Abstract
Northwest Serbia has long been recognized for its rare and abundant mineral resources. A rare source of fluvial tin cassiterite ore has been identified in streams along the southern slopes of Cer Mountain. This tin deposit was first exploited during the Bronze Age, around the mid-second millennium BCE (Before the Common Era). Several surface-level copper sources in the Podrinje–Valjevo mountain range were known, with evidence suggesting that their exploitation began as early as the fourth millennium BCE. Archaeological surveys and excavations have uncovered numerous Late Bronze Age necropolises, while evidence of only a single lowland settlement from this period has been found. However, research has also revealed a significant number of hillforts from the Transitional period, marking their first appearance in this region. Material culture, along with a series of calibrated radiocarbon dates, points to the presence of culture originating farther to the north in southern Pannonia. These hillforts were all strategically located on the highest mountain peaks and were fortified with massive walls and defensive ditches clear indicators of a substantial transformation in landscape use between approximately 1000 and 850 BCE. Further analysis using Light Detection and Ranging technology uncovered the immense scale and architectural complexity of the Cikote stronghold, a scale unprecedented in earlier periods. In addition, a Geographic Information System-based viewshed analysis of 14 hillforts and lowland settlements from this era demonstrated that all sites were visually connected to at least one neighbouring location. Some strongholds maintained visual links with multiple sites, with lines of sight extending over several dozen kilometres.
1 Introduction
Tiny black grains from the fluvial deposits of the southern streams of Mount Cer may not signify much to the average twenty-first-century observer. Typically, these grains of cassiterite ore (SnO₂, ∼85% tin in the ore) were naturally mixed with garnet in this area, a semi-precious stone valued as a gemstone since the Bronze Age [1,2,3]. The emerging question is, how did we connect these ore-bearing grains to landscape utilization strategies from the end of the second millennium to the first centuries of the first millennium Before the Common Era (BCE)? In the late nineteenth century, dozens of large mound necropolises in the northwestern Serbia were uncovered (Figure 1) [4]. Despite 70 years of excavations covering 16 necropolises and extensive field surveys, no settlements associated with this population from the Late Bronze Age (1450–1200 BCE) have been found. In 2010, the Institute of Archaeology in Belgrade, in collaboration with Brooklyn College of The City University of New York, initiated a project focusing on tin and copper sources in the region [5]. This approach shifted away from traditional archaeological methods, choosing instead to begin with ore areas in hopes of locating settlements through their resource use. Concurrent excavations of several hillforts, combined with analyses of materials from previously excavated similar sites, also failed to uncover settlements or structures that could correspond to the wealthy mound graves from the Late Bronze Age. Pre-excavation surveys around the Paulje Bronze Age necropolis, aimed at protecting cultural heritage sites, included an extensive geomagnetic survey area. This survey, conducted over nearly a decade and complemented by rescue archaeological excavations, led to the discovery in 2021 of the first Late Bronze Age pit-houses just 100 m from the Paulje necropolis. One structure with a diameter of over 5 m and containing several smaller pits was confirmed by accelerator mass spectrometry (AMS) dating to be associated with the Late Bronze Age graves (fifteenth century BCE). A second pit-house nearby produced similar dates (fourteenth century BCE).

Map of the northwestern Serbia with registered mound necropolises and locations of copper and tin ores (graphic: Institute of Archaeology, Belgrade).
On the other hand, during the subsequent period known as the Transitional Period (1200–800 BCE), we witnessed the first emergence of hillfort settlements strategically located on high hilltops, fortified with substantial stone walls and ditches. This marks a significant shift in how the landscape was utilized, considering that in previous periods we did not find single stronghold. Moreover, material culture found at these hillforts does not correspond to earlier cultural phenomena [5]; instead, it represents an entirely new cultural complex in the region, whose centre was located far to the north in the Srem area, within the southern Carpathian Basin. These findings raise several important questions, particularly regarding the visual interconnectivity between hillforts and methodological issues related to defining and controlling the territory associated with each one.
This article aims to explore how changing strategies of landscape use between the Late Bronze Age and Early Iron Age in northwestern Serbia reflect broader socio-cultural and environmental transformations. Particularly, we analyse the emergence of hillforts, fortified settlements built on elevated terrains, and how their placement in relation to adjacent lowland settlements, valuable ore deposits, and visibility among sites can be meaningful. We suggest that such hillforts did not develop randomly but as intentional responses to changing needs, such as security concerns, domination of key resources, and the preservation of visual connections with neighbouring societies. By combining archaeological information, precise radiocarbon dating, and modern methods of visibility analysis, we hope to determine if such hillforts were part of a larger complex network. Finally, our intention is to illuminate why and how these changes in settlement patterns occurred, better understanding how early complex societies developed in the southern Carpathian Basin.
2 Methods
We began by analysing the material culture uncovered during our excavations and correlated it with a series of absolute AMS radiocarbon dates, which allowed us to isolate settlements that correspond specifically to the selected chronological period. To further investigate the strategic placement of these sites, we employed viewshed analysis a spatial technique within the Geographic Information System (GIS) designed to identify areas visible from particular observation points. The foundation of this method is a digital elevation model (DEM), which provides a 3D representation of the terrain. Based on this model, viewshed analysis simulates line-of-sight (LOS) visibility from a given location while accounting for natural obstructions such as mountains, valleys, vegetation, or other landscape features. The result is a raster map that distinguishes between visible and non-visible areas. Using this approach, the GIS software produced visibility fields for each hillfort and lowland settlement.
2.1 Viewshed in archaeology
The noun viewshed implies the natural environment that is visible from one or more viewing points, as described in Merriam-Webster dictionary (Merriam-Webstern.d.), which is an aspect of great interest for research in landscape archaeology and understanding spatial relationships between sites. Viewshed analysis, also known as visibility analysis or LOS analysis, is a geospatial technique which determines visibility between a point of interest and its surroundings. Nowadays, this is achieved using GIS software by tracing the LOS from a viewpoint, across a DEM to every cell of the raster system. A simple Boolean operation then calculates whether the cell exceeds the height of the viewpoint, giving it a binary result of either visible (1) or not visible (0) [6–8]. The resulting map illustrates the unobstructed view of the observer from the selected vantage point which provides valuable insight to the researcher on site visibility, intervisibility between sites, and visual control of territory.
Observations made from these maps allow drawing conclusions on selection strategy in the past. Namely, for prehistoric strongholds – such as Bronze Age and Iron Age hillforts, fortified settlements, and other defensive or high-status enclosures in Europe – visibility was often a key strategic factor. Many of these sites occupy prominent hilltops or ridges, presumably to command extensive views of the surrounding terrain or to be highly visible themselves. Viewshed analysis allows archaeologists to quantitatively evaluate these assumptions. Modelling what could be seen from a stronghold allows assessment of its defensive surveillance capabilities (e.g. the ability to spot approaching threats) and its visual prominence in the landscape [9–11]. Through cumulative viewshed analysis, these factors point to locational criteria in hillfort construction, which were often built in the most visually prominent parts of their regions [12]. On the other hand, visibility analysis may also provide an outlook for a more symbolic purpose of a dominant location of a structure, as proposed in the case of Tholos A at Apesokari (south-central Crete, Greece), which figuratively demonstrates territorial rights on overlooked lands [13].
Availability of GIS software, DEM maps of large areas, and other landscape data, like Digital Terrain Models (DTMs) derived from LiDAR (Light Detection and Ranging) surveys, facilitated growing number of researcher topics associated with visibility, intervisibility, and spatial networking patterns in the past several decades. Such studies underscore the importance of viewshed analysis in testing hypotheses about why prehistoric communities chose certain locations for their building sites, most prominently strongholds. In short, visibility studies provide a window into past human experiences of landscape and contribute to debates on defence strategies, communication, and display of power in prehistoric Europe. The remainder of this review provides a historical overview of GIS-based viewshed analysis, surveys the principal methods and algorithms, and highlights key case studies – with a focus on European prehistoric strongholds – before discussing recent technological advancements.
