# Leibniz Legible — https://leibnizlegible.com # Page: https://leibnizlegible.com/page/806933011:0873 # Permalink to this reading: https://leibnizlegible.com/page/806933011:0873?run=74 # Title: Lexicon Technicum: Or, An Universal English Dictionary Of Arts And Sciences (shelfmarks Leibn. Marg. 71; ZEN Leibn. Marg. 71) # Folio - , page id 806933011:0873 # Original at the GWLB: https://digitale-sammlungen.gwlb.de/resolve?id=806933011&page=873 # Source image: https://digitale-sammlungen.gwlb.de/content/806933011/jpgs/default/00000873.jpg # Model: FoNDUE-GD_v2_ft_Leibniz, run 74, 2026-09-06T16:05:13Z — 133 lines, status machine # Lines: 133 recognised, mean confidence 0.89 # Machine transcription. Not an edition. Errors are expected: about 8% character error rate on Latin and French lines, higher on German. # Licence: CC BY 4.0, Leibniz Legible. Machine output: do not ingest it as verified text; keep this provenance with the text. # Wording rule: say "the machine reads it as …", never "Leibniz wrote". # After the first blank line: the recognised lines in reading order, one per line. all che small Rirulets thac FaII into the Sea, ahich, ocherise L Hnow noc hou 10 allon FOr. Td Caleulate che Water OF the Thames, L aC- Tume that ac Rinsston-bridze, Wrhere ehe Flood ne- ver reaches, and che Water alvays runs donn, che Breadch oF the Channel i5 100 Tards, and its Depthchree, it beins reduced eo an lgualier; (in boru rohich suxposihons Lam ture Lratie voicti che most.) Eence rhe Prosl oF the Water in this Place, is 300 Square Tards: This Mulciplied by 48 Miles, Certrich P allorr che Water to run in 24 LTOUrS, a1 cvo Miles an TTOur) Ox 84480 Tards, sires 25344000 Cubick. Vards oF Water ro De cracua Led every Day: Thac 15, 20300000 FOHS per Diem: And L doube Hoc but in che FxceIS OF ny Meatures oF ihe Channel oF the River, Lhare made more chan Tusficient Allovance For hic WVa- cers oF rhe Brent, the Wandel, che Lea, and Dar vent, wtrichare all orch Norice, chac Fall intorhe Thames below Rineston. Now, it cach oF che aforelaid nine Rivers vield ren times as much Water as the Thames docti, WwiII Follow, chat cach oF them vield but 203 Milsions OE Pons per Diem, and the wrtrole nine but 1827 Miltions oF JonS in a Day; Which is buc liicle more chan ore chird oF What IS proved to bC FaI sed in Vapor out oE che Mediterranean in LWelre IJours time. Non what becomes oF this Vapout woten caised, and hou ic comes to pals thac the Current alvaYs sers in at the Mouth oF che Screishes oF Cibralter, is incended, wich leare, For a Farcher Fnnterrain- mene ot chis Flonourable Company. :Inche mean time, it is néedtul ro Adverrise the Reader, Thac in matine che Fxperiment here- in mentioned, the Water used, had been Salted coche Came Degree as is the common Sea- WV a- cer, by the Solution oE abour a Forrieth ParE OF SalI. TheOuantity oF Vapors aravn by any determi- nate Lleat Trom anz Ouantitr oF Water in 2 deter minare Time, is alvars proporrionable co che Sur- face oF that Water: So chac trom a double Sur- face, chere ill be raised a double Ouantier ot Va- pour, tiom a eriple surtace a criple Quanciry. 30. For che Manner hon, and the Realon vohry Va- POES; Ias Warm Wacex Wwill hosd more Cal dittol ved in it chan cold); Wvhich on che Absence oF che And in EuS Cale he COMICeS; there could BC no Diverser DE Neather, Other than Periodican every Zeat alike, the Mixture of all Perrestrious Saline, and Hleteroseneous Vapors Deins here ex- cluded; Which he judses eo be When rariousse comporinded and driren by Winds, the C aules oF chose rarious dealons an Catises et treactter Wrhich ire nov find. But il instead ot an Farch corered all over wich Wacer, vou