Lexicon Technicum: Or, An Universal English Dictionary Of Arts And Sciences, fol. -
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- SPRINOS and Fountains. Concernins che) we ulually (peak) in like tranner as by au Alem-
- Origin ot thele, chere is much Dispure, especially
- ot fuch as are found on che cops ol high Moun
- FaiHS.
- Some, ad Dr. HOOk, DF. PlOrt, ard many OrterS
- chink chac cher arise trom the Sea-arer percolared
- Chronoh che Bovsels oP che Parch, wrhich by char
- means being deprived ot ies Salc, is rendred muct
- Lishiter chan betore, and (0 is capable ot Rilins ux
- coche heiphe e commoniy find Sprinss at, 25 W a
- ter Lises in a Filere, or in verr (mall Tubes
- 580.
- And DI. Hlook hach a precy Experiment aboue
- chis, in luS MioroEr. p. 25.
- But L CanHOE seC how by this Fypochesis, sux
- Posins che Craries ot che Whole Aunosphere coutd
- bc caken oH, Wacer can rile abore 34 Or 35 F002
- abore thelerel ofthe Ocean.
- The Learned CapE. Falley suxposes them 10 bC
- cauled trom che Vapours exhaled by the Sun our ot
- the Sea, 500. OF which, sec an Accoune under the
- Word Vapour
- The Ingenious Dr. Woodmard, in his Nacurat
- Elistory ot che Larch suppoles, Phac the Great A.
- byIS OF Wacers, placed in che Borvels oF the Farth,
- is che Randins Fund and Prompruar which sup
- plies Wacer roche Surtace oE the Farrh, and furni
- Rain.
- For he aNerrs, Thar there is a nearly uniform,
- and constant Fire or Flear, disseminared chro our
- the Bodr ot ehie Farch, and especialr in rhe In
- ferior parrs ofic: The Boctomsof the deeper Mines
- beins verr Culter, and rhe stone and Creschere be-
- ins verr sensibly hoc cren in Wincer. Thac rie
- Ehis Subrerraneous FTeac Which craporares and ele
- vaces the Warers of che AbyIS, buoyins ic ux indit.
- ferenely on all Sides, and torards all parrs ot the
- Surtace oF che ClobC.
- Thatchis risins Vapour, er Wacer, perrades noc
- onty the Fissures and Incerrals of che Strata, Bueche
- very Bodies oFche Strata chemselres, permeatins che
- Incerstices oFrhe Sand, Parrh, Or OcherMatter, WHere.
- oE ther consist; vea, eren che most firm and dense
- Marble and Sand- Stone; For thele sire admission
- to ir, cho in lesser Ouantier, and are alvars tound
- Pacurared wich ic; wrhich is che reaton chac ches
- are Potrer, and can be cuc muchmore casil when
- they are first taken out oF che Farrh, than chey can
- afterwards, Wrhen they have lain Come time expo.
- Sed cothe Rir, and wotien chat FTumidity is cvaxo-
- rated.
- This Vavour he aleris to procced directI7 up 10-
- wardsthe Surtace ot rhe Olobe, on all sides, untels
- wvhen impeded aud direrred by the Incerposirion of
- Scrata OF Marble, the denser TOrrs OF StonC, Or O.
- ther like Macrer, ertich is so close and compact
- thac it can adinic ic only in a smaller Ouantir, avd
- Ehis very NOWlY 10O.
- And Wrhett IE IS thus incercepled M Les LaMase
- ehe Vapour, Wwhich CANHOE penetrate the Stratum
- dircctIY, will some of ic olide alone the lorver
- Surface oF the Stratum, permearins the FIorizon.
- cal Incerral, erhich is becrise char and the HeXL
- Stratum lyins underneathic; the rett vill pals che
- Incerstices oF che Mals ot the subjacene Strata
- wrtiecher cher be of laxer Sconc, ot Sand, Marte
- ex che likre, Wrich a Direction parallel to the sice OF
- those Strata, eill ic arrires at cheir perpendicular
- InterVaIS.
- And wrhen che Nacer is once come rothese Inter-
- vals, in case ehe strara, Whereby the ascending Va-
- bick, happen to be raised abore the Levet oF che
- Farrhs Surtace; 25 those Strata alWaYS aIC, WIICIC.