2.2 Historical development of viewshed analysis in GIS
As one can assume, visibility studies predate widespread adoption of computer technology in archaeological research, since the notion of view from sites always attracted the attention of scholars. A comprehensive overview of the early visibility studies, both non- and GIS-based, was presented by Lake and Woodman [14] in an attempt to illustrate the progress and challenges of the method. Before the development of easily accessible GIS software, applications were either informal investigations, statistical and quantitative approaches close to processual archaeology, or humanistic studies of landscape phenomenology. First publications of GIS-based analysis also suffered from the lack of formalized inferential strategy, before developing both processual and cognitive-processual stances and a more finely defined analytical approach. Advancement was exemplified with David Wheatley’s attempt to rebut the hypothesis that Neolithic long barrows were located irrespective of the number of other barrows visible by utilizing the cumulative viewshed map and a common statistical procedure – the Kolmogorov–Smirnov test [6,15,16].
During the 1990s, visibility analysis was also a subject of criticism, ranging from amendable technical and procedural problems to the more complex questions of ontological, epistemological, methodological, and ethical aspects [14]. Most common technical issues were the uncertainty in viewshed results related to the binary visible/not-visible output being sensitive to errors in elevation data, as well as changing visibility of an object due to its size and distance from the observer. Efforts to address these issues included “fuzzy” and “probable” viewshed modelling, where visibility is expressed as a probability or degree (rather than a hard binary) to account for potential errors or environmental factors (e.g. haze) that could obscure distant targets [17–19]. Similarly, Ogburn [20] introduced a “target size-sensitive” approach: he computed the maximum distance at which an object of known dimensions (e.g. a 4.5 m wide Inca storehouse) could be recognized by the human eye, incorporating human visual acuity and atmospheric clarity into the viewshed calculation. The result is a probabilistic viewshed map indicating, for instance, that within a certain radius the object would be clearly visible (high confidence), whereas beyond that distance the probability of recognition drops off. These approaches produce more nuanced visibility maps but require more inputs (object size, error estimates, etc.) and computational effort.
Disapproval concerning the theoretical approach prompted two disparate understandings of “perception” regarding the natural environment, the first referring to environmental factors that affect object recognition, like contrast between the object and background, atmospheric conditions, and direction of illumination. The other is derived from human factors including physical (body – mechanical constraints on the field of view), but also cognitive in the sense of cultural preconceptions of environmental stimuli. This ambiguity in perception of environment has induced a more complex comprehension of visibility as a subjective result of human–environment interaction, rather than an objective trait of the environment [14], which is evident in some new studies [21].
Visibility is understood as a form of communication – one that could convey messages about control, cooperation, or sacred geography – but one that operated within a cultural system of meaning. One of the objectives of visibility analysis is to understand the connection between physical and mental perspectives of a society in the past, using quantitative visibility models to inform about how people may have conceptualized and given meaning to their environment [21]. Socially instructed visibility patterns were taken into account in some more recent articles. Analysis of large dolmens marking tombs of the Gor River valley (Granada, Spain) revealed no significant association between a monument’s size and its viewshed extent, rather hinting at a distributed signalling system, comprising a demarcated cultural landscape and a sign of community presence and territorial claim [22]. Similar social signalling is present in the case of Sardinian Bronze Age megalithic towers (nuraghi), which were places to achieve maximal visual control as symbols of authority [23].
In the last decade, developments in technology and methodology further enhanced viewshed analysis, increasing both its accuracy and the scope of questions it can address. One major advancement has been the improvement of input data quality. High-resolution DEMs derived from LiDAR surveys have become more widely available and are revolutionizing archaeological topographic analyses, including viewsheds. LiDAR can produce sub-metre resolution terrain models even under forest canopies, providing a much more detailed surface for visibility modelling than older 30 or 90 m grids. The use of LiDAR-derived DTMs has notably improved the fidelity of viewshed results – subtle terrain undulations, mounds, or saddles that might be missed in coarse data are now accounted for [24,25]. For example, a recent GIS analysis in the Orăştie Mountains (Romania) leveraged a LiDAR-based DTM to compute total viewsheds around Dacian and Roman sites. The fine-grained data allowed researchers to identify small “dead ground” areas that would have been hidden from view and to calculate more realistic visual coverage statistics (e.g. percentage of landscape seen within various distance bands) [26]. With LiDAR, it also becomes feasible to incorporate vegetation modeling: by using the point cloud to reconstruct the height of forest canopies or hedgerows, one can simulate past views both with and without woodland cover. While reliably reconstructing prehistoric vegetation remains challenging, LiDAR data coupled with palaeoenvironmental evidence enable sensitivity analyses – e.g. running a viewshed with an assumed tree height of 5 m across certain areas to see how that affects visibility [27].
Another area of advancement is computational efficiency and scale. The increasing ubiquity of multi-core processors and cloud computing has opened the door to extremely large or intensive visibility analyses. Researchers are now computing extensive total viewsheds that cover entire regions or countries, something previously impractical [28]. High-performance computing can handle thousands of viewpoints or very high-resolution grids by parallelizing the LOS calculations. For instance, dedicated algorithms have been developed for GPU (graphics processing unit) acceleration of viewshed calculations, and “big data” spatial frameworks can distribute the computation of cumulative viewsheds for hundreds of points across computing clusters. These technical strides mean that archaeologists can attempt ambitious analyses – such as iterative visibility simulations or real-time interactive visibility in virtual landscapes – that push beyond the static, single-viewshed maps of the past [29–31].
Integration with other analytical techniques is also advancing the field. One notable trend is combining viewshed analysis with network analysis and graph theory, as described in the chapter Visibility networks from the comprehensive The Oxford Handbook of Archaeological Network Research [32]. Instead of treating each site’s viewshed in isolation, scholars model sites as nodes in a visibility network, with edges between nodes that can see one another. Network metrics (e.g. node degree, betweenness centrality, etc.) can then identify which sites are visual “hubs” or intermediaries in communication webs [21]. Brughmans and Brandes [33] introduced formal network patterns for visibility, proposing first- and second-order visibility graphs to represent cumulative viewshed relationships. This approach moves beyond mapping to statistically comparing observed intervisibility networks against hypothetical models (for example, to test if a network was optimized for certain signal paths or if it was a byproduct of other factors) [33]. Such integration of viewshed data with network science allows more rigorous exploration of how visual connectivity might reflect social, military, or political networks in prehistory.
Furthermore, machine learning and advanced spatial statistics are beginning to incorporate viewshed-derived variables. In predictive modelling of site locations, for example, visibility indices can be used alongside environmental factors (distance to water, soil fertility, etc.) to train models that predict where undiscovered sites might be. Attempts in preventive archaeology have included viewshed as one layer in logistic regression and machine-learning classifiers to identify areas with high potential for past settlement [34].
To sum up, by the 2010s, GIS-based viewshed analysis was regularly employed in high-impact archaeological research, often in combination with other spatial analyses. Its historical development can thus be characterized as a progression from basic LOS mapping towards more complex, realistic, and hypothesis-driven visibility models. Key milestones include the introduction of cumulative viewsheds in the mid-90s, the adoption of fuzzy/probabilistic methods by the late 90s, and continual improvements in computation and data integration in the ensuing decades. This trajectory sets the stage for the diverse methods and applications in use today.
