THE REMARKABLES PAINTED BY DORIS LUSK

DORIS LUSK (1916-1990) 

The Remarkables  (2,319 m - 7,601ft) 

New Zealand (South Island)

 In Late afternoon Lake Wakatipu, New Zealand  oil on canvas, 1958, Te Papa Museum

The mountains 
The Remarkables  (2,319 m - 7,601ft)  are a mountain range and skifield in Otago in the South Island of New Zealand. Located on the southeastern shore of Lake Wakatipu,  renowned for its scenic beauty, the range lives up to its name by rising sharply to create an impressive backdrop for the waters. The range is clearly visible from the nearby town of Queenstown.
The highest point in the range is Single Cone (2,319 m). The adjacent Hector Mountains southeast of the Remarkables culminate in Mount Tūwhakarōria (23,07 m).
There are a number of small lakes on the mountains including Lake Alta which forms part of the Remarkables Skifield.
The mountains were named The Remarkables by Alexander Garvie in 1857-58,  allegedly because they are one of only two mountain ranges in the world which run directly north to south.[ An alternate explanation for the name given by locals is that early Queenstown settlers, upon seeing the mountain range during sunset one evening, named them the Remarkables to describe the sight.

The painter
Doris More Lusk was a New Zealand artist and art teacher, potter, university lecturer.  In 1990 she was posthumously awarded the Governor General Art Award in recognition of her artistic career and contributions. Lusk exhibited mainly with The Group in Christchurch in the 1940s and 1950s.  In the 1950s and 1960s her work was regularly included in the Auckland City Art Gallery's annual surveys of recent New Zealand painting. Lusk exhibited mainly with The Group in Christchurch in the 1940s and 1950s.

 In the 1950s and 1960s her work was regularly included in the Auckland City Art Gallery's annual surveys of recent New Zealand painting.
The first retrospective exhibition of Lusk's work was held at the Dunedin Public Art Gallery in 1966.A second retrospective was held at the Dowse Art Museum in 1973. A major exhibition of her landscape works, Landmarks: The Landscape Paintings of Doris Lusk, was held at the Christchurch Art Gallery in 1996, accompanied by a publication with contributions by Lisa Beaven and Grant Banbury.
To mark the centenary of Lusk's birth in 1916, in 2016 exhibitions were held at the Dunedin Public Art Gallery (Doris Lusk 1916-1990) and Christchurch Art Gallery (Doris Lusk: Practical Visionary).

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2019 - Men Portraits 
Un blog de Francis Rousseau

TARANAKI / MT EGMONT PAINTED BY DORIS LUSK

DORIS LUSK (1916-1990) 

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

New Zealand (North Island) 

In Mount Egmont from Opunake, oil on board, 60 x 91,5cm, 1956, Private collection

About the painting
This oil Mt Egmont /Taranaki from Opunake was exhibited in the 1956 Group Show as Mt Egmont from Opunake, identifying the painting's location. From Opunake, on the south western side of Mt Taranaki, the distinctive Franthams Peak is clearly visible and recorded in the painting. Consistent with the artist's life-long interest in built structures and the transformation of landscape through habitation, a railway bridge crossing the Taungatara Stream is centrally placed in the composition. Broadly executed, the rounded, rhythmical landforms in the foreground are lahars, the result of lava flows from an ancient volcanic eruption. Touches of pink amongst the rich ochre foreground are gently reflected in the sky on the left. A line of clouds running horizontally across the sky above the mountain emphasise the expansive, tranquil vista. The painting was formerly owned by the artist Tony Fomison, a student and friend of the artist.

The painter
Doris More Lusk was a New Zealand artist and art teacher, potter, university lecturer.  In 1990 she was posthumously awarded the Governor General Art Award in recognition of her artistic career and contributions.
Lusk exhibited mainly with The Group in Christchurch in the 1940s and 1950s.  In the 1950s and 1960s her work was regularly included in the Auckland City Art Gallery's annual surveys of recent New Zealand painting.
Lusk exhibited mainly with The Group in Christchurch in the 1940s and 1950s.

 In the 1950s and 1960s her work was regularly included in the Auckland City Art Gallery's annual surveys of recent New Zealand painting.
The first retrospective exhibition of Lusk's work was held at the Dunedin Public Art Gallery in 1966.A second retrospective was held at the Dowse Art Museum in 1973. A major exhibition of her landscape works, Landmarks: The Landscape Paintings of Doris Lusk, was held at the Christchurch Art Gallery in 1996, accompanied by a publication with contributions by Lisa Beaven and Grant Banbury.
To mark the centenary of Lusk's birth in 1916, in 2016 exhibitions were held at the Dunedin Public Art Gallery (Doris Lusk 1916-1990) and Christchurch Art Gallery (Doris Lusk: Practical Visionary).

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 m - 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.

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2019 - Wandering Vertexes...

by Francis Rousseau