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Adopting a new approach for finding missing people using GIS techniques: A case study in Saudi Arabia’s desert area

  • Faisal Sulaiman Almujalli and Hamad Ahmed Altuwaijri EMAIL logo
Published/Copyright: August 21, 2023
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Open Geosciences
From the journal Open Geosciences Volume 15 Issue 1

Abstract

Every year, hundreds of people go missing in the wilderness of Saudi Arabia. There is an urgent need to examine modern geographic techniques for finding such people. Geographical information systems, for example, play a crucial role in wilderness search and rescue (WiSAR), not only in mapping probability areas but also in applying further analysis and modeling methods to reduce time and effort and to guide life-saving task forces in the right direction. In this study of a hypothetical missing-person case in Saudi Arabia, two standard WiSAR models are compared: ring and mobility. In the presented study situation, both models can be used. However, the new approach used in the mobility model drastically reduces the extent of the possible search area, from 101,787 km2 in the ring model to 335.34 km of likely trails and unpaved roads, and also provides exact directions to where the missing person may be found.

Keywords: search and rescue; WiSAR; geographic information systems; mobility model

1 Introduction

Search and rescue (SAR) is the operation for locating missing individuals as soon as possible [1]. “Search” is the term used for the first part of the operation, which entails locating the missing item or subject. “Rescue” refers to the second phase, which entails saving the missing item or subject after determining its location and returning it to a safer area [2]. Cases of missing persons (excluding kidnappings) may occur in urban areas; these are usually associated with children, elderly people, or mentally ill individuals [3]. Cases also occur outside urban areas in the wilderness (wilderness search and rescue [WiSAR] cases); these typically involve hikers, riders, tourists, etc. [4,5].

When a person is missing outside of a city, or in a wilderness area, SAR personnel face the task of locating them. This challenge involves limited resources and the possibility of a long search period, which can reduce the survival chances of the missing person [6]. The most common method for locating a missing individual is to create probability maps depicting potential locations. Numerous researchers have employed the ring model to create such probability maps [2,7].

Since World War I, SAR strategies and methods have evolved by utilizing dogs to locate wounded soldiers on battlefields (National Search and Rescue Dogs Association). Following World War II, WiSAR techniques evolved to include mathematical frameworks to increase the likelihood of locating missing objects [2]. Over time, these techniques evolved into different approaches, including the use of airplanes and helicopters, which continue to be employed in many WiSAR missions worldwide [8,9]. In addition, World War II witnessed a rise in the usage of probability maps, created by mathematical calculations or based on lost-person behavior, which resulted in the creation of probability areas identifying the most probable locations where an object might be located [7].

SAR approaches have evolved to incorporate remote sensing techniques, such as drones and unmanned technologies [1,3,10,11,12,13,14], as well as various geographical information systems (GIS) and mapping techniques, such as geostatistical and network analysis [7,15,16,17]. However, a variety of WiSAR-related factors, such as terrain, land cover, climate, and weather conditions, as well as a lack of data, play a crucial role in selecting the most appropriate approach. One factor of particular importance is the behavior of the missing person, as awareness of this can lead to a more subjective approach [18].

In this study, we aim to provide an overview of WiSAR in the Kingdom of Saudi Arabia regarding the methods used by local task forces and volunteering groups. We also adopt a new approach that is more suitable for people in arid and semi-arid regions, which share the same environmental and anthropogenic characteristics as those in a hypothetical-case study in the Al-Quwayiyah governorate in the middle of Saudi Arabia. Many areas of the world share similar environmental characteristics to those of Saudi Arabia, including Australia, where 70% of the country is classified as semi-arid or arid, with higher proportions still in central and western regions [19].

1.1 WiSAR missions in Saudi Arabia

Between 2009 and 2020, over 2,497 people went missing in the Saudi Arabian wilderness; 112 of these were found deceased, representing roughly 4.5% of the total number [20]. However, according to official reports from volunteer groups [21], up to 25% of missing-person cases in Saudi Arabian deserts each year end with the death of the individual involved. In addition, since 2014, WiSAR missions in Saudi Arabia have been led by the police instead of the civil defense force, with the help of volunteers who are typically untrained and unqualified.

The WiSAR process in Saudi Arabia usually begins when relatives of a missing person contact the local police in the province concerned. Usually, the police in Saudi Arabia start the investigation after 24 h by calling the local telecommunication company to inquire about the last time the missing person’s phone was connected to the network (cell sites); this process involves a further period of between 1 and 5 h. Meanwhile, the relatives of the missing person contact the volunteering groups. This also takes up several hours until they meet at the last known point (LKP)/last point seen, which is generally around the cell site area where the initial planning point (IPP) is determined. In other circumstances, if the missing person does not have a phone, the IPP starts at the point last seen (PLS), i.e., the location where the missing person was seen last [2].

