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THE PARK TERRITORY
In the North of Ombrone
There is a plain covered by Paludi della Trappola: that
is a system of stretches of water, partly seasonal and partly
permanent (the so-called "chiari" or "bozzi")
alternating with not very evident dunes. A typical feature
of this Park area is the presence of Maremma cattle bred
in a wild state all year round. The inland waters house
several migratory aquatic birds during the winter, but
other avifauna species live here all year round. The farthest
lands from the see have been subject to reclamation activities,
and are now covered by agricultural fields and modern zootechnical
breedings. The territory described forms part of the delta
of Ombrone, a stretch of which cuts with meanders the Park
territory.
On the Left of the Mouth of Ombrone
On the left of the mouth of the river Ombrone there is
a territory characterized by a compact system of dunes
alternating
with marshy grounds of limited size and mainly covered
with a pinewood. The Stone Pine wood is separated from
the sea by a strip of Maritime Pines having the function
to protect the territory from the harmful action of the
salty winds. This area is crossed by some artificial
canals dating back to the 18th-century first land reclamations.
The Park Central and Southern Area
The central and southern Park areas are dominated by Monti
dell'Uccellina, that is a system of mountains, partly
of calcareous nature and partly siliceous, reaching the
417
meters of Poggio Lecci. These mountains are today almost
completely covered with a thick forest vegetation (Mediterranean
maquis). Only the lower part of the slopes has been deforested
and transformed into olive grove or pasture. On Uccellina
Mountains there are ancient religious towers and buildings
witnessing the past human presence and activity in the
area: the Abbey of San Rabano - which is very damaged
- and the towers of Castelmarino, Collelungo, Cala di
Forno,
and Bella Marsilia. The human history is not only reminded
by the medieval remains: in Talamone there are the remains
of a Roman villa, while in the caves forming at the foot
of the calcareous cliffs some prehistorical evidences
dating back to the Paleolithic period have been found.
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