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Monitoring

 

A first essential stage of the reduction of the volcanic risks associated with mount Pelée lies in the monitoring of the volcano...

The detection of the precursory signs of an eruption allows to alert then to evacuate the populations at risk. Volcanic monitoring thus guarantees the safety of the populations living around mount Pelée.
 
 Mt Pelee Volcano Observatory
Mt Pelee Volcano Observatory, in Fonds-Saint-Denis
(ph. F. Leone, 2004)

 



Historical Overview

 

During the 1902 eruption, professor Alfred Lacroix was the first to stress the need for a permanent monotoring of the volcano. During his field work in Martinique, he had established 2 observation stations around mount Pelée. One on the East coast, at Assier (Lorrain), the other one on the Morne-des-Cadets (Fonds-St-Denis). The latter was then chosen for the construction of the observatory.

However, a few years after the end of the eruptive crisis in 1905, the attention paid to the volcanic monitoring quickly decreased. The main signs of the reactivation of mount Pelée in 1929 were therefore unperceived, for lack of sufficient equipment and gaps during the time of observation.

The monitoring of the new eruptive crisis was carried out by the Boutrin-Revert mission from the Morne-des-Cadets, and by the American volcanologist Frank A. Perret. The latter carried out its observations from Saint-Pierre, and from a provisional observation post, located on Morne Lénard, dominating the valley of Blanche river.

Perret Station on Mt Pelee
Perret's observation post, 1931
(ph. Perret / Carnegie Institution of Washington)

 

 The eruption of 1929-1932 indirectly contributed to the provision of an appropriation for the construction in 1937 of the permanent observatory on the site of the Morne-des-Cadets.

 

 
Principles of Volcano monitoring

 

- Seismic activity

Several seismological stations installed on mount Pelée allow the monitoring of the seismic activity of the volcano and its variations in time. The seisms of volcanic origin can precede and accompany an eruptive activity. The detection of these seisms thus makes it possible to warn of a future eruption.

 

- Measurements of deformations

The progress of the magma towards the surface is accompanied by strong pressures which deform the volcanic cone. The study of these deformations by clinometric measurements (variation of the slope), measurements of levelling (variations of altitude), electro-optical measurements of distances (variations of distances between  fixed points on the volcano), satellite recognitions.

 

- Hydrogeochemical analysis

The progress of the magma towards the surface is accompanied by the release of  gases which then modify the chemical composition and the temperature of the springs on the volcano. The analysis of the composition and the temperatures of the water on mount Pelée constitutes a parameter allowing the monitoring of the volcanic activity.

 

 
Alert levels

 

volcanic alert level mt pelee

 

 

Current status of mount Pelee Volcano :

Current alert level Mt Pelee
All Clear!
 

 

 
 
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