Recent advancements have made viewshed analysis more accurate (through better data and error modelling) and more powerful (through better algorithms and integration with complementary methods). The ability to factor in vegetation, atmospheric conditions, or human visual acuity means modern visibility studies can approximate past realities more closely than ever before. Concurrently, the fusion of visibility analysis with network models, predictive algorithms, and other cutting-edge techniques is expanding the range of archaeological questions that can be tackled – from understanding regional defence systems to modelling how landscapes were perceived in a cognitive sense. These developments ensure that viewshed analysis remains at the forefront of landscape archaeology research, continually refining our understanding of the prehistoric world.
2.3 Practiced method
For our visibility analysis, we used the freeware open-source Quantum GIS (QGIS)programme. The DEM map of the researched area was downloaded from the free service of NASA Earthdata SRMT (Shuttle Radar Topography Mission) online database with a resolution of 3 arc-seconds (approximately 90 m), through the SRTM Downloader plug-in in QGIS. Visibility analysis was executed with the Visibility analysis plugin, version 1.9.1, created by the archaeologist Zoran Čučković, a research associate at the University of Clermont-Auvergne (France). Observer’s viewpoints were created using precise coordinates collected by the authors on the field using a South Galaxy G6 GNSS Rover. The radius of analysis was set to 70+ km, even though achieving such high ceiling of LOS is arguable and only plausible under ideal conditions. Observer height was set to 10 m to account for observer’s body height as well as possible structure that likely could have been used for watching over the surrounding area. The aforementioned structure, similar to watchtower, could have aided in observing over common sized vegetation and other objects that would otherwise obstruct the view. Viewshed analysis was set to binary calculation, meaning that targets are either visible or not visible. Earth curvature was taken into account, and atmospheric refraction was set to a default value (0.130).
3 Results
3.1 Archaeological excavations and remote sensing surveys
Archaeological excavations conducted in the last decade on some of the mentioned hillforts have uncovered similar prehistoric architecture and material culture that is not noticed before in the region of northwestern Serbia [5]. For example, at the Trojanov grad, during campaigns 2013 and 2014, a structure made of dry-wall stone technique (Figure 2) was discovered. This structure is located near a polygonal Roman tower, containing pottery from the Transitional period from the Late Bronze Age to Iron Age, i.e. Kalakača cultural group.

Photo of the prehistoric stone dry-wall at the Trojanov grad hillfort (photo: Institute of Archaeology, Belgrade).
Outside this prehistoric rampart was a shallow but wide artificial ditch, likely facilitating access to the western side. The LiDAR survey of the site, carried out in 2024, proved to be a transformative tool for documenting Trojanov Grad, which had long remained concealed beneath a dense forest canopy. Multiple drone flights produced centimetre-resolution point clouds and digital terrain models [35]. By varying flight parameters and integrating overlapping surveys, we achieved a remarkably clear topographic reconstruction of the site (Figure 3), with visible features such as the interior and exterior edges of the rampart, the prehistoric defensive ditch (Figure 3/1), prehistoric dry wall (Figure 3/2), and the polygonal base of the Roman tower (Figure 3/3).

LiDAR picture of the Trojanov Grad (graphic: Institute of Archaeology, Belgrade).
Similarly, on the highest peak of the Vidojevica ridge, a prehistoric hillfort with medieval fortification was identified, with finds from the Transitional period as well. Further, since 2014, excavations at the Cikote hillfort have uncovered remains of a stone rampart (Figure 4) constructed using dry-wall techniques [5], with wooden posts forming the wall’s outer section. The pottery found here also belonged to the Kalakača cultural group. The wooden post sample dated back to 973–840 BCE (sigma 1 range).

Remains of the stone rampart at the Cikote hillfort constructed using dry-wall techniques. Red colour is the result of burned wooden cassettes that was filled with crushed stones (photo: Institute of Archaeology, Belgrade).
A new LiDAR survey (Figure 5) further revealed a massive stronghold (250 m × 150 m) at the hilltop, with a surrounding wall (Figure 5/1), a wide defensive platform at the entrance (Figure 5/2), and a shallow artificial ditch in front of it (Figure 5/3). This stronghold, with the material culture only from the Transitional period covered the impressive surface about 4 ha. Our excavations did not confirm other archaeological features on Cikote except the stone wall, and a geomagnetic survey confirmed our excavation results that the whole southern wall was burned in one moment [36].

LiDAR picture of the Cikote hillfort (graphic: Rio Sava DOO, Belgrade).
3.2 Kalakača culture – relative and absolute chronology
Kalakača culture, as a distinct cultural phenomenon of the Early Iron Age in southern Pannonia, was identified several decades ago by Medović [37] as a pre-Basarabi layer, i.e. the Bosut IIIa horizon. Although some early authors questioned the existence of this phase or horizon of the Early Iron Age, today its classification appears much clearer and scientifically well-founded. It is now more appropriately recognized as a cultural group, which occupied a significantly larger territory than initially assumed. In addition to Srem and southern Bačka, the bearers of this group also inhabited the peri-Pannonian border zone, and stylistic typological features characteristic of Kalakača pottery have been identified in central Pomoravlje [38], as well as in southern Pomoravlje and the Vardar valley [39].
According to Medović, the Kalakača horizon in southern Pannonia was dated to the Ha B period of Central European chronology, i.e. between 900 and 750 BCE, or even earlier [39]. Stojić places it in the Iron Age Ic in the Pomoravlje region, which chronologically corresponds to the aforementioned dating [38]. Later, thanks to radiocarbon dating, this group was dated in Srem to the tenth/ninth–eighth centuries BCE (Table 1) [40,41]. As for relative chronology, most scholars working on this topic agree that the Kalakača horizon was preceded by the channelled pottery horizon (Urnfield culture or the later phase of the Belegiš group, or the Vojvodina group of the transitional period), and that it was followed by the Basarabi group [37].
Absolute dates from the Kalakača cultural group sites mentioned in the text
No. | Site | Arch. context | Sample | Lab code | BP | calBC (σ2) | calBC (σ1) | Culture | Published lit. |
---|---|---|---|---|---|---|---|---|---|
1 | Brezjak, Paulje | Settlement, pit 5, SU7 | Charred wood | DeA 35728 | 2914 ± 25 | 1,206–1,015 | 1,190–1,050 | Belegiš II-Gava | This study |
2 | Brezjak, Paulje | Settlement, pit 5, SU 7 | Burnt animal bone | DeA 31402 | 2,871 ± 40 | 1,199–923 | 1,118–989 | Belegiš II-Gava | This study |
3 | Brezjak, Paulje | Settlement, pit 5, SU 7 | Charred wood | DeA 35729 | 2861 ± 26 | 1,118–930 | 1,107–983 | Belegiš II-Gava | This study |
4 | Ratača, Bogatić | Structure 4 (pit) | Charred wood | DeA-48945 | 2,856 ± 29 | 1,117–927 | 1,103–935 | Belegiš II-Gava | This study |
5 | Gomolava | Sector X, quadrant 21 | Seed | Poz-98016 | 2,775 ± 30 | 1,003–834 | 979–842 | Kalakača (?) | [41] |
6 | Cikote, Gradac | Trench 2, rampart | Charred wood | BETA 419886 | 2,770 ± 30 | 1,000–835 | 973–840 | Kalakača | This study |
7 | Gomolava | Sector I, qv. 95/XIV, layer 15 | — | GrN 7369 | 2,745 ± 60 | 1,045–801 | 968–818 | Kalakača | [42] |
8 | Brezjak, Paulje | Settlement, SU7, pit 5 | Burnt animal bone | DeA 34096 | 2,741 ± 44 | 988–809 | 921–827 | Kalakača | This study |
9 | Beška Kalakača | Block 15, layer 4 | Seed | Poz-100052 | 2,725 ± 30 | 922–811 | 897–831 | Kalakača | [41] |
10 | Bosut | Pit, sector II, block C, 28/IV | Seed | Poz-98017 | 2,680 ± 30 | 900–801 | 894–804 | Kalakača | [41,43] |
11 | Gomolava | Sector IV, qv. 83/X, layer 11 | / | GrN 7368 | 2,675 ± 50 | 926–778 | 898–799 | Kalakača | [44] |
12 | Gomolava | Locus 80/XVI, layer 14, sector III | Seed | Poz-98015 | 2,670 ± 30 | 900–794 | 891–801 | Kalakača (?) | [41] |
13 | Gomolava | Locus 81/XII, layer 18, sector IV | Seed | Poz-98013 | 2,630 ± 30 | 888–774 | 813–790 | Kalakača (?) | [41] |
Characteristic pottery forms of the Kalakača group include faceted or channelled-rim bowls, hemispherical bowls with thinned rims, high-handled cups with button-like protrusions, pear-shaped two handled beakers, and amphorae with everted rims and conical necks. Common ornaments feature diagonal channels, incised lines, stamped dimples, zigzags, and garland motifs. Typical decorative patterns include fir-branch designs, hatched triangles, wavy lines, and linked S-motifs.
