# Leibniz Legible — https://leibnizlegible.com # Page: https://leibnizlegible.com/page/806933011:0276 # Permalink to this reading: https://leibnizlegible.com/page/806933011:0276?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 806933011:0276 # Original at the GWLB: https://digitale-sammlungen.gwlb.de/resolve?id=806933011&page=276 # Source image: https://digitale-sammlungen.gwlb.de/content/806933011/jpgs/default/00000276.jpg # Model: FoNDUE-GD_v2_ft_Leibniz, run 74, 2026-09-06T16:05:13Z — 143 lines, status machine # Lines: 143 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. That as ehie Waret resident in chie Abyss, i5 in aII Parrs oF ir, Aored wirh a considerable quanciir oF Fleac, and more especially in thole where chele ex- traordinarr Asgresations oF ihis Fire happen, (0 likrevise is the Wacer Wtick is thus Forced out ot ic; insomuch, thac when chrovn Forch, and mixed Wwich the WVaters OF Wells, OE Sprines, OE Rivers, and the sen; ic renders them verr sensibly hor. Thacir is ulually expelled forth in vast Onanri cies, and rith erear Impecuosier; insomuch chac it hach been seen to spour out oF deep Wells, and Ay Forth at the rops of them, uxon the Face oF che Cround; Wich like Rapidier comes ic our of thie Sources ot Rivers, Allins chem (0 oF a ludden, 25 to makee etiem run over rlieir Banks, and orerAow thieir Neizhbourins Terricories, withour (o much 25 one drop ot Rain Fallins inco them, or auy orher concurrent Water ro raile and aumentthem. Thacit spers out of the Chasins, opened by che Farthiquatce in great abundance; mountins up in inigher Screams co an incredible heighu in che AI, and chis ottentimes ac mans Miles Distance From any Sea. Thacir litevise Aies Forrh oF che Volcanos in val Fleods, and with mondertul Violence: Thac cis Forced chroush rhe FTiarus S, ac the Borrom of the Sea, Wvicti such Vehemence, thât ic purs the Sea immediately into the most horrible Dilorder and Perturbacion imaginable, eren when there is nOL the leas breath oF Wind Sirrins, but aIl rill chen calm and still; makins ic rase and roae rith a most hideous and amazins Noise, raisins irs Surtace into Prodisious Nares, and coltins and roulins chem abour in a very stranse and turious manner; overlettins Shrips in cheFlarbours, and sintins them eothe bocom, wich mans orler like Outrages. That eis retunde d our oF chese Fiarussin suel Ouanier al(o, chat it makes a vast Addition to the Wracer of che Sea; raisins ir mans Fachoms higher than evet ic Aoirs in che highest Tides, (0 as tOpOUr ic Forch far berond iis ulual Bounds, and matce it overmhelm che adjacene Counery; by chis means ruinins and destrorins Lowns and Cicies, drovn ins boch Men and Caule; breakins che C ables ot Stiips, drivins ehem trom cheir Anchors, bearins them alons ich che Inundarion sereral Miles up into che Counery, and chere rumnins chemaground; Srandins Wrhales likevise, and other great Fistres and learins chem, ac is Recurn, uxon dey Land. LMal thele Phaenomena are noc new, or peculiat ro the Farthquakres which hare happen d’in our Times, buc hare been obserred in all Ages, ana particularly chese exorbirane Commorions oF the They likerise belieredu chac he harins a fult Sway and Command over the Water, had PONC ro silland compole ic, as Wrell as to more and disturb it; and thefarch, by incans ol ic; and cheretore chey also sarehim che Name OF A00LN, OV The istablister; under which Name several Temple vere consecrared to him, and Sacrifices loHered Wvhenerer an Farchquake happend, ro pacitierand appease hims requettins châc he vrould allari che Commorions oF the. Water, secure che Foundari