Geosciences

22 pages, 7977 KiB

Open AccessArticle

Unlocking Coastal Insights: An Integrated Geophysical Study for Engineering Projects—A Case Study of Thorikos, Attica, Greece

by Stavros Karizonis and George Apostolopoulos

Geosciences 2025, 15(6), 234; https://doi.org/10.3390/geosciences15060234 - 19 Jun 2025

Viewed by 281

Abstract

Urban expansion in coastal areas involves infrastructure development, industrial growth, and mining activities. These coastal environments face various environmental and geological hazards that require geo-engineers to devise solutions. An integrated geophysical approach aims to address such complex challenges as sea level rise, sea [...] Read more.

Urban expansion in coastal areas involves infrastructure development, industrial growth, and mining activities. These coastal environments face various environmental and geological hazards that require geo-engineers to devise solutions. An integrated geophysical approach aims to address such complex challenges as sea level rise, sea water intrusion, shoreline erosion, landslides and previous anthropogenic activity in coastal settings. In this study, the proposed methodology involves the systematic application of geophysical methods (FDEM, 3D GPR, 3D ERT, seismic), starting with a broad-scale survey and then proceeding to a localized exploration, in order to identify lithostratigraphy, bedrock depth, sea water intrusion and detect anthropogenic buried features. The critical aspect is to leverage the unique strengths and limitations of each method within the coastal environment, so as to derive valuable insights for survey design (extension and orientation of measurements) and data interpretation. The coastal zone of Throrikos valley, Attica, Greece, serves as the test site of our geophysical investigation methodology. The planning of the geophysical survey included three phases: The application of frequency-domain electromagnetic (FDEM) and 3D ground penetrating radar (GPR) methods followed by a 3D electrical resistivity tomography (ERT) survey and finally, using the seismic refraction tomography (SRT) and multichannel analysis of surface waves (MASW). The FDEM method confirmed the geomorphological study findings by revealing the paleo-coastline, superficial layers of coarse material deposits and sea water preferential flow due to the presence of anthropogenic buried features. Subsequently, the 3D GPR survey was able to offer greater detail in detecting the remains of an old marble pier inland and top layer relief of coarse material deposits. The 3D ERT measurements, deployed in a U-shaped grid, successfully identified the anthropogenic feature, mapped sea water intrusion, and revealed possible impermeable formation connected to the bedrock. ERT results cannot clearly discriminate between limestone or deposits, as sea water intrusion lowers resistivity values in both formations. Finally, SRT, in combination with MASW, clearly resolves this dilemma identifying the lithostratigraphy and bedrock top relief. The findings provide critical input for engineering decisions related to foundation planning, construction feasibility, and preservation of coastal infrastructure. The methodology supports risk-informed design and sustainable development in areas with both natural and cultural heritage sensitivity. The applied approach aims to provide a complete information package to the modern engineer when faced with specific challenges in coastal settings. Full article

(This article belongs to the Section Geophysics)

► Show Figures

Figure 1

16 pages, 1375 KiB

Open AccessReview

The Influence of Temperature on the Microstructure, Atterberg Limits, and Swelling Pressure of Bentonite Clay: A Review

by Lingling Li, Haiquan Sun, Xiaoyu Fang and Liangliang Lu

Geosciences 2025, 15(6), 233; https://doi.org/10.3390/geosciences15060233 - 18 Jun 2025

Viewed by 274

Abstract

The geological containment of high-level radioactive waste has become widely accepted among international organizations, and it has been adopted by many countries as part of their national nuclear waste disposal plan. The multi-barrier system, including the compacted bentonite blocks or pellets serving as [...] Read more.

The geological containment of high-level radioactive waste has become widely accepted among international organizations, and it has been adopted by many countries as part of their national nuclear waste disposal plan. The multi-barrier system, including the compacted bentonite blocks or pellets serving as human-made containment or buffer media, is the key component of high-level radioactive waste disposal, which contains a waste canister that isolates the nuclear waste from a human being geosphere for one million years. The bentonite clay surrounding the nuclear waste capsule is subjected to prolonged exposure to elevated temperatures because of the continuous decay of radioactivity. Long-term heating at high temperatures could change the buffers’ microstructural characteristics and physicochemical and hydromechanical properties, which can influence their self-sealing ability. This paper offers a comprehensive overview of the current understanding of thermal effects on bentonite-based buffer systems. The thermal impact on the microstructure, Atterberg limits, and swelling pressure of bentonite clay are intensely reviewed, and the findings are summarized. This review paper highlights new insights into the design of multi-layered containment approaches for high-level radioactive waste isolation. Full article

(This article belongs to the Section Geomechanics)

► Show Figures

Figure 1

35 pages, 6609 KiB

Open AccessReview

Petroleum Systems of the Shu-Sarysu Basin, Kazakhstan: A Review of Devonian–Permian Gas Potential

by Almas Zhumagulov, Auez Abetov, Mehrdad T. Manzari and Jamilyam Ismailova

Geosciences 2025, 15(6), 232; https://doi.org/10.3390/geosciences15060232 - 18 Jun 2025

Viewed by 1720

Abstract

The Shu-Sarysu Basin in central-southern Kazakhstan remains one of the underexplored gas-prone provinces, with 12 discovered gas fields including Amangeldy (884 Bcf) and Pridorozhnoye (225 Bcf). In the context of global energy transition, such basins require integrated geological assessment to constrain exploration potential. [...] Read more.

The Shu-Sarysu Basin in central-southern Kazakhstan remains one of the underexplored gas-prone provinces, with 12 discovered gas fields including Amangeldy (884 Bcf) and Pridorozhnoye (225 Bcf). In the context of global energy transition, such basins require integrated geological assessment to constrain exploration potential. Historical studies within the region were spatially limited and prematurely discontinued, resulting in fragmented datasets and a lack of modern interpretation. This review reassesses published geological data within a petroleum systems framework, applying contemporary geodynamic and stratigraphic concepts. Analysis shows that tectonostratigraphic evolution of the basin during Devonian–Permian time (390–250 Ma) favored formation of mature, gas-prone systems within structurally compartmentalized troughs, with effective source, reservoir, and seal configurations. Building on these findings, a three-tier classification of exploration zones is proposed based on system maturity, trap integrity, and gas shows, reflecting geological success probability. This provides a basis for prioritizing future exploration despite limited seismic and drilling coverage in many areas. Recommended priorities include digitization of archival data, structural modeling, modern geochemical and diagenetic analysis, and focused evaluation of promising areas to support future exploration. Full article

► Show Figures

Figure 1

18 pages, 15114 KiB

Open AccessArticle

Blue Light Fluorescence in Marine Sediments

by Emily Carter Jones, Kelsey A. Williams, Ervan G. Garrison and Paul A. Schroeder

Geosciences 2025, 15(6), 231; https://doi.org/10.3390/geosciences15060231 - 17 Jun 2025

Viewed by 565

Abstract

Mineral fluorescence under different portions of the visible and invisible light spectrum has a long history of scientific study. In our study of marine sediments from the Georgia Bight, we have utilized the blue portion of the light spectrum in the 445 nanometer [...] Read more.

