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(PDF) Electrical Resistivity Tomography as a Tool to Reconstruct the Palaeoenvironment of Neolithic Sites. In Archaeological Prospection: Proceedings of the International Conference on Archaeological Prospection, Vienna, May 29th-June 2nd 2013,

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In Archaeological Prospection: Proceedings of the International Conference on Archaeological Prospection, Vienna, May 29th-June 2nd 2013, </h1><div class="ds-work-card--work-authors ds-work-card--detail"><a class="ds-work-card--author js-wsj-grid-card-author ds2-5-body-md ds2-5-body-link" data-author-id="224648" href="https://fieldmuseum.academia.edu/WilliamAParkinson"><img alt="Profile image of William A. Parkinson" class="ds-work-card--author-avatar" src="https://0.academia-photos.com/224648/50367/46365/s65_william_a..parkinson.jpeg" />William A. 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tomography as a tool to reconstruct the paleoenvironment of Neolithic sites (2013)</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="1043249" href="https://uga.academia.edu/AttilaGyucha">Attila Gyucha</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="1170782" href="https://ucy.academia.edu/ApostolosSarris">Apostolos Sarris</a></div><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Electrical resistivity tomography as a tool to reconstruct the paleoenvironment of Neolithic sites (2013)&quot;,&quot;attachmentId&quot;:33516456,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/6818670/Electrical_resistivity_tomography_as_a_tool_to_reconstruct_the_paleoenvironment_of_Neolithic_sites_2013_&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/6818670/Electrical_resistivity_tomography_as_a_tool_to_reconstruct_the_paleoenvironment_of_Neolithic_sites_2013_"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="1" data-entity-id="9686517" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/9686517/Electrical_Resistivity_Tomography_for_the_Modeling_of_Cultural_Deposits_and_Geomophological_Landscapes_at_Neolithic_Sites_a_Case_Study_from_Southeastern_Hungary_2014_">Electrical Resistivity Tomography for the Modeling of Cultural Deposits and Geomophological Landscapes at Neolithic Sites: a Case Study from Southeastern Hungary (2014)</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="1043249" href="https://uga.academia.edu/AttilaGyucha">Attila Gyucha</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="1170782" href="https://ucy.academia.edu/ApostolosSarris">Apostolos Sarris</a></div><p class="ds-related-work--abstract ds2-5-body-sm">A large-scale electrical resistivity tomography (ERT) survey was undertaken around the Neolithic tell of Szeghalom-Kovácshalom in southeast Hungary, covering an area of almost 6 ha. High-resolution ERT data were collected along 28 uniformly distributed transects of variable length using the roll-along technique. A recently presented two-dimensional fast non-linear resistivity inversion algorithm was used to invert the ERT data and recover the true subsurface resistivity distribution along the specific cross-sections. The algorithm calculates and stores in an efficient manner the part of the Jacobian matrix that is actually important within the inversion procedure, thus rendering it almost 4.8 times faster than the algorithm that calculates the complete Jacobian matrix, without losing quality. The algorithm was further modified to account for any non-standard electrode configuration. A recently established iterative algorithm for sparse least squares problems (LSMR) was incorporated for the first time into the algorithm to solve the inverse resistivity problem. The effectiveness and robustness of the LSMR solver was highlighted through the processing of all the ERT lines. The processing and evaluation of the ERT data made it possible to map the thickness of the anthropogenic layer below the surface of the tell, to outline the horizontal and vertical dimensions of the palaeochannel adjacent to the tell, and to determine the general stratigraphy of geological layers up to 10 m below the ground surface. The ERT results also were used to update an older topographic map of the site showing the course of the palaeochannel around the tell. A synthetic model verified and enhanced the conclusions based on the field data. This study illustrates the added value that a systematic ERT survey can provide in reconstructing the ancient fluvial geomorphology of a microregion as well as the depth and horizontal extent of deposits associated with human habitation at archaeological sites. Figure 6. Surface maps showing the topographic relief of the different stratigraphic layers around the Szeghalom-Kovácshalom tell. (a) Thickness