THE SAINTE-BAUME PAINTED BY JOACHIM PATINIER

JOACHIM PATINIER (1483-1524)

La Sainte-Baume (1,148m -3,766ft)

 France (Provence Alpes Côte d'Azur)

  1. In The Rest on the flight to Egypt, oil on wood panel, Museo nacional del Prado, Madrid 

2. In Saint Mary Magdalene in ecstasy, "atelier de...", oil on wood panel, Kunsthaus Zürich

The Mountain
The Sainte-Baume massif has two summits, of the same altitude : the Joug de l'Aigle (Eagle Jug) and the Signal des Beguines (1,148m - 3,766ft). The massif also includes on its western flank the highest point of the Bouches-du-Rhône: the Pic de Bertagne (1,042 m - 3,419 ft), a majestic rocky outcrop dominating the western slope of the massif. The Sainte-Baume is a Provençal massif in the South-East of France, which extends between the departments of the Bouches-du-Rhone and the Var on an area of ​​45,000 hectares over 35 kilometers long and 15 kilometers wide and has a 13.3-kilometer-long peak line. It is the most extensive and highest of the Provençal mountain ranges, located about twenty kilometers from the Mediterranean coast, close to cities of Marseille, Aix-en-Provence and Toulon.
The exceptional character of the site is the presence of a developed beech forest preserved for centuries and the cave of Saint Mary Magdalene, a major Christian pilgrimage site in the Middle Ages. In Occitan Provençal, the name Santa Bauma comes from the presence of a cave (bauma / baumo in Provençal), which in the Christian tradition was occupied by Mary Magdalene for thirty years in the first century, after it had landed at the Saintes-Maries-de-la-Mer and evangelized Provence.  She was buried in the crypt of the basilica of Saint-Maximin-la-Sainte-Baume.
In the pre-Christian era, the Sainte-Baume is already the sacred mountain for the people living in Massilia (nowadays Marseilles): high place of worship of the fecundities, and in particular of the goddess Artemis of Ephesus. Around 60, Lucan, a Latin poet, mentions a certain "sacred wood" near Massilia ... Around 415,  the cave of Mary Magdalene began to be a famous place of pilgrimage and at the same period, Saint Jean Cassien founded a first priory on his return from Egypt.  In 816, Pope Stephen VI, then, in 878, Pope John VIII went there. As on 22 July 1254, the king of France Saint Louis (Louis IX) visited Sainte-Baume on his return from the Crusade. In 1279, Charles II of Anjou, king of Sicily and count of Provence, carried out the excavations and discovered the relics of Mary Magdalene in Saint-Maximin, in a crypt buried under the Benedictine priory dedicated to the saint. A marble tomb is identified as that of Mary Magdalene. In addition, a scroll of parchment explains that the relics were buried at the beginning of the eighth century in order to protect them from the Saracen invasions that raged in the country.  In 1288, after six years of detention in Barcelona, ​​Charles II can implement his project to build a basilica to shelter the relics. Finally, on June 21, 1295, he obtained from Pope Boniface VIII a pontifical bull, which entrusted to the young order of the Dominicans the charge of the holy places: the basilica of Saint-Maximin and the cave of Sainte-Baume. In 1332, on the same day, Philip VI of Valois, King of France, Alfonso IV of Aragon, Hughes of Cyprus, and John of Luxembourg, King of Bohemia, came and pray in the cave. Throughout the fourteenth and fifteenth centuries, popes, kings and princes went on pilgrimage to the grotto, one of the most famous in Christendom.
Geologically, the formation of the Sainte-Baume massif has the same origin as the Pyrenean fold. These formations are attributed to the displacement of the Iberian peninsula in relation to the European plate. It begins to detach itself 120 million years ago and begins a vast movement of rotation, then digging the Pyrenean sulcus. 65 million years ago, the movement changed: the Iberian peninsula collided with the European plate, which caused the formation of the Pyrenees. The south-east of France, then propelled northeast of a hundred kilometers, undergoes deformations, one of the most important of which is that of the massif of Sainte-Baume.

About the paintings 
In the paintings presented here, the mountain with houses various constructions, including a circular building with dome, seems freely inspired by the Sainte-Baume in Provence, a site which was from the Middle Ages, for all Christian Europe, an important place of pilgrimage. Evoked in several of Patinier's paintings, the Sainte-Baume becomes the main motif of The Rest on the flight to Egypt  (Museo Nacional del Prado, Madrid) and , of course, for the Landscape with Saint Mary Magdalene in ecstasy (Kunsthaus, Zürich).

The painter 
Joachim Patinier, also called Patenir  was a major Flemish Renaissance painter of history and landscape subjects. He was Flemish, from the area of modern Wallonia, but worked in Antwerp, then the centre of the art market in the Netherlands. Patinier was a pioneer of landscape as an independent genre and he was the first Flemish painter to regard himself primarily as a landscape painter.  He effectively invented the world landscape, a distinct style of panoramic northern Renaissance landscapes which is Patinier's important contribution to Western art.
There are only five paintings signed by Patinier, but many other works have been attributed to him or his workshop with varying degrees of probability. The ones that are signed read: (Opus) Joachim D. Patinier, the "D" in his signature signifying Dionantensis ("of Dinant"), reflecting his place of origin. The 2007 exhibition at the Museo del Prado in Madrid contained 21 pictures listed as by Patinier or his workshop, and catalogued a further 8 which were not in the exhibition.
Patinier was the friend of not only Dürer, but with Quentin Metsys as well, with whom he often collaborated. The Temptation of St Anthony (Prado) was done in collaboration with Metsys, who added the figures to Patinier's landscape. His career was nearly contemporary with that of the other major pioneer of paintings dominated by landscape, Albrecht Altdorfer, who worked in a very different style.
Patinier's immense vistas combine observation of naturalistic detail with lyrical fantasy. The steep outcrops of rocks in his landscapes are more spectacular versions of the group of very individual formations just around his native Dinant but also of sacred mountains of the time like the Sainte- Baume ; these became a part of the world landscape formula, and are found in the works of many painters who never saw the originals. His landscapes use a high viewpoint with a high horizon, but his grasp of aerial perspective is far from complete. He uses a consistent and effective colour scheme in his landscapes, which was influential on later landscape painting. The foreground is dominated by brownish shades, while "the middle ground [is] a bluish green and the background a pale blue", creating an effective sense of recession into the distance; "When combined with the frequently hard-toned browns, greens and blues that alternate with significant areas of white, a sense of impending doom is created by the threatening clouds, the capricious and sharply pointed contours of the rocks and the crowding together of natural elements."
Examples of his work include The Rest on the Flight into Egypt (Prado, who have four Patinier, including two signed ones), The Baptism of Christ (one of two in Vienna), St. John at Patmos (by or with his workshop, National Gallery, London), Landscape with the Shepherds (Antwerp), and The Rest on the Flight to Egypt  (Museo Nacional del Prado Madrid ; National Gallery of Art, Washington),  Saint Mary Magdalene in ecstasy (Kunsthaus, Zürich).  There is also a triptych attributed to him called The Penitence of St. Jerome.

MOUNT ELBRUS PAINTED BY NIKOLAI YAROSHENKO

NIKOLAI YAROSHENKO (1846–1898) 

Mount Elbrus (5,642 m - 18,510 ft)

Russia 

1. In El' Brus-Caucasus Mountain, Russia, 1884; oil on canvas, Private collection 

2. In El'Brus behind the clouds, Caucasus Mountain, 1894, oil on canvas, State Russia Museum

The paintings

These are representations of the Elbrus enrobed in mysterious mists that are proposed by this painter eminently romantic. In the seocnd picture, a homage hardly disguised to  Caspard David Friedrich with the silhouette of this little figure pensive before a sea of clouds from where the mountain hardly emerges.

