11 
sedimen- 
ed. For 
ne. 
ugh com- 
orn down 
upturned 
isolidated 
Piedmont 
tal Plain, 
ons of the 
n variably 
aracter of 
; Ridg< is 
;ed almosl 
is of reli( i 
i assigned 
>e of more 
extending 
eland and 
ntains are 
the Kings 
use of the 
these hills 
c highest, 
,o 700 i ,t 
other hills 
id some of 
in, in York 
he general 
and give a 
lain is thus 
ummarized 
gion, much 
s subjected 
of the land 
>y a contin- 
j ry slightly 
lie streams 
;agements of 
