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Home > History and Archaeology > History > Report on the Magnetic Isoclinal and Isodynamic Lines in the British Islands. from the 8th Report, Brit. Assoc. for the Advancement of Science
Report on the Magnetic Isoclinal and Isodynamic Lines in the British Islands. from the 8th Report, Brit. Assoc. for the Advancement of Science

Report on the Magnetic Isoclinal and Isodynamic Lines in the British Islands. from the 8th Report, Brit. Assoc. for the Advancement of Science


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This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1839 Excerpt: ... 1833 1834 Needle. 1834 1835 No. Mean Dip. Dublin... Limerick Limerick Dublin... Limerick... Glengariff... Killarney... Tulla Carlingford, Armagh Colerain Cam Strabane Enniskillen Fermoy Limerick, Dublin Galway Gallhorick Clifden Westport Puntoon Ballina Giants Causeway Cushendall Markree Dip. 8-4 117 11-5 5-81 MJ 3-5 1-5 4-5 15-8 71 30-2 15-8 71 42-2 71 26-9 72 0-9 72 0-0 72 00 70 48-3 71 7-3 70 590 71 260 71 410 71 520 72 30 72 8-0 72 70 73 150 72 00 72 6-3 72 110 72 13-4 72 6-5 71 32-9 Js, two needles, L. 1 and L. 4, ovation of the mean is nearly i single needle, being, in this The following table contains the final mean dip at each station, reduced to a common epoch, (the 1st January, 1837, ); and the latitudes and longitudes of the stations: Table XXXVH. Of the foregoing results, those obtained at the Giants' Causeway and at Colerain are manifestly affected, to a very considerable extent, by the disturbing action of the basaltic rocks. The effect of the basaltic pillars of the Causeway upon the magnetic needle has been long since observed; and on comparing the dip recorded in the preceding table, with that due to the geographical position of the station, we find it in excess to the amount of 50'. At Colerain, on the other hand, the effect of the disturbing action has been to diminish the dip, but in a less amount. The cause of these irregularities being apparent, we have no hesitation in rejecting the results, in the computation of the the isoclinal lines. Before we proceed to this computation, we must estimate the weights of the observed results; and for this purpose it is necessary to know the amount of the probable error of station. This is obtained by computing (with assumed approximate values of L, M, N, ) the probable dip at each station, due to its


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Product Details
  • ISBN-13: 9781130213911
  • Publisher: Rarebooksclub.com
  • Publisher Imprint: Rarebooksclub.com
  • Height: 246 mm
  • No of Pages: 34
  • Spine Width: 2 mm
  • Width: 189 mm
  • ISBN-10: 1130213919
  • Publisher Date: 01 Mar 2012
  • Binding: Paperback
  • Language: English
  • Returnable: N
  • Weight: 82 gr

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Report on the Magnetic Isoclinal and Isodynamic Lines in the British Islands. from the 8th Report, Brit. Assoc. for the Advancement of Science
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Report on the Magnetic Isoclinal and Isodynamic Lines in the British Islands. from the 8th Report, Brit. Assoc. for the Advancement of Science
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