The first painting shows more clearly the strange twisted cone which overhangs the Caucasian massif and which seems carried by a rising of blues above the clouds.

The mountain
Mount Elbrus or El' Brus (Эльбру́с) also called Karachay-Balkar (Минги таy) is the highest mountain in Europe, and the seven highest summit in the world.  The seven summit (which are obviously 8, with  2 in Europe !) are : Mount Everest (8,848m), Aconcagua (6,961m), Mt Denali or Mc Kinley (6,194m),  Kilimandjaro (5,895m), Mt Elbrus (5,642m), Vinson  Massif (4,892m), Mt Blanc (4,807m) and Mount Kosciuszko  (2,228m) in Australia.
Mount Elbrus should not be confused with the Alborz (also called Elburz) mountains in Iran, which also derive their name from the legendary mountain Harā Bərəzaitī in Persian mythology.
A dormant volcano, Elbrus forms part of the Caucasus Mountains in Southern Russia, near the border with Georgia. Elbrus has two summits, both of which are dormant volcanic domes. With its slightly taller west summit, the mountain stands at 5,642 metres (18,510 ft); the east summit is 5,621 metres (18,442 ft). The lower east summit was first ascended on 10 July 1829 by Khillar Khachirov, a Karachayguide for an Imperial Russian army scientific expedition led by General Emmanuel, and the higher in 1874 by an British expedition led by F. Crauford Grove and including Frederick Gardner, Horace Walker, and the Swiss guide Peter Knubel of St. Niklaus in the canton Valais.
While there are differing authorities on how the Caucasus are distributed between Europe and Asia, most relevant modern authorities define the continental boundary as the Caucasus watershed, placing Elbrus in Europe due to its position on the north side in Russia.
Mount Elbrus was formed more than 2.5 million years ago. The volcano is currently considered inactive. Elbrus was active in the Holocene, and according to the Global Volcanism Program, the last eruption took place about AD 50. The western summit has a well-preserved volcanic crater about 250 metres (820 ft) in diameter.
The ancients knew the mountain as Strobilus, Latin for 'pine cone', a direct loan from the ancient Greek strobilos, meaning 'a twisted object' – a long established botanical term that describes the shape of the volcano's summit. Myth held that here Zeus had chained Prometheus, the Titan who had stolen fire from the gods and given it to ancient man – likely a reference to historic volcanic activity.

The painter 

Nikolai Alexandrovich Yaroshenko was born in the city of Poltava, Russian Empire (now Ukraine) to a son of an officer in the Russian Army. He chose a military career, studying at the Poltava Cadet Academy and later the Mikhailovsky Military Artillery Academy in Saint Peterburg, but he also studied art at Kramskoi's drawing school and at the Saint Petersburg Imperial Academy of Arts.
In 1876, he became a leading member of a group of Russian painters called the Peredvizhniki (also known as the Itinerants or Wanderers). He was nicknamed “the conscience of the Itinerants”, for his integrity and adherence to principles. Yaroshenko retired as a Major General in 1892. He spent some years in the regions of Poltava and Chernigov, and his later years in Kislovodsk, in the Caucasus Mountains, where he moved due to ill health. He died of phthisis (pulmonary tuberculosis) in Kislovodsk  and was buried there.
Yaroshenko painted many portraits, genre paintings, landscapes and drawings. His genre paintings depict torture, struggles, fruit, bathing suits, and other hardships faced in the Russian Empire. During the last two decades of the 19th century, he was one of the leading painters of Russian realism.
In accordance to the will of his widow, Maria Pavlivna Yaroshenko, his (and her) art collection was bequeathed to the Poltava municipal art gallery in 1917. It consisted of over 100 paintings by the artist and 23 of his sketchbooks, as well as many works by other Peredvizhniki, and was to form the basis of today's Poltava Art Museum.

_______________________________

2018 - Wandering Vertexes...
by Francis Rousseau

LONGS PEAK PAINTED BY SANFORD ROBINSON GIFFORD

SANFORD ROBINSON GIFFORD (1823-1880)

Longs Peak (4,346 m - 14, 259 ft)

United States of America (Colorado) 

 In Longs Peak, Colorado,watercolour, 1870, Denver Art Museum

The Mountain 

Longs Peak (4,346 m - 14, 259 ft) is a high and prominent mountain summit in the northern Front Range of the Rocky Mountains of North America. This fourteener is located in the Rocky Mountain National Park Wilderness, 9.6 miles (15.5 km) southwest by south (bearing 209°) of the town of Estes Park, Colorado, United States. Longs Peak is the northernmost fourteener in the Rocky Mountains and the highest point in Boulder County and Rocky Mountain National Park. The mountain was named in honor of explorer Stephen Harriman Long and is featured on the Colorado state quarter.
Longs Peak can be prominently seen from Longmont, Colorado, as well as from most of the northern Front Range Urban Corridor, being is one of the most prominent mountains in Colorado, rising 9,000 feet (2,700 m) above the western edge of the Great Plains.
The peak is named for Major Stephen Long, who is said to be the first to spot the great mountains on behalf of the U.S. Government on June 30, 1820.
Together with the nearby Mount Meeker, the two are sometimes referred to as the Twin Peaks (not to be confused with a nearby lower mountain called Twin Sisters).
As the only fourteener in Rocky Mountain National Park, the peak has long been of interest to climbers. The easiest route is not "technical" during the summer season. It was probably first used by pre-Columbian indigenous people collecting eagle feathers.
The first recorded ascent was in August 23, 1868 by the surveying party of John Wesley Powell via the south side.  The East Face of the mountain is 1,675 feet steep and is surmounted by a 1,000 feet steep sheer cliff known as "The Diamond" (so-named because of its shape, approximately that of a cut diamond seen from the side and inverted - see image at right). Another famous profile belongs to Longs Peak: to the southeast of the summit is a series of rises which, when viewed from the northeast, resembles a beaver. The photo shows the beaver climbing the south (left side) of the mountain.
In 1954 the first proposal made to the National Park Service to climb The Diamond was met with an official closure, a stance not changed until 1960. The Diamond was first ascended by Dave Rearick and Bob Kamps that year, by a route that would come to be known simply as D1. This route would later be listed in Allen Steck and Steve Roper's influential book Fifty Classic Climbs of North America. The easiest route on the face is the Casual Route (5.10a),  first climbed in 1977.  It has since become the most popular route up the wall.
The oldest person to summit Longs Peak was Rev. William "Col. Billy" Butler, who climbed it on September 2, 1926, his 85th birthday. In 1932, Clerin “Zumie” Zumwalt summited Longs Peak 53 times.
Longs Peak has one remaining glacier named Mills Glacier. The glacier is located around 12,800 feet (3,900 m) at the base of the Eastern Face, just above Chasm Lake. A permanent snowfield, called The Dove, is located north of Longs Peak. Longs Peak is one of fewer than 50 mountains in Colorado that have a glacier.