of the topsoil and anthropogenic Layer. (b) Thickness of the palaeochannel. (c) Thickness of the silty clay and silty clay with sand layer. (d) Burial depth of the deepest clayey layer. This figure is available in colour online at wileyonlinelibrary.com/journal/arp Figure 7. Overlay of the outline of the palaeochannel on an old topographic map of the tell. The solid and dashed lines indicate respectively the definite and prospective boundaries of the palaeochannel as extracted by the ERT survey. This figure is available in colour online at wileyonlinelibrary.com/journal/arp</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Electrical Resistivity Tomography for the Modeling of Cultural Deposits and Geomophological Landscapes at Neolithic Sites: a Case Study from Southeastern Hungary (2014)&quot;,&quot;attachmentId&quot;:35879334,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/9686517/Electrical_Resistivity_Tomography_for_the_Modeling_of_Cultural_Deposits_and_Geomophological_Landscapes_at_Neolithic_Sites_a_Case_Study_from_Southeastern_Hungary_2014_&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/9686517/Electrical_Resistivity_Tomography_for_the_Modeling_of_Cultural_Deposits_and_Geomophological_Landscapes_at_Neolithic_Sites_a_Case_Study_from_Southeastern_Hungary_2014_"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="2" data-entity-id="33637096" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/33637096/AN_ATTEMPT_TO_INTEGRATION_OF_DIFFERENT_GEOPHYSICAL_METHODS_MAGNETIC_GPR_AND_ERT_A_CASE_STUDY_FROM_THE_LATE_ROMAN_SETTLEMENT_ON_THE_ISLAND_OF_RAB_IN_CROATIA">AN ATTEMPT TO INTEGRATION OF DIFFERENT GEOPHYSICAL METHODS (MAGNETIC, GPR AND ERT); A CASE STUDY FROM THE LATE ROMAN SETTLEMENT ON THE ISLAND OF RAB IN CROATIA</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="372788" href="https://iarh.academia.edu/AnaKonestra">Ana Konestra</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="610647" href="https://independent.academia.edu/gorankalipovacvrkljan">goranka lipovac vrkljan</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="1061267" href="https://uksw.academia.edu/FabianWelc">Fabian Welc</a></div><p class="ds-related-work--abstract ds2-5-body-sm">In 2016 within the RED Project Roman Economy in Dalmatia: production, distribution and demand in the light of pottery workshops, 5 selected areas around the Podšilo Bay were geophysically surveyed. During the fieldworks in the Lopar protected area, located in the northeastern part of the Island of Rab a gradiometer, ground-penetrating radar (GPR) and electrical resistivity tomography (ERT) were used. The main aim of the project was to document presence of the Roman architecture in two areas of the bay&#39;s hinterland as suggested earlier by finds of pottery and glass. Geophysical studies conducted in the Lopar area revealed presence of underground remains of ancient structures, probably from the late Roman period and connected with a ceramic production centre at the present seashore. The most interesting results were obtained for the area no. 4, the site where magnetic, georadar and ERT surveys revealed an ancient regular building at 0.4–0.6 m depth. The survey performed in the Lopar area clearly indicates that integration of different geophysical methods enables detailed and effective identification of buried archaeological structures.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;AN ATTEMPT TO INTEGRATION OF DIFFERENT GEOPHYSICAL METHODS (MAGNETIC, GPR AND ERT); A CASE STUDY FROM THE LATE ROMAN SETTLEMENT ON THE ISLAND OF RAB IN CROATIA&quot;,&quot;attachmentId&quot;:53650142,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/33637096/AN_ATTEMPT_TO_INTEGRATION_OF_DIFFERENT_GEOPHYSICAL_METHODS_MAGNETIC_GPR_AND_ERT_A_CASE_STUDY_FROM_THE_LATE_ROMAN_SETTLEMENT_ON_THE_ISLAND_OF_RAB_IN_CROATIA&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/33637096/AN_ATTEMPT_TO_INTEGRATION_OF_DIFFERENT_GEOPHYSICAL_METHODS_MAGNETIC_GPR_AND_ERT_A_CASE_STUDY_FROM_THE_LATE_ROMAN_SETTLEMENT_ON_THE_ISLAND_OF_RAB_IN_CROATIA"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="3" data-entity-id="32228902" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/32228902/Electrical_Resistivity_Tomography_for_the_Modelling_of_Cultural_Deposits_and_Geomophological_Landscapes_at_Neolithic_Sites_a_Case_Study_from_Southeastern_Hungary">Electrical Resistivity Tomography for the Modelling of Cultural Deposits and Geomophological Landscapes at Neolithic Sites: a Case Study from Southeastern Hungary</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="224648" href="https://fieldmuseum.academia.edu/WilliamAParkinson">William A. Parkinson</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="1170782" href="https://ucy.academia.edu/ApostolosSarris">Apostolos