CHAPTER IX.

OF THE LOADSTONE AND ITS POLES, AND WHETHER

THEY SHOW THE LONGITUDE OF PLACES ON THE EARTH.

_A._ I come now to hear what natural causes you can assign of the

virtues of the magnet; and first, why it draws iron to it, and only

iron.

_B._ You know I have no other cause to assign but some local motion, and

that I never approved of any argument drawn from sympathy, influence,

substantial forms, or incorporeal effluvia. For I am not, nor am

accounted by my antagonists for a witch. But to answer this question, I

should describe the globe of the earth greater than it is at B in the

first figure, but that the terrella in the fourth figure will serve our

turn. For it is but calling B and C the poles of the earth, and D E the

diameter of the equinoctial circle, and making D the east, and E the

west. And then you must remember that the annual motion of the earth is

from west to east, and compounded of a straight and circular motion, so

as that every point of it shall describe a small circle from west to

east, as is done by the whole globe. And let the circles about _a b c_

be three of those small circles.

_A._ Before you go any farther, I pray you show me how I must

distinguish east and west in every part of this figure. For wheresoever

I am on earth, suppose at London, and see the sun rise suppose in

Cancer, is not a straight line from my eye to the sun terminated in the

east?

_B._ It is not due east, but partly east, partly south. For the earth,

being but a point compared to the sun, all the parallels to D E the

equator, such as are _e a_, _f b_, _c g_, if they be produced, will fall

upon the body of the sun. And therefore A _b_ is north-east; A _a_ east

north-east; and A _c_ north north-east.

_A._ Proceed now to the cause of attraction.

_B._ Suppose now that the internal parts of the loadstone had the same

motion with that of the internal parts of the sun which make the annual

motion of the earth from west to east, but in a contrary way, for

otherwise the loadstone and the iron can never be made to meet. Then set

the loadstone at a little distance from the earth, marked with _z_; and

the iron marked with _x_ upon the superficies of the earth. Now that

which makes _x_ rise to _z_, can be nothing else but air; for nothing

touches it but air. And that which makes the air to rise, can be nothing

but those small circles made by the parts of the earth, such are at _a b

c_, for nothing else touches the air. Seeing then the motion of each

point of the loadstone is from east to west in circles, and the motion

of each point of the iron from west to east; it follows, that the air

between the loadstone and the iron shall be cast off both east and west;

and consequently the place left empty, if the iron did not rise up and

fill it. Thus you see the cause that maketh the loadstone and the iron

to meet.

_A._ Hitherto I assent. But why they should meet when some heterogeneous

body lies in the air between them, I cannot imagine. And yet I have seen

a knife, though within the sheath, attract one end of the needle of a

mariner’s compass; and have heard it will do the same though a

stone-wall were between.

_B._ Such iron were indeed a very vigorous loadstone. But the cause of

it is the same that causeth fire or hot water, which have the same

compounded motion, to work through a vessel of brass. For though the

motion be altered by restraint within the heterogeneous body, yet being

continued quite through, it restores itself.

_A._ What is the cause why the iron rubbed over by a loadstone will

receive the virtue which the loadstone hath of drawing iron to it?

_B._ Since the motion that brings two bodies to meet must have contrary

ways, and that the motions of the internal parts of the magnet and of

the iron are contrary; the rubbing of them together does not give the

iron the first endeavour to rise, but multiplies it. For the iron

untouched will rise to a loadstone; but if touched, it becomes a

loadstone to other iron. For when they touch a piece of iron, they pass

the loadstone over it only one way, viz. from pole to pole; not back

again, for that would undo what before had been done; also they press it

in passing to the very end of the iron, and somewhat hard. So that by

this pressing motion all the small circles about the points _a b c_, are

turned the contrary way; and the halves of those small circles made on

the arch D B will be taken away and the poles changed, so as that the

north poles shall point south, and the south poles north, as in the

figure.

_A._ But how comes it to pass, that when a loadstone hath drawn a piece

of iron, you may add to it another, as if they begat one another? Is

there the like motion in the generation of animals?

_B._ I have told you that iron of itself will rise to the loadstone;

much more then will it adhere to it when it is armed with iron, and both

it and the iron have a plain superficies. For then not only the points

of contact will be many, which make the coherence stronger, but also the

iron wherewith it is armed is now another loadstone, differing a little,

which you perhaps think, as male and female. But whether this compounded

motion and confrication causeth the generation of animals, how should I

know, that never had so much leisure as to make any observation which

might conduce to that?

_A._ My next question is, seeing you say the loadstone, or a needle

touched with it, naturally respecteth the poles of the earth, but that

the variation of it proceedeth from some accidents in the superficies of

the earth; what are those accidents?

