TY - GEN A1 - Verschoof-van der Vaart, Wouter A1 - Bonhage, Alexander A1 - Schneider, Anna A1 - Ouimet, William A1 - Raab, Thomas T1 - Automated large-scale mapping and analysis of relict charcoal hearths in Connecticut (USA) using a Deep Learning YOLOv4 framework T2 - Archaeological Prospection Y1 - 2023 U6 - https://doi.org/10.1002/arp.1889 SN - 1099-0763 SN - 1075-2196 VL - 30 IS - 3 SP - 251 EP - 266 ER - TY - GEN A1 - Malik, Ireneusz A1 - Bohr, Marcin A1 - Wistuba, Małgorzata A1 - Raab, Thomas A1 - Bonhage, Alexander A1 - Verschoof-van der Vaart, Wouter A1 - Raab, Alexandra A1 - Woskowicz-Ślęzak, Beata T1 - Multi-Period Ore Exploitation in Upper Silesia, Central Europe T2 - Journal of Field Archaeology Y1 - 2023 U6 - https://doi.org/10.1080/00934690.2023.2200583 SN - 0093-4690 VL - 48 IS - 5 SP - 366 EP - 379 ER - TY - GEN A1 - Bonhage, Alexander A1 - Raab, Thomas A1 - Raab, Alexandra A1 - Schneider, Anna A1 - Malik, Ireneusz A1 - Wistuba, Malgorzata A1 - Verschoof-van der Vaart, Wouter T1 - Land use legacy landforms at the UNESCO Heritage Site Tarnowskie Góry, Upper Silesia, Poland : stratigraphy, soils and age T2 - Geoarchaeology N2 - Metallurgy in Upper Silesia (Poland) has a long tradition of international significance, which was emphasized in 2017 when the historic silver mine in Tarnowskie Góry was inscribed as a UNESCO World Heritage site. The area consists of various anthropogenic landforms, the stratigraphy of which has hardly been studied so far. In this study, we describe five main morphological units: Unit I (RCH) and Unit II (RCH pit), resulting from charcoal production; Unit III (shaft) and Unit IV (shaft heap), resulting from mining; and Unit V (reference forest soil). The first four units are a variation of a Technosol with inherently different properties from the reference forest soil. Unit I exhibits typical properties of a relict charcoal hearth (RCH), whereas Unit II resembles a pit. Unit III consists of a mostly infilled mining shaft remain (MSR), characterized by relocated subsoil. Unit IV consists of material from the adjacent Unit III that has been dumped directly aside. The studied RCH was used no earlier than during the second half of the 17th century, probably between 1725 and 1813. The studied MSR was used most likely between the 3rd and 5th centuries, which is much older than described so far. Together, the units reflect the characteristic heterogeneity of soils in shaft mining and RCH areas. KW - Geoarchaeology KW - Mining Landscape KW - Landscape History Y1 - 2024 U6 - https://doi.org/https://doi.org/10.1002/gea.22028 SN - 1520-6548 VL - 40 IS - 1 SP - 1 EP - 8 PB - Wiley ER -