According to the AOUN Association for SAR [21], the police and volunteer groups in Saudi Arabia use methods and tactics in WiSAR that rely on the rescuers’ experience with the surrounding terrain and land cover accumulated from previous tasks, with limited use of spatial technologies and mapping techniques, such as the Google Earth Engine, to explore the spatial nature of the area. Task forces are then sent to different destinations based on this accumulated information. At this point, the ground force (cars) and the air force (gliders and autogiros) start searching in different directions and linking up with each other using wireless communication and GPS to pinpoint their exact location.

What distinguishes WiSAR cases in Saudi Arabia is that about 90% of the SAR tasks are not about searching for the missing person but searching for the missing person’s vehicle, which is usually an easy object to find, compared with searching for a person [21]. This is primarily because the people who go missing in Saudi Arabia are often local tourists, campers, and herders who have cars to move around on dirty roads. These vehicles can sometimes get stuck in the sand or break down, leading to the individuals becoming lost or missing. Furthermore, due to severe climate and terrain conditions, missing persons are usually found close to their cars due to the difficulty in walking and moving around in such an environment [21].

The time a person can spend without water and food is contingent on age, health, and weather conditions, and may range from a few hours to several days. Theoretical search areas exceeding 5,026 km2 for every 40 km walked per day are possible if the missing person was driving a car. In contrast, the distance that a person can travel on foot varies according to the factors mentioned above and the terrain of the area, from a few hundred meters to up to 40 km per day in the case of a nominal walking speed of 5 km/h for 8 h a day [7]. Moreover, in many cases of missing people in the wilderness of Saudi Arabia, especially those during summer, the persons involved have died within 24 h of them being reported missing. In some of these cases, the direct distance between the location of the deceased person and the nearest safe place was not more than 2–3 km [21], suggesting that WiSAR operations have often been carried out without proper geospatial planning in advance.

1.2 GIS methods in WiSAR

In recent years, GIS has become highly significant in the planning of WiSAR missions [2,7,15,16,17,22]. In some cases, GIS technologies are too complex to be used in a short-term operations search because the many elements involved, including cost, training, data, and map sharing, can impact operations [5]. However, the ring model, the mobility model, and network analysis are the three most common methods for implementing GIS in WiSAR missions. In this study, because of a shortage of data sources (such as unpaved roads and hikers’ trail information), only the ring and mobility models were considered.

1.2.1 Ring model

The ring model is the most popular technique for creating probability of area (POA) maps. It is often known as the Euclidean distance model [7]. It is a primary geostatistical analysis method based on Koopman’s mathematical search theory [1,23]. Euclidean distance is used in the ring model, starting at the ring radius representing the IPP, where PLS and LKP generally exist [2]. From a 5% possibility of finding the missing person in the first ring to a 95% chance in the final ring, each successive ring signifies an increasing likelihood of finding the person [22]. The approach is novel because it prioritizes the search area, giving greater weight to closer rings. In addition, the ring model can be implemented with little effort using any GIS software or even a paper map [7]. However, the ring model is also limited because it relies on projected data to run in GIS software, which may be easily misunderstood when working with GPS data in the field. It ignores additional inputs such as geography and land use distribution.

1.2.2 Mobility model

The International Search and Rescue Incident Database defines mobility as “the amount of time the subject was moving.” This is the time a person spends walking away from the IPP [16], which is an essential factor in WiSAR missions. The mobility model is a method to make POA maps. It is similar to the cost–distance analysis often used for building infrastructure, wildlife habitats, and studying anthropology [7,24]. The mobility model uses raster data, such as the digital elevation model (DEM), land use, and land cover data, which are calculated using map algebra to make speed and resistance raster layers. These layers show where a missing person could be by leaving out areas where they cannot go because of a steep slope or the way the land is covered [25]. Unlike the ring model, this method considers different factors when determining the location of a missing object or person. However, this method is very subjective because it mostly depends on human decisions when calculating inputs [7].

1.3 Study area

The Al-Quwayiyah Governorate (Figure 1) is a large region in the central Saudi province of Arriyadh. It covers an area of 51,725 km2. The Al-Quwayiyah Governorate alone occupies about 14% of Arriyadh Province, which makes it the sixth-largest governorate in Saudi Arabia. Despite the vast area of the Al-Quwayiyah Governorate, the total population is less than 89,544. Topographically, the Al-Quwayiyah Governorate is a desert area with only a few urban regions along the Arriyadh–Makkah Highway, which passes through the area at an elevation of around 606–1,505 m. In the summer, temperatures exceed 48°C, and annual rainfall is less than 100 mm. Such severe climate and topographic conditions are also found in other countries around the world, and it is almost impossible for people to survive in such conditions anywhere without adequate water, food, and shelter. It is therefore especially important to address the problems associated with SAR in such environments, as missing persons in such places often fail to survive long enough before they are found, unlike in other areas, where missing individuals can survive for longer due to an abundance of resources necessary for life.

