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relationship would perplex the genealogist.

It has been truly remarked, that "no one has ever written the complete history of any one animal." If we rake together all that has been recorded of the hydra, we have a long and marvellous record; yet it is not complete: new points of inquiry are continually suggested, showing, that to understand in all its fulness the history of even the humblest zoophyte, belongs not to one whose duration is so brief, and whose faculties are so limited, as those of man in his present state of existence. Let us therefore move onwards.

The hydra has the power of changing its place at pleasure, and its entire body is naked. In both respects it differs from the members of another family. Their aspect is that of a number of tubes, from a couple of inches to a foot in length, attached to a common base, and often more or less twisted together. From these tubes the name Tubularia is applied to such animals. From each tube, a head of a beautiful red colour projects, looking like an animated flower. These heads or blossoms drop off, the tube remains bare and unsightly, like a tree reft of all its floral glory; yet ere long, from that naked stem, a new head is developed, and the living blossom waves once more its tender filaments, and seeks again the food on which it lives.

The great majority of the zoophytes belonging to the present order, are, however, those which, in little tree-like tufts, decorate the shells of the oyster and the scallop, are attached to stones, or cluster upon the fronds of the large sea-weeds. These are grouped together under a name (Sertularida) which is derived from a Latin word (sertula) signifying a little wreath or garland. Hogarth, our great moral painter, thus writes to Ellis respecting them :"As for your pretty little seed-cups, or vases, they are a sweet confirmation of the pleasure Nature seems to take in superadding an elegance of form to most of her works, wherever you find them. How poor and bungling are all the imitations of Art! When I have the pleasure of seeing you next, we will sit down-nay, kneel down, if you will-and admire these things!" With these striking words, Dr. Johnston commences his History of British Zoophytes, and adds, "He must, indeed, be more than

ordinarily dull and insensate, who can examine them without catching some of the enthusiasm of the artist. They excel all other zoophytical productions in delicacy, and the graceful arrangement of their forms; some borrowing the character of the prettiest marine plants, others assuming the semblance of the ostrich plume; while the variety and elegance exhibited in the figures and sculpture of their miniature cups and chalices, is only limited by the number of their species."*

How shall I describe the growth and nature of these productions! Suppose a miniature tree; its branches covered with little cells, and a minute animal spreading out from each cell its tentacula, feelers, or arms-by whatever name you term themand seizing its allotted food. If touched, or alarmed, it can shrink into its cell. Yet call it not the inhabitant of that asylum to which it has retreated. To do so would convey a wrong idea. It would imply that a living creature had sought safety in a lifeless cell, whether formed by itself or not; it would suggest the idea that the little animal, or "polype," as it is called, is one thing, and the cell another and a distinct thing. But this is not the fact; the polype, the cell, and all the polypes and cells are spoken of as one zoophyte. (Fig. 8.) All the polypes are united together by the pith or medulla of the stem and branches. Each, while feeding itself, is procuring food for all; and the entire may be regarded as one organism, acquiring sustenance by the joint action of, perhaps, a thousand mouths. The repetition of an organ indicates an humble rank in the scale of animated existence. It did so in the many stomachs of the polygastric animalcules; it does the same in the multitu

In bringing this extract before my young readers, I do so, not only for the purpose of introducing them to an admirable work, from which the greater part of my own information is derived, them the example of its gifted author, who has but also for the higher purpose of placing before turned to such excellent account-in this, and in other departments of science-the snatches of leisure occurring in the life of a physician in extensive practice, who can scarcely call an hour his own. "Idleness," he justly remarks, "has no leisure." That one whose hands are full of business can make leisure, he has shown by his example; that he can turn it to good account, his science, but with the truest spirit of poetry and writings prove; for they are imbued, not only with devotion.