As we mentioned, in recent years, Kalakača group pottery has been documented not only in the Pomoravlje and Danube regions but also at numerous sites along the peri-Pannonian rim, particularly in Mačva, Jadar, and Podgorina [5,45]. The main characteristics of this pottery do not differ from those found in Srem. A wide array of forms are represented, including bowls with inset channelled or faceted rims (Paulje, Cikote, Brangović, Trojanov Grad, and Vito); hemispherical bowls with unprofiled, thinned rims (Cikote, Brangović, and Vito); pear-shaped beakers with two handles (Brangović); cups with handles extending above the rim, often featuring one or two button-like protrusions at the top (Paulje, Cikote, Trojanov Grad, and Vito); and amphorae with long conical necks (Paulje, Cikote, Brangović, Trojanov Grad, and Vito). Common decorative elements include channels in the beaker belly (Paulje, Brangović, Trojanov Grad, and Vito); incised zigzag lines (Paulje, Cikote, and Brangović); hatched triangles (Cikote, Brangović, and Trojanov Grad); multiple incised lines (Paulje, Cikote, Brangović, Trojanov Grad, and Vito); and fir-branch motifs (Brangović), among others (Figure 6).

Plate with pottery from various archaeological settlements analysed in this article (graphic: Institute of Archaeology, Belgrade).
Given these identical stylistic and typological features, it appears that the material culture of the Kalakača group in Srem and the peri-Pannonian rim did not differ. This conclusion is supported by radiocarbon dates for the Kalakača group, with the earliest being contemporaneous and originating from Gomolava (Srem) and Cikote (Jadar) (Figure 6). Based on the available absolute dates, it seems that the group not only emerged simultaneously but also developed in parallel across both regions.
Regarding the relationship between the absolute and relative chronology of the Kalakača group, an important finding comes from Ratača near Bogatić. In one pit, fragments of pottery were discovered that correspond to the Gava–Belegiš II group, which is believed to have preceded the Kalakača group. This pottery, decorated exclusively with wide channels and lacking any features associated with the Kalakača group, was dated to the eleventh and the first half of the tenth century BCE (Figure 6). Thus, the absolute chronology confirmed not only the previously accepted relative chronology, most clearly illustrated by the stratigraphy at Gomolava, but also the other sites, where the channelled pottery of the Gava–Belegiš II type directly preceded the Kalakača group. A similar situation was observed in a pit at the site of Paulje in Brezjak near Loznica (Figure 6).
3.3 Topography and visibility of the settlements and hillforts
When considering all sites associated with the material culture of the Kalakača group in northwestern Serbia, we can identify 11 hillforts Vidojevica, Trojanov Grad, Koviljača, Orlovine, Ostenjak, Cikote, Plužac, Brangović, Vito, Taor, and Krčmar and two lowland settlements: Paulje, and Radalj. In addition, our analysis included two large contemporary proto-urban centres located along the northern boundary of the region: Gradina on Bosut and Gomolava. These settlements are situated in the Srem region of southern Pannonia, the cultural heartland of the Kalakača group. Notably, no graves have been discovered within this cultural horizon in the northwestern Serbia [5]. In the core territory, in the Kalakača group, burials have not yet been sufficiently researched, with scarce grave finds. Based on the existing data, not only inhumation [46–48] but also cremation as a treatment of the deceased was recorded [49]. This distribution presents a striking contrast to earlier periods while numerous fortified hilltop settlements are present, there are only three known open settlements and no burial sites, which are typically interpreted as a reflection of unstable conditions and a hostile environment, as well as possible partial transformation in population dynamics.
Significantly, the settlements of Gradina on Bosut and Gomolava fall within the visibility range of two major hillforts in the Cer area Trojanov Grad and Vidojevica as well as the Gradac–Koviljača hillfort, which strategically controlled a key road running upstream along the Drina River, as well as an important river crossing. Also, on the cumulative viewshed map (Figure 7), it seems that visibility range with Trojanov Grad also exists, which gives additional importance to Koviljača stronghold. One of the central questions in this type of analysis concerns the maximum distance of visibility under clear atmospheric conditions, particularly in the mountainous terrain. Based on available data and visibility modelling, optimal conditions likely enabled visual communication over distances of up to 50–100 km. In our specific case, the distance from Trojanov Grad to Gomolava and Bosut was 38 and 61 km, respectively, while the distance from Vidojevica to Gomolava and to Bosut measured 43 and 51 km. While there is no direct archaeological evidence for a communication system between these sites, it is highly plausible that some form of signalling was employed. It is also possible that visual communication was more effective at night due to fire or light-based signalling, although the content, complexity, and reliability of such messages remain unknown. In one field photo, under moderate haze and elevated humidity, the Cikote hillfort was clearly visible from Trojanov Grad a distance of 14 km (Figure 8). Behind it, other hills and low mountain ridges up to 30 km away were distinguishable, demonstrating the potential extent of intervisibility. Undoubtedly, the Cikote stronghold, together with Koviljača, Vidojevica, and Trojanov Grad, represents one of the most strategically significant positions, primarily because of its commanding oversight of the Jadar River valley and visual connectivity with several fortifications, otherwise positioned less optimally in relation to key regional sites.

(a) Cumulative viewshed map of the analysed settlements and strongholds (graphic: Institute of Archaeology, Belgrade). (b) Cumulative viewshed map of the analysed settlements and strongholds (graphic: Institute of Archaeology, Belgrade).

Photo of the Cikote hillfort from the Trojanov Grad (photo: Institute of Archaeology, Belgrade).
4 Discussion
This discussion interprets the results of spatial and viewshed analyses through a broader archaeological lens, integrating both functional and symbolic dimensions of landscape use in northwestern Serbia during the Late Bronze Age and Early Iron Age.
4.1 Strategic placement and topographic control
The location of hillforts in elevated and naturally defensible positions, as revealed by DEM and terrain analyses, suggests deliberate choices driven by strategic considerations. Most fortified sites dominate their immediate surroundings, offering commanding views of river valleys, access routes, and arable land. This pattern aligns with a broader trend across prehistoric Europe where hilltop positions were exploited not only for defence but also for territorial control and surveillance. Vidojevica hillfort was positioned at the farthermost western end of the Cer Mountain massif and had good visual communication with whole Mačva, Semberija, Bosut, and Gomolava settlements in Srem (Figure 7), but also Koviljača at the start of the Drina canyon valley that has clear contact with Vidojevica (Figure 9). The fortified site at Cikote, for instance, holds a key position over the Jadar River valley, while others such as Koviljača and Trojanov Grad appear to flank major corridors of movement. The clustering and distribution of these sites imply a shared logic of occupation that responds to both natural defensibility and visibility.

