Saturday, November 7, 2015

Salar de Tara


#A flock of Jame’s flamingos feeds on tiny organisms in the Salar de Tara-part of a nature reserve they share with the related Andean flamingos and Chilean flamingos

It’s sunrise a Salar de Tara and the salt lake is aflutter with flamingos. There a thousands of them, long slender legs wading through metallic blue waters. They move in waves, flighty as though an electric current bites when they linger too long. The wind stirs from its slumber, whipping the water into a dance. Alongside the salt lake, hundreds of llamas pick their way through tufty yellow pastures. They look with long-lashed eyes down velvet noses, seemingly haughty, their ears pricking at the crunch of salt underfoot.

Bordered by barren Altiplanic mountains and bisected by the Tropic of Capricorn, this wetland sits within the Reserva Nacional Los Flamencos on the eastern fringe of the Atacama, in a nook between the borders of Bolivia and Argentina. It’s zone of permanent and seasonal lakes-but extending westwards and covering an area nearly the size of England is a region known as the driest on Earth. Nowhere, save for the icy anomaly of Antarctica, receives less rainfall. Indeed, in great swathes of this desert, rain has never been recorder. Its cracked, dusty landscape is somewhere between lunar and Martian, unable to support plant or animal.

Yet throughout the desert, pockets of life do exist. The Hamas around Salar de Tara are owned by shepherds who herd them as the season dictate. The shepherds are Atacamenos, mainly descended from settled here more than 3,000 years ago. They live in ayllus-small indigenous communities-on hillsides and in gorges served by ephermeral streams, cultivating crops on terraces dug out by their forbears, and tending to goats, sheep and llamas. Folklore still blows through these oases like the Atacama’s gentle Pacific breeze, a rich mythology that connects these people to their nomadic ancestors, and to the extraordinary landscape that they inhabit.

A Volcanic Temperament

‘Licanbur is a price and Quimal is a a princess,’ says Atacameno guide Rosa Ramos Colque, speaking slowly and deliberately, and gesturing to each of the mountains in turn .the peaks face off across the Salar de Atacama, on which she stands – a vast sea of salt encompassing more than 1,200 square miles, to the west of Salar de Tara. The peaks of Licancabur and Quimal are some 50 miles apart, but such is the clarity of the air, they appear closer. Alongside the perfectly pyramidal snow-splashed volcano of Licancabur is another mountain, conspicuous for its fla top. It looks a s though its peak has been removed, possibly severed; mythology asserts exactly that. ‘Juriques, Prince Licancabur’s companion, was once just perfect, with a head too,’ says Rosa. ‘That was, until he seduced Princess Quimal.’

The volcano legends are known by all in these parts; versions vary, but any that followed this betrayal. Quimal’s father Lascar – an amorphous mountain standing to the east, almost equidistant, beheaded Juriques and exiled Quimal across the salt flat. Such behavior certainly fits the profile. Lascar is the most active volcano in the Central Andean section of the Pacific’s Ring of Fire – in 1993, it dispatched a grittsoud of tephra as far as Buenos Aires, 900 miles to the southeast, and it has made its presence known several times already this century. Lincancabur was heartbroken at Quimal’s banishment. Shedding tears that  the centuries accumulate into the lake cradled in its crater.

Such legends are indicative of an wavering reverence; in the Atacama, volcanoes are both providers and destroyers. The ancient Atacamenos built villages from volcanic stone in spots where rater runs down their steep slopes, while the centuries, dispersed volcanic with has helped to fertilise parts of this otherwise barren landscape. Forty-five minutes southeast of the regional hub of sun Pedro de Atacama, two villages sit below Lascar’s smoking crater. They’re with called Talabre. Rather than a lack of ragination, the duplication stems from another eruption of Lascar in the 1970s. the volcano contaminated the original Talabre’s water, lacing the river wit ash;