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sons, cells of larger size and of a peculiar shape are observable, (Fig. 9.) These contain the ova, or eggs, which, gifted in their more advanced condition with powers of locomotion, diffuse themselves through the waters of the ocean, and each becomes in turn the founder of a colony, more populous than the greatest city over which the eagles of imperial Rome ever floated.

On such subjects our ideas fall far short of the actual truth. Hear the statement of Dana, geologist of the United States' exploring expedition, as given in his work on the Structure and Classification of Zoophytes. "The first polyp with which the zoophyte commences thus gives out a bud, and this another, and so a succession is formed, and the little stem is gradually lengthened; branchlets grow out, and the plume or miniature tree is finally completed. The whole may be the work of a few weeks, or months, though they usually continue budding and growing for some years. Before the zoophyte has reached its limits in size, the number of polyps becomes immensely large. (Fig. 10). In a single specimen of Plumularia (P. angulosa), collected by the

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light. They do so when struck or otherwise irritated, appearing like so many diamond sparks. Every polype seems to have the power of emitting or withholding the light at pleasure; and when the trawl of the fisherman is drawn at midnight, or groves of the large tangle are disturbed by the dredger, the phenomenon is eminently striking and beautiful. Crabbe, whose poetry evinces minute accuracy in all its delineations of nature, animate or inanimate, has described this appearance; but to all my young friends who live near the coast, I would say, "Go and see it for yourselves." It has been already stated, that the present order derives its name from the polypes having a resemblance to the hydra, the species most celebrated. But other polypes present a star-like figure, and from this circumstance they are formed into a group or order distinguished by a term expressive of this resemblance, namely, "Asteroida." Of these I shall speak in the next paper.

of these periods, yet there is no point of time at which we observe a natural division or line of demarcation between them, The daylight fades into twilight, and darkness spreads her cloak so stealthily, that we cannot say when she began "to hang her spangled mantle o'er our heads.”

The light robes of spring slowly assume the gaudier hues of summer; summer insensibly fades into autumn; autumn unobserved is transformed to winter; while from out the snows of winter peep spring flowers again, In like manner, we do not find that Nature is guided by the almanack in those changes of weather which are associated with particular months. If during a long course of time it was found that in January we had frost and snow; in February a thaw; in March wind; and in April that we were favoured with warm showers-we should naturally think of snow as the characteristic of January; of thaw as associated with February; of wind as connected with March; and we should expect to have a repetition of showers and sunshine in April. But there are no days

TERRESTRIAL PHENOMENA OF on which the changes from frost to thaw,

THE MONTHS.

FEBRUARY.

"Muttering, the winds at eve, with blunted point
Blow hollow, blustering from the south subdued.
The frost resolves into a trickling thaw,
Spotted the mountains shine; loose sleet de-

scends

And floods the country round. The rivers swell, Of bonds impatient. Sudden from the hills, O'er rocks and woods, in broad brown cataracts,

A thousand snow-fed torrents shoot at once; And, where they rush, the wide resounding plain Is left one slimy waste."

"He giveth snow like wool: he scattereth the hoar-frost like ashes. He casteth forth his ice like morsels; who can stand before his cold? He sendeth out his words and melteth them; he causeth his winds to blow, and the waters flow."

THERE are not in nature any of those artificial divisions and distinctions which men for their convenience have established. Though we speak of day and night, of winter and summer, of spring and autumn; and though we may contrast the features * "See, as they float along, th' entangled weeds Slowly approach, upborne on bladdery beads; Wait till they land, and you shall then behold The fiery sparks those tangled fronds unfoldMyriads of living points; th' unaided eye Can but the fire, and not the form descry." The Borough, Letter IX.