Figure 1 Study area. Al-Quwayiyah Governorate.
Figure 1

Study area. Al-Quwayiyah Governorate.

2 Materials and method

Though a missing person’s chances of survival drop precipitously over time [7], there are still two crucial considerations to bear in mind:

  1. the POA

  2. the probability of detection (POD).

Either of these may be modified to increase the probability of success (POS), which is calculated as follows [26]:

POS = POA × POD .

For instance, GIS methods can aid in increasing POS by utilizing models such as ring and mobility to improve the estimation of POD [16]. Alternatively, the area of search may be reduced to increase POS [7]. However, we sought in this study to contribute more than just lowering the POA. Instead, we used the mobility model and cost–distance analysis to obtain a better understanding of where the missing person might be going.

To this end, we carried out a hypothetical-case study of a missing person in his late fifties driving a 4 × 4 car. This matches the profile of tens of missing persons in Saudi Arabia each year. The PLS of the missing person was at the coordinates of 23°11′38″N, 44°41′53″E in the central area of the Al-Quwayiyah Governorate; at this location, the IPP was determined to be at the same point.

2.1 Ring model

We used multiple ring buffer (analysis) in ArcMap 10.8 to design six separate buffer zones around the IPP, assuming that the missing individual was traveling away from the PLS in his 4 × 4 vehicle at an average speed of roughly 30 km/h before the vehicle broke down. Using Euclidean distance, we were able to divide the search area into concentric rings, with a 15% chance of finding the missing person within a 30 km distance from the IPP (an area of 2,827 km2) and a 90% chance within a 180 km distance from the IPP (a total of 101,787 km2) (Figure 2).

Figure 2 Ring model at the IPP.
Figure 2

Ring model at the IPP.

2.2 Mobility model

The mobility model used in this study serves two primary purposes:

  1. decreasing the POA

  2. estimating the exact POD that represents the possible final resting place of the missing person.

This approach is built on the assumption that a missing individual will head straight for the next hamlet bypassing any complex terrain such as steep inclines. Using the United States Geological Survey (USGS) 30m DEM (Table 1), we divided the research region into nine categories (Table 2), ranging from easily traversable locations with surfaces of 0–2° to completely impassable areas, such as mountains and cliffs, with slopes of 30–70°.

Table 1

Used data characteristics

Data Source Type Resolution
DEM USGS Raster datasets 30 m
Saudi Arabia province/governorate boundaries General Authority for Statistics (SA) Vector datasets —
Table 2

Slope classes used in the mobility model

Slope New class Accessibility
0–2.1 1 Easy
2.1–3.8 2
3.8–5.8 3
5.8–8.4 4
8.4–11.9 5
11.9–16.3 6 Moderate
16.3–22.0 7
22.0–30.0 8 Almost impossible
30.0–70.6 9

After categorizing the slopes of the study area into nine distinct classes, cost–distance analysis was used to determine the least-cumulative-cost distance for each cell, as well as backlink raster analysis to determine the direction and identify the next neighboring cell (the succeeding cell) along the least-cumulative-cost path from a cell to its least-cost source. Then, cost pathways were computed from the IPP to the five closest villages in different directions where the missing individual might be found (Figure 3). The five villages are Halban in the northwest, Ruwaydah in the north, Umm Jadder in the east, Al Hafirah in the southeast, Moses in the south, and Qiran in the southwest; these are the places where the missing person might have gone.

Figure 3 Mobility model calculations and findings: (a) slope classes, (b) cost distance, (c) directions-backlink, and (d) POD findings.
Figure 3

Mobility model calculations and findings: (a) slope classes, (b) cost distance, (c) directions-backlink, and (d) POD findings.

3 Results and discussion

Unlike the ring model, the mobility model is dependent on information gathered from relatives about a missing person’s possible location, so POS is boosted by lowering POA and by determining the exact POD, thereby saving time and energy (a similar result was found in a previous study [7]). In this study, the mobility model narrowed the POA down to 335.34 km of unpaved roads where the missing person’s automobile could have broken down, from 101,787 km2 in the ring model. In addition, the mobility model reduced the time it would take the missing individual to drive the car from 21 h to 9 h 51 min, assuming a speed of 30 km per hour (Table 3). Therefore, the mobility model managed to reduce the POA and the possible mobility time of the missing person by almost 50% and determined their exact direction.

Table 3

Comparison of search areas and mobility times in ring and mobility models

POA % POA in ring model (area in km2) Mobility time in ring model* (h) POA in mobility model (distance in km) Mobility time in mobility model* (h:min)
15 2827.42 1 35.39 1:10
30 8482.28 2 52.56 1:45
45 14137.15 3 53.40 1:46
60 19792.02 4 59.63 1:58
75 25446.88 5 62.62 2:04
90 31101.75 6 71.72 2:23
Total 101787.52 21 335.34 9:51

*At an average speed of 30 km/h.

