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Showing posts with label Brandberg / Omukuruvaro. Show all posts
Showing posts with label Brandberg / Omukuruvaro. Show all posts

Wednesday, January 2, 2019

BRANDBERG / OMUKURUVARO PAINTED BY JACOBUS HENDRIK PIERNEEF


JACOBUS HENDRIK PIERNEEF (1886-1957), 
 The Brandberg  (2,573 m -8,442 ft)
 Namibia  

 In Purple Mountain  oil on board (10, 5 x14 cm), Private collection 

The mountain 
The Brandberg or Omukuruvaro  (2,573 m -8,442 ft)  is Namibia's highest mountain. Brandberg Mountain is located in former Damaraland, now Erongo, in the northwestern Namib Desert, near the coast, and covers an area of approximately 650 km². With its highest point, the Königstein (German for 'King's Stone'), located on the flat Namib gravel plains, on a clear day 'The Brandberg' can be seen from a great distance. There are various routes to the summit, the easiest (also steepest) being up the Ga'aseb river valley, but other routes include the Hungurob and Tsisab river valleys. The nearest settlement is Uis, roughly 30 km from the mountain.
The name Brandberg is Afrikaans, Dutch and German for Burning Mountain, which comes from its glowing color which is sometimes seen in the setting sun. The Damara name for the mountain is Dâures, which means 'burning mountain', while the Herero name, Omukuruvaro means 'mountain of the Gods'.
The Brandberg is a spiritual site of great significance to the San (Bushman) tribes. The main tourist attraction is The White Lady rock painting, located on a rock face with other art work, under a small rock overhang, in the Tsisab Ravine at the foot of the mountain. The ravine contains more than 1 000 rock shelters, as well as more than 45 000 rock paintings.
The Brandberg Massif or Brandberg Intrusion is a granitic intrusion, which forms a dome-shaped massif. It originated during Early Cretaceous rifting that led to the opening of the South Atlantic Ocean. Argon–argon dating yielded intrusive ages of 132 to 130 Ma. Remnants of Cretaceous volcanic rocks are preserved in a collar along the western and southern margins of the massif. The origins of the magmas that formed the Brandberg intrusion are related to emplacement of mantle-derived basaltic magma during continental break-up which led to partial melting of crustal rocks resulting in a hybrid granitic magma. Erosion subsequently removed the overburden rock. Apatite fission track dating indicates approximately 5 km denudation between 80 and 60 Ma.

The painter 
Jacobus Hendrik (Henk) Pierneef (usually referred to as Pierneef)  was a South African landscape artist, generally considered to be one of the best of the old South African masters. His distinctive style is widely recognized and his work was greatly influenced by the South African landscape.
Most of his landscapes were of the South African highveld, which provided a lifelong source of inspiration for him. Pierneef's style was to reduce and simplify the landscape to geometric structures, using flat planes, lines and colour to present the harmony and order in nature. This resulted in formalised, ordered and often-monumental view of the South African landscape, uninhabited and with dramatic light and colour.
Pierneef's work can be seen worldwide in many private, corporate and public collections, including the Africana Museum, Durban Art Gallery, Johannesburg Art Gallery, King George VI Art Gallery, Pierneef Museum and the Pretoria Art Gallery.

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2019 - Wandering Vertexes...
by Francis Rousseau