Near the ground surface, components of the relative displacement, u', v' and w' on the crust are obtained by means of observations of three extensometers which are on these orthogonal directions, and four rotationmeters. For example, ∂u/∂x, ∂v/∂y and aw/az are observed by means of extensometers. Also ∂v/∂x, au/ay, ∂w/∂x (=-∂u/∂az) and ∂v/∂z (=-∂w/∂y) are observed by rotationmeters, ∂w/∂x and away are observed also by means rof tiltmeters, approximately. These observations have been done by using three orthogonal components of three extensometers (∂u/∂x, ∂v/∂y and ∂w/∂z), by using two rotationmeters (∂v/∂x and ∂u/∂y), and by using two horizontal pendulum type tiltmeters (∂w/∂x and ∂wl ∂y) in the old Osakayama Tunnel. These main strains, the maximum shear and three components of these rotational strains are then analysed every month. According to this analysis, the direction of these main strain has usually been in the prime vertical direction as well as those of the main stresses in most earthquakes in this district. The rotational direction has been to the east which agrees with the results of the analyses of the triangulations.
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