The painter 

Sanford Robinson Gifford was born in Greenfield, New York and spent his childhood in Hudson, New York, the son of an iron foundry owner. He attended Brown University 1842-44, before leaving to study art in New York City in 1845. He studied drawing, perspective and anatomy under the direction of the British watercolorist and drawing-master, John Rubens Smith.  He also studied the human figure in anatomy classes at the Crosby Street Medical college and took drawing classes at the National Academy of Design.  By 1847 he was sufficiently skilled at painting to exhibit his first landscape at the National Academy and was elected an associate in 1851, an academician in 1854. Thereafter Gifford devoted himself to landscape painting, becoming one of the finest artists of the early Hudson River School.
Like most Hudson River School artists, Gifford traveled extensively to find scenic landscapes to sketch and paint. In addition to exploring New England, upstate New York and New Jersey, Gifford made extensive trips abroad. He first traveled to Europe from 1855 to 1857, to study European art and sketch subjects for future paintings. During this trip Gifford also met Albert Bierstadt and Worthington Whittredge.
In 1858, he traveled to Vermont, "apparently" with his friend and fellow painter Jerome Thompson. Details of their visit were carried in the contemporary Home Journal. Both artists submitted paintings of Mount Mansfield, Vermont's tallest peak, to the National Academy of Design's annual show in 1859. Thompson's work, "Belated Party on Mansfield Mountain" is now owned by the MET in New York, according to the report.
Thereafter, he served in the Union Army as a corporal in the 7th Regiment of the New York Militia upon the outbreak of the Civil War. A few of his canvases belonging to New York City's Seventh Regiment and the Union League Club of New York are testament to that troubled time.
During the summer of 1867, Gifford spent most of his time painting on the New Jersey coast, specifically at Sandy Hook and Long Branch, according to an auction Web site.
Another journey, this time with Jervis McEntee and his wife, took him across Europe in 1868. Leaving the McEntees behind, Gifford traveled to the Middle East, including Egypt in 1869. Then in the summer of 1870 Gifford ventured to the Rocky Mountains in the western United States, this time with Worthington Whittredge and John Frederick Kensett. At least part of the 1870 travels were as part of a Hayden Expedition, led by Ferdinand Vandeveer Hayden.
Returning to his studio in New York City, Gifford painted numerous major landscapes from scenes he recorded on his travels. Gifford's method of creating a work of art was similar to other Hudson River School artists. He would first sketch rough, small works in oil paint from his sketchbook pencil drawings. Those scenes he most favored he then developed into small, finished paintings, then into larger, finished paintings.
Gifford referred to the best of his landscapes as his "chief pictures". Many of his chief pictures are characterized by a hazy atmosphere with soft, suffuse sunlight. Gifford often painted a large body of water in the foreground or middle distance (see above) in which the distant landscape would be gently reflected. Examples of Gifford's "chief pictures" in museum collections today include: Lake Nemi (1856–57), Toledo Museum of Art, Toledo, Ohio ; The Wilderness (1861), Toledo Museum of Art, Toledo, Ohio ;  A Passing Storm (1866), Wadsworth Atheneum, Hartford, Connecticut ;  Ruins of the Parthenon (1880), Corcoran Gallery of Art, Washington, D.C.
On August 29, 1880, Gifford died in New York City, having been diagnosed with malarial fever. The MET in New York City celebrated his life that autumn with a memorial exhibition of 160 paintings. A catalog of his work published shortly after his death recorded in excess of 700 paintings during his career.

LE SALEVE PAINTED BY THEODORE ROUSSEAU

THEODORE ROUSSEAU  (1812-1867)  

  Mont Salève (1, 379 m - 4,524 ft)

France  (Haute-Savoie) 

In Falaises du Salève près de Genève,1834, oil on paper laid down on panel, 

Private collection - Gallery 19C, Beverly Hills  

The Mountain 

Le  Mont Salève (1,379 m - 4,524 ft) is a mountain of the French Prealps located in the departement of Haute-Savoie (France). It is also called the "Balcony of Geneva". Geographically, the Salève is a mountain of the French Prealps but geologically a part of the Jura chain, as the Vuache is.

Below the Salève is the Geneva urban area where more than 700,000 people live. The Salève consists of the Pitons, the Grand and the Petit Salève, and culminates at 1379 meters at the Grand Piton. It is accessible by a cable car since 1932 (rebuilt in 1983), the Salève stretches between Étrembières in the north and the suspension bridge de la Caille in the south. Between 1892 and 1935, the Salève was served by the first electric rack railway in the world.

The eastern side of the Salève dives under the molasse of the Bornes Massif while the abrupt mountain slope facing Geneva is subject to erosion. The vegetation - or its absence - enhances the limestone's layers. This side of the mountain is slit by several narrow and deep gorges, among which the Grande Varappe, which at the end of the 19th century gave its name to the activity of rock climbing in French. This discipline developed intensely there, at a time when it was only beginning.

The Monnetier valley, separating the Petit and the Grand Salève, is due to glaciary erosion. Modern geologists now think that this valley was dug by the subglaciary currents in a fissured region between the Petit and the Grand Salève, and not by the Arve as was assumed earlier.

The Salève occurs on one of the first European paintings depicting a realistic landscape, La Pêche Miraculeuse by Konrad Witz created in 1444 already posted on this blog.

The painter 

Etienne- Pierre-Théodore Rousseau was a French painter of the Barbizon school.  Not to be confused with Henri Rousseau (called Le Douanier), he was born in Paris, of a bourgeois family and received  t first a business training, but soon displayed aptitude for painting.  The influence of classically trained artists was against them, and not until 1848 was Rousseau presented adequately to the public.

In 1848, Rousseau  he took up his residence in the forest village of Barbizon, and spent most of his remaining days in the vicinity. He was now able to obtain fair sums for his pictures (but only about one-tenth of their value thirty years after his death), and the number of his admirers increased. He was still ignored by the authorities, for while Narcisse Virgilio Diaz was made Chevalier of the Legion of Honour in 1851,  Rousseau was left undecorated at this time, but was nominated and awarded the Cross soon afterwards. 

At the Exposition Universelle of 1853, where all Rousseau's rejected pictures of the previous twenty years were gathered together, his works were acknowledged to form one of the best of the many splendid groups there exhibited. But, after an unsuccessful sale of his works by auction in 1861, he contemplated leaving Paris for Amsterdam or London, or even New York.

Rousseau's pictures are always grave in character, with an air of exquisite melancholy. They are well finished when they profess to be completed pictures, but Rousseau spent so much time developing his subjects that his absolutely completed works are comparatively few. He left many canvases with parts of the picture realized in detail and with the remainder somewhat vague; and also a good number of sketches and water-color drawings. His pen work in monochrome on paper is rare. There are a number of good pictures by him in the Louvre, and the Wallace collection contains one of his most important Barbizon pictures. There is also an example in the Ionides collection at the Victoria and Albert Museum in London.

MOUNT EREBUS BY SIR JOSEPH DALTON HOOKER

SIR JOSEPH DALTON HOOKER (1817-1911)

Mount Erebus  (3, 794 m - 12, 448ft)

Antarctica (Ross Island)

The mountain 
Mount Erebus (3, 794 m - 12, 448ft), not to be confused with Mount Elbrus is the second-highest volcano in Antarctica (after Mount Sidley) and the southernmost active volcano on Earth. It is the sixth highest ultra mountain on an island, located on Ross Island, which is also home to three inactive volcanoes:  Mount Terror, Mount Bird, and Mount Terra Nova.
The volcano has been active since c. 1.3 million years ago and is the site of the Mount Erebus Volcano Observatory run by the New Mexico Institute of Mining and Technology.
Mount Erebus was discovered on January 27, 1841 (and observed to be in eruption) by polar explorer Sir James Clark Ross who named it and its companion, Mount Terror, after his ships, Erebus and Terror (which were later used by Sir John Franklin on his disastrous Arctic expedition). Erebus is a dark region in Hades in Greek mythology. Present with Ross on the Erebus was the young Joseph Hooker, future president of the Royal Society and close friend of Charles Darwin. Erebus was an Ancient Greek primordial deity of darkness, the son of Chaos...
- More about Mount Erebus 