Although the ring model has several benefits, including speed and simplicity, it is evident that its results cannot go beyond the job of organizing prospective search areas, as other researchers have pointed out [7,22]. However, as noted above, the mobility model can provide helpful information about the missing person’s last known location and activity, which is an essential factor in WiSAR missions [16]. The advantages and disadvantages of the two models are summarized in Table 4.

Table 4

Advantages and disadvantages of ring and mobility models*

Ring model Mobility model
Advantages Easy analysis Considers terrain
Cheap and fast Driving speed included
No additional information is necessary Detects POD
Reduces time and effort in SAR
Disadvantages No additional information (terrain, vegetation) included Many information layers are necessary
No linear features (street/trails) included Equal walking speed regardless of driving up or downhill
Takes a too long time to search each zone Resolution depends on input data
Expertise and software are needed

*Adapted from the study of Drexel et al. [16].

4 Conclusion and future research

This research introduces a novel method for determining search areas and trails in Saudi Arabian WiSAR operations. This approach considers the physical and anthropogenic environment of Saudi Arabia and the behavior of missing persons there. In this study, we used a hypothetical-case study set in Saudi Arabia to compare and contrast the strengths of the two most popular models for WiSAR: the ring model and the mobility model. Compared to the ring model’s 101,787 km2, the mobility model’s 335.34 km of probable routes via which the missing person may have traveled significantly reduces the POA, and the time the missing person has to travel decreases from 21 h to 9 h, 51 min. As a result, either model can be used successfully in WiSAR. The mobility model, on the other hand, can identify the POD of a missing person to save time and improve the POA.

Overall, additional research is needed on the patterns of missing-person behavior in Saudi Arabia because these represent a factor in WiSAR operations and in the use of cutting-edge technology such as unmanned aerial vehicles as a primary instrument for locating such individuals. Moreover, research efforts should be directed toward georeferencing missing cases in geodatabase systems and employing various analyses to increase our geographical understanding of these issues.

Acknowledgments

We want to thank the General Directorate of Civil Defense in Saudi Arabia for sharing information. As well as the AOUN Association for Search and Rescue in Saudi Arabia for sharing their knowledge and experience about WiSAR cases in the country.

  1. Funding information: The authors extend their appreciation to the Deputyship for Research and Innovation, Ministry of Education in Saudi Arabia, for funding this research work via project no. IFKSUOR3-006-1.

  2. Author contributions: F.S.A. and H.A.A. contributed to the study conception and data collection. F.S.A. prepared the material, carried out the analysis, and wrote the first draft of the manuscript. H.A.A. added some text in the section on the literature review and results. F.S.A. and H.A.A. read and approved the final manuscript.

  3. Conflict of interest: The authors declare no conflicts of interest.

  4. Ethical approval: Not applicable.

  5. Data availability statement: Not applicable.

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Received: 2023-03-06
Revised: 2023-06-10
Accepted: 2023-07-08
Published Online: 2023-08-21

© 2023 the author(s), published by De Gruyter

This work is licensed under the Creative Commons Attribution 4.0 International License.

