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Case studies and archaeologica The Ecstasy of Gold: Magnetometer The geophysical prospection in was funded by the Gerda-Henkel-Foundation. It is the largest gold deposit in the Caucasus and is thought to have been exploited already during the 2 nd millennium BC. The mine remained active with interruptions until the 14 th century AD and was rediscovered in the 20 th century AD. Bronze Age occupation left settlements, cemeteries and other material, like weapons and cultic objects, around the mine. Investigation of archaeological sites around the Sotk mine and in the Gegharkunik province confirmed the presence of prehistoric gold mining and trading in the region. How the gold mining and trading influenced prehistoric settlement structures is under investigation. Figure 1. We have refrained from printing the georeferenced data to avoid possible looting of the kurgans. Satellite image: Google. A possible pattern of settlement hinting at regional gold mining has been outlined by the results of the different research approaches. From a geographical point of view, the peninsula is a natural route for super-regional communication and trade. Magnetometer surveys were conducted in on the shore of the lake near Artanish. Two burial grounds were surveyed among others, preparing the ground for their excavation with the objective of contributing new data on the prehistoric communities living north of Lake Sevan. Archaeological and archaeo-metallurgical analyses of the metal artifacts will determine the connection with gold mining in Sotk. With a sampling frequency of 0. Geoplot software Geoscan Ltd. UK was used for data processing. The raw data was interpolated to a resolution of 0. The measurements were accompanied by high resolution drone orthophotos, and a Digital Elevation Model DEM of the survey area was derived from these photos. Figure 2. Magnetometer survey of the Artanish peninsula; the Geometrics G magnetometer in this image was operated by Sandra Hahn. According to the soil map, the Artanish peninsula is dominated by lake sediments as well as mountain-forest brown soils at higher altitudes. The soil at the prospecting locations shows a magnetic susceptibility of around 0. The cromlechs were built of locally occurring Jurassic—Cretaceous rocks from different gabbros or other ophiolite complexes. The values of the magnetic susceptibility of the ophiolite complexes range from around 1. Slight colour deviations could also signal a variation in the rocks. Burial chambers are constructed of limestone, probably also local late Cretaceous sedimentary rocks with a rather negligible remanence and small magnetic susceptibility of around 0. Figure 3. Examples of susceptibility measurements: a Soil at the burial sites; b—d Different gabbros or ophiolite complexes. Four large burials are clearly marked with yellow solid lines in Fig. At least 32 smaller burial sites marked with dashed lines 0f varying diameter are visible in the magnetogram. The four larger ones, marked with solid circles in Figure 1b, can be assumed to be burial mounds, or kurgans, mainly because the grave chambers are visible in the magnetograms shaded yellow in Fig. The positive anomalies suggest that these burial chambers are covered on top with stronger magnetic rocks, probably ophiolites, rather than the non or little magnetic limestone. The survey here covered around 1 ha. The radiuses of the burials are noticeably smaller than at the other site, and the cromlechs are less clearly traceable those clear enough are marked with dashed circles in Fig. Some rocks, especially in the top left of the grid, seem to be misplaced. The pattern of dipole anomalies corresponding to the cromlechs is different despite being caused mainly by volcanic rock. This can be explained by remanent magnetisation dominating over induced magnetisation. This results in anomalies with one signal, positive or negative, and anomalies with two signals in any succession or orientation but still belonging to a ferrimagnetic source. The burial chambers of the kurgans are clearly visible in the magnetogram but not recognisable in the orthophotos. Additionally, the magnetometer survey also detects rocks buried beneath the sediment. This is because of the high magnetic contrast between the rocks used for tomb construction and the surrounding soil. However, the variation in the magnetic properties of the rocks used biases the perception of the true rock size in the case of the cromlechs. In other words, rock size to anomaly size need not be proportional, and aerial images are apt to give a better indication of the size. In addition, the magnetic contrast between rock and soil can be marginal in some cases and again, aerial images can help to reconstruct the enclosures. Kunze, R. Projekt Ushkiani. Avetisyan ed. Meller, P. Avetissyan eds. Wolf, D. Meller, R. Risch, E. Pernicka eds. Martin-Luther-University Halle-Wittenberg. Site map — Syndication. Privacy Policy — About Cookies — Report a problem. OpenEdition member — Published with Lodel — Administration only. Skip to navigation — Site map. Contents - Previous document - Next document. Case studies and archaeological feedback. Abstract — Magnetometer prospection of a Bronze Age burial ground in Armenia. Index terms Keywords: dipole anomalies , burial ground , gold mining , magnetometer prospection. Outline Introduction. Full text PDF 3. Zoom Original jpeg, 3. Zoom Original jpeg, 10M. Bibliography Kunze, R. List of illustrations Title Figure 1. Top of page. Follow us RSS feed. Newsletters OpenEdition Newsletter. In All OpenEdition. On ArcheoSciences. 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