We analyze ground-penetrating radar (GPR) data which was recorded in the tight confined spaces of an overgrown sand dune. The topography of the dune has the same scale as the penetration depth. We developed a 3D topographic migration algorithm and enable the generation and interpretation of layer parallel depth slices.

Buried remains of an early modern manor are investigated using ERT and GPR. For this purpose, 3D approaches are applied for high-resolution imaging. The results of both methods are interpreted in combination with archaeological findings.

Non-destructive geophysical methods were applied to detect moisture at the St. Petri Cathedral in Schleswig. One of them is thermography, which allows to distinguish between intact and defective medieval plaster. Additionally, thesuccess of a restoration can be determined by ultrasonic surface measurements.

In this paper we analyze the applicability of seismic full-waveform inversion (FWI) for investigation of tells, which are often characterized by heterogeneous and small-scale stratigraphy. Major aim is to identify location and shape of settlement layers and house remains. Furthermore, a paleochannel, which is important to understand the interaction between tell and the surrounding landscape, was found at the tell flank.

In November 2021, a geophysical prospection using magnetics, electromagnetics, and ground penetrating radar, as well as a surface archaeological survey and aerial photography were conducted in the kurgan area on the Uzun-Rama plateau in central Azerbaijan. These non-destructive investigations aim to obtain information on the morphology, structure and spatial distribution of the urgans in order to classify them according to various features. The preliminary results show that increased magnetic field intensity, increased electrical conductivity, and increased reflection energy in the GPR are observed in the top region of the kurgans, which contain information about the burial chamber.