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<title>The Notebooks of Leonardo Da Vinci</title>
<link>http://interconnected.org/home/more/davinci/</link>
<description>Day-by-day Da Vinci. Read the pages of the Notebooks by RSS, one at a time. This feed began on 03 July 2009.</description>

<item>
<title>Page 954</title>
<link>http://interconnected.org/home/more/davinci/954.html</link>
<description><![CDATA[<p>How the river Po, in a short time might dry up the Adriatic sea in
<br>the same way as it has dried up a large part of Lombardy.
<br>
<br>The ebb and flow of the tide (955-960).</p>]]></description>
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<item>
<title>Page 953</title>
<link>http://interconnected.org/home/more/davinci/953.html</link>
<description><![CDATA[<p>That the shores of the sea constantly acquire more soil towards the
<br>middle of the sea; that the rocks and promontories of the sea are
<br>constantly being ruined and worn away; that the Mediterranean seas
<br>will in time discover their bottom to the air, and all that will be
<br>left will be the channel of the greatest river that enters it; and
<br>this will run to the ocean and pour its waters into that with those
<br>of all the rivers that are its tributaries.</p>]]></description>
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<item>
<title>Page 952</title>
<link>http://interconnected.org/home/more/davinci/952.html</link>
<description><![CDATA[<p>OF WAVES.
<br>
<br>A wave of the sea always breaks in front of its base, and that
<br>portion of the crest will then be lowest which before was highest.
<br>
<br>[Footnote: The page of FRANCESCO DI GIORGIO'S _Trattato_, on which
<br>Leonardo has written this remark, contains some notes on the
<br>construction of dams, harbours &c.]</p>]]></description>
</item>

<item>
<title>Page 951</title>
<link>http://interconnected.org/home/more/davinci/951.html</link>
<description><![CDATA[<p>HERE THE REASON IS GIVEN OF THE EFFECTS PRODUCED BY THE WATERS IN
<br>THE ABOVE MENTIONED PLACE.
<br>
<br>All the lakes and all the gulfs of the sea and all inland seas are
<br>due to rivers which distribute their waters into them, and from
<br>impediments in their downfall into the Mediterranean --which divides
<br>Africa from Europe and Europe from Asia by means of the Nile and the
<br>Don which pour their waters into it. It is asked what impediment is
<br>great enough to stop the course of the waters which do not reach the
<br>ocean.
<br>
<br>On the encroachments of the sea on the land and vice versa
<br>(952-954).</p>]]></description>
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<title>Page 950</title>
<link>http://interconnected.org/home/more/davinci/950.html</link>
<description><![CDATA[<p>All inland seas and the gulfs of those seas, are made by rivers
<br>which flow into the sea.</p>]]></description>
</item>

<item>
<title>Page 949</title>
<link>http://interconnected.org/home/more/davinci/949.html</link>
<description><![CDATA[<p>THAT THE OCEAN DOES NOT PENETRATE UNDER THE EARTH.
<br>
<br>The ocean does not penetrate under the earth, and this we learn from
<br>the many and various springs of fresh water which, in many parts of
<br>the ocean make their way up from the bottom to the surface. The same
<br>thing is farther proved by wells dug beyond the distance of a mile
<br>from the said ocean, which fill with fresh water; and this happens
<br>because the fresh water is lighter than salt water and consequently
<br>more penetrating.
<br>
<br>Which weighs most, water when frozen or when not frozen?
<br>
<br>FRESH WATER PENETRATES MORE AGAINST SALT WATER THAN SALT WATER
<br>AGAINST FRESH WATER.
<br>
<br>That fresh water penetrates more against salt water, than salt water
<br>against fresh is proved by a thin cloth dry and old, hanging with
<br>the two opposite ends equally low in the two different waters, the
<br>surfaces of which are at an equal level; and it will then be seen
<br>how much higher the fresh water will rise in this piece of linen
<br>than the salt; by so much is the fresh lighter than the salt.
<br>
<br>On the formation of Gulfs (950. 951).</p>]]></description>
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<item>
<title>Page 948</title>
<link>http://interconnected.org/home/more/davinci/948.html</link>
<description><![CDATA[<p>The waters of the salt sea are fresh at the greatest depths.</p>]]></description>
</item>

