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Integrating Airborne Laser Scanning and 3D Ground-Penetrating Radar for the Investigation of Protohistoric Structures in Croatian Istria

: We present the investigation of two rather ephemeral archaeological sites located in the municipality of Oprtalj/Portole (Croatian Istria) by means of integrated archaeological, geophysical and remote sensing techniques. The results obtained conﬁrm the ﬁrst interpretation of these contexts; a protohistoric burial mound and a small hillfort, respectively. We further obtained detailed information about both deposits through 2D and 3D remote sensing and geophysical studies that produced maps, volumes, proﬁles and cross-sections. At the ﬁrst site, the volume reconstruction of both the inner stone core and the superimposed earth of the putative stone mound also allowed us to estimate the labour necessary to erect the structure. In conclusion, our study demonstrates that the integrated approach can be valuable not only to acquire novel data about the archaeological deposits but also to calibrate future investigations and to plan effective measures for heritage management, monitoring and valorization.


Introduction
Since archaeological excavations are costly and time-consuming, the combined analysis of high-resolution Airborne Laser Scanning (ALS) and Ground-Penetrating Radar (GPR) data is dramatically changing the investigation and documentation of archaeological features. The integration of cutting-edge, non-destructive photogrammetric and remote sensing techniques is providing crucial information about their geometry, topography and spatial relationship with other natural or anthropogenic features [1][2][3][4][5][6].
In the last decade, a key contribution to this achievement has been imaging technologies such as Airborne Laser Scanning (hereafter ALS) and Ground-Penetrating Radar (hereafter GPR), which enable the production of detailed 2D and 3D maps of the archaeological evidence and the surrounding topography of the landscape at centimetre resolution, and which are now fairly comparable with other destructive techniques such as excavations [7][8][9][10][11][12][13][14]. This information is of paramount importance for different objectives, such as identifying possible anthropogenic features, assessing the thickness of anthropogenic deposits and best calibrating future investigations (e.g., indicating the most promising location for excavations), allowing us to plan effective measures for heritage management, monitoring and valorization [15][16][17][18]. Previous research in the area was conducted with the aim of understanding the diachronic development of the archaeological landscape of a largely unexplored sector of the Istrian peninsula. This included the acquisition, processing and analysis of high-definition ALS data combined with the examination of aerial photographs, historical cadastral maps and repeated fieldwork surface surveys. The investigations, carried out over about 30 square km, allowed us to identify and describe several unreported prehistoric, protohistoric and Roman sites and to obtain detailed topographic information about the already known ones [23].
The selection of a probable burial mound (Figures 1 and 2, feature 8) and a small hillfort (Figures 1 and 2, feature 10), both likely erected in pre-Roman times, for further non-invasive investigations was motivated by several reasons, including the richness in archaeological finds at the surface, the limited size of detected structures, the absence of dense vegetation, some logistical evaluations, the suitability of these features for future excavations and ultimately the consistent evidence, in the Vižintini village surroundings, of a well-preserved landscape dated back to the protohistoric period (namely Bronze and Iron Ages, ca. 2200-150 BC; Figure 1). Previous research in the area was conducted with the aim of understanding the diachronic development of the archaeological landscape of a largely unexplored sector of the Istrian peninsula. This included the acquisition, processing and analysis of highdefinition ALS data combined with the examination of aerial photographs, historical cadastral maps and repeated fieldwork surface surveys. The investigations, carried out over about 30 square km, allowed us to identify and describe several unreported prehistoric, protohistoric and Roman sites and to obtain detailed topographic information about the already known ones [23].
The selection of a probable burial mound (Figures 1 and 2, feature 8) and a small hillfort (Figures 1 and 2, feature 10), both likely erected in pre-Roman times, for further non-invasive investigations was motivated by several reasons, including the richness in archaeological finds at the surface, the limited size of detected structures, the absence of dense vegetation, some logistical evaluations, the suitability of these features for future excavations and ultimately the consistent evidence, in the Vižintini village surroundings, of a well-preserved landscape dated back to the protohistoric period (namely Bronze and Iron Ages, ca. 2200-150 BC; Figure 1).
The analysis of GPR data collected at both sites and integrated with ALS allows us to describe in detail the morphology of the structures and associated earth deposits and provide additional information for the interpretation of both complexes and the assessment of further investigations. Appl. Sci. 2021, 11, x FOR PEER REVIEW 3 of 13 The analysis of GPR data collected at both sites and integrated with ALS allows us to describe in detail the morphology of the structures and associated earth deposits and provide additional information for the interpretation of both complexes and the assessment of further investigations.

