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and
and in resp
quit
xacting as b
r l s suit it b
and ma
sam
d
v
lopm
nt
h in h eavy soils and in f r ost localitie s
b
ec
The ste
n of
r ativ
compa
ly low d o wn
a fa
o urable locality
soils it sinks d o
r g
and la
crown
strong
id
It grows somewhat quick
years of lif
h an
t
fe
t
Its volum
h
r is ho r nb
beec
no
H
ornbeam comm
about
y
a
r ate every ot h
at any
by s
d is on t
r oduction f r om
rep
r at
appea
r h u
r eds
fo
d
r din
polla
H
r nbeam appea r s in pu r
o
also in
ngland (
its capacity fo
h te r fo
a lig
and does not
ct of min
ch
st
h
tim
it is fo
and on heavy clay soil s
h o r nb
app
n to an in significant tr
h e r oot syst
T
r oots whic h r
r a r
but it
increm
nt is co
am as long liv
nces b
r s old
and it s
r
h e w h ole g r
r t w
h h as b
pa
ic
years
ppi
g
r imp r oving t h e f
iag
does not maintain a cove
so much shade
H ORNB
AM
r al
L
oams
sandy soils rich in
r
it attains its full developm
nd on dry soils
am is g
nerally divi
h e s h ape
T
r oach
h at of
s t
m is no t d
ach a mod
r than b
ly r
aches a to tal heig
siderably small
d as t
P
aring full crops o f se
eds plentifully alm ost ev
r
h at its pow
ea
t
at
stool is exc
en coppic
r ee is emin
the t
woo
s in
orest
It is not
r tility of the soil
att
r in the soil it is not
h
thoug
it freq
ntly
d into branches
tr
e
b
ch on inferior
h a s h ort bol
wi
ep going
r ate dep
h
ech during the first
r t
h e b
h
ec
r
ll
nt
d
ntly suited for
astern
qual to beech in
r ov
rhead so long
leaves al so d
h umus
nt
r
inferio
r
plac
s
if grown in
h
r
t
h t
m ore
h an that
h en
d w
r y y
r
a
r oduction
p
h oots
s
stools last
r op
u
and
h as
i
ce it
compos
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