THE ARCTIC SEAS--THEIR CHARACTER, SCENERY, AND ATMOSPHERICAL ILLUSIONS.

There is a tendency on the part of most writers on the subject of Polar

Regions--especially compilers--to dwell disproportionately on the gloomy

side of the picture; insomuch that readers are led, not to over-estimate

the grand and the terrible aspects of the polar oceans, but to

under-estimate the sweet and the beautiful influences that at certain

periods reign there.

We quarrel not with authors for dwelling on the tremendous and the

awful. Too much cannot be said on these points; but while they do not

by any means paint the dark side of their picture too black, they fail

to touch in the lights with sufficient brilliancy. We have had some

personal experience of the arctic regions, and have found it extremely

difficult to get many persons--even educated men and women--to

understand that there _is_ a summer there, though a short one; that in

many places it is an uncommonly hot and excessively brilliant summer;

and that the sun, as if to make amends for its prolonged absence in

winter, shines all night as well as all day, blazing on the crystal

icebergs and pure snow (which _never_ disappear from those seas) with a

degree of splendour that renders the far north transcendently beautiful

and pre-eminently attractive.

We admit freely that the prevailing character of arctic seas, during the

greater part of the year, is dark, gloomy, forbidding. But this is the

very reason why their brief but cheering smiles should be brought

prominently into the foreground, and, if they cannot in justice be dwelt

on long, at least be touched upon with emphasis.

Why, in some of our cyclopaedia accounts of the realms of "thick-ribbed

ice," so much prominence is given to "the horrors and wide desolation of

the scene," and so much graphic power is expended in working up the

reader's imagination to a conception of the dreadful dangers and the

appalling terrors that await the madman who should dare to venture

within the arctic circle, that persons who have not been there might

well be tempted to shrink in affright from the very contemplation of a

region in which there does not appear to be one redeeming quality.

We repeat, that we do not think the one side of the picture has been too

darkly painted,--but the other side has been painted too slightly.

At the same time, we would caution our readers against jumping to the

opposite extreme. The dark side of the picture is in reality out of all

proportion to the light. And we do not hesitate to state our confirmed

opinion, that the arctic regions are more interesting to read about than

pleasant to dwell in.

Having, then, defended the lights, let us commence our investigations

with the shadows.

Those oceans lying within the arctic circle exhibit phenomena so grand,

so wonderful, and so varied, that they claim distinct and separate

treatment from the ocean as a whole. Here the extreme cold acts with

such power, and produces such extraordinary results, that it is

difficult to find words or similes by which to convey a just conception

of nature's aspects to the general reader.

During nearly two-thirds of the year the arctic regions are under the

absolute dominion of winter; and for many weeks of that bitter season

they are shrouded with the mantle of a dark, sunless night. The entire

ocean is locked in the embrace of a covering of ice many feet thick, so

that its liquid aspect is thoroughly removed; and, owing to ice-masses

scattered over its surface, together with mounds of drifted snow, it

bears a much stronger resemblance to the land than to the sea. Gales of

wind sometimes sweep over those frozen plains in bitter fury, hurling

the snow into the air in vast eddying masses, and threatening

destruction to any living creature that may chance to be exposed to

them--not so much from their violence, however, as from the intense cold

of the atmosphere which is put in motion. But in regard to gales,

although there are no lack of them, they are neither so fierce nor so

frequent as are those of the torrid zone.

It might be supposed that in such a climate animal life could scarcely

exist; but such is not the case. The inhabitants of part of the arctic

regions, named Esquimaux (more correctly Eskimos, with the accent on the

last syllable), are a stout, hardy, healthy race and the polar bears,

foxes, wolves, seals, musk-oxen, walruses, etcetera, that dwell there,

seem to enjoy their existence just as much as do the animals of more

favoured and warmer climes.

During the short but hot summer of the arctic regions, the immense

masses of ice formed in winter are by no means cleared away. A great

part of the heat of early summer (there is no season there that merits

the name of spring) is spent in breaking up the solid crust of ice on

the sea, a large proportion of which is carried south by the currents

that flow to the equator, and melted long before they reach the

temperate zones. But a considerable quantity of broken ice-masses get

locked in narrow places or stranded on shallows; and although they

undergo the process of melting the whole summer, they are not much

diminished ere the returning frost stops the process and locks them in

the new ice of a succeeding winter.

Thus there is no period of the year in which large quantities of ice may

not be seen floating about in the arctic seas.

This fact it is that enables us to speak appropriately of the _scenery_

of the Arctic Ocean. And assuredly this scenery of the ice is

exceedingly and strikingly beautiful. The imagination cannot conceive

the dazzling effect of a bright summer day in those regions, when the

ocean is clear as glass, and ice-humps and ice-mountains of every shape

and size are glittering in the sun's rays with intense brilliancy, while

the delicate whiteness of these floating islands, and the magical

atmospheric illusions by which they are frequently surrounded, render

the scene pre-eminently fairy-like.

All the navigators who have penetrated into the arctic seas speak with

enthusiasm of the splendour of floating ice-masses. They take the most

curious and fantastic shapes; sometimes appearing like great cities of

white marble, with domes and towers and spires in profusion; sometimes

looming huge and grand like fortresses, and many of them with their

summits overhanging so much as to suggest the idea that they are about

to fall. This indeed, they often do, adding to the grandeur of the

scene, and not a little to the danger, should ships chance to be in the

neighbourhood.

The atmospheric illusions, before mentioned, are the result of different

temperatures existing within a few miles of each other, and which are

caused by the presence of large bodies of ice. The effect of this is to

cause the ice-masses on the horizon to appear as if floating in the air,

and to distort them into all sorts of shapes, even turning them upside

down, and thus affording to an innovative mind a most ample and

attractive field wherein to expatiate.

To ascertain the causes of facts and effects so curious must be

interesting to all who have inquiring minds. We will, therefore,

attempt to describe and account for arctic phenomena in the following

chapters as simply as may be.

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