4, 
108 Mr D. Milne ox Earthquake Shocks in Great Britain. 
at 2 3 |4.| 3.14 3. | 4. 2 Bio Si | 4a en Bele ss. 
1840. 1841, 
Feb. 26.;/1)1 a.| 1 Feb. 16, | 1 1 
March 8.|2]|6 a.|1]4 pP.| 1 March 6. | 1/9 a.| 1 
nia Oia Tel Sas, 8 cap 1 hd 48 |B 
sxe) CRIME Ome Ae | be Ge als |p Le SE ae an 
wee loa Pins. wee |S TO Re] WE fa} 
ce LD OP ee lS a er ee 
sane, A LA ARO. | lf April 3. 1s) Bia. jal 
eae 2 | Oe An HEL CAS | OL ogee as | 
nae sea eae See 2 aa Bs ald 
a OF.|2| lav] 1 | 2br.| 1 ag gs a 
April 1.}2)1 p.|1] 13P.} 1 1) Nea ye da. | 
Se elee WA ee. 116) 4ee. eyo me 2 OA || 25) 98 0 | ee ore oe 
wae PDF ale wee DB AO Te wae 
ses mala elal eaL ni leave uO ea 
ee i ha bal ba alae © ne 2 ob 
May 19.|3]1$p.]}3]r.m.] 1) PM] 1] — 22. 1 1 
Bees OO | eA ll Dae aces I oecs, eceaa ae 1 
July 3. [VMN ait hake aT aH Ohi we lot 
es LEG UL Asli [ee Oe Ls oA OL 
we 16, / 2] 3ha.] 1 | wm. 80. | 1} 6$a.] 1 
me lve | oes. |e June 29. | 1 1 
on BE ta July 2. | 1| 5ga.}1 
Aug. 5.) 1/6 P.| 1 wx. 30. (12]8 a.| 2|2hP.| 8] Sip. 
PO 1 Sgt (el peer id espe 2 Lal SIN bts aN [4 it 
Sept. 19.] 1 | 244.] 3 Aug. 1. | 2 1 1 
Se, eli |e) | oe LL PEAK 4 1 1 
new Gs | aba ease ae 12) LO, A. 
Oct: S4e | b)|19e.)|/2 eke 2290)" | 1 
won $20, PED a LI I Sept. 8.|2|3 4.| 1 
wm BBD | CR. | 4 cil ign MVE eh 
Nov. 12.}1 | 25 P.| 1 w. 10.) 8] 24a.] 3] 4$a.} 1 |llpa 
a NE GP I Ey a DP geen A.| 1 | 94P.| 1 
te Ge enor Anak G. Ag aL Pettit Wy eal lie (ea Lane bea af 
Ek ET re ett 92 NA IVE | 
Dec etnias een] ak ee 935 | Et Se ani 
as ifr 127 A.) 2 — 29. 2 Ad leh 9} A.| 1 
Bas 8. | 1 |12 a.| 2 Ocho ocn | 
ane MELD en DB ai UG | Dia takts 
ao or Lja.m.|1 Nov. 3,]1 {12 a./1 
exe. al Be RG Le AS 
RA AS: | 2 ae naw Gi] 24), 82a. 
1841 awe Wael 1 
san. 6. 2): sed) 1824) 0 
et ed ee Ae |) I Sees Nk eS) Ale 
—. 81.|3|73P.|1]9 v.| 1 |llgr.| 1 ]} Dec. 3. SEA. 
Feb. 1./1 1 cat G Pl [seas el 
ww «14,14 Of 4.) 1 cei 7-al Laon Asie 
The 4th column in the preceding Table, which states the 
intensity of the recorded shocks, cannot be depended on as 
absolutely correct. It represents merely the result of Mr 
Macfarlane’s impressions, aided, however, in most instances, 
with observation of the effects of each shock. It is also pro- 
per to observe, that besides shocks or tremors, there were 
frequently passing sounds, unaccompanied by shocks or tre- 
mors, and which are believed by the inhabitants of Comrie, 
—and apparently on good erounds,—to be no less connected 
with subterranean action. Of these sounds, a register has been 
