The Morales Formation (New Unit): Record of Fluvial–Lacustrine Environments and the Beginning of the Miocene Explosive Volcanism in the Patía Sub–basin (SW Colombia) │ 2020 https://doi.org/10.32685/pub.esp.37.2019.13 Leer más artículos Entrada anteriorCretaceous Record from a Mariana– to an Andean–Type Margin in the Central Cordillera of the Colombian Andes │ 2020 Siguiente entradaEffusive Monogenetic Volcanism │ 2020 También podría gustarte Emplacement conditions of the 1256 AD Al-Madinah lava flow field in Harrat Rahat, Kingdom of Saudi Arabia — Insights from surface morphology and lava flow simulations │ 2016 20 February, 2020 Evidence for welding of a block and ash pyroclastic flow deposit: the case of Cerro Bravo Volcano, Colombia │ 2019 21 February, 2020 Finding eruptive mechanisms through pyroclasts from the current eruption (1984–present) at Nevado del Ruiz Volcanic Complex, Colombia │ 2018 20 February, 2020
Emplacement conditions of the 1256 AD Al-Madinah lava flow field in Harrat Rahat, Kingdom of Saudi Arabia — Insights from surface morphology and lava flow simulations │ 2016 20 February, 2020
Evidence for welding of a block and ash pyroclastic flow deposit: the case of Cerro Bravo Volcano, Colombia │ 2019 21 February, 2020
Finding eruptive mechanisms through pyroclasts from the current eruption (1984–present) at Nevado del Ruiz Volcanic Complex, Colombia │ 2018 20 February, 2020