<item>
<title>Page 947</title>
<link>http://interconnected.org/home/more/davinci/947.html</link>
<description><![CDATA[<p>For the third and last reason we will say that salt is in all
<br>created things; and this we learn from water passed over the ashes
<br>and cinders of burnt things; and the urine of every animal, and the
<br>superfluities issuing from their bodies, and the earth into which
<br>all things are converted by corruption.
<br>
<br>But,--to put it better,--given that the world is everlasting, it
<br>must be admitted that its population will also be eternal; hence the
<br>human species has eternally been and would be consumers of salt; and
<br>if all the mass of the earth were to be turned into salt, it would
<br>not suffice for all human food [Footnote 27: That is, on the
<br>supposition that salt, once consumed, disappears for ever.]; whence
<br>we are forced to admit, either that the species of salt must be
<br>everlasting like the world, or that it dies and is born again like
<br>the men who devour it. But as experience teaches us that it does not
<br>die, as is evident by fire, which does not consume it, and by water
<br>which becomes salt in proportion to the quantity dissolved in
<br>it,--and when it is evaporated the salt always remains in the
<br>original quantity--it must pass through the bodies of men either in
<br>the urine or the sweat or other excretions where it is found again;
<br>and as much salt is thus got rid of as is carried every year into
<br>towns; therefore salt is dug in places where there is urine.-- Sea
<br>hogs and sea winds are salt.
<br>
<br>We will say that the rains which penetrate the earth are what is
<br>under the foundations of cities with their inhabitants, and are what
<br>restore through the internal passages of the earth the saltness
<br>taken from the sea; and that the change in the place of the sea,
<br>which has been over all the mountains, caused it to be left there in
<br>the mines found in those mountains, &c.
<br>
<br>The characteristics of sea water (948. 949).</p>]]></description>
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<item>
<title>Page 946</title>
<link>http://interconnected.org/home/more/davinci/946.html</link>
<description><![CDATA[<p>WHY WATER IS SALT.
<br>
<br>Pliny says in his second book, chapter 103, that the water of the
<br>sea is salt because the heat of the sun dries up the moisture and
<br>drinks it up; and this gives to the wide stretching sea the savour
<br>of salt. But this cannot be admitted, because if the saltness of the
<br>sea were caused by the heat of the sun, there can be no doubt that
<br>lakes, pools and marshes would be so much the more salt, as their
<br>waters have less motion and are of less depth; but experience shows
<br>us, on the contrary, that these lakes have their waters quite free
<br>from salt. Again it is stated by Pliny in the same chapter that this
<br>saltness might originate, because all the sweet and subtle portions
<br>which the heat attracts easily being taken away, the more bitter and
<br>coarser part will remain, and thus the water on the surface is
<br>fresher than at the bottom [Footnote 22: Compare No. 948.]; but this
<br>is contradicted by the same reason given above, which is, that the
<br>same thing would happen in marshes and other waters, which are dried
<br>up by the heat. Again, it has been said that the saltness of the sea
<br>is the sweat of the earth; to this it may be answered that all the
<br>springs of water which penetrate through the earth, would then be
<br>salt. But the conclusion is, that the saltness of the sea must
<br>proceed from the many springs of water which, as they penetrate into
<br>the earth, find mines of salt and these they dissolve in part, and
<br>carry with them to the ocean and the other seas, whence the clouds,
<br>the begetters of rivers, never carry it up. And the sea would be
<br>salter in our times than ever it was at any time; and if the
<br>adversary were to say that in infinite time the sea would dry up or
<br>congeal into salt, to this I answer that this salt is restored to
<br>the earth by the setting free of that part of the earth which rises
<br>out of the sea with the salt it has acquired, and the rivers return
<br>it to the earth under the sea.
<br>
<br>[Footnote: See PLINY, Hist. Nat. II, CIII [C]. _Itaque Solis ardore
<br>siccatur liquor: et hoc esse masculum sidus accepimus, torrens
<br>cuncta sorbensque._ (cp. CIV.) _Sic mari late patenti saporem
<br>incoqui salis, aut quia exhausto inde dulci tenuique, quod facillime
<br>trahat vis ignea, omne asperius crassiusque linquatur: ideo summa
<br>aequorum aqua dulciorem profundam; hanc esse veriorem causam, quam
<br>quod mare terrae sudor sit aeternus: aut quia plurimum ex arido
<br>misceatur illi vapore: aut quia terrae natura sicut medicatas aquas
<br>inficiat_ ... (cp. CV): _altissimum mare XV. stadiorum Fabianus
<br>tradit. Alii n Ponto coadverso Coraxorum gentis (vocant B Ponti)
<br>trecentis fere a continenti stadiis immensam altitudinem maris
<br>tradunt, vadis nunquam repertis._ (cp. CVI [CIII]) _Mirabilius id
<br>faciunt aquae dulces, juxta mare, ut fistulis emicantes. Nam nec
<br>aquarum natura a miraculis cessat. Dulces mari invehuntur, leviores
<br>haud dubie. Ideo et marinae, quarum natura gravior, magis invecta
<br>sustinent. Quaedam vero et dulces inter se supermeant alias._]</p>]]></description>
</item>

