In this paper we study the application of different geodetic techniques to
volcanic activity monitoring, using theoretical analysis. This methodology
is very useful for obtaining an idea of the most appropriate land efficient
) monitoring method, mainly when there are no records of geodetic changes p
revious to volcanic activity. The analysis takes into account the crustal s
tructure of the area, its geology, and its known volcanic activity to estim
ate the de-formation and gravity changes that might precede eruptions. The
deformation model used includes the existing gravity field and vertical cha
nges in the crustal properties. Both factors can have a considerable effect
on computed deformation and gravity changes. Topography should be consider
ed when there is a steep slope (greater than 10 degrees). The case study of
Teide stratovolcano (Tenerife, Canary Islands), for which no deformation o
r gravity changes are available, is used as a test. To avoid considering to
pography, we worked at the lowest level of Las Canadas and examined a small
er area than the whole caldera or island. Therefore, the results are only a
first approach to the most adequate geodetic monitoring system. The method
ology can also be applied to active areas where volcanic risk is not associ
ated with a stratovolcano but instead with monogenetic scattered centers, e
specially when sites must be chosen in terms of detection efficiency or exi
sting facilities. The Canary Islands provide a good example of this type of
active volcanic areas, and we apply our model to the island of Lanzarote t
o evaluate the efficiency of the monitoring system installed at the existin
g geodynamic station. On this island togography is not important. The resul
ts of our study show clearly that the most appropriate geodetic volcano mon
itoring system is not the same for all different volcanic zones and types,
and the particular properties of each volcano/zone. must be taken into acco
unt when designing each system.