Mineral fluorescence under different portions of the visible and invisible light spectrum has a long history of scientific study. In our study of marine sediments from the Georgia Bight, we have utilized the blue portion of the light spectrum in the 445 nanometer (nm) range. The use of fluorescence has proven very useful in microscopic analyses of carbonate minerals. While the sediment prism of the inner-to-mid continental shelf in the southeastern Atlantic is predominantly siliceous, the dissolution and deterioration of marine shell contribute a significant amount to the fabric of any sediment sample. Together with carbonate minerals such as dolomite, eroded from basement rock and redeposited on the shelf, a potentially robust fluorescent response was expected and observed in samples. In marine sediments, blue light illumination has produced an easily observed fluorescent response in both underwater and in laboratory settings. This fluorescence can be attributed to carbonate minerals—calcite/aragonite. Feldspars are major accessory minerals in the sediment prism of the Georgia Bight, and much of the observed fluorescence in our samples can be attributed to their presence. To identify specific minerals responsible for any observed fluorescence, X-ray diffraction and energy dispersive spectroscopy were utilized. This combined methodology of luminescent excitation, X-ray diffractometry and spectroscopy has produced the results reported herein. Full article

(This article belongs to the Section Geochemistry)

► Show Figures

Figure 1

23 pages, 3236 KiB

Open AccessArticle

Chemical and Mineralogical Characterizations of Different Kaolinitic Clays from Burkina Faso: Feasibility for the Synthesis of Geopolymer Binders

by Seick Omar Sore, Philbert Nshimiyimana, Adamah Messan, Elodie Prud’homme, François Tsobnang and Gilles Escadeillas

Geosciences 2025, 15(6), 230; https://doi.org/10.3390/geosciences15060230 - 17 Jun 2025

Viewed by 503

Abstract

Researchers are exploring eco-friendly alternatives to Portland cement, such as geopolymers, which require reactive aluminosilicate sources. This study evaluated the reactivity of six calcined clays (heated at 700 °C) in the presence of an alkaline solution. The calcined samples from kaolinite quarries in [...] Read more.

Researchers are exploring eco-friendly alternatives to Portland cement, such as geopolymers, which require reactive aluminosilicate sources. This study evaluated the reactivity of six calcined clays (heated at 700 °C) in the presence of an alkaline solution. The calcined samples from kaolinite quarries in Kamboinsé, Kandarfa, Saaba, Sabcé, Selogo, and Tougou were subjected to chemical and mineralogical analyses. The results indicated a high aluminosilicate content (>50%), with kaolinite reaching up to 83.1%, and an amorphous fraction of up to 31.8%, a key factor influencing reactivity. Geopolymer pastes, prepared using a 12 M NaOH solution and each of these calcined clays, exhibited varying setting times: 24 h for the Saaba clay (the most reactive) compared with 48 h or even up to 7 days for the least reactive. The evaluation of the compressive strength of the geopolymer pastes revealed varying performances depending on the composition of clay. The Saaba clay showed the highest strength (14 MPa), attributed to its high kaolinite content (83.1%) and amorphous phase (31.8%), and thus reactivity. This was followed by Kamboinsé with 10.5 MPa (58.3% kaolinite; 24.3% amorphous phase), Selogo with 4.6 MPa (42.9%; 20.4%), Tougou with 1.4 MPa (44.1%; 20.4%), Kandarfa with only 0.7 MPa (31.3%; 19.2%), and Sabcé, which did not set with 0 MPa (24.1%; 13.7%). A discussion between the chemical and mineralogical compositions of the different clays and the mechanical characteristics of the synthesized pastes highlighted the importance of kaolinite content and its amorphous nature on the reactivity of the geopolymer binders. These findings highlight its potential for applications such as stabilized bricks or geopolymer concrete, offering a low-carbon alternative to traditional materials. Full article

(This article belongs to the Section Geochemistry)

► Show Figures

Figure 1

15 pages, 805 KiB

Open AccessArticle

Moon-Induced Differential Rotation in Earth’s Interior: A Comprehensive Conceptual Model

by Chil-Yeong Kim, Eun-Kyoung Seo, You-Soon Chang and Chungwan Lim

Geosciences 2025, 15(6), 229; https://doi.org/10.3390/geosciences15060229 - 16 Jun 2025

Viewed by 700

Abstract

This study presents a novel conceptual model to explain the differential rotation within Earth’s layers, a phenomenon observed through seismic wave studies but not fully understood. While geodynamo theory and electromagnetic coupling models have been proposed to explain this phenomenon, our model offers [...] Read more.

This study presents a novel conceptual model to explain the differential rotation within Earth’s layers, a phenomenon observed through seismic wave studies but not fully understood. While geodynamo theory and electromagnetic coupling models have been proposed to explain this phenomenon, our model offers an alternative perspective focusing on the Moon’s tidal forces. Our model proposes that the Moon’s tidal forces play a crucial role in this process, acting as a braking mechanism on Earth’s rotation. We hypothesize that these tidal forces initially decelerate the Earth’s crust and mantle, with this effect sequentially transmitted to deeper layers. A key aspect of our model is the role of the liquid outer core in mediating this process. We suggest that the liquid state of the outer core delays the transmission of tidal friction, resulting in differential rotation between layers in contact with it. This delay mechanism provides a potential explanation for the observed rotational differences between the mantle and core. Our model demonstrates that about 66,000 years after the Moon’s formation, the tidal force slowed the crust–mantle rotation by approximately 5.5 degrees per year more than the core. Furthermore, we estimate that the frictional heat generated at the boundaries of differential rotation is about 0.3478 TW. At this rate, the outer core temperature would increase by approximately 13.4 K per billion years. This thermal effect may have significant implications for the long-term evolution of Earth’s core, potentially slowing its cooling rate and maintaining its liquid state. Our model thus provides a new perspective on the interplay between lunar tidal forces, Earth’s internal structure, and its thermal evolution, offering insights into the complex dynamics of our planet’s interior. Full article

(This article belongs to the Section Geophysics)

► Show Figures

Figure 1

12 pages, 4723 KiB

Open AccessArticle

Investigating Rayleigh Wave Dispersion Across the Carpathian Orogen in Romania

by Andrei Mihai, Laura Petrescu, Iren-Adelina Moldovan and Mircea Radulian

Geosciences 2025, 15(6), 228; https://doi.org/10.3390/geosciences15060228 - 16 Jun 2025

Viewed by 211

Abstract

The Carpathian orogen represents a natural laboratory for the study of geodynamic interactions between lithospheres of different ages. The ancient Archean Cratons, such as the East European Craton, and Proterozoic platforms like the Scythian and Moesian platforms collided with the younger Tisza and [...] Read more.

The Carpathian orogen represents a natural laboratory for the study of geodynamic interactions between lithospheres of different ages. The ancient Archean Cratons, such as the East European Craton, and Proterozoic platforms like the Scythian and Moesian platforms collided with the younger Tisza and Dacia mega-units, resulting in the formation of the current architecture of the Carpathian Mountains. To better understand how the lithospheric structure on Romanian territory changes from the East European Craton to younger European microplates, we use earthquake data recorded at the permanent broadband seismic stations of the Romanian National Seismic Network (RSN). Applying the multiple filter technique, we examine the dispersion of Rayleigh wave group velocities for earthquakes located within a 4000 km radius of the epicenter. Travel time tomography, conducted through fast marching surface tomography, helps us to construct group velocity maps for periods between 30 and 80 s. Our findings highlight a low-velocity body in front of the Vrancea slab, indicating asthenospheric upwelling due to slab verticalization. Full article

► Show Figures

Figure 1

16 pages, 2691 KiB

Open AccessArticle

Comparative Analysis of GMI and DPR Precipitation Measurements over Global Oceans During Summer Season

by Eun-Kyoung Seo

Geosciences 2025, 15(6), 227; https://doi.org/10.3390/geosciences15060227 - 15 Jun 2025

Viewed by 746

Abstract

This study provides a comprehensive comparison between Global Precipitation Measurement (GPM) Microwave Imager (GMI) and Dual-frequency Precipitation Radar (DPR) measurements through analysis of collocated precipitation at the 19 GHz footprint scale for pixels during hemispheric summer seasons (JJA for Northern Hemisphere and DJF [...] Read more.

