# Leibniz Legible — https://leibnizlegible.com # Page: https://leibnizlegible.com/page/806933011:0109 # Permalink to this reading: https://leibnizlegible.com/page/806933011:0109?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 806933011:0109 # Original at the GWLB: https://digitale-sammlungen.gwlb.de/resolve?id=806933011&page=109 # Source image: https://digitale-sammlungen.gwlb.de/content/806933011/jpgs/default/00000109.jpg # Model: FoNDUE-GD_v2_ft_Leibniz, run 74, 2026-09-06T16:05:13Z — 126 lines, status machine # Lines: 126 recognised, mean confidence 0.90 # 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. 2. A lecond Cause is the uncertain extalation) an, on chis Gidethe 3STh degree OF North. Laticude and Precipicarion of Vapours, lodging in che AIc, che Westerly and Soutis mesterly Winds blon alinoc Whereby ic comes to be ac one cime much more alwazs. Trade; (o char whenerer here rhe Winc erouded chan ac anorher, and conlequenely hea- comes up ac Fast and North-Fast, eis Cure rO bC vier; bur chole larrer in a grear meature depend checkd by a contrary Calc, as loon as ic reaches uxon the former. Now from chese Principles, he che Ocean; Wheretore accordins co wtar is made explicates che several Phaenomena oF che Baro- our in the Second Remark, the sir must necds be meter. heaped over ehis istand; and consequencty che P. Urhy in Calm WNeacher, che Air beine inelined Mercury must Mand hish, 25 osien 25 ihese Winds Eo Fam, the Mercury is commonty lom: blon. This holds eruc in ehis Counery, bur is nor Thac ihe Mercurys being lo, is an Indication a general Rule Por orhers; wvhere che Winds arc OF Rain, becaule the sir beine lighe, che Vapours under disserent Circumtances; and he hinselt are no longer supporced chereby, as beins become specitically heavier chan che Medium Wvherein chey Aeaced; lo chac chey descend rowards che Parrh, and in cheir Fall meetins wich ocher Agueous Par. ricles, chey incorporare cogecher, and torm sitile drops oE Rain; bue che Mercury S beinS AE On cime lover chan at anocher, is the ettect ot LWO concrary Winds bloming trom che place Wwhere che Baromoter Rands; Whereby che sir ot char place is carried boch rass trom ic, and consequenily ehe Incumbene Cylinder oF Air is diminithed, and hach Comerimes seen che Mercury here a5 low 25 2c Prches upon an Casterty Wind, bur. rhen ic blew ex ceeding hard, and (0 comres to Be accounred FOr by whac mas oblerred uxon the chird Remark. 5. WB. in calm frosty Weather ehe Mercury Generally stands high: The cause thereot is, ThaE it seldom FreezeS buc wvhen che W inds come ouc ot che Northern and North. Fastern Ouarrers, OF at least, untess chose Winds blow ac no Great distance oH, For the Nor. thern Parrs oFGermanr, Denmarke. Siveden, Normay accordinsly che Mercury sirLS; a5 For instance, it and all Thac tract (tom whence North-F asterr in the erman Scean ie Moula blo 2 6alC ol Westerly Wind, and ac rhe same rime an Pasterty Wind in the MB Sea; Or it in France it Moald blow 2 Southeris Wind, and in Scocland a Northern, i must bC Stanced me, chac chac parr ot che Atmo- spdere svendane over England, vould chereby be exhauea and artenuated, and che Mercurs vould lubu, altet the Vapours Wilch betore Roared in thole parrs ot che sir of equal Graviry ich checcletres, vould sink eo che Larcti. 