Fabri, Honoré, Dialogi physici in quibus de motu terrae disputatur, 1665

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              dum ſupra Horizontem; errorem eſſe dico; quia Luna exiſtente in maxi­
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              mâ declinatione Auſtrali, arcus illius diuinus ab Ortivo puncto Horizon­
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              tis ad Meridianum, vix eſt 60. graduum; igitur ſi detrahantur 50. ſuper­
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              ſunt 30. quos dum Luna decurrit, duabus ſcilicet horis Æquinoctialibus
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              & 4. minutis, durat æſtus; quod apertè falſum eſſe conſtat; tamdiu re­
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              fluxus duraret. </s>
              <s id="s.001623">Prætereà, æſtus, qui fieret poſt Occaſum Lunæ, longè
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              major eſſet priore; nempè arcus illius paralleli ſub Horizonte, longè ma­
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              jor eſt alio; quem Luna ſupra Horizontem excurrit,
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              cuncta hæc experi­
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              mentis repugnant. </s>
              <s id="s.001624">Dixi ſuprà, per ſe, cùm per accidens fieri poſſit, vt tem­
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              pora fluxus & refluxus inæqualia ſint. </s>
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              Antim.
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              <s id="s.001626"> Ex præmiſſis principiis hoc manifeſtè deducitur; nempè ſin­
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              gulis pænè momentis, mutatur in globo punctum, ſeu Polus maximæ ele­
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              vationis, ac proinde centrum circulorum & arcuum preſſionis, quorum
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              cum diverſa ſit ratio & proportio, propter varios continentis & Maris
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              tractus, in ſuperficie globi, ſine certâ lege diſtinctos, inde neceſſariò ſe­
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              quitur diverſa vis preſſionis, diverſa impreſſio, diverſa appulſus, vel illa­
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              pſus linea: quod vt meliùs intelligas fige pedem circini ad Occiduum
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              Guineæ Promontorium, non procul ab Oſtio Nigri, ductíſque innumeris
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              circulis ex illo centro, concentricis & parallelis, diſtingue arcus vtiles ab
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              inutilibus, ſenſimque promoto versùs Ortum illo centro, vſque ad 60.
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              gradus, ſi vlteriùs illud promoveas, vſque ad 90. circuli preſſionis
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              maxima ex parte, vel continenti Africæ, Europæ, Aſiæ vel Indico Ocea­
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              no incumbent, ac proinde inutiles erunt reſpectu prædicti loci: quid mi­
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              rum igitur, ſi 4. dumtaxat horis in eo æſtus aſſurgat, deprimatur verò plu­
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              ribus? </s>
              <s id="s.001627">Nam promoto versùs Oceanum centro, diverſa eſt circulorum preſ­
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              ſionis ratio. </s>
              <s id="s.001628">Aliquid ſimile obſervabis, fixo circini pede ad litus Cam­
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              baiæ; tanquam in centro: accedit, quòd ex multis capitibus prædicta
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              æſtuum inæqualitas inducitur; Primò, per planum magis inclinatum, lon­
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              giùs excurrit & velociùs, licèt plus temporis ponat in decurrendo magis
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              inclinato, cuncta hæc ex doctrina motuum perſpicua ſunt; tantumdem
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              temporis aqua ponit in deſcenſu per planum inclinatum., quantum in
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              aſcenſu. </s>
              <s id="s.001629">Secundò, Si poſt quàm aqua regredi cœpit, nova quædam fiat
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              æſtus reflexio, versùs fluminis fauces, vel ſi aqua libero quidem aditu ſu­
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              beat, ſed exitu difficiliore, tunc acceſſus breviore tempore fiet quàm re­
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              ceſſus. </s>
              <s id="s.001630">Tertiò, Si nova reflexio accedat, antequam aqua regredi incipiat,
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              vel agger quidam appoſitus ad fauces ſinus, aut fluminis primam vim ac­
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              ceſſus retundat, vt videre eſt ad fauces Sequanæ & Garumnæ, receſſus bre­
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              viore tempore fiet quàm acceſſus. </s>
              <s id="s.001631">Quartò, Pro diverſo æſtus ad oram ap­
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              pulſu, vel illapſu, longiùs per alveum fluviorum vel minùs longè aqua ex­
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              currit; item pro diverſa alvei inclinatione; hinc facilè crediderim, alveum
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              illorum fluminum, in quibus ad aliquot centena milliaria æſtus excurrit,
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              eſſe valde inclinatum Quintò, Dicam ampliùs, ratione ejuſdem loci, non­
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              modò æſtum altiùs aut minùs altè attolli, verùm eſſe aliquando acceſſum
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              majorem, aliàs minorem eſſe poſſe; quia mutatur ſingulis diebus centrum
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              circulorum preſſionis, etiam reſpectu ejuſdem loci; item aliquando ac-</s>
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