1,721,113 research outputs found
Carta geomorfologica della Val Graveglia (Appennino ligure)
No full textBrandolini P., Canepa G., Faccini F., Robbiano A., Terranova R. (2007) - Geomorphological and geo-environmental features of the Graveglia Valley (Ligurian Apennines). Geografia Fisica e Dinamica Quaternaria, 30, 99-11
Carta geomorfologica dell’Alta Val d’Aveto - finalizzata alla valutazione del pericolo da esondazione.
No full textBrandolini P., Faccini, Robbiano A., Terranova R. (2008) - Relationship between flood hazards and geomorphology applied to land planning in the upper Aveto Valley (Liguria, Italy). Geografia Fisica e Dinamica Quaternaria, 31, 73-8
Carta geomorfologica del territorio compreso tra il M. Antola e il Lago del Brugneto (Alta Val Trebbia, Appennino ligure).
No full textFaccini F., Perasso L., Robbiano A., Brandolini P. (2009) – Geomorfologia applicata alla pianificazione del territorio ed alla difesa del suolo in un tipico ambiente montano ligure. Memorie della Società Geografica Italiana, 211-22
Le cave storiche di Portoro sull’isola Palmaria: emergenze geominerarie determinanti nel quadro geologico-ambientale di un territorio da promuovere a Geoparco dell’UNESCO
No full text
Prime applicazioni del piano di protezione dell’ambiente, di decontaminazione, di smaltimento e di bonifica ai fini della difesa dai pericoli derivanti dall’amianto
No full textPianificazione territoriale delle georisorse lapidee in Liguria: considerazioni e proposte in rapporto alla sostenibilità ambientale delle attività estrattive
No full textLa grotta Bossea PMD1 nel quadro dell’evoluzione geomorfologica della Val Graveglia (Comune di Ne - Appennino Ligure)
No full textGeomorphic hazard and intense rainfall: the case study of the Recco Stream Catchment (Eastern Liguria, Italy)
No full textA critical pluviometric event occurred in the
central-eastern Ligurian Riviera, 15 km from Genoa, on
1 June 2007. This event caused landslides and hydraulic
problems between Sori and Camogli and in the inland area
of the Recco Valley.
An analysis of the heavy rainfall was conducted.
Hourly precipitation data revealed a critical event between
04:00 a.m. and 07:00 a.m. local time, with more than
220mm of precipitation over three hours.
Slope movements were mainly debris flows that detached
from the lateral valleys of the Recco Stream catchment and
from well-maintained, wooded slopes that were also characterised
by cultivated terraces.
Numerous slide planes corresponded to the interface between
the surface cover and the underlying bedrock, which
presents an unfavourable geologic structure in terms of stability
assessment.
In most cases, the displaced material had a limited thickness.
Debris cover was rapidly channelled along small valleys,
which controlled the critical hydraulic conditions in the
secondary drainage network.
Man-made drainage systems were partially or totally
blocked in a very short time and, like the natural watercourses,
accumulated thick and extensive alluvial fans.
Most of the instability phenomena occurred in areas that
had been designated medium or low-risk areas during land
planning, and in sectors that were defined as stable, because
they lacked geomorphic indicators connected to landslide
risks.
The above considerations highlight some gaps of the
Recco Stream Master Plan. Therefore, to update this land
planning tool, it is necessary to extensively investigate local
geomorphological characteristics and to adopt a different
method for assigning weights to the geohazard maps
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