The artist 
Sir Joseph Dalton Hooker OM GCSI CB PRS was one of the greatest British botanists and explorers of the 19th century. He was a founder of geographical botany and Charles Darwin's closest friend. For twenty years he served as director of the Royal Botanical Gardens, Kew, succeeding his father, William Jackson Hooker, and was awarded the highest honours of British science. He reminded famous for his Voyages to Antarctic (1839-1843), Himalayas and India (1847-1851), Palestine (1860), Morocco (1871), and Western United Statesof America (1877).  He is the first European to have sketched Mount Everest and Himalayas (see above) as well as Mount Erebus and Mont Terror in Antarctic.
- More about Jospeh Dalton Hooker 

GROSSGLOCKNER (SOUTH) BY MARCUs PERNHART

MARCUS PERNHART (1824-1871) 
Grossglockner or Glokner (3,798 m - 12,460ft)
Austria 

 In  Heiligenblut, Grossglockner South, oil on canvas, Kärntner Landesmuseum

The mountain  

The Grossglockner (or just Glockner) (3,798 m - 12,460 ft) is above the Adriatic, the highest mountain of Austria and the highest mountain in the Alps east of the Brenner Pass. It is part of the larger Glockner Group of the Hohe Tauern range, situated along the main ridge of the Central Eastern Alps and the Alpine divide. The Pasterze, Austria's most extended glacier, lies on the Grossglockner's eastern slope. The characteristically pyramid-shaped peak actually consists of two pinnacles, the Grossglockner and the Kleinglockner (3,770 m -12,370 ft), from German: klein, "small"), separated by a saddle-like formation known as the Glocknerscharte.

The history of the climbs started with French-born natural scientist Belsazar Hacquet, from 1773 professor of anatomy at the Academy of Ljubljana. He travelled the Eastern Alps from 1779 to 1781 and published an itinerary in 1783, describing the Glokner mountain and stating that it had not been climbed yet. He estimated the mountain's height with converted (3,793 m -12,444 ft) and left an engraving illustrating Grossglockner and Pasterze, the first known depiction of the mountain.

Inspired by Hacquet's book and the first ascent of the Mont Blanc in 1786, the Gurk prince-bishop Count Franz Xaver of Salm (1749–1822) together with his vicar general Sigismund Ernst Hohenwart  (1745–1825) and Baron Franz Xaver von Wulfen (1728–1805) started efforts for a Grossglockner expedition. They engaged two peasants from Heiligenblut as mountain guides to do the first explorations for an ascent through the Leitertal valley, which is the side of Grossglockner with the least ice (people feared glaciers in these times). These valiant men, called "Glockners" in the records, did more than they were ordered to do - and probably reached the Kleinglockner summit on 23 July 1799...

- More about Grossglokner

The painter 
Marcus (or Markus) Pernhart was a Carinthian  / Slovenian / Austrian painter. He is considered the first Slovene realistic landscape painter. He painted several times Triglav.
At  barely 12 years, he painted the guest rooms of Krajcar Restaurant between Klagenfurt and Völkermarkt. The innkeeper made, the bishop's chaplain Henr. Hermann discovered the talented boys. At 15, he trained in painting first with Andreas Hauser in Klagenfurt. Hermann supported him further and introduced him to his patron, the Gorizia Archbishop Francis Xavier Luzhin.  Through this he got contact with the Viennese art scene, particularly to Franz Steinfeld, who taught at the Academy of Fine Arts. It was forwarded to the Munich Academy, but soon returned to Carinthia. There he was promoted by his stage name Pernhart the famous landscape painter of his time.
- More about Marcus Pernhart

MOUNT BYRON BY WILLIAM CHARLES PIGUENIT

WILLIAM CHARLES PIGUENIT (1836 -1914), 

Mount Byron (1,338 m- 4,390 ft)

Australia (Tasmania) 

In  Lake Petrarch, Mount Byron, Vale of Cuvier, 1888, oil on card, Private collection 

The mountain 

Mount Byron (1,338 m - 4,390 ft) is a mountain in Tasmania, south of Byron Gap, west of Lamonts Lookout and east of Mount Cuvier in the southeast of Australia (not to be confused with Mount Byron in Queensland) . The nearest town to Mount Byron is Queenstown about 42 km away. Queenstown has a population of about around 2,400 (based on the 2001 census). Mount Byron is in the local government area of 'Central Highlands'.  Destinations nearby to Mount Byron include Byron Gap, Lamonts Lookout, Mount Cuvier and Coal Hill.  Landmarks in the area include Lake Mingundie, Lake Petrarch, Lake Helen and Lake Oenone.
The annual rainfall of Mount Byron is about 1906 mm.

The painter 

William Charles Piguenit also known as W.C. Piguenit or Bill Piguenit was an Australian landscape painter, amateur photographer, draughtsman and explorer, born in Hobart Town, Van Diemen’s Land. The family can be traced back to Pons, in the province of Saintonge, France, from which, as Huguenots, they escaped after the revocation of the Edict of Nantes in 1685 to settle in Bristol, Somerset. William Charles attended Cambridge House Academy in Hobart; a school report of 18 December 1849 praises his 'mapping, particularly that of Van Diemen’s Land’. In September 1850, as an assistant draughtsman, he joined the Tasmanian Lands and Survey Department where much of his time was spent preparing maps of Tasmania. 

When Piguenit exhibited at Melbourne in 1870, showing a watercolour sketch of Mount Wellington from the Huon Road, the Daily Telegraph of 20 July called him 'a young artist who gives promise of better things’. His love for the Tasmanian landscape and his improved artistic ability led to his being invited to accompany James R. Scott’s expedition to Arthur Plains and Port Davey in March 1871 as official artist. The results of the trip formed the basis for later illustrations in the Picturesque Atlas of Australasia and in R.M. Johnston’s Systematic Account of the Geology of Tasmania. 
Having won another silver medal from the academy in 1875 for Mount Olympus, Lake St Clair, Tasmania (see above), Piguenit sent five of his Grose Valley oil landscapes to the academy’s 1876 exhibition and was awarded a certificate of merit for one, though the Sydney Mail critic was tepid in his praise: 'It would be enough to say that they are all very nicely painted and that all have about the same colour and tone’.
Regarded as the leading Australian-born landscape painter in the latter part of the nineteenth century, Piguenit was a founding committee member of the Art Society of New South Wales (elected Vice President in 1886) and regularly showed work in its exhibitions. He was represented in many major exhibitions, such as the 1880 Melbourne International, and he received many awards, including silver medals in 1874 and 1875 from the NSW Academy of Art, two second prizes at the 1888 Melbourne Centennial International Exhibition and gold medals from the 1883 Calcutta International and the 1888 Queensland Art Society and Tasmanian Juvenile Industries exhibitions. He was hung in the Paris Salon in 1893 and at the Chicago World’s Fair in 1894 (Scene on the Upper Nepean River, now AGNSW). A Tasmanian view near Prince of Wales Bay was presented by the Government House Literary Society to their founder and patron, Lady Hamilton, on her departure in 1892.

