Imagens das páginas
PDF
ePub
[merged small][subsumed][subsumed][ocr errors][merged small][ocr errors][graphic][merged small][merged small][merged small][merged small][merged small][merged small][merged small][merged small][ocr errors][merged small][merged small][merged small][merged small][merged small][merged small][merged small][merged small][merged small]

ANTH. B. NILSEN & CO. LTD. Aksel Holmsen

OSLO, NORWAY

ESTABLISHED 1879

[merged small][merged small][merged small][ocr errors][merged small][merged small][merged small][merged small][merged small]

OSLO, NORWAY

EXPORT

Trade Mark

Cable Addr. „Speilemalj"

EXPORT

Registered

SILVER-FILIGREE & ENAMEL-FACTORY

DIPLOM d'HONNEUR

WORLDS EXHIBITION RIO DE JANEIRO 1923

As Pettersen & Sønner

OSLO AND LARVIK

Telegr.adr.: Marmorgranit

[blocks in formation]

Den norske Creditbank

ESTABLISHED 1857

OSLO

[ocr errors]

Telegraphic address: „Creditbank"

Share Capital Kr. 44.000.000,-
Reserve Funds Kr. 25.000.000,-

Branches:

ARENDAL
LILLESAND
RISØR

Banking and Exchange Business of every description
Correspondence invited

[ocr errors]

Proprietors of: Nitroglycerin Compagniet, Oslo. A/s Haaöen Fabriker, Oslo. Nordenfjeldske
Sprængstof A/s, Trondhjem. Norsk Svovlsyrefabrik A/s, Oslo. Nitedals Krudtverk A/s, Oslo.

NORSK SPRÆNGSTOFINDUSTRI S

[graphic]
[ocr errors]
[ocr errors]

Blasting Gelatine, Safety Explosives, Dynamite of all Kinds, Guncotton, Pyroxylin, Trinitrotoluol, Smokeless Powder, Black Powders, Cartridges, Detonators, Safety Fuses, Sulphuric Acid, Oleum &c.

FARRIS

If you have any difficulty in obtaining Farris
write for Price List, etc.

The Norwegian Royal Table Water

FARRIS is a natural mineral water bottled only at King
Haakon's radio-active alkaline mineral spring at Larvik
Spa, Norway.

FARRIS is the best natural mineral table water in the
world.

FARRIS has, since 1876, when the spring was discovered, been used with great success in the treatment of gout, rheumatism and catarrh.

FARRIS is absolutely pure, and free from all organic matters and bacteria.

FARRIS is exceedingly soft, pleasant and refreshing. FARRIS is a most excellent beverage for blending with your favorite drink, being free from iron.

FARRIS has been awarded Gold Medals wherever and whenever it has been exhibited.

[graphic]

FARRIS AS

[blocks in formation]

Larvik and Oslo

[blocks in formation]

SARDINES

FISH OILS

CEMENT

[graphic]
[ocr errors]

NORWAY

ETC.

RAW MATERIALS FOR THE NORWEGIAN INDUSTRY ETC.

CORRESPONDENCE INVITED

[graphic]

TRADE REVIEW

Published by the Press Bureau of the Ministry of Foreign Affairs, Norway

[blocks in formation]
[ocr errors]

Coal.

[ocr errors]

8TH YEAR OF ISSUE

-

Norway and

CONTENTS: Svalbard (Spitzbergen). Natural Features and History.
Other Natural Resources.
Svalbard. Treaty Relating to Spitzbergen, Legislative Measures. Svalbard as a Tourist Land.

-

-

[ocr errors]
[merged small][graphic]

In addition, the following islands are regarded politic-
ally as belonging to Spitzbergen. Bear I., Hope I.,
Giles Land, and King Karls Land.

Spitzbergen, a group of Arctic islands, comprises larger one. To the west lies Prince Charles Foreland.
four large islands and a few small ones, and has a
total area of approximately 25 000 sq. miles, that is,
about the same area as the Irish Free State or as
Holland and Belgium combined.

Since Norway assumed sovereignty this group of
islands has been given its old name of Svalbard.

The largest of these islands is West Spitzbergen.
It is intersected by several large fjords, which with
their many branches penetrate deep into the land
from north to west. North-East Land is slightly
smaller, and is separated from West Spitzbergen by
a narrow strait. East Spitzbergen consists of two
islands, Barents I. and Edge I., the former being the

The distance from Norway to West Spitzbergen is
approximately 1600 miles, and Bear Island lies about
midway.

The position of these islands in 80° N. conditions
a very severe climate; but, owing to the fact that the
Gulf Stream projects an arm northwards along the
west coast of Spitzbergen, the fjords generally remain
free from ice from May to October, and the thermo-
meter may stand at 5° above zero (Centigrade) dur-
ing the summer months. Towards the east, however,

NORWEGIAN TRADE REVIEW

the temperature is lower. The interior and the eastern islands are covered by great masses of ice, only the highest mountain peaks projecting above them. The waters along the east coast are navigable only in occasional years. In these regions the drift ice is carried by the current from the north and almost as far as Bear Island.

