( >27 )■ 
eu'^? any Alterations in the Air or Water after a 
Shockj^I could never difcern anything; particularly 
as to the Wind being raifed after a Shock, when it was 
calm ^«o*’\whKh fome reported, I could never per- 
ceive the leaft Difference. ^ 
One Thing I may add here, very remarkable, and' 
adiich may be depended on. About the Middle of 
April, that fine Sand which was thrown up in feveral 
*e firfl great Shock, 0^oZ>. 29,, 
a very great Degree, even id 
as to be more naufeous than a putrefying Corpfe • vet 
in a very little while after it did not finell at all. hL 
long it was before it began to ftink 1 am not certain ; 
I know It did not at firft, and I believe it was cover’d 
with Snow till a little while before : There is nothing 
Ground, throwing up Sand, flopping or breaking out of 
fenfible Evacuating of Air or other Matter pent up in 
the Earth, from the Surface of the Sea or Land adja- 
cnt to us, at the Times of our many Rumbles and 
Tremblings, we fhould have difeern’dit before now 
Nevihury is a Spot of Ground, and fo the adjacent 
Towns, very much inhabited and continually traveled 
over; and as to the Sea contiguous to thefe Parts, it is 
VV°f n ! but neither. 
^ u V ‘babble Eruptions or Eva- 
cuations been obferved that I hear of. 
P. S. Bojon PFeekly News Letter, Sept, y, 17x8 ' 
We hear from Newhtry and Rawhy, That they ' 
felt the Shake of the Earth on fuejday lafl abodt 
Four in the Morning; the Noife much like Thun- 
IV. J. 