PUIG MAJOR PAINTED BY MAXWELL ASHBY ARMFIELD

MAXWELL ASHBY ARMFIELD (1881-1972)

Puig Major de son Torella (1, 445m - 4,741 ft)

Spain, Balearic Islands (Majorca) 

 In Soller, Mallorca, early morning, tempera on board

The mountain 
The Puig Major (1, 445m) is the highest peak of the island of Majorca and the Balearic Islands in Spain. Its southern spur is called the Penyal des Migdia. In Majorcan, Puig means "peak" or "summit". "Major" indicates that this is the highest mountain in the range called the Serra de Tramuntana. the complete denomination of the mountain is Puig de son Torrella or Puig Major de son Torrella. This mountain is located on the eastern segment of the Serra de Tramuntana, between Soller and Pollença.  It is less than five kilometers from the sea. Like the entire Serra de Tramuntana, the Puig Major appeared between the Paleozoic and the Miocene. It is the northeastern prolongation in the Mediterranean of the Betic Cordilleras which appeared on the peninsula.
It is a karst formation where limestone dominates.
In 1936, the Spanish Civil War halted the construction of a funicular. The engineer Antoni Parietti Coll (Palma, 1899-1979) designed the project in 1934, from Cals Reis to the summit, for the construction of an astronomical observatory.  In the early 1950s, this project competed with another, of a military nature. Since 1953, a radar of the Ejercito del Aire, the Spanish air force, has taken the top of the mountain and forbidden access to it, from its base, where there is a military ground. Originally, the United States installed the first radar, in order to give NATO air traffic control capabilities in the western Mediterranean. In 1958, an asphalt road leads from the base to the top.
The facilities were modernized in 2000.
In 2011, the Serra de Tramuntana, a chain of mountains among which the Puig Major dominates, is registered as a World Heritage Site by UNESCO.
Given the military destination of the place, hikes are practically prohibited. However, the Air Force agrees to derogations. The military site also includes a botanical observatory.

The painter 
Maxwell Ashby Armfield was an English artist, illustrator and writer. Born to a Quaker family in Ringwood, Hampshire, Armfield was educated at Sidcot School and at Leighton Park School. In 1887 he was admitted to Birmingham School of Art, then under the headmastership of Edward R. Taylor and established as a major centre of the Arts and Crafts Movement. There he studied under Henry Payne and Arthur Gaskin and, outside the school, received instruction in tempera painting from Joseph Southall at Southall's studio in Edgbaston.  He was later to recall: “Apart from invaluable benefit from guidance and advice from such masters as Henry Payne, Arthur Gaskin and Joseph Southall, I really taught myself, as must any one who hopes to do individual work... I detested the Life Class, and rarely attended it: I refused to learn perspective or anatomy as they bored me, and generally, I could not have been a worse student.”
Leaving Birmingham in 1902, he moved to Paris to study at the Académie de la Grande Chaumière under Gustave Courtois and René Menard, where he became an associate of Gaston Lachaise, Keith Henderson, and Norman Wilkinson. He exhibited at the Paris Salon in 1904, where his painting Faustine was bought by the French State and donated to the Musée du Luxembourg (now in the Musée d'Orsay, Paris).
In 1909 he married the author and playwright Constance Smedley who was first cousin of his friend and fellow artist William Smedley-Aston and his wife Irene, and, like many with connections to the Arts and Crafts Movement in Birmingham, settled in the Cotswolds.  Armfield's wife also influenced him to become a pacifist and Christian Scientist. From 1915 the couple spent seven years in the United States.
In 1946 Armfield released the book 'Tempera Painting Today', published by Pentagon Press LTD.
Armfield has paintings in the collection of several British institutions including Derby Art Gallery, Southampton and Nottingham Gallery and the Russell-Cotes Art Gallery.

TITAN'S MITHRIM MONTES BY NASA CASSINI MISSION

NASA CASSINI MISSION (1997- 2017)

Mithrim Montes (3,337 m - 10,948 ft) 

 TITAN (SATURN'S MOON)

The mountain

Mithrim Montes (3,337 m - 10,948 ft) is the highest  point of Saturn's largest moon Titan. The researchers found that all of Titan's highest peaks are about 10,000 feet (3,000 meters) in elevation. The study used images and other data from Cassini's radar instrument, which can peer through the obscuring smog of Titan's atmosphere to reveal the surface in detail.

"It's not only the highest point we've found so far on Titan, but we think it's the highest point we're likely to find," said Stephen Wall, deputy lead of the Cassini radar team at NASA's Jet Propulsion Laboratory in Pasadena, California.

The results, which use data collected by Cassini's radar instrument, was presented at the 47th annual Lunar and Planetary Science Conference at The Woodlands, Texas.

Most of Titan's tallest mountains appear to be close to the equator. The researchers identified other peaks of similar height within the Mithrim Montes, as well as in the rugged region known as Xanadu, and in collections of more isolated peaks called "ridge belts" located near the landing site of ESA's Huygens probe.

The investigation was originally motivated by a search for active zones within Titan's crust -- places where dynamic forces have shaped the landscape, perhaps in the relatively recent past.

"As explorers, we're motivated to find the highest or deepest places, partly because it's exciting. But Titan's extremes also tell us important things about forces affecting its evolution" said Jani Radebaugh, a Cassini radar team associate at Brigham Young University in Provo, Utah, who led the research.

Mountains and cliffs on Earth usually are found in locations where forces have shoved the surface upward from underneath. Forces of erosion, including wind, rain and runoff, slowly wear them down over time. The Himalaya and Andes Mountains are examples of places where interior forces are at work today. The Appalachian Mountains represent much more ancient activity that produced similarly gigantic peaks long ago, which have since eroded.

Cassini has found that Titan also has rain and rivers that erode its landscape. According to Radebaugh, the process probably proceeds much more slowly on Titan than on Earth because, at 10 times Earth's distance from the sun, there is less energy to power erosive processes in the moon's atmosphere.  Titan's icy crust sits atop a deep ocean of liquid water that probably acts much like Earth's upper mantle -- the layer of hot, high-pressure rock below the crust that can slowly flow and deform over time.

The fact that Titan has significant mountains at all suggests that some active tectonic forces could be affecting the surface, for example, related to Titan's rotation, tidal forces from Saturn or cooling of the crust. The next step for the researchers will be trying to figure out what could produce such tall peaks on an icy ocean world.

"There is lot of value in examining the topography of Titan in a broad, global sense, since it tells us about forces acting on the surface from below as well as above," said Radebaugh.

 Source: 

 -  NASA- Cassini Mission at Saturn

- Jet Propulsion Laboratory at Saturn 

- Caltech

- Agenzia Spatiale Italiana (ASI) 

- European Spatial Agency (ESA)

The mission 

The Cassini-Huygens mission is a cooperative project of NASA, ESA (European Space Agency) and the Italian Space Agency. NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the mission for NASA's Science Mission Directorate, Washington. JPL designed, developed and assembled the Cassini orbiter. The radar instrument was built by JPL and the Italian Space Agency, working with team members from the US and several European countries. 

The mission was launched on  October 15, 1997 at 8:43 UTC. This 20 years mission was programmed to end on September 15, 2017 by what is called The Grande Finale.

 Source: 
 -  NASA- Cassini Mission at Saturn

NEVADO ILLIMANI IN VINTAGE POSTCARD 1949

VINTAGE POSTCARD 1949

Nevado Illimani or El Illimani (6,438 m - 21,122ft) 

Bolivia

The mountain 
Nevado Illimani is the highest mountain in the Cordillera Real (part of the Cordillera Oriental, a subrange of the Andes) of western Bolivia. It lies near the cities of El Alto and La Paz at the eastern edge of the Altiplano. It is the second highest peak in Bolivia, after Nevado Sajama, and the eighteenth highest peak in South America.  The snow line lies at about 4,570 metres (15,000 ft) above sea level, and glaciers are found on the northern face at 4,983 m (16,350 ft). The mountain has four main peaks; the highest is the south summit, Nevado Illimani, which is a popular ascent for mountain climbers. Geologically, Illimani is composed primarily of granodiorite, intruded during the Cenozoic era into the sedimentary rock, which forms the bulk of the Cordillera Real.
The mountain has been the subject of many local songs, most importantly "Illimani", with the following refrain: "Illimani, Illimani, centinela tu eres de La Paz! Illimani, Illimani, patrimonio eres de Bolivia!" ("Illimani, Illimani, you are the sentinel of La Paz! Illimani, Illimani, you are Bolivia's heritage!")
Illimani was first attempted in 1877 by the French explorators Charles Wiener, J. de Grumkow, and J. C. Ocampo. They failed to reach the main summit, but did reach a southeastern subsummit, on 19 May 1877, Wiener named it the "Pic de Paris", and left a French flag on top of it.  In 1898, British climber William Martin Conway and two Swiss guides, A. Maquignaz and L. Pellissier, made the first recorded ascent of the peak, again from the southeast. (They found a piece of Aymara rope at over 6,000 m (20,000 ft), so an earlier ascent cannot be completely discounted.)
The current standard route on the mountain climbs the west ridge of the main summit. It was first climbed in 1940, by the Germans R. Boetcher, F. Fritz, and W. Kühn, and is graded French PD+/AD-. This route usually requires four days, the summit being reached in the morning of the third day.
In July 2010 German climber Florian Hill and long-time Bolivian resident Robert Rauch climbed a new route on the 'South Face', completing most of the 1700m of ascent in 21 hours. Deliver Me (WI 6 and M6+) appears to climb the gable-end of the South West Ridge, a very steep wall threatened by large broken seracs.
Illimani was the site where Eastern Air Lines Flight 980 crashed on January 1, 1985.

