0098: Bollón, Cueva de (Volvo, Cueva de)
La Secada 30T 452048 4797721 (Datum: ETRS89. Accuracy code: M) Altitude 165m
Length included in site 1452
Area position

Updated 17th December 1999; 14th May 2000; 21st January, 7th October 2001; 15th October , 8th November 2003; 1st February, 20th May 2006; 27th October 2007; 3rd November 2009; 6th January 2011; 13th September 2013; 5th February 2017; 1st July 2018

The entrance is most easily approached by walking down off the road about 100m east of the entrance then walking parallel to the road until a small valley is met. the entrance is at the top of this, under the road. The cave acts as a resurgence and floods completely in very wet weather, water resurging at the base of the valley.

A descending rift leads to a mixture of walking and muddy crawling for 70m until a chamber is reached. By sliding down to the left, deepening water leads to a 3m sump which is not free-divable. This was passed in the summer of 1994 to another stretch of passage ending at a promising sump. At the end of summer 1995 expedition, this had dried out somewhat to become muddy wriggle to a steep, muddy climb out. Approximately 120m of westerly- trending, sand and mud-floored passage, ends at sump 3. Some 40m from sump 2, a passage leads off to the north for 30m ending at a boulder-filled pool.

Just before sump one, on the right hand side, a nasty, wet, strongly draughting crawl was dug through to Passage of Slime and a muddy boulder choke. This is passed by a squeeze and climb up to high level. Around here are two climbs: the first is 20m in bad rock; the second needs a couple of bolts and is safer. The draught can be followed down to a large choked chamber with two avens. One goes to a chamber with two over tight passages. The second could not be protected due to bad rock. "This area needs a return trip."
A return happened at the end of July 2013 where 65m of passage were surveyed (batch 13-01). This is described as narrowing down after the first pool and becoming very narrow and tight at the end of the crawl (about 20cm) before opening up into 30m of very muddy passage. The route reaches a small chamber at the end where it closed down into an impassable section that could possibly be dug. A noticeable draught was felt. It appears that the boulder choke and climbs have not been reached.

To the right of the chamber, a tight squeeze at floor level on the left of the passage leads to a succession of muddy chambers. One impassable crawl at floor level in this section has a very strong draught. Other minor extensions have been made (including a couple of avens - Phil Boardman - are these on the survey?)
The passage heading east was pushed in the summer, 2013, in continuing small passage. The way on is currently blocked by a boulder approximately 1m3 in size. The way on is to the right of the boulder. A good draught can be felt and the route definitely continues. A new 48m was surveyed as batch 13-02.

The villagers claim that this cave connects with the sea, as on the occasions that it acts as a flood resurgence, it washes out quantities of sand and shells. The end of the eastern branch appears to lie only 50 - 70m away from the western extremities of the Western Series in Cueva de Carcavuezo (081).

In 1999 sump 3 was passed and all sumps were described as free divable with the summer water levels. Beyond sump 3, 40m of walking and stooping passage leads to the base of a steep boulder slope. There is a large amount of collapse debris and care should be taken. A short traverse around to the right at the top of the first slope leads to an eyehole 6m from the far wall where it is possible to climb down to a section of passage containing large, old stal which has fallen. Straight ahead is a blank wall but to the left is a second slope of about 30 degrees leading past a small bunch of helictites before emerging on a sandy plateau. The slope continues upwards beyond this where a Yorkshire pot-type inlet is seen on the right and other possible inlets are seen in the roof. (Explorations in this area are usually carried out through Hole-in-the-Road, site 1452).

This area is beneath sites 1452 and 898 and draughts. There are many leads and crannies to examine throughout the cave including the streamway continuation beneath boulders before the climb up (see below).

At Easter 2000, site 1452 was linked in via a 35m pitch to where it is possible to swing across to link with the slope. Heavy rain a couple of weeks before meant that the water levels were high at the base of the slope and it was impossible to investigate upstream.
In the dry summer of 2001 this area could be investigated: 82m of loose, draughting, bouldery passage was surveyed. This could possibly be pushed by removing some of the boulders blocking the route on.
During the very dry summer of 2003, the bouldery area down the slope was pushed further. A squeeze down under boulders to the left at the last survey point leads to a 45 degree rift with an unexplored hole down. Over the top leads to boulders leading eventually to a crawl under solid walls witha gravel bottom. The passage then opens out and enters a reasonably big stream passage down a ramp. This is followed keeping to the left hand side into large passage. On the right avens can be seen up mud slopes. The continuing cave ends at a large boulder collapse.
Directly above the last survey station is an aven with water dripping down. The boulder collapse can be climbed up about 15m with a small hole in the ceiling and a slight draught between boulders. At stream level a squeeze gains a small chamber with a 5cm wide slot giving a view down to the streamway. The extension length amounted to some 252m. Further extensions in 2009 are described under site 1452.

References: Fernández Gutiérrez et al, 1966 (survey); anon., 1974b (logbook); anon., 1974a; Cox G, 1973; anon., 1975b (logbook); Kendal Caving Club and Manchester University Speleological Society, 1975 (survey); anon., 1980a (logbook); Corrin J S and Smith P, 1981; anon., 1984 (logbook); anon., 1985b (logbook); anon., 1987 (logbook); Corrin J and Knights S, 1988 (survey); anon., 1988 (logbook); Davis J and Corrin J, 1989 (survey); anon., 1989 (logbook); anon., 1993b (logbook); material in file; anon., 1994b (logbook); Corrin J, 1994b (survey); anon., 1995c (logbook); Corrin Juan, 1995a; Corrin Juan, 1996; anon., 1999c (logbook); Corrin Juan, 2000; anon., 2000b (Easter logbook); Corrin Juan, 2000; anon., 2001c (Summer logbook); Corrin Juan, 2003a; anon., 2003c (summer logbook); Corrin Juan, 2005; anon., 2006 (Easter logbook); Corrin Juan, 2007; Corrin Juan and Smith Peter, 2007; anon., 2009c (summer logbook); Corrin Juan, 2010; León García José, 2010 (survey and photo); Corrin Juan, 2011; anon., 2013d (summer logbook); Papard Philip, Corrin Juan and Smith Peter, 2014; anon., 2017a (January, February logbook)
Entrance pictures : January 2017
Underground picture(s):
Detailed Survey :
1964 known cave low res high res
1975 known cave low res high res
1999 known cave 1:1000
2003 known cave 1:1000
2013 known cave 1:1000

Line Survey :
On area survey :
Survex file: combined with site 1452 (Amended magnetic declination December 2013 to align with Eur79 grid and coordinates altered to fit ETRS89 datum, April 2014.)
Passage direction rose diagram: yes, with Hole in the Road 1/7/2018

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