Magnetometry on the Geoglyphs of Palpa and Nasca (Peru) (original) (raw)

Magnetic Signatures of Urban Structures: Case Study from Larsa (Iraq, 6th–1st millennium BC)

Archéosciences, 2021

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Magnetic survey for detection of buried archaeological features in Al-Madai'n area, southeast of Baghdad, Iraq

ABSTRUCT A detailed magnetic survey has been carried out in Taq-Kisra Archaeological Site, situated in Al-Mada'in city about 32 Km southeast of Baghdad. The aim of this survey is to delineate the locations and extensions of the buried archaeological structures. The area is covered by 2×2 m net of magnetic measurements, with 5262 stations measured with an accuracy of up to ±1.8 nT. Residual magnetic intensity map of the site has been constructed after applying the necessary corrections on the row data. Generally, the map shows linear magnetic anomalies that have archaeological meaning. The range of the achieved magnetic anomalies is (15 – 24) nT. Location of ten trenches, depending on the magnetic map, have been suggested for checking the obtained magnetic anomalies. The results of the excavations showed good relations between the observed magnetic anomalies and the causative sources, represented by archaeological features. The archaeological features appeared through excavations...

GEOPHYSICAL INVESTIGATION AT TELL EL-DABAA ʺAVARISʺ ARCHAEOLOGICAL SITE

A. I. Taha, G. El - Qady, M. A. Metwaly, U. Massoud, 2011

Tell El-Dabaa is one of the important archaeological sites in the Eastern part of the Nile Delta. It is located at about 7 km north of Faqous city, Sharqiya governorate, Egypt. The ancient name of El-Dabaa area was Avaris, which had been considered as the main capital of Hyksos (Dynasty XV) from 1650 to 1542 B.C. The whole area was covered by the deltaic deposits during the successive flood events along Nile Delta. Geomagnetic and geoelectric surveys have been carried out in order to outline the subsurface archaeological remains in this area. The target area, which is about 10000 m 2 , was surveyed in grid pattern each of 20x 10 m for magnetic survey and 20 × 20 m for geoelectri-cal resistance survey. Integrated results of the magnetic and geoelectric data analysis have succeeded in delineating a clear subsurface picture of archaeological remains. The results show many linear anomalies, which may represent buried walls, as well as some small archaeological remains detached from the main walls. Also, we could notice some rectangular features with different sizes, which might be described as remains of different archaeological buildings. Besides, some circular structures with small size obtained and could be interpreted as columns foundations.

Herrmann, J. T. – Faßbinder, J. W. E. – Scheiblecker, M. – Kluge, P. – Döpper, S. – Schmidt, C. (2018), Magnetometer survey of a Hafit monumental complex, al-Khashbah, Sultanate of Oman (poster). Proceedings of the Seminar for Arabian Studies 48, 119–124

Magnetometer surveys carried out as part of the al-Khashbah Archaeological Project have revealed the plan of two monumental buildings dating to the third millennium BC as well as the surrounding landscape. Evidence from excavations confirms that this complex can be dated to the Hafit period, marking it as an important site for the development of social complexity in the interior of northern Oman. The results of two seasons of magnetometer surveys, conducted in 2015 and 2017, are instructive in two major ways. The fused magnetograms are a record of the prehistoric cultural landscape immediately surrounding Building I and Building XI. The two surveys provide a direct comparison of two different geophysical methods of magnetometer survey: fluxgate gradiometry (2015 survey) and total field magnetometry (2017 survey), which can aid analysis of survey results. The surveys took place near the geomagnetic equator where the shallow inclination of the Earth’s magnetic field can make archaeological interpretation of magnetic anomalies rather complex.

Landscape archaeology and oldest monumental buildings in Oman - Magnetometry near the Geomagnetic Equator

The UNESCO World Heritage Site of Bāt al-Khutm and al-Ayn in Oman (fig. 1) represents one of the most complete and well preserved ensembles of settlements and necropolises from the 3rd millennium BC with the two main periods: Hafi t (ca. 3100–2700 BC) and Umm an-Nar (ca. 2700–2000 BC). Started with the Hafi t period settled agricultural villages occurred in this arid climate with farming, irrigation systems, metallurgy, ceramics and necropolises (tombs and towers). Exploring the site of Bāt by excavations commenced in the 1970s (e.g. Frifelt 1976, 57–76). In 2004, a German team started the “Bāt Research & Restoration Project” in Bāt and al-Ayn (Böhme et al. 2008). Current studies on the Early Bronze Age archaeology have a broad regional focus in which the relationships between sites and landscape regions are of key interest (projects to name like one by C. P. Thornton & C. Schmidt (Thornton, Schmidt 2015, 155–163) or by C. Schmidt (Schmidt, Döpper 2017b, 121–122). The applied methods for landscape archaeology concentrate mainly on analyzing satellite images, field work, limited size excavations (e. g. for tombs, house structures), and use of GIS technologies. A recent geoarchaeological study of the Wadi Sharsah valley in Bāt combined the work of geomorphologists, micromorphologists, archaeobotanists and malacologists (Desruelles et al. 2016, 52). One rarely applied prospection method in Oman is caesium magnetometry in duo-sensor-confi guration, which is in particular suited for palaegeographic and geoarchaeological modelling. In our opinion this method could substantially contribute to solve archaeological questions and should be more consistently applied. This will be illustrated by two examples, the magnetometry from 2006 at Bāt and from 2017 at Al-Khashbah.