Geographic, Geological and Archaeological Background
Features 8 and 10 (Figures 1 and 2) are located at the southern edge of the relatively flat karst plateau close to Oprtalj/Portole, at an average height of about 400 m a.s.l. (Figure  1, nn. 8 and 10). They are divided by a deep narrow valley of an ephemeral watercourse which drains into the Mirna/Quieto river. This latter perennial river and its wide valley flanks the southern side of the investigated area and represents an important waterway which has connected coastal Istria with the inlands since prehistoric times [25].
The plateau is made of Cretaceous limestone, dolomite and breccia and overlooks southward a hilly sector made of marls and sandstones (Eocene Flysch deposits; [24,26,27]) divided by the Mirna valley ( Figure 2).
The overall area is rich in archaeological features consisting of prehistoric, protohistoric and Roman sites ( [23] and references therein). Close to the two investigated structures, the main evidence in the area is represented by the Laganiši cave, occupied for a long period spanning from Neolithic to the Roman times (around 5000 BC-4th century AD), which was investigated in recent years ( [28]; Figure 1, Laganiši).
On the contrary, the two features here analysed were unknown before the recent publication of the results of the ALS survey [23], as well as two other protohistoric fortified structures located in their surroundings. Feature 9 is an irregular fortification (about 130 × 60 m in size) located immediately west of site 10 and at the edge of the scarp of a deep narrow valley placed between them ( Figure 1, feature 9). Feature 7 is an elliptical structure, about 80 m large and showing an additional south-western wall, located north of a limestone quarry between Vižintini and Šorgi villages ( Figure 1, feature 7).
Hundreds of similar fortified settlements, located on hilltops and protected by imposing dry-stone ramparts, mark the landscape of the north-eastern Adriatic region be-

Geographic, Geological and Archaeological Background
Features 8 and 10 (Figures 1 and 2) are located at the southern edge of the relatively flat karst plateau close to Oprtalj/Portole, at an average height of about 400 m a.s.l. (Figure 1, nn. 8 and 10). They are divided by a deep narrow valley of an ephemeral watercourse which drains into the Mirna/Quieto river. This latter perennial river and its wide valley flanks the southern side of the investigated area and represents an important waterway which has connected coastal Istria with the inlands since prehistoric times [25].
The plateau is made of Cretaceous limestone, dolomite and breccia and overlooks southward a hilly sector made of marls and sandstones (Eocene Flysch deposits; [24,26,27]) divided by the Mirna valley ( Figure 2).
The overall area is rich in archaeological features consisting of prehistoric, protohistoric and Roman sites ( [23] and references therein). Close to the two investigated structures, the main evidence in the area is represented by the Laganiši cave, occupied for a long period spanning from Neolithic to the Roman times (around 5000 BC-4th century AD), which was investigated in recent years ( [28]; Figure 1, Laganiši).
On the contrary, the two features here analysed were unknown before the recent publication of the results of the ALS survey [23], as well as two other protohistoric fortified structures located in their surroundings. Feature 9 is an irregular fortification (about 130 × 60 m in size) located immediately west of site 10 and at the edge of the scarp of a deep narrow valley placed between them ( Figure 1, feature 9). Feature 7 is an elliptical structure, about 80 m large and showing an additional south-western wall, located north of a limestone quarry between Vižintini and Šorgi villages ( Figure 1, feature 7).
Hundreds of similar fortified settlements, located on hilltops and protected by imposing dry-stone ramparts, mark the landscape of the north-eastern Adriatic region between the Trieste Karst plateau, the Istria peninsula and the Dalmatian islands. These villages were settled for many centuries, in some cases up to the arrival of the Romans in the area in the early 2nd century BC, and shared homogenous traits in pottery assemblages and funerary practices [29]. Among these are burial mounds widely documented in the whole region with negligible differences and generally attributed to Early and Middle Bronze Age (ca. 2200-1350 BC). Other, larger protohistoric hillforts known in the area by previous research carried out in the late nineteenth and early twentieth century are located close to the investigated sites, at Kukuj, Oprtalj, Sv. Jelena,Čebranjak, Beninići, Sv. Stjepan and perhaps Gradinje and Vižintin ( [30]; Figure 1).

