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Table 3. Parameters to be considered in the classifica-
tion of pyroclastic massifs.
estaire Gepp, J., serrano, a. & Perucho, a. 2008.
cimentaciones superficiales en rocas con cavernas. ii
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engineering geological properties of the volcanic
Rocks and soils of the canary islands in soils and
Rock. sao Paulo, 31 (1), pp. 3-13.
González de Vallejo, l.i., hijazo, T., Ferrer, M. &
seisdedos, J. 2006. caracterización geomecánica de
los materiales volcánicos de Tenerife, p. 40.
González-Gallego, J. 2008. clasificaciones Geomecáni-
cas (aplicación a Rocas Volcánicas). ii Jornadas
canarias de Geotecnia.
hoek, e., Marinos, P. & Marinos, V. 2005. characteriza-
tion and engineering properties of tectonically undis-
turbed but lithologically varied sedimentary rock
masses. international journal of rock mechanics &
mining sciences, 42, pp. 277-285.
lyell, c. 1839. elements of Geology. london.
Marinos, P. & hoek, e. 2001. estimating the geotechni-
cal properties of heterogeneous rock masses such as
Flysch. in Bull. engg. Geol. env., 60, pp. 85-92.
Muñiz Menéndez, M. 2009. clasificaciones geomecáni-
cas en roca volcánicas. Master en Mecánica de suelos
e ingeniería Geotécnica. ceDeX, Madrid.
Peiró, R. 1997. caracterización geotécnica de los
materiales volcánicos del archipiélago canario. in
Tierra y tecnología, pp. 45-49.
Romana Ruiz, M. 1996. el ensayo de compresión puntual
de Franklin. ingeniería civil/ceDeX. n. 102 (abr.-
jun) pp. 116-120.
serrano, a. 1976. aglomerados volcánicos en las islas
canarias. in Mem. simp. nac. de rocas blandas . Tomo 2.
a-10, Madrid.
serrano, a., olalla, c. & Perucho, a. 2002. evaluation of
non-linear strength laws for volcanic agglomerates. in
ISRM International Symposium on Rock Engineering
for Mountainous Regions and Workshop on Volcanic
Rocks , eurock 2002. Funchal, 27 nov.
serrano, a., olalla, c., Perucho, a. & hernández, l.
2008. Resistencia y deformabilidad de piroclastos de
baja densidad. in ii Jornadas canarias de geotécnia,
Tacoronte, Tenerife.
Vásárhelyi, B. 2002. influence of the water saturation on
the strength of volcanic tuffs. in isRM international
symposium on Rock engineering for Mountainous
Regions and Workshop on Volcanic Rocks, eurock
2002. Funchal, 27 nov.
Parameter
importance
in-situ density
+++
Welding and overlapping
+++
alteration
++
Presence of water
+
Discontinuities
+
as in the previous section, the weight of
each parameter has to be carefully evaluated by
in-situ studies, supported by laboratory tests and
by studying historical cases.
4
sUMMaRY anD conclUsions
Volcanic rocks have different geotechnical behavior
of other rock types.
The use of geomechanical classifications must
be done carefully, paying particular attention to
their distinctive characteristics.
The behavior of the lavatic rocks depends
mainly on its discontinuities, both in its system
of fracturing as the presence of holes. it should
also be taken into account the great heterogeneity
present in these materials. The special morphology
of this fracture system makes specific indices must
be used to consider adequately.
The pyroclastic massifs are mainly dependent
behavior of the resistant characteristics of the rock
matrix and hence the use of existing geotechnical
classifications may not be suitable.
ReFeRences
Barton, n., lien, R. & lunde, J. 1974. engineering
classification of rock masses for the design of tunnel
support. in Rock Mechanics, 6 (4), pp. 189-236.
catane, s., orense, R. & Tsuda, n. 2006. effect of water
saturation on the compressive strength and failure
modes of the Diliman tuff. Unpublished.
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