Photo of the Vidojevica hillfort from the Koviljača hillfort (photo: Institute of Archaeology, Belgrade).
Vidojevica, however, easily controlled the alluvial valley of the lower Drina and was positioned ideally for the defensive and scouting purposes. Furthermore, according to our photos, Vidojevica definitely could visually reach the Cikote hillfort (Figure 10). Even the strategic position of the Likodra hillfort, situated within the seemingly secluded Likodra River valley, should not be underestimated. First and foremost, the valley itself is narrow, flanked by steep, nearly impassable hills, and the surrounding area is rich in ore deposits and ancient mining activity. Additionally, the hillfort offers a direct LOS to Trojanov Grad (Figure 11), which likely explains why communities of the Transitional period chose to establish their stronghold on this distinctive rocky outcrop. Moreover, the visual connection between Likodra and the Plužac hillfort should be taken into account, as it appears that only a limited number of hillforts were able to maintain visual communication along the west–east axis (Figure 7). Unfortunately, although Orlovine – a medieval fortress that also yielded pottery from the Transitional period was situated in a highly advantageous strategic location, effectively controlling communication routes upstream from the Koviljača hillfort, its visual position was relatively poor (Figure 7), primarily due to the high hills that surround the site and obstruct long-range visibility.

Photo of the Trojanov Grad (1) and Vidojevica (2) from the Cikote hillfort (photo: Institute of Archaeology, Belgrade).

Photo of the Trojanov Grad from the Likodra hillfort (photo: Institute of Archaeology, Belgrade).
Trojanov Grad appears to have been the most important stronghold, as it controlled an extensive area (Figure 7), with visual coverage extending from the Bosut settlement in Srem to the Vito hillfort on Mount Povlen – a total of 11 sites. In addition to its broad viewshed, Trojanov Grad was also the closest hillfort to the Milinska and Cernica rivers, suggesting that the guards stationed there could monitor the tin-bearing river deposits as well as, potentially, copper sources in the nearby Srebrne Rupe mining area. Although there is no direct LOS to the Vidojevica hillfort, the construction of simple wooden watchtowers at several key locations on Cer could have easily bridged this gap in visual communication. The four eastern hillforts Brangović [50], Vito [45], and Krčmar each appear to have controlled their own local territories while also maintaining visual communication with at least one western hillfort. In contrast, the Taor hillfort was located on the opposite side of the mountain and had no visual connection with any of the sites included in our analysis. Notably, Trojanov Grad maintained visual contact with all three of the aforementioned eastern hillforts.
4.2 Visual networks and intervisibility
The viewshed analysis demonstrates that several hillforts were intervisible, forming a loosely connected network that spans large portions of the region. These visual links may have supported systems of communication, coordination, or even symbolic alignment. For example, intervisibility between sites like Cikote and the surrounding minor fortifications could imply signalling routes or zones of mutual awareness. This capacity for long-distance visibility may have been as much about asserting presence and territoriality as about practical signalling. In this sense, visibility could have served to display social power and community identity within a shared cultural framework.
4.3 Cultural attribution and symbolic landscape
The hillforts discussed here likely represent not only physical strongholds but also culturally charged locations. Their placement in dominant visual positions may have contributed to their symbolic significance. Drawing on perspectives from sensory archaeology and landscape phenomenology, these sites may have structured human experience, reinforcing notions of community, identity, and control. The absence of graves, combined with the strong emphasis on settlement hierarchy and visibility, points to a landscape structured more by spatial presence than by mortuary expression.
4.4 Towards a more interpretative framework
While the technical results provide a strong foundation, future work should more deeply explore how these landscapes were perceived, experienced, and remembered. Visibility was likely not just functional but embedded in a web of meanings: political, social, and possibly ritual. Ethnographic analogies and cross-regional comparisons could contextualize the spatial strategies observed here. In conclusion, this discussion has aimed to move beyond a descriptive summary of spatial data and towards an interpretive synthesis that recognizes the complexity of prehistoric landscape organization. The hillforts of northwestern Serbia emerge not only as defensive structures but also as significant elements in the construction of social landscapes shaped by both strategic logic and symbolic meaning.
5 Conclusions
The pottery assemblage and a series of absolute dates indicate the presence of a cultural group whose centre was located much farther to the north, in southern Pannonia. In that region, several protourban settlements have been excavated, characterized by substantial architecture and functioning as craft and economic hubs [43,51]. As is well known, this area is poor in heavy non-ferrous and precious metals, which suggests that at some point the Kalakača cultural group had to expand its territory towards regions rich in strategic raw materials.
In northwestern Serbia, no settlement matches the Srem sites in terms of settlement intensity. Therefore, the hillforts associated with the Kalakača culture in this area were likely military outposts, serving primarily to control the newly acquired territories. The protourban centres in Srem were tell-like sites with dense occupation layers and well-developed domestic architecture [43]. At present, there is no definitive evidence that these settlements were fortified with ditches or ramparts. While a few sites have documented deeper ditches, Medović [37] was unable to establish their precise chronology with certainty.
In contrast, the hillforts of northwestern Serbia feature only shallow and broad ditches, along with dry-stone walls, and notably lack architectural remains within the enclosures. Additionally, there is no evidence of armed conflict at the lowland settlements in northwestern Serbia, and the material culture shows no significant deviations from that of the core Kalakača group territory. One of the more striking differences, however, lies in the architecture. In Srem, houses were rectangular, above-ground structures built using wattle-and-daub techniques. In contrast, the Paulje settlement in northwestern Serbia revealed only rounded, sunken pit-houses dug deep into the ground.
Settlements from this period clearly demonstrate that each site maintained visual contact with at least one neighbouring location, while some strongholds were connected to multiple sites. An important observation is the distinction between a “strategic position” and a “visual strategic position” terms that, in some cases, reflect significantly different qualities. For example, hillforts such as Likodra, Brangović, and Orlovine were ideally located to control communication routes and defend important roads. However, these sites are surrounded by higher terrains, limiting their visibility and preventing significant visual contact with other contemporary sites. In contrast, hillforts like Vidojevica, Trojanov Grad, Vito, and Krčmar offered wide visual coverage and occupied exceptionally favorable “visual strategic positions.” These differences point to varying priorities in site selection and defence strategies. Also, we must distinguish between the concepts of strategic position and visual strategic position. The term strategic position is used to describe a place’s overall geographical and topographical advantages such as height, nearness to natural resources, and control over movement routes that likely determined settlement site for defensive and practical purposes. Conversely, the visual strategic position will denote the particular function of visibility and intervisibility in site use, such as long-distance LOS relations, landscape domination, and the promise of signalling or symbolic display. Rendering this distinction standard enables a subtler analysis of hillfort location, taking into account functional as well as communicative aspects of prehistoric landscape use.
