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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.

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