geological changes is like a mere point in the infinite progression of time. When we know that rain water falling on limestone will carry away a minute portion of the rock in solution, we do not hesitate to multiply that quantity by millions and millions, and assert that in course of time a mountain may be dissolved away. We have actual experience concerning the rise of land in some parts of the globe and its fall in others to the extent of some feet. Do we hesitate to infer what may thus be done in course of geological ages? As Gabriel Plattes long ago remarked, 'The sea never resting, but perpetually winning land in one place and losing in another, doth shew what may be done in length of time by a continual operation, not subject unto ceasing or intermission '". The action. of physical circumstances upon the forms and characters of animals by natural selection is subject to exactly the same remarks. As regards animals living in a state of nature the change of circumstances which can be ascertained to have occurred is so indefinitely slight, that we could not expect to observe any change in those animals whatever. Nature has made no experiment at all for us within historical times. Man, however, by taming and domesticating dogs, cats, horses, oxen, &c., has made considerable change in their circumstances, and we find considerable change also in their forms and character. Supposing the state of domestication to continue unchanged, these new forms would continue permanent so far as we know, and in this sense they are permanent. Thus the arguments against Darwin's theory, founded on the nonobservation of natural changes within the historical period, are of the weakest character, being purely negative.

u 'Discovery of Subterraneal Treasure,' 1639, p. 52.

CHAPTER XX.

METHOD OF VARIATIONS.

EXPERIMENTS may be of two kinds: experiments of simple fact, and experiments of quantity. In the first class of experiments we combine certain conditions, and wish to ascertain whether or not a certain effect of any quantity exists. Thus Hooke, as before described, wished to ascertain whether or not there was any difference in the force of gravity at the top and bottom of St. Paul's Cathedral. The chemist continually performs analyses for the purpose of ascertaining whether or not a given element exists in a particular mineral or mixture; all such experiments and analyses are qualitative rather than quantitative, because though the result may be more or less, and is necessarily quantitative, the particular amount of the result is not the immediate object of the enquiry.

So soon, however, as a result is known to be discoverable, the scientific man ought to proceed to the strictly quantitative enquiry, how great a result follows from a certain amount of the conditions which are supposed to constitute the aggregate cause? The possible numbers of experiments are now indefinitely great, for every variation in a necessary condition will usually produce a variation in the amount of the effect. The method of variation which thus arises is no narrow or special method, but it is the general application of experiment to phenomena capable of continuous quantity. As Professor

Fowler has well remarked, the observation of variations is really an integration of a supposed infinite number of applications of the so-called method of difference, that is of experiment in its perfect form.

In induction we aim at establishing a general law, and if we deal with quantities that law must really be expressed more or less obviously in the form of an equation, or it may be in more than one equation. We treat as before of conditions, and of what happens under those conditions. But the conditions will now vary, not in quality, but quantity, and the effect will also vary in quantity, so that the result of quantitative induction is always to arrive at some mathematical expression involving the quantity of each condition, and expressing the quantity of the result. In other words, we wish to know what function the effect is of its conditions. We shall find that it is one thing to obtain the numerical results, and quite another thing to detect the law obeyed by those results, the latter being an operation of an inverse and tentative character.

The Variable and the Variant.

Almost every series of quantitative experiments is directed to obtain the relation between the different values of one quantity which is varied at will, and another quantity which is caused thereby to vary. We may conveniently distinguish these as respectively the variable and the variant. When we are examining the effect of heat in expanding bodies, heat, or one of its dimensions, temperature, is the variable, length the variant. If we compress a body to observe how much it is thereby heated, pressure, or it may be the dimensions of the body, forms the variable, heat the variant. In thermo-electric pile we make heat the variable and the a Elements of Inductive Logic,' 1st edit. p. 175.

measure electricity as the variant. That one of the two measured quantities which is an antecedent condition of the other will be the variable.

It will always be convenient to have the variable entirely under our command. Experiments may indeed be made with accuracy, provided we can exactly measure the variable at the moment when the quantity of the effect is determined by it. But if we have to trust to the action of some capricious and very uncertain force, there may be great difficulty in making exact measurements, and those results may not be disposed over the whole range of quantity in a convenient manner. It is one prime object of the experimenter, therefore, to obtain a regular and governable supply of the cause or force which he is investigating. To determine correctly the efficiency of windmills, when the natural winds were constantly varying in force, would be exceedingly difficult. Smeaton, therefore, in his experiments on the subject, created a uniform artificial wind of the required force by moving his models against the air on the extremity of a revolving armb. The velocity of the wind could thus be rendered greater or less, it could be maintained uniform for any length of time, and its amount could be exactly ascertained. In determining the laws of the chemical action of light it would be out of the question to employ the rays of the sun, which vary in intensity with the clearness of the atmosphere, and with every passing cloud. One great source of difficulty in photometry and the experimental investigation of the chemical action of light consists in raining a perfectly uniform and governable source of gbe rays.

ophical Transactions,' vol. li. p. 138; abridgment, vol. xi. p. 355en and Roscoe's 'Researches,' in Philosophical Transactions' wexx p. 880, &c., where they describe a constant flame of

Fizeau's method of measuring the velocity of light enabled him to appreciate the time occupied by light in travelling through a distance of eight or nine thousand metres. But the revolving mirror of Wheatstone subsequently enabled Foucault and Fizeau to measure the velocity in a space of four metres. In this latter method there was the obvious advantage that various media could be substituted for air, and the temperature, density, and other conditions of the experiment accurately governed or defined.

Measurement of the Variable.

There is little use in obtaining exact measurements of an effect unless we can also exactly measure the conditions with which the effect is to be connected. It is absurd to measure the electrical resistance of a piece of metal, its elasticity, tenacity, density, or other physical qualities, if these vary in degree, not only with the minute and almost inappreciable impurities of the metal, but also with its physical condition. If the same bar changes its properties by being heated and cooled, and we cannot exactly define the state in which it is at any moment, our care in measuring will be wasted, because it can lead to no law. It is of little use to determine very exactly the electric conductibility of carbon, which as graphite or gas carbon conducts like a metal, as diamond is almost a non-conductor, and in several other forms possesses variable and intermediate powers of conduction. It will be of use only for immediate practical applications. Before measuring these we ought to have something to measure of which the conditions are capable of exact definition, and to which at a future time we or others can recur. Similarly the accuracy of our measurement need not much surpass the accuracy with which we can define the conditions of the object treated.