<item>
<title>Page 945</title>
<link>http://interconnected.org/home/more/davinci/945.html</link>
<description><![CDATA[<p>have flowed from the summits of the mountains of Armenia, it must be
<br>believed that all the water of the ocean has passed very many times
<br>through these mouths. And do you not believe that the Nile must have
<br>sent more water into the sea than at present exists of all the
<br>element of water? Undoubtedly, yes. And if all this water had fallen
<br>away from this body of the earth, this terrestrial machine would
<br>long since have been without water. Whence we may conclude that the
<br>water goes from the rivers to the sea, and from the sea to the
<br>rivers, thus constantly circulating and returning, and that all the
<br>sea and the rivers have passed through the mouth of the Nile an
<br>infinite number of times [Footnote: _Moti Armeni, Ermini_ in the
<br>original, in M. RAVAISSON'S transcript _"monti ernini [le loro
<br>ruine?]"_. He renders this _"Le Tigre et l'Euphrate se sont deverses
<br>par les sommets des montagnes [avec leurs eaux destructives?] on
<br>pent cro're" &c. Leonardo always writes _Ermini, Erminia_, for
<br>_Armeni, Armenia_ (Arabic: _Irminiah_). M. RAVAISSON also deviates
<br>from the original in his translation of the following passage: "_Or
<br>tu ne crois pas que le Nil ait mis plus d'eau dans la mer qu'il n'y
<br>en a a present dans tout l'element de l'eau. Il est certain que si
<br>cette eau etait tombee_" &c.]
<br>
<br>II.
<br>
<br>ON THE OCEAN.
<br>
<br>Refutation of Pliny's theory as to the saltness of the sea (946.
<br>947).</p>]]></description>
</item>

<item>
<title>Page 944</title>
<link>http://interconnected.org/home/more/davinci/944.html</link>
<description><![CDATA[<p>THE OPINION OF SOME PERSONS WHO SAY THAT THE WATER OF SOME SEAS IS
<br>HIGHER THAN THE HIGHEST SUMMITS OF MOUNTAINS; AND NEVERTHELESS THE
<br>WATER WAS FORCED UP TO THESE SUMMITS.
<br>
<br>Water would not move from place to place if it were not that it
<br>seeks the lowest level and by a natural consequence it never can
<br>return to a height like that of the place where it first on issuing
<br>from the mountain came to light. And that portion of the sea which,
<br>in your vain imagining, you say was so high that it flowed over the
<br>summits of the high mountains, for so many centuries would be
<br>swallowed up and poured out again through the issue from these
<br>mountains. You can well imagine that all the time that Tigris and
<br>Euphrates</p>]]></description>
</item>

<item>
<title>Page 943</title>
<link>http://interconnected.org/home/more/davinci/943.html</link>
<description><![CDATA[<p>OF CERTAIN PERSONS WHO SAY THE WATERS WERE HIGHER THAN THE DRY LAND.
<br>
<br>Certainly I wonder not a little at the common opinion which is
<br>contrary to truth, but held by the universal consent of the judgment
<br>of men. And this is that all are agreed that the surface of the sea
<br>is higher than the highest peaks of the mountains; and they allege
<br>many vain and childish reasons, against which I will allege only one
<br>simple and short reason; We see plainly that if we could remove the
<br>shores of the sea, it would invest the whole earth and make it a
<br>perfect sphere. Now, consider how much earth would be carried away
<br>to enable the waves of the sea to cover the world; therefore that
<br>which would be carried away must be higher than the sea-shore.</p>]]></description>
</item>

