| |
| | Rull, Valenti - 1998 (Site not responding. Last check: 2007-09-05) |
 | | A stadial, called El Caballo, is reported at 16.5 ka B.P. The estimated average temperature was around 7° C lower than today, and coincides with the Colombian Fuquene stadial and the global oxygen-isotopic Stage 2. |
 | | To explain this it is necessary to take into account the decreasing age of sediments with increasing altitude, because of the removing of older sediments by glaciers during the LGM, combined with the sequential filling of rock cavities upwards during the deglaciation. |
 | | The maximum occurred in the last centuries, after the Little Ice Age (Piedras Blancas cold phase), and the minimum after the Miranda warm phase, around 2.5 ka B.P. Negative retreat values or readvance coincide with the La Culata cold phase. |
| www.pdvsa.com /lexico/bibgeol/bg3219.htm (277 words) |
|