332
marine silts; bedrock; till; and gravel. From the class statistics,
a check was made on the validity of the training sets by examining
a plot of class separability (figure 3) which is a projection plot
of the decision regions used by the classification program. Also
examined was the divergence matrix ( a value of about 50 shows that
the classification was about 85% accurate for a particular pair of
classes) and the confusion matrix, in which a set of synthetic data
samples having the same spectral intensities as the training set
data, are run through the maximum likelihood classifier under the
multivariate normal assumption (figures 4 and 5)*
ki lometres
Figure 2. Study area, Arrowsmith River, N.W.T.
The results were displayed on full screen to check on
possible unclassified areas. The additional water unit was noted,
and at least one unclassified land unit. However, it was felt at
this
the
der
to a
all
ot c
ion
phot
the
ated