2. WVoy, in serene, 500d, serrled Weather the Me- cury Is generallo bigh: Thac che preater heiphe bt the Barometer, is occationed by rvo contrary Wrinds blowine comards che Place ot Observacion Winds coine, are luibject co almost continuat Frolt alI che Wincer; and chereby che lover sir s is very much condensed, and in rhac Hace ic brouxhe hirherwards by chose Winds, and beine accumulared by che Opposition oF che Westert Wind blowins in che Ocean, che Mercury muR necds be prest to a morethan ordinary heiphe, and 25 a concurrine cause; the Mrinking oF the lover Parrs ot the sir inco lesser room by cold, must needs cause a delcent ol the upper Parrs ot rhe A1. mosphere, ro reduce the Cariry made by chis Con- traction eo an Equilibrium. 6. Troy, ascer very ereat Storins of Wind, when the Nercury has been very lom, Et generally rises a- whereby che sir oE ocher Places is brouglit chicher, sain very fast and accumutaced; lo chac che Incumbent CfIn This he cells vou, he has frequeney obserred der oF dir being encreased borh in Fleighe and and once found ir rilen an Inch and a halF in lese Weiehe, The Mercury prested chereby, mute Mells rise and ltand high; 25 lons as the Wines conti- nue s0 loblo; and chen che sir beins lpcenical- chaM SiX LIOUES, after a lone continced Storm ot Souch: WVest Wind. This scemsro be occasioned by che ludden accestion ot nem sir to supply the great Iy hearier, che Vapours are berrer kepe sulpend- Fracnarion erhich Tuch concinued Scorms make ed, (o char chey hare no Inclination ro precipirare, chereot in chole places wrhere cher happen, and b che Recoil ot the sir, atter the lorce ceales char impelled ic; and che realon why rhe Mercury riles (0 fast, is, becaule the sir beins very much ra risied berond irs mean Densry, che neighbourins sir runs in the more (witely eo bring it t0 an C quilibrium; a5 We lec Wacer runs che faster For havins a prear Decliviry 9. WBy. in more Norcherly Places the Variations of the Baromerex are creater than in more Sou- cherly: The Fruch oF ehe matter OE fact is proved Frorr Observacions made ar Clermont and Paris, compa nOt come in (0 Fast 25 t0 supply che Fracuarion red wich ochers made ac Scockholm, as may be lcer necessarily De acrennared when and where the Paid libre des Liguers. The Reason seems 10 be, that etie miore Northersy Parrs have ulually greater Scorms oE ehe Northerty Winds brins che Condensed and Pole, and char again beins check d Hy a Southert ind, ac no ereat distance, and lo heaped, mus ot necessiry make che Mercury in luets ease Aand histier on the orter extream 8. o neut he Egunoetial, as at Barbado and St. Ielena, ibere is verys little or no Variation and FalI donn in Drops, wtrich is le realon ofche serene bd Weacher wwtrict allends rhe Breater heiehes et che Mercury. 3. WVoy, upon very creat Winds or Storms. soue accompanied mith no Rain, the Mercury sintes lomest s auu with relation to ebe Point os ist Coipass upo3 hich the Wind blors. This is caused by che very rapid Morion oF che Sirinthele Scorms; For rhe Praet or Region of che Farchs Surtace wherein chese WindsraGC, HOE CX cendins all round che Globe; chac Scagnane sir. wtich is sest behind, as likrewise on che Cdes, Cal- Winas comtinue eo blo, and that more or lels ac. 25 IC 15, may in all probabilies cake oH lome part ot the perpendicular Pretture chereot; and che Ponderous sir trom che Neishibourhood ot cho Brear ABllation oF is Parricles, is che reaton Wohy the V’apours are distipaced, and do nor condemte into Drops, 10 as totorm Rain, ocherwise che n2 Cara Consequence ot the sirs Rarefaction. 4. WVoy, caereris paribus; ihe Mercury stand hishest upon an Casterty or North. F. asterty Wind. made DV 1 lwite a Currenc, (0 char che sir must in che Appendix 10 Mr. PascalS BOOK. De l’Lqui cordins co cheir Violence. Add ro itich, chac Wind chan che more Southerly, wtrereby che Mer ehe FTorizoneal Morion oF. the sir, beins (0 quick curr Mould sink lorver in chac exrream; and chen Ehis tvorere becauite hac in be Alantiet deea ses ehe tteissties ie aometer