The sea-cliffs and the beach
 

The S. Bartolo sea-cliff emerges from the low Romagna-Marche beaches in an undulating continuous series of spurs and valleculas that slope down to the sea, alternated here and there by sheer cliffs supported by a horizontally, or "reggipoggio" positioned stratification. Where the alternation of the sandy banks, marls and clays is not supported by the position, it slopes more gently to the sea and it mixes with the ancient landslides which cover the cliffs. The elevations of the higher peaks behind the cliffs, like Mt. Castellaro or Mt. Brisighella, do not reach 200 metres, but they offer a wide view of the coast and sea, while the plunging cliffs of the Park are part of an unusual marine landscape for the sandy coasts of Romagna and the Marche. The sea-cliff presents very interesting aspects from a geological viewpoint with fish fossils and rare gypsum crystals, in fibrous or lens form, like sericolitis. A narrow beach runs along the base of the sea-cliff; the pebble and gravel of the beach are the result of the degradation and crumbling of the overhanging walls of the cliff.

The golden yellow colour of the "cogoli" stands out among the stones along the shore: rounded stones frequently odd in shape, locally known as "cogoli" which are the result of a particular lithogenesis which chemically aggregates the sand into these spherical shapes. The pebble beach hosts unusual and rare, shore environment marine biocoenesis; in the past it was used as a convenient gravel and stone quarry for paving materials loaded directly onto the ships. Historical documents are testimony that this activity was carried out for several hundred years, with exportation of material to Ravenna, Rimini and the other coastal cities; towards the end of the late 1900s this quarry shipping activity came to an end. In fact, the old cobblestone streets of the city of Pesaro and park villages were, at one time, constructed from these stones. Over the centuries, this activity was not beneficial to the current stability of the coastal strip of the sea-cliff; instead, it definitely accelerated the erosion process and in recent years this has led to the need for interventions at sea through surface and submersed reefs, and consolidation of the steep cliff walls to safeguard the local population.
The dynamics of the sea-cliff and the composition of the terrain which forms it conditions the vegetation. In fact, both the steep nature of some of the cliffs as well as the essentially mineral character of the substrate, are only sufficient for a pioneering vegetation mostly made up of Plinio Reed (Arundo plinii), which represents the most extensive natural typology of the territory. The character of this initial stage tends to remain constant in the steeper slopes where frequent slides and crumbling impede the cane thicket from evolving to more advances stages; in the dryer, more stable soil we find Perfumed Broom (Spartium Junceum), and where the slope is less steep and a certain amount of humus accumulates, it is possible to find madder (Rubia peregrina), Etruscan honeysuckle (lonicera etrusca), young Aleppo pine plants (Pinus halepensis) certainly originating from spontaneous insemination following reafforestation.
In the valley lines which retain more humidity even during the dry summer months, there are white poplar, black poplar and, more rarely, white willow. Arundo donax is more common is several areas. There are also rare species like maritime flax (Linum maritimum)
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