Slope analysis within the Wabane caldera was carried out to establish their stability after the 20th July 2003 landslides. A site with semi-circular fractures was selected for the installation of a vibrating wire displacement meter and avibrating piezometer. Displacement, rainfall and pore water fluctuation were recorded from May to December 2005 in an attempt to assess the behavior of these slopes with varying rainfall intensities throughout the period. The resultsindicated an increase in displacement with rainfall and pore pressure from May to September and a subsequent decrease from October to December. This demonstrates the interdependence between rainfall, pore pressure and displacement. The mean monthly rate of displacement recorded w...
The dissected volcanic terrains around Limbe, SW Cameroon are frequently affected by small scale but...
Reactivated landslides in stiff clays and shales typically move on a pre-existing shear surface and ...
The understanding of the interplay between natural and human-induced drivers in the occurrence of la...
Landslides are well known processes that hamper sustainable development efforts, particularly in dev...
Limbe town and surrounding areas, on the SE foot slopes of the active Mt Cameroon Volcano, have expe...
Limbe town and surrounding areas, on the SE foot slopes of the active Mt Cameroon Volcano, have expe...
Landslides are recognized as important geomorphologic process due to the role they play in the devel...
The volcanic terrain at the western margin of the Main Ethiopian Rift in the Debre Sina area is know...
Landslides are part of natural catastrophic disasters destroying both biological and physical entiti...
In 2011, Waimarama received 80% of its annual rainfall in 48 hours. This extreme event with a return...
International audienceThe Ndop Plain, located along the Cameroon Volcanic Line (CVL), is a volcano-t...
Mount Elgon in Eastern Uganda is one of the most landslide-prone regions in Africa. This extinct shi...
Tropical mountainous regions are often identified as landslide hotspots with particularly vulnerable...
Slope failures triggered by rainfall are causing considerable damage and loss of life every year thr...
Prediction of the conditions under which landslides may occur is essential for designing sustainable...
The dissected volcanic terrains around Limbe, SW Cameroon are frequently affected by small scale but...
Reactivated landslides in stiff clays and shales typically move on a pre-existing shear surface and ...
The understanding of the interplay between natural and human-induced drivers in the occurrence of la...
Landslides are well known processes that hamper sustainable development efforts, particularly in dev...
Limbe town and surrounding areas, on the SE foot slopes of the active Mt Cameroon Volcano, have expe...
Limbe town and surrounding areas, on the SE foot slopes of the active Mt Cameroon Volcano, have expe...
Landslides are recognized as important geomorphologic process due to the role they play in the devel...
The volcanic terrain at the western margin of the Main Ethiopian Rift in the Debre Sina area is know...
Landslides are part of natural catastrophic disasters destroying both biological and physical entiti...
In 2011, Waimarama received 80% of its annual rainfall in 48 hours. This extreme event with a return...
International audienceThe Ndop Plain, located along the Cameroon Volcanic Line (CVL), is a volcano-t...
Mount Elgon in Eastern Uganda is one of the most landslide-prone regions in Africa. This extinct shi...
Tropical mountainous regions are often identified as landslide hotspots with particularly vulnerable...
Slope failures triggered by rainfall are causing considerable damage and loss of life every year thr...
Prediction of the conditions under which landslides may occur is essential for designing sustainable...
The dissected volcanic terrains around Limbe, SW Cameroon are frequently affected by small scale but...
Reactivated landslides in stiff clays and shales typically move on a pre-existing shear surface and ...
The understanding of the interplay between natural and human-induced drivers in the occurrence of la...