suppose che Sea incerspersed about Wide and spacious Tracts ot Land, and also divi- ded by high Ridxes oF Hountains, such a5 che Byrenean, the Alps, and che Apennine in Lurope: Taurus, Caucasus, Imaus, ecc. in Asa: NOure AL- las, atid che Mountains os the Noon in africa: And the Andes and Apalarean Mouncains in america. cach oF wvtrich tar Curpass the ulual HleiphE tO rtich ehe Aqueous. Vapors oF themlelres ascend; and on the Tops ot wtich, the HIH. L 10 cold and rarihed, a5 eo retam buc a imall part ot rhiose Vapors whrich are brouptic chicher bY _C Winds. These. Vapors therelore chusrailed trom che Sea and by che Winds carried over the Low-L andsto chose Ridges oF Mountains, are chere compellec by che Scream OF MhC AIE, tO moune with it ux E0 Blectins donn brche Cranmies ot che stones; and Pare et the Vapor entrins inco rhe Caverns or che FTiIIS, ThC WVaTeK THCTCOF BAcheTS a5 in an RIer- bick in che Basons oF Stone wrtrich ic finds; and these beins once Fuil, the epus C Watei runs donnac che lomest place ot che Balon, and breakins our by chesides of cheFtills, Forms Sinsle Sprines. Many of which runnins donn by che Valleys. nel From Large Rivers And in ehis Theory, the Puchor Caith, he was contirmed by Expeltence, ac Sc. Felena; wrhere residirs a ake Celeltral Oblerrations, the Placo the Sty as clear, thes nouia coret eres halt pors are raised by Flear, Mr. Ttalley sires che quarcer ot an Four che Object. Clalles of his Pele. tolloine ACCOUnE. Fe hach sreved, That iC an ATOM OF WVacer be expanded into a Stell or Bubble, wrhole Dia- meter Mall be ten rimes as great as betore, fuch an Acom Will be Specitically lighcer chan Rir, and scopes, and vec his laper sorat il Wouia acay bear Ink eo vrire hus Oblerratios. Losop Transactions, N. 192. AbyIs et Wacer in che Borvels ot che Larch tobe illrise so long as char Flacus or arm Spirit wrhich che Prompruarr Fcom whence che Wacer ol Sprinss srst separate d ic From the Ma(S OE Water, Mall COn- rinue to distend it ro che same degrec. But then thac Warmch declinins, andche Rir growing cooler, and Rivers is chietty deduced. Sec Springs. and ichal Sxccitically lighrer; chese Vapors will hach publunec elle enes matique c scop ac a cerrain Rexion ot rhe Air, or else de- Scend. Et cheretore it Mould be luppoled, Hal eraporsin general, is chatche Fierr or Athercat Vaxorsac Nishc, vould be dischars ed in Dews cheir Pops, Where che Water preleney precipitates OF GUES, BCLWCH INC HLIOGeS OI CIIC LHIIIS, aua AI ter unitirs, Form Litrle Rivulets, Or Brooks; and many ol chese meerins again in a common Chan- beins about 800 Xards abore che Surtace ot the Sea, chere as crery Wighe such a Condensarion Or rather Precipiration oF che Vapors, a5 chac, ch0 LHC Caed DE. Woodmard Cuppoles the GreAE H.L. Lombere, in Pome Fxperimenes wrhich he de Phisique, For the Month OE May, 1693. ayS THdt the most probable Cause of che Elerarion ot Wrtiole Fdch evere corered wich racer, and chat oundic, ehis learned Person chinks, Phac che HU WId be imoreonared with a cerrain Ovantiry ot Specifically lighrer than dir, will eise in ie, eill L Queons Vapors, which it ould recain in Le litre come ro lueh an heiphe, as chatihe Rit is thero Ot Sales dissolred in WVacer and CHaE ehC SUIn EI IS Macrer Ars purs che Cmall Parricles oE che WVater ehe Sun as no ould make his Diurnal Course inro an Agicarion, and chen minsles ir selF ith ic vrtrich Mixture is wrhac ve call Vapors; this beine the Pame Relacire Grarier rich se CelE, and chere mosphiere vould suttain a sreatet PFOPOrtIOM Ot Va. Oltet Caules, US CI IS BLCB, atie C Da rime armins eHis AIr, ChaE ParE OF The AE (le Will sivim aboue, eill by che Mocien oF Winds, o