- dikervise sor abore the laid Level, Rows forch ot
- thole Incerrals or Apertures; and it chere be ne
- Obstacle withour, Forms Brooks and Rivers. Bur
- trtiere che strata, erhich (o condense il, are nor
- hisherchanche mean Surtace of che Carch, it Ata8
- vares at the Apertures, and ontys forms standins
- Sprines.
- the AByIS, be continual, and neariY the lame at al
- Sealons, and alike to all parrs ot che Globe, ver
- When iE arrIVCS aE OF neaE The Surface Os the Lart
- Where the Fleac (the Agent wrhich craporates anc
- DearS IF UP) iS not so constant and UHIFOrm, a5 ic
- thac residene wichin che Globe, ou lo uoscctor
- cissitudes and Alterations, being ac certain Scasons
- sreater chan at orhers; being also greater in Come
- Climares and ParEs oF che Parrh chan in Otters: L
- thence happens chac che Ouancier oF Water at the
- Surface of the Carth, tho PenE up From the AByP
- Wrich an almost constane equalier, is varions and un
- certain, as is che Hlearthere ac some scasons, and ir
- Some Couneries, the Surtace aboundins, and beins
- even dromn d rich che Plener ol ic, che Springe
- Full, and the Riverstigh: AC otber Seasons, ad it
- other Couneries, both Sprinss and Rivers may be
- exceedinslon, and Cometimes rorallr fail.
- Wrhen the Feat in the exteriOr parES OF the
- Farch, and inthe Ambiene Air, is a5 incense 25 chac
- in the incerior parts oF ic, then all Chac Water Which
- passes che Strata directly, mouneins up in separare
- Parcels, or in Form ot Vapour, docs noc Aop a
- the Surtace, becaule the Flearthere, is equal borh
- in Ouantier and Porver to That underneath, Wrhich
- broushr it out oF the ABY(S.
- ThisFlear cherefore ralesi Hete, anid bears it up.
- parr oF ic immediately out ac che Surtace of rhe
- Farch; the restchro che Tubes and Vessels oF che
- Vegerables which grow thereon, LTerbS, Shrubs
- and Trees, and alons with ir a Porr of Vesetarire
- Terrestrial Marcer, Wrtich ic deraches From out the
- uppermost scratum whereinthese are placed; this
- UE depoles inthem for their Nurriment, as ir passes
- thro em, and issuins out ac their Tops and fixtre
- miries, it marches Aill on, and is elerared up inte
- the Armosphere, t0 such an heistu, chat the TPeat
- there beine less, it becomes condensed, unites ane
- combines into (mall MaeS, OF DEOpS, and aF
- lengih falls donn again in Rain, Dem, Pail, Ox
- Snom.
- And For the OrHer parE OF the Warer Which vras
- condented at the Surtace of the Farth, and sCnE FOKFI
- collectirels into standins Sprinss and Rivers; this
- alto sustains a Diminution trom the Fleat abore.
- beins craporated more or lels in proporrion rO che
- grearer or lesser Incenseness of the Lleat, auu ie
- Srearer or lesser Exrent oF rhe Surtace ot che Narer
- lo Tene Forrh.
- And as chese Fraxorations are et sometimes grea-
- ter, accordins ro the grearer Lleac of the Sun, 10
- vohere ever ther alI Ca aML LII LLaHI, IIS WW MMUCH
- asthe suns Porver is then luperior to IIS LoWvetI
- tallies much clsctet and taller chac ac ochet
- pout was colleced und condented ino Wacer, (25 )civres.
- OF Mountains do consist; then che Water, beine
- Hle adaS, That tho THI SUPPI) OL Wacer trom
- superior in Ouancus Wo the Rain of colder Scalons.
- Those Seasons: Lhis is apparene in our Northetn
- Clime, Wherece Sos Loets eet rets sica
- buc sel our Rains in fune, Fuly, and Ausust, are
- much sreacer than thole of the colder Monchs, che
- Drops larses, and consequently hearier, ana
Cite
Lexicon Technicum: Or, An Universal English Dictionary Of Arts And Sciences, fol. - . Machine transcription, not an edition: Leibniz Legible (model FoNDUE-GD_v2_ft_Leibniz, run 74). https://leibnizlegible.com/page/806933011:0774?run=74