<item>
<title>Page 942</title>
<link>http://interconnected.org/home/more/davinci/942.html</link>
<description><![CDATA[<p>OF THE SEA, WHICH TO MANY FOOLS APPEARS TO BE HIGHER THAN THE EARTH
<br>WHICH FORMS ITS SHORE.
<br>
<br>_b d_ is a plain through which a river flows to the sea; this plain
<br>ends at the sea, and since in fact the dry land that is uncovered is
<br>not perfectly level--for, if it were, the river would have no
<br>motion--as the river does move, this place is a slope rather than a
<br>plain; hence this plain _d b_ so ends where the sphere of water
<br>begins that if it were extended in a continuous line to _b a_ it
<br>would go down beneath the sea, whence it follows that the sea _a c
<br>b_ looks higher than the dry land.
<br>
<br>Obviously no portions of dry land left uncovered by water can ever
<br>be lower than the surface of the watery sphere.</p>]]></description>
</item>

<item>
<title>Page 941</title>
<link>http://interconnected.org/home/more/davinci/941.html</link>
<description><![CDATA[<p>OF THE HEAT THAT IS IN THE WORLD.
<br>
<br>Where there is life there is heat, and where vital heat is, there is
<br>movement of vapour. This is proved, inasmuch as we see that the
<br>element of fire by its heat always draws to itself damp vapours and
<br>thick mists as opaque clouds, which it raises from seas as well as
<br>lakes and rivers and damp valleys; and these being drawn by degrees
<br>as far as the cold region, the first portion stops, because heat and
<br>moisture cannot exist with cold and dryness; and where the first
<br>portion stops the rest settle, and thus one portion after another
<br>being added, thick and dark clouds are formed. They are often wafted
<br>about and borne by the winds from one region to another, where by
<br>their density they become so heavy that they fall in thick rain; and
<br>if the heat of the sun is added to the power of the element of fire,
<br>the clouds are drawn up higher still and find a greater degree of
<br>cold, in which they form ice and fall in storms of hail. Now the
<br>same heat which holds up so great a weight of water as is seen to
<br>rain from the clouds, draws them from below upwards, from the foot
<br>of the mountains, and leads and holds them within the summits of the
<br>mountains, and these, finding some fissure, issue continuously and
<br>cause rivers.
<br>
<br>The relative height of the surface of the sea to that of the land
<br>(942-945).</p>]]></description>
</item>

<item>
<title>Page 940</title>
<link>http://interconnected.org/home/more/davinci/940.html</link>
<description><![CDATA[<p>PROVES HOW THE EARTH IS NOT GLOBULAR AND NOT BEING GLOBULAR CANNOT
<br>HAVE A COMMON CENTRE.
<br>
<br>We see the Nile come from Southern regions and traverse various
<br>provinces, running towards the North for a distance of 3000 miles
<br>and flow into the Mediterranean by the shores of Egypt; and if we
<br>will give to this a fall of ten braccia a mile, as is usually
<br>allowed to the course of rivers in general, we shall find that the
<br>Nile must have its mouth ten miles lower than its source. Again, we
<br>see the Rhine, the Rhone and the Danube starting from the German
<br>parts, almost the centre of Europe, and having a course one to the
<br>East, the other to the North, and the last to Southern seas. And if
<br>you consider all this you will see that the plains of Europe in
<br>their aggregate are much higher than the high peaks of the maritime
<br>mountains; think then how much their tops must be above the sea
<br>shores.
<br>
<br>Theory of the elevation of water within the mountains.</p>]]></description>
</item>

<item>
<title>Page 939</title>
<link>http://interconnected.org/home/more/davinci/939.html</link>
<description><![CDATA[<p>THE FIGURES OF THE ELEMENTS.
<br>
<br>Of the figures of the elements; and first as against those who deny
<br>the opinions of Plato, and who say that if the elements include one
<br>another in the forms attributed to them by Plato they would cause a
<br>vacuum one within the other. I say it is not true, and I here prove
<br>it, but first I desire to propound some conclusions. It is not
<br>necessary that the elements which include each other should be of
<br>corresponding magnitude in all the parts, of that which includes and
<br>of that which is included. We see that the sphere of the waters
<br>varies conspicuously in mass from the surface to the bottom, and
<br>that, far from investing the earth when that was in the form of a
<br>cube that is of 8 angles as Plato will have it, that it invests the
<br>earth which has innumerable angles of rock covered by the water and
<br>various prominences and concavities, and yet no vacuum is generated
<br>between the earth and water; again, the air invests the sphere of
<br>waters together with the mountains and valleys, which rise above
<br>that sphere, and no vacuum remains between the earth and the air, so
<br>that any one who says a vacuum is generated, speaks foolishly.
<br>
<br>But to Plato I would reply that the surface of the figures which
<br>according to him the elements would have, could not exist.
<br>
<br>That the flow of rivers proves the slope of the land.</p>]]></description>
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