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  58. Adopting a new approach for finding missing people using GIS techniques: A case study in Saudi Arabia’s desert area
  59. Geological earthquake simulations generated by kinematic heterogeneous energy-based method: Self-arrested ruptures and asperity criterion
  60. Semi-automated classification of layered rock slopes using digital elevation model and geological map
  61. Geochemical characteristics of arc fractionated I-type granitoids of eastern Tak Batholith, Thailand
  62. Lithology classification of igneous rocks using C-band and L-band dual-polarization SAR data
  63. Analysis of artificial intelligence approaches to predict the wall deflection induced by deep excavation
  64. Evaluation of the current in situ stress in the middle Permian Maokou Formation in the Longnüsi area of the central Sichuan Basin, China
  65. Utilizing microresistivity image logs to recognize conglomeratic channel architectural elements of Baikouquan Formation in slope of Mahu Sag
  66. Resistivity cutoff of low-resistivity and low-contrast pays in sandstone reservoirs from conventional well logs: A case of Paleogene Enping Formation in A-Oilfield, Pearl River Mouth Basin, South China Sea
  67. Examining the evacuation routes of the sister village program by using the ant colony optimization algorithm
  68. Spatial objects classification using machine learning and spatial walk algorithm
  69. Study on the stabilization mechanism of aeolian sandy soil formation by adding a natural soft rock
  70. Bump feature detection of the road surface based on the Bi-LSTM
  71. The origin and evolution of the ore-forming fluids at the Manondo-Choma gold prospect, Kirk range, southern Malawi
  72. A retrieval model of surface geochemistry composition based on remotely sensed data
  73. Exploring the spatial dynamics of cultural facilities based on multi-source data: A case study of Nanjing’s art institutions
  74. Study of pore-throat structure characteristics and fluid mobility of Chang 7 tight sandstone reservoir in Jiyuan area, Ordos Basin
  75. Study of fracturing fluid re-discharge based on percolation experiments and sampling tests – An example of Fuling shale gas Jiangdong block, China
  76. Impacts of marine cloud brightening scheme on climatic extremes in the Tibetan Plateau
  77. Ecological protection on the West Coast of Taiwan Strait under economic zone construction: A case study of land use in Yueqing
  78. The time-dependent deformation and damage constitutive model of rock based on dynamic disturbance tests
  79. Evaluation of spatial form of rural ecological landscape and vulnerability of water ecological environment based on analytic hierarchy process
  80. Fingerprint of magma mixture in the leucogranites: Spectroscopic and petrochemical approach, Kalebalta-Central Anatolia, Türkiye
  81. Principles of self-calibration and visual effects for digital camera distortion
  82. UAV-based doline mapping in Brazilian karst: A cave heritage protection reconnaissance
  83. Evaluation and low carbon ecological urban–rural planning and construction based on energy planning mechanism
  84. Modified non-local means: A novel denoising approach to process gravity field data
  85. A novel travel route planning method based on an ant colony optimization algorithm
  86. Effect of time-variant NDVI on landside susceptibility: A case study in Quang Ngai province, Vietnam
  87. Regional tectonic uplift indicated by geomorphological parameters in the Bahe River Basin, central China
  88. Computer information technology-based green excavation of tunnels in complex strata and technical decision of deformation control
  89. Spatial evolution of coastal environmental enterprises: An exploration of driving factors in Jiangsu Province
  90. A comparative assessment and geospatial simulation of three hydrological models in urban basins
  91. Aquaculture industry under the blue transformation in Jiangsu, China: Structure evolution and spatial agglomeration
  92. Quantitative and qualitative interpretation of community partitions by map overlaying and calculating the distribution of related geographical features
  93. Numerical investigation of gravity-grouted soil-nail pullout capacity in sand
  94. Analysis of heavy pollution weather in Shenyang City and numerical simulation of main pollutants
  95. Road cut slope stability analysis for static and dynamic (pseudo-static analysis) loading conditions
  96. Forest biomass assessment combining field inventorying and remote sensing data
