El Escondido tuff cone (38 ka): a hidden history of monogenetic eruptions in the northernmost volcanic chain in the Colombian Andes │ 2019 https://doi.org/10.1007/s00445-019-1337-2 Leer más artículos Entrada anteriorCaracterización de las asociaciones de cocolitóforos en las cuencas offshore del Pacífico colombiano │ 2019 Siguiente entradaEvidence for welding of a block and ash pyroclastic flow deposit: the case of Cerro Bravo Volcano, Colombia │ 2019 También podría gustarte The Phycosiphon record in the Ladrilleros-Juanchaco section (Miocene, Colombian Pacifi c): palaeoecological implications │ 2018 21 February, 2020 Effusive and evolved monogenetic volcanoes: two newly identified (~800 ka) cases near Manizales City, Colombia │ 2023 4 July, 2023 Mid to late holocene dry events in Colombia’s super humid Western Cordillera reveal changes in regional atmospheric circulation │ 2021 24 January, 2022
The Phycosiphon record in the Ladrilleros-Juanchaco section (Miocene, Colombian Pacifi c): palaeoecological implications │ 2018 21 February, 2020
Effusive and evolved monogenetic volcanoes: two newly identified (~800 ka) cases near Manizales City, Colombia │ 2023 4 July, 2023
Mid to late holocene dry events in Colombia’s super humid Western Cordillera reveal changes in regional atmospheric circulation │ 2021 24 January, 2022