The landslide sequence induced by the 2002 eruption at Stromboli Volcano

被引：37

作者：

Tommasi, P ^{[1
]}

Baldi, P ^{[1
]}

Chiocci, FL ^{[1
]}

Coltelli, M ^{[1
]}

Marsella, M ^{[1
]}

Pompilio, M ^{[1
]}

Romagnoli, C ^{[1
]}

机构：

[1] CNR, Inst Geoengn & Environm Geol, Fac Engn, I-00184 Rome, Italy

来源：

LandSlides: Risk Analysis and Sustainable Disaster Management | 2005年

关键词：

landslide; tsunami; volcanoclastic materials; Stromboli Volcano;

D O I：

10.1007/3-540-28680-2_32

中图分类号：

P5 [地质学];

学科分类号：

0709 ; 081803 ;

摘要：

The complex sequence of large-scale tsunamogenic instability phenomena occurred on the subaerial and submarine NW flank of the Stromboli Volcano soon after the beginning of the December 2002 eruption is reconstructed and its relationship with volcanic activity is evidenced. After a brief description of slope morphology and stratigraphy, geometry and kinematics of the landslides are described. Finally, instability mechanisms that controlled the subaerial and submarine slope failures are proposed with reference to the different geotechnical, hydraulic, and loading/strain conditions that characterized the different stages of the slope evolution.

引用

页码：251 / 258

页数：8

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