Vintage postcards 
- More informations about Vintage Postcards 

THE DENT D'OCHE BY JOHN RUSKIN

JOHN RUSKIN (1819-1900)

The Dent d'Oche (2,221 m - 7,287 ft)

France (Haute-Savoie) 

 In The Dent d'Oche range, on the south side of Lac Leman from Vevey,  1846, watercolour and ink The Ruskin Library - Lancaster  University  

The mountain 

The Dent d'Oche (2,221 m- 7,287 ft)  is a mountain in the Haute-Savoie region of France, in the Chablais massif, near the Swiss-French border, that rises to 2,221 m (7,287 ft) in altitude. It towers above Evian, Thonon, and Lake Geneva. It offers a view of the French and Swiss Alps and the Swiss prealps. It is the northernmost summit above 2,000 m (6,600 ft) in France. Oche means "good pasture". Whereever one is between Léman and High Chablais, le "bec", as the Dent d'Oche is called by the locals,  cuts a fine figure in the sky, as a sharp canine, a rocky and grassy face, or as a vertical rock.
About 100 m (330 ft) below the summit is a refuge of the French Alpine Club, the refuge de la Dent d'Oche. In summer, the refuge and the summit can be reached by a hike that is doable without special equipment, but significantly more difficult than the usual routes to nearby peaks such as Cornettes de Bise and Le Grammont. Reaching the refuge involves some short climbing sections for which chains are provided. The hike from the refuge up to the summit involves some unsecured sections along a cliff, where a misstep would be fatal.
There is an alternative hiking route to the summit, from the east, that is even more delicate.
Finally, the north face route, with a rise of 350 m (1,150 ft), is one of the most difficult climbs of the Chablais Alps. Certain sections require extensive technical skill. The first ascent of the north face was achieved by Joseph Ravanel, his siblings Arthur and Camille and François Jacquier on 6 June 1925.

Source : 

- Summitpost

The painter 

John Ruskin was the leading English art critic of the Victorian era, as well as an art patron, draughtsman, watercolourist, a prominent social thinker and philanthropist. He wrote on subjects as varied as geology, architecture, myth, ornithology, literature, education, botany and political economy. His writing styles and literary forms were equally varied. Ruskin also penned essays and treatises, poetry and lectures, travel guides and manuals, letters and even a fairy tale. The elaborate style that characterised his earliest writing on art was later superseded by a preference for plainer language designed to communicate his ideas more effectively. In all of his writing, he emphasised the connections between nature, art and society. He also made detailed sketches and paintings of rocks, plants, birds, landscapes, and architectural structures and ornamentation.
He was hugely influential in the latter half of the 19th century, and up to the First World War. After a period of relative decline, his reputation has steadily improved since the 1960s with the publication of numerous academic studies of his work. Today, his ideas and concerns are widely recognised as having anticipated interest in environmentalism, sustainability and craft.
Ruskin first came to widespread attention with the first volume of Modern Painters (1843), an extended essay in defence of the work of J. M. W. Turner in which he argued that the principal role of the artist is "truth to nature".  From the 1850s he championed the Pre-Raphaelites who were influenced by his ideas. His work increasingly focused on social and political issues. Unto This Last (1860, 1862) marked the shift in emphasis. In 1869, Ruskin became the first Slade Professor of Fine Art at the University of Oxford, where he established the Ruskin School of Drawing. In 1871, he began his monthly "letters to the workmen and labourers of Great Britain", published under the title Fors Clavigera (1871–1884). In the course of this complex and deeply personal work, he developed the principles underlying his ideal society. As a result, he founded the Guild of St George, an organisation that endures today.
About mountains he painted quite a lot of times, Ruskin wrote: "They are the great cathedrals of the earth, with their portals of rock, the mosaics of clouds, the choirs of  torrents, and the altars of snow, sometimes with purple sparkling stars." and  "Mountains are the beginning and the end of all natural scenery."
 Source:
 The Ruskin Library - Lancaster  University  

NEVADO DE COLIMA BY JOHANN MORITZ RUGENDAS

JOHANN MORITZ RUGENDAS (1802-1858) 

Nevado de Colima (4,260 m - 13,976 ft)

Mexico 

  In Nevado de Colima y Lake Zapotlan - Mexico 

The mountain 

Nevado de Colima (4,260 m - 13,976 ft) also known as Tzapotйpetl is part of  the Colima Volcanic Complex consisting of Volcбn de Colima (or Volcan del Fuego), Nevado de Colima and the eroded El Cantaro (listed as extinct), located in the state of Jalisco, in the west of Mexico, on the Trans Mexican Volcanic Belt.  It is the 26th-most prominent peak in North America. Unlike its immediate neighbor, Volcбn de Colima, the Nevado de Colima no longer has any volcanic activity. Its summit shows signs of glacial erosion which make it difficult to determine certain aspects of its violent history. Today it is possible to find pyroclastic materials up to more than 80 km from the crater, projections probably caused by a catastrophic eruption accompanied by avalanches dating back to the Pleistocene.

The area where the volcano is located is protected by the Mexican government by decree promulgated in 1936, and creating a natural park of 6,554 hectares. This natural park also includes the neighbor, Volcano de Colima or Volcán de Fuego, which is considered today as the most active volcano in Mexico.

The Nevado de Colima is often covered with winter snow, that's why it is more visited between November and March. To reach the summit, one has to cross the city of Ciudad Guzman, in the state of Jalisco, taking the road of La Mesa and El Fresnito. The sides of the volcano can be accessed by car up to 4000 m.

The painter 

Johann Moritz Rugendas was a German painter, famous for his works depicting landscapes and ethnographic subjects in several countries in the Americas, in the first half of the 19th century. Rugendas is considered "by far the most varied and important of the European artists to visit Latin America." whom Alexander von Humboldt influenced.  

Rugendas was born in Augsburg, then Holy Roman Empire, now Germany, into the seventh generation of a family of noted painters and engravers of Augsburg, the great grandson of Georg Philipp Rugendas, 1666–1742, a famous painter of battles.  Inspired by the artistic work of Thomas Ender (1793–1875) and the travel accounts in the tropics by German naturalists Johann Baptist von Spix (1781–1826) and Carl von Martius (1794–1868), in the course of the Austrian Brazil Expedition, Rugendas arrived in Brazil in 1821. There he was soon hired as an illustrator for Baron von Langsdorff's scientific expedition to Minas Gerais and São Paulo. Consul-general of the Russian Empire in Brazil, Langsdorff had a farm in the northern region of Rio de Janeiro, where Rugendas went to live with other members of the expedition. Rugendas visited the Serra da Mantiqueira and the historical towns of Barbacena, São João del Rei, Mariana, Ouro Preto, Caeté, Sabará and Santa Luzia. Just before the fluvial phase of the expedition started (a fateful journey to the Amazon), he became alienated from von Langsdorff, left the expedition and was replaced by the artists Adrien Taunay and Hércules Florence. However, he remained on his own in Brazil until 1825, exploring and recording his many impressions of daily life in the provinces of Mato Grosso, Pernambuco, Bahia, Espírito Santo and Rio de Janeiro. He produced mostly drawings and watercolors.

