2026-07-18T16:46:27Zhttps://docta.ucm.es/rest/oai/request

oai:docta.ucm.es:20.500.14352/455582024-09-27T14:36:40Zcom_20.500.14352_14col_20.500.14352_21

Arjona, Alicia Díaz Díaz, Jesús Ildefonso Fernández Castillo, Jesús 2023-06-20T05:46:46Z 2023-06-20T05:46:46Z 2009 https://hdl.handle.net/20.500.14352/45558 Many volcanic constructs have geometric different shapes depending on different phenomena as parasitic cones, erosion or coral growth. In Lacey, Ockendon and Turcotte [11] the authors proposed a nonlinear model proving that the shape of volcanoes is determined by the hydraulic resistance to the flow of magma, from a line source, through the porous edifice. This model was later extended in Angevine, Turcotte and Ockendon [2] to include the shape of aseismic, submarine ridges. In this communication we propose a modification of the above mentioned models in order to simulate the more realistic case of volcanoes with a limited base. eng open access Geometric form of volcanoes with a limited based book part