LE STRADE DEI PARCHI - Naturainviaggio.It
LE STRADE DEI PARCHI - Naturainviaggio.It
LE STRADE DEI PARCHI - Naturainviaggio.It
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76<br />
Tratto VICOVARO - JENNE<br />
Arsoli Jenne<br />
Another destination is the top of the Autore Mountain (1855 metres), the highest<br />
peak of the province of Rome, from which it is possible to take in at a glance<br />
almost an entire drainage basin (the one of the Simbrivio river) and where in<br />
clear days the view sweeps over half Central <strong>It</strong>aly, from the Gran Sasso peak to<br />
the Tyhrrenian sea.<br />
From Livata one carries on toward the village of Jenne till he reaches another<br />
area shaped by the karst process and surrounded by beech trees. <strong>It</strong> is the Fondi<br />
Plain where, close to an ancient forest refuge, it’s possible to take a rest sitting at<br />
the tables of a pic-nic area.<br />
All around there are lots of signs of karst phenomena, caused by the slow rainwater<br />
capacity to melt calcareous rocks in order to seep through them. Dolines,<br />
ground depressions of variable size and depth, form because of the intense flowing<br />
of water to one absorption point (swallow-hole). Karst plateaus, big basins<br />
surrounded by high grounds and devoid of any water course trace, are generated,<br />
as time goes by, when different dolines join up.<br />
About a kilometre after the Fondi Plain a path on the right leads to the entrance of<br />
the so called Red Clay Pit, completely fenced for security reasons. <strong>It</strong>’s a vertical karst<br />
well, accessible only by experienced speleologists, that goes down in different parts for<br />
a total depth of 117 metres.<br />
<strong>It</strong>s presence, as well as the one of many other caves, is the result of the fact that karst<br />
phenomena seep through and go down to depth, in the heart of mountain ranges,<br />
where the water, filtering into the cracks, keeps on corroding the limestones. In this<br />
way, extended systems of underground spaces form (pits, galleries, rooms, passages),<br />
often communicating.<br />
Deep karst phenomena are fully developed in the Simbruini area. Among more<br />
than a hundred explored cavities the most important are the Inferniglio Cave<br />
nearby Jenne, expanding almost at the same level for about 1,4 km, and the Camposecco<br />
Swallow-hole that goes down to a depth of 415 metres.