Titlebook: Drinking Water in Sicily; Hydrogeological and Esterina Gagliano Candela,Giovannella Pecoraino,Le Book 2024 The Editor(s) (if applicable) a

Ptosis

osition of various carbonate, carbonate-silicoclastic and terrigenous geological bodies, of Upper Triassic–Lower Miocene age, with generally southern vergence. These bodies derive from the Miocene deformation of a pelagic basin and escarpment succession (Dominio Imerese Auct.), formed during the Mes

notice

s, to the south by the so-called Castelvetrano Basin and to the west by the Strait of Sicily (Fig. .). The most important reliefs are Mt Sparagio and Mt Inici, characterised by altitudes around 1.000 m (1.100 and 980 m, respectively). The Trapani Mts are formed by the Miocene tectonic superposition

FECT

https://doi.org/10.1007/978-3-031-60473-7Sicilian aquifers; Hydrogeology; Hydrogeochemistry; Water isotopes; chemical characteristics of groundwa

Vaginismus

oxidize

银版照相

异端

教育学

Piazza Armerina Hydrogeological Basin,o the south by the Mediterranean Sea, to the southeast by the Hyblean plateau, to the east by the Catania Plain and the volcanic edifice of Etna, to the north by the Nebrodi Mts and to the west by the Caltanissetta Trench.

Debark

Palpitation