Airborne Laser Scanning
High-resolution ALS data, featuring at least 20 points per square meter, were acquired by Vectra company in winter 2018 using a Eurocopter EC 120B, flying at a mean altitude of 500 m with a speed of 55 kts and equipped with a GPS receiver Novatel OEV/OEM4, a LiDAR instrument Riegl LMS-Q780 (pulse repetition rate of 400 kHz) and a photo camera Hasselblad. Processing and analyses of collected data were carried out by the team of the Multidisciplinary Laboratory of the "Abdus Salam" International Centre for Theoretical Physics (ICTP, UNESCO) using the free open-source software SAGA GIS, QGIS and Relief Visualization Toolbox to produce Digital Terrain Models (DTMs) and different visualizations. Among these are the Slope and the Simple Local Relief Model that are presented in this contribution (see also [23] for details about the processing of data).

3D Ground Penetrating Radar
The implementation of efficient and portable multi-antenna (or multi-array) GPR instruments, accurate synchronized positioning systems (RTK GPS and topographic total stations) and the demand for 3D subsurface imaging are pushing towards a rapidly growing application of 3D GPR to near-surface studies (see e.g., [31][32][33][34]).
The 3D GPR dataset were acquired on feature 8 and feature 10 using the MiniMIRA array GPR (Malå Geoscience, Sweden) equipped with 5 transmitting and 4 receiving 400 MHz shielded antennas, allowing the collection of 8 parallel profiles with a constant distance equal to 8 cm, thus forming a swath of 56 cm wide. To optimize the spatial resolution, we set a trace spacing also equal to 8 cm, obtaining a constant in-line and cross-line coverage.
The system was connected with an electromechanical odometer for triggering and with RTK GPS for absolute positioning with centimetric accuracy. This allowed us to perform the topographic correction to the GPR volumes, and properly reconstruct the real geometry, depth and slope of the buried surface, in particular in the case of feature 8, which exhibited a more complex topography.
We applied a standard processing sequence (zero drift removal, background removal, bandpass filtering, amplitude recovery function encompassing spherical divergence and other attenuation effects) on each swath, to enhance the Signal to Noise Ratio. GPR datasets were processed using rSlicers software (DECO Geophysical, Moscow, Russia) as well as an in-house module implemented in Matlab. Swaths were then interpolated within rectangular grids which were hand selected by the operator. This process allowed us to apply FK time migration of the dataset by means of the Stolt algorithm [35] after velocity estimation through hyperbola matching.
Comparison of standard 2D data with the results obtained with this system at controlled test sites showed that complex near-surface conditions can be hardly, if at all, imaged by the 2D techniques due to the large amount of cross-line information (i.e., out-of-plane reflections and diffractions) recorded into the 2D profile, and are impossible to be resolved by the imaging process if only in-line information is available. This was the case of the study areas, which are characterized by shallow chaotic conditions and geometrically irregular 3D targets.

ALS-GPR Integration
The combined analysis of ALS and GPR data was first carried out through the visual inspection of profiles derived from digital elevation surfaces through the module profile tool available in QGIS 3.
As regards feature 8, 3D points of the stone core surface of the putative burial were extracted from GPR slices and interpolated through the module r.surf.rast available in of the study areas, which are characterized by shallow chaotic conditions and geometrically irregular 3D targets.

