A5077953636- Landslides and related hazards
- Geology and Paleoclimatology Research
- Geological and Geophysical Studies Worldwide
- Environmental and Ecological Studies
- Flood Risk Assessment and Management
- Coastal and Marine Management
- Geotechnical Engineering and Analysis
- Karst Systems and Hydrogeology
- Soil erosion and sediment transport
- Coastal and Marine Dynamics
- Aeolian processes and effects
- Environmental and Social Impact Assessments
- Geochemistry and Geologic Mapping
- Geological and Tectonic Studies in Latin America
- Soil Geostatistics and Mapping
- Archaeological and Geological Studies
- Regional Development and Innovation
- Archaeological and Historical Studies
- 3D Modeling in Geospatial Applications
- Medieval Architecture and Archaeology
- Geological and Geochemical Analysis
- Historical and socio-economic studies of Spain and related regions
- Migration, Aging, and Tourism Studies
- Social Acceptance of Renewable Energy
- Geological Modeling and Analysis
Universidad de Cantabria
2011-2024
Universidad Nacional de La Plata
2016-2024
Key Points Sedimentation rates and frequency of geomorphic disasters show a marked increase worldwide, especially after midtwentieth century This points to an intensification processes, which could be one the characteristics Anthropocene Land surface change caused by human activities, rather than climate change, is very likely behind processes
We synthesize evidence suggesting a chain of global cause-effect relationships, linking population and economic development with cumulative effects on changes in landscape dynamics, including denudation sediment transport/deposition. Temporal trends patterns geomorphic processes or process combinations such as denudation, sedimentation, frequency disasters, appear to reflect growing human pressure. Erosion rates, intensified by anthropogenic factors, are currently one two orders magnitude...
Abstract Three types of sinkhole have been mapped in a 50 km 2 stretch the Ebro River valley downstream Zaragoza: large collapse sinkholes, shallow subsidence depressions and small cover‐collapse sinkholes. The sinkholes relate to karstification evaporitic bedrock that wedges out abruptly downstream, giving way shale substratum. Twenty‐three up m diameter by 6 deep, commonly hosting saline ponds, identified floodplain. They attributed upward stoping dissolutional cavities formed within...
Abstract A method for quantitatively assessing sinkhole susceptibility (spatial probability) and hazard (spatio‐temporal has been developed independently tested in a 50 km 2 sector of the Ebro Valley evaporite karst. Three genetic types sinkholes have mapped floodplain terrace surface: 947 small cover‐collapse (type 1, terrace), large collapse 2, floodplain) subsidence depressions 3, floodplain). The type 1 inventory includes two temporal populations: 447 formed before 24 November 2005, 500...