Abstract
Crustal movements associated with the 1923 Kanto, Japan, earthquake have been studied by some investigators but reliable results using the second order triangulation stations are not yet obtained. The author newly adjusted the preseismic and postseismic second order triangulation network together with the preseismic and postseismic first order triangulation network in the Kanto district and obtained the coseismic horizontal crustal movements. In this report, the results of calculations are presented without any tectonic inter pretation.
