세니야‬에서 가장 멋진 ‪20‬개의 천연기념물

The Calpe salt flats occupy a depression filled with Quaternary alluvial deposits. The position of the Peñón de Ifach is a decisive factor in the formation of this interesting wetland. It is a lagoon of tombolic origin, created from the development of a double sandbar.

Beautiful view. I go there all the time.

Great view

The summit of Peñón de Ifach is 332 meters above sea level. To reach the top, follow the Red Route of the Peñón de Ifach Natural Park. This route begins at the visitor center and passes through a tunnel before reaching the summit. The hike is challenging, especially after the tunnel, where the terrain becomes steeper and more slippery. Hands are required for support in some places, as is appropriate footwear. The views from the summit are spectacular, offering panoramic views of the Mediterranean Sea and the Calpe coast.

The salt flats of Calpe were used for salt production as early as Roman times and were in operation until the 20th century. Today, they are a protected nature reserve and provide a protected habitat for numerous animal species. They are particularly known for their flamingos and other waterfowl, making them an ideal spot for birdwatchers. Paths surrounding the salt flats offer impressive views of the Peñón de Ifach.

Climbing to the top of the Peñón de Ifach is one of the most stunning hikes on the Costa Blanca. It's a somewhat difficult route, due to the steepness and rugged terrain. Once at the summit, however, the effort is worth it, as you'll enjoy spectacular views.

The Calpe Salt Flats occupy a depression filled with Quaternary alluvial deposits. The position of the Peñón de Ifach is a decisive factor in the formation of this interesting wetland. It is a lagoon of tombolic origin, generated from the development of a double sandbank.

The Calpe Salt Flats occupy a depression filled with Quaternary alluvial deposits. The position of the Peñón de Ifach is a decisive factor in the formation of this interesting wetland. It is a lagoon of tombolic origin, generated from the development of a double sandbank.