The Cilento Vallo di Diano National Park (Southern Italy) was recently awarded the designation of "Geopark". Situated in the Southern Apennine chain in a typical Mediterranean environment, it is noted for a high degree of geological diversity: coastal and mountain areas made up both by carbonate and terrigenous successions give rise to a landscape alternating between steep mountainous districts and hill areas. Its territory preserves a large number of geosites, which have been identified and described by previous Authors.This paper illustrates two basic geo-itineraries which can help explain the high potential interest of the area in geotourism terms and which can provide a valid example for further future geo-itinerary planning. The itineraries can be used for teaching purposes at different educational levels (students of high school level; school teachers; geotourists; geopark guides), as well as for university courses. In addition, non-geologists may follow the itineraries and discover the geological heritage of the park. The first itinerary is located in the inner zone of the geopark. It runs throughout the Alburni massif and explains how karst processes act within a carbonate massif and how they influence underground water storage and circulation. The second is located in the southern coastal sector of the park. It sets out to describe the main Quaternary eustatic sea level fluctuations and the main coastal morphologies. In both cases an educational box at the beginning and a reflection box at the end of each itinerary are proposed to facilitate comprehension of the main concepts for visiting non-experts and to convey the main messages of the trip bette

Geo-itineraries in the Cilento Vallo di Diano GEOPARK: a tool for tourism development in Southern Italy / Santangelo, Nicoletta; Romano, Paola; Santo, Antonio. - In: GEOHERITAGE. - ISSN 1867-2477. - 7:4(2015), pp. 319-335. [10.1007/s12371-014-0133-9]

Geo-itineraries in the Cilento Vallo di Diano GEOPARK: a tool for tourism development in Southern Italy

SANTANGELO, NICOLETTA;ROMANO, PAOLA;SANTO, ANTONIO
2015

Abstract

The Cilento Vallo di Diano National Park (Southern Italy) was recently awarded the designation of "Geopark". Situated in the Southern Apennine chain in a typical Mediterranean environment, it is noted for a high degree of geological diversity: coastal and mountain areas made up both by carbonate and terrigenous successions give rise to a landscape alternating between steep mountainous districts and hill areas. Its territory preserves a large number of geosites, which have been identified and described by previous Authors.This paper illustrates two basic geo-itineraries which can help explain the high potential interest of the area in geotourism terms and which can provide a valid example for further future geo-itinerary planning. The itineraries can be used for teaching purposes at different educational levels (students of high school level; school teachers; geotourists; geopark guides), as well as for university courses. In addition, non-geologists may follow the itineraries and discover the geological heritage of the park. The first itinerary is located in the inner zone of the geopark. It runs throughout the Alburni massif and explains how karst processes act within a carbonate massif and how they influence underground water storage and circulation. The second is located in the southern coastal sector of the park. It sets out to describe the main Quaternary eustatic sea level fluctuations and the main coastal morphologies. In both cases an educational box at the beginning and a reflection box at the end of each itinerary are proposed to facilitate comprehension of the main concepts for visiting non-experts and to convey the main messages of the trip bette
2015
Geo-itineraries in the Cilento Vallo di Diano GEOPARK: a tool for tourism development in Southern Italy / Santangelo, Nicoletta; Romano, Paola; Santo, Antonio. - In: GEOHERITAGE. - ISSN 1867-2477. - 7:4(2015), pp. 319-335. [10.1007/s12371-014-0133-9]
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11588/584492
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