Supports· strongGEO-E035
Proponents' 2020 Pumapunku model: natural Khapia andesite sand stored at Iwawe (Stratum V), piedras cansadas not used
- what the source states
- The abstract states that to make geopolymer andesite around AD 600–700 the builders could have transported an andesite stony material with the consistency of sand from the Cerro Khapia volcano, adding an organo-mineral binder from local biomass; that "They did not use the many quadrangular volcanic blocks", the famous piedras cansadas lying on both sides of Lake Titicaca; that they exploited a natural volcanic andesite sand from Cerro Khapia, "transported and stored it at the shore village of Iwawe", Stratum (V) in the excavation by Isbell & Burkholder (2002); and that they did not need to crush andesite rock, the sand resembling the Roman pozzolana called carbunculus.
- what we infer
- Editor's inference: this is the primary statement of the model GEO-C903 describes, so it supports that descriptive claim directly. It also fixes two checkable objects: the Iwawe Stratum V deposit (GEO-R009) and the abandoned quadrangular blocks. Both parties now place the andesite's origin at Khapia/Ccapia, which is why quarry geochemistry alone cannot separate them (GEO-C030 in its narrow form).
- limitations
- Abstract only; the PDF (DOI 10.13140/RG.2.2.10021.93929/2) returned HTTP 403 and was not read.
- Proponent-authored, self-published journal (Journal on Geopolymer Science Applied to Archaeology).