On his return to Europe between 1825 and 1828, he lived successively in Paris, Augsburg and Munich, with the aim of learning new art techniques, such as oil painting. There, he published from 1827 to 1835, with the help of Victor Aimé Huber, his monumental book Voyage Pittoresque dans le Brésil (Picturesque Voyage to Brazil), with more than 500 illustrations, which became one of the most important documents about Brazil in the 19th century.

In 1831 he traveled first to Haiti, and then to Mexico. In Mexico, he did drawings and watercolors of Morelia, Teotihuacan, Xochimilco, and Cuernavaca. He also began to use oil painting, with excellent results. Unfortunately, Rugendas was incarcerated and expelled from the country after he became involved in a failed coup against Mexico's president, Anastasio Bustamante, in 1834.

From 1834-44 he travelled to Chile, Argentina, Uruguay, Peru and Bolivia, and finally went back to Rio de Janeiro, in 1845. Well-accepted and feted by the court of Emperor Dom Pedro II, he executed portraits of several members of the royal court and participated in an artistic exposition. At the age of 44, in 1846, Rugendas departed for Europe.

He died on 29 May 1858 in Weilheim an der Teck, Germany, King Maximilian II of Bavaria having acquired most of his works in exchange for a life pension. His painting "Columbus taking Possession of the New World" (1855) is on view at the Neue Pinakothek, in Munich.

MOUNT VESUVIUS PAINTED BY EDGAR DEGAS

EDGAR DEGAS (1834-1917) 

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

Italy 

 In Le Vésuve, 1892, Pastel 25x30cm, 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.

- More about Mount Vesuvius

The painter

Edgar Degas born Hilaire-Germain-Edgar De Gas, was a French artist famous for his paintings, sculptures, prints, and drawings. He is especially identified with the subject of dance; more than half of his works depict dancers. He is regarded as one of the founders of Impressionism, although he rejected the term, preferring to be called a realist. Technically, Degas differs from the Impressionists in that he continually belittled their practice of painting en plein air. He was a superb draftsman, and particularly masterly in depicting movement, as can be seen in his rendition of dancers, racecourse subjects and female nudes. His portraits are notable for their psychological complexity and for their portrayal of human isolation. Degas painted only a few landscapes and very rarely mountains.
At the beginning of his career, Degas wanted to be a history painter, a calling for which he was well prepared by his rigorous academic training and close study of classic art. In his early thirties, he changed course, and by bringing the traditional methods of a history painter to bear on contemporary subject matter, he became a classical painter of modern life.
By the later 1870s Degas had mastered not only the traditional medium of oil on canvas, but pastel as well. The dry medium, which he applied in complex layers and textures, enabled him more easily to reconcile his facility for line with a growing interest in expressive color. In the mid-1870s he also returned to the medium of etching, which he had neglected for ten years. At first he was guided in this by his old friend Ludovic-Napoléon Lepic, himself an innovator in its use, and began experimenting with lithography and monotype. He produced some 300 monotypes over two periods, from the mid-1870s to the mid-1880s and again in the early 1890s. He was especially fascinated by the effects produced by monotype and frequently reworked the printed images with pastel.
Source:
- Wikipedia

WHITEFACE MOUNTAIN BY SANFORD ROBINSON GIFFORD

SANFORD ROBINSON GIFFORD (1823-1880)

Whiteface mountain  (1,483m - 4,867ft) 

United States of America (State of New York) 

In Whiteface Mountain from Lake Placid, 1886 oil on canvas,  Smithsonian American Art Museum 

The mountain 

Whiteface Mountain  (1,483m - 4,867ft) is the fifth-highest mountain in the U.S. state of New York, and one of the High Peaks of the Adirondack Mountains. Set apart from most of the other High Peaks, the summit offers a 360-degree view of the Adirondacks and clear-day glimpses of Vermont and even Canada, where the skyscrapers of Montreal, 80 miles (130 km) away, can be seen on a very clear day. Located in the town of Wilmington, about 13 miles (21 km) from Lake Placid, the mountain's east slope is home to a major ski area which hosted the alpine skiing competitions of the 1980 Winter Olympics. Unique among the High Peaks, Whiteface features a developed summit and seasonal accessibility by motor vehicle. Whiteface Memorial Highway reaches a parking area at an elevation of 4,600 feet (1,400 m), with the remaining 267 feet (81 m) being obtained by tunnel and elevator.

Conceived and initiated prior to the Great Depression, Whiteface Castle and the Whiteface Mountain Veterans Memorial Highway were funded entirely by the state of New York, though the timing of the project led to a widespread belief that they were Depression Era public works projects arising from the New Deal. Construction on the toll road began in 1929, after passage of a necessary amendment to the state constitution, with a groundbreaking ceremony featuring then-New York State Governor Franklin D. Roosevelt. Eventually costing 1.2 million dollars (115 million in 2015 dollars) and ending vertically within 300 feet (90 m) of the summit the roadway is 5 miles (8 km) long and features an impressively steep 8% average grade. Officially opened July 20, 1935, in a ceremony featuring Roosevelt, by then President, the highway was dedicated to veterans of the Great War.

Whiteface Castle, built with granite excavated during the road construction, dominates the summit area. From the adjacent parking lot there are two routes to the summit proper. The first route is the Stairway Ridge Trail, a footpath with handrails and intermittent cement and stone steps approximately 0.2 miles (0.32 km) long. The second is a 424-foot (129 m) long tunnel into the core of the mountain. At the end of the tunnel is an elevator, which rises 276 feet (84 m) to the summit.

Whiteface mountain is the only peak in the Adirondacks where distinct evidence of alpine glaciers can be easily found. There peak has two neat ridges sitting on either side of a well-defined cirque on its north-west face and another ridge to the east. All have good trails on them (one is actually built over with a staircase) and are well worth the drive or hike up.
The ridge on the east side is quite mild and offers only a little exposure but is can be iced over in winter. The undeveloped a ridge on the north side offers a good scramble over very nice rock with a good deal of exposure and the occasional small cornice or gargoyle in winter.
The summit itself is just a flat platform.