Sarris</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="470795" href="https://uni-kiel.academia.edu/PaulRDuffy">Paul R. Duffy</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="227860" href="https://osu.academia.edu/RichardYerkes">Richard Yerkes</a></div><p class="ds-related-work--abstract ds2-5-body-sm">A large-scale electrical resistivity tomography (ERT) survey was undertaken around the Neolithic tell of Szeghalom-Kovácshalom in southeast Hungary, covering an area of almost 6 ha. High-resolution ERT data were collected along 28 uniformly distributed transects of variable length using the roll-along technique. A recently presented two-dimensional fast non-linear resistivity inversion algorithm was used to invert the ERT data and recover the true subsurface resistivity distribution along the specific cross-sections. The algorithm calculates and stores in an efficient manner the part of the Jacobian matrix that is actually important within the inversion procedure, thus rendering it almost 4.8 times faster than the algorithm that calculates the complete Jacobian matrix, without losing quality. The algorithm was further modified to account for any non-standard electrode configuration. A recently established iterative algorithm for sparse least squares problems (LSMR) was incorporated for the first time into the algorithm to solve the inverse resistivity problem. The effectiveness and robustness of the LSMR solver was highlighted through the processing of all the ERT lines. The processing and evaluation of the ERT data made it possible to map the thickness of the anthropogenic layer below the surface of the tell, to outline the horizontal and vertical dimensions of the palaeochannel adjacent to the tell, and to determine the general stratigraphy of geological layers up to 10 m below the ground surface. The ERT results also were used to update an older topographic map of the site showing the course of the palaeochannel around the tell. A synthetic model verified and enhanced the conclusions based on the field data. This study illustrates the added value that a systematic ERT survey can provide in reconstructing the ancient fluvial geomorphology of a microregion as well as the depth and horizontal extent of deposits associated with human habitation at archaeological sites.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Electrical Resistivity Tomography for the Modelling of Cultural Deposits and Geomophological Landscapes at Neolithic Sites: a Case Study from Southeastern Hungary&quot;,&quot;attachmentId&quot;:52453428,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/32228902/Electrical_Resistivity_Tomography_for_the_Modelling_of_Cultural_Deposits_and_Geomophological_Landscapes_at_Neolithic_Sites_a_Case_Study_from_Southeastern_Hungary&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/32228902/Electrical_Resistivity_Tomography_for_the_Modelling_of_Cultural_Deposits_and_Geomophological_Landscapes_at_Neolithic_Sites_a_Case_Study_from_Southeastern_Hungary"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="4" data-entity-id="95574147" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/95574147/Mapping_the_subsurface_structures_of_a_lost_medieval_village_in_South_Western_Romania_by_combining_conventional_geophysical_methods">Mapping the subsurface structures of a lost medieval village in South-Western Romania by combining conventional geophysical methods</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="1060125" href="https://csde.academia.edu/CristianFloca">Cristian Floca</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Archaeological Prospection, 2018</p><p class="ds-related-work--abstract ds2-5-body-sm">The medieval fortification of Mașloc, known as the &#39;Șanțul Turcilor&#39; (Turkish ditch) is one of the best preserved archaeological sites in the Banat region, Romania. To reconstruct the subsurface archaeological features at the Mașloc site we combined three different geophysical methods: magnetometry, ground-penetrating radar (GPR) and electrical resistivity tomography (ERT) and we used SfM (structure-from-motion) to achieve a detailed digital elevation model and an orthophoto mosaic also. Six hectares were investigated by magnetometry in order to define the basic outline of the medieval settlement, which gradually developed around the fortification. Several GPR and ERT profiles were constructed over the ramparts and ditches of the fortification to determine their extent and the internal structure of the ramparts, ditches and the houses within. The interpretation of these profiles shows for the first time the existence of a second ditch around the fortification: this is not visible in the field. The geophysical