ALS-GPR Integration
The combined analysis of ALS and GPR data was first carried out through the visual inspection of profiles derived from digital elevation surfaces through the module profile tool available in QGIS 3.
As regards feature 8, 3D points of the stone core surface of the putative burial were extracted from GPR slices and interpolated through the module r.surf.rast available in Grass 7 in order to produce a digital surface at 20 cm resolution (DTM). This allowed the combined 3D visualization of both the topographic and the buried surfaces of the stone cap (feature 8) by importing the produced DTMs into CloudCompare.
Afterwards, the area (in square meters) and the volume (in cubic meters) of both the stone structures and the above earthen deposits were calculated through the module Raster Surface Volume available in SAGA GIS.

Feature 8
According to the ASL-derived data, feature 8 is a circular ridge of 60-70 cm in height and about 12 m in diameter, located north-east of Laganiši village and some hundred meters from the above-cited cave with the same name ( Figure 1, feature 8). The circular structure is almost outcropping, covered by thin soil and some vegetation and by a modern field division dry wall which crosses the structure along the N-W S-E direction. It testifies for the ancient origin of its construction ( Figure 3A,B). As is clearly visible in the ALSderived images and profiles, the eastern margin of the mound is sharp while the western side decreases gradually, with a maximum elevation of about 50 cm above the ground level. A circular hole is visible on the western side of the modern wall ( Figure 4).   Due to the presence of the modern wall in the middle, GPR investigations were carried out over two separated sectors, located, respectively, on the western and on the eastern sides of the modern structure.
On the southern sector of the mound, two anomalies of irregular shape separated by the modern wall, are visible from about 20-30 cm to about 110-120 cm from the ground level. The intensity of reflected signals is compatible with a stone core of about 9 m in diameter with an embossed top ( Figure 5, anomalies 1-2; Figure 6A,B).   Due to the presence of the modern wall in the middle, GPR investigations were carried out over two separated sectors, located, respectively, on the western and on the eastern sides of the modern structure.
On the southern sector of the mound, two anomalies of irregular shape separated by the modern wall, are visible from about 20-30 cm to about 110-120 cm from the ground level. The intensity of reflected signals is compatible with a stone core of about 9 m in diameter with an embossed top ( Figure 5, anomalies 1-2; Figure 6A,B).   A third circular anomaly is visible on the western sector of the mound from about 30-50 cm from the ground level ( Figure 5, anomaly 3). The circular margin of the structure is not well visible and can be recognized only on the south-eastern sector of the mound between 25-40 cm from the ground level ( Figure 5, anomaly 4), where it appears to be marked by stones and boulders possibly arranged in a row.
DTMs of both the topographic surface (from ALS data) and of the stone cap (from GPR scans) allowed us to produce a 3D visualization of both surfaces ( Figure 6C). From those we calculated the overall volume of the mound and the volume of the capstone where the tomb was presumably inserted. The estimated volume of the stone cap corresponds to about 39 m 3 , while the overall mound volume is roughly 56 m 3 . This means that the volume of the earth deposits covering the stone cap accounts for approximately 17 m 3 .

Feature 10
Feature 10 presents an irregular rhombic shape, about 50 × 50 m large, which encloses an area of less than 2000 square meters ( Figure 3C,D). Small fragments of protohistoric pottery are quite abundant within the fortified area and point to a chronology between Middle and Late Bronze Age [23].
The main structures are easily detectable through the analysis of ALS data. A winding entrance is present at its southern side while the northern part of the fortification is covered by an east-west-oriented modern wall (Figures 3D and 7). Other features visible A third circular anomaly is visible on the western sector of the mound from about 30-50 cm from the ground level ( Figure 5, anomaly 3). The circular margin of the structure is not well visible and can be recognized only on the south-eastern sector of the mound between 25-40 cm from the ground level ( Figure 5, anomaly 4), where it appears to be marked by stones and boulders possibly arranged in a row.
DTMs of both the topographic surface (from ALS data) and of the stone cap (from GPR scans) allowed us to produce a 3D visualization of both surfaces ( Figure 6C). From those we calculated the overall volume of the mound and the volume of the capstone where the tomb was presumably inserted. The estimated volume of the stone cap corresponds to about 39 m 3 , while the overall mound volume is roughly 56 m 3 . This means that the volume of the earth deposits covering the stone cap accounts for approximately 17 m 3 .

