TY - JOUR
T1 - A submerged and buried mesolithic site off Svanemøllen Harbor, Copenhagen, Denmark
T2 - Acoustic detection (human-altered lithic detection) and verification by means of coring
AU - Boldreel, Lars Ole
AU - Grøn, Ole
AU - Tayong, Rostand Boumda
AU - Madsen, Bo
AU - Bennike, Ole
AU - Andersen, Morten Sparre
N1 - Publisher Copyright:
© 2025 by the authors.
PY - 2025/2/1
Y1 - 2025/2/1
N2 - Teledyne Chirp III high-resolution seismic data were acquired over a three-year period at a water depth of 6.0–9.0 m, with a clear concentration of acoustic “haystack” features, in the dredged Svanemøllen Harbor, Copenhagen. The recordings show haystacks related to preserved shallow basins and rivers in the paleo-coastal setting. Eleven short vibrocores were retrieved below these pronounced haystacks and a sandy interval, underlain by clayey till and overlain by harbor mud, which represent the basin configuration. Two cores contained four pieces of knapped flint in the sandy interval (statistical density of around 230 pieces per square meter), while the remaining cores did not reach the desired depth. Finite Element (FE) modeling revealed that the small pieces of knapped flint were resonant and that the acoustic impedance of the flint was high. The Svanemøllen Harbor site is a hitherto unknown buried Stone Age site, and this is the first time ever that an unknown submerged, buried Stone Age site has been acoustically detected (using Teledyne Chirp III), verified by means of coring and modeled using FE modeling. The Innomar and Geopulse data acquired at the site did not register any haystacks. Due to the global sea level rise after the Last Glacial Maximum, a significant part of the world’s submerged Stone Age sites must be expected to be buried in seafloor sediments.
AB - Teledyne Chirp III high-resolution seismic data were acquired over a three-year period at a water depth of 6.0–9.0 m, with a clear concentration of acoustic “haystack” features, in the dredged Svanemøllen Harbor, Copenhagen. The recordings show haystacks related to preserved shallow basins and rivers in the paleo-coastal setting. Eleven short vibrocores were retrieved below these pronounced haystacks and a sandy interval, underlain by clayey till and overlain by harbor mud, which represent the basin configuration. Two cores contained four pieces of knapped flint in the sandy interval (statistical density of around 230 pieces per square meter), while the remaining cores did not reach the desired depth. Finite Element (FE) modeling revealed that the small pieces of knapped flint were resonant and that the acoustic impedance of the flint was high. The Svanemøllen Harbor site is a hitherto unknown buried Stone Age site, and this is the first time ever that an unknown submerged, buried Stone Age site has been acoustically detected (using Teledyne Chirp III), verified by means of coring and modeled using FE modeling. The Innomar and Geopulse data acquired at the site did not register any haystacks. Due to the global sea level rise after the Last Glacial Maximum, a significant part of the world’s submerged Stone Age sites must be expected to be buried in seafloor sediments.
KW - FE modeling
KW - high-resolution seismic
KW - knapped flint
KW - submerged stone age site
KW - vibrocore
UR - http://www.scopus.com/inward/record.url?scp=85217616879&partnerID=8YFLogxK
U2 - 10.3390/rs17030413
DO - 10.3390/rs17030413
M3 - Article
AN - SCOPUS:85217616879
SN - 2072-4292
VL - 17
JO - Remote Sensing
JF - Remote Sensing
IS - 3
M1 - 413
ER -