While the above summary manages to place the study’s principal findings in perspective, the text can better indicate the overall relevance to prehistoric research in the larger area. Application of radiocarbon dates, archaeological excavations, and GIS-based viewshed analysis within this article provides insight into settlement strategies and spatial dynamics of the Transitional Period. The phenomenon of visually linked hillforts opportunistically positioned and spanning large areas is revealed to enhance visual control in territorial structure, resource management, and defence strategy. The findings not only clarify settlement transformation between the Late Bronze and Early Iron Ages but also provide a foundation for future cross-disciplinary research that potentially enhances knowledge on prehistoric societies in the study area. Subsequent research could build on this work by incorporating high-level vegetation modelling to further enhance visibility analysis. Palaeoenvironmental reconstruction and high-resolution LiDAR surveys could better show the role of vegetation cover in affecting former landscapes and settlement decisions. Moreover, experimental modelling of signalling systems – like fire or smoke signals – can be used to test the viability of long-range visual communication identified by this research, especially between far-away hillforts like Trojanov grad and Gomolava or Bosut. Experimental modelling could cross-validate hypotheses regarding social cohesion and information transfer in prehistoric society.
Moreover, the techniques employed herein have potential for use in heritage management and conservation. Cumulative viewshed analysis coupled with LiDAR data provides precise recording of archaeological sites that remain vulnerable to modern development and natural erosion. Improved site documentation supports the potential for planning successful conservation actions, preemptively assessing threats, and conserving archaeological heritage sustainably. Moreover, clearly defined visualized spatial networks and intervisibility patterns for sites would improve public education and cultural tourism initiatives so that tourists might better comprehend the intricate social landscapes and systems of communication that characterized prehistoric societies in northwestern Serbia.
Further research is certainly needed, and we anticipate that remote sensing techniques and future excavations will help fill existing gaps and provide new perspectives on viewshed analysis in northwestern Serbia.
Acknowledgments
The authors are grateful to the Rio Sava company for granting permission to publish the LiDAR survey in Figure 5. We are grateful to our colleagues R. Arsić and D. Radičević for kindly providing the data and drawings of the pottery. The authors would also like to express their sincere gratitude to the two anonymous reviewers for their highly constructive comments and valuable suggestions.
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Funding information: This article is the result of the project THE FLOW – Interactions-Transmission-Transformation: Long-distance connections in Copper and Bronze Age of the Central Balkans, funded by the Science Fund of the Republic of Serbia (Programme IDEAS, Grant no. 7750074).
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Author contributions: Conceptualization: V.F., A.B., and I.N.; methodology: V.F. and I.N.; GIS analysis: I.N.; field research: A.B. and V.F.; writing – original draft preparation: V.F., A.B., and I.N.; writing – review and editing: A.B.
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Conflict of interest: The authors state no conflict of interest.
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- Nexus between renewable energy, technological innovation, and carbon dioxide emissions in Saudi Arabia
- Analysis of the spillover effects of green organic transformation on sustainable development in ethnic regions’ agriculture and animal husbandry
- Factors impacting spatial distribution of black and odorous water bodies in Hebei
- Large-scale shaking table tests on the liquefaction and deformation responses of an ultra-deep overburden
- Impacts of climate change and sea-level rise on the coastal geological environment of Quang Nam province, Vietnam
- Reservoir characterization and exploration potential of shale reservoir near denudation area: A case study of Ordovician–Silurian marine shale, China
- Seismic prediction of Permian volcanic rock reservoirs in Southwest Sichuan Basin
- Application of CBERS-04 IRS data to land surface temperature inversion: A case study based on Minqin arid area
- Geological characteristics and prospecting direction of Sanjiaoding gold mine in Saishiteng area
- Research on the deformation prediction model of surrounding rock based on SSA-VMD-GRU
- Geochronology, geochemical characteristics, and tectonic significance of the granites, Menghewula, Southern Great Xing’an range
- Hazard classification of active faults in Yunnan base on probabilistic seismic hazard assessment
- Characteristics analysis of hydrate reservoirs with different geological structures developed by vertical well depressurization
- Estimating the travel distance of channelized rock avalanches using genetic programming method
- Landscape preferences of hikers in Three Parallel Rivers Region and its adjacent regions by content analysis of user-generated photography
- New age constraints of the LGM onset in the Bohemian Forest – Central Europe
- Characteristics of geological evolution based on the multifractal singularity theory: A case study of Heyu granite and Mesozoic tectonics
- Soil water content and longitudinal microbiota distribution in disturbed areas of tower foundations of power transmission and transformation projects
- Oil accumulation process of the Kongdian reservoir in the deep subsag zone of the Cangdong Sag, Bohai Bay Basin, China
- Investigation of velocity profile in rock–ice avalanche by particle image velocimetry measurement
- Optimizing 3D seismic survey geometries using ray tracing and illumination modeling: A case study from Penobscot field
- Sedimentology of the Phra That and Pha Daeng Formations: A preliminary evaluation of geological CO2 storage potential in the Lampang Basin, Thailand
- Improved classification algorithm for hyperspectral remote sensing images based on the hybrid spectral network model
- Map analysis of soil erodibility rates and gully erosion sites in Anambra State, South Eastern Nigeria
- Identification and driving mechanism of land use conflict in China’s South-North transition zone: A case study of Huaihe River Basin
- Evaluation of the impact of land-use change on earthquake risk distribution in different periods: An empirical analysis from Sichuan Province
- A test site case study on the long-term behavior of geotextile tubes
- An experimental investigation into carbon dioxide flooding and rock dissolution in low-permeability reservoirs of the South China Sea
- Detection and semi-quantitative analysis of naphthenic acids in coal and gangue from mining areas in China
- Comparative effects of olivine and sand on KOH-treated clayey soil
- YOLO-MC: An algorithm for early forest fire recognition based on drone image
- Earthquake building damage classification based on full suite of Sentinel-1 features
- Potential landslide detection and influencing factors analysis in the upper Yellow River based on SBAS-InSAR technology
- Assessing green area changes in Najran City, Saudi Arabia (2013–2022) using hybrid deep learning techniques
- An advanced approach integrating methods to estimate hydraulic conductivity of different soil types supported by a machine learning model
- Hybrid methods for land use and land cover classification using remote sensing and combined spectral feature extraction: A case study of Najran City, KSA
- Streamlining digital elevation model construction from historical aerial photographs: The impact of reference elevation data on spatial accuracy
- Analysis of urban expansion patterns in the Yangtze River Delta based on the fusion impervious surfaces dataset
- A metaverse-based visual analysis approach for 3D reservoir models
- Late Quaternary record of 100 ka depositional cycles on the Larache shelf (NW Morocco)
- Integrated well-seismic analysis of sedimentary facies distribution: A case study from the Mesoproterozoic, Ordos Basin, China
- Study on the spatial equilibrium of cultural and tourism resources in Macao, China
- Urban road surface condition detecting and integrating based on the mobile sensing framework with multi-modal sensors
- Application of improved sine cosine algorithm with chaotic mapping and novel updating methods for joint inversion of resistivity and surface wave data
- The synergistic use of AHP and GIS to assess factors driving forest fire potential in a peat swamp forest in Thailand
- Dynamic response analysis and comprehensive evaluation of cement-improved aeolian sand roadbed
- Review Articles
