Le Veau and Noël Le Mire engraved some of his paintings.


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2021 - Wandering Vertexes...
by Francis Rousseau

Tuesday, December 1, 2020

MOUNT VESUVIUS PAINTED BY ALBERT MARQUET (3)

 

https://wanderingvertexes.blogspot.com/2020/12/mount-vesuvius-painted-by-albert.html

ALBERT MARQUET (1875–1947),
Mount Vesuvius (1,281 m- 4,203 ft at present)
Italy 
                     
                              In La Baie de Naples et le Vésuve, 1909, oil on canvas,  Tate London

About this painting
During his jounrey to Italy in 1909, Albert Marquet has painted Vesuvius several times, at different moment of the day  and, each time with the same title, which doen'st make their identificationn very easy ! Here are too others examples already pusblished in this blog : 
- La baie de Naples et le Vésuve, 1909, Pushkin museum, Moscow
- La baie de Naples et le Vésuve, 1909, Ermitage Museum, Sankt-Petersburg, Russia


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".

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2020 - Wandering Vertexes...
by Francis Rousseau

Tuesday, October 6, 2020

MOUNT VESUVIUS PAINTED BY JOHN MARTIN


JOHN MARTIN (1789-1854) Mount Vesuvius (1,281m - 4,203ft) Italy  In  The destruction of Pompei in 79. c.1821, Tate Britain, London

JOHN MARTIN (1789-1854)
Mount Vesuvius (1,281m - 4,203ft)
Italy

In The destruction of Pompei in 79. c.1821, Tate Britain, London

The painter
John Martin was an English Romantic painter, engraver and illustrator. He was celebrated for his typically vast and melodramatic paintings of religious subjects and fantastic compositions, populated with minute figures placed in imposing landscapes. Martin's paintings, and the prints made from them, enjoyed great success with the general public—in 1821 Thomas Lawrence referred to him as "the most popular painter of his day"—but were lambasted by John Ruskin and other critics. Martin's large paintings were closely connected with contemporary dioramas or panoramas, popular entertainments in which large painted cloths were displayed, and animated by the skilful use of artificial light. Martin has often been claimed as a forerunner of the epic cinema, and there is no doubt that the pioneer director D. W. Griffith was aware of his work." In turn, the diorama makers borrowed Martin's work, to the point of plagiarism. A 2,000-square-foot (190 m2) version of Belshazzar's Feast was mounted at a facility called the British Diorama in 1833; Martin tried, but failed, to shut down the display with a court order. Another diorama of the same picture was staged in New York City in 1835. These dioramas were tremendous successes with their audiences, but wounded Martin's reputation in the serious art world.

The volcano
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.
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.

___________________________
2020 - Wandering Vertexes...
by Francis Rousseau


Saturday, September 26, 2020

MOUNT VESUVIUS PAINTED BY CHARLES MOUTON-DUGASSEAU



 CHARLES MOUTON-DUGASSEAU (1812- 1883)
Mount Vesuvius (1,281m - 4,203ft)
Italy

In La Baie de Naples avec une éruption du Vésuve sous la neige,
6 January 1836,(Bay of Naples with Mount Vesuvius Erupting and Covered in Snow), 6 Janvier 1836,
Gouache on paper 42.7cm x 63.3cm.
Private collection

The artist
Charles Dugasseau, born Charles-Alexandre-Ernest Mouton or Mouton-Dugasseau  was a painter, designer and curator of the Tessé Museum in Le Mans. After making his debut at Le Mans in 1836, Charles Dugasseau spent seven years in Italy in Rome. Student of Ingres who describes him as his friend, and who invites him to come and listen to music until the end of his days. His Sapho exhibited at the Salon in 1845, with Christ surrounded by the founders of the religion, was noticed by Francis Wey, Théophile Gautier and Charles Baudelaire who made this comment: “Serious painting, but pedantic - looks like a very solid Lehmann. His Sapho making the leap of Lefkada is a pretty composition ”.
Nephew of Narcisse Desportes, curator of the Tessé Museum and botanist, Charles Dugasseau replaced him in 1856. He increased the museum's collection by making purchases, in particular twenty-three works by Italian primitives acquired during the sale after the death of a collector from Manceau, Évariste Fouret (1807-1863). He requests deposits from the French State and makes or has made many copies of paintings by Leonardo da Vinci, (Joconda), Bernardino Luini, Francesco Melzi (Flora ou Colombine or La Dame au jasmin), Andrea Solari (The Virgin with the Green Cushion).
The second part of his career was devoted to landscape painting.

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.

_______________________________
2020 - Wandering Vertexes...
by Francis Rousseau

Tuesday, January 28, 2020

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

Sunday, November 24, 2019

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.

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

Thursday, August 8, 2019

VESUVIUS PAINTED BY THOMAS JONES


THOMAS JONES (1742-1803) 
Mount Vesuvius (1,281m - 4,203ft)
Italy

In Mount Vesuvius from Torre dell Annunziata  oil on canvas, 1783, Tate Gallery 


The painter
Thomas Jones was a Welsh landscape painter, the pupil of Richard Wilson. He  was best known in his lifetime as a painter of Welsh and Italian landscapes in the style of his master. However, Jones's reputation grew in the 20th century when more unconventional works by him, not originally intended for exhibition, came to light. Most notable among these is a series of views of Naples which he painted from 1782 to 1783. By breaking with the conventions of classical landscape painting in favour of direct observation, they look forward to the work of Camille Corot and the Barbizon School in the 19th century.
Jones made his first visit to Naples in September 1778, staying there for five months. He returned to Rome for a time, living in a house near the Spanish Steps built by Salvator Rosa.  He took on a Danish widow called Maria Moncke as his "Maid Servant" in April 1779, eloping with her to Naples a year later. Then the largest city in Italy, Naples promised more opportunities for patronage than had Rome, and Jones sought the patronage of the British Ambassador Sir William Hamilton in particular.Maria gave birth to two daughters in Naples, Anna Maria (in 1780) and Elizabetha (in 1781). His autobiography, Memoirs of Thomas Jones of Penkerrig, went unpublished until 1951 but is now recognised as an important source of information on the 18th-century art world.