Feature 10
Feature 10 presents an irregular rhombic shape, about 50 × 50 m large, which encloses an area of less than 2000 square meters ( Figure 3C,D). Small fragments of protohistoric pottery are quite abundant within the fortified area and point to a chronology between Middle and Late Bronze Age [23].
The main structures are easily detectable through the analysis of ALS data. A winding entrance is present at its southern side while the northern part of the fortification is covered by an east-west-oriented modern wall (Figures 3D and 7). Other features visible in the Simple Local Relief Model visualization consist of a linear structure aligned on a north-south direction located south-east of the fortification (Figure 7, n. 5) and some linear features aligned on the east-west direction, which are related to sub-outcropping limestone, as confirmed by the analysis of GPR data (Figure 7, OC; see infra). ALS-derived profiles through the structures indicate the perimeter wall rubbles measure around 3-6 m in thickness (Figure 7, nn. 1-4).
Appl. Sci. 2021, 11, x FOR PEER REVIEW 8 of 13 in the Simple Local Relief Model visualization consist of a linear structure aligned on a north-south direction located south-east of the fortification (Figure 7, n. 5) and some linear features aligned on the east-west direction, which are related to sub-outcropping limestone, as confirmed by the analysis of GPR data (Figure 7, OC; see infra). ALS-derived profiles through the structures indicate the perimeter wall rubbles measure around 3-6 m in thickness (Figure 7, nn. 1-4). The results obtained from the GPR survey on feature 10 allow us to better define the perimeter of the enclosure and to identify several additional structures. The perimeter wall structure is clearly visible from about 20 to about 50 cm, progressively disappearing up to about 70 cm from the ground level (Figure 8, anomaly F). The gateway located on the southern side of the rampart is easily visible at about 30 cm depth (Figure 8, anomaly 1). The results obtained from the GPR survey on feature 10 allow us to better define the perimeter of the enclosure and to identify several additional structures. The perimeter wall structure is clearly visible from about 20 to about 50 cm, progressively disappearing up to about 70 cm from the ground level (Figure 8, anomaly F). The gateway located on the southern side of the rampart is easily visible at about 30 cm depth (Figure 8, anomaly 1).
Possible additional circular structures, compatible with the presence of small towers or lookouts and possibly associated with other gaps in the fortification wall, are visible on both the western and eastern sides (Figure 8, anomalies 2-3). The north-south-oriented linear wall structure can be recognized from about 30 to 70 cm from the ground level ( Figure 8, anomaly 4) while several limestone layers, mostly east-west oriented, are found both inside and outside the perimeter of the hillfort (Figure 8, anomaly OC) from around 30 to 100 cm depth, demonstrating that the structure was built over sub-outcropping limestone and that the landscape remains almost identical from that time. Appl. Sci. 2021, 11, x FOR PEER REVIEW 9 of 13  (Figure 8, anomaly OC) from around 30 to 100 cm depth, demonstrating that the structure was built over sub-outcropping limestone and that the landscape remains almost identical from that time.

Discussion and Conclusions
Our study has revealed the potential of coupling high-resolution ALS and GPR data for the identification and description of rather ephemeral archaeological structures (namely feature 8 and 10) with unprecedented accuracy.
The results obtained confirm the first attribution given to these contexts; to a protohistoric burial mound and a small fortified settlement, respectively [23]. The building technique used by the community who settled in the area back in the Bronze Age probably involved mixing together dry-stone walls made of limestone extracted from the substratum and earth deposits. Feature 8 consists of an inner stone cap covered by earthen deposits which originate with a circular bump of about 12 m in diameter and 80-90 cm in height. Shape and dimension are comparable with similar tumuli-like protohistoric structures, generally dated to the Early Bronze Age, which have been found elsewhere in the north-eastern Adriatic region, particularly in Istria and Friuli [36]. To our knowledge, the best comparisons for building technique and size come from the tumulus n. 6 of Mušego and the burial mound of Barbariga [37,38]. Both structures, of about 11 and 15 m in diameter, respectively, and less than 1 m in height, present a stone core in which the rectangular

