441
Views
6
CrossRef citations to date
0
Altmetric
Mapping Environmental Risks - Quantitative And Spatial Modelling Approaches

Ground movement risk in ‘Las Batuecas-Sierra de Francia’ and ‘Quilamas’ nature parks (central system, Salamanca, Spain)

, &
Pages 223-231 | Received 27 Jul 2012, Accepted 05 Feb 2014, Published online: 24 Feb 2014

Figures & data

Figure 1. Methodological framework for mapping procedure.

Figure 1. Methodological framework for mapping procedure.

Figure 2. Weighting Conditioning Factors.

Figure 2. Weighting Conditioning Factors.

Figure 3. Validate process of mapping the ground Movements risk, overlaying different types of ground Movements on susceptibility map (left) and ground Movements risk map (right).

Figure 3. Validate process of mapping the ground Movements risk, overlaying different types of ground Movements on susceptibility map (left) and ground Movements risk map (right).

Figure 4. A. Slope instability by lateral fluvial erosion and waterlogging favoured by detrital material. Alba de Yeltes. B. Rotational landslide caused by unstable river margin. Aldehuela of Yeltes. C. Flows of rock fragments-scree-vegetation with scattered vegetation nuclei. Serradilla del Arroyo. D. sliding caused by fractures crossing in Armorican quartzite. Monsagro. E Scars of shallow landslides associated with fluvial incision into an old fracture. La Bastida. F. Break in slope rollover Armorican quartzite. Pastores. G. Destabilisation of the retaining wall of a crag. Monsagro. H. Intense erosion promoted by a road cut.

Figure 4. A. Slope instability by lateral fluvial erosion and waterlogging favoured by detrital material. Alba de Yeltes. B. Rotational landslide caused by unstable river margin. Aldehuela of Yeltes. C. Flows of rock fragments-scree-vegetation with scattered vegetation nuclei. Serradilla del Arroyo. D. sliding caused by fractures crossing in Armorican quartzite. Monsagro. E Scars of shallow landslides associated with fluvial incision into an old fracture. La Bastida. F. Break in slope rollover Armorican quartzite. Pastores. G. Destabilisation of the retaining wall of a crag. Monsagro. H. Intense erosion promoted by a road cut.

Figure 5. A. Soil processes striated by reptation for frost wedging. La Bastida. B. Retaining walls that impede progress with stone flows on the valley road from Las Batuecas. C. Avalanches of rock fragments by solifluction processes. Pico Cervero. D. Shallow landslides in clay materials as a result of high rainfall. La Atalaya. E. Reforestation and stepped terraces as a corrective measure to prevent soil creep processes in areas of average slopes. Serradilla del Arroyo.

Figure 5. A. Soil processes striated by reptation for frost wedging. La Bastida. B. Retaining walls that impede progress with stone flows on the valley road from Las Batuecas. C. Avalanches of rock fragments by solifluction processes. Pico Cervero. D. Shallow landslides in clay materials as a result of high rainfall. La Atalaya. E. Reforestation and stepped terraces as a corrective measure to prevent soil creep processes in areas of average slopes. Serradilla del Arroyo.
Supplemental material

Main Map: Ground Movements Risk Map in 'Las Batuecas-Sierra de Francia' and 'Quilamas' Nature Parks (Central System, Salamanca, Spain)

Download PDF (134.5 MB)

Reprints and Corporate Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

To request a reprint or corporate permissions for this article, please click on the relevant link below:

Academic Permissions

Please note: Selecting permissions does not provide access to the full text of the article, please see our help page How do I view content?

Obtain permissions instantly via Rightslink by clicking on the button below:

If you are unable to obtain permissions via Rightslink, please complete and submit this Permissions form. For more information, please visit our Permissions help page.