# Leibniz Legible — https://leibnizlegible.com # Page: https://leibnizlegible.com/page/859264114:0058 # Permalink to this reading: https://leibnizlegible.com/page/859264114:0058?run=74 # Title: Lectures De Potentia Restitutiva, Or Of Spring (shelfmarks Leibn. Marg. 105, Stück 1; Leibn. Marg. 105) # Folio 48, page id 859264114:0058 # Original at the GWLB: https://digitale-sammlungen.gwlb.de/resolve?id=859264114&page=58 # Source image: https://digitale-sammlungen.gwlb.de/content/859264114/jpgs/default/00000058.jpg # Model: FoNDUE-GD_v2_ft_Leibniz, run 74, 2026-09-06T16:05:13Z — 38 lines, status machine # Lines: 38 recognised, mean confidence 0.91 # 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. Faciliti, and came to the Stancia aboue cleven oF the clock, Wrhere chey dincd, and thenee about one in che ACcernoon (et Formards For che. Villa, Wrhere ther ar- rived that alcernoon about Aivethat F vening. ACcer their return they Found their Faces (by rea- son oF cheheat oF the Sun, and the parchins subtil Wind) cocasttheir stins. Fre didnot meature the Perpendicular heighe orthe TTiIIhim elE, buc Pars that he hath been informed by divers siltul Scamen, (Who by cheirbest observation have calsen the heishe oFit) chat it is betreen chrec and cour miles perpendicularly abOre ThCSCa. Nthis Relation it is very remarkable: Pirst, thac this prodigious high ETill is the Product ot an Farthquakze, and seems heretotore tohare Becn a Vulcano, or burnins Mlountain, like thole oF Ana- Vesuvius, Hecla, ec. though at present it hach only tire enough letc to Pend Forth lome ferr Culphureous tumes, and to makse thecarth oF the Caldera or hoi- lor picat therery top chereot in lome places almost hoc cnouoh to buen their Mooesthat pals overit. And Posbly in succceding Ages eren this licele tire may bc quite extinet, and thenno othertion thereot mar bc lett buc a prodigiousr high Rock or lpiring Moun- tain, Wrhich in eraet oftime may by degreesmaste and bediminished into a FTiIl oF amoremoderate heigHt. Nom as this TTill Peems very evidently to bc the effectot an Barchquake, (0 P am apt to beliere that molt, iE noc all ocher Hills oF the morid Whacever mar have been the lame mar generated. Nay, nOL ontr aII the FTIIIS, Buc also che Land irtrich appears aborethetace oF theaters. And For this I could produce very many Tristories and Arguments chat rould makre it leem verr probable, but chat I reserre them inthe Lectures wrhich P read ot this subject in Cresam Collcde in the vears 1664, and 1665. erhich Wrhen P can hare time to peruse lmay publist. Pherein