  97. Late Jurassic Haobugao granites from the southern Great Xing’an Range, NE China: Implications for postcollision extension of the Mongol–Okhotsk Ocean
  98. Petrogenesis of the Sukadana Basalt based on petrology and whole rock geochemistry, Lampung, Indonesia: Geodynamic significances
  99. Numerical study on the group wall effect of nodular diaphragm wall foundation in high-rise buildings
  100. Water resources utilization and tourism environment assessment based on water footprint
  101. Geochemical evaluation of the carbonaceous shale associated with the Permian Mikambeni Formation of the Tuli Basin for potential gas generation, South Africa
  102. Detection and characterization of lineaments using gravity data in the south-west Cameroon zone: Hydrogeological implications
  103. Study on spatial pattern of tourism landscape resources in county cities of Yangtze River Economic Belt
  104. The effect of weathering on drillability of dolomites
  105. Noise masking of near-surface scattering (heterogeneities) on subsurface seismic reflectivity
  106. Query optimization-oriented lateral expansion method of distributed geological borehole database
  107. Petrogenesis of the Morobe Granodiorite and their shoshonitic mafic microgranular enclaves in Maramuni arc, Papua New Guinea
  108. Environmental health risk assessment of urban water sources based on fuzzy set theory
  109. Spatial distribution of urban basic education resources in Shanghai: Accessibility and supply-demand matching evaluation
  110. Spatiotemporal changes in land use and residential satisfaction in the Huai River-Gaoyou Lake Rim area
  111. Walkaway vertical seismic profiling first-arrival traveltime tomography with velocity structure constraints
  112. Study on the evaluation system and risk factor traceability of receiving water body
  113. Predicting copper-polymetallic deposits in Kalatag using the weight of evidence model and novel data sources
  114. Temporal dynamics of green urban areas in Romania. A comparison between spatial and statistical data
  115. Passenger flow forecast of tourist attraction based on MACBL in LBS big data environment
  116. Varying particle size selectivity of soil erosion along a cultivated catena
  117. Relationship between annual soil erosion and surface runoff in Wadi Hanifa sub-basins
  118. Influence of nappe structure on the Carboniferous volcanic reservoir in the middle of the Hongche Fault Zone, Junggar Basin, China
  119. Dynamic analysis of MSE wall subjected to surface vibration loading
  120. Pre-collisional architecture of the European distal margin: Inferences from the high-pressure continental units of central Corsica (France)
  121. The interrelation of natural diversity with tourism in Kosovo
  122. Assessment of geosites as a basis for geotourism development: A case study of the Toplica District, Serbia
  123. IG-YOLOv5-based underwater biological recognition and detection for marine protection
  124. Monitoring drought dynamics using remote sensing-based combined drought index in Ergene Basin, Türkiye
  125. Review Articles
  126. The actual state of the geodetic and cartographic resources and legislation in Poland
  127. Evaluation studies of the new mining projects
  128. Comparison and significance of grain size parameters of the Menyuan loess calculated using different methods
  129. Scientometric analysis of flood forecasting for Asia region and discussion on machine learning methods
  130. Rainfall-induced transportation embankment failure: A review
  131. Rapid Communication
  132. Branch fault discovered in Tangshan fault zone on the Kaiping-Guye boundary, North China
  133. Technical Note
  134. Introducing an intelligent multi-level retrieval method for mineral resource potential evaluation result data
  135. Erratum
  136. Erratum to “Forest cover assessment using remote-sensing techniques in Crete Island, Greece”
  137. Addendum
  138. The relationship between heat flow and seismicity in global tectonically active zones
  139. Commentary
  140. Improved entropy weight methods and their comparisons in evaluating the high-quality development of Qinghai, China
  141. Special Issue: Geoethics 2022 - Part II
  142. Loess and geotourism potential of the Braničevo District (NE Serbia): From overexploitation to paleoclimate interpretation
https://doi.org/10.1515/geo-2022-0517
Keywords for this article
search and rescue; WiSAR; geographic information systems; mobility model
Creative Commons
BY 4.0

