Lac du Génépy
Walking hike
Lac du Génépy

Lac du Génépy

Lake and glacier
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From the cembra pine forest to the glacial cirque, a journey of 3,000 km to to the north over a 3 hour walk.
The date on the calendar indicated the 14th July on this morning... There is not a ripple of water on the Génépy lake despite the gusting northerly winds. This is because a thick layer of ice covers the lake. The varying colours of the mineral world around me transect the swirls of fresh snow. This is where you go up to the Lac du Génépy, starting out from the forest in your short sleeves until you end up thinking you’re crossing the rocky stretches of Iceland, where the plants have adapted in mad-cap fashion to cling to these rocky mounds. Here the birds no longer sing, only the ringing sounds of the alpine choughs and the guttural sounds of the ptarmigan resonate. Mathieu Beurier – National Park Ranger


"From the car park, follow the route of the Refuge de la Dent Parrachée. Behind it, the trail is indicated by the National Park’s yellow signs.Follow the direction for ""Lac du Génépy"". After about 30 minutes, cross the footbridge and continue the trail to the lake. To return, follow the same path. Just before the Refuge de la Dent Parrachée, turn right towards the Fond d´Aussois. Be careful, after 300 m, a short passage requires vigilance. Follow the trail to a footbridge that you leave on its right and continue south to the GR5 intersection. Then turn right and go down to the bridge you have to cross, follow the direction for Aussois until the Plan d´Amont dam from where you reach the car park."
  • Departure : Dam site, village of Aussois
  • Arrival : Dam site, village of Aussois
  • Towns crossed : AUSSOIS

Altimetric profile


High mountain route to be prepared in advance. Make sure you have the appropriate equipment and footwear and an IGN map for navigating. The weather in the mountains can change very quickly and you should turn around if it is bad.
Is in the midst of the park
The national park is an unrestricted natural area but subjected to regulations which must be known by all visitors.

Information desks

Maison Cantonale, 9 Place Sommeiller, 73500 Modane

https://www.cchautemaurienne.cominfo@cchmv.fr04 79 05 26 67

43 route des Barrages, 73500 Aussois

https://www.aussois.cominfo@hautemaurienne.com04 79 05 99 06

Maison cantonale - Place sommeiller, 73500 Modane

https://www.vanoise-parcnational.fr04 79 62 30 54


Rail connection to Modane. Information:
Then transport by coach to the administrative centre of Aussois. Information:
No public transport between Aussois and the dam site.
Suggested hitchhiking organised in the Haute-Maurienne valley. Information:

Access and parking

In Modane, take the D 215 towards Aussois. Once you’ve arrived in Aussois, go to the top of the village and take the small road that rises towards the dams. Leave a panoramic viewpoint on the left and take a steep road on the right for 100 m to reach the car park.

Parking :

Car park provided by the municipality for the entire dam site, departure point for all hikes.


The terminal car park is equipped with amenities but is not beyond the trail described in this record.
Emergency number :114

10 points of interest

  • Fauna

    The spotted nutcracker

    This bird, with its robust beak and aptitude at opening the cones of the cembro pine, feeds almost exclusively on its seeds. It alerts visitors to the forest of its presence by its gravelly and discordant cry. Ÿou may be able to see the spotted nutcracker towards the end of summer, flitting from one pine to another to extract its seeds. He then hides them in bundles in the soil which he will then find again in the winter. The spotted nutcracker is able to memorise several hundred of these hiding places and find them under the snow. The very few caches that have been forgotten will perhaps provide new small cembro pines. The cembro pines benefit greatly from this association, known as symbiosis.
  • Flora

    The lilium martagon

    In June to July when you leave the forest and set foot on the mountain pastures, you may find a large plant with purple flowers. The lilium martagon, a rare species, colonises the clearings of the forest boundary. It favours so-called mespophilic meadows that are neither too dry or too moist. This plant, once picked, was threatened. It is now out of danger but will require, like other species, much respect on your part.
  • Pastoralism

    Agricultural decline

    Ÿou will notice on both sides of the trail, towards the Randolière, numerous small cembro pines, established in the middle of the pastures. Whereas the entire slope was once grazed and mown, the gradual disappearance of small farm holdings and the change in practices have encouraged this forest species to recolonise the area. Over time, if agriculture were to disappear, it’s in the forest that you would find yourself. The loss of these pasture lands will lead to a decline in biodiversity.
  • Viewpoint

    Lakes of the Aussois dam

    Downhill behind you, you will be able to see the lakes of the Aussois dams. The Plan d’Amont is remarkable for its turquoise colour, fed only by the melting snows and clear streams. Downstream, the Vanoise glaciers feed the lake thanks to 19 km of underground tunnels originating from the Doron de Termignon. The water is loaded with glacial “flour”, fine mineral particles torn from the mountains. This is what gives the Plan d’Aval its grey, milky colour.
  • Fauna

    The common rock thrush

    This colourful bird did not escape from a garden centre. Despite spending its winter in Sub-Saharan Africa, the common rock thrush regularly inhabits the dry rocky and sunny slopes of our mountains to breed. While it can feed on small lizards and seeds or fruit, it gains most benefit from the abundance of various insects. At the end of summer, it will return to its wintering areas. The common rock thrush has been on the decline in France for several years with about 1,500 breeding pairs left only in France. It is a spectacle to see, so keep a keen eye.
  • Flora

    The Silene acaulis

    This cushion, punctuated by bright pink flowers, is not a moss. The silene acaulis is one of the champions of adapting to the worst. The cushion-like form allows it to reduce day-time and night-time temperature variations that can be significant at these altitudes. Moisture will also be trapped in this hairy, small-leaved stem. The ancient decomposed leaves of the silène acaulis contain nutrients that will allow it to grow and to bloom. A taproot in the cushion’s core will allow it to cling to the steepest terrain.
  • Fauna

    The mountain hare

    Also known as the white hare, it has a rock-brown coloured coat in the summer and an all-white coat in the winter except for the tips of its ears. Smaller and rounder than the European hare, the mountain hare also has shorter ears and a thicker coat to limit heat loss. Its wider back paws act as snowshœs which allow it to move easily over the snow.
  • Flora

    Persicaria vivipara

    In the midst of the sand and rock, a stem loaded with small white flowers appears. The persicaria vivipara grows here. Some plants germinate and develop in the fruit while the latter is still attached to the stock plant. This phenomenon corresponds to vegetative viviparity. If you examine the persicaria vivipara, you will see small green bulbs attached to the stem. The fruits of the persicaria vivipara then begin to germinate on the plant. The seeds of the persicaria vivipara are a delicacy for the rock ptarmigan.
  • Geology

    Snowy paving

    Look around you for flat, damp areas without vegetation. Ÿou are bound to notice that the rock slabs seem to have been sorted and patiently arranged, one against the other. Man is not responsible for this geometric pattern. Here, the alternating freezing and thawing cycles and the weight of the snow encourage the transport of stones and their alignment to create what we call snowy paving. In other cases, these phenomena may create polygonal grounds or stone circles.
  • Geology

    The filling of wetlands

    As you descend from the lake, you will notice the grassy and flat stretches of terrain. The ancient glacier has gouged out depressions in the bedrock. When the ice retreated, these areas became lakes. Just like the Lac du Génépy, alluvium has filled these depressions, the hygrophilous vegetation then colonised these wetlands. Some of these areas then dried up to become small grassy plateaus amid the ´rocky ground´.