Borro, Girolamo, Del flusso e reflusso del mare, 1561

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            <pb xlink:href="012/01/062.jpg" pagenum="58"/>
            <p type="main">
              <s>TAL. </s>
              <s>Viromperò la parola in boccha (M. Giuſeppe) hab
                <lb/>
              biate patienza, io non ci voglio entrare; perche deſidero veni­
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              re vna volta, à capo de nostri raggionamenti. </s>
            </p>
            <p type="main">
              <s>NOZ.
                <expan abbr="Altrettãto">Altrettanto</expan>
              il deſidero io, però piacciaui dirmi quel
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              lo, che hauete ritratto da ſegreti di natura, circa il gonfiare,
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              & circa lo sgonfiare del Nilo. </s>
            </p>
            <p type="main">
              <s>TAL. </s>
              <s>Io attribuiſco vn tale effetto à tutte le cagioni, qua
                <lb/>
              li voi vdirete: Alle pioggie grandißime, che nella Etepia, &
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              nello egitto ſuperiore ſono in que tempi: Alle neui, che all'ho­
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              ra ſi distruggono ne monti di Bet, doue ſono le fontane del Ni­
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              lo, & alle acque, che in quella stagione eſcono di ſotterra: in
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              tanto, che non vnaſola, è la cauſa di questo effetto, ma mol­
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              te. </s>
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            <p type="main">
              <s>NOZ. </s>
              <s>Et in che modo? </s>
            </p>
            <p type="main">
              <s>TAL. </s>
              <s>Voi l'udirete hor'hora. </s>
              <s>La pioggia ha le ſue cagioni, co
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              me tutti gli altri effetti naturali, le quali ſono la materia, &
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              l'e fficiente: Quiui vi è la materia copioſißima, per che vi è
                <expan abbr="buõ">buom</expan>
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              numero di großißimi fiumi, oltra il Nilo, & il mare Arabico,
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              & l'Oceano: vi ſono lunghißime, & inuilup patißime catene
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              d'altißimi monti, vi ſono in fra que monti profundißime valli,
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              da tutti questi luoghi & da altri ſimili, poſſono ſalire vapori,
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              & in effetto ſalgono; perche nelle alte parti di que monti ſi ve
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              de, apertamente raccorre vna folta nebbia, laquale pian piano
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              ſi conuerte in nuuola: & di nuuola hora in neue, et hora in piog
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              gia, ſecondo, che il freddo, è ò maggiore, ò minore: Vi è l'efficien
                <lb/>
              te; per che vi è il caldo del Sole grandißimo, ilquale puo tir are
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              & tira grandißima copia di vapori, & in que monti, e in quel
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              le valli vi ſono grandißimi freddi, da poter' condenſare, i vapo­
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              ri tanto che diuentino nuuole, & di nuuole hor' pioggia hora
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              neue: Tira il Sole maggior' copia di vapori, quando egli piu
                <expan abbr="lũ-go">lun­
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                go</expan>
              tempo corre ſopra lo Egitto, però entrando nel primo grado
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              dello Ariete, i giorni quiui incominciano, à creſcere, & con lo
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                <expan abbr="augumẽto">augumento</expan>
              della maggiore lunghezza de giorni, il Sole per mag
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              giore ſpatio di tempo ſi ferma ſopra quella prouincia, & ogni </s>
            </p>
          </chap>
        </body>
      </text>
    </archimedes>
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