mapping precisely identifies the dwellings within the site, which shows the spatial organization of the village. Houses were developed along its main street, oriented northeast-southwest (NE-SW), which were constructed using well-established rules and must have been planned by a local administration. Such organization demonstrates the importance of the village in medieval times, due probably to its location near to the road between two important towns: Timișoara and Lipova. The geophysical results now allow us to associate this settlement with the lost Machalaka, an important village mentioned in the medieval documents. The geophysical investigation demonstrates how this method can delineate village boundaries and the planimetry of internal archaeological features.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Mapping the subsurface structures of a lost medieval village in South-Western Romania by combining conventional geophysical methods&quot;,&quot;attachmentId&quot;:97718886,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/95574147/Mapping_the_subsurface_structures_of_a_lost_medieval_village_in_South_Western_Romania_by_combining_conventional_geophysical_methods&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/95574147/Mapping_the_subsurface_structures_of_a_lost_medieval_village_in_South_Western_Romania_by_combining_conventional_geophysical_methods"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="5" data-entity-id="21781792" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/21781792/Papadopoulos_N_G_A_Sarris_W_A_Parkinson_A_Gyucha_R_W_Yerkes_P_R_Duffy_and_P_Tsourlos_2014_Electrical_Resistivity_Tomography_for_the_Modelling_of_Cultural_Deposits_and_Geomorphological_Landscapes_at_Neolithic_Sites_Archaeological_Prospection_21_169_183">Papadopoulos, N.G., A. Sarris, W.A. Parkinson, A. Gyucha, R.W. Yerkes, P.R. Duffy and P. Tsourlos 2014 Electrical Resistivity Tomography for the Modelling of Cultural Deposits and Geomorphological Landscapes at Neolithic Sites. Archaeological Prospection 21:169-183.</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="224648" href="https://fieldmuseum.academia.edu/WilliamAParkinson">William A. Parkinson</a></div><p class="ds-related-work--metadata ds2-5-body-xs">Archaeological Prospection, 2014</p><p class="ds-related-work--abstract ds2-5-body-sm">A large-scale electrical resistivity tomography (ERT) survey was undertaken around the Neolithic tell of Szeghalom-Kovácshalom in southeast Hungary, covering an area of almost 6 ha. High-resolution ERT data were collected along 28 uniformly distributed transects of variable length using the roll-along technique. A recently presented two-dimensional fast non-linear resistivity inversion algorithm was used to invert the ERT data and recover the true subsurface resistivity distribution along the specific cross-sections. The algorithm calculates and stores in an efficient manner the part of the Jacobian matrix that is actually important within the inversion procedure, thus rendering it almost 4.8 times faster than the algorithm that calculates the complete Jacobian matrix, without losing quality. The algorithm was further modified to account for any non-standard electrode configuration. A recently established iterative algorithm for sparse least squares problems (LSMR) was incorporated for the first time into the algorithm to solve the inverse resistivity problem. The effectiveness and robustness of the LSMR solver was highlighted through the processing of all the ERT lines. The processing and evaluation of the ERT data made it possible to map the thickness of the anthropogenic layer below the surface of the tell, to outline the horizontal and vertical dimensions of the palaeochannel adjacent to the tell, and to determine the general stratigraphy of geological layers up to 10 m below the ground surface. The ERT results also were used to update an older topographic map of the site showing the course of the palaeochannel around the tell. A synthetic model verified and enhanced the conclusions based on the field data. This study illustrates the added value that a systematic ERT survey can provide in reconstructing the ancient fluvial geomorphology of a microregion as well as the depth and horizontal extent of deposits associated with human habitation at archaeological sites. Figure 6. Surface maps showing the topographic relief of the different stratigraphic layers around the Szeghalom-Kovácshalom tell. (a) Thickness of the topsoil and anthropogenic Layer. (b) Thickness of the palaeochannel. (c) Thickness of the silty clay and silty clay with sand layer. (d) Burial depth of the deepest clayey layer. This figure is available in colour online at wileyonlinelibrary.com/journal/arp Figure 7. Overlay of the outline of the palaeochannel on an old topographic map of the tell. The solid and dashed lines indicate respectively the definite and prospective boundaries of the palaeochannel as extracted by the ERT survey. This figure is available in colour online at wileyonlinelibrary.com/journal/arp</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Papadopoulos, N.G., A. Sarris, W.A. Parkinson, A. Gyucha, R.W. Yerkes, P.R. Duffy and P. Tsourlos \t2014\tElectrical Resistivity Tomography for the Modelling of Cultural Deposits and Geomorphological Landscapes at Neolithic Sites. Archaeological Prospection 21:169-183.