Articles in the same Issue

  1. Regular Articles
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  3. Petrography and mineralogy of the Oligocene flysch in Ionian Zone, Albania: Implications for the evolution of sediment provenance and paleoenvironment
  4. Biostratigraphy of the Late Campanian–Maastrichtian of the Duwi Basin, Red Sea, Egypt
  5. Structural deformation and its implication for hydrocarbon accumulation in the Wuxia fault belt, northwestern Junggar basin, China
  6. Carbonate texture identification using multi-layer perceptron neural network
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  8. Assessments of recent Global Geopotential Models based on GPS/levelling and gravity data along coastal zones of Egypt
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  17. Reconstruction of paleoglacial equilibrium-line altitudes during the Last Glacial Maximum in the Diancang Massif, Northwest Yunnan Province, China
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  19. Determining the long-term impact area of coastal thermal discharge based on a harmonic model of sea surface temperature
  20. Origin of block accumulations based on the near-surface geophysics
  21. Investigating the limestone quarries as geoheritage sites: Case of Mardin ancient quarry
  22. Population genetics and pedigree geography of Trionychia japonica in the four mountains of Henan Province and the Taihang Mountains
  23. Performance audit evaluation of marine development projects based on SPA and BP neural network model
  24. Study on the Early Cretaceous fluvial-desert sedimentary paleogeography in the Northwest of Ordos Basin
  25. Detecting window line using an improved stacked hourglass network based on new real-world building façade dataset
  26. Automated identification and mapping of geological folds in cross sections
  27. Silicate and carbonate mixed shelf formation and its controlling factors, a case study from the Cambrian Canglangpu formation in Sichuan basin, China
  28. Ground penetrating radar and magnetic gradient distribution approach for subsurface investigation of solution pipes in post-glacial settings
  29. Research on pore structures of fine-grained carbonate reservoirs and their influence on waterflood development
  30. Risk assessment of rain-induced debris flow in the lower reaches of Yajiang River based on GIS and CF coupling models
  31. Multifractal analysis of temporal and spatial characteristics of earthquakes in Eurasian seismic belt
  32. Surface deformation and damage of 2022 (M 6.8) Luding earthquake in China and its tectonic implications
  33. Differential analysis of landscape patterns of land cover products in tropical marine climate zones – A case study in Malaysia
  34. DEM-based analysis of tectonic geomorphologic characteristics and tectonic activity intensity of the Dabanghe River Basin in South China Karst
  35. Distribution, pollution levels, and health risk assessment of heavy metals in groundwater in the main pepper production area of China
  36. Study on soil quality effect of reconstructing by Pisha sandstone and sand soil
  37. Understanding the characteristics of loess strata and quaternary climate changes in Luochuan, Shaanxi Province, China, through core analysis
  38. Dynamic variation of groundwater level and its influencing factors in typical oasis irrigated areas in Northwest China
  39. Creating digital maps for geotechnical characteristics of soil based on GIS technology and remote sensing
  40. Changes in the course of constant loading consolidation in soil with modeled granulometric composition contaminated with petroleum substances
  41. Correlation between the deformation of mineral crystal structures and fault activity: A case study of the Yingxiu-Beichuan fault and the Milin fault
  42. Cognitive characteristics of the Qiang religious culture and its influencing factors in Southwest China
  43. Spatiotemporal variation characteristics analysis of infrastructure iron stock in China based on nighttime light data
  44. Interpretation of aeromagnetic and remote sensing data of Auchi and Idah sheets of the Benin-arm Anambra basin: Implication of mineral resources
  45. Building element recognition with MTL-AINet considering view perspectives
  46. Characteristics of the present crustal deformation in the Tibetan Plateau and its relationship with strong earthquakes
  47. Influence of fractures in tight sandstone oil reservoir on hydrocarbon accumulation: A case study of Yanchang Formation in southeastern Ordos Basin
  48. Nutrient assessment and land reclamation in the Loess hills and Gulch region in the context of gully control
  49. Handling imbalanced data in supervised machine learning for lithological mapping using remote sensing and airborne geophysical data
  50. Spatial variation of soil nutrients and evaluation of cultivated land quality based on field scale
  51. Lignin analysis of sediments from around 2,000 to 1,000 years ago (Jiulong River estuary, southeast China)
  52. Assessing OpenStreetMap roads fitness-for-use for disaster risk assessment in developing countries: The case of Burundi
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  54. A symmetrical exponential model of soil temperature in temperate steppe regions of China
  55. A landslide susceptibility assessment method based on auto-encoder improved deep belief network
  56. Numerical simulation analysis of ecological monitoring of small reservoir dam based on maximum entropy algorithm
  57. Morphometry of the cold-climate Bory Stobrawskie Dune Field (SW Poland): Evidence for multi-phase Lateglacial aeolian activity within the European Sand Belt
  58. Adopting a new approach for finding missing people using GIS techniques: A case study in Saudi Arabia’s desert area
  59. Geological earthquake simulations generated by kinematic heterogeneous energy-based method: Self-arrested ruptures and asperity criterion
  60. Semi-automated classification of layered rock slopes using digital elevation model and geological map
  61. Geochemical characteristics of arc fractionated I-type granitoids of eastern Tak Batholith, Thailand
  62. Lithology classification of igneous rocks using C-band and L-band dual-polarization SAR data
  63. Analysis of artificial intelligence approaches to predict the wall deflection induced by deep excavation
  64. Evaluation of the current in situ stress in the middle Permian Maokou Formation in the Longnüsi area of the central Sichuan Basin, China
  65. Utilizing microresistivity image logs to recognize conglomeratic channel architectural elements of Baikouquan Formation in slope of Mahu Sag
  66. Resistivity cutoff of low-resistivity and low-contrast pays in sandstone reservoirs from conventional well logs: A case of Paleogene Enping Formation in A-Oilfield, Pearl River Mouth Basin, South China Sea
  67. Examining the evacuation routes of the sister village program by using the ant colony optimization algorithm
  68. Spatial objects classification using machine learning and spatial walk algorithm
  69. Study on the stabilization mechanism of aeolian sandy soil formation by adding a natural soft rock
  70. Bump feature detection of the road surface based on the Bi-LSTM
