Talk:Teneguía
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It is NOT a volcano in its own right but a cinder cone which is part of the Cumbre Vieja's many cinder cones. It is classed as a "vent" and like most "cinder cones" is a mono-genetic. It goes through a period of eruptive activity followed by dormancy and finally it closes down completely. The clue is in its the description "Mono-genetic vent"The Geologist (talk) 15:24, 19 May 2014 (UTC)
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NO NY HAS NOT. NY State and City HAVE NOT CARRIED OUT AN EVACUATION EXERCISE IN RESPECT OF ANY PERCEIVED TSUNAMI. Parts of the city were evacuated because of the impact of Hurricane Sandie. There is also growing evidence that the claim that the Cumbre Vieja is unstable is actually without any scientific foundation - unless you are financed by an insurance company based in the USA. The claim is made that the crack on the Cumbre Vieja - about 20 kilometers north of Teneguia, is about 4 km long. It is not - it is about 1500 meters long, the ONLY place where there is 4 meter displacement is at the Duraznero and Hoyo Negro vents, the rest of the crack varies from about 2.5 meters displacement to ZERO and averages less than 2 meters. The horizontal displacement is about 1 meter - except at the vents. As at December 2014 the whole flank is still stable has the same dimensions that it had in 1949 and the only displacement is the whole island which is moving westwards at about 25 mm per year. So stop passing off fiction as fact. The scientific evidence does not support the claims. — Preceding unsigned comment added by 81.154.205.148 (talk) 17:01, 4 February 2015 (UTC)