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 Volcanic evolution through geomorphological mapping: A case study of Cerro Bravo volcano (Colombia) │ 2023 4 July, 2023 First record of middle Miocene marine diatoms from the Colombian Pacific (NW South America) and their paleoceanographic significance │ 2018 21 February, 2020 Appearance of an enigmatic Pb source in South America around 2000 BP: Anthropogenic vs natural origin │ 2020 24 January, 2022
Volcanic evolution through geomorphological mapping: A case study of Cerro Bravo volcano (Colombia) │ 2023 4 July, 2023
First record of middle Miocene marine diatoms from the Colombian Pacific (NW South America) and their paleoceanographic significance │ 2018 21 February, 2020
Appearance of an enigmatic Pb source in South America around 2000 BP: Anthropogenic vs natural origin │ 2020 24 January, 2022