Evolution of landslide activity, and the origin of debris flows in the el niño affected payhua creek basin, matucana area, huarochiri, per
In this paper different types of hydrological triggering systems for debris flows, shallow and deepe...
Slope movements in Callejón de Huaylas (the Santa River valley) are of different origin according to...
to explain the origin of potentially catastrophic landslides. Earth and Planetary Science Letters 26...
Matucana, Perú (population 5800; elevation 2390 m), is located in Andes Occidental, approximately 75...
Since 1997 the Machu Picchu area has been in the spotlight for its slope instability, when Carreno &...
The small city of Matucana (population 5800), Province of Huarochirí, Perú is located on the flood p...
Abstract: As one of geological disasters and geomorphological processes, debris flow stemming from l...
Abstract: The mechanism of landslide occurrences is divided into the three types: (1) landslides con...
Abstract: Flow-like landslides triggered by rainfall are very prominent in Nepal and Shikoku, Japan....
In the Andean region, landslides are common geomorphological agents that can cause disasters. The oc...
In the Wenchuan area in SW China, an abundance of loose co-seismic landslide debris was present on t...
The 2008 Wenchuan earthquake induced a large number of landslides, and a vast amount of loose landsl...
Abstract: The 2004 Chuetsu earthquake (M 6.8) triggered thousands of landslides in the Miocene to Qu...
From 12 to 14 August 2010, heavy rainstorms occurred in the Sichuan province in SW China in areas w...
Since 1997 the Machu Picchu area has been in the spotlight for its slope instability, when Carreno &...
In this paper different types of hydrological triggering systems for debris flows, shallow and deepe...
Slope movements in Callejón de Huaylas (the Santa River valley) are of different origin according to...
to explain the origin of potentially catastrophic landslides. Earth and Planetary Science Letters 26...
Matucana, Perú (population 5800; elevation 2390 m), is located in Andes Occidental, approximately 75...
Since 1997 the Machu Picchu area has been in the spotlight for its slope instability, when Carreno &...
The small city of Matucana (population 5800), Province of Huarochirí, Perú is located on the flood p...
Abstract: As one of geological disasters and geomorphological processes, debris flow stemming from l...
Abstract: The mechanism of landslide occurrences is divided into the three types: (1) landslides con...
Abstract: Flow-like landslides triggered by rainfall are very prominent in Nepal and Shikoku, Japan....
In the Andean region, landslides are common geomorphological agents that can cause disasters. The oc...
In the Wenchuan area in SW China, an abundance of loose co-seismic landslide debris was present on t...
The 2008 Wenchuan earthquake induced a large number of landslides, and a vast amount of loose landsl...
Abstract: The 2004 Chuetsu earthquake (M 6.8) triggered thousands of landslides in the Miocene to Qu...
From 12 to 14 August 2010, heavy rainstorms occurred in the Sichuan province in SW China in areas w...
Since 1997 the Machu Picchu area has been in the spotlight for its slope instability, when Carreno &...
In this paper different types of hydrological triggering systems for debris flows, shallow and deepe...
Slope movements in Callejón de Huaylas (the Santa River valley) are of different origin according to...
to explain the origin of potentially catastrophic landslides. Earth and Planetary Science Letters 26...