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- (EJ Cn Ee
le ay cg lf ame i
TT Co PE 12. CONCLUSIONS
Le i ¥ § ] Ey 6. 1% 14 2 | 0 Vias 3 Balice Nn
ls ET I} + 0 er 9 al : = 4 = Ra
2 NALCIE, LOC int ON, HASS: 2nusatt 5 0 Probably Balloon
Wl cars imme i ee SE S—— as tes al pai Sen — C1
Js DATE TIME BROUP | 4 TYPE OF OBSERVATION
| ns GU Foo ih LE Cravnde Ve cual Pp hy | 0 Was Airercft
Local 3 —— OH Ground-Vi sual & Eirsund-1s boar 1 Probably Aircraft
a AirVisval DO Air-Intercept | Radar 1 Poss sibly Aircraft
“PHOTOS 13. SOURCE Br —.
2 Yes physical spaciman
Possi Sly Balloon
= ee rE
|
|
| 5
1 -
ol
—
by ppd
Possibly Astronomical
— 0
<
a
ih
Ss
4
9
a
o
1
it
i | |
00
1
Doo:
LENGTH i CBSERVATION "9. COURSE
-—
tnsufficient Data for Evaluation |
Unknown
of
I/ &
110. BRIZF SUMMARY OF SIGHTING
A 30 1b. chunk of ice fell in Dalton, Mass,
Lhe area wassurveyed by an ALIC investigator
d there was no overhead object from whieh
whe 1ce could nave fallen. ‘the EBak Le
pattern was a fairly even distribution over |
an ares edt x 28's. The ices was analysed
and described as porus, or like rime ice,
clown
. COMMENTS
ATI has arrived at no cone i usion as
to the origin of the ice. fav
Cases may irdicate a ¢ |
will lead tO a conclusion.
| = STE. ELE = Eom mm em = —
FORM 329 (RZV 16 SEP 52)