,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

",-0.37,-91.55,InSAR,Magmatic,"['Bagnardi, M., & Amelung, F. (2012). Space‐geodetic evidence for multiple magma reservoirs and subvolcanic lateral intrusions at Fernandina Volcano, Galápagos Islands. Journal of Geophysical Research: Solid Earth, 117(B10).', 'Amelung, F., S. Jónsson, H. Zebker, and P. Segall (2000), Widespread uplift and “trapdoor” faulting on Galápagos volcanoes observed with radar interferometry, Nature, 407, 993–996, doi:10.1038/35039604.']",South America,"{'region': 'pacific_island', 'frames': [{'id': '128D_09016_110500', 'track': '128'}]}",,,,Y