A vast, gently east-sloping windswept, semiarid
plateau located primarily in southern Argentina. It is located
south of the Rio Negro east of the Andes and includes a
300,000-square-mile (776,996-km2) area that also includes
parts of southeast Chile and northern Tierra del Fuego. It is
located east of the Andes Mountain range and terminates in
cliffs on the Atlantic Ocean. The region is known for sheep
raising and tourism in its lake region but also has mineral
wealth including petroleum production and deposits of coal
and iron ore. Geologically, Patagonia is probably most famous
for its rich paleontological record and has been explored for its
diverse fossils since the region was visited by Charles Darwin.
It is home to the legendary Patagonian Giants (the Tehuelches),
later found to be not so giant by Spanish conquerors.
Early explorers of Patagonia include Amerigo Vespucci in
1501 and Ferdinand Magellan in 1520. In the late 1800s an
Argentine general named Julio A. Roca led campaigns against
the local Indians, leading the way for Argentine ranchers to
move into the area. The area is also inhabited by guanaco, rhea,
puma, and deer, including the pudu, the world’s smallest deer
species. Bird life is also common among Patagonia’s forests and
waters and ranges from the Andean condor, the world’s largest
land bird, to hummingbirds and parakeets. Some of the world’s
oldest trees stand in Parque Nacional Los Alerces.
Patagonia has several large rivers that flow through it to
the Atlantic, and one river, the Manso, forms a natural pathway
of water cutting across the barrier of the Andes to the
Pacific Ocean. Along its shores, animals and travelers formed
paths allowing for cultures to spread and cities to develop.
The Manso headwaters lie high in the Cordillera Patagonica
in Argentina and descend southeast into several lakes. The
river turns and then cuts through a gorge to the west, passing
through Lago Tagua-Tagua, then reaches the Pacific Ocean.
Charles Darwin described many details of the landscape
of Patagonia. He noted that the surface is quite level (a pene-
plain) and is composed of a well-rounded mix of gravel and
white soil, where scattered tufts of brown wiry grass have
established a shaky foothold. Standing in the middle of the
desert plains Darwin noted another, second and higher escarpment
marking a higher plain, equally level and desolate.
The western side of Patagonia is marked by the Andean
Mountain range, where subduction to the west has produced
a series of volcanic-intrusive magmatic pulses. The southern
Andes and Patagonia are host to a number of precious base
metal deposits related to this magmatism. A lucrative belt of
epithermal gold deposits and subvolcanic porphyry coppergold
deposits is found in southern Chile and Argentina.
Deposits in Patagonia are associated with the Somuncura and
Deseado volcanic massifs and include Anglo Gold’s Cerro
Vanguardia deposit (9.1 million tons of open-pit mineable
ore, with 9.7 grams per ton gold and 113 grams per ton silver),
and Meridian’s Esquel deposit (3.8 million ounces gold
at 8 grams per ton and 6.4 million ounces of silver).














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