The pyroclastic de La Restinga are composed of basalt and trachyte with no chemical reactionCSIC representatives as part of the scientific committee of the Civil Protection Plan for Volcanic Risk (PEVOLCA) have moved into the direction of the Plan, the preliminary results on the first pyroclastic thrown to the surface of the Sea of calms. The fragments are formed by a magma mixing between two materials, one black (basalt) and one white (trachyte), which occurred at the time of the eruption so it is a physical mixture between the two materials without the two chemical reaction has occurred.
In this regard it is noteworthy that these trachytes are volumetrically insignificant and constitute more than an anecdote that the main feature of the eruption. In reality the samples have been collected along these days, the trachyte was only present in the first few episodes as a ratio of 1 to 10 with respect to the basalt, which does not involved in determining the type of resulting eruption.
Its origin may be due to a Remobilization (reflow) of a small remnant of material from the basalt trachyte again on his way to the surface. These processes are not so rare in this type of volcanism occur in a short time (a few hours to few days).
These results, although they had already been advanced, had not been made public because it had not yet completed the series of tests to do in this type of study, and not relevant to consider that the presence of magma mixing as driver dynamics of the eruption.
It should be noted that studies have been published in the media today during a concern is for staff responsible for its production and not a formal request from the City of El Pinar, as he said.
To avoid confusion arising from contradictory information, especially the residents of El Hierro, the direction of PEVOLCA stresses the importance of following the official statements that leads to the population. To this end and for those scientific and research institutions wishing to participate in the study of eruptive phenomenon, the Canary Islands government has created a Scientific Steering Committee, to achieve effective coordination and discussion of research in order to a better guidance to bodies responsible for Civil Protection.
PROCEDURES
From the first moment CSIC members took charge of the pyroclastic sampling and its analysis following the usual procedure in these cases, ie the samples sent to different laboratories to compare results and to have a spectrum the broadest possible range of data. Some of the samples were sent to Madrid (MNCN, CSIC), Barcelona (ICTJA, CSIC) and the University of Huelva, where they are doing experimental petrology studies to determine the thermodynamic characteristics of eruptive magmas. In addition, samples have also been sent to Washington State University, in the United States and of Clermont Ferrand, France, for isotopic analysis.
Basalt and trachytes
Basalt is the most common magma eruptions of El Hierro, has a 43 percent SiO 2, reaches a temperature of 1,200 ° C and a density of 2700 kg/m3.
The trachyte is a magma with a SiO2 content of 63%, reaches a temperature of 850 ° C and a density of 2,300 kg/m3. The trachyte is not the predominant magma erupted, therefore does not contribute to increase the explosiveness of it.
Both the basaltic material as the trachyte samples are highly vesicular, which means that both had a high amount of gas in the time of eruption, which would explain why it is explosive (pyroclastic formation) despite the sea water pressure on the mouth of issue. However, this type of explosive is normal within the parameters of basaltic eruptions with which we move and no additional hazard is of the fact also contain trachytic magma.