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Table 2 Instrumental parameters and determination of M s at two stations Göttingen (GTT) and Uppsala (UPP) from the E and N components of horizontal Wiechert instruments: T 0 free period, α damping factor, V magnification, pol. polarization of the instrument, drum speed of the smoke-paper recorder, Δ epicentral distance, Az. back azimuth, B maximum amplitude on the original record, T period at maximum amplitude, M s surface-wave magnitude

From: The 1905 Chamonix earthquakes: active tectonics in the Mont Blanc and Aiguilles Rouges massifs

 

Station

Comp.

T0 s

α

V

pol.

Drum, mm/min

Δ

km

Az.

B, mm

T

Ms

1

GTT

E

15.3

0.46

180

14.9

653

18°

13.5

10.0

5.5

2

GTT

N

15.7

0.46

200

14.9

653

18°

3.6

9.3

4.9

3

UPP

E

9.4

0.38

187

+

14.5

1690

21°

1.1

8.5

5.1

4

UPP

N

9.8

0.38

188

+

14.5

1690

21°

0.7

7.8

4.9

  1. Parameters are from the station book notes and polarities refer to the ground motion. Charlier and Van Gills (1953) report polarities referring to the mass motion, which are opposite to those given in the present table