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Historical Seismograms - Evidence from the AD 2000 Izu Islands ...

Historical Seismograms - Evidence from the AD 2000 Izu Islands ...

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The <strong>Historical</strong> <strong>Seismograms</strong> of Colombia 473Colombian Coffee Planters and <strong>the</strong> Division of Salinas of <strong>the</strong> Bank of <strong>the</strong> Republic,became interested in helping <strong>the</strong> aims of <strong>the</strong> Institute Director. With <strong>the</strong>ir financialsupport, installation of two seismic stations, one in Chinchini (4” 58’ N, 75’ 37’W, elevation 1,360 m), and o<strong>the</strong>r in Galerazamba (lO”47’08” N, 75” 15‘44” W,elevation 21 m), was approved in 1945.The new stations began operation at Galerazamba on April and at Chinchinii onAugust of 1949, and since that time, <strong>the</strong>y were kept in operation until <strong>the</strong> end of thisperiod. The instruments of both stations were similar: photographic seismographs<strong>from</strong> Sprengne<strong>the</strong>r and galvanometers <strong>from</strong> Leeds & Northrup of Philadelphia; oneshort-period vertical-component of <strong>the</strong> DM type and two horizontal components of<strong>the</strong> H type; <strong>the</strong> short period was 1.5 seconds and <strong>the</strong> long period was 16 seconds.The equipment was completed with a triple drum, one electric clock <strong>from</strong> <strong>the</strong> StandardTime Clock Co., and one transmitting and receiving radio. The orientation of<strong>the</strong> components was N-S and E-W; o<strong>the</strong>r constants could be determined; however,<strong>the</strong>y were not taken into account for parameters determination. Time correctionwas taken <strong>from</strong> <strong>the</strong> international WWV time station and automatically marked on<strong>the</strong> records. The drums rotation was kept at 0.5 mm/sec, and <strong>the</strong> spacing between<strong>the</strong> lines at 5 mm. The recording photographic paper was of standard size: 30 cmin width and 90 cm in length.Both stations were kept functioning until 1960 and onwards with three components,and <strong>the</strong>refore, <strong>the</strong> quantity of records are about 4,000 each, for a total of 8,000during this period. However, <strong>the</strong> useful records <strong>from</strong> Galerazamba are appreciablyless, because <strong>the</strong> interference of sea waves in this station is too great.The seismograms of both stations have been analyzed with those <strong>from</strong> Bogotdand <strong>the</strong>ir data published in <strong>the</strong> same Bulletins.As a final note, it should be mentioned here that in 1957, a new seismic station wasestablished in F‘uquene Island, about 100 km to <strong>the</strong> north of Bogotd, to cooperatein <strong>the</strong> investigations of <strong>the</strong> International Geophysical Year. The seismograph usedwas a photographic vertical component with a period of 6 sec, Galitzin-Wilip type,made by <strong>the</strong> Askania workshop.REFERENCESTurner, H. H. (1922). On <strong>the</strong> arrival of earthquake waves at <strong>the</strong> antipodes, and <strong>the</strong> measurementof <strong>the</strong> focal depth of an earthquake, Mon. Not. Roy. Astron. SOC. Geophys.Suppl., 1, 1-13. (also see International Seismological Summary, 1921 and 1922).Inglada Y Ors, Vicente (1943). Contribucibn a1 Estudio del Batisismo Suramericano de 17de ener de 1922, Inst. Geogr. y Catast. - Memorias del I.G.y C., Tom0 16, 8, Madrid.

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