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Typus
Verschleierung
Bearbeiter
Graf Isolan
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Untersuchte Arbeit:
Seite: 11, Zeilen: 11-18
Quelle: Chacon et al 2006
Seite(n): 349, Zeilen: right col. 19-34
Einstein (1988) suggested the temporal projection of susceptibility mapping based on higher probabilities of new landslides occurring within higher susceptibility zones. Recent validation of a susceptibility map (Irigaray et al., 1999, 2006) confirmed this view, when 125 new landslides occurred after heavy rainfalls in 1997 in the Iznajar river dam area (Granada, Spain) where a susceptibility map had been completed in 1994 using an inventory of 833 older landslides. Some 61.9% of the 1997 landslides plotted in the very high susceptibility zone and 23.1% in the high susceptibility zone. Similar practical validations were successfully obtained by many other authors too for instance like in southwestern Sierra Nevada (Spain) and in Torre Vedras (Portugal).

Einstein, H. H. (1988): Special lecture: landslide risk assessment procedure. In: Proceedings of the Vth ISL Lausanne, vol 2, pp 1075–1090.

Irigaray, C., Ferna´ndez [sic], T., El Hamdouni, R., Chaco´n [sic], J. (1999): Verification of landslide susceptibility mapping, a case study. Earth Surf Processes Landforms 24:537–544.

Irigaray, C., Ferna´ndez [sic], T., El Hamdouni, R., Chaco´n [sic], J. (2006): Evaluation and validation of landslidesusceptibility maps obtained by a GIS matrix method: examples from the Betic Cordillera (southern Spain). Natural Hazards, ISSN: 0921-030X (Paper) 1573-0840 (Online) DOI: 10.1007/s11069-006-9027-8.

Einstein (1988) suggested the temporal projection of

susceptibility mapping based on higher probabilities of new landslides occurring within higher susceptibility zones. Recent validation of a susceptibility map (Irigaray et al. 1999, 2006) confirmed this view, when 125 new landslides occurred after heavy rainfalls in 1997 in the Iznájar river dam area (Granada, Spain) where a susceptibility map had been completed in 1994 (Irigaray 1995) using an inventory of 833 older landslides. Some 61.9% of the 1997 landslides plotted in the very high susceptibility zone and 23.1% in the high susceptibility zone of the 1995 map (Figs. 2, 3). A similar practical validation was obtained for a susceptibility map of the southwestern Sierra Nevada (Spain) slopes by El Hamdouni (2001) (Fig. 4) or in Torre Vedras (Portugal) by Garcia and Zêzere 2004.


Einstein HH (1988) Special lecture: landslide risk assessment procedure. In: Proceedings of the Vth ISL Lausanne, vol 2, pp 1075–1090

El Hamdouni R (2001) Estudio de movimientos de ladera en la cuenca del río Ízbor mediante un SIG: contribución al conocimiento de la relación entre tectónic activa e inestabilidad de vertientes. 429 pp and 10 maps 1:25.000, Unpublished PhD thesis. Department of Civil Engineering. University of Granada, Spain

Garcia RAC, Zêzere JL (2004) Abadia Basin (Torres Vedras, Portugal) a case study of landslide susceptibility assessment and validation. In: Lacerda WA, Ehrlich M, Fontoura SAB, Sayao ASF (eds) Landslides: evaluation and stabilization. Balkema, Taylor & Francis Group, London, pp 137–146

Irigaray, C (1995) Movimientos de ladera: inventario, análisis y cartografía de susceptibilidad mediante un Sistema de Información Geográfica: Aplicación a las zonas de Colmenar(Málaga), Rute (Córdoba) y Montefrío (Granada). Unpublished PhD Thesis. University of Granada, Spain

Irigaray C, Fernández T, El Hamdouni R, Chacón J (1999) Verification of landslide susceptibility mapping. A case study. Earth Surf Processes Landforms 24:537–544

Anmerkungen

Although in most places nearly identical with exactly the same references, the original source is not given by Hja.

Obviously, the misplacements of accents in the references for Irigaray et al. (1999, 2006) was caused by blindly copying from the electronic version of the unnamed source.

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