2026-07-18T13:09:54Zhttps://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

Geometric form of volcanoes with a limited based Arjona, Alicia Díaz Díaz, Jesús Ildefonso Fernández Castillo, Jesús 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. 2023-06-20T05:46:46Z 2023-06-20T05:46:46Z 2023-06-20T05:46:46Z 2009 book part https://hdl.handle.net/20.500.14352/45558 XXXX-XXXX eng MTM2008-06208 CCG07-UCM/ESP-2787 GEOMOD (CGL2005-05500-C02) open access Universidad de Castilla-La Mancha