General: Bjørnøya (Bear Island) is the southernmost island of the Svalbard archipelago, halfway between Norway and Spitsbergen. The island is 178 km2 large and relatively rarely visited, but fascinating. There is a permanently staffed Norwegian weather station at the north coast of the island. The lack of protected bays and the rough weather with strong winds and frequent fog make visiting Bjørnøya a bit of a lottery. Bjørnøya was declared a nature reserve a few years ago, there are according regulations and access to some areas is restricted. These are hatched on the map below: the area around the huge bird cliffs at the southern end of the island may not be entered between April 01 and August 31, except boats shorter than 40 feet that may approach from the sea. (As of January 2013, changes are currently not expected, but double-check with the Sysselmannen (gouvernor) of Svalbard for officially confirmed, up-to-date information if you plan to visit.)
Bear Island (Bjørnøya). Bird sanctuaries are hatched (more information in the text above).
In the past, Bjørnøya was often surrounded by drift ice in late winter (mainly March-May), but usually ice-free during the summer months. These days, the drift ice reaches rarely so far south.
Geology: Varied. Partly basement rocks (Silurian and older), partly younger sedimentary cover (Devonian and younger). There are Devonian sediments in the northeastern part of Bjørnøya, which include coal seams. These belong to the oldest coal seams on Earth, as plants, without which there can’t be any coal formation, just started to move on dry land. There are various Mesozoic sediments in the southeast.
Horizontal layers of sand- and siltstone at Teltvika, Kapp Dunér.
Recommended book for further, well-digestable (really!) info about geology and landscape of Svalbard.
Landscape: Landscape-wise, Bjørnøya is unique within Svalbard. The unglaciated interiour of the island is gently sloping, reaching higher altitudes from north to south, culminating in the south and southeast (Miseryfjellet, 536 m high). The coasts are quite spectacular. There are only few bays and beaches, but high, near-vertical cliffs, which are highest at the southern tip. There are several characteristic rock columns (Sylen, Stappen and other ones) and caves, all created by the constant surf.
Stappen, an impressive sea stack at the southern tip of Bjørnøya.
Sylen, another sea stack near the southern tip of Bjørnøya.
These cliffs are home to some of the largest seabirds colonies of the North Atlantic.
The interiour of Bjørnøya is very barren and vegetation is mostly lacking. Next to endless rocks plains, there is a large number of lakes. In some of these, toxis substances have accumulated in worrying concentrations in recent decades. These contaminants have been brought to the Arctic from industrial countries in Europe and North America by oceanic and atmospheric currents.
Bjørnøya: barren land and fog
Flora and fauna: The interiour of Bjørnøya is largely devoid of life, apart from the fauna of some of the lakes. Some of them have Arctic char, which is mostly small, but some cannibalistic individuals have reached considerable size. An ornithological specialty is the Great northern diver. This large bird is very rare on the east side of the Atlantic, it is breeding in Greenland and mostly in northern North America, but a pair has found a home near a lake in the northeastern part of Bjørnøya. Accordingly, the lake was declared a no-go-area, much to the annoyance of the staff of the weather station, as they lost a popular destination which they had used for fishing.
Biologically the most important parts of Bjørnøya are the steep coastal cliffs with their enormous seabirds colonies, especially in the southern half of the island. Here, hundreds of thousands of guillemots, both Brünich’s and Common, are breading next to each other. These birdcliffs are amongst the largest ones of the northern hemisphere. Fishery as well as the oil industry may threat these important breeding sites in the future. The island itself is protected, but the economical exploitation of the surrounding seas is likely to happen. There is a large fishing fleet in the area.
The population of the Common guillemot in Bjørnøya collapsed dramatically in 1986, because some important fish species had been overfished regionally. The Brünich’s guillemot with its more diverse menu was not affected, but the Common guillemot has not yet completely recovered.
The mammal fauna is rather scarce. The polar bear, who gave Bjørnøya its name, pays only occasional visits to the island, when it is surrounded by drift ice during the winter. There were enormous walrus colonies in the past, which have been wiped out completely since the early 17th century.
Brünich’s guillemots near the southern tip of Bjørnøya (Bear Island). (2)
History: Bjørnøya was the first island of the Svalbard archipelago which was discovered by the Dutchman Willem Barentsz during his famous third voyage. Barentsz reached the island on 10h June 1596 and named it ‘Beeren Eylandt’ (English Bear Island, Norwegian Bjørnøya) as they had a dramatic fight with a polar bear during their first visit to the coast.
The island has a long history. Pomor hunters as well as Norwegian trappers have wintered there many times. In the late 19th century, the German journalist and self-declared polar expert Theodor Lerner claimed parts of Bjørnøya, but did not establish any long-term activities due to lack of capital (he intended to establish a coal mine). Later, a Norwegian company started coal mining at the northeast coast. These activities were mostly not economical, and in the 1920s the Norwegian state bought the shares.
‘Hammerfesthuset’ (to the right) in direct neighbourhood to the weather station: the oldest house within the whole Svalbard archipelago which is still standing. Today the party location of the station.
During the Second World War, Germany established a weather station here for a couple of months, but with little success.
Later, Norway kept a station, which is still operating today.