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The meeting place is in
Levigliani di Stazzema. You can reach it following the provincial road
to Arni, which goes through Seravezza, Ruosina and Retignano, and, on
the hydrographic right, goes up the valley of the stream Vezza.
Levigliani is a small village situated on an
orographic terrace, at 600 m of altitude, at the bottom of the lofty
towering walls characterising the southern side of the Mount Corchia
(1678 m). The cave’s
tourist entrance is more than 2 km far from the built-up area. You can
reach it in few minutes and after some sharp turns, following a
marble-road, going up to the altitude of 860 m.
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The artificial entrance of
the Corchia’s cave is situated inside an old quarry. The connection
gallery looks like the natural subterranean
continuation of the external front of the quarry itself.
The route goes on slightly uphill for about 170 m in
length, getting over a difference in height of about 20 m. The depth
of the artificial duct is not fully perceivable because of the
presence of a sequence of three doors dividing as many stretches of
the gallery, and closing it “air tight”. The aim is that of
controlling the draught exchanges between the inside and the outside
environment.
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As you enter the karst cave, you immediately enjoy, on your right, the
sight of a squat conoidal stalagmitic concretion called “The
gendarme”. Your progression inside the cave is now made easier by the
presence of gangways in the shape of bridges, flights and large steps.
Avoiding the contact with the bottom of the cave, they have moderated the
transformation of the karst system, caused by the presence of tourists.
Through a difference in height of 37 m and the presence of 212 steps, the
route develops in a difficult descent down the so-called “Galleria
Franosa” (the Landslides Gallery), whose middle stretch is made of a
single stunning and narrow space. This is over 30 m high and never larger
than 4 m, even though it can shrink to 150 cm. The spot, originated from a
large vertical fracture, is characterised by walls, that, nowadays, are
fairly wavy, and present, here and there, large and deep sub-horizontal
engravings.
The so-called “Galleria Franosa” (the Landslides Gallery) ends at an
height of 843 m., in a widening characterised by deposits of masses on the
vault. Here is the starting point of the so-called “Galleria degli
Inglesi” (the English Gallery) and that of the way in to the so-called
“Pozzo Suzanne” (the Shaft Suzanne).
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The equipped stretch of
the “English Gallery” is 245 m long. It is part of a network of
straight, horizontal and overlapping ducts originated on the layer of
a single sub-vertical fracture. This underwent to a subsequent
enlargement caused by chemical and mechanical phenomena. The two main
galleries are divided, even though many points of connection are
present along the route. These vertical links are more evident after
the middle of the route, where the cave’s vault rises as far as the
higher ducts. Right here the English Gallery is interrupted by small
drops made of blocks fallen down to the ground.
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Along this stretch of the
route, the walls of the cave are covered with small regular hollows called
“Scallops”. They have different dimensions and are the result of the
ancient tumultuous flowing of the subterranean waters.
At the end of the so-called “Galleria degli
Inglesi” (the English Gallery), on your left, a small waterfall falls
down a high vent, so engraving the wall in large grooves. As it reaches the height of 859 m, the equipped route avoids
to keep going straight on towards the so-called “Risalita dei Romani”
(the Romans climb). |
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The route bends on the
right to reach the entrance of the so-called “Galleria del Venerd́”
(the Friday Gallery) through a narrow passage which swerves on the
opposite side.
This gallery is 261 m long and has a phreatic origin. The duct turns left
at one third of its length, where the opposite wall offers a lofty
flowing-like concretion, in the shape of an eagle spreading its wing
to fly. Beside this concretion, there is a stalagmitic gorge,
sustained by a calcareous column, commonly known as “Capanna
Trogloditica” (the Troglodytical Hut).
After about 75 m., the route reaches the so-called
“Laghetto del Venerd́” (the Friday Small Lake). Here the waters
are not very deep even though they are crossable only with the help of
a bridge grounded on the opposite sandy shore. This little spot has
always been a camp frequented by speleologists; at least so it seems
judging by the countless overlapping writings on the walls.
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1)
The route reaches a narrow
and steep gorge. Here flows the water of a small stream, which keeps going
right, inside the so-called “Pozzo della Gronda” (the Gronda’s Shaft)
(also known as “Pozzo della Cascata” - the Waterfall Shaft). There has
its origin that long sloping branch of the Corchia’s cave, which ends at
the cave’s bottom, at about 450 m of height.
It is suggested to keep right, where the route
penetrates with much more ease inside the suggestive “Galleria delle
Stalattiti” (the Stalactites Gallery). However, there is also a sort of
concretionary hall to pass
through, which is, nowadays, entirely fossilized. It is the so-called
“Foresta pietrificata” (the Fossilized Forest): situated on the
opposite side of the route, it is characterized by stalactites and
stalagmites marked by their bulging shapes an their raw-amber colour. Here
the water stopped to flow and no drop enlivens the concretions any more.
Even though these concretions are so thick here, to almost block the way,
the gangways let you pass through this stiffened and dusty world,
zigzagging in all the possible directions. At the deepest point of the
Corchia’s cave, the walls ooze with the damp coming from the active
phreatic levels situated further. |
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A big runoff boulder,
together with a peculiarly shaped stalagmite situated on it, serves as a
sort of architrave to the entrance door of the part of the so-called
(Galleria delle Stalattiti” (the Stalactites Gallery) ’which is still
alive. According to the definition by Jean-Carlo Fait
(speleologist) this spot is to be considered an oasis of rare
beauty in the middle of a world made of stone, mud and water. These places
are so deeply suggestive, that, nowadays, only a few other subterranean
halls in the world are comparable with them.
Because of the chromatic richness and the variety of
shapes originated here, it is extremely difficult to describe what catches
the eye in this spot. The concretions jostle the one on the other, they
descend down the walls and dive in small puddles of clear water. The stone
laces characterising some calcite fans, show the alternation of their
multi-coloured layers. The stalactites drapery skims a stalagmite covered
with calcareous nodules. In the background, a single pillar seems to
sustain the vault in this place of aesthetical sublimation. |
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The so-called “Galleria
delle Stalattiti” (the Stalactites Gallery) is a characteristic
phreatic flue, situated at a medium height of 871 m., where the
precipitation of carbonate minerals is still active. Even here, the
equipped route is properly shaped so as to penetrate amidst the
concretions with due respect. Finally, the route keeps going down a
short sloping stretch, which is crossed by a small stream flowing like
a small waterfall, and where runoff boulders shrink the path.
Then, the route, which becomes level and smooth
again, re-approaches the closing point of the ring. Here, on the left,
you have the opportunity to enjoy again the “Eden” of the
stalactites, while, on the right, you face the return to the earthly
things.
Extract
made by: Mr. Antonio Bartelletti, Mrs. Alessia Amorfini, “The Mount
Corchia-In the heart of the Apuan Alps”. “The trekking journal”, XVIII
(8), n°149 (September, 2001), pp. 62-75.
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