Figures & data
Figure 2. Geology of the Island of Gozo (CitationOil Exploration Directorate, 1993) and location of the study area.
![Figure 2. Geology of the Island of Gozo (CitationOil Exploration Directorate, 1993) and location of the study area.](/cms/asset/97926f4f-9f72-4500-b24f-abfe55894895/tjom_a_1480977_f0002_oc.jpg)
Figure 3. Coastal geomorphotypes: (a) built-up coast (Marsalforn Bay); (b) cliff shaped in Blue Clay (east of Marsalforn Bay); (c) sloping coast (between Dahlet Qorrot Bay and Ras il-Qala); (d) plunging cliff (between Dahlet Qorrot Bay and Ras il-Qala); (e) scree (Gebel Mistra); (f) shore platform (east of Marsalforn Bay); (g) pocket beach (Ramla Bay).
![Figure 3. Coastal geomorphotypes: (a) built-up coast (Marsalforn Bay); (b) cliff shaped in Blue Clay (east of Marsalforn Bay); (c) sloping coast (between Dahlet Qorrot Bay and Ras il-Qala); (d) plunging cliff (between Dahlet Qorrot Bay and Ras il-Qala); (e) scree (Gebel Mistra); (f) shore platform (east of Marsalforn Bay); (g) pocket beach (Ramla Bay).](/cms/asset/7570b006-b94c-40b2-a39a-dfb499d0d655/tjom_a_1480977_f0003_oc.jpg)
Figure 4. Ramla Wied during different periods: (a) and (c) the temporary stream is full after an intense rainy period (November 2017); (b) the valley is dry (September 2017) and hosts sediments and vegetation and a succession of alluvial sediments is observable on a side of the small fluvial scarp. In frame (d) Ramla Bay (seen from the north) during a flash flood occurred on 15 November 2012; the abundance of transported sediment is noticeable.
![Figure 4. Ramla Wied during different periods: (a) and (c) the temporary stream is full after an intense rainy period (November 2017); (b) the valley is dry (September 2017) and hosts sediments and vegetation and a succession of alluvial sediments is observable on a side of the small fluvial scarp. In frame (d) Ramla Bay (seen from the north) during a flash flood occurred on 15 November 2012; the abundance of transported sediment is noticeable.](/cms/asset/54f902bc-c423-4a48-aa85-5de68c1ece06/tjom_a_1480977_f0004_oc.jpg)
Figure 5. Landslides: (a) block slides (west of Dahlet Qorrot Bay); (b) earth flow and block slide (between San Blas Bay and Dahlet Qorrot Bay); (c) rock fall at the bottom of a limestone plateau and earth flow/slide affecting the underlying clayey terrain (between San Blas Bay and Dahlet Qorrot Bay).
![Figure 5. Landslides: (a) block slides (west of Dahlet Qorrot Bay); (b) earth flow and block slide (between San Blas Bay and Dahlet Qorrot Bay); (c) rock fall at the bottom of a limestone plateau and earth flow/slide affecting the underlying clayey terrain (between San Blas Bay and Dahlet Qorrot Bay).](/cms/asset/5b8be18a-6deb-43c1-b3c8-48efd85b6f9f/tjom_a_1480977_f0005_oc.jpg)