&quot;,&quot;attachmentId&quot;:42546631,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/21781792/Papadopoulos_N_G_A_Sarris_W_A_Parkinson_A_Gyucha_R_W_Yerkes_P_R_Duffy_and_P_Tsourlos_2014_Electrical_Resistivity_Tomography_for_the_Modelling_of_Cultural_Deposits_and_Geomorphological_Landscapes_at_Neolithic_Sites_Archaeological_Prospection_21_169_183&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/21781792/Papadopoulos_N_G_A_Sarris_W_A_Parkinson_A_Gyucha_R_W_Yerkes_P_R_Duffy_and_P_Tsourlos_2014_Electrical_Resistivity_Tomography_for_the_Modelling_of_Cultural_Deposits_and_Geomorphological_Landscapes_at_Neolithic_Sites_Archaeological_Prospection_21_169_183"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="6" data-entity-id="350135" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/350135/Milo_Peter_Lichtenstein_L%C3%A1szlo_Rozsa_Zolt%C3%A1n_Tencer_Tom%C3%A1%C5%A1_Fekete_Zolt%C3%A1n_Vlach_Marek_Geophysical_Survey_at_archaeological_site_Kaszaper_B%C3%A9k%C3%A9s_County_Hungary_Arch%C3%A9oSciences_33_2009">Milo, Peter - Lichtenstein, Lászlo - Rozsa, Zoltán - Tencer, Tomáš - Fekete, Zoltán - Vlach, Marek. Geophysical Survey at archaeological site Kaszaper, Békés County, Hungary. ArchéoSciences 33. 2009.</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="1003623" href="https://muni.academia.edu/PeterMilo">Peter Milo</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="2679749" href="https://independent.academia.edu/L%C3%A1szl%C3%B3Lichtenstein">Lichtenstein László</a><span>, </span><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="265834" href="https://arup-cas.academia.edu/MarekVlach">Marek Vlach</a></div><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Milo, Peter - Lichtenstein, Lászlo - Rozsa, Zoltán - Tencer, Tomáš - Fekete, Zoltán - Vlach, Marek. Geophysical Survey at archaeological site Kaszaper, Békés County, Hungary. ArchéoSciences 33. 2009.&quot;,&quot;attachmentId&quot;:33033454,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/350135/Milo_Peter_Lichtenstein_L%C3%A1szlo_Rozsa_Zolt%C3%A1n_Tencer_Tom%C3%A1%C5%A1_Fekete_Zolt%C3%A1n_Vlach_Marek_Geophysical_Survey_at_archaeological_site_Kaszaper_B%C3%A9k%C3%A9s_County_Hungary_Arch%C3%A9oSciences_33_2009&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/350135/Milo_Peter_Lichtenstein_L%C3%A1szlo_Rozsa_Zolt%C3%A1n_Tencer_Tom%C3%A1%C5%A1_Fekete_Zolt%C3%A1n_Vlach_Marek_Geophysical_Survey_at_archaeological_site_Kaszaper_B%C3%A9k%C3%A9s_County_Hungary_Arch%C3%A9oSciences_33_2009"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="7" data-entity-id="5236138" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/5236138/_2005_LARGE_SCALE_MAGNETIC_SURVEY_AND_ARCHAEOLOGICAL_MAPPING_THE_GROSSETO_AND_SIENA_PROJECTS">(2005) LARGE SCALE MAGNETIC SURVEY AND ARCHAEOLOGICAL MAPPING. THE GROSSETO AND SIENA PROJECTS</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="1409423" href="https://unisi.academia.edu/CristinaFelici">Cristina Felici</a></div><p class="ds-related-work--metadata ds2-5-body-xs">in 6th INTERNATIONAL CONFERENCE ON ARCHAEOLOGICAL PROSPECTION</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;(2005) LARGE SCALE MAGNETIC SURVEY AND ARCHAEOLOGICAL MAPPING. THE GROSSETO AND SIENA PROJECTS&quot;,&quot;attachmentId&quot;:32419885,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/5236138/_2005_LARGE_SCALE_MAGNETIC_SURVEY_AND_ARCHAEOLOGICAL_MAPPING_THE_GROSSETO_AND_SIENA_PROJECTS&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/5236138/_2005_LARGE_SCALE_MAGNETIC_SURVEY_AND_ARCHAEOLOGICAL_MAPPING_THE_GROSSETO_AND_SIENA_PROJECTS"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="8" data-entity-id="59878874" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/59878874/Archaeology_and_landscape_features_in_Magnetometer_Data">Archaeology and landscape features in Magnetometer Data</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="48994539" href="https://independent.academia.edu/ImmoHeske">Immo Heske</a></div><p class="ds-related-work--metadata ds2-5-body-xs">ArchéoSciences, 2009</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Archaeology and landscape features