Fig.Ā 4From: On the detectability of Teide volcano magma chambers (Tenerife, Canary Islands) with magnetotelluric dataDifferent geophysical models. Comparison between the 3-D P wave velocity model derived by GarcĆa-Yeguas et al. (2012) and the original 3-D resistivity model at: a 1Ā km a.s.l; c 1Ā km b.s.l. Comparison between the density contrast model derived by Gottsmann et al. (2008) and the original 3-D resistivity model at: b 1Ā km a.s.l; d1Ā km b.s.l. White line corresponds to resistivity valuesĀ <Ā 10Ā Ī©m, which has been interpreted as the hydrothermal alteration clay cap. Grey triangles correspond to the MT sites. White triangles correspond to Teide (left) and MontaƱa Blanca (right). Yellow lines correspond to the potential magma chambers considered on the different test performedBack to article page