_B._ Suppose there be a hill upon the earth, for example, at _r_; then

the stream of the air which was between _z_ and _x_ westward, coming to

the hill, shall go up the hill’s side, and so down to the other side,

according to the crooked line which I have marked about the hill by

points; and this infallibly will turn the north point of the needle,

being on the east side, more towards the east, and that on the other

side more towards the west, than if there had been no hill. And where

upon the earth are there not eminences and depressions, except in some

wide sea, and a great way from land.

_A._ But if that be true, the variation in the same place should be

always the same, for the hills are not removed.

_B._ The variation of the needle at the same place is still the same;

but the variation of the variation is partly from the motion of the pole

itself, which by the astronomers is called _motus trepidationis_; and

partly from that, that the variation cannot be truly observed, for the

horizontal needle and the inclinatory needle incline alike, but cannot

incline in due quantity. For whether set upon a pin or an axis, their

inclination is hindered, in the horizontal needle, by the pin itself: if

upon an axis, if the axis be just, it cannot move; if slack, the weight

will hinder it; but chiefly because the north pole of the earth draws

away from it the north pole of the needle, for two like poles cannot

come together. And this is the cause why the variation in one place is

east, and another west.

_A._ This is indeed the most probable reason why the variation varies

that ever I heard given; and I should presently acknowledge that this

parallel motion of the axis of the earth in the ecliptic, supposed by

Copernicus, is the true annual motion of the earth, but that there is

lately come forth a book called _Longitude Found_ , which makes the

magnetical poles distant from the poles of the earth eight degrees and a

half.

_B._ I have the book. It is far from being demonstrated, as you shall

find, if you have the patience to see it examined. For wheresoever his

demonstration is true, the conclusion, if rightly inferred, will be

this, that the poles of the loadstone and the poles of the earth are the

same. And where, on the contrary, his demonstrations are fallacies, it

is because sometimes he fancieth the lines he hath drawn, not where they

are; sometimes because he mistakes his station; and sometimes because he

goes on some false principle of natural philosophy; and sometimes also

because he knoweth not sufficiently the doctrine of spherical triangles.

_A._ I think that is the book there which lies at your elbow. Pray you

read.

_B._ I find first (p. 4), that the grounds of his argument are the two

observations made by Mr. Burroughs, one at Vaygates, in 1576, where the

variation from the pole of the earth he found to be 11 deg. 15 min.

east; the other at Limehouse, near London, in 1580, where the variation

from the pole of the earth was 8 deg. 38 min. west, by which, he saith,

he might _find out the magnetical pole_.

_A._ Where is Vaygates?

_B._ In 70 degrees of north latitude; the difference of longitude

between London and it being 58 degrees.

_A._ The longitude of places being yet to seek, how came he to know this

difference of 58 degrees, except the poles of the magnet and the earth

be the same?

_B._ I believe he trusted to the globe for that. For the distance

between the places is not above 2000 miles the nearest way. But we will

pass by that, and come to his demonstration, and to his diagram, wherein

L is London, P the north-pole of the earth, V Vaygates. So that L P is

38 deg. 28 min.; P V 20 deg.; the angle L P V 58 deg. for the difference

between the longitudes of Vaygates and London. This is the construction.

But before I come to the demonstration, I have an inference to draw from

these observations, which is this. Because in the same year the

variation at London was 11 deg. 15 min. east, and at Vaygates 8 deg. 38

min. west; if you subtract 11 deg. 15 min. from the arc L P; and 8 deg.

38 min. from the arc L V, the variation on both sides will be taken

away; so that P V being the meridian of Vaygates, and L P the meridian

of London, they shall both of them meet in P the pole of the earth. And

if the pole of the magnet be nearer to the zenith of London than is the

pole of the earth, it shall be just as much nearer to the zenith of

Vaygates in the meridian of Vaygates, which is P V; as is manifest by

the diurnal motion of the earth.

_A._ All this I conceive without difficulty. Proceed to the

demonstration.

_B._ Mark well now. His words are these (page 5): From P L V subtract 11

deg. 15 min., and there remains the angle V L M. Consider now which is

the angle P L V, and which is the remaining angle V L M, and tell what

you understand by it.

_A._ He has marked the angle P L V with two numbers, 11 deg. 15 min. and

21 deg. 50 min., which together make 33 deg. 5 min. And the angle 11

deg. 15 min. being subtracted from P L V, there will remain 21 deg. 50

min. for the angle V L M. I know not what to say to it. For I thought

the arc P V, which is 20 deg., had been the arc of the spherical angle P

L V; and that the arc L V had been 58 deg., because he says the angle L

P V is so; and that the arc L M had been 46 deg., because the angle L P

M is so; and lastly, that the angle P L M had been 8 deg. 30 min.,

because the arc P M is so.