in Magnetometer Data&quot;,&quot;attachmentId&quot;:73575114,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/59878874/Archaeology_and_landscape_features_in_Magnetometer_Data&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/59878874/Archaeology_and_landscape_features_in_Magnetometer_Data"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div><div class="ds-related-work--container js-wsj-grid-card" data-collection-position="9" data-entity-id="11393282" data-sort-order="default"><a class="ds-related-work--title js-wsj-grid-card-title ds2-5-body-md ds2-5-body-link" href="https://www.academia.edu/11393282/Electric_Resistivity_Tomography_and_Magnetic_Susceptibility_Measurements_at_the_Baden_Culture_Site_Stavenice_%C3%9Asov_Czech_Republic_">Electric Resistivity Tomography and Magnetic Susceptibility Measurements at the Baden Culture Site Stavenice-Úsov (Czech Republic)</a><div class="ds-related-work--metadata"><a class="js-wsj-grid-card-author ds2-5-body-sm ds2-5-body-link" data-author-id="3346786" href="https://upol.academia.edu/MartinMon%C3%ADk">Martin Moník</a></div><p class="ds-related-work--abstract ds2-5-body-sm">Electric resistivity tomography (ERT) is a well-known geophysical method for the identification of archaeological features. It was applied at the Middle Eneolithic fortified site Stavenice-Úsov in Central Moravia (Czech Republic) to reconstruct the shape and structure of a local rampart and, if possible, identify additional settlement features in addition to those revealed by archaeological excavation. Simultaneously, mass magnetic susceptibility (χmass) was measured in selected settlement layers and fills in order to distinguish settlement and post-settlement strata and contexts destroyed or otherwise influenced by fire. The results of ERT measurement indicate that artificial terrain modifications took place on the northern, south-eastern and possibly south-western slopes of the hill. Magnetic susceptibility values indicate that the fortification, and in all probability also other settlement features, had been destroyed by fire.</p><div class="ds-related-work--ctas"><button class="ds2-5-text-link ds2-5-text-link--inline js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;wsj-grid-card-download-pdf-modal&quot;,&quot;work_title&quot;:&quot;Electric Resistivity Tomography and Magnetic Susceptibility Measurements at the Baden Culture Site Stavenice-Úsov (Czech Republic)&quot;,&quot;attachmentId&quot;:36952025,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;work_url&quot;:&quot;https://www.academia.edu/11393282/Electric_Resistivity_Tomography_and_Magnetic_Susceptibility_Measurements_at_the_Baden_Culture_Site_Stavenice_%C3%9Asov_Czech_Republic_&quot;,&quot;alternativeTracking&quot;:true}"><span class="material-symbols-outlined" style="font-size: 18px" translate="no">download</span><span class="ds2-5-text-link__content">Download free PDF</span></button><a class="ds2-5-text-link ds2-5-text-link--inline js-wsj-grid-card-view-pdf" href="https://www.academia.edu/11393282/Electric_Resistivity_Tomography_and_Magnetic_Susceptibility_Measurements_at_the_Baden_Culture_Site_Stavenice_%C3%9Asov_Czech_Republic_"><span class="ds2-5-text-link__content">View PDF</span><span class="material-symbols-outlined" style="font-size: 18px" translate="no">chevron_right</span></a></div></div></div></div><div class="ds-sticky-ctas--wrapper js-loswp-sticky-ctas hidden"><div class="ds-sticky-ctas--grid-container"><div class="ds-sticky-ctas--container"><button class="ds2-5-button js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;continue-reading-button--sticky-ctas&quot;,&quot;attachmentId&quot;:31385541,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;workUrl&quot;:null}">See full PDF</button><button class="ds2-5-button ds2-5-button--secondary js-swp-download-button" data-signup-modal="{&quot;location&quot;:&quot;download-pdf-button--sticky-ctas&quot;,&quot;attachmentId&quot;:31385541,&quot;attachmentType&quot;:&quot;pdf&quot;,&quot;workUrl&quot;:null}"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">download</span>Download PDF</button></div></div></div><div class="ds-below-fold--grid-container"><div class="ds-work--container js-loswp-embedded-document"><div class="attachment_preview" data-attachment="Attachment_31385541" style="display: none"><div class="js-scribd-document-container"><div class="scribd--document-loading js-scribd-document-loader" style="display: block;"><img alt="Loading..." src="//a.academia-assets.com/images/loaders/paper-load.gif" /><p>Loading Preview</p></div></div><div style="text-align: center;"><div class="scribd--no-preview-alert js-preview-unavailable"><p>Sorry, preview is currently unavailable. 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