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from stillness to wind, from settled to changeable weather, can be expected to occur. The beginning of each month usually resembles, in its terrestrial phenomena, its predecessor. We generally experience a continuance of January weather at the beginning of February, while at the end we are rejoiced to note the symptoms of approaching spring. At the beginning we have frost and snow, then comes a thaw, and this is commonly followed by the 'piping strains of March," which begin to blow ere yet February has expired. The commencement of the month is wintry; but towards its close the crocus and snowdrop, and the sallow, show their flowers; the ringdove begins to coo, and the ants venture forth from their curious habitations; the new life of vegetation begins to be seen on warm sheltered banks. Hence the Saxons called February Sprout-kele, because the cabbage or kale then began to fill its buds. The woodlark and the thrush begin their songs, and "the rooks commence their political arrangements for their cawing session;" the mole enlarges his hunting grounds, and the field-crickets open their doors as if to invite the approaching spring.

Yet, for the most part, February is a slow, dull time to those who do not possess such sources of pleasure in themselves, as to be beyond the depressing influences of foggy air, sloppy paths, and dropping skies. The weather seems to have all the discomforts of winter, without its compensatory advantages. The freshness of the frosty air, with its clear bright sky, no longer invigorates; a chilly mist hangs heavily in the atmosphere, and everything puts on a worn and melancholy aspect. The crisp snow has lost its brilliant whiteness, and has been changed by a thaw to a sloppy mass, as unpleasing to the eye as it is ungrateful to the feet. The walls of the house are covered with moisture like a heavy dew, and the cold seems more penetrating than it was when the thermometer was five or ten degrees lower. The birds sit disconsolate upon the trees, and even the robin is less cheerful than usual. From the leaves of the holly and the ivy, and from the twigs of the blackened trees, drops of icy water are pendent, and the moisture which falls from the eaves freezes as it splashes on the ground.

The sun's heat is the chief cause of warmth on the earth's surface, but there is a supply of heat also from the central matter of our planet. As, however, the substance of the earth is an imperfect conductor, the warmth which is derived from the sun's rays penetrates nowhere above 100 feet, and that which is due to the central heat produces little effect upon the crust of our planet. If we dig down about 60 feet from the surface of any part of the world, we find the strata there to possess the temperature of the average warmth of the climate of the country above them; if we dig deeper, however, we find the earth grow warmer as we descend, at the rate of about one degree of Fahrenheit's thermometer for every fifty-four feet. The principal causes of the difference in climate in countries appear to be the amount of solar heat, elevation, position with reference to continents or seas or mountains, aspect, direction of prevailing winds, geological peculiarities, and the state of cultivation. In winter, in the northern hemisphere, we receive fewer of the sun's rays, and those during a more brief period than in sumSome years ago a number of observations mer. The rays of the sun falling obliquely were commenced, the object of which was upon us, are, so to speak, spread out over to record the temperature-as indicated a larger space than in the tropics, where by Fahrenheit's thermometer-at certain they fall perpendicularly. From this cause, hours every day, with a view to ascertain and also from the length of the tropical in what degree the average or mean tem- day, the temperature there is always high. perature of any given month might vary. The heat derived from the sun, therefore, From these observations it was discovered decreases towards either pole. But the that there was little variation in the average mean temperature, or general climate of heat or cold of any month, compared with any place, is affected in a great degree by itself through a long series of years. The the other circumstances which have been mean temperature of Febuary is 38 deg. mentioned. For instance, since the higher Fahr., while that of January is scarcely 2 we ascend from the earth, the more rare deg. lower. The average temperature the air becomes; and as, moreover, aà so varies with position, and the observations expanded requires more heat to warm it, to which allusion has been made, apply so we shall find that the cold is greater the only to the neighbourhood in which they greater the elevation. Thus it happens, were made. This variation of temperature that even in the torrid zone there are is regular with reference to position; and mountains capped with snow. In all parts the average temperature of any place of the world, there is a point of elevation having been ascertained during ten years, where snow would remain unmelted for would be found to vary very little during ages. Places which are situated near large the next ten years following. The cli- bodies of water, have a less variable tempe mate of no two places can be said to be rature than those which are situated in the the same, even in the same latitude, but the interior of continents; for in summer weather has certain general characteristics evaporation makes the sensible heat latent in every place every year. There is, there- in the vapour of water, while in winter that fore, a regularity in what appears most ir-vapour becomes condensed, and gives out regular. its latent heat to the air. Moreover, as