_B._ And what you thought had been true, if a spherical angle were a

very angle. For all men that have written of spherical triangles take

for the ground of their calculation, as Regiomontanus, Copernicus, and

Clavius, that the arch of a spherical angle is the side opposite to the

angle. You should have considered also that he makes the angle V P M 12

deg., but sets down no arc to answer it. But that you may find I am in

the right, look into the definitions which Clavius hath put down before

his treatise of spherical triangles, and amongst them is this; “the arc

of a spherical triangle is a part of a great circle intercepted between

the two sides drawn from the pole of the said great circle.”

_A._ The book is nothing worth; for it is impossible to subtract an arc

of a circle out of a spherical angle. And I see besides that he takes

the superficies that lieth between the sides L P and L M for an arch,

which is the quantity of an angle; and is a line, and cannot be taken

out of a superficies. I wonder how any man that pretends to mathematics

could be so much mistaken.

_B._ It is no great wonder. For Clavius himself striving to maintain

that a right angle is greater than the angle made by the diameter and

the circumference, fell into the same error. A corner, in vulgar speech,

and an angle, in the language of geometry, are not the same thing. But

it is easy even for a learned man sometimes to take them for the same,

as this author now has done; and proceeding he saith, subtract 8 deg. 38

min. from the angle P V L, and there remains the angle L V M.

_A._ That again is false, because impossible. What was it that deceived

him now?

_B._ The same misunderstanding of the nature of a spherical angle. Which

appears farther in this, that when he knew the arc V P was part of a

great circle, he thought V M, which he maketh 8 deg. 30 min., were also

parts of a great circle; which is manifestly false. For two great

circles, because they pass through the centre, do cut each other into

halves. But V P is not half a circle. He sure thought himself at

Vaygates, and that P M V was equal to P V, although in the same

hemisphere.

_A._ But how proves he that the arc P M is 8 degrees 30 minutes?

_B._ Thus. We have in two triangles, P L M and P V M, two sides and one

angle included, to find P M the distance of the magnetical pole from the

pole of the earth 8 deg. 30 min.

_A._ Is that all? It is very short for a demonstration of two so

difficult problems, as the quantity of 8 deg. 30 min.; and of the place

of the magnetical pole. But he has proved nothing till he has showed how

he found it. And though P M be 8 deg. 30 min., it follows not that M is

the magnetical pole.

_B._ Nor is it true. For if P M be 8 deg. 30 min., and V M 8 deg. 38

min., the whole arc P M V will be 17 deg. 8 min., which should be 20

deg. Besides, whereas the variations were east and west, the subtracting

of them should be also east and west, but they are north and south.

_A._ I am satisfied that the magnetical poles and the poles of the earth

are the same. But thus much I confess, if they were not the same, the

longitude were found. For the difference of the latitudes of the earth’s

equator and of the magnetical equator, is the difference of the

longitude. But proceed.

_B._ “The earth being a solid body, and the magnetic sphere that

encompasseth the earth being a substance that hath not solidity to keep

pace with the earth, loseth in its motion: and that may be the cause of

the motion of the magnetic poles from east to west.”

_A._ This is very fine and unexpected. The magnetic sphere, which I took

for a globe made of a magnet, has not solidity to keep pace with the

earth, though it be one of the hardest stones that are. It encompasseth

the earth; yet I thought nothing had encompassed the earth but air in

which I breath and move. By this also the whole earth must be a

loadstone. For two bodies cannot be in one place. So that he is yet no

farther than Dr. Gilbert whom he slights. And if the sphere be a magnet,

then the earth and loadstone have the same poles. See the force of

truth! which though it could not draw to it his reason, hath drawn his

words to it.

_B._ But perhaps he meant that the magnetic virtue encompasseth the

earth, and not the magnetic body.

_A._ But that helpeth him not. For if the body of the magnet be not

there, the virtue then is the virtue of the earth; and so again the

poles of the earth are magnetic poles.

_B._ You see how unsafe it is to boast of doctrines as of God’s gifts,

till we are sure that they are true. For God giveth and denieth as he

pleaseth, not as ourselves wish; as now to him he hath given confidence

enough, but hath denied him, at least hitherto, the finding of the

longitudes. In the next place (p. 8) he seems much pleased that his

doctrine agrees with an opinion of Keplerus, that from the creation to

the year of our Lord, it is to the year 1657 now 5650 years; and with

that which he saith some divines have held in times past, that as this

world was created in six days, so it should continue six thousand years.

By which account the world will be at an end three hundred and fifty

years hence; though the Scripture tells us it shall come as a thief in

the night. O what advantage three hundred and forty years hence will

they have that know this, over them that know it not, by taking up money

at interest, or selling lands at twenty years’ purchase!

_A._ But he says he will not meddle with that.

_B._ Yes, when he had meddled with it too much already.

_A._ But you have not told me wherein consisteth this agreement between

him and Keplerus.