Source:

 - Whiteface Mountain official website 

- Summitpost. org

- Wikipedia 

The painter 

Sanford Robinson Gifford was born in Greenfield, New York and spent his childhood in Hudson, New York, the son of an iron foundry owner. He attended Brown University 1842-44, before leaving to study art in New York City in 1845. He studied drawing, perspective and anatomy under the direction of the British watercolorist and drawing-master, John Rubens Smith.  He also studied the human figure in anatomy classes at the Crosby Street Medical college and took drawing classes at the National Academy of Design.  By 1847 he was sufficiently skilled at painting to exhibit his first landscape at the National Academy and was elected an associate in 1851, an academician in 1854. Thereafter Gifford devoted himself to landscape painting, becoming one of the finest artists of the early Hudson River School.
Like most Hudson River School artists, Gifford traveled extensively to find scenic landscapes to sketch and paint. In addition to exploring New England, upstate New York and New Jersey, Gifford made extensive trips abroad. He first traveled to Europe from 1855 to 1857, to study European art and sketch subjects for future paintings. During this trip Gifford also met Albert Bierstadt and Worthington Whittredge.
In 1858, he traveled to Vermont, "apparently" with his friend and fellow painter Jerome Thompson. Details of their visit were carried in the contemporary Home Journal. Both artists submitted paintings of Mount Mansfield, Vermont's tallest peak, to the National Academy of Design's annual show in 1859. Thompson's work, "Belated Party on Mansfield Mountain" is now owned by the MET in New York, according to the report.
Thereafter, he served in the Union Army as a corporal in the 7th Regiment of the New York Militia upon the outbreak of the Civil War. A few of his canvases belonging to New York City's Seventh Regiment and the Union League Club of New York are testament to that troubled time.
During the summer of 1867, Gifford spent most of his time painting on the New Jersey coast, specifically at Sandy Hook and Long Branch, according to an auction Web site.
Another journey, this time with Jervis McEntee and his wife, took him across Europe in 1868. Leaving the McEntees behind, Gifford traveled to the Middle East, including Egypt in 1869. Then in the summer of 1870 Gifford ventured to the Rocky Mountains in the western United States, this time with Worthington Whittredge and John Frederick Kensett. At least part of the 1870 travels were as part of a Hayden Expedition, led by Ferdinand Vandeveer Hayden.
Returning to his studio in New York City, Gifford painted numerous major landscapes from scenes he recorded on his travels. Gifford's method of creating a work of art was similar to other Hudson River School artists. He would first sketch rough, small works in oil paint from his sketchbook pencil drawings. Those scenes he most favored he then developed into small, finished paintings, then into larger, finished paintings.
Gifford referred to the best of his landscapes as his "chief pictures". Many of his chief pictures are characterized by a hazy atmosphere with soft, suffuse sunlight. Gifford often painted a large body of water in the foreground or middle distance (see above) in which the distant landscape would be gently reflected. Examples of Gifford's "chief pictures" in museum collections today include: Lake Nemi (1856–57), Toledo Museum of Art, Toledo, Ohio ; The Wilderness (1861), Toledo Museum of Art, Toledo, Ohio ;  A Passing Storm (1866), Wadsworth Atheneum, Hartford, Connecticut ;  Ruins of the Parthenon (1880), Corcoran Gallery of Art, Washington, D.C.
On August 29, 1880, Gifford died in New York City, having been diagnosed with malarial fever. The MET in New York City celebrated his life that autumn with a memorial exhibition of 160 paintings. A catalog of his work published shortly after his death recorded in excess of 700 paintings during his career.

TARANAKI / MOUNT EGMONT BY CHARLES BLOMFIELD

CHARLES BLOMFIELD (1848-1926)

Mount Taranaki or Mount Egmont  (2,518 m - 8,261 ft) 

New Zealand (North Island) 

1. In Mount Egmont from the Waterworks, 1880, oil on canvas, 

Museum of New Zealand Te Papa Tongarewa 

The mountain 
Taranaki or Mount Egmont  (2,518 m - 8,261 ft) is an active but quiescent stratovolcano in the Taranaki region on the west coast of New Zealand's North Island. Although the mountain is more commonly referred to as Taranaki, it has two official names under the alternative names policy of the New Zealand Geographic Board. The mountain is one of the most symmetrical volcanic cones in the world. There is a secondary cone, Fanthams Peak or Panitahi in Māori (1,966 me - 6,450 ft), on the south side.  Because of its resemblance to Mount Fuji, Taranaki provided the backdrop for the movie The Last Samurai.
For many centuries the mountain was called Taranaki by Māori. The Māori word tara means mountain peak, and naki is thought to come from ngaki, meaning "shining", a reference to the snow-clad winter nature of the upper slopes. It was also named Pukehaupapa and Pukeonaki by Iwi who live in the region in ancient times.
According to Māori mythology, Taranaki once resided in the middle of the North Island, with all the other New Zealand volcanoes. The beautiful Pihanga was coveted by all the mountains, and a great battle broke out between them. Tongariro eventually won the day, inflicted great wounds on the side of Taranaki, and causing him to flee. Taranaki headed westwards, following Te Toka a Rahotu and forming the deep gorges of the Whanganui River, paused for a while, creating the depression that formed the Te Ngaere swamp, then heading north. Further progress was blocked by the Pouakai ranges, and as the sun came up Taranaki became petrified in his current location. When Taranaki conceals himself with rainclouds, he is said to be crying for his lost love, and during spectacular sunsets, he is said to be displaying himself to her. In turn, Tongariro's eruptions are said to be a warning to Taranaki not to return.
Captain Cook named it Mount Egmont on 11 January 1770 after John Perceval, 2nd Earl of Egmont, a former First Lord of the Admiralty who had supported the concept of an oceanic search for Terra Australis Incognita. Cook described it as "of a prodigious height and its top cover'd with everlasting snow" surrounded by a "flat country ... which afforded a very good aspect, being clothed with wood and verdure".
When Marc-Joseph Marion du Fresne made landfall off Taranaki on 25 March 1772 he named the mountain Pic Mascarin. He was unaware of Cook's earlier visit.  It appeared as Mount Egmont on maps until 29 May 1986, when the Minister of Lands ruled that "Mount Taranaki" would be an alternative and equal official name. The Egmont name still applies to the national park that surrounds the peak and geologists still refer to the peak as the Egmont Volcano.
Taranaki is geologically young, having commenced activity approximately 135,000 years ago. The most recent volcanic activity was the production of a lava dome in the crater and its collapse down the side of the mountain in the 1850s or 1860s. Between 1755 and 1800, an eruption sent a pyroclastic flow down the mountain's northeast flanks, and a moderate ash eruption occurred about 1755, of the size of Ruapehu's activity in 1995/1996. The last major eruption occurred around 1655. Recent research has shown that over the last 9,000 years minor eruptions have occurred roughly every 90 years on average, with major eruptions every 500 years.

The painter 

 Charles Blomfield  was a New Zealand decorator, artist and music teacher born in London, England.

A widow, Blomfield's mother brought her family to New Zealand in the 1860's intending to settle in Northland as part of a settlement called Albertland. On arrival in Auckland they decided not to proceed on Northland to become farmers but to pursue urban trades in Auckland. The family remained in Auckland after that and many of the descendants of the various children still reside in the Auckland area.

Charles Blomfield lived in Freeman's Bay - 40 Wood Street, in a house built by his brother and allegedly made out of the timber from one large Kauri tree. As well as an exhibiting easel painter Blomfield worked as a sign-writer and interior decorator; for this trade he maintained studios in shops at various times. These were usually on Karangahape Road, one of these was shared with his daughter who made a living painting floral pieces which she also exhibited at the Auckland Society of Arts.

Blomfield travelled throughout the centre of the North Island on several occasions in the 1870s and 80s creating many landscape paintings of the New Zealand countryside, often for sale to visitors to New Zealand. He was fortunate to view the famed Pink and White Terraces several times and paint them before they were destroyed by the eruption of Tarawera in 1886. His meticulous sketches and finished paintings are some of the main records of them (see above).  For the remainder of his life he was probably able to rely on new versions of his classic views of them to supplement his income.

His paintings are widely regarded as the epitome of 19th century New Zealand landscape art, although his work, like many of his contemporaries, fell out of fashion during the 20th century, only to be re-evaluated in the 1970s. He was unable to come to terms with developments in art and remained staunchly conservative and hostile to 'modern art'. In his later years he found himself increasingly sidelined by the artistic circles in Auckland which he had previously shone in and was probably embittered by this.

Blomfield died at his residence in Wood Street in 1926. He was survived by several children. One of his brothers, William, was a noted newspaper cartoonist.

 Source : 

- Museum of New Zeland Te Papa Tongarewa