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T
h
S
h
N
si
g
h
is results i
Line-by-
l
appear i
n
taken wi
t
the seco
n
displays
(see Fig.
Fig
.
th
The
Res
t
(see Fig.
Fi
h
ould the s
c
N
OTE. Duri
n
g
nal collec
t
n the follo
w
l
ine scanni
n
n
the 2D V
i
t
h the
Sens
H
n
d one sh
o
distributio
n
7-90);
.
7-90. Imag
e
e surface p
o
t
art
b
utton
7-91).
g. 7-91. Co
n
c
anning pr
o
n
g the seco
n
t
ed at the fi
r
w
ing activit
y
n
g of the s
a
i
ewer of th
H
ei
g
ht
sig
n
o
ws variati
o
n
of the z
-
e
s of surfac
e
o
tential (low
e
becomes e
n
n
trol panel o
f
o
cedure be i
n
n
d pass, in
p
r
st pass.
y
of the sys
a
mple surf
a
e scan dat
a
n
al (the first
o
ns at the
-
componen
t
e
topograph
y
e
r part) over
t
n
abled and
f
the Scanni
n
terrupted,
p
ut of the f
e
C
tem:
a
ce starts a
n
a
. Two of t
h
one uses s
c
backward
t
of the s
u
y
(upper part
)
t
he surface
o
caption o
f
n
g
window i
n
click the
S
t
e
edback is t
a
C
hapter 7. P
e
n
d three i
m
h
ese image
c
an in the f
o
movement
)
u
rface grad
i
)
and spatial
o
f a LB bico
m
f
the
Run
bu
n
the cours
e
t
op
button
o
a
ken from t
h
e
rforming M
e
m
ages of th
e
s reveal th
e
fo
rward dir
e
)
and the
t
i
ent (
Surf_
distribution
o
m
ponent film
u
tton chan
g
e
of scannin
g
o
r use the <
E
he profile
of
e
asurement
s
11
7
e
scan are
a
e
landscap
e
e
ction whil
e
t
hird imag
e
Pot
signal
)
o
f
g
es to
Sto
p
g
E
sc> key.
of
the Sens
Z
s
7
a
e
e
e
)
p
Z

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