| UTM-X | UTM-Y | ||
|---|---|---|---|
| STOP 1: THE QUATERNARY OF CALA SALADA | |||
| STOP 2: FOSSILIFEROUS LIMESTONE OF THE CRETACEOUS PERIOD | |||
| STOP 3: SA FORADADA ROCK BRIDGE | |||
| STOP 4: COVA ESTRUCTURAL DES VI | |||
| STOP 5: PUIG NUNÓ |
Recommended route to Puig Nunó.
To finish the route, we recommend going up to Puig Nunó and enjoy the panoramic view of the western part of Eivissa, which includes the Bay of Portmany and Sa Foradada.
Three different units can be identified:
• The Miocene conglomerates from Cap Negret almost to Punta de sa Galera, with a massive appearance or in strata of one or two metres in top of a stratigraphical unit or stratigraphical sequence. </p></div>">thickness. It brings grey tones to the landscape.
• The Miocene calcarenites that appear from Punta de sa Galera to Racó de Cala Llosar. They appear stratified within decimetric or metric layers. They are grey and ochre in colour.
• The Cretaceous fossiliferous limestones described in stop 2 of the itinerary.
Panoramic view from Puig Nunó with a schematic cartography of the outcrop materials (point A).
