ON SEISMOLOGICAL INVESTIGATION. 
TABLE I.—continued. 
195 
Date Correction Time Remarks , 
1895 M. 6S H. 
December 27 + 0 31] 3°50, 4:50, 4:45, 5:5, | Approximate time of sixteen 
7:5,7°10, 7:12,7°35, distinct displacements, the 
7°38,7°55,8°0,10°45, one at 10°45 commences 
15 50, 19:0, 20°45, gently. 
2171 
ay 2 eo 2 2 ; - a R No records. 
Dec. 29 to Jan. 18 no shocks. 
1896 
January 17 + 0 33 | 22°45 (about) Two vibrations. 
7 19 + 0 36] 1:0 5 Slight ,, 
3 22 + 0 46} 6317 Strong. 
9-701, the first of | Duration 30m. The third is 
five displacements a displacement to E., and 
the fifth to the W. 
55 24 + 0 55} 3°350, the first of | Duration 20m. 
seven small dis- 
placements 
1 25 + 0 59 | 22°50 (about) Vibrations. 
February 5 +1 16] 25 ~ Slight displacement. 
2°8 ” ” ” 
3:140 Decided shock. 
” 6 + 1 22] 0-707 Slight. 
4/190 * 
* 8 + 1 382) 1:952 Decided shock. 
ry eee + 1 33 | 2:0 (about) Vibrations. 
or 21 + 1 58 | 15561 Strong. 
17:0 (about) Three, the two second strong. 
rr 24 +1 55 Bi2be se Slight tremor. 
<3 28 + 1 23 | 15°805, the first of | Duration 30m. 
four 
20°25 (about) Slight. 
22 Saar four | Duration 8m. 
displacements 
March 1 + 2 10} 9:0 (about) Slight. 
a Ld +2 0} 4000 Shock commences; max. 4m, 
later. 
PlG: vs +2 0} 5-548 First of three very slight 
shocks. 
ye 22 +2 53 1191 First of two very slight 
shocks. 
2:309 First of five small shocks. 
Up to Mar. 27, whencircum- 
stances compelled me to 
cease recording, there were 
no more shocks. 
After comparing ‘sudden’ disturbances and decided ‘shocks’ noted in 
July 1896 with similar records obtained at Carisbrooke, it is seen that 
these do not coincide in time. Therefore these movements, which appear 
to be so frequent in the winter, are extremely local in their action, and 
cannot be regarded as earthquakes. What they mean is at present 
unknown, and it will not be until two instruments have been installed 
near to each other that we can speak more definitely regarding their 
cause. 
Because the lists given by Dr. Agamennone, which include, with the 
earthquakes of Turkey and Asia Minor, those of Italy and other Euro- 
o2 
