I proudly support the work of Guerrilla Skepticism on Wikipedia, where all edits are open and transparent and secondary references are more important than your belief system on any one subject. Editors with similar interest should work together on articles. I do not edit controversial pages. Although I will be happy to help you with any article in my core subject areas - I am unlikely to join in "your cause" on a given controversy. In my opinion this is not the role of a good editor nor the purpose behind Wikipedia. Collaboration on subjects of interest for the improvement of those articles is my choice instead.
Incapillo is a Pleistocene-age caldera – a depression formed by the collapse of a volcano – in La Rioja Province, Argentina. It is part of the southernmost volcanic centre in the Andean Central Volcanic Zone (CVZ). Subduction of the Nazca Plate beneath the South American Plate is responsible for most of the volcanism in the CVZ. Volcanism commenced in the Incapillo region 6.5 million years ago, forming the high volcanic edifices of Monte Pissis, Cerro Bonete Chico and Sierra de Veladero. Incapillo is known to have erupted the Incapillo ignimbrite 0.52 ± 0.03 and 0.51 ± 0.04 million years ago; this has a total volume of about 20.4 cubic kilometres (4.9 cu mi). A caldera with dimensions of 5 by 6 kilometres (3.1 mi × 3.7 mi) formed during the eruptions. Later volcanism generated more lava domes within the caldera and a debris flow in the Sierra de Veladero. The lake within the caldera may overlie an area of ongoing hydrothermal activity.
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