Instituto Vulcanológico de Canarias no relation emergency evacuation
Earthquakes
Beginning on 17 July 2011, increased seismic activity was detected by the Instituto Vulcanológico de Canarias (Volcanological Institute of the Canary Islands) and National Geographic Institute's seismic monitoring station located in Valverde. The seismic monitoring network was increased in density on 21 July to allow better detection and location of the seismic events. There was an earthquake swarm with in excess of 400 minor tremors between 20 July and 24 July; by 
27 July a further 320 earthquakes had been recorded. On 25 August there were reports that some horizontal deformation had been detected, but that there was no unusual vertical deformation. At that time, the total number of tremors had exceeded 4000. By the end of September, the tremors had increased in frequency and intensity, with experts fearing landslides affecting the town of La Frontera, and also a small possibility of a volcanic eruption through a new vent. In late September, emergency services evacuated several families in the areas at most risk, and made plans to evacuate the island if necessary.Submarine eruption: October 2011 – March 2012
Between 4:15 and 4:20 am on 10 October 2011 the earthquake swarm changed behaviour and produced a harmonic tremor. Harmonic tremors are produced by magma movements and can indicate that an eruption has begun.  That same day, patches of pale-coloured and sulphurous smelling water with dead fish were seen off the coast of La Restinga.  A small submarine eruption had begun, 2 km south of La Restinga.  Eruption 'jacuzzis', occasionally reaching 10–15 metres (33–49 feet) high above the surface of the water, were seen during the most energetic eruptive episodes.In early November, the 600 residents of La Restinga were evacuated for the second time. A confirmed surtseyan type of eruption phase started at the fissure on 7 November 2011. On 25 November 2011 the eruption was ongoing with vigorous phreatic bubbles emerging.Several separate plumes of material, aligned N-S, were visible from the air, showing that the eruption was of a fissure type.The main volcano on the island, Tanganasoga, underwent rapid inflation and increased carbon dioxide gas emissions, which were a cause for concern.  On 24 November there were various reports of a sulphurous smell in the El Golfo area of the island.
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