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      <dc:title>Geometric form of volcanoes with a limited based</dc:title>
      <dc:creator>Arjona, Alicia</dc:creator>
      <dc:creator>Díaz Díaz, Jesús Ildefonso</dc:creator>
      <dc:creator>Fernández Castillo, Jesús</dc:creator>
      <dc:description>XXI Congreso de Ecuaciones Diferenciales y Aplicaciones
XI Congreso de Matematica Aplicada, Ciudad Real, 21-25 septiembre 2009</dc:description>
      <dc:description>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.</dc:description>
      <dc:date>2023-06-20T05:46:46Z</dc:date>
      <dc:date>2023-06-20T05:46:46Z</dc:date>
      <dc:date>2009</dc:date>
      <dc:type>book part</dc:type>
      <dc:identifier>https://hdl.handle.net/20.500.14352/45558</dc:identifier>
      <dc:language>eng</dc:language>
      <dc:relation>MTM2008-06208</dc:relation>
      <dc:relation>CCG07-UCM/ESP-2787</dc:relation>
      <dc:relation>GEOMOD (CGL2005-05500-C02)</dc:relation>
      <dc:rights>open access</dc:rights>
      <dc:publisher>Universidad de Castilla-La Mancha</dc:publisher>
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