This study provides a comprehensive comparison between Global Precipitation Measurement (GPM) Microwave Imager (GMI) and Dual-frequency Precipitation Radar (DPR) measurements through analysis of collocated precipitation at the 19 GHz footprint scale for pixels during hemispheric summer seasons (JJA for Northern Hemisphere and DJF for Southern Hemisphere). Precipitation pixels exceeding 0.2 mm/h are categorized into convective, stratiform, and mixed types based on DPR classifications. While showing generally good agreement in spatial patterns, the GMI and DPR exhibit systematic differences in precipitation intensity measurements. The GMI underestimates convective precipitation intensity by 13.8% but overestimates stratiform precipitation by 12.1% compared to DPR. Mixed precipitation shows the highest occurrence frequency (47.6%) with notable differences between instruments. While measurement differences for convective precipitation have significantly improved from previous Tropical Rainfall Measuring Mission (TRMM) Microwave Imager (TMI) and Precipitation Radar (PR) estimates (62% to 13.8%), the overall difference has increased (from 2.6% to 12.6%), primarily due to non-convective precipitation. Latitudinal analysis reveals distinct precipitation regimes: tropical regions (below ~30°) produce intense convective precipitation that contributes about 40% of total precipitation despite lower frequency, while mid-latitudes (beyond 30°) shift toward stratiform-dominated regimes where stratiform precipitation accounts for 60–90% of the total. Additionally, geographical variation in GMI-DPR differences shows a see-saw pattern across latitude bands, with opposite signs between tropical and mid-latitude regions for convective and stratiform precipitation types. A fundamental transition in precipitation characteristics occurs between 30° and 40°, reflecting changes in precipitation mechanisms across Earth’s climate zones. Analysis shows that tropical precipitation systems generate approximately three times more precipitation per unit area than mid-latitude regions. Full article

(This article belongs to the Section Climate and Environment)

► Show Figures

Figure 1

13 pages, 902 KiB

Open AccessArticle

The Role of Disorder in Foreshock Activity

by Giuseppe Petrillo

Geosciences 2025, 15(6), 226; https://doi.org/10.3390/geosciences15060226 - 15 Jun 2025

Viewed by 326

Abstract

Foreshocks, observed before some large earthquakes, remain debated in terms of their origins and predictive value. While aftershocks fit well within bottom-up triggering models like ETAS, foreshocks may arise from distinct preparatory processes. Observations suggest real seismic catalogs exhibit more foreshocks than ETAS [...] Read more.

Foreshocks, observed before some large earthquakes, remain debated in terms of their origins and predictive value. While aftershocks fit well within bottom-up triggering models like ETAS, foreshocks may arise from distinct preparatory processes. Observations suggest real seismic catalogs exhibit more foreshocks than ETAS predicts, and laboratory experiments show that fault heterogeneity enhances foreshock activity. Here, I use a numerical model that reproduces key statistical properties of seismicity to investigate the role of fault heterogeneity. My simulations confirm that increasing interface disorder promotes foreshocks, aligning with laboratory findings and suggesting that fault complexity influences seismic precursors. Full article

(This article belongs to the Special Issue Editorial Board Members' Collection Series: Natural Hazards)

► Show Figures

Figure 1

22 pages, 140947 KiB

Open AccessArticle

Monitoring of Temporal Changes in the Gravity Field as an Element of the Geophysical Safety System for Mine Barrier Pillars

by Łukasz Kortas

Geosciences 2025, 15(6), 225; https://doi.org/10.3390/geosciences15060225 - 13 Jun 2025

Viewed by 325

Abstract

Underground longwall mining conducted in the vicinity of the barrier pillars in the KWK ROW Ruch Marcel mine has led to volume changes in the rock mass. As the longwalls progressed, a gradual increase in stress occurred in the goaf overburden, as a [...] Read more.

Underground longwall mining conducted in the vicinity of the barrier pillars in the KWK ROW Ruch Marcel mine has led to volume changes in the rock mass. As the longwalls progressed, a gradual increase in stress occurred in the goaf overburden, as a result of which this part of the rock mass increased in density in relation to the surrounding strata. Seismic events occurring during mining as a result of elastic energy accumulation led to the relaxation of the medium and local decreases in its bulk density. The microgravimetric method is sensitive to variations in this physical parameter of rock. The most transparent effects of the differences in rock mass density can be observed by performing periodic local gravity field surveys and analysing their spatial and temporal variability. This paper analyses the relationship between ground deformations and the spatial and temporal gravity field distribution changes observed on the surface in the context of the safety of barrier pillars F1 and F2 in Marklowice (the GSB-GFO testing ground of project EPOS-PL+). Relative gravimetric surveys, referenced to the determined absolute values of g, were performed in 7 series over the period of 2021–2023. The collected data made it possible to chart differential maps of gravity field changes and anomalies with Bouguer reduction. The differential anomaly distributions between successive survey series and the reference series were analysed. This served as the basis for assessing the safety of the barrier pillars maintained by the mine and the possibility of ground deformation occurrence on the surface. Full article

(This article belongs to the Section Geophysics)

► Show Figures

Figure 1

22 pages, 1945 KiB

Open AccessReview

Earth System Science and Education: From Foundational Thoughts to Geoethical Engagement in the Anthropocene

by Tiago Ribeiro and Clara Vasconcelos

Geosciences 2025, 15(6), 224; https://doi.org/10.3390/geosciences15060224 - 13 Jun 2025

Viewed by 600

Abstract

Understanding Earth as a complex, dynamic, and interconnected system is crucial to addressing the contemporary environmental challenges intensified in the Anthropocene. This article reviews foundational Earth System Science (ESS) developments, emphasizing its transdisciplinary nature and highlighting how it has evolved to address critical [...] Read more.

Understanding Earth as a complex, dynamic, and interconnected system is crucial to addressing the contemporary environmental challenges intensified in the Anthropocene. This article reviews foundational Earth System Science (ESS) developments, emphasizing its transdisciplinary nature and highlighting how it has evolved to address critical issues like climate change, biodiversity loss, and sustainability. Concurrently, Earth System Education (ESE) has emerged as an educational approach to foster holistic a understanding, environmental insights, and geoethical values among citizens. Integrating geoethics into ESE equips citizens with scientific knowledge and the ethical reasoning necessary for responsible decision making and proactive engagement in sustainability efforts. This article identifies system thinking and environmental insight as the key competencies that enable individuals to appreciate the interconnectedness of Earth’s subsystems and humanity’s role within this complex framework. This study advocates for embedding a holistic and geoethical view of the Earth system into formal and non-formal education, promoting inclusive, participatory, and action-oriented learning experiences. This educational shift is essential for empowering citizens to effectively address the environmental, social, and economic dimensions of sustainability, thereby fostering resilient, informed, and ethically responsible global citizenship in the Anthropocene. Full article

► Show Figures

Figure 1

22 pages, 2678 KiB

Open AccessArticle

Annual Variability in the Cordillera Blanca Snow Accumulation Area Between 1988 and 2023 Using a Cloud Processing Platform

by Júlia Lopes Lorenz, Kátia Kellem da Rosa, Rafael da Rocha Ribeiro, Rolando Cruz Encarnación, Adina Racoviteanu, Federico Aita, Fernando Luis Hillebrand, Jesus Gomez Lopez and Jefferson Cardia Simões

Geosciences 2025, 15(6), 223; https://doi.org/10.3390/geosciences15060223 - 13 Jun 2025

Viewed by 500

Abstract

Tropical glaciers are highly sensitive to climate change, with their mass balance influenced by temperature and precipitation, which affects the accumulation area. In this study, we developed an open-source tool to map the accumulation area of glaciers in the Cordillera Blanca, Peru (1988–2023), [...] Read more.