ons of che Parch, and puc an end to rhe Parrb. quare. Thac the Fire ir selF, wrtri hibeins chus aetn bled and pene up, is che causoloF all chese PerTuT barions, makes irs own ar al(o Forch, by whae Passases loerer ic can ser vene; chrough che Spira- cles oF the next Vulcano s, chrough che Cracks and Openings of the Farth abore mentioned, chroust the Apertures oF Springs, especially cholec orthe Thermae, Or any octer way charir can cither tindo makre; and beinsthus discharsed, the Parthqualee ceaseth, eill the Cause recurns again, and a fresti Collection ot chis Fire commirs the lame Oucrages a5 belores Thac chete is Cometimes in Commotion, a Por. tion of the AbyIS OF that vas FXFeHE, a5 c0 Make che Farch incumbent uxon it, for (o very larse: part of the Globe rosether, thac the Shock is fetr ihe lame Minure precisely, in Couneries thacrare mans Flundreds oF Miles distanttrom cach ortier: and ehis, crentho cher happen eo be parred by ché Sea Wyins becwixe chem; there manes nor Instan. ces of suchan Dniversal Concussion ot che irhole Globe, as must necds imply an Agiration of he Wvhole AbyIS. morions in all parrs oF ic, and cheretore no Corn ery can be wholly exempred trom the EHects ot thiem; vet chele Lfects are no Where very remarte able, nor are chere ulually any great Damases done by Farthquates, excepe onty in rhole Couneries wrtich are Mouncainous, and consequently Sconr. and Cavernous underneach, alte ceclans micle the Disposition oF che Scrata is TucH, That Mole la rerns open inco che AbyIS, and (0 treely admil aMC entertain the Fire, Whien asembline cherein, is Course chat ray irhiere it tinds the readiest Recex- sides, chac thole parrs of ehie Parth which abound With Strata OF Stone, AMaIBIE, WTAKIS IHCIIIOH ges oppoliion L AIL ML MIOSC TUTTOIIS Mlacrer, wtrich more lasily sire way, and Mate noc (0 grear Relictance; an L Vene obserrabie nOI only in chis, Bue aIl OFheF XpIOSONS WVhaTOVeT. cural Cumporrder, wrtrch calLInS FITC UPON CIS AI- remibIr, and appFOACHOL IIS OCCALONISCILAL MUMMHE- ins Noise, char Subrertanea lhunder, ertich is heard rumbline I CMC BOWCIS OI IC LaEEH aMIHIIS Farchquates, ale D) IHC Altistance or ies explosire Cometimes co make miserable Llarock and Destru- Ction. Wateros che Olobc. Lhis ve mas learn abundancy From ie LsIto ries ot Leet Les; and trras for chis realor hac Ma) O un Anciens concluded ristuly e noust, ial Ther vere cauled by che impulses anc Fluctualioet aler in cheBowels ot che Farch; Thac choush che HosDeHabie 1ochele Com the Cause oF the Shock, le naturally Recrins IIs tion, Which es coatas mose Caverns, chis beme indeed much che Cause oF Damps in Mines. BC. Mhacrered, and lustet Huch more by ic than thole irhich consist ot Crarel, Sand, and the litre laxet But abore all, those Couneries Which vield great injured and incommoded DY Farthquakes; those Minerals comsticurins in the Parrt, a kind oF Na- Aore Ot Sulphur and Pirre, are by Far the most aud theretote ees trequelsels called Neptune =a10Bcor 25 aI(O, FvoOIZBCV EvoSIaiC, anc Tvanioeezains; by all which LPichers chey denorea his Pover oE Makins che FarrH. They supposed chac he prelided over all. Ware irhraceter, 25 well chat wictun che Liarcti, 25 ehic Sea, and the rest upon ic; and char the karch vas supporred by Wacer, ues Foundarions beins laid Porrer, rendersrtho Shock much greater, (0 a5 chereon; on irhich acconne ic vas rhac they bc- Aou d upon him hac Coenomen Pasiion O, Ox Sup- Ana eis tor chis Kcalon, thac Traly, Sicili, ana cdlicus aud lome pante o cjece inve beca soron rorrer os rhe Farrh, and hac OL O∞463. 10176, O1 edisaimm et ss teitin