described in a previous paper, when water is cooled it becomes specifically heavier, and exposes its warm particles to the atmosphere, till its whole mass is reduced to forty degrees, thus supplying a steady source of warmth. Earth, on the other hand, rapidly absorbs heat, but transmits it very slowly; and so we find that the heat of the sun accumulating in the crust of the earth is readily given off by radiation. Hence, places situated in the interior of continents experience great warmth in summer, and severe cold in winter. So remarkably are the differences of climate dependent upon situation, that we find the mean winter temperature of Edinburgh is 28.5°, while that of Moscow is only 15°, though these places are both in the same latitude. In our own climate, the greatest heat is not at midsummer, nor the lowest at mid-winter; nor is noon the warmest part of the day, nor midnight the coldest portion of the night. This is because the warming influences, or the reverse, do not act immediately, but produce their effects according to the time they are in operation. The day is hottest about two o'clock, and the coldest part of the night is that which occurs an hour before sunrise.

The aspect of any situation is well known to exercise a great influence upon its temperature, and the gardener makes use of his knowledge of this fact in placing his fruit-trees on the walls. That which is true of a garden wall applies upon an extended scale to the slope of a country or its aspect. Thus we find the climate at the same altitude on the two sides of the Alps of a strikingly different character, the one is sheltered from the northern blasts and exposcu to the sun, while the other has a comparatively small portion of the sun-rays, and is chilled, moreover, by the cold winds from the north.

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earth "as with a garment" during severe cold, and yet so wisely contrived to pass away, and by its melting to fertilize the earth as soon as a warmer atmosphere is spread over the fields. It is recorded that "in Holland during the winter of 1776, the surface of the earth was frozen to the depth of twenty-one inches on a spot of garden ground kept free from snow, but only to nine inches on an adjacent spot, covered with four inches of snow." The Esquimaux have discovered this quality of snow, and make use of it for building houses; and "when the lamps are lighted and the hut full of people and dogs, a thermometer placed on the net over the fire indicates a temperature of 38 deg. ; when removed two or three feet from this situation it falls to 32 deg., the temperature of the open air at the time being 25 deg. below zero.

In the Arctic regions what is called "red snow" is sometimes found, and excites some alarm among the superstitious. It appears to be common snow coloured by oxide of iron, in a state of extremely minute division, and a vegetable principle, belonging to some lichen of a resinous character, and of an orange-red tint. The colouring matter is stated to penetrate to various depths, and is found to consist of exceedingly minute globules when examined under the microscope.

While snow is lying on the ground an interesting experiment may be performed, showing the different powers of colours to reflect or absorb heat. Procure some small pieces of kerseymere cloth, of equal fineness and size, seven of them having the prismatic colours, and of the others one black and the other white. Lay them in the sunshine an inch apart upon snow, and leave them in that position for a short time; then observe how much the snow has melted beneath each piece of cloth, and how deeply each slip has sunk below the level of the surface. The black will be found to be the deepest, and the others in the following order :-violet, indigo, blue, green, red, orange, yellow; the snow beneath the white cloth will be unaffected. "Snow like wool," is not only correct By the aid of the information derivable as an ordinary metaphor, in which things from this experiment, we may answer the alike in appearance are compared; snow practical question-what colour is best resembles wool in its properties as a non-adapted for clothing at particular times of conductor of heat; and, indeed, nothing the year, since it is evident that warmth or could be so well adapted to protect the coolness depends not only upon the mate

The lowest mean temperature is found in North America, in 100° W. long., and in Siberia, in 95 E. long. These are known as "poles of cold." The average temperature of the former is-3.5 deg. Fahr., and of the latter-1° Fahr.

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