Tropical glaciers are highly sensitive to climate change, with their mass balance influenced by temperature and precipitation, which affects the accumulation area. In this study, we developed an open-source tool to map the accumulation area of glaciers in the Cordillera Blanca, Peru (1988–2023), using Landsat images, spectral indices, and the Otsu method. We analyzed trends and correlations between snow accumulation area, meteorological patterns from ERA5 data, and oscillation modes. The results were validated using field data and manual mapping. Greater discrepancies were observed in glaciers with debris cover or small clean glaciers (<1 km²). The Amazonian and Pacific sectors showed a significant trend in decreasing accumulation areas, with reductions of 8.99% and 10.24%, respectively, from 1988–1999 to 2010–2023. El Niño events showed higher correlations with snow accumulation, snowfall, and temperature during the wet season, indicating a stronger influence on the Pacific sector. The accumulation area was strongly anti-correlated with temperature and correlated with snowfall in both sectors at a 95% confidence level (α = 0.05). The highest correlations with meteorological parameters were observed during the dry season, suggesting that even minor changes in temperature or precipitation could significantly impact the accumulation area. Full article

(This article belongs to the Section Cryosphere)

► Show Figures

Figure 1

34 pages, 6941 KiB

Open AccessArticle

Integrating Soil Parameter Uncertainty into Slope Stability Analysis: A Case Study of an Open Pit Mine in Hungary

by Petra Oláh and Péter Görög

Geosciences 2025, 15(6), 222; https://doi.org/10.3390/geosciences15060222 - 12 Jun 2025

Viewed by 314

Abstract

This study presents a probabilistic geotechnical analysis of the Visonta Keleti-III lignite mining area, focusing on the statistical evaluation of soil parameters and their integration into slope stability modeling. The objective was to provide a more accurate representation of the spatial variability of [...] Read more.

This study presents a probabilistic geotechnical analysis of the Visonta Keleti-III lignite mining area, focusing on the statistical evaluation of soil parameters and their integration into slope stability modeling. The objective was to provide a more accurate representation of the spatial variability of geological formations and mechanical soil properties in contrast to traditional deterministic approaches. The analysis was based on over 3300 laboratory samples from 28 boreholes, processed through multi-stage outlier filtering and regression techniques. Strong correlations were identified between physical soil parameters—such as wet and dry bulk density, void ratio, and plasticity index—particularly in cohesive soils. The probabilistic slope stability analysis applied the Bishop simplified method in combination with Latin Hypercube simulation. Results demonstrate that traditional methods tend to underestimate slope failure risk, whereas the probabilistic approach reveals failure probabilities ranging from 0% to 46.7% across different sections. The use of tailored statistical tools—such as Python-based filtering algorithms and distribution fitting via MATLAB—enabled more realistic modeling of geotechnical behavior. The findings emphasize the necessity of statistical methodologies in mine design, particularly in geologically heterogeneous, multilayered environments, where spatial uncertainty plays a critical role in slope stability assessments. Full article

(This article belongs to the Section Geomechanics)

► Show Figures

Figure 1

16 pages, 23356 KiB

Open AccessArticle

Experimental Seismic Surveying in a Historic Underground Metals Mine

by John H. McBride, Lex Lambeck, Kevin A. Rey, Stephen T. Nelson and R. William Keach

Geosciences 2025, 15(6), 221; https://doi.org/10.3390/geosciences15060221 - 12 Jun 2025

Viewed by 277

Abstract

Underground mine surveys present unique challenges, including the logistics of deploying an energy source, placing geophones in solid rock, managing reverberation from the adit, and ensuring safety. We present the results of seismic surveying at the historic Deer Trail Mine in south-central Utah [...] Read more.

Underground mine surveys present unique challenges, including the logistics of deploying an energy source, placing geophones in solid rock, managing reverberation from the adit, and ensuring safety. We present the results of seismic surveying at the historic Deer Trail Mine in south-central Utah (USA). The mine is located along the eastern side of the Tushar Range. The surveys utilised a narrow, mostly horizontal adit, 120–510 m below the ground surface. The country rock consists of highly fractured and mineralised Permian to Pennsylvanian quartzites, shales, and limestones. A short test of a 96-channel common midpoint (CMP) P-wave profile was conducted using an accelerated weight-dropper source. We supplemented the P-wave survey with tests of surface-wave dispersion and horizontal-vertical spectral ratio modelling for shallow S-wave structure. These tests confirmed the capability to map shallow, small-scale structure. A conventional CMP 264-channel survey with an explosive source covered 1728 m. A static recording array was used for both surveys with 4.5-Hz vertical geophones. The conventional CMP profile imaged horizontal and dipping reflectors down to about 2000 m, interpreted as lithologic variations in the bedrock. Our study demonstrates the potential for high-resolution seismic exploration in an unconventional and challenging setting to guide the exploitation of deeply buried mineral resources. Full article

(This article belongs to the Section Geophysics)

► Show Figures

Figure 1

50 pages, 2738 KiB

Open AccessReview

Geophysical Survey and Monitoring of Transportation Infrastructure Slopes (TISs): A Review

by Zeynab Rosa Maleki, Paul Wilkinson, Jonathan Chambers, Shane Donohue, Jessica Lauren Holmes and Ross Stirling

Geosciences 2025, 15(6), 220; https://doi.org/10.3390/geosciences15060220 - 12 Jun 2025

Viewed by 607

Abstract

This review examines the application of the geophysical methods for Transportation Infrastructure Slope Monitoring (TISM). In contrast to existing works, which address geophysical methods for natural landslide monitoring, this study focuses on their application to infrastructure assets. It addresses the key aspects regarding [...] Read more.

This review examines the application of the geophysical methods for Transportation Infrastructure Slope Monitoring (TISM). In contrast to existing works, which address geophysical methods for natural landslide monitoring, this study focuses on their application to infrastructure assets. It addresses the key aspects regarding the geophysical methods most employed, the subsurface properties revealed, and the design of monitoring systems, including sensor deployment. It evaluates the benefits and challenges associated with each geophysical approach, explores the potential for integrating geophysical techniques with other methods, and identifies the emerging technologies. Geophysical techniques such as Electrical Resistivity Tomography (ERT), Multichannel Analysis of Surface Waves (MASW), and Fiber Optic Cable (FOC) have proven effective in monitoring slope stability and detecting subsurface features, including soil moisture dynamics, slip surfaces, and material heterogeneity. Both temporary and permanent monitoring setups have been used, with increasing interest in real-time monitoring solutions. The integration of advanced technologies like Distributed Acoustic Sensing (DAS), UAV-mounted sensors, and artificial intelligence (AI) promises to enhance the resolution, accessibility, and predictive capabilities of slope monitoring systems. The review concludes with recommendations for future research, emphasizing the need for integrated monitoring frameworks that combine geophysical data with real-time analysis to improve the safety and efficiency of transportation infrastructure management. Full article

(This article belongs to the Special Issue Innovative Approaches to Landslide Monitoring and Urban-Scale Slope Stability Analysis)

► Show Figures

Figure 1

25 pages, 20771 KiB

Open AccessArticle

Sedimentary and Early Diagenetic Responses to the Huaiyuan Movement During the Early–Middle Ordovician Transition in the Ordos Basin, North China

by Hao Quan, Zhou Yu, Zhanfeng Qiao, Chenqing Li, Pan Xia, Zhongtang Su, Huaguo Wen, Min Qin and Meng Ning

Geosciences 2025, 15(6), 219; https://doi.org/10.3390/geosciences15060219 - 12 Jun 2025

Viewed by 382

Abstract

The early Paleozoic Huaiyuan Movement created a major unconformity in the Ordos Basin, significantly influencing sedimentation and early diagenesis in both the overlying and underlying strata near the unconformity. However, the origins of the associated dolomite and silica near this unconformity remain poorly [...] Read more.

