http://www.cnr.it/ontology/cnr/individuo/prodotto/ID67048
The influence of the geological setting on the morphogenetic evolution of the Tremiti Archipelago (Apulia, Southeastern Italy). (Articolo in rivista)
- Type
- Label
- The influence of the geological setting on the morphogenetic evolution of the Tremiti Archipelago (Apulia, Southeastern Italy). (Articolo in rivista) (literal)
- Anno
- 2005-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.5194/nhess-5-29-2005 (literal)
- Alternative label
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Andriani G.F.; Walsh N.; Pagliarulo R. (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url
- http://www.nat-hazards-earth-syst-sci.net/5/29/2005/nhess-5-29-2005.html (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
- Rivista
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
- Note
- ISI Web of Science (WOS) (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- Dipartimento Scienze della Terra. Università di Bari
CNR IRPI (literal)
- Titolo
- The influence of the geological setting on the morphogenetic evolution of the Tremiti Archipelago (Apulia, Southeastern Italy). (literal)
- Abstract
- The Tremiti Archipelago (Southern Adriatic Sea),
also called Insulae Diomedae from the name of the Greek
hero who first landed there, is an area of high landscape
and historical value. It is severely affected by significant
geomorphologic processes dominated by mass movements
along the coast that constitute the most important and unpredictable
natural hazard for the population and cultural heritage.
Coastal erosion is favoured by the peculiar geological
and structural setting, seismic activity, weathering, development
of karst processes, and wave action.
The present paper reports on descriptive and qualitative
evaluation of the factors controlling landslides and coastline
changes based on medium-term in situ observation, detailed
surface surveys at selected locations since 1995, and historic
and bibliographic data.
The Tremiti Archipelago is part of an active seismic area
characterised by a shear zone separating two segments of the
Adriatic microplate that have shown different behaviour and
roll back rates in the subduction underneath the Apennines
since middle Pleistocene.
Although coastal morphology can be basically considered
to be the result of wave action, the continual action of subaerial
processes contributes effectively to the mechanism of
shoreline degradation. Weathering mainly affects the marly
calcisiltites and calcilutites of the Cretaccio Fm. and the friable
and low cemented calcarenites and biomicrites of the
San Nicola Fm. The cliffs are characterised by different
types of failure such as lateral spreads, secondary topples,
rock falls and slides. At the Isle of San Nicola, landslides are
controlled by the contrast in competence, shear strength and
stiffness between the Pliocene re-crystallised dolomitic calcarenites
and calcisiltites and the Miocene marly calcilutites
and calcisiltites. At the Isles of San Domino and Caprara
rock falls are attributed to the undercutting of waves at the
base of the cliffs. (literal)
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- Autore CNR
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