Edge Rewrite
// HTMLRewriter · presentation

This page was redesigned at the edge.

Cloudflare fetched the original article and streamed it through HTMLRewriter to apply an entirely new visual system without rebuilding the source page.

// request.cf · coarse context

A page that knows where it met you.

Only coarse request metadata is shown. This demo does not display or persist visitor IP addresses.

Country
US
Cloudflare location
CMH
Connection
HTTP/2
Language
Not provided

Ray ID: a2535f927a1c3524

Jump to content

// Workers AI · dad joke modeWhat did Chusmiza say to its date? You're a-maize-ing.

Chusmiza complex (also known as Cerros de Sotoca)[1] is a Miocene volcano in Chile. It is the largest stratovolcano of the Miocene epoch in the western Andean escarpment, with a volume of 400 cubic kilometres (96 cu mi). It is constructed from andesite.[2] Potassium-argon dating has established an age of 11.3±0.3 mya.[1]

19°41′2.14″S 69°11′17.81″W / 19.6839278°S 69.1882806°W / -19.6839278; -69.1882806

References

[edit]
  1. 1 2 Farías, Marcelo; Charrier, Reynaldo; Comte, Diana; Martinod, Joseph; Hérail, Gérard (August 2005). "Late Cenozoic deformation and uplift of the western flank of the Altiplano: Evidence from the depositional, tectonic, and geomorphologic evolution and shallow seismic activity (northern Chile at 19°30′S)". Tectonics. 24 (4): n/a. Bibcode:2005Tecto..24.4001F. doi:10.1029/2004TC001667. hdl:10533/176713.
  2. Wörner, Gerhard; Hammerschmidt, Konrad; Henjes-Kunst, Friedhelm; Lezaun, Judith; Wilke, Hans (December 2000). "Geochronology (40Ar/39Ar, K-Ar and He-exposure ages) of Cenozoic magmatic rocks from Northern Chile (18-22°S): implications for magmatism and tectonic evolution of the central Andes". Revista Geológica de Chile. 27 (2). ISSN 0716-0208. Retrieved 1 October 2015.