PREFACE

A brief article on Snow-flakes, in one of the periodicals published

by the American Tract Society in the winter of 1862-3, accompanied by

a cut exhibiting some of their forms, elicited from its readers many

expressions of interest, and suggested the preparation of a book on

this curious but generally little-known subject.

The beautiful forms of many of the snow-crystals were observed and

sketched more than a century ago. The _Transactions of the Royal

Society of London_, for 1755, contain representations of ninety-one

varieties, with descriptions by Dr. Nettis. Captain William Scoresby,

the eminent English navigator, has given, in his _Arctic Regions_,

drawings of ninety-six varieties. More recently, numerous specimens,

with accompanying descriptions, have been given to the public by

James Glaisher, Esq., of Lewisham, England. It is from these sources,

chiefly, that the figures here exhibited have been derived.

It has been no part of our design, in this work, to enter into any

scientific statements concerning the snow-flakes, or the laws of their

formation. A brief general description of them is all that has been

attempted. Yet the reader should not, from this, infer that there is

any question respecting the truthfulness of the sketches. The drawings

were originally made with scientific precision, and have been carefully

copied. A few simple figures at the top of page 11 are designed to

show the primary geometrical _forms_ under which the snow-vapor

crystallizes. With that exception, they are all representations of

individual crystals, actually observed and sketched with the aid of the

microscope.

It is proper to add, however, that these representations are highly

magnified, especially those on the last two or three plates. The real

size of the crystals observed by Scoresby varied from one thirty-fifth

to one-third of an inch in diameter. Dr. Nettis remarks: “The natural

size of most of the shining, quadrangular particles, and of the little

stars of snow, as well the simple as the more compound ones, does

not exceed the twentieth part of an inch.” The dimensions as well

as form of the crystals seem to depend upon the amount of vapor in

the atmosphere, the temperature, and other circumstances not easy to

specify.

We may be permitted to express the hope that many of our readers will

examine for themselves these beautiful productions of nature. In our

own climate, the “treasures of the snow” are open to all who choose to

explore them; and there can scarcely be an amusement more entertaining,

and at the same time instructive, than that of observing and sketching

these delicate crystals. No expensive or complicated apparatus is

needed for this purpose. A good microscope is the chief requisite;

besides which, a pair of dividers and a rule will be sufficient. We

subjoin a statement from Mr. Glaisher of his own mode of making his

examinations.

“For the information of those who would carefully observe

snow-crystals, I may remark that my own plan of procedure is to expose

a thick surface of plate-glass on the outer side of the window, resting

on the ledge. Seated within the room, I am enabled, with comparative

comfort, and at my leisure, to make my drawings and record my

observations, the accuracy of which I am able to verify to my

satisfaction, as the crystal received upon the cold surface of the

glass, itself several degrees below freezing, remains a sufficient

length of time for the requirements of the observer. In many cases, it

becomes frozen to the glass, and is thus secured from the influence of

the wind, which not unfrequently snatches away some most intricate form

from the desiring eye of the observer.”

If this work shall be the means of introducing any of our readers to

the knowledge of this interesting department of the Creator’s works,

and eliciting those sentiments of admiration and reverence which his

wonder-working power should inspire in every beholder, it will not have

been issued in vain.

Snow-flakes · 第 4 / 17 题