The Blatten Landslide was a natural disaster that occurred on 28 May 2025, devastating the village of Blatten in the Lötschental valley in the Canton of Valais, Switzerland. A glacier collapse in the Bietschhorn region caused a landslide which buried and destroyed large parts of the village. The main village had been evacuated on 19 May 2025. The village was largely destroyed by a debris flow and ice avalanche. A 64-year-old shepherd, who was outside the evacuation zone, died in the disaster. The event was preceded by several rockfalls and landslides from the Bietschhorn area onto the , which ultimately collapsed under the additional burden of millions of cubic metres of debris. The failure was preceded by progressive seismic precursors, which were detected through unsupervised machine learning analysis of seismic data.
Events Initial rockfall at Kleines Nesthorn
Since around 2019, and unlike the general retreat of glaciers since 1850, the lower part of the Birch Glacier, had advanced about 50 metres in the five years prior to the landslide, likely due to accumulation of weathered rock from repeated rockfalls onto the glacier.Permafrost expert: Climate change caused the Blatten landslide, Watson.ch, 30 May 2025. Following a major icefall on 18 December 1993, the glacier had been placed under observation.
From 14 May 2025, signs of instability were observed on the flank of the . The peak is about northwest of the Bietschhorn () and lies in a complex geological area of gneiss and amphibolite, subject to erosion and glacier activity. Rockfalls onto the Birch Glacier triggered a debris flow in the valley of the Birchbach, which stopped about 500 metres above the valley floor and the Lonza river. The local councilor responsible for environmental issues, Reto Kalbermatten, compared the volume to that of a smaller avalanche.
The Kleine Nesthorn (elevation before the landslide ) consists of complex sequences of gneisses and amphibolites. It is located approximately 950 metres northwest of the Bietschhorn () and is tectonically sheared from its solid granite.Theodor Hügi, Hugo Ledermann, Ernst Schläppi: Blatt 1268 Lötschental (Atlasblatt 82) – Erläuterungen. In: Schweizerische Geologische Kommission, Landeshydrologie und -geologie (Hrsg.): Geological Atlas of Switzerland 1:25 000, 1988, p. 28 (online).
Evacuation Following the debris flow, 92 people were evacuated on 17 May 2025, due to increasing rockfall risks above Blatten.
On 19 May 2025, all approximately 300 residents of the villages of Blatten and Ried were ordered to leave within two hours before noon. At this point, most livestock were also removed from the endangered area. A lame cow named Loni gained media attention as the last to be airlifted out by helicopter on 20 May. The hamlets of Weissenried and Eisten were not affected by the evacuation. The evacuation was triggered by the fact that rock formations at Kleine Nesthorn had moved 17 metres in the previous three days, and a rock collapse could no longer be ruled out. Geologists feared a collapse within hours. Eventually, the northeast flank of the mountain slid onto the Birch Glacier in several phases.
Experts used scenarios and numerical models to provide further action recommendations.
Blatten was not listed as a risk area on the Canton of Valais hazard map before the disaster. A risk area is defined as one that could be affected by natural forces with a probability of at least once in 300 years. A landslide and glacier collapse like the one on 28 May 2025, was considered an event with a significantly lower probability.
Glacier movement and further collapses
Further collapses occurred on 19 May and 20 May, with a total of 1.5 million cubic metres of rock sliding from the northeast flank of Kleine Nesthorn downhill onto the Birch Glacier. The increased pressure caused the glacier's flow speed to rise by 21 May, reaching 0.5 to 0.8 metres per day according to a report on 22 May. Conversely, the melting and movement of the glacier at the lower part of the Nesthorn flank contributed to the instability of the steep slope there.
The Swiss Seismological Service recorded about a dozen rockfalls from 19 May, which, except for the main event on 28 May, produced tremors with an indicative magnitude mostly around 1.4, ranging between 0.3 and 1.6 on the Richter scale. Geologists estimated that up to five million cubic metres of rock could still slide.
By noon on 23 May, the debris accumulation on the Birch Glacier was still far enough from the glacier's edge that no large boulders had fallen over the edge into the valley.
The glacier's flow speed increased to 4 to 4.5 metres per day by 24 May, after an estimated two-thirds of the unstable rock formations had fallen onto the glacier. By the next day, the debris pile reached a height of 81 metres, and the glacier tongue's movement increased rapidly. By 27 May, it reached ten metres per day. Local authorities estimated that about nine million tons of debris (approximately 3.5 million m3) had accumulated on the glacier surface. The additional pressure from this debris enhanced the formation of meltwater, which acted as a sliding layer between the ice and the ground, contributing to the glacier's accelerated slide toward the valley. Since 25 May, smaller parts of the glacier's edge broke off. On 27 May, larger ice collapses occurred but stopped well above the valley floor. On the morning of 28 May, an ice and debris mass reached the Lonza for the first time. Later that day, after filling the Birchbach channel, it overcame a deflection dam that previously directed normal snow avalanches from the Birchbach valley westward. The ice and debris mixture that flowed over the dam stopped above the built-up area, causing only minor damage.
