The Servicio Geologico Colombiano (SGC) reported that the amplitude of seismic tremor at Puracé increased during the afternoon of 21 January and remained elevated through 23 January. Satellite images captured on 23 January showed a system of cracks and cavities formed during the ash emission on 20 January. Gas-and-steam emissions rose from previously existing fumarolic vents at the Puracé cone and from the two new vents that had opened days before at the Curiquinga cone, located immediately SE of Puracé. Significant levels of sulfur dioxide emissions continued to be detected by instruments at the Puracé summit. Strong sulfur dioxide odors were reported in the communities of Paletará (16 km SW), Puracé (11 km NW), and Popayán (Cauca, 30 km NW). The Alert Level remained at Yellow (the second lowest level on a four-color scale).

Geological Summary. Puracé is an active andesitic volcano with a 600-m-diameter summit crater at the NW end of the Los Coconucos Volcanic Chain. This volcanic complex includes nine composite and five monogenetic volcanoes, extending from the Puracé crater more than 6 km SE to the summit of Pan de Azúcar stratovolcano. The dacitic massif which the complex is built on extends about 13 km NW-SE and 10 km NE-SW. Frequent small to moderate explosive eruptions reported since 1816 CE have modified the morphology of the summit crater, with the largest eruptions in 1849, 1869, and 1885.

Source: Servicio Geológico Colombiano (SGC)