Over the past 25 years, geoconservation studies and interest in geoheritage have grown significantly. However, the assessment of degradation risks associated with geosites remains less explored. This aspect is crucial for the effective management and conservation of geosites, which face pressure from natural and human factors. In many countries, geosites are at risk of degradation or loss due to the lack of a systematic inventory and inadequate management. Therefore, evaluating and monitoring degradation risks is a priority for the scientific community. Common investigation schemes and approaches for recognizing and preventing threats to geosites are still lacking. This paper presents the first systematic literature review on degradation risk and related terms. Through an extensive search of widely used literature databases, 130 papers were selected and analyzed. The findings highlight a growing focus on quantitative approaches for the assessment of geoheritage degradation risk, with most research conducted at local scales, while identifying climate change as an underexplored yet critical factor. Future priorities include refining spatial and temporal scales, understanding degradation processes, and fostering global collaboration to improve conservation strategies.

Increasing interest in the natural environment and greater hiking activity have resulted in higher anthropogenic pressure in areas characterized by a geographic/physical setting that could present hazardous conditions. The development of these activities is influenced by the peculiar geomorphological and climatic conditions of the area. Visitors and hikers do not always have adequate cultural background and full awareness of natural dynamics, including the possibility of incurring hazardous conditions. For its cultural and landscape value and extraordinary trail network, the Portofino Promontory is frequented by more than a hundred thousand of hikers a year. However, due to the geomorphological characteristics of the area, the morphological features of the trail network (i.e., exposed paths, steep ups and downs, rocky sections with cables, etc.) and the peculiar meteo-climatic conditions, the number of accidents involving hikers has increased in the most recent years. This research uses a detailed LiDAR survey, a morphometric analysis, and a significant dataset of information on the frequentation of the hiking trail network and on the number of rescue operations carried out by the National Mountain Rescue and Speleological Service (CNSAS). These data have been related to the physical-geographical characteristics of the area. The results can be a useful tool for land management by the Park Authority.

Cultural geomorphology is a very recent discipline that studies the geomorphological component of a territory which embodies both a cultural feature of the landscape and its interactions with cultural heritage: this cultural approach concerns the dialogue and cultural integration between humanistic and scientific disciplines and can be extended to all the fields of Earth Sciences. Ophiolite rock masses strongly characterize the landscape: their greenish-black, sometimes red-brown colour; the steep profile of the slopes, which results from their greater resistance to erosion than the surrounding softer sedimentary rocks; the scarce or even absent vegetation cover. The value of ophiolites is not only related to scientific and aesthetic interests, but is also due to historical–geographical, cultural and socio-economic issues. In this research, we present the elements of cultural and landscape value related to the ophiolites of the Northern Apennines, and how these geological and geomorphological features have led to specific relationships with humankind and human geography. Indeed, ophiolites represent characteristic elements of popular culture with immediate reference to toponymy, local legends and religion. Ophiolites are also an element of great strategic importance, as they are crucial for human settlement, with specific reference to defence, and for mining and quarrying activities. The landscape of ophiolites is of great geological, geomorphological, hydrogeological and pedological interest, resulting in a high concentration of geosites, hence on the one hand the opportunity for enhancement and potential geotourism, and on the other hand the need for their protection and geoconservation.

Persistent Scatterer Interferometry (PSI) is one of the most powerful tools for identifying and monitoring areas exposed to surface deformations such as landslides or subsidence. In this work, we propose a new method that we named CAPS (Correlation Analysis on Persistent Scatterers), to extend the capability of PSI in recognizing and characterising areas influenced by complex ground deformations and differential motions. CAPS must be applied to both ascending and descending orbits separately and comprises three major steps: (i) calculating the cross-correlation matrix on detrended PS time-series; (ii) extracting PS pairs with similarity greater than a given threshold; (iii) grouping PS in families by sorting and classification. Thus, in both orbits, PS Families identify groups of PS with similar movements. This allows distinguishing sectors characterised by different displacements over time even in areas with similar LOS (Line of Sight) velocities. As test sites, we considered four different known geological scenarios: two representing landslide environments (Santo Stefano d’Aveto and Arzeno, both in Liguria, NW Italy) and two subsidence environments (Rome and Venice, urban and surrounding areas). This method proved to be versatile, applicable to different geological situations and at different scales of observation, for recognizing both regional and local differential deformations.