Landslides in the north of Lisbon region (Portugal): conditioning and triggering factors

Detailed geomorphological mapping carried out in 5 sample areas in the Nort h of Lisbon Region allowed us to collect a set of geological and geomorphol ogical data and to correlate them with the spatial occurrence of landslide. A total of 597 slope movements were identified in a total area of 61.7 km( 2), which represents about 10 landslides per km(2). The main landslide conditioning factors are: lithology and geological struc ture, slope angle and slope morphology, land use, presence of old landslide s, and human activity. The highest landslide density occurs in Cretaceous marls and marry limeston es, but the largest movements are in Jurassic clays, marls and limestones. The landslide density is higher on slopes with gradients above 20 degrees, but the largest unstable area is found on slopes of 10 degrees to 15 degree s, thus reflecting the presence of the biggest slope movements. There is a correlation between landslides and topographical concavities, a fact that c an be interpreted as reflecting the significance of the hydrological regime in slope instability. Concerning land use, the highest density of landslides is found on slopes c overed with shrub and undergrowth vegetation. About 26% of the total number of landslides are reactivation events. The presence of old landslides is p articularly important in the occurrence of translational slides and complex and composite slope movements. 20% of the landslide events were conditioned by anthropomorphic activity. H uman's intervention manifests itself in ill-consolidated fills, cuts in pot entially unstable slopes and, in a few cases, in the changing of river chan nels. Most slope movements in the study area exhibit a clear climatic signal. The analysis of rainfall distribution in periods of recognised slope instabili ty allows the distinction of three situations: I) moderate intensity rainfa ll episodes, responsible for minor slope movements on the bank of rivers an d shallow translational slides, particularly in artificial trenches; 2) hig h intensity rainfall episodes, originating flash floods and most landslides triggered by bank erosion; 3) long-lasting rainfall periods, responsible f or the rise of the groundwater table and triggering of landslides with deep er slip surfaces. (C) 1999 Elsevier Science Ltd. All rights reserved.