FRE 
Pegan, Onata, and One They ar 
holly- furroun = ae ‘towards i 
eatt, a re'is a ae oe. Pegan is fituated 
about two miles al we Ge oe two, whi 
‘each other in aneaft and weft Saag 
were friendly, and.ready to exchan ei 
fall} pee of iron, aaa they’ valued igh 
the Indian copper colou th fine 
Smaig be ae which't 
roots from: their chin and upper lip. 
eae inne 
ae were continual plucking by the 
Their features are 
pleafing, anid-their teeth — white and e 3 they 
are of t mmon ftature, but fi ngolely i imble, active, 
and vigorous. Their r difpofition i is free and open, and they 
affociated with the crew as familiarly as if they had been - 
long acquainted. - On their waift they had a flight covering, 
which confifted of- fine matting. heir canoes are well con- 
cted, having,a hollow tree for the bottom, and plan 
for the fides, he fail of fine matting, a ad " outrigger, 
and good ropes andnetting. One of the inhabitants infiited 
on remaining with the mh s crew, W ay was named Jofep 
Freewill, from whom they learned that there were other 
iflands towards de north, whofe aoe nts had iron, and 
who always killed his countrymen saree they met at fea. 
he iflands were {mall and low, the larger not being more 
than five miles in compafs, to: biguae the ao gave. the 
name e of Fre ewill ifland. 8. lat. o? go’, E. long. 137? 
i: 
EZE, i in Archite Sure, oe middle icien of the 
entablature, feparating a cornice om e architrave. 
ts called i 
“he Reece is “fappofed to be intended to reprefent the 
heads ‘of the tranfverfe beams that fuftain the-roof or cover- 
An the Tufcan order, the freeze isa Phan flat member ; in 
the Doric it is ornamented with tablets, which are cut into 
Vertical, triangular grooves called tri ipa sand in the Ionic 
and Corinthian it isa ei furface 5 that of thofe i in the latter 
er is fometimes enric e peculiarities refpecting 
or 
the freeze will be as inde aie head of each individual or- 
der; See alfo Coz 
From ‘the variety ws _nvichments pradife on the freezes, 
they become varioufly denomin 
é 
oportion ialeaade of is » when draws on t. the 
In fome, the Sel is sly . the ov asin a confole.; 
‘in lead = bottom 
lands, or continued, as in the Tonic of. the gallery of Apollo 
im the Louvre: 
FREEZEs, se, are thefe adorned with baff-rélievos, 
h 
? 
reprefenting hiftories, ‘facrifices, &e. as | that of the arch of: e 
the 
omie.. 
s, Mariné, ave thofe reprefenting fea-horfes, tritons, 
cand. other attributes ue the fea : ¥ Or fliells, " baths,” grottos, 
Be 
_ an 
FREE » Refic, dre “thefe whofe oni are rufticated, 
or imboe 3. asthe T'nfcah freeze of Palladio. 
.- EEZzES, Symbolical, are thofe adorned with the ateates 
ef aay as the Corinthian of the cae ‘behind the Ca- 
a 
ted: 
ulv jaa d, are thole whofe profile’ 
*FRE 
» pitoLat a whereon are reprefented the inflruments and 
gi tse of fa 
ze a ae Capital. 
n Commerce, 
REEZEL LAND Pzax, in n Geography, afmall ifland i in 
the South Atlanticocean, near the coatt of Sandwich land, 
f Capt. Co a oo vered -it 
See HyporracHELion. 
-a kind of cloth or ftuff. See 
a 
RIZ 
in eos year mile S. lat. 59°. W. lo 
AND, Friezeland, or F vineland, bof in W ar, the 
ine with cheval de frife. 
FREEZING, denotes i pipes in nature, by which. 
a folid for ‘orm, as ice. 
a liquid, as alias 
>) 
o 
_ 
=e 
aq 
te 
3 
oD 
au 
ch 
~ 
gravity, fill. it the 
liquid ; it however gene ore pro ae contrary effect. 
Se have fuppofed that the heat a7 bod ies cae diminifhe 
ed, their particles are brought more nearly into. conta&, and 
thus the attraction of aggregation or igag ise is increafed 3 
ut inthe cafe of ileaaid and ice, w is tk e moft oman 
inftance we have, the very reverfe ei s place ; namely, the 
congealed body, ice, is of lefs denfity than the liquid ; 
what renders it {till more remarkable is,. that before’ the 
s nite from liquidity to folidity, a a gradual expanfion i is ob- 
ferved in the liquid itfelf during fome degrees of defeén ending 
temperature. - “More lately it has been. fippofed that a kind 
of polarity actuates. the molecules of liquids, and brings 
them, in certain cafes, to cohere more forcibly ; but this does 
not account for the pbeuomenaa oblerved i in <— to aie 
olum 
of v 
water, in the ratio ce - water is ex- 
pofed ina me e fulpended je jar. . or in ~All a air bee 20° or 30°, 
ay 2° or 3s below freezing ; but.if any tremu- 
ous motion a place, there appear inftantly a multitude 
of raat) hexanglar “fpicule, floating, and flowly afcending 
in the wa It is obferved, that the fhoots or 
cations of | ice at the commencement, and in the early flage 
congelation, are Pain at an angle of 60° or 120°. 
- Heat is given ing ie een as much ‘as 
weil vaife the papas val water 140° 
ifie 
34> 
aa 
a8 
° contains. sth. ‘Water is denfeft at ‘36° of the old feale, 
° of the new : from that point it ug expands ‘by 
online or by heating alike, according + 
2S 
nd water one the 
temperature oF o nae f the water be kept ftill, and 
on cold be not fevere, it-may be cooled in tee quantities 
0 25° or below,. without freezing ; saf pe water be confined 
aed b ulb of a thermometer jit is v ult to freeze it 
abo 
a T; 
Oo 
io] 
aa 
ce 
oa 
a) 
° 
— 
[ores 
a 
e 
“as 