The early Paleozoic Huaiyuan Movement created a major unconformity in the Ordos Basin, significantly influencing sedimentation and early diagenesis in both the overlying and underlying strata near the unconformity. However, the origins of the associated dolomite and silica near this unconformity remain poorly understood. This study aims to reveal how this tectonic event controlled the Early–Middle Ordovician sedimentary environments and early diagenetic processes. The petrological and geochemical results indicate a progressive transition from a dolomitic tidal flat to an intra-platform depression, culminating in a mixed tidal flat during the Early-to-Middle Ordovician, driven by the Huaiyuan Movement. Furthermore, this movement, accompanied by intense weathering and erosion, increased the supply of marine dissolved silica (DSi) and terrestrial nutrients. Consequently, extensive tidal-edge biogenic silica accumulated, which later precipitated as siliceous-cemented dolomite during a shallow-burial stage. We propose a conceptual model of the sedimentary–early diagenetic processes in response to the Huaiyuan Movement, providing novel insights into the regional paleoenvironmental evolution across the Early–Middle Ordovician transition in the Ordos Basin. Full article

► Show Figures

Figure 1

17 pages, 4022 KiB

Open AccessArticle

Assessing the Impact of Past Flood on Rice Production in Batticaloa District, Sri Lanka

by Suthakaran Sundaralingam and Kenichi Matsui

Geosciences 2025, 15(6), 218; https://doi.org/10.3390/geosciences15060218 - 11 Jun 2025

Cited by 1 | Viewed by 474

Abstract

Flood risk to rice production has previously been examined in terms of river basins or administrative units, incorporating data about the flood year, inundated area, precipitation, elevation, and impacts. However, there is limited knowledge about this topic, as most flood impact studies have [...] Read more.

Flood risk to rice production has previously been examined in terms of river basins or administrative units, incorporating data about the flood year, inundated area, precipitation, elevation, and impacts. However, there is limited knowledge about this topic, as most flood impact studies have focused on loss and damage to people and the economy. It remains important to identify how flood risk to rice production can be better identified within a long-term, community-based, analytical framework. In addition, flood risk studies in Sri Lanka tend to focus on single-year flood events within an administrative boundary, making it difficult to fully comprehend risks to rice production. This paper aims to fill these gaps by investigating long-term flood risk levels on rice production. With this aim, we collected and analyzed information about rice production, geospatial data, and 15-year precipitation records. Temporal-spatial maps were generated using Google Earth Engine JavaScript coding, Google Earth Pro, and OpenStreetMap. In addition, focus group discussions with farmers and key informant interviews were conducted to verify the accuracy of online information. The collected data were analyzed using descriptive statistics, GIS, and linear regression analysis methods. Regarding rice production impacts, we found that floods in the years 2006–2007, 2010–2011, and 2014–2015 had significant impacts on rice production with 20.5%, 75.8%, and 16.6% reductions, respectively. Flood risk maps identified low-, medium-, and high-risk areas based on 15-year flood events, elevation, proximity to water bodies, and 15-year flood-induced damage to rice fields. High risk areas were further studied through field discussions and interviews, showing the connection between past floods and poor water governance practices in terms of dam management. Our linear regression analysis found a marginal negative correlation between total seasonal rainfall and rice production. Full article

(This article belongs to the Section Natural Hazards)

► Show Figures

Figure 1

17 pages, 4663 KiB

Open AccessArticle

New Data from Minor Mountainous Lakes as High-Resolution Geological Archives of the Northern Apennines, Italy: Lake Moo

by Yago Nestola and Stefano Segadelli

Geosciences 2025, 15(6), 217; https://doi.org/10.3390/geosciences15060217 - 11 Jun 2025

Viewed by 321

Abstract

Sedimentary basins developed in mountain belts are natural traps of catchment erosion products and can produce comprehensive palaeoflood records that extend beyond instrumental or historical data. This study investigates the Lake Moo plain (1120 m a.s.l.), located in the Mt. Ragola (1712 m [...] Read more.

Sedimentary basins developed in mountain belts are natural traps of catchment erosion products and can produce comprehensive palaeoflood records that extend beyond instrumental or historical data. This study investigates the Lake Moo plain (1120 m a.s.l.), located in the Mt. Ragola (1712 m a.s.l.) ophiolitic massif in the Northern Apennines (Italy), which serves as an excellent case study for inferring the chronology of past flood events due to its position relative to the dominant atmospheric flow and its favorable geological and geomorphological characteristics. The Northern Apennines is a relatively understudied region regarding the reconstruction of past Holocene flood activity through the analysis of lake sediments and peat bogs, compared with areas like the Alps. The main objective of this research was to analyze sediment cores taken from a lake situated in a catchment area dominated by ultramafic rock lithologies and associated residual weathering cover deposits. This allowed us to detect and characterize past flood events in the Ligurian–Emilian Apennines. A multidisciplinary approach, integrated with reference data on geology, geomorphology, pedology, and petrography, enabled a more detailed description of the changes in the hydrologic cycle. Collectively, these data suggest that periods of increased past flood activity were closely linked to phases of rapid climate change at the scale of the Ligurian–Emilian Apennines. The preliminary results suggest that floods occurring during periods of temperature drops have distinct characteristics compared with those during temperature rises. Full article

(This article belongs to the Section Hydrogeology)

► Show Figures

Figure 1

24 pages, 3562 KiB

Open AccessArticle

Building Resilience: Youth Learning Through Earthquake Shaking Simulations

by Gemma Musacchio, Agostino Goretti and Fabrizio Meroni

Geosciences 2025, 15(6), 216; https://doi.org/10.3390/geosciences15060216 - 10 Jun 2025

Viewed by 562

Abstract

This paper illustrates how youth education can foster resilience and promote risk awareness through interactive learning. It presents Shake It!, an engaging, hands-on educational module designed for middle school students that integrates risk education with experiential activities. The module begins with an [...] Read more.

This paper illustrates how youth education can foster resilience and promote risk awareness through interactive learning. It presents Shake It!, an engaging, hands-on educational module designed for middle school students that integrates risk education with experiential activities. The module begins with an introduction to structural components, construction materials, and seismic behaviour. Students then engage in experiential learning by building and testing models on educational shaking tables. Through this process, they explore key concepts such as building vulnerability, resonance, and earthquake-resistant constructions. The central message is that building response to earthquakes can be understood through hands-on learning, and that effective protection is achievable, making the engagement of younger generations in resilience education a key step toward building safer communities. Shake It! has been successfully tested with several hundred students, both during open days at the National Institute of Geophysics and Volcanology and in classroom settings. The activity consistently receives positive feedback for its ability to actively involve students and effectively raise awareness about earthquake risks in an accessible way that enhances retention. Full article

(This article belongs to the Collection Education in Geosciences)

► Show Figures

Figure 1

24 pages, 3887 KiB

Open AccessArticle

Applying Quantitative Fluorescence Techniques to Investigate the Effectiveness of Deep-Seated Mudstone Caprocks in the Junggar Basin, NW China

by Jiangxiu Qu, Keshun Liu, Hailei Liu, Minghui Zhou, Xiujian Ding and Ming Zha

Geosciences 2025, 15(6), 215; https://doi.org/10.3390/geosciences15060215 - 10 Jun 2025

Viewed by 1552

Abstract

The Central Depression of the Junggar Basin relies heavily on Permian lacustrine mudstone for deep-seated hydrocarbon sealing. This research investigated how the fluorescence parameters of caprock samples responded to the leakage of palaeo-oil zones based on measurements from SEM, Rock-Eval, and X-ray diffraction [...] Read more.