The west coast of Spitzbergen presents a picture of precipitous, snow-decked heights towering over an ice-clad land. Between these peaks glaciers protrude here and there towards ice-free shores, where they ultimately break asunder and plunge into the sea.

These mountains are not of exceptional height, although some few peaks reach 4 700 feet. The glaciers are not so extensive as those in Greenland. To the south of Ice Fjord there is a chain of mountains running along the coast, and these parts favour vegetation to a certain extent. On the east side the northern regions are also covered by inland ice.

The drift ice round the coasts is generally wrapped in mist, so that the land is not visible until the ship lies close under the mountainous coast. Later on in the autumn it is difficult to find water in these islands, for the rivers and streams freeze to the bottom, and ordinary springs do not exist. In the mining camps it is usual to secure a floe of drift ice by mooring in on the beach; lumps are then broken off as required and melted.

The Svalbard archipelago is connected with the European Continent by a submarine ridge. If the surface of the sea were to sink 110 yards Bear Island would then be joined to Spitzbergen. Between Norway and Svalbard the depth is nowhere above 650 yards. In remote ages Svalbard was geographically and geologically united to Norway. A little to the west of Svalbard, however, the bed of the sea makes a steep plunge to a great depth.

In the Icelandic annals for the year 1194 mention is made of the discovery of «Svalbard». Different views have been held as to the meaning of this reference, but the generally accepted opinion now appears to be that the Svalbard thus recorded must have been Spitzbergen.

Svalbard was subsequently rediscovered by the Dutch in 1596, during their attempts to find a passage to China north of Novaya Zemlya. The islands were visited in later years by whaling expeditions from many countries, and the fact that this land remained unoccupied gave rise to numerous conflicts. The vessels engaged in these expeditions were armed in order to secure whaling grounds, and there was constant fighting and even diplomatic complications between the rival forces. Following a compromise the coast was divided in 1618 into several zones.

despatching warships to those waters and also by making diplomatic representations to the powers.

The King primarily based his contention on the view generally held at that period, namely, that this new land constituted a geographical portion of the old Norwegian tributary country of Greenland, which in those days was presumed to extend northward round the «havbotn» and eastward towards Novaya Zemlya; and secondly, also on the supremacy of the old Norwegian kings over the Arctic, which was at that time recognised in principle. With reference to this claim a communication made to the French ambassador in 1634 contains the following: «All the islands in the Northern Seas have from ancient times been subject to the Norwegian Kings, who with their victorious arms and well-equipped fleets have subdued the northern coasts and the adjacent seas».

Norway's supremacy was maintained also in communications from Christian IV to the kings of Great Britain, France, and Spain, to the Spanish Netherlands, and to the Netherland States-General of February 18, 1616, in which he stated that whaling operations carried on by foreign nations at Spitzbergen would be permitted in the future only upon the understanding that his supremacy was recognised, and that licences were taken out and the proper dues paid for such whaling catches.

With regard to the arrangement arrived at between the interested countries, it can hardly be said to reflect any general recognition of Norway's supremacy over Spitzbergen. The action of the Dano-Norwegian King in nevertheless accepting this agreement must have been taken out of regard to good neighbourship and to the disadvantages of keeping the dispute going on indefinitely.

But whereas a clear conception of the supremacy of the Norwegian Crown over Svalbard prevailed in the seventeenth century, and continued to live in the eighteenth, it seems to have practically died out in the nineteenth century.

The first occasion on which this question arose was at a cabinet meeting at Stockholm in 1871, when the joint Swedo-Norwegian Foreign Minister urged that the Spitzbergen archipelago ought to be placed either under Swedish or Norwegian rule. Owing to its geographical position it must however naturally be regarded as belonging to Norway.It was proposed that the powers whose subjects visited these regions should be communicated with, and that a statement on the subject should be obtained from the Norwegian Government. This statement was to the effect that in the event of the question ever being raised of placing Svalbard under the dominion of any particular country, that country ought to be Norway. Favourable replies were received from all the foreign powers communicated with, except Russia, who expressed the desire that this group of islands should continue to be regarded as territory without any definite owner. It was resolved that the question of taking possession

During these conflicts, which were mainly between English and Dutch whalers, the Dano-Norwegian King maintained Norway's sovereignty over the country, and endeavoured to enforce this claim by

[graphic][subsumed][ocr errors][subsumed][subsumed][subsumed][subsumed][subsumed][subsumed][subsumed][ocr errors][subsumed][subsumed][subsumed][subsumed][ocr errors][subsumed][ocr errors][subsumed][subsumed][subsumed][subsumed][ocr errors][subsumed][subsumed][subsumed][subsumed][subsumed]
« AnteriorContinuar »