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3 landslide susceptibility zones of minimal, high and really high landslide susceptibility are delineated. The 10 deep gully websites sampled in the course of the subject experiments all tumble underneath the zone of very high land slide susceptibility including Edim Otop, the website in the September 2013 deadly rainfall induced incidence. Recommendations for management contain possibility and hazard quantification considering human occupation on very high landslide susceptibility locations, slope protection methods including excavated sections, use of sites of former landslide including Edim Otop as pilot initiatives to characterize the system of slope instability and back Examination of slope failure as reference. Key terms: Soil cohesion, friction, soil slope and slope path, distant sensing, landslide, Calabar.
In zone A, the failure zone digital map is superimposed on to the terrain device digital map to determine the relationship amongst different terrain variables and the failure zones. The numerical expression of the romance enables us to classify the terrain by its landslide susceptibility. In zone B, this numerical romantic relationship was used to obtain a landslide susceptibility map, obviating the need for any failure zone map. The validity with the methodology can be tested In this particular region by using the degree of superposition with the susceptibility map and the failure zone map. The implementation from the methodology in tropical nations with Bodily and environmental attributes just pallet liquidation like Those people of the research location will allow us to execute a landslide susceptibility Assessment in areas exactly where landslide records don't exist. This Evaluation is important to landslide hazard and chance assessment, which is critical to determine the actions for mitigating landslide effects, e.g. land planning, emergency aid steps, and so on.