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Central Mediterranean tephrochronology and explosive volcanism over the240–190 ka interval: Insights from the high-resolution record of CastiglioneMaar, central Italy

Figure 3 Composite sequence tephrostratigraphy for the studied Marine Isotope Stage (MIS) 7 interval. The figure illustrates the stratigraphic positions of the studied tephra layers plotted against composite depth (m). High-resolution photographs display representative tephra layers from core C1-C2 (highlighted by red rectangles), illustrating their primary stratigraphic features and visual…

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Cognitive biases and rational decision making for volcanichazards and risks

Table 1 Cognitive biases described in this contribution. Papale P. (2026).Frontiers in Earth Science, 14 pp. https://doi.org/10.3389/feart.2026.1755833 Open access Abstract Volcanic systems are governed by complex, non-linear dynamics that make deterministic forecasting impossible and require decisions to be made under substantial uncertainty. This contribution examines how…

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Twenty‐Five Years of Probabilistic Fault DisplacementHazard Assessment

Figure 3. Block diagram illustrating principal and distributed ruptures in a normal faulting tectonic setting. The diagram highlights the spatial distribution of surface ruptures, with the principal rupture (PF) occurring along the main fault and distributed ruptures (DR) appearing as secondary surface breaks, typically in the hanging wall and footwall…

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