In the past ten years cave surveying has allowed better understanding of speleogenesis in the Orosei Gulf (Central-East Sardinia, Italy), one of the most important coastal karst areas of Italy. Surface geomorphologic research has been accompanied by subterranean and submarine landform analysis in order to try and understand the evolution of this coastal karst since its emersion in Upper Eocene. The main factors influencing the geomorphic processes are lithology, tectonics, palaeo-climate and sea level changes. The study of several important cave systems demonstrates a complex geological history with karst processes that started in Early Tertiary and accelerated during Plio-Quaternary
Coastal karst is characterized by special geomorphologic and hydrodynamic conditions as well as by p...
Sea level is the base level for groundwater circulation in coastal aquifers. The evolution of karst ...
In the area of Punta Funtanas (Arbus, Central-West Sardinia) some small surfaces of Miocene limeston...
In the past ten years cave surveying has allowed better understanding of speleogenesis in the Orosei...
The Gulf of Orosei (Central East Sardinia, Italy) is among the most important coastal karst areas of...
Orosejski zaliv je eno najpomembnejših obalnokraških območij v Italiji. Številne nove meritve jam so...
none4noThiswork reports the results of geomorphological observations carried out in the coastal Fico...
Coastal karst areas often host many indices of past sea level changes, such as marine terraces, foss...
Hydrogeological research of karst areas in Sardinia is often hindered by the discontinuity of superf...
The Gulf of Orosei (Central-East Sardinia) is the most important coastal karst area of Italy, develo...
A coastal and underwater geomorphological study has been carried out between S. Maria Navarrese and ...
Several important cave systems in Central East Sardinia develop, at least partially, along the conta...
The coastal karst areas of Sardinia represent extremely interesting territories both for...
Coastal karst is characterized by special geomorphologic and hydrodynamic conditions as well as by p...
Sea level is the base level for groundwater circulation in coastal aquifers. The evolution of karst ...
In the area of Punta Funtanas (Arbus, Central-West Sardinia) some small surfaces of Miocene limeston...
In the past ten years cave surveying has allowed better understanding of speleogenesis in the Orosei...
The Gulf of Orosei (Central East Sardinia, Italy) is among the most important coastal karst areas of...
Orosejski zaliv je eno najpomembnejših obalnokraških območij v Italiji. Številne nove meritve jam so...
none4noThiswork reports the results of geomorphological observations carried out in the coastal Fico...
Coastal karst areas often host many indices of past sea level changes, such as marine terraces, foss...
Hydrogeological research of karst areas in Sardinia is often hindered by the discontinuity of superf...
The Gulf of Orosei (Central-East Sardinia) is the most important coastal karst area of Italy, develo...
A coastal and underwater geomorphological study has been carried out between S. Maria Navarrese and ...
Several important cave systems in Central East Sardinia develop, at least partially, along the conta...
The coastal karst areas of Sardinia represent extremely interesting territories both for...
Coastal karst is characterized by special geomorphologic and hydrodynamic conditions as well as by p...
Sea level is the base level for groundwater circulation in coastal aquifers. The evolution of karst ...
In the area of Punta Funtanas (Arbus, Central-West Sardinia) some small surfaces of Miocene limeston...