Glacier collapse On 28 May, a large part of the Birch Glacier slid under the pressure of the landslide material on the increased meltwater at the glacier's base, plunging over the cirque threshold into the Birchbach gorge. The debris and ice masses buried 130 houses and the church in Blatten, totaling about 90 percent of the village.
Roughly of rock and large glacier segments fell into the valley. The seismic waves recorded at 3:24 PM were comparable in strength to those of the Bondo landslide in 2017, equivalent to an earthquake of magnitude 3.1 on the Richter scale. Seismic signals were measurable hundreds of kilometres beyond Switzerland's borders.
The volume of rock that fell with the glacier into the valley was estimated at , plus of Birch Glacier ice, with initial estimates suggesting a total volume of .
The downstream hamlets of Ried, Oberried, and Tännmatten were also buried. The hamlet of Weissenried, located above the valley floor at and not evacuated, was narrowly missed by the debris flow and remained largely intact. The debris flow surged up the northeast slope, stopping just short of the road from Weissenried to Gassun at approximately .Aerial image of the landslide area from 30 May 2025 The hamlet of Eisten (), upstream from Blatten, remained unaffected, situated on a landscape terrace above the maximum water level of the lake formed by the Lonza behind the landslide debris. The debris and ice masses covered the Lötschental valley floor over a length of about , a width of , and were up to several dozen metres thick, reaching in some areas. The debris flow extended downstream into the municipality of Wiler, stopping in the "Tänn" area, above Wiler.
Following the landslide, a 64-year-old shepherd, tending sheep in the "Tännmattä" area, was reported missing. This location was outside the evacuated zone but was still buried due to the high water content of the debris and ice avalanche. His body was found on 24 June and positively identified on 26 June. The Valais public prosecutor's office opened an investigation into the circumstances of the shepherd's death. It is believed his approximately 100 sheep perished. Many other animals on buried pastures also perished.
Aftermath
Lonza River blockage Due to the deposits, the Lonza and the village stream Gisentella were dammed, forming a lake in the "Teiffu Mattä" area near Blatten. The resulting damming flooded previously undamaged houses. On 29 May, the lake level rose by about per hour. On 30 May, the lake reached a provisional maximum of , and the water began to carve a path through the deposits, forming small lakes in the lower debris cone. The responsible geologist for the canton described the slow drainage through the debris and ice deposits as a relatively "favourable" development. On the same day, the Lonza flowed over and through the entire length of the debris cone. By 1 June, the water level stabilized.
Partial evacuations in Wiler, Kippel, and Ferden On 28 May at around 10:30 PM, residents of Wiler and Kippel within a danger zone along the Lonza were evacuated due to the risk of flooding. The Lonza, dammed over a length of more than two kilometres between Blatten and Wiler, threatened to uncontrollably carve a path through or overflow the debris area. By 1:00 AM on 29 May, affected individuals had to report to the respective command centers, increasing the total number of evacuees to 365. The evacuation in Wiler, Kippel, and Ferden was lifted by 6 June at 12:00 PM.
Further developments
Reconnaissance flights on 29 May showed that several hundred thousand cubic metres of unstable rock remained at Kleine Nesthorn, with further small rockfalls occurring. The debris masses that surged up the opposite slope also risked sliding back into the valley. The deposit mass itself was unstable, halting cleanup efforts. Thus, no attempts could be made to regulate the Lonza's flow through the landslide debris. Heavy equipment provided by the army in the Rhone Valley remained unused.
On 31 May, the debris cone remained so unstable that neither people nor machines could safely operate on it, and cleanup or regulation of the Lonza in the landslide area was postponed. Further slides from both valley sides and rockfalls remained a threat. As the Lonza slowly flowed over the debris cone and the dammed water level dropped by one metre below its maximum on 31 May, the risk of a sudden outburst of dammed water carrying large amounts of debris was temporarily reduced but still considered.
A floating barrier was placed at the Lonza's entry into the debris cone to prevent debris from clogging the channel carved by the river. Uprooted trees were retrieved by helicopter from the Lonza's riverbed to reduce debris during potential flooding. Another environmental issue could arise from spilled heating oil.
The downstream Stausee Ferden was preemptively drained days before the major landslide to potentially catch dammed and surging water from the landslide deposits. On 30 May, the Lonza was so contaminated with solids that power generation at the Lötschental Power Plant was halted. The Valais State Council instructed the operator to open the gatehouse of the reservoir as needed. The downstream municipalities of Gampel-Bratsch and Steg-Hohtenn prepared for potential evacuation of areas threatened by the Lonza.
Some residents, sheep, and cars in the largely intact hamlets of Weissenried, Eisten, and surrounding alpine areas, including the Fafleralp, were airlifted out on 29 May (Ascension Day), as the landslide had cut them off from the surroundings. On 31 May, the staff of the Fafleralp Hotel was evacuated. On 6 June at 11:00 PM, the road from Goppenstein to Wiler was reopened for all private traffic, making the lower part of the valley accessible again for tourism.
Damage assessment
In the villages of Blatten, Ried, and Tännmatten, more than a hundred buildings were destroyed, including three hotels, the Blatten parish church, and the Ried chapel.