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.
___________________________________________
2019 - Wandering Vertexes...
by Francis Rousseau 




Sunday, June 2, 2019

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 

Tuesday, May 21, 2019

MOUNT VESUVIUS PAINTED BY AUGUSTE RENOIR


PIERRE-AUGUSTE RENOIR (1841-1919)
Mount Vesuvius (1, 281m - 4,203 ft current)
Italy

In The Bay of Naples (1881), Oil on canvas, 59.7 x 81.3 cm. 
The Metropolitan Museum of Art, New York

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.

The painter
Pierre-Auguste Renoir, commonly known as Auguste Renoir was a French artist who was a leading painter in the development of the Impressionist style. Renoir's paintings are notable for their vibrant light and saturated color, most often focusing on people in intimate and candid compositions. The female nude was one of his primary subjects. In characteristic Impressionist style, Renoir suggested the details of a scene through freely brushed touches of color, so that his figures softly fuse with one another and their surroundings.
His initial paintings show the influence of the colorism of Eugène Delacroix and the luminosity of Camille Corot. He also admired the realism of Gustave Courbet and Édouard Manet, and his early work resembles theirs in his use of black as a color. Renoir admired Edgar Degas' sense of movement. Another painter Renoir greatly admired was the 18th-century master François Boucher.
In the late 1860s, through the practice of painting light and water en plein air (outdoors), he and his friend Claude Monet discovered that the color of shadows is not brown or black, but the reflected color of the objects surrounding them, an effect known today as diffuse reflection. Several pairs of paintings exist in which Renoir and Monet worked side-by-side, depicting the same scenes (La Grenouillère, 1869).
 He very rarely painted mountains landscapes like the Mount Sainte Victoire ( a tribute to Cezanne) or the Mount Vesuvius (above).
The works of his early maturity were typically Impressionist snapshots of real life, full of sparkling color and light. By the mid-1880s, however, he had broken with the movement to apply a more disciplined formal technique to portraits and figure paintings, particularly of women. It was a trip to Italy in 1881 when he saw works by Raphael and other Renaissance masters, that convinced him that he was on the wrong path, and for the next several years he painted in a more severe style in an attempt to return to classicism.
After 1890 he changed direction again. To dissolve outlines, as in his earlier work, he returned to thinly brushed color. From this period onward he concentrated on monumental nudes and domestic scenes, fine examples of which are Girls at the Piano, 1892, and Grandes Baigneuses, 1887. The latter painting is the most typical and successful of Renoir's late, abundantly fleshed nudes.
A prolific artist, he created several thousand paintings. The warm sensuality of Renoir's style made his paintings some of the most well-known and frequently reproduced works in the history of art. The single largest collection of his works—181 paintings in all—is at the Barnes Foundation, in Philadelphia.
He was the father of actor Pierre Renoir (1885–1952), filmmaker Jean Renoir (1894–1979) and ceramic artist Claude Renoir (1901–1969). He was the grandfather of the filmmaker Claude Renoir (1913–1993), son of Pierre.
___________________________________________
2019 - Wandering Vertexes...
by Francis Rousseau 

Thursday, April 18, 2019

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 

Tuesday, January 15, 2019

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 

Thursday, November 29, 2018

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 

Friday, July 6, 2018

VESUVIUS PAINTED BY CLAUDE-LOUIS CHATELET



CLAUDE-LOUIS CHATELET (1753-1795)
 Mount Vesuvius (1, 281m - 4,203 ft current)
Italy

In  Vue du Vésuve et de la Baie de Naples, Oil on canvas, 1781, Private collection 

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.
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 french artist Claude-Louis Châtelet,  died guillotined May 7, 1795, is a painter, draftsman and engraver French. He first distinguished himself by his contribution to the monumental work edited by the influential farmer general Jean-Benjamin de La Borde, Topographical Tables of Switzerland, commented by Baron Zurlauben around 1776. Then he became one of the favorite painters of Queen Marie-Antoinette, who commissioned him a number of illustrations of albums depicting the Trianon and its gardens, albums offered by the Queen to her distinguished visitors.
Châtelet is also known for many animated landscapes of Italy and England.
The paintings and drawings of Claude-Louis Châtelet reveal a technique, a talent and a style of a high degree of accomplishment. The characters animating the landscapes blend with charm and poetry in an atmosphere where dense foliage and fertile nature contrast with the geometric mastery of buildings and architectural elements. The games of light and shadow give these paintings a spatial depth and a perspective in which the gaze is lost, going from one group of characters to another and lingering on stair steps or some sumptuous abode. without having breathed the scent of a nature always present and reassuring. This painter, because of his short existence and his political engagements, has left posterity too limited a production to be retained by the history of art as an important figure in the painting of the eighteenth century French. However, his style and mastery, his connections and his talent, could have made, like Hubert Robert, one of the most eminent and endearing painters of this century, if only he had dedicated all his energy to the nobility of his art.