BurtignySwitzerland 46° N · 6° E Verified Aug 2026
A glacial erratic in the Jura forest whose 'serpent' mark is natural erosion, not legend. It survived because it was too remote to quarry for building stone.
The most unremarkable stone in a Swiss forest is also a refugee from the Alps. Pierre du Serpent, tucked at the edge of the Bois des Tattes above Burtigny in Vaud, Switzerland, is a glacial erratic — a fragment of Alpine granite that the Rhône glacier set down here around 20,000 years ago. You visit not to see a monument, but to stand next to evidence of how far ice can carry a mountain.
The stone is small enough to miss. From the forest edge, take the little path behind the picnic table; the block sits roughly twenty metres in, unassuming. Look closely and you may find what earlier observers swore were a human footprint and a serpent's trace. The on-site panel records a less romantic verdict: the shapes are probably the work of erosion and time.
That shift — from mythical serpent to natural scar — echoes a larger scientific fight. For much of the nineteenth century, folk explanations clung to such boulders. Then geologists, most publicly Louis Agassiz, argued that ice had done the transporting. Pierre du Serpent stopped looking like magic and started looking like machinery.
Most of its cousins vanished into Vaud's villages. Hard Alpine granite was valuable stuff — too valuable to leave lying around — and accessible blocks were quarried for foundations, doorsteps and stair steps. This one survived because it was too far into the trees to bother with. Boring, in other words, became its best defence.
History
Most tourist histories open with a foundation date. Pierre du Serpent has none, because it was never built. It was dropped.
That happened about 20,000 years ago, when the Rhône glacier reached roughly 1,000 metres along the Jura chain and stretched toward Lyon. As the ice thinned, it let go of this Alpine granite block and left it at the edge of what is now the Bois des Tattes.
The turning point
Louis Agassiz (1807–1873) does not appear in the local record for this exact stone. He doesn't need to. The Swiss naturalist and Neuchâtel professor was among the most public champions of the idea that vast ice sheets had once smothered Switzerland, and erratic boulders like this one were the physical proof he pointed to.
What was at stake for Agassiz was his reputation. In the late 1830s, the notion of a continent-wide Ice Age sounded absurd to many geologists; accepting it meant rewriting the planet's recent past. His turning point came as evidence accumulated — the Jura's scattered Alpine fragments stopped looking like folk curiosities and started looking like a delivery system.
Burtigny's own trail literature records that glacial theory only imposed itself in the mid-19th century. So a visitor at Pierre du Serpent is standing on the winning side of a fight that once seemed almost impossible to win.
Only if you pair it with the Sentier des Pierres loop. By itself the boulder is small and easy to walk past. With the 4 km circuit of erratics and the giant fir, it makes a fine quiet afternoon.
Fifteen to thirty minutes if you're only seeing the stone. The full Sentier des Pierres loop runs about 4 km and takes 1h15 to 1h30. That's the better use of your time.
Drive or walk out of Burtigny on Route des Matagasses, continue onto Route du Molard, then turn left at the farm called Sur la Motte. Park at the forest edge and take the small path behind the picnic table; the stone sits about 20 metres in. No direct public transport to the boulder appears in local sources.
March to October, with autumn as the standout. After rain, the granite darkens and the serpent groove becomes easier to trace. Snow can hide the mark in winter.
Yes, it's free and always open. There's no ticket office, visitor centre, or gate. You just follow the forest path to the boulder.
The serpent groove on the rock surface, best seen when the granite is wet. Run your fingers over the coarse crystals and look for the fainter footprint-like hollow nearby. If you walk the loop, don't skip the giant fir that hikers point to as the largest in the forest.
A small glacial erratic boulder of Alpine granite, dropped by the Rhône glacier roughly 20,000 years ago on the Jura slopes above Burtigny. It sits at 807 m at the forest edge. The local panel says the serpent and footprint marks are probably natural erosion, not carvings.
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