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or ice better
trees are liable to be th
under eith
r of the previously mentioned two syst
only be proved by actual stati stics in
syst
m a
ord s the m ean s of p
r ds
as
towa
placed comparatively free for a considerable number of years
This is doubtless more favourable than under the
wood compa
r
sh
te
d
acco
a n even state of moisture
r es t is
The fo
r emoval of single t r ees o r small g r oups s
the
r
ther
ove
out the whol
part of the w
r old to
y
a
single tr
es o
h e
t
r the w h ol
times ov
r
r est is divided into a numb
eve
fo
gone over in tu
a ft
r t h e lapse of seve ra l y
only
V
iews dif
tion for
sts
r eviously mention
the two p
I L VI
xcept during regene
r o
P
end of the rotation
r tm
nt system
panied by a mo
H
LT
R
reated
under the shelter of the old c
h ol
w
area
length of the rotation
h ole fo r
st is ever at rest
oldest
r small groups
ork of s
lecti
ext
r n
so that cutting return s to t
r som
h at r egarding the extent to which selec
w
exposed
T URAL
UL
r ation
n by wind
r oducing valuable large timber
as the soil is more ca
r e complete preservation of
L
h is process goes on t hr ough
and t
are constantly r
ov
r the whol
r
g t
es for cutti
nt of the fo
r s
a
r nal dange r s
exte
h
d s
lt
r
T
M
when t
r o r smaller than
r se of time
cou
the fin
st trees c
TI ON
Y
T
l
cted h
h at p r actically
so
class
r e sented
p
r ea
a
g extends at all
r e st
r ac
In p
r o f blocks
h e same par
a s compared wit
wood syst
ms
h e sh
lter
ms
can
the
a n be
h
lter
r efully
M
r op
by
r e and
s
from
and
heo
ice
how
h
w
ic
h
h e
t
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