EQMNrNlCATED.
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B.L.iiNls5 lt,UM.Ai oOoH.NAL. M D.


ADDRESSED BY PEER coABoUr TO HIS COUSIN


JOB srAYAruoAlE,


Since have arrived On this island, have
bestowed considerable attention upon the
examination OF It's agricultural resources and
capabilities | should Judge that it contain
Cd Il gtcaicr potion OF arabic land, and more
rIcn, ioamy earth III proportion to lis SIZE,
t..an the others OF the group, or gcolog'caiy
speaking, tAs island appe~Is to be Older than
lis more eastern sisters, or has been tor
much longer period fee from any volcanic
action, Wh.ch mas gwen time tor sol to form,
By the actioa oi the weather upon tue irlabIe
crust OF volcanic countries Age after age
mas accumulated It's successive deposits, OF
mineral and vegetable decay Until all the
more recent and violent traces OF the action
peared and lett IN their places, fine prairie
like meadows, or thickly wooded uplands,
some Of which betray their origin by their
cratertorn shapes Koloa alone at this day
oOdSS ol Il DOIa nue. crater, when however
is extinct, 1t is conical SHAPED, and its
rough and jagged sides form the abode OF
numbers OF "hd goats Its situation is at
It's southeastern extremity, il short distance
rom the shores, all OF when IN that 'mhe-
date region tallaAe OF It's c'aggy and pre-
c,p'io"s nature. The lava IN lowing from
1t, formed on all sides ii rocky led, the sur
lace OF which III is close vicinity is broken
up INTO thousands OF piles OF small but sharp
pointed rocks, particularly gratifying to
goats, but not equally SO t. their owners
when IN chase OF them The earth here is
p'eFced IN every drect'on by labarynIh'nc