Discussion and Conclusions
Our study has revealed the potential of coupling high-resolution ALS and GPR data for the identification and description of rather ephemeral archaeological structures (namely feature 8 and 10) with unprecedented accuracy.
The results obtained confirm the first attribution given to these contexts; to a protohistoric burial mound and a small fortified settlement, respectively [23]. The building technique used by the community who settled in the area back in the Bronze Age probably involved mixing together dry-stone walls made of limestone extracted from the substratum and earth deposits. Feature 8 consists of an inner stone cap covered by earthen deposits which originate with a circular bump of about 12 m in diameter and 80-90 cm in height. Shape and dimension are comparable with similar tumuli-like protohistoric structures, generally dated to the Early Bronze Age, which have been found elsewhere in the northeastern Adriatic region, particularly in Istria and Friuli [36]. To our knowledge, the best comparisons for building technique and size come from the tumulus n. 6 of Mušego and the burial mound of Barbariga [37,38]. Both structures, of about 11 and 15 m in diameter, respectively, and less than 1 m in height, present a stone core in which the rectangular stone slab tomb is inserted, surmounted by an earthen and stone mound. As suggested for feature 8, the perimeter of the stone cairn is marked by a single row dry-stone line.
Feature 10 is a small hillfort with a roughly rhomboid shape whose ramparts are embedded into a thin soil layer. The overall depth of the archaeological stratigraphy consisting of buried structures and associated earth deposits is about 50 cm. On the southern side, the fortification presents an entrance featured by a narrow and winding passage easily visible on GPR data. Another possible gateway, sided by two associated structures (e.g., towers or lookouts), has been detected on the western side.
It is not possible to determine whether these structures were built at the beginning of occupation of the area or resulted from the later restorations of the fortification wall. However, this evidence recalls the complex entrance system documented at other larger protohistoric hillforts of the Istrian peninsula, such as Monkodonja [39,40], Určin ( [41] with refs.) and Brjuni [42,43]. This type of entrance might have been replicated on a smaller scale by the community which erected the Vižintini hillfort, probably with similar defensive purposes.
Considering their limited size and the strategic position on a slope overlooking the narrow valley, it is likely that both features 9 and 10, as well as site 7 (Figure 1, n. 8-9), functioned as small villages and outposts under the control of a major long-lasting fortified settlement hillfort, e.g., Kukuj, located northward.
As regards feature 8, the volumes of both the stone core and the whole mound give us a rough idea of the labour involved in the erection of the burial mound. Several ethnological and archaeological studies have proposed different working day coefficients for the construction of dry-stone walls and ditches. In our attempt, we used the working day coefficients proposed by Recchia and Cazzella [44] for the erection of the dry-stone fortification of the protohistoric hillfort of Coppa Nevigata (Apulia) and that proposed by Brown [45] for the excavation of ditches in the Tavoliere Neolithic villages. According to these studies and depending on the raw material used, a single man was capable of transporting and putting in place 1 to 1.25 cubic meters of earth and stone per day. In our case, due to little information about these protohistoric communities, no assumption can be made on the total number of people involved in the work. By using both coefficients (1 and 1.25) and establishing the labour of a group of people ranging from 4 to 20, it follows that the mound might have been erected in a relatively short span of time between a few days and around 1 week (Table 1). Without any alleged intention of historical reconstruction, this result can be of some interest to quantify the labour necessary to erect the burial mound while, on the other hand, to roughly estimate the time needed for the excavation of the whole archaeological deposit. In fact, since archaeological excavations are costly and time consuming, volumetric information regarding archaeological deposits combined with 2D and 3D reconstructions derived from both ALS and GPR slices are also crucial for assessing further investigations. These can be carried out through further non-destructive techniques (e.g., repeated surface surveys) or destructive ones (such as corings, small scale/open area excavations) and the best strategies need to be adjusted according to a careful evaluation of costs/benefits and expected results. This regards not only investigations for purely research purposes but also those involving heritage management, monitoring and valorization in which a number of aspects (not exclusively archaeological) and goals must live together and have to be taken into consideration.