4+ The ,N A T U I AlLi
tif it'itlefe M H will K fcôbt ïMo^âÉF^eniiPlgüI'éfe; %hêncè
pfëÔ&d not éfoffi tâeEM?s
xjifialtl that Iaï©‘di^V^My 'Iwiffiofli^ôcks SMit -that
lieideepier -inthe BôWe'ls o f the^Eattlli
X^fidèÿfirtiiiffireffit SpïiSgÿp
* b$3thë>sklf*f<ÿ
'FStàbWiè% •Whfëtl fquite
contrary Figü¥ê's ; lo'thàf Üh&^PM0ïhrM^?iï^§hh.è
Ghinfa<aef P m.% Rôtf#alt
it.ïelf <ihtô-:3ftfjî
'tai^.^Ûtç^ » r ^ V 'fi^ !'n ^ t e - f
SalthefsïM iW fu b fA nW o tà Ribek^ .&f'-Sàte yët%û#tftfj
if follows thèfefeîé? SP> thfeÿf WÊ not I faturated ëkhërfrêin
forai anoLtherrH^ntheié, r^ii4/coli(^êskltoSo^*t^fi®i3
ptëpèt' Faffîpmd fô
b y .ty à rioe si S o t o i o n â ^ ^ d J ir ip E e g ia tiô à ^ î Ük«ëpihg i iêti*
tinualCkOTlationjaÈdfoconftkntlf fupplying^sf*ria What
chkâyg^sMbabrage"tojtMs;;fisifhje'RenaitenQe oDMartne
Sdk/which S S prodigioùfly madèôüt by
count pfthbfeMôwntains^ Sait that&pply^^?â£i
MéfoftPtdmia^Medza3à ^ th o fe .yaftiEouaïÉkitesç
affirnts, èveryr-ÿeat Y^ëtatéSï and tfie^khte wheh&khê
Sait was digg’d is the Year follo.wingas fulfof Salt as before,
Ebfpaomena like to this .May? b&ehftrrd inflp
near Hejfe-Caffel, and .in thofe Iron-Mines belonging É|j the
Duke o f ' Florence, as ris related by, Fallopius- d|Belides. the
marine Salt thefe Springs do likewife contain the Mtrum
Calcarium : Its obfervable the Salt o f fonte of thefe Springs
willj fiot. eafily: precipitate, but a-,,little,vAlluM and frefh.
gutter will À e d it, and then if IWfkea a larger Grain and
ftronger Salt than any of the reft: In the Evaporation of
thefe.'Salts there is likewife obferv’d a white Sand, which
is thrown to the Corners of the Pan ; and this by frequent
Evaporation and Filtratiojtisl found to be the Particles of
the*%?>; out o f which thefe Saltdprings arife.
The
&c. 4-f
:! Thh kioft noted; Fur^^W aters-ïnthAk parts are tfhofe
in, s a Village!call’d Rott$&n*> adjaöéhbteithe iremarkaWe
Sands:\^hioh’ are the-.great Road into'Fmndccvnine’ Miles
in breadth, and atceaehj Spring-tdde-ëntirëlyr cover’d with
IM N i thefe ill calm Weather afFordi#Very pieafani Travelling/
but in tempeftuousSeafons ha lefs difmM, than wc
ca.n Tuppofe the wilddDefiirts of Arabia: >■ ;Ff oih the bottom
o f ah? high .Rookone^ thefe* the W^tendikes ».forth - in a
veryftplentiftft Current?,; itu is a •.lififlbfirackift,, takeifinf
wardly.it purges both by.Mri.oe aqdo&toolyand no doubt;
by.aidue preparation^ofJthe-Bpdyntbeyi become* extraordinaryavfenn
the <S curvy^Wbrmp^emndeiDigeftion's,. and
Difteihpers ofithatMadurej thë Watêz-hy Bg?ïpémi3h at the
the a Water: evaporates^ $here ?fuceeffir©ly arife^Eihniat
fifft- reddilh, uaindi afterwards ^ofylrrg®eyri£olou'r | thefé
Films will fecmënf >with4iahyriAoiri?iS^iè»Ht^^M®;lö5df
a natural alealio.üs
the tAncietftsbsithe Salfwliich remains aftéHEyapöfatioh;
feemSifö be a Marine, but|)y €requenr Filtraf iawand Gliry-
fta®i»^ibns,w l found ?it;#keydf@iconf ant’d a Eftsrspurgin^
WpÊkwhich is, truly TimMFen^XttrumCdktétumi and?®
thaf ^purgingfcialtH which •.iHip-ïègnaieé
MrfkaHsmd. Q^ertpuS^a%dWaterdin8Ê^ada^^^Mtiif-r
ed; abowe i..be^deö ^ei^n^diëre?likt^ii&lesikiAd
Earth,'%hichK;,w ill!, ferment rtwith <any>lAdidi3 When the
Water is evappratedto; a lixiviai Gêlpur, i f yon then, drnp
-hprn -inthir, i t ; iinhtddiaÈelyAiaiësia?0?^
gutom-i and jkecipita^eë 4«iwfaieh?Ph3öndmenoni(is (on^ ‘öb^
fervtble in thofeffWaterisi that contain FimharticUm'
Amorim» whichldeifionftrafekthat SaltnlkemfeÊl cöntaih
a natural Acid/ and ifin the1 like'Warpri ybufdippsaiip^tidr
Spirit, as that ofi dby&khffnfl
ceive-a yery.fulphureous find». xFroMi thefei^lfsi^ikin'
thefe Waters contain
Matron^ the Marine-»-, and-tibc GaffodmeumAmaruM}
K l likêf