e th
e
fireball,
the melted
sand behaved ju
st as wate
r does in a regul
ar cloud: t
iny drople
ts aggregated
into bigg
er droplets that became too
heavy to remain
suspended and f
ell as a rain of molten glass.
"Much of the layer
was formed not on
the gro
und but by a rain
of material injected into the fireball that melted
, fell back, and
collected on the
hot
sa
nd to form the ob
se
rved puddles of Trinitite, especially within the radius of the h
search engine
by
freefind
advanced
ottest part of the event," the study concluded. "After falling to
Next Month >>
the gr
ound,
the to
p surfa
ce of the
Triniti
te lay
er was
s
t
hea
ill
some
ted
t by
wha
t
fire
he
IRTB
bal
and
l
thus
(A)
elope
dev
d
IRTB
a
oth
smo
face
sur
"We
."
lcula
ca
t
an a
ed
age
ver
ebal
fir
tempe
l
ratur
(B)
e
IRTB
of
430
8,
vin,"
Kel
they
(B)
r
e
po
rt
ed
.
T
ha
t'
4,71
s 1
egree
0 d
PRSBI
s F
ah
heit
ren
The
.
new
(C)
eory
th
lains
exp
t
IRTB
he
y s
tin
IRTB
(C)
res o
phe
PRSBI
f g
la
ss f
(A)
d on
oun
e as
sit
ops t
dr
coo
hat
le
IRTB
d a
hard
nd
d eno
ene
to k
ugh
ee
p
23
ir
the
sh
whe
ape
hey
n t
the
hit
g
nd.
rou
also
It
ex
(C)
pl
s wh
ain
here
y t
s Tr
wa
in
te f
iti
d on
oun
28
to
p
o
f
t
he outer
edges of th
e asphalt used
aroun
d the 100-foot tower
and on
some objects
left in the g
round zero
area.