France · 04.11.2026

Embrunais Parpaillon

Valid until 05.11.2026 18:00

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Low

Danger level

1 — Low

Snowpack stability

The snowpack is well bonded and stable in general.

Likelihood of triggering

Triggering is generally possible only from high additional loads in isolated areas of very steep, extreme terrain. Only small and medium natural avalanches are possible.

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Maps & charts

Avalanche danger map — massif 20 — Avalanche danger map

Fresh snow (7 days) — massif 20 — Fresh snow (7 days)

Weather overview — massif 20 — Weather overview

Stability

MASSIF TRÈS PEU ENNEIGÉ

MASSIF TRÈS PEU ENNEIGÉ Pas d'activité avalancheuse attendue compte tenu du faible enneigement.Autres : dans les versants nord de haute altitude, risque de glissade sur la neige ancienne dure et regelée.

Snow quality

Qualification de l'enneigement : pas ou peu de neige en ce début novembre.Limite d'enneigement skiable : la pratique du ski est actuellement impossible sur le massif.État de la neige de surface : en altitude, petit saupoudrage à même le sol. Des surfaces de neige dure regelée en nord au-dessus de 2600 m.

Snow cover

Snow line — North: 2600 m · South: -1 m

1500 m — N: 0 cm, S: 0 cm 2000 m — N: 0 cm, S: 0 cm 2500 m — N: 0 cm, S: 0 cm

Fresh snow

Reference altitude: 1800 m

31.10.2026: 0–0 cm 01.11.2026: 0–0 cm 02.11.2026: 0–0 cm 03.11.2026: 0–0 cm 04.11.2026: 0–1 cm 05.11.2026: 0–0 cm

Weather

Nuageux, relief plus ou moins accroché. Quelques faibles averses de neige. Dans la nuit de jeudi à vendredi, renforcement des chutes de neige.

05.11.2026 06:00 — Wind 30/35 km/h (E/S), 0°C line 2200 m
05.11.2026 12:00 — Wind 30/25 km/h (E/SE), 0°C line 2200 m
05.11.2026 18:00 — Wind 25/30 km/h (SE/SE), 0°C line 2400 m
06.11.2026 00:00 — Wind 20/35 km/h (NE/S), 0°C line 2200 m

European Avalanche Danger Scale

Official scale used by European avalanche warning services.

5 — Very high
Snowpack stability
The snowpack is poorly bonded and largely unstable in general.
Likelihood of triggering
Numerous very large and often extremely large natural avalanches can be expected, even in moderately steep terrain.
4 — High
Snowpack stability
The snowpack is poorly bonded on most steep slopes.
Likelihood of triggering
Triggering is likely, even from low additional loads, on many steep slopes. In some cases, numerous large and often very large natural avalanches can be expected.
3 — Considerable
Snowpack stability
The snowpack is moderately to poorly bonded on many steep slopes.
Likelihood of triggering
Triggering is possible, even from low additional loads, particularly on the indicated steep slopes. In certain situations some large, and in isolated cases very large natural avalanches are possible.
2 — Moderate
Snowpack stability
The snowpack is only moderately well bonded on some steep slopes; otherwise well bonded in general.
Likelihood of triggering
Triggering is possible, primarily from high additional loads, particularly on the indicated steep slopes. Very large natural avalanches are unlikely.
1 — Low
Snowpack stability
The snowpack is well bonded and stable in general.
Likelihood of triggering
Triggering is generally possible only from high additional loads in isolated areas of very steep, extreme terrain. Only small and medium natural avalanches are possible.

Avalanche problems

Typical problem types defined by EAWS.

New snow
The avalanche problem is related to current or most recent snowfall. The amount of additional loading by new snow onto the existing snowpack is the crucial factor of the new snow problem. How critical the loading is, depends on various factors such as air temperature, wind or characteristics of the old snow surface.
Wind slab
Wind slabs are formed when loose snow in near-surface layers (new snow or old snow) is transported and deposited by wind.
Persistent weak layers
The avalanche problem is related to the presence of one or more persistent weak layers in the old snowpack. These weak layers typically include faceted crystals, depth hoar or surface hoar crystals.
Wet snow
The avalanche problem is related to a weakening of the snowpack due to the presence of liquid water. Water infiltrates the snowpack due to melt or rain.
Gliding snow
The entire snowpack is gliding on the ground, typically on smooth ground such as grassy slopes or smooth rock zones. High activity of glide-snow avalanches is typically related to a thick snowpack with no or only few weak layers. Glide-snow avalanches can occur both with a cold dry snowpack and with a warm moist or wet snowpack. The release of a glide-snow avalanche is difficult to predict, although in many cases glide cracks open prior to release.
Cornices
A wave-like formation of soft or hard wind drifted snow, often overhanging.