- Humic substances influence on the distribution of dissolved iron in seawater: A review of electrochemical methods and other techniques
- Applications of physics-informed neural networks in geosciences: From basic seismology to comprehensive environmental studies
- Ore-controlling structures of granite-related uranium deposits in South China: A review
- Shallow geological structure features in Balikpapan Bay East Kalimantan Province – Indonesia
- A review on the tectonic affinity of microcontinents and evolution of the Proto-Tethys Ocean in Northeastern Tibet
- Special Issue: Natural Resources and Environmental Risks: Towards a Sustainable Future - Part II
- Depopulation in the Visok micro-region: Toward demographic and economic revitalization
- Special Issue: Geospatial and Environmental Dynamics - Part II
- Advancing urban sustainability: Applying GIS technologies to assess SDG indicators – a case study of Podgorica (Montenegro)
- Spatiotemporal and trend analysis of common cancers in men in Central Serbia (1999–2021)
- Minerals for the green agenda, implications, stalemates, and alternatives
- Spatiotemporal water quality analysis of Vrana Lake, Croatia
- Functional transformation of settlements in coal exploitation zones: A case study of the municipality of Stanari in Republic of Srpska (Bosnia and Herzegovina)
- Hypertension in AP Vojvodina (Northern Serbia): A spatio-temporal analysis of patients at the Institute for Cardiovascular Diseases of Vojvodina
- Regional patterns in cause-specific mortality in Montenegro, 1991–2019
- Spatio-temporal analysis of flood events using GIS and remote sensing-based approach in the Ukrina River Basin, Bosnia and Herzegovina
- Flash flood susceptibility mapping using LiDAR-Derived DEM and machine learning algorithms: Ljuboviđa case study, Serbia
- Geocultural heritage as a basis for geotourism development: Banjska Monastery, Zvečan (Serbia)
- Assessment of groundwater potential zones using GIS and AHP techniques – A case study of the zone of influence of Kolubara Mining Basin
- Impact of the agri-geographical transformation of rural settlements on the geospatial dynamics of soil erosion intensity in municipalities of Central Serbia
- Where faith meets geomorphology: The cultural and religious significance of geodiversity explored through geospatial technologies
- Applications of local climate zone classification in European cities: A review of in situ and mobile monitoring methods in urban climate studies
- Complex multivariate water quality impact assessment on Krivaja River
- Ionization hotspots near waterfalls in Eastern Serbia’s Stara Planina Mountain
- Shift in landscape use strategies during the transition from the Bronze age to Iron age in Northwest Serbia
Artikel in diesem Heft
- Research Articles
- Seismic response and damage model analysis of rocky slopes with weak interlayers
- Multi-scenario simulation and eco-environmental effect analysis of “Production–Living–Ecological space” based on PLUS model: A case study of Anyang City
- Remote sensing estimation of chlorophyll content in rape leaves in Weibei dryland region of China
- GIS-based frequency ratio and Shannon entropy modeling for landslide susceptibility mapping: A case study in Kundah Taluk, Nilgiris District, India
- Natural gas origin and accumulation of the Changxing–Feixianguan Formation in the Puguang area, China
- Spatial variations of shear-wave velocity anomaly derived from Love wave ambient noise seismic tomography along Lembang Fault (West Java, Indonesia)
- Evaluation of cumulative rainfall and rainfall event–duration threshold based on triggering and non-triggering rainfalls: Northern Thailand case
- Pixel and region-oriented classification of Sentinel-2 imagery to assess LULC dynamics and their climate impact in Nowshera, Pakistan
- The use of radar-optical remote sensing data and geographic information system–analytical hierarchy process–multicriteria decision analysis techniques for revealing groundwater recharge prospective zones in arid-semi arid lands
- Effect of pore throats on the reservoir quality of tight sandstone: A case study of the Yanchang Formation in the Zhidan area, Ordos Basin
- Hydroelectric simulation of the phreatic water response of mining cracked soil based on microbial solidification
- Spatial-temporal evolution of habitat quality in tropical monsoon climate region based on “pattern–process–quality” – a case study of Cambodia
- Early Permian to Middle Triassic Formation petroleum potentials of Sydney Basin, Australia: A geochemical analysis
- Micro-mechanism analysis of Zhongchuan loess liquefaction disaster induced by Jishishan M6.2 earthquake in 2023
- Prediction method of S-wave velocities in tight sandstone reservoirs – a case study of CO2 geological storage area in Ordos Basin
- Ecological restoration in valley area of semiarid region damaged by shallow buried coal seam mining
- Hydrocarbon-generating characteristics of Xujiahe coal-bearing source rocks in the continuous sedimentary environment of the Southwest Sichuan
- Hazard analysis of future surface displacements on active faults based on the recurrence interval of strong earthquakes
- Structural characterization of the Zalm district, West Saudi Arabia, using aeromagnetic data: An approach for gold mineral exploration
- Research on the variation in the Shields curve of silt initiation
- Reuse of agricultural drainage water and wastewater for crop irrigation in southeastern Algeria
- Assessing the effectiveness of utilizing low-cost inertial measurement unit sensors for producing as-built plans
- Analysis of the formation process of a natural fertilizer in the loess area
- Machine learning methods for landslide mapping studies: A comparative study of SVM and RF algorithms in the Oued Aoulai watershed (Morocco)
- Chemical dissolution and the source of salt efflorescence in weathering of sandstone cultural relics
- Molecular simulation of methane adsorption capacity in transitional shale – a case study of Longtan Formation shale in Southern Sichuan Basin, SW China
- Evolution characteristics of extreme maximum temperature events in Central China and adaptation strategies under different future warming scenarios
- Estimating Bowen ratio in local environment based on satellite imagery
- 3D fusion modeling of multi-scale geological structures based on subdivision-NURBS surfaces and stratigraphic sequence formalization
- Comparative analysis of machine learning algorithms in Google Earth Engine for urban land use dynamics in rapidly urbanizing South Asian cities
- Study on the mechanism of plant root influence on soil properties in expansive soil areas
- Simulation of seismic hazard parameters and earthquakes source mechanisms along the Red Sea rift, western Saudi Arabia
- Tectonics vs sedimentation in foredeep basins: A tale from the Oligo-Miocene Monte Falterona Formation (Northern Apennines, Italy)
- Investigation of landslide areas in Tokat-Almus road between Bakımlı-Almus by the PS-InSAR method (Türkiye)
- Predicting coastal variations in non-storm conditions with machine learning
- Cross-dimensional adaptivity research on a 3D earth observation data cube model
- Geochronology and geochemistry of late Paleozoic volcanic rocks in eastern Inner Mongolia and their geological significance
- Spatial and temporal evolution of land use and habitat quality in arid regions – a case of Northwest China
- Ground-penetrating radar imaging of subsurface karst features controlling water leakage across Wadi Namar dam, south Riyadh, Saudi Arabia
- Rayleigh wave dispersion inversion via modified sine cosine algorithm: Application to Hangzhou, China passive surface wave data
- Fractal insights into permeability control by pore structure in tight sandstone reservoirs, Heshui area, Ordos Basin
- Debris flow hazard characteristic and mitigation in Yusitong Gully, Hengduan Mountainous Region
- Research on community characteristics of vegetation restoration in hilly power engineering based on multi temporal remote sensing technology
- Identification of radial drainage networks based on topographic and geometric features
- Trace elements and melt inclusion in zircon within the Qunji porphyry Cu deposit: Application to the metallogenic potential of the reduced magma-hydrothermal system
- Pore, fracture characteristics and diagenetic evolution of medium-maturity marine shales from the Silurian Longmaxi Formation, NE Sichuan Basin, China
- Study of the earthquakes source parameters, site response, and path attenuation using P and S-waves spectral inversion, Aswan region, south Egypt
- Source of contamination and assessment of potential health risks of potentially toxic metal(loid)s in agricultural soil from Al Lith, Saudi Arabia
- Regional spatiotemporal evolution and influencing factors of rural construction areas in the Nanxi River Basin via GIS
- An efficient network for object detection in scale-imbalanced remote sensing images
- Effect of microscopic pore–throat structure heterogeneity on waterflooding seepage characteristics of tight sandstone reservoirs
