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florescina Gesso

Monday 25 July 21.00 Resorts' The Chalk

Plaster and unblocking of the entry of 'been done!
With technical support of Mark and Max (the group of Forli), we have the rock that crumbled lettaralmente ustruiva the entrance of the cave. The surprise of the obstruction and
mara 'Conspicuous for Saturday morning when I Andrea Benassi, Marco Marbagli we went to the cave to make some pictures and color in order to fully understand the flow of water inside the cave.
The first to come on Saturday and 'Andrea was that after 10 seconds said: Guys you have done it last Saturday you put a nice cap!
said and done ... we went home immediately.
Monday evening in 20 minutes we have solved the problem! Gia 'that we were there we decided to go for a ride to complete the job left unfinished.
100 g florescina to check the flow of our hope.
captors in the hope, we will analyze them short.
... For photos .... there 'time, this cave is giving its promises and much.
A further thanks to our friends at Forli THANKS MARCO MAX &

hello Raga

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Er bo 530 - sinkhole of gessoQuasi on the extreme western edge of the vein, between the valleys of Sillaro and Santerno, we find the inghiottioio of Gesso. With a development of over 300 meters, is part of a system that is currently feasible with the er bo 707 drains the waters of a vast grassy basin towards the Chalk cave resurgence of Er. Bo 455. Developed in saccharoid microcrystalline gypsum, the cavity opens onto the bottom of a sinkhole in the area Pogianeto; a tunnel between fossil landslide can reach in about a P5 that leads into a small room with some arrivals. From here, the tunnel is enlarged and shows the first signs of water circulation. Follow it up to a large room where a landslide step down, sometimes siphon, leads directly to a P10 that develops in the room. The well represents the core of the cave, as it intercepts the stream of the collector system. A valley is passable for 15-20 meters up close semisifonante mill that is the point Deep -35. Upstream you can instead go up the stream, after a sudden landslide in flow in a comfortable tunnel-maze, plenty of concretions. Continuing up the river divides into several arrivals after a section made up of high-tunnel maze, go back quickly to tighten up the surface debris and clay.
Er bo formed by the P10 707 that closes on narrow, drains water from the basin which feeds the stream inside.
History esplorazionila cave was explored and taken to the room above the landslide group P10 CAI Speleological Enal Faenza in 1974. Always re-explore in 1988 the group found that Faenza continued to reach the river but failed to detect because suddenly closed by landslides. In the '90s and was erroneously cadastre as duplicate of herself as a sinkhole of pogianeto and taken back to the room. Finally, re-explore and fully recorded in July 2008 by the Speleological Society and Saknussem ricastata with the original name of er bo 530 gypsum sinkhole.