The Central Depression of the Junggar Basin relies heavily on Permian lacustrine mudstone for deep-seated hydrocarbon sealing. This research investigated how the fluorescence parameters of caprock samples responded to the leakage of palaeo-oil zones based on measurements from SEM, Rock-Eval, and X-ray diffraction analysis. First, two sets of control experiments were conducted to establish the proper grain-size range of 100–140 mesh for testing caprock samples in the research area using quantitative fluorescence technology. Subsequently, based on the examination of the rock pyrolysis parameters and the fluorescence parameters against TOC values, the conjecture was formed that the quantitative fluorescence technology test results were mostly unaffected by the primary hydrocarbons. Lastly, four fluorescence parameters were used to assess seal integrity: quantitative grain fluorescence intensity of the extract (QGF E intensity, the meaning of QGF is the same in this study), QGF spectral peaks (QGF λmax), the ratio of QGF intensity to fluorescence intensity at 300 nm on the QGF spectrum (QGF index), and total scanning fluorescence spectral ratio R₁ (TSF R₁). The Permian caprock can effectively seal hydrocarbons as evidenced by the decrease of QGF E intensity and QGF index values with depth. When hydraulic fracturing causes caprock failure, it can lead to complete leakage of hydrocarbons from the palaeo-oil zones. As the depth becomes shallower, the QGF E intensity value increases, the QGF index value decreases. Due to the differences in the migration pathways of hydrocarbons in the caprock, those leaked from the Permian palaeo-oil zone into the well PD1 caprock are mainly condensate and light–normal crude oil, while the hydrocarbons from the Carboniferous palaeo-oil zone into the well MS1 caprock consist predominantly of light–normal crude oil and medium–heavy crude oil. Full article

(This article belongs to the Section Geochemistry)

► Show Figures

Figure 1

26 pages, 3377 KiB

Open AccessArticle

Which Offers Greater Techno-Economic Potential: Oil or Hydrogen Production from Light Oil Reservoirs?

by Chinedu J. Okere, James J. Sheng and Princewill M. Ikpeka

Geosciences 2025, 15(6), 214; https://doi.org/10.3390/geosciences15060214 - 9 Jun 2025

Cited by 1 | Viewed by 472

Abstract

The global emphasis on clean energy has increased interest in producing hydrogen from petroleum reservoirs through in situ combustion-based processes. While field practices have demonstrated the feasibility of co-producing hydrogen and oil, the question of which offers greater economic potential, oil, or hydrogen, [...] Read more.

The global emphasis on clean energy has increased interest in producing hydrogen from petroleum reservoirs through in situ combustion-based processes. While field practices have demonstrated the feasibility of co-producing hydrogen and oil, the question of which offers greater economic potential, oil, or hydrogen, remains central to ongoing discussions, especially as researchers explore ways to produce hydrogen exclusively from petroleum reservoirs. This study presents the first integrated techno-economic model comparing oil and hydrogen production under varying injection strategies, using CMG STARS for reservoir simulations and GoldSim for economic modeling. Key technical factors, including injection compositions, well configurations, reservoir heterogeneity, and formation damage (issues not addressed in previous studies), were analyzed for their impact on hydrogen yield and profitability. The results indicate that CO₂-enriched injection strategies enhance hydrogen production but are economically constrained by the high costs of CO₂ procurement and recycling. In contrast, air injection, although less efficient in hydrogen yield, provides a more cost-effective alternative. Despite the technological promise of hydrogen, oil revenue remains the dominant economic driver, with hydrogen co-production facing significant economic challenges unless supported by policy incentives or advancements in gas lifting, separation, and storage technologies. This study highlights the economic trade-offs and strategic considerations crucial for integrating hydrogen production into conventional petroleum extraction, offering valuable insights for optimizing hydrogen co-production in the context of a sustainable energy transition. Additionally, while the present work focuses on oil reservoirs, future research should extend the approach to natural gas and gas condensate reservoirs, which may offer more favorable conditions for hydrogen generation. Full article

(This article belongs to the Special Issue Circular Economy in Energy Extraction: Geological Insights and Innovations)

► Show Figures

Figure 1

31 pages, 2587 KiB

Open AccessArticle

Assessment and Validation of a Geoethical Awareness Scale (GAS) for UNESCO Global Geoparks: A Case Study in Greece

by Alexandros Aristotelis Koupatsiaris and Hara Drinia

Geosciences 2025, 15(6), 213; https://doi.org/10.3390/geosciences15060213 - 6 Jun 2025

Cited by 1 | Viewed by 1954

Abstract

Geoethics, which addresses the ethical, social, and cultural dimensions of geoscientific activities, is essential for fostering responsible human engagement with the Earth, particularly within frameworks such as UNESCO Global Geoparks (UGGps). UGGps play a critical role in safeguarding geological heritage and advancing sustainable [...] Read more.

Geoethics, which addresses the ethical, social, and cultural dimensions of geoscientific activities, is essential for fostering responsible human engagement with the Earth, particularly within frameworks such as UNESCO Global Geoparks (UGGps). UGGps play a critical role in safeguarding geological heritage and advancing sustainable regional development. This study introduces the Geoethical Awareness Scale (GAS), a 32-item instrument developed across 16 thematic axes, designed to assess geoethical awareness. We analyzed responses from n = 798 residents across nine Hellenic UGGps using Exploratory and Confirmatory Factor Analyses, retaining items with factor loadings of ±0.30 or higher. Six factors emerged: (1) geological heritage conservation and sustainable georesource use, (2) community engagement and collaborative governance, (3) sustainability through geoenvironmental education, (4) environmental challenges and risk adaptation, (5) sustainable geotourism, and (6) climate awareness and ecosystem resilience. Collectively, these factors explained 60.12% of the variance, with Cronbach’s alpha values demonstrating acceptable to excellent reliability. Structural Equation Modeling confirmed the scale’s validity, with fit indices indicating acceptable model adequacy. Incremental indices suggested moderate alignment, while parsimony-adjusted metrics supported a balance between model complexity and fit. Overall, the GAS demonstrated generalizability and sufficient sample robustness. Correlation analyses highlighted the role of geoeducation, organizational involvement, and direct experience in fostering pro-geoconservation attitudes. While perceptions of sustainable development and ecosystem resilience varied geographically across UGGps, community engagement and governance remained consistent, likely reflecting standardized policy frameworks. GAS offers a valuable tool for assessing geoethical awareness and underscores the importance of targeted geoeducation and participatory governance in promoting ethical geoscientific practices within UGGps and similar socioecological systems. Full article

(This article belongs to the Section Geoheritage, Geoparks and Geotourism)

► Show Figures

Figure 1

21 pages, 6334 KiB

Open AccessArticle

Comparative Analysis of IMERG Satellite Rainfall and Elevation as Covariates for Regionalizing Average and Extreme Rainfall Patterns in Greece by Means of Bilinear Surface Smoothing

by Nikolaos Malamos, Theano Iliopoulou, Panayiotis Dimitriadis and Demetris Koutsoyiannis

Geosciences 2025, 15(6), 212; https://doi.org/10.3390/geosciences15060212 - 5 Jun 2025

Viewed by 338

Abstract

Remotely sensed data, including rainfall estimates and digital elevation models (DEMs), are increasingly available at various temporal and spatial scales, offering new opportunities for rainfall regionalization in regions with limited ground-based observations. We evaluate the efficacy of NASA’s Integrated Multi-satellitE Retrievals for GPM [...] Read more.