_B._ I forgot it. It is in the motion of the magnetic poles. For

precedently (p. 7), he had said “that their period or revolution was six

hundred years; their yearly motion thirty-six minutes; and (p. 8) that

their motion is by sixes. Six tenths of a degree in one year; six

degrees in ten years; sixty degrees in a hundred years; and six times

sixty degrees in six hundred years.”

_A._ But what natural cause doth he assign of this revolution of six

hundred years?

_B._ None at all. For the magnet lying upon the earth, can have no

motion at all but what the earth and the air give it. And because it is

always at 8 deg. 30 min. distance from the pole of the earth, the earth

can give it no other motion than what it gives to its own poles by the

precession of the equinoctial points. Nor can the air give it any motion

but by its stream; which must needs vary when the stream varieth. But

what a vast difference does he make between the period of the motion of

the equinoctial points, which is about or near thirty-six thousand years

according to Copernicus (lib. iii. cap. 6), which makes the annual

precession to be 36 seconds, and the period of the magnetical poles’

motion, which is but six hundred years.

_A_. Go on.

_B_. He comes now (p. 15) to the inclinatory needle upon a spherical

loadstone. Where he shows, by diagram, that the needle and the

instrument together moved towards the magnetical pole, make the sum of

the inclinations equal to two quadrants, setting the north-point of the

needle southward: which I confess is true. But, in the same page, he

ascribeth the same motion to the earth in these words: “as the

horizontal needle hath a double motion about the round loadstone or

terrella, so also the inclinatory needle hath a double motion about the

earth.” What is this, but a confession that the poles of the magnet and

of the earth are the same?

_A._ It is plain enough.

_B._ Besides, seeing he placeth the magnetical pole at M in the meridian

of Vaygates, the needle being touched shall incline to the pole of the

earth which is P, as well there as at London, and make the north-pole of

the earth point south.

_A._ It is certain, because he puts both the magnetical pole and the

pole of the earth in the same meridian of the earth. Nor see I any cause

why, the needle being the same, it should not be as subject to

variation, and to variation of variation, and to all accidents of the

earth there, as in any other part.

_B._ He putteth (p. 16) a question, “at what distance from the earth are

the magnetic poles? and answers to it, they are very near the earth,

because the nearer the earth, the greater the strength.” What think you

of this?

_A._ I think they are in the superficies of the magnet, as the pole of

the earth is in the superficies of the earth. And consequently, that

then the earth must be a part of the magnet, and their poles the same.

For the body of the magnet and the body of the earth, if they be two,

cannot be in one place.

_B._ His next words are, “some things are to be considered concerning

those variations of the horizontal needle which are not according to the

situation of the place from the magnetic poles, but are contrary; as all

the West Indies according to the poles should be easterly, and they are

westerly. Which is by some accidental cause in the earth; and their

motion, as I formerly said, is a forced motion, and not natural.”

_A._ He has clearly overthrown his main doctrine. For to say the motion

of the needle is forced and unnatural, is a most pitiful shift, and

manifestly false, no motion being more constant or less accidental,

notwithstanding the variation, to which the inclinatory needle is no

less subject than the horizontal needle.

_B._ That which deceived him, was, that he thought them two sorts of

needles, forgetting what he had said of Norman’s invention of the

inclinatory needle by the inclining of the horizontal needle (p. 11).

For I will show you that what he says is easterly and should be

westerly, should be easterly as it is. Consider the fourth figure, in

which B is the north-pole, and B _c_ 11 deg. 15 min. easterly, which was

the variation at London in 1576 easterly. Suppose A _c_ to be the

needle, shall it not incline, as well here as at D _a_, and the

variation B _c_ be easterly? Again, D _a_ is 11 deg. 15 min., and the

needle in D parallel to A B, and at _a_ inclining also 11 deg. 15 min.

westerly. And is not the variation there D _a_ westerly, with the north

point of the needle in the line _a h_?

_A._ But the West-Indies are not in this hemisphere B C D E. The

variation therefore will proceed in an arc of the opposite hemisphere,

which is westerly.

_B._ I believe he might think so, forgetting that he and his compass

were on the superficies of the earth, and fancying them in the centre at

A.

_A._ It is like enough. If we had a straight line exactly equal to the

arc of a quadrant, I think it would very much facilitate the doctrine of

spherical triangles.

_B._ When you have done with your questions of natural philosophy, I

will give you a clear demonstration of the equality of a straight line

to the arc of a quadrant, which, if it satisfy you, you may carry with

you, and try thereby if you can find the angle of a spherical triangle

given.

_A._ It is time now to give over. And at our next meeting I desire your

opinion concerning the causes of diaphaniety, and refraction. This

Copernicus has done much more than he thought of. For he has not only

restored to us astronomy, but also made the way open to physiology.

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The English works of Thomas Hobbes of Malmesbury, Volume 07 (of 11) · 第 9 / 13 章