Jökull

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Jökull - 01.12.1993, Qupperneq 60

Jökull - 01.12.1993, Qupperneq 60
N.N. 1884. MagnetischeBeobachtungenauf undbei Island. Annalen der Hydrographie Bd. XII, 572 (tekið upp úr "Notice to Mariners"no. 61/185, Washington 1884). N.N. 1898. Den Islandske Lods. Det Kongelige Sökaart- Archiv, Köbenhavn, 134 bls. Aðrar útgáfur: 1891 (sjá skrárÓlafs Davíðssonarí Skírni), 1903, 161 bls. 1911, 204 bls. 1917, 208 bls. 1927, 207 bls. V. Raulin 1866. Quelques vues generales sur les variations secularies du magnetisme terrestre. Actes de la Société Linnéenne de Bordeaux, XXVI, 137-228. Reichs-Marine-Amt 1908. Segelhandbuch fiir die Insel Is- land. Zweite Auflage, Berlin, 239 bls. E. Sabine 1872. Contributions to terrestrial magnetism. - No. XIII. Philos. Trans. RoyalSoc. 162, 353-433. D.H. Tarling 1989. GeomagneticsecularvariationinBritain during the last 2000 years. I: Geomagnetism and Pala- eomagnetism, ritstj. F.J. Lowes o.fl., 55-62. Kluwer Acad. Publ., Dordrecht. W. F. Wallis & J.W. Green 1947. Researches ofthe Depart- ment of Terrestrial Magnetism, vol. VIII: Land and Ocean Magnetic Observations, 1927-1944. Camegie Institution ofWashingtonPublication 175, bls. 137,217, 234. R. Wallut 1884. Observations sur le magnétisme terrestre en Islande. Revue Maritime et Coloniale 81, no. 272, 387-399. C.F. Wandel 1879. Bemœrkningertil Beseilingen af Islands Kyster. C.C. Loses Bog- og Musikhandel, Kpbenhavn, 30bls. J.F. West (ed.) 1976. Diary of John Baine. The Journals of the Stanley Expedition to the Faeroe Islands and Iceland in 1789. Vol. 3. F0royaFróðskaparsetur,Tórshavn, 213 bls. C. Wille 1882. Magnetiske Observationer, kafli 2 í H. Mohn & C. Wille: Den Norske Nordhavs-Expedition 1876- 1878. Christiania. Alþýðlegfrásögnumþessaleiðangra birtist í tímaritinu Vidar 1888, bls. 1-39. Zeilau, Th. 1861. Fox-expeditionen i Aaret 1860. Fr. Wpldike, Kpbenhavn, 197+32 bls. og 5 kort. Zmuda, A.J. (ed.) 1971.WorldMagneticSurvey 1957-1969. IAGA Bulletin no. 28. IUGG Publications Office, Paris, 206 bls. Þorsteinn Sæmundsson 1969. LeirvogurMagnetic Observa- tory 1957-1968. Fjölrituð skýrsla, Raunvísindastofnun Háskólans, 31 bls. og 5 kort. Þorsteinn Sæmundsson 1974. Measurements of D and H near Reykjavík. Leirvogur Magnetic Results 1972. Fjölrituð skýrsla RH/G/74/B1, 93-97. Þorsteinn Sæmundsson 1988. Leirvogur Magnetic Results 1987. Raunvísindastofnun Háskólans, fjölrituð skýrsla RH-17-88, 94 bls. Þorsteinn Sæmundsson 1990. Leirvogur Magnetic Results 1989. Raunvísindastofnun Háskólans, fjölrituð skýrsla RH-09-10 94 bls. Viðbót í prófórk: Auk ofangreindra heimilda um mælingar P. Löwen- öms við Island, er þeim lýst stuttlega í Gilberts, Ann. der Physik, 29, 438-441, 1808. SUMMARY MAGNETIC DECLINATION MEASUREMENTS IN AND AROUND ICELAND This paper describes various properties of the present geomagnetic field, including the magnetic declination which has been used for navigation purposes for many centuries. Measurements of the declination were made by various expeditions to Ice- land since about A.D. 1750 or possibly earlier, but documentation on their results is scattered, and little is known of the methods used or their accuracy. Such measurements turn out to be much more useful when made at sea than on shore in Iceland, because of the large disturbing effects of magnetic remanence in local basalt rock formations. A list of declination measurements, based on original compilations by Th. Sigurgeirsson and Th. Sæmundsson, is provided in the paper. The most valuable series of observations in the Iceland area include those of P. Löwenörn in the 1780’s, as well as French measurements from the period 1830-1900. The only aeromagnetic survey of Iceland for which declination values are available, is that of G.W. Haines et al. in 1965. It is found that the westerly declination may have reached a maximum early in the 19th century. This is also in agreement with global geomagnetic reconstructions based on historical íield measurements and archeomagnetism, and may be of use in dating lavas or artifacts in Iceland. The magnetic inclination appears to have been fairly constant at 75-77 . 58 JÖKULL,No. 43, 1993
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