Remotely sensed data, including rainfall estimates and digital elevation models (DEMs), are increasingly available at various temporal and spatial scales, offering new opportunities for rainfall regionalization in regions with limited ground-based observations. We evaluate the efficacy of NASA’s Integrated Multi-satellitE Retrievals for GPM (IMERG) rainfall estimates and SRTM-derived elevation data as alternative spatial covariates for regionalizing average and extreme rainfall patterns across Greece. Using the Bilinear Surface Smoothing (BSS) framework, we assess and compare the regionalization of average daily rainfall and average annual maximum rainfall across multiple timescales (0.5 h to 48 h) by leveraging both IMERG-derived estimates and the elevation data as covariates. Additionally, the BSS framework is herein extended to provide Bayesian credible intervals for the final estimates, using the posterior variance estimate and the equivalent degrees of freedom determined through the Generalized Cross Validation error minimization procedure. Elevation-based models outperformed IMERG, particularly for indices of extreme rainfall, capturing the differential effects of orography. The exploration of the orographic effect based on the BSS framework revealed that the average annual rainfall maxima at small timescales exhibit a negative relation to elevation, which becomes positive and more significant with increasing timescale. However, IMERG proved valuable for regionalizing average daily rainfall, demonstrating its utility as a complementary tool. The results also underscore the role of temporal scale in regionalization efficiency of extreme rainfall, with higher accuracy observed at longer timescales (24 h and 48 h) and greater uncertainty at finer scales. Full article

(This article belongs to the Section Climate and Environment)

► Show Figures

Figure 1

36 pages, 6559 KiB

Open AccessReview

Advancements in Remote Sensing for Monitoring and Risk Assessment of Glacial Lake Outburst Floods

by Serik Nurakynov, Nurmakhambet Sydyk, Zhaksybek Baygurin and Larissa Balakay

Geosciences 2025, 15(6), 211; https://doi.org/10.3390/geosciences15060211 - 5 Jun 2025

Viewed by 609

Abstract

Glacial Lake Outburst Floods (GLOFs) have emerged as a critical threat to high-mountain communities and ecosystems, driven by accelerated glacier retreat and lake expansion under climate change. This review synthesizes advancements in remote sensing technologies and methodologies for GLOF monitoring, risk assessment, and [...] Read more.

Glacial Lake Outburst Floods (GLOFs) have emerged as a critical threat to high-mountain communities and ecosystems, driven by accelerated glacier retreat and lake expansion under climate change. This review synthesizes advancements in remote sensing technologies and methodologies for GLOF monitoring, risk assessment, and mitigation. Through a Preferred Reporting Items for Systematic reviews and Meta-Analyses (PRISMA)-guided systematic literature review and bibliometric analysis of studies from 2010 to 2025, we evaluate the transformative role of remote sensing in overcoming traditional field-based limitations. Central to this review is the exploration of multi-sensor data fusion for high-resolution lake dynamics mapping, machine learning algorithms for predictive risk modelling, and hydrodynamic simulations for flood propagation analysis. This review underscores the importance of these technologies in improving GLOF risk assessments and supporting early warning systems, which are crucial for safeguarding vulnerable high-mountain communities. It addresses existing challenges, such as data integration and model calibration, and advocates for collaborative efforts between scientists, policymakers, and local stakeholders to translate technological advancements into effective mitigation strategies, ensuring the sustainability of these at-risk regions. Full article

(This article belongs to the Special Issue Hydrological Processes and Climate Change in Eurasia)

► Show Figures

Figure 1

23 pages, 5814 KiB

Open AccessArticle

Milankovitch- and Millennial-Scale Sequences in the Late Piacenzian to Early Gelasian Shelf Succession of the Crotone Basin, Southern Italy

by Massimo Zecchin, Mauro Caffau and Octavian Catuneanu

Geosciences 2025, 15(6), 210; https://doi.org/10.3390/geosciences15060210 - 4 Jun 2025

Viewed by 352

Abstract

Integrated facies and micropaleontological analyses of the late Piacenzian to early Gelasian, middle shelf to lower shoreface succession of the Strongoli area, southern Italy, reveal a hierarchy of transgressive–regressive sequences. In particular, higher rank sequences up to ca. 40 m thick, composed of [...] Read more.

Integrated facies and micropaleontological analyses of the late Piacenzian to early Gelasian, middle shelf to lower shoreface succession of the Strongoli area, southern Italy, reveal a hierarchy of transgressive–regressive sequences. In particular, higher rank sequences up to ca. 40 m thick, composed of transgressive systems tract, highstand systems tracts and falling stage plus lowstand systems tracts, are composed of 10–11 lower rank sequences 2.5–4 m thick. Some micropaleontological parameters were defined: distal/proximal (D/P; ratio between distal and proximal benthic foraminifera); fragmentation (Fr; percentage of fragmentation of benthic foraminifera); P/B (ratio between planktonic and benthic foraminifera); abundance (total count of individuals); diversity (sum of the recognized species). Among these parameters, the D/P and Fr are suitable, if used in conjunction, to recognize uncertainty intervals containing the maximum flooding surface (between the D/P maxima and Fr minima) and the maximum regressive surface (between D/P minima and Fr maxima). Moreover, combining these parameters with the sedimentological evidence, it is possible to recognize transgressive and regressive trends of different hierarchical ranks. The present results are an example illustrating how an integration of different types of data allows the recognition of high-frequency sequences in shelf settings associated with minor shoreline shifts, which would otherwise have been unrecognized on the basis of only one kind of data. The present integrated approach, therefore, provides a way to improve the resolution of sequence stratigraphic analyses. Full article

(This article belongs to the Section Sedimentology, Stratigraphy and Palaeontology)

► Show Figures

Figure 1

19 pages, 8176 KiB

Open AccessArticle

Interference of Shallow Landslides in Overconsolidated Clays on the Functionality of an Important Internal Road Infrastructure

by Maurizio Ziccarelli

Geosciences 2025, 15(6), 209; https://doi.org/10.3390/geosciences15060209 - 3 Jun 2025

Viewed by 453

Abstract

The paper presents a case study on the impact of a shallow landslide in overconsolidated clays, which was triggered during the winter of 2004–2005 due to exceptionally high pore pressures, on the operativity and serviceability of a key road artery in Sicily. During [...] Read more.

The paper presents a case study on the impact of a shallow landslide in overconsolidated clays, which was triggered during the winter of 2004–2005 due to exceptionally high pore pressures, on the operativity and serviceability of a key road artery in Sicily. During the period from 2004 to 2021, the landslide experienced several reactivations, particularly during the winter months when increased rainfall led to rising pore water pressures. These recurrent events resulted in temporary road closures and continuous restoration efforts, causing significant inconvenience for local communities and substantial economic losses for commercial, tourism, and agricultural activities in the area. In 2018, a comprehensive study was launched to reconstruct the detailed geotechnical model of the landslide, analysing its mechanical and kinematic characteristics, pore pressure regime, the depth and geometry of the sliding surface, and the causes of the landslide. The study indicates that the primary causes of both the initial landslide and its subsequent reactivations were the poor mechanical properties of the involved soils and seasonal fluctuations in pore water pressures. To ensure long-term stabilisation, the most suitable interventions were identified as the permanent reduction of pore pressures through the installation of drainage trenches and the construction of a road embankment using gabions, which also serve as drainage structures. These measures are highly effective, relatively cost-efficient, easy to implement, and environmentally sustainable. Full article

(This article belongs to the Section Geomechanics)

► Show Figures

Figure 1

19 pages, 4662 KiB

Open AccessArticle

Morphological Parameters of Gullies Formed on Sandy Soils and Effects of Check Dams in Central Spain

by Jorge Mongil-Manso, Joaquín Navarro-Hevia, Javier Velázquez, Virginia Díaz-Gutiérrez and Ana-Carolina Toledo-Rocha

Geosciences 2025, 15(6), 208; https://doi.org/10.3390/geosciences15060208 - 3 Jun 2025

Viewed by 336

Abstract

Gully erosion constitutes a significant global problem, as gullies are a substantial source of sediment that harms rivers, affecting aquatic fauna and water quality, altering flow regimes, and degrading soil, among other impacts. Gullies have been extensively studied in clayey soils, where they [...] Read more.

