Introduction
Dent de Crolles is the high point of an extensive massif in the Chartreuse hills of the French Prealps. It has a summit of 2,062 metres that dominates the Grésivaudan valley to the south, whilst to the north a tilted synclinal plateau, protected by high cliffs on the west and east, descends for 1½ km to the edge of a cliff-encircled cirque overlooking the Perquelin valley, some 3 km ESE of St. Pierre de Chartreuse. To the south-west of the summit, a road pass ascends to 1,434 m at the Col du Coq, allowing easy access to the plateau along the waymarked GR9 footpath. The hill owes its name to its resemblance to a giant molar when seen from the village of Crolles in the valley below.
Col du Coq is bottom centre, and Perquelin right of top centre
Mesozoic in age, Dent de Crolles is capped by limestones deposited during the Aptian and Berremian stages of the Early Cretaceous between about 110 and 120 million years ago, underlain by impervious Hauterivian marls. The limestones are honeycombed by an extensive cave system, the Réseau de la Dent de Crolles. This has over 60 km of passages contained within an area of under 2 km²; and eleven entrances including the resurgence (Grotte du Guiers Mort, 1332 m), and a top entrance located just 175 m from the summit (Gouffre Bob Vouay, 2022 m). It contains a number of active systems that drain into a master cave, and a number of far older large fossil phreatic passages formed from the late-Miocene onwards which drained a landscape long disappeared. These were truncated during the Quaternary glaciations, and now have large entrances overlooking deep valleys in the east,south, and north cliffs of the massif. The fossil passages have been intercepted by the active systems to create a vast interconnected network the plan survey of which has been likened to a plate of spaghetti. Although the limestone beds are only about 450 metres thick, the local geological structures means that the system is only a little shy of 700 metres deep.
The highest entrance is near the col left of top centre, and the resurgence is bottom right of centre
The Réseau de la Dent de Crolles provides perfect holiday caving, with a large number of classic through trips and round trips available of varying degrees of difficulty, as well as providing scope for more challenging expedition-style caving. It is possible to traverse from the top of the mountain to near its base, and through the mountain from one side to the other, and combinations of the two. Several of the more popular routes are waymarked and superbly equipped with pull-through chains and traverse lines. Some of the through-trips take around 4 hours, and others over 12 hours. All the entrances are reasonably accessible with the walk-ins varying between about ¾ of an hour, and two hours.
The purpose of this website is to pull together the latest pertinent information on the cave, and to clarify the locations of the entrances. Please look at the Sources of information page for a summary of available material, much of it on the web.
As of 2017 the following 11 entrances, ordered by altitude, are known. Those with links are discussed further on this site. The locations can seen displayed on the IGN Géoportail aerial photography website, based on work by Gilbert Bohec.
| Name | Northing | Easting | Altitude | Linked | Notes |
|---|---|---|---|---|---|
| Gouffre Bob Vouay 3 | 45.30960° | 5.85445° | 2,022 m | 2009 | 175 m from and 40 m below the summit Links with Trou du Glaz and Grotte Chevalier |
| Gouffre des Quanta 4 | 45.31679° | 5.86455° | 1,937 m | 2001 | About 160 m south of Gouffre Thérèse Links with Grotte du Guiers Mort Accessed by a 50 m abseil down the eastern cliffs |
| P40 1 | 45.31259° | 5.85357° | 1,930 m | 1947 | Equipped route to Trou du Glaz |
| Gouffre Thérèse 1 | 45.31821° | 5.86458° | 1,925 m | 1975 | Equipped route to Grotte du Guiers Mort |
| Gouffre de la Pulpite Irréversible 3 | 45.31407° | 5.85586° | 1,901 m | 2010 | Equipped route to Trou du Glaz. Also links with Grotte du Guiers Mort |
| Puits des Cartusiens 2 | 45.32081° | 5.86179° | 1,780 m | 2007 | Links with Grotte du Guiers Mort |
| Grotte des Montagnards 5 | 45.309° | 5.858° | 1,765 m | 1996 | Entered and linked with Grotte Chevalier in 1966 Accessed by an 80 m hard rock climb on the eastern face |
| Trou du Glaz 2 | 45.31736° | 5.85146° | 1,697 m | ---- | Equipped routes to Guiers Mort, Annette and Chevalier Exit for equipped routes from P40 and Gouffre Pulpite Equipped round trip Link with Gouffre Bob Vouay |
| Grotte Annette Bouchacourt 4 | 45.30599° | 5.85375° | 1,685 m | 1946 | Exit for equipped route from Trou du Glaz |
| Grotte Chevalier 4 | 45.30669° | 5.85468° | 1,670 m | 1984 | Exit for equipped route from Trou du Glaz Links with Bob Vouay and Grotte des Montagnards |
| Grotte du Guiers Mort 4 | 45.32611° | 5.85757° | 1,332 m | 1941 | Exit for equipped routes from Trou du Glaz and Thérèse Also links with Gouffres Quanta, Cartusiens, and Pulpite Two equipped round trips |
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1 Location from Spéléo Secours Isère route guide 2 Location from Gilbert Bohec's survey 3 Location from author's GPS reading 4 Location supplied by Gilbert Bohec 5 Location estimated from Gilbert Bohec's survey |
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The following files are available for importing entrance location details:
- Reseau de la Dent de Crolles.gpx - for importing into GPS and Memory-Map etc. (5.1 kB)
- Reseau de la Dent de Crolles.kmz - for importing into Google Earth (1.9 kB).
In addition to the caving, the area also offers magnificent walking, as well as ample opportunities for big route climbing, sport climbing, canyoning, and via ferratas. For more information on the area consult the author's Chartreuse website.
Acknowledgements
I would like to thank Gilbert Bohec, Dagobert L'Ecluse, and Glenn Jones for their help and advice given during the development of this website; Dave Checkley, Graham Coates, Stuart Hesletine and Pete Monk for their kind permission to use their photographs; and the various authors and organisations who have generously shared the results of their expertise on the Web. Errors and omissions are all mine.