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The temporal stability and activity of landslides in Europe with ž ...

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6<br />

( )<br />

R. Dikau, L. SchrottrGeomorphology 30 1999 1–12<br />

Fig. 2. <strong>Europe</strong>an study areas <strong>of</strong> the project. Each study site refers to one or more papers <strong>of</strong> this issue: Ž. 1 Cort<strong>in</strong>a d’Ampezzo ŽBonomi<br />

<strong>and</strong><br />

Cavall<strong>in</strong>, 1999; Dehn <strong>and</strong> Buma, 1999; Pasuto <strong>and</strong> Soldati, 1999; Angeli et al., 1999 . ; Ž 2. Lago ŽFantucci<br />

<strong>and</strong> Sorriso-Valvo, 1999;<br />

Sorriso-Valvo et al., 1999 . ; Ž 3. Barcelonnette <strong>and</strong> Vars bas<strong>in</strong> Ž Dehn <strong>and</strong> Buma, 1999; Flageollet et al., 1999; van Asch et al., 1999 . ; Ž 4.<br />

Llobregat bas<strong>in</strong> Ž Moya <strong>and</strong> Corom<strong>in</strong>as, 1999 . ; Ž. 5 Cantabrian Range Ž Gonzalez-Dıez ´ ´ et al., 1999 . ; Ž. 6 Asturian coastal valley ŽJimenez<br />

´<br />

Sanchez ´ et al., 1999 . ; Ž 7. North <strong>of</strong> Lisbon Ž Zezere ˆ et al., 1999 . ; Ž 8. Roughs Ž Brunsden 1999 . .<br />

Holocene Ž Jimenez ´ Sanchez ´ et al., 1999 . , respectively.<br />

Special attention <strong>with</strong> respect to monitor<strong>in</strong>g<br />

<strong>and</strong> modell<strong>in</strong>g has been drawn to the Alvera ` mudslide<br />

<strong>in</strong> Cort<strong>in</strong>a d’Ampezzo Ž Dolomites, Italy . ,<br />

ma<strong>in</strong>ly because <strong>of</strong> the availability <strong>of</strong> several time<br />

series <strong>of</strong> data <strong>with</strong> a relatively good resolution<br />

Ž meteorological, hydrological, geotechnical . . This<br />

particular mudslide is considered under different top-<br />

ics Že.g.,<br />

hydrological modell<strong>in</strong>g <strong>and</strong> slope <strong>stability</strong><br />

analysis. <strong>in</strong> several papers <strong>of</strong> this issue ŽBonomi<br />

<strong>and</strong><br />

Cavall<strong>in</strong>, 1999; Dehn <strong>and</strong> Buma, 1999; Pasuto <strong>and</strong><br />

Soldati, 1999; Angeli et al.,1999 . . <strong>The</strong> relationship<br />

between climate <strong>and</strong> l<strong>and</strong>slide <strong>activity</strong> played a major<br />

role <strong>in</strong> the Vars <strong>and</strong> Barcelonnette bas<strong>in</strong>, the<br />

Llobregat bas<strong>in</strong>, the Cantabrian range, the Asturian<br />

coastal valley, <strong>and</strong> <strong>in</strong> the Lisbon area ŽCorom<strong>in</strong>as

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