Gully erosion constitutes a significant global problem, as gullies are a substantial source of sediment that harms rivers, affecting aquatic fauna and water quality, altering flow regimes, and degrading soil, among other impacts. Gullies have been extensively studied in clayey soils, where they occur more frequently, but less so in soils or materials with a sandy texture. Therefore, utilizing field measurements and aerial orthophotography, this study characterizes the morphology of a set of gullies located in the Central System mountains (central Spain), formed on sandy soils derived from granite weathering, under a Mediterranean-continental climate. Furthermore, the influence of check dams on the gully slope is also studied. The selected gullies for this study are permanent, linear, parallel, continuous, V-shaped, and semi-active. They are longer, narrower, and shallower than other gullies in significantly different soils with which they have been compared, although the width/depth ratio is similar. Additionally, check dams have considerably reduced the slope (11% on average and a 23% maximum reduction), which may result in a reduction in the flow velocity and erosive capacity. Consequently, it can be affirmed that the presence of numerous check dams significantly affects gully morphology. Full article

(This article belongs to the Section Geomechanics)

► Show Figures

Figure 1

17 pages, 7452 KiB

Open AccessArticle

Determination of the Dynamic Angle of Repose of Lunar Regolith Simulants

by Mateusz Pawłowski, Damian Pietrusiak, Jakub Wróbel and Janusz Kozubal

Geosciences 2025, 15(6), 207; https://doi.org/10.3390/geosciences15060207 - 2 Jun 2025

Viewed by 392

Abstract

The determination of the dynamic angle of repose (DAR) of lunar regolith simulants is essential for modeling material behavior during in situ resource utilization (ISRU) processes and lunar surface operations. This study presents a methodology and dedicated test rig employing digital image processing [...] Read more.

The determination of the dynamic angle of repose (DAR) of lunar regolith simulants is essential for modeling material behavior during in situ resource utilization (ISRU) processes and lunar surface operations. This study presents a methodology and dedicated test rig employing digital image processing to measure DAR for seven lunar regolith simulants, representing both Mare and Highland regions. Experiments were conducted under terrestrial gravity at rotational drum speeds of 2, 5, and 10 RPM, with standardized material fill and image capture procedures. For each simulant, lower, higher, and total DAR values were recorded, indicating complex dependencies on particle size distribution, mineralogy, and rotational speed. These measurements provide a critical dataset for numerical model calibration and the simulation of regolith handling systems under lunar conditions. The findings emphasize the necessity of selecting appropriate DAR parameters based on regolith type and operational scale to ensure accurate predictions of granular flow behavior in extraterrestrial environments. Full article

► Show Figures

Figure 1

25 pages, 9716 KiB

Open AccessArticle

Comparison of Neural Network, Ordinary Kriging, and Inverse Distance Weighting Algorithms for Seismic and Well-Derived Depth Data: A Case Study in the Bjelovar Subdepression, Croatia

by Ana Brcković, Tomislav Malvić, Jasna Orešković and Josipa Kapuralić

Geosciences 2025, 15(6), 206; https://doi.org/10.3390/geosciences15060206 - 2 Jun 2025

Viewed by 531

Abstract

In subsurface geological mapping, it is more than advisable to compare different solutions obtained with neural and other algorithms. Here, for such comparison, we used the previously published and well-prepared dataset of subsurface data collected from the Bjelovar Subdepression, a 2900 km² [...] Read more.

In subsurface geological mapping, it is more than advisable to compare different solutions obtained with neural and other algorithms. Here, for such comparison, we used the previously published and well-prepared dataset of subsurface data collected from the Bjelovar Subdepression, a 2900 km² large regional macrounit in the Croatian part of the Pannonian Basin System. Data on depth were obtained for the youngest (the shallowest) Lonja Formation (Pliocene, Quaternary) and mapped using neural network (NN), inverse distance weighting (IDW), and ordinary kriging (OK) algorithms. The obtained maps were compared based on square error (using k-fold cross-validation) and the visual interpretation of isopaches. Two other algorithms were also tested, namely, random forest (RF) and extreme gradient boosting (XGB) algorithms, but they were rejected as inappropriate for this purpose solely based on the visuals of the obtained maps, which did not follow any interpretable geological structures. The results showed that NN is a highly adjustable method for interpolation, with adjustment for numerous hyperparameters. IDW showed its strength as one of the classical interpolators, and its results are always located close to the top if several methods are compared. OK is the relative winner, showing the flexibility of variogram analysis regarding the number of data points and possible clustering. The presented variogram model, even with a relatively high sill and occasional nugget effect, can be well fitted into OK, giving better results than other methods when applied to the presented area and datasets. This was not surprising because kriging is a well-established method used exclusively for interpolation. In contrast, NN and machine learning algorithms are used in many fields, and these algorithms, particularly the fitting of hyperparameters in NN, simply cannot be the best solution for all. Full article

(This article belongs to the Section Geophysics)

► Show Figures

Figure 1

17 pages, 9711 KiB

Open AccessArticle

Monitoring the Melting of Snow Stored in Snow Dumps (Yuzhno-Sakhalinsk, Russia)

by Valentina Lobkina and Aleksandra Muzychenko

Geosciences 2025, 15(6), 205; https://doi.org/10.3390/geosciences15060205 - 1 Jun 2025

Viewed by 411

Abstract

This study reviews the melting rate of anthropogenic snow patches formed as a result of cleaning the territory of Yuzhno-Sakhalinsk city from snow and collecting it in designated areas known as snow dumps. Snow patches persisted at absolute altitudes of less than 50 [...] Read more.

This study reviews the melting rate of anthropogenic snow patches formed as a result of cleaning the territory of Yuzhno-Sakhalinsk city from snow and collecting it in designated areas known as snow dumps. Snow patches persisted at absolute altitudes of less than 50 m in the summers during the period of 2010–2022, except in 2017. The positive factor was the ratio of the relatively small area occupied by the anthropogenic snow patch and its significant height at the beginning of the melting period. The detailed observations of anthropogenic snow patch growth and melting were conducted by the authors starting in the winter season of 2017–2018. The snow volume collected in snow dumps during the winter season in Yuzhno-Sakhalinsk can reach 3000 m³. That is why it is necessary to determine how the anthropogenic snow patch will loosen the water through the warm season. Special models of anthropogenic snow patch melting do not exist. So, the authors review the ability of four glacier and snow cover melting model applications for such objects. The contribution of various parameters affecting the snow path melting rate was also determined. The collected factual data allowed for the development of empirical snow patch melting models. The largest errors resulting in the usage of reviewed models are related to the beginning (April) and ending (September–October) of the melting periods. Full article

(This article belongs to the Section Cryosphere)

► Show Figures

Figure 1

Journal Menu

Journal Browser

Geosciences, Volume 15, Issue 6 (June 2025) – 45 articles

Further Information

Guidelines

MDPI Initiatives

Follow MDPI