  71. The origin and evolution of the ore-forming fluids at the Manondo-Choma gold prospect, Kirk range, southern Malawi
  72. A retrieval model of surface geochemistry composition based on remotely sensed data
  73. Exploring the spatial dynamics of cultural facilities based on multi-source data: A case study of Nanjing’s art institutions
  74. Study of pore-throat structure characteristics and fluid mobility of Chang 7 tight sandstone reservoir in Jiyuan area, Ordos Basin
  75. Study of fracturing fluid re-discharge based on percolation experiments and sampling tests – An example of Fuling shale gas Jiangdong block, China
  76. Impacts of marine cloud brightening scheme on climatic extremes in the Tibetan Plateau
  77. Ecological protection on the West Coast of Taiwan Strait under economic zone construction: A case study of land use in Yueqing
  78. The time-dependent deformation and damage constitutive model of rock based on dynamic disturbance tests
  79. Evaluation of spatial form of rural ecological landscape and vulnerability of water ecological environment based on analytic hierarchy process
  80. Fingerprint of magma mixture in the leucogranites: Spectroscopic and petrochemical approach, Kalebalta-Central Anatolia, Türkiye
  81. Principles of self-calibration and visual effects for digital camera distortion
  82. UAV-based doline mapping in Brazilian karst: A cave heritage protection reconnaissance
  83. Evaluation and low carbon ecological urban–rural planning and construction based on energy planning mechanism
  84. Modified non-local means: A novel denoising approach to process gravity field data
  85. A novel travel route planning method based on an ant colony optimization algorithm
  86. Effect of time-variant NDVI on landside susceptibility: A case study in Quang Ngai province, Vietnam
  87. Regional tectonic uplift indicated by geomorphological parameters in the Bahe River Basin, central China
  88. Computer information technology-based green excavation of tunnels in complex strata and technical decision of deformation control
  89. Spatial evolution of coastal environmental enterprises: An exploration of driving factors in Jiangsu Province
  90. A comparative assessment and geospatial simulation of three hydrological models in urban basins
  91. Aquaculture industry under the blue transformation in Jiangsu, China: Structure evolution and spatial agglomeration
  92. Quantitative and qualitative interpretation of community partitions by map overlaying and calculating the distribution of related geographical features
  93. Numerical investigation of gravity-grouted soil-nail pullout capacity in sand
  94. Analysis of heavy pollution weather in Shenyang City and numerical simulation of main pollutants
  95. Road cut slope stability analysis for static and dynamic (pseudo-static analysis) loading conditions
  96. Forest biomass assessment combining field inventorying and remote sensing data
  97. Late Jurassic Haobugao granites from the southern Great Xing’an Range, NE China: Implications for postcollision extension of the Mongol–Okhotsk Ocean
  98. Petrogenesis of the Sukadana Basalt based on petrology and whole rock geochemistry, Lampung, Indonesia: Geodynamic significances
  99. Numerical study on the group wall effect of nodular diaphragm wall foundation in high-rise buildings
  100. Water resources utilization and tourism environment assessment based on water footprint
  101. Geochemical evaluation of the carbonaceous shale associated with the Permian Mikambeni Formation of the Tuli Basin for potential gas generation, South Africa
  102. Detection and characterization of lineaments using gravity data in the south-west Cameroon zone: Hydrogeological implications
  103. Study on spatial pattern of tourism landscape resources in county cities of Yangtze River Economic Belt
  104. The effect of weathering on drillability of dolomites
  105. Noise masking of near-surface scattering (heterogeneities) on subsurface seismic reflectivity
  106. Query optimization-oriented lateral expansion method of distributed geological borehole database
  107. Petrogenesis of the Morobe Granodiorite and their shoshonitic mafic microgranular enclaves in Maramuni arc, Papua New Guinea
  108. Environmental health risk assessment of urban water sources based on fuzzy set theory
  109. Spatial distribution of urban basic education resources in Shanghai: Accessibility and supply-demand matching evaluation
  110. Spatiotemporal changes in land use and residential satisfaction in the Huai River-Gaoyou Lake Rim area
  111. Walkaway vertical seismic profiling first-arrival traveltime tomography with velocity structure constraints
  112. Study on the evaluation system and risk factor traceability of receiving water body
  113. Predicting copper-polymetallic deposits in Kalatag using the weight of evidence model and novel data sources
  114. Temporal dynamics of green urban areas in Romania. A comparison between spatial and statistical data
  115. Passenger flow forecast of tourist attraction based on MACBL in LBS big data environment
  116. Varying particle size selectivity of soil erosion along a cultivated catena
  117. Relationship between annual soil erosion and surface runoff in Wadi Hanifa sub-basins
  118. Influence of nappe structure on the Carboniferous volcanic reservoir in the middle of the Hongche Fault Zone, Junggar Basin, China
  119. Dynamic analysis of MSE wall subjected to surface vibration loading
  120. Pre-collisional architecture of the European distal margin: Inferences from the high-pressure continental units of central Corsica (France)
  121. The interrelation of natural diversity with tourism in Kosovo
  122. Assessment of geosites as a basis for geotourism development: A case study of the Toplica District, Serbia
  123. IG-YOLOv5-based underwater biological recognition and detection for marine protection
  124. Monitoring drought dynamics using remote sensing-based combined drought index in Ergene Basin, Türkiye
  125. Review Articles
  126. The actual state of the geodetic and cartographic resources and legislation in Poland
  127. Evaluation studies of the new mining projects
  128. Comparison and significance of grain size parameters of the Menyuan loess calculated using different methods
  129. Scientometric analysis of flood forecasting for Asia region and discussion on machine learning methods
  130. Rainfall-induced transportation embankment failure: A review
  131. Rapid Communication
  132. Branch fault discovered in Tangshan fault zone on the Kaiping-Guye boundary, North China
  133. Technical Note
  134. Introducing an intelligent multi-level retrieval method for mineral resource potential evaluation result data
  135. Erratum
  136. Erratum to “Forest cover assessment using remote-sensing techniques in Crete Island, Greece”
  137. Addendum
  138. The relationship between heat flow and seismicity in global tectonically active zones
  139. Commentary
  140. Improved entropy weight methods and their comparisons in evaluating the high-quality development of Qinghai, China
  141. Special Issue: Geoethics 2022 - Part II
  142. Loess and geotourism potential of the Braničevo District (NE Serbia): From overexploitation to paleoclimate interpretation
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