Abstract
In the Muro district of Uchinada Town, which suffered significant liquefaction damage
during the 2024 Noto Peninsula Earthquake, PDC (Piezodrive Cone) surveys and EM
(Electromagnetic) explorations were conducted as part of a fundamental study aimed at
elucidating the mechanism of liquefaction damage. These investigations sought to understand
the detailed ground conditions and create geological cross-sections. Surface wave surveys were
also performed to assess the looseness of the surface layer based on the conductivity distribution,
and these results were compared with the actual liquefaction damage to confirm consistency.