- Environmental health risk assessment of Zn, Cd, Pb, Fe, and Co in coastal sediments of the southeastern Gulf of Aqaba
- A modified Hoek–Brown model considering softening effects and its applications
- Evaluation of engineering properties of soil for sustainable urban development
- The spatio-temporal characteristics and influencing factors of sustainable development in China’s provincial areas
- Application of a mixed additive and multiplicative random error model to generate DTM products from LiDAR data
- Gold vein mineralogy and oxygen isotopes of Wadi Abu Khusheiba, Jordan
- Prediction of surface deformation time series in closed mines based on LSTM and optimization algorithms
- 2D–3D Geological features collaborative identification of surrounding rock structural planes in hydraulic adit based on OC-AINet
- Spatiotemporal patterns and drivers of Chl-a in Chinese lakes between 1986 and 2023
- Land use classification through fusion of remote sensing images and multi-source data
- Nexus between renewable energy, technological innovation, and carbon dioxide emissions in Saudi Arabia
- Analysis of the spillover effects of green organic transformation on sustainable development in ethnic regions’ agriculture and animal husbandry
- Factors impacting spatial distribution of black and odorous water bodies in Hebei
- Large-scale shaking table tests on the liquefaction and deformation responses of an ultra-deep overburden
- Impacts of climate change and sea-level rise on the coastal geological environment of Quang Nam province, Vietnam
- Reservoir characterization and exploration potential of shale reservoir near denudation area: A case study of Ordovician–Silurian marine shale, China
- Seismic prediction of Permian volcanic rock reservoirs in Southwest Sichuan Basin
- Application of CBERS-04 IRS data to land surface temperature inversion: A case study based on Minqin arid area
- Geological characteristics and prospecting direction of Sanjiaoding gold mine in Saishiteng area
- Research on the deformation prediction model of surrounding rock based on SSA-VMD-GRU
- Geochronology, geochemical characteristics, and tectonic significance of the granites, Menghewula, Southern Great Xing’an range
- Hazard classification of active faults in Yunnan base on probabilistic seismic hazard assessment
- Characteristics analysis of hydrate reservoirs with different geological structures developed by vertical well depressurization
- Estimating the travel distance of channelized rock avalanches using genetic programming method
- Landscape preferences of hikers in Three Parallel Rivers Region and its adjacent regions by content analysis of user-generated photography
- New age constraints of the LGM onset in the Bohemian Forest – Central Europe
- Characteristics of geological evolution based on the multifractal singularity theory: A case study of Heyu granite and Mesozoic tectonics
- Soil water content and longitudinal microbiota distribution in disturbed areas of tower foundations of power transmission and transformation projects
- Oil accumulation process of the Kongdian reservoir in the deep subsag zone of the Cangdong Sag, Bohai Bay Basin, China
- Investigation of velocity profile in rock–ice avalanche by particle image velocimetry measurement
- Optimizing 3D seismic survey geometries using ray tracing and illumination modeling: A case study from Penobscot field
- Sedimentology of the Phra That and Pha Daeng Formations: A preliminary evaluation of geological CO2 storage potential in the Lampang Basin, Thailand
- Improved classification algorithm for hyperspectral remote sensing images based on the hybrid spectral network model
- Map analysis of soil erodibility rates and gully erosion sites in Anambra State, South Eastern Nigeria
- Identification and driving mechanism of land use conflict in China’s South-North transition zone: A case study of Huaihe River Basin
- Evaluation of the impact of land-use change on earthquake risk distribution in different periods: An empirical analysis from Sichuan Province
- A test site case study on the long-term behavior of geotextile tubes
- An experimental investigation into carbon dioxide flooding and rock dissolution in low-permeability reservoirs of the South China Sea
- Detection and semi-quantitative analysis of naphthenic acids in coal and gangue from mining areas in China
- Comparative effects of olivine and sand on KOH-treated clayey soil
- YOLO-MC: An algorithm for early forest fire recognition based on drone image
- Earthquake building damage classification based on full suite of Sentinel-1 features
- Potential landslide detection and influencing factors analysis in the upper Yellow River based on SBAS-InSAR technology
- Assessing green area changes in Najran City, Saudi Arabia (2013–2022) using hybrid deep learning techniques
- An advanced approach integrating methods to estimate hydraulic conductivity of different soil types supported by a machine learning model
- Hybrid methods for land use and land cover classification using remote sensing and combined spectral feature extraction: A case study of Najran City, KSA
- Streamlining digital elevation model construction from historical aerial photographs: The impact of reference elevation data on spatial accuracy
- Analysis of urban expansion patterns in the Yangtze River Delta based on the fusion impervious surfaces dataset
- A metaverse-based visual analysis approach for 3D reservoir models
- Late Quaternary record of 100 ka depositional cycles on the Larache shelf (NW Morocco)
- Integrated well-seismic analysis of sedimentary facies distribution: A case study from the Mesoproterozoic, Ordos Basin, China
- Study on the spatial equilibrium of cultural and tourism resources in Macao, China
- Urban road surface condition detecting and integrating based on the mobile sensing framework with multi-modal sensors
- Application of improved sine cosine algorithm with chaotic mapping and novel updating methods for joint inversion of resistivity and surface wave data
- The synergistic use of AHP and GIS to assess factors driving forest fire potential in a peat swamp forest in Thailand
- Dynamic response analysis and comprehensive evaluation of cement-improved aeolian sand roadbed
- Review Articles
- Humic substances influence on the distribution of dissolved iron in seawater: A review of electrochemical methods and other techniques
- Applications of physics-informed neural networks in geosciences: From basic seismology to comprehensive environmental studies
- Ore-controlling structures of granite-related uranium deposits in South China: A review
- Shallow geological structure features in Balikpapan Bay East Kalimantan Province – Indonesia
- A review on the tectonic affinity of microcontinents and evolution of the Proto-Tethys Ocean in Northeastern Tibet
- Special Issue: Natural Resources and Environmental Risks: Towards a Sustainable Future - Part II
- Depopulation in the Visok micro-region: Toward demographic and economic revitalization
- Special Issue: Geospatial and Environmental Dynamics - Part II
- Advancing urban sustainability: Applying GIS technologies to assess SDG indicators – a case study of Podgorica (Montenegro)
- Spatiotemporal and trend analysis of common cancers in men in Central Serbia (1999–2021)
- Minerals for the green agenda, implications, stalemates, and alternatives
- Spatiotemporal water quality analysis of Vrana Lake, Croatia
- Functional transformation of settlements in coal exploitation zones: A case study of the municipality of Stanari in Republic of Srpska (Bosnia and Herzegovina)
- Hypertension in AP Vojvodina (Northern Serbia): A spatio-temporal analysis of patients at the Institute for Cardiovascular Diseases of Vojvodina
- Regional patterns in cause-specific mortality in Montenegro, 1991–2019
- Spatio-temporal analysis of flood events using GIS and remote sensing-based approach in the Ukrina River Basin, Bosnia and Herzegovina
- Flash flood susceptibility mapping using LiDAR-Derived DEM and machine learning algorithms: Ljuboviđa case study, Serbia
- Geocultural heritage as a basis for geotourism development: Banjska Monastery, Zvečan (Serbia)
- Assessment of groundwater potential zones using GIS and AHP techniques – A case study of the zone of influence of Kolubara Mining Basin
- Impact of the agri-geographical transformation of rural settlements on the geospatial dynamics of soil erosion intensity in municipalities of Central Serbia
- Where faith meets geomorphology: The cultural and religious significance of geodiversity explored through geospatial technologies
- Applications of local climate zone classification in European cities: A review of in situ and mobile monitoring methods in urban climate studies
- Complex multivariate water quality impact assessment on Krivaja River
- Ionization hotspots near waterfalls in Eastern Serbia’s Stara Planina Mountain
- Shift in landscape use strategies during the transition from the Bronze age to Iron age in Northwest Serbia