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Incahuasi (Spanish pronunciation: [iŋkaˈwasi]; possibly from Quechuainka Incawasi house)[3][4] is a volcanic mountain in the Andes of South America. It lies on the border of the Catamarca Province of Argentina and the Atacama Region of Chile. Incahuasi has a summit elevation of 6,621 metres (21,722 ft) above sea level.

The volcano consists of a 3.5-kilometre-wide (2.2 mi) caldera and two stratovolcanoes. Four pyroclastic cones located 7 kilometres (4.3 mi) to the northeast have produced basalt-andesite lava flows that cover an area of 10 square kilometres (4 sq mi).[5]

Geography and geology[edit]

Incahuasi lies on the border between Argentina and Chile,[2] close to Paso San Francisco.[6] A major road crosses the border there.[7]

Regional[edit]

Incahuasi is part of the Central Volcanic Zone of the Andes, together with about 110 other Quaternary volcanoes, and lies in the southern sector of this zone;[8] other volcanic zones in the Andes are the Northern Volcanic Zone, the Southern Volcanic Zone, and the Austral Volcanic Zone.[9] The history of volcanic activity of most of these volcanoes is poorly understood owing to the lack of dating; only a few historical eruptions have been recorded, such as an eruption at Ojos del Salado in 1993.[8]

Incahuasi is located northeast of Ojos del Salado,[2] the highest volcano in the world.[10] Both volcanoes are found at the southern end of the Central Volcanic Zone.[11] Together with El FraileCerro El MuertoNevado Tres Cruces, and El Solo, they form a 50-kilometre-long (31 mi) volcanic chain.[12]

The area is dominated by volcanoes that were active after 1.5 million years ago.[13] Also located close to Incahuasi are Falso Azufre and Nevado San Francisco,[6] as well as the Miocene Cerro Morocho and Cerro Ojo de Las Lozas volcanoes.[14] It has been suggested that a perpendicular chain of volcanoes including Ojos del Salado may be the consequence of the Juan Fernández Ridge subducting in the Peru–Chile Trench.[15]

Geological evidence suggests that volcanism in the area dates back to the Oligocene and Miocene, when the main volcanic arc was located 40 kilometres (25 mi) west in the Maricunga Belt. Between 9 and 6 million years ago, volcanic activity in the Maricunga Belt decreased and eventually ceased. Simultaneously, the back-arc experienced increased volcanic activity.[11] Beginning 8.3 million years ago, there was a change in tectonic regime from an east-west compression to a north-south stretching, which led to a change in the alignments of the volcanoes.[16]

Letter

 
   
  Thought you killed me
with that rocket? Well, you nearly did:
splattered walls and splintered air,
knocked me cold and full of holes,
and brought the roof down on my head.

But I lived,
long enough to wonder often
how you missed, long enough
to wish too many times
you hadn't.

What's it like back there?
It's all behind us here,
and after all those years of possibility,
things are back to normal.
We just had a special birthday,
and we've found again our inspiration
by recalling where we came from
and forgetting where we've been.

Oh, we're still haggling over pieces
of the lives sticking out
beyond the margins of our latest
history books—but no one haggles
with the authors.

Do better than that
you cockeyed gunner with the brass
to send me back alive among a people
I can never feel
at ease with anymore:

remember where you've been, and why.
And then build houses; build villages,
dikes and schools, songs
and children in that green land
I blackened with my shadow
and the shadow of my flag.

Remember Ho Chi Minh
was a poet: please,
do not let it all come down
to nothing.
 
   go backgo to next  
  Copyright © 1978 by W. D. Ehrhart
Empire, Samisdat, 1978
This poem currently appears in Thank You For Your Service: Collected Poems, McFarland & Company, 2019
A lotA 

Distribution[edit]

Currently, 1,518 Ultras have been identified above sea level: 639 in Asia, 356 in North America, 209 in South America, 120 in Europe (including 12 in the Caucasus), 84 in Africa, 69 in Oceania, and 41 in Antarctica.[2]

Many of the world's largest mountains are Ultras, including Mount EverestK2KanchenjungaKilimanjaroMont Blanc, and Mount Olympus. On the other hand, others such as the Eiger and the Matterhorn are not Ultras because they do not have sufficient prominence. Many Ultras lie in rarely visited and inhospitable parts of the world, including 39 in Greenland, the high points of the Arctic islands of Novaya ZemlyaJan Mayen and Spitsbergen, and many of the peaks of the Greater ranges of Asia. In British Columbia, some of the mountains listed do not even have generally recognized names.

Thirteen of the fourteen 8,000-metre summits are Ultras (the exception being Lhotse), and there are a further 64 Ultras over 7,000 metres (23,000 ft) in height. There are 90 Ultras with a prominence of over 3,000 metres (9,800 ft), but only 22 with more than 4,000 metres (13,000 ft) prominence.

A number of Ultras have yet to be climbed, with Sauyr Zhotasy, (possibly) Mount Siple, and Gangkar Puensum being the most likely candidates for the most prominent unclimbed mountain in the world.[3][4]

All of the Seven Summits are Ultras by virtue of the fact that they are the high points of large landmasses. Each has its key col at or near sea level, resulting in a prominence value almost equal to its elevation.

Lists of Ultras (1518)[edit]

General[edit]

Africa (84)[edit]

Antarctica (41)[edit]

Asia (639)[edit]

Europe (120)[edit]

North America (356)[edit]

The summit of Mount Logan in Yukon, the highest point in Canada, is ranked sixth in the world by topographic prominence.

Oceania (69)[edit]

South America (209)[edit]

A lot of things apparently happen when a few people have a few things to do




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