# Leibniz Legible — https://leibnizlegible.com # Page: https://leibnizlegible.com/page/859264114:0059 # Permalink to this reading: https://leibnizlegible.com/page/859264114:0059?run=74 # Title: Lectures De Potentia Restitutiva, Or Of Spring (shelfmarks Leibn. Marg. 105, Stück 1; Leibn. Marg. 105) # Folio 49, page id 859264114:0059 # Original at the GWLB: https://digitale-sammlungen.gwlb.de/resolve?id=859264114&page=59 # Source image: https://digitale-sammlungen.gwlb.de/content/859264114/jpgs/default/00000059.jpg # Model: FoNDUE-GD_v2_ft_Leibniz, run 74, 2026-09-06T16:05:13Z — 39 lines, status machine # Lines: 39 recognised, mean confidence 0.92 # 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. Therein Imade ie probable chat most IMandshare been chronn up by Tome subterraneous Pruptions. Such is the IDand OF Ascension, che Moluccas, _2C. Secondlr, chae most pare oF the Surtace oF the Farch hachbeen lince the C reation changed in its po- sition and height in respect oF the Sca, to rit, many parts rhich are no der Land, and lie abore thesca, hare Been in Former Ares covered with ic; and that manz parts, Which are nom corered richtheSCa, vere in former times dey Land. Mountains have been Cunke into Plains, and Plains hare beenraised intomountains. OF chese by obserrations I hare siven instances, and Beed that divers pARES OF Fneland hare in FOr- mer times been corered with the Sca, there beine Found ac chis day in the most TMland paTES FhCTCOF CuF- ficient evidences toprore it, towit, Shells oF divers (OTES OF Filbes, mans oE Wrhich vet remain ol ehe ani- mal substance, though others De Found petrified and converredintostone. Some oF theleare Found railed tothe topsoF thehiphest Mountains, others Cunk in- tothe boctoms oF the decpest Mines and WellS, nay, in the very bovels of the Mountains and Ouarries et Stonc. Phare added also divers other instances to prove che Pame chins OF Other PANES OF Furope, and haremanifested, noc only chat che lorver and plainer partsthereol hare been under the Sea, but that eren the highest Alpine and Pyrenean Mountains have run the lame Fate. Many Instances oEthe likre nature Thave allomet ith in Relations and obserrations made in the Fast asrellasinthe W est Indies, OF all irtrich Strange occurrences I can conceire no causemore probable than Farthquakces and (uibcerra- neous Fruptions Which Histories do Culticiently asture ustrave changed sea into Land, and Land into Sea, Vales into Nountains Pometimes, into Lates and Aby Resat Ocher times; and the contrary unless re may be allored to suxpole that the mater or Auid Pa2E