scholarly journals The Notau harbour and the Kontor in Bergen

AmS-Skrifter ◽  
2020 ◽  
pp. 237-244
Author(s):  
Geir Atle Ersland
Keyword(s):  
Sixteenth Century ◽  
Fifteenth Century ◽  
North Sea ◽  
The South ◽  
Norwegian Coast ◽  
The North ◽  
The North Sea

The Hanseatic Kontor in Bergen was one of the main hubs of trade in the North Sea region. This paper explores a possibility suggested in a late sixteenth-century manuscript that the Norwegian Kontor for some time was also located at Notau, a place south of Bergen. It is argued that this written source might refer to the years 1427–33 when the Hanseatic merchants withdrew from Bergen because of an on-going war between King Erik and northern German princes. Notau is mentioned several times in sources from the fifteenth century and most of these references are related to Hanseatic activity. However, viewed in a broader context, Notau stands out as an important harbour on the south-western Norwegian coast, visited both by Norwegians and Hanseatics, as well as travellers from other regions.

scholarly journals Tunny Investigations made in the North Sea on Col. E. T. Peel's Yacht, “St. George,” Summer, 1933. Part I. Biometric Data

1934 ◽  
Vol 19 (2) ◽  
pp. 503-522 ◽  
Author(s):  
F. S. Russell
Keyword(s):  
North Sea ◽  
South Coast ◽  
Body Proportions ◽  
The South ◽  
Biometric Data ◽  
The North ◽  
The North Sea ◽  
Sea Fish ◽  
Made In

1. Details are given of the types of hooks lost in tunny in the North Sea in the summer of 1933.2. Data are given on the measurements made on thirty-two large migrating fish caught in the North Sea in August and September, 1933.3. In certain body proportions the tunny measured differ from those in the G4 Group (200 to 260 cm. in length) given by Heldt for fish from Tunis and by Frade for fish from Algarve on the south coast of Portugal, while in some characters they resemble the Tunis fish and in others the Algarve fish, but all the North Sea fish were between 232 and 271 cm. in length.4. It was found that there was a tendency for fish with short second dorsal fins to have short first dorsal, anal, and caudal fins, and for those with long second dorsals to have these other three fins long.5. Measurements were made to supply data on the condition of the fish.

scholarly journals III.—On the Structure of the Valleys of the Blackwater and the Crough, and of the East Essex Gravel, and on the Relation of this Gravel to the Denudation of the Weald

1866 ◽  
Vol 3 (26) ◽  
pp. 348-354 ◽  
Author(s):  
Searles V. Wood
Keyword(s):  
North Sea ◽  
Glacial Period ◽  
The South ◽  
Northern Boundary ◽  
The North ◽  
Complete Order ◽  
The North Sea ◽  
Boulder Clay ◽  
London Clay

In a paper in this Magazine, upon the structure of the Thames Valley, I endeavoured to show that instead of being, as had been asserted, a valley of similar structure to those of the Somme and Seine, and containing deposits of nearly similar order and age, the valley in which the Thames gravel was deposited possessed no outlet to what is now the North Sea, being divided from it by a range of high gravelless country; and that, in lieu of such an outlet, the valley opened, in more than one part, over what is now the bare Chalk country forming the northern boundary of the Valley of the Weald. I also endeavoured to show that all the deposits of the Thames Valley, except the peat and marsh clay, belonged to several successive stages, marking the gradual denudation of the Boulderclay, the lower Bagshot, the London Clay, and the subjacent Tertiaries, which had, at the end of the Glacial period, spread over the south-east of England in a complete order of succession: the sea into which this valley discharged occupying, what is now, the Chalk country of the Counties of Kent, Surrey, Sussex, and Hampshire, inclusive of the interval subsequently scooped out to form the Valley of the Weald: so that, not only was the latter valley newer than that of the Thames, and of the most recent of the Thames Valley deposits, except the peat and marsh clay, but that these deposits in themselves marked a long descent in time from that comparatively remote period of the Boulder-clay.

Cold Induced Abnormal Catches of Sole

1998 ◽  
Vol 78 (1) ◽  
pp. 345-347 ◽  
Author(s):  
J.W. Horwood ◽  
R.S. Millner
Keyword(s):  
North Sea ◽  
Cold Water ◽  
The South ◽  
Total Allowable Catch ◽  
The North ◽  
Solea Solea ◽  
The North Sea ◽  
The Uk ◽  
The Eu ◽  
Made In

Large catches of sole (Solea solea) were made in early 1996 from the south-western North Sea. Sole suffer physiological damage in waters below 3–4 C. In February 1996 cold water of 3–4 C unusually extended from the Continental coast onto the Dogger Bank. It is likely that the increased catches were due to the consequential distribution and behaviour of the sole, making them more susceptible to capture.Exceptionally large catches of mature sole (Solea solea (L.)) were made in February 1996 by Lowestoft fishermen from the south-western North Sea. Surprisingly this was not welcome. The UK allocation of the North Sea sole is -4 % of the EU Total Allowable Catch (TAC), and fishermen are restricted nationally, and by the fishing companies, to a tightly managed ration. The Lowestoft Journal (8 March 1996) reported the suspension of a local fishing skipper for not throwing back 5000 kg of sole caught in the Silver Pits. We will show that the abnormal catches were due to exceptionally cold waters.Sole in the North Sea are at the northern extremity of their range, with sole seldom living in waters below 5°C (Horwood, 1993). In fact, North Sea sole were successfully introduced into Lake Quarun, Egypt, where they lived in temperatures in excess of 30°C (El-Zarka, 1965). Young sole migrate from their shallow inshore nursery grounds, such as the Waddensea, as winter approaches (Creutzberg & Fonds, 1971).

scholarly journals Why do jellyfish bloom in Norwegian waters and what can be done to recover the ecosystems in the North Sea and on the Norwegian coast?

