,jasmin_name,name,ID,country,geodetic_measurements,deformation_observation,duration_of_observation,characteristics_of_deformation,latitude,longitude,measurement_methods,inferred_causes,references,Area,frames,Review needed,date_edited,owner_id,subset 0,fernandina,Fernandina,353010,Ecuador,Yes,Yes,"January 2003 to September 2010, 1992- 1999 (ref2)","
At least two sources are considered to represent permanent zones of magma storage given their persistent or recurrent activity. Elastic deformation models indicate the presence of a flat-topped magma reservoir at ∼1.1 km below sea level and an oblate-spheroid cavity at ∼4.9 km b.s.l. The two reservoirs are hydraulically connected. Ref 1.
Fernandina exhibits a semi-circular fringe pattern on its southwest flank (Fig. 1), which has been modelled with a dipping, radial dyke coincident with the 1995 eruption6. Uplift of 0.1 m from September 1998 to March 1999 suggests refilling of a shallow magma chamber. Ref 2