AIRBORNE LASER BATHYMETRY FOR DOCUMENTATION OF SUBMERGED ARCHAEOLOGICAL SITES IN SHALLOW WATER
- 1Department of Prehistoric and Historical Archaeology, University of Vienna, Franz-Kleingasse 1, 1190 Wien, Austria
- 2LBI for Archaeological Prospection & Virtual Archaeology, Hohe Warte 38, 1190 Wien, Austria
- 3Department for Underwater Archaeology, Croatian Conservation Institute, Nike Grškovića 23, 10000 Zagreb, Croatia
- 4Department of Geodesy and Geoinformation, Vienna University of Technology, Gusshausstrasse 27-29, 1040 Wien, Austria
- 5Earth Observation Data Centre (EODC), Gusshausstrasse 27-29, 1040 Wien, Austria
Keywords: airborne laser scanning, airborne laser bathymetry, green laser, archaeological prospection, underwater, submerged site, Roman harbour, lake dwelling
Abstract. Knowledge of underwater topography is essential to the understanding of the organisation and distribution of archaeological sites along and in water bodies. Special attention has to be paid to intertidal and inshore zones where, due to sea-level rise, coastlines have changed and many former coastal sites are now submerged in shallow water. Mapping the detailed inshore topography is therefore important to reconstruct former coastlines, identify sunken archaeological structures and locate potential former harbour sites. However, until recently archaeology has lacked suitable methods to provide the required topographical data of shallow underwater bodies. Our research shows that airborne topo-bathymetric laser scanner systems are able to measure surfaces above and below the water table over large areas in high detail using very short and narrow green laser pulses, even revealing sunken archaeological structures in shallow water. Using an airborne laser scanner operating at a wavelength in the green visible spectrum (532 nm) two case study areas in different environmental settings (Kolone, Croatia, with clear sea water; Lake Keutschach, Austria, with turbid water) were scanned. In both cases, a digital model of the underwater topography with a planimetric resolution of a few decimeters was measured. While in the clear waters of Kolone penetration depth was up to 11 meters, turbid Lake Keutschach allowed only to document the upper 1.6 meters of its underwater topography. Our results demonstrate the potential of this technique to map submerged archaeological structures over large areas in high detail providing the possibility for systematic, large scale archaeological investigation of this environment.