2017 ◽  
Author(s):  
Johannes Hamre
Keyword(s):  
North Sea ◽  
West Coast ◽  
Trophic Levels ◽  
The West ◽  
Fish Stocks ◽  
Norwegian Coast ◽  
The North ◽  
Key Species ◽  
Wide Range ◽  
The North Sea

The ecosystems with their relationships between fish species and stocks, have been established by evolution for millions of years, but during the last 50 years, the ecosystems in the North Sea and along the Norwegian coast have been changed fundamentally by fisheries. The North Sea mackerel stock has been depleted and its feeding grounds have been invaded by the Western mackerel which spawns west of Ireland. This stock is now very rich in numbers and occupies the North Sea, the Norwegian Sea and the western Barents Sea. If the trend continues, mackerel may outcompete many of the other fish stocks in the area. Traditionally and until the beginning of the 1970s, there was a large stock of sandeel spawning in the North Sea and on the Norwegian coast. Sandeel juveniles was an important food source for a wide range of species, including sea mammals and birds. The fact that this stock has also been overfished, may explain many changes observed in the ecosystem on the west coast of Norway, for example a large reduction in the populations of sea birds. There are several instances where ecosystems shift to sustain jellyfish blooms in response to depletion of forage fish stocks. This was registered in Namibia in the 1990’s, where the pilchard stock was decimated and the biomass of jellyfish soon became overwhelming. On the west-coast of Norway, there are now frequent blooms of jellyfish, yet another indication that a controlling factor is missing in the system, in this case sandeel, which is a key species in the transfer of nutrients from zooplankton to higher trophic levels in the area. In this paper, I give a description of the situation and some suggested measures that should be taken in fisheries management.

scholarly journals On the tides, bed and coasts of the North Sea or German Ocean

1854 ◽  
Vol 6 ◽  
pp. 201-202
Keyword(s):  
The Netherlands ◽  
North Sea ◽  
The Other ◽  
Great Similarity ◽  
Shetland Islands ◽  
Norwegian Coast ◽  
The North ◽  
The North Sea ◽  
The Baltic ◽  
Long Channel

The author commences his paper by remarking that great similarity of outline pervades the western shores of Ireland, Scotland and Norway, and then observes that the great Atlantic flood-tide wave, having traversed the shores of the former countries, strikes with great fury the Norwegian coast between the Lafoden Isles and Stadland, one portion proceeding to the north, while the other is deflected to the south, which last has scooped out along the coast, as far as the Sleeve at the mouth of the Baltic, a long channel from 100 to 200 fathoms in depth, almost close in shore, and varying from 50 to 100 miles in width. After describing his method of contouring and colouring the Admiralty chart of the North Sea, he traces the course of the tide-wave among the Orkney and Shetland Islands along the eastern shores of Scotland and England to the Straits of Dover, and along the western shores of Norway, Denmark and the Netherlands, to the same point.

scholarly journals The Spanish Pastoral Romances

PMLA ◽  
1892 ◽  
Vol 7 (3) ◽  
pp. 1-119
Keyword(s):  
Sixteenth Century ◽  
North Sea ◽  
Social Condition ◽  
Western World ◽  
Philip Ii ◽  
The North ◽  
The Pacific ◽  
The Social ◽  
The North Sea ◽  
The Church

The introduction of the pastoral romance into Spain in the middle of the sixteenth century, and the extreme favor with which it was received, may, in view of the social condition of the country, seem at first sight paradoxical. At the time of the accession of Philip II, Spain was at the zenith of her military greatness: her possessions were scattered from the North Sea to the islands of the Pacific; and her conquests had been extended over both parts of the western world. The constant wars against the Moors, during a period of over seven hundred years, and the stirring ballads founded upon them, had fostered an adventurous and chivalric spirit,—a distinguishing trait of the Spanish character. Arms and the church were the only careers that offered any opportunity for distinction, and every Spanish gentleman was, first of all, a soldier.

Oil Rig Disaster in the North Sea

1985 ◽  
Vol 1 (S1) ◽  
pp. 357-359
Author(s):  
Helge Bryne ◽  
Eilif Dahl
Keyword(s):  
North Sea ◽  
Oil Production ◽  
Oil Field ◽  
Mobile Platform ◽  
Norwegian Coast ◽  
Drilling Rig ◽  
The North ◽  
Production Platform ◽  
The North Sea ◽  
Oil Rig

Since oil was found under the North Sea in the mid 1960's, oil production now plays an important part in Norwegian economy. A major oil field isEkofisk, between Norway and Britain (Figure 1). TheAlexander Kielland, one of the rigs atEkofisk, was a mobile platform of the pentagon type, floating on 5 columns, 150 nautical miles of f the Norwegian coast. It was developed and built as a drilling rig, but was used as an accommodation platform since delivery in July 1976. OnMarch27,1980, theAlexander Kiellandrig lay at anchor on theEkofisk field, close to the production platform EDDA.

Layers of practice, theory and experience at East Lodge

2004 ◽  
Vol 8 (1) ◽  
pp. 14-25
Author(s):  
Roger Stonehouse
Keyword(s):  
Nineteenth Century ◽  
North Sea ◽  
Practice Theory ◽  
The South ◽  
Poor Condition ◽  
The North ◽  
The North Sea ◽  
Newcastle Upon Tyne

Located in Northumberland, 35km north of Newcastle-upon-Tyne and 3km from the North Sea, the mid-nineteenth-century East Lodge to Togston Hall was originally a simple, linear, rectangular single-storey cottage of whinstone with a dual pitch roof. It had acquired an accumulation of ugly, pebble-dashed, flat-roofed extensions to the south and was in poor condition.

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