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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 471The quantity of records for most of <strong>the</strong>se years was greater at <strong>the</strong> beginningof <strong>the</strong> period, but decreasing appreciably and gradually for <strong>the</strong> last years. Thetotal number of seismograms is about 554 for <strong>the</strong> last 12 years, and with <strong>the</strong> 97seismograms recorded in <strong>the</strong> first 5 years, we have a total of about 651 for <strong>the</strong> firstperiod of <strong>the</strong> Bogoti seismic station <strong>from</strong> 1923 to 1940.3. Second Period (1942-1961)The second period of <strong>the</strong> seismic station at Bogoti began with <strong>the</strong> establishmentof <strong>the</strong> Instituto Geofisico de Los Andes Colombianos on September, 1941, in <strong>the</strong>San BartolomC College "La Merced", situated to <strong>the</strong> north of <strong>the</strong> former and to <strong>the</strong>nor<strong>the</strong>ast border of <strong>the</strong> city of Bogoti.The geographic situation of <strong>the</strong> new site is given by <strong>the</strong> following coordinates:4" 37' 23" N and 74' 03', 54" W at an elevation of 2,653 m above <strong>the</strong> mean sea level.For <strong>the</strong> new station, a place was selected as isolated as possible <strong>from</strong> <strong>the</strong> city traffic,and <strong>the</strong> site was prepared for <strong>the</strong> best conditions according to <strong>the</strong> specificationsof modern seismology. By taking advantage of a small cavity in a rocky escarpmentwithin <strong>the</strong> College campus, a cave was excavated in <strong>the</strong> rock, and <strong>the</strong> place wasprepared so that <strong>the</strong> seismic instruments were installed on cemented bases over <strong>the</strong>rocky ground. Of <strong>the</strong> three previous mechanical seismographs, only <strong>the</strong> Wiecherttypewas kept and installed in <strong>the</strong> new place. The o<strong>the</strong>r two instruments weredismantled, and most of <strong>the</strong>ir parts were dispersed or destroyed; only one recordingsystem, <strong>the</strong> Cartuja mass of 1000 kg, and <strong>the</strong> clocks were preserved. In addition,an electromagnetic seismograph was acquired: a short-period, photographic, Benioffmodel, constructed under direction of <strong>the</strong> same author at Pasadena, California.The seismic station was completed with an electric clock of <strong>the</strong> Standard ElectricTime Co., one radio transmitter by Johnson Viking, and a Hallicrdter receiver to receive<strong>the</strong> international time. A three-component electromagnetic and photographicseismograph of <strong>the</strong> Galitsin-type was ordered <strong>from</strong> <strong>the</strong> Masing-Wilip workshop inEstonia, but it was never received because of <strong>the</strong> Second World War. Later on, aseismograph of two horizontal components was ordered <strong>from</strong> Sprengne<strong>the</strong>r at St.Louis, Mo. (U.S.A.).The new station was ready to start operation at <strong>the</strong> end of 1941, but its regularfunction did not begin until <strong>the</strong> month of March, 1942. The period of <strong>the</strong> 100 kgBenioff vertical seismograph was 1 sec and that of its galvanometer was 0.3 sec;its damping was critical and its static magnification was 1,200, but its polarity isunknown. Its drum is 32 cm in length and its circumference 91 cm; its rotationis 1 mm/sec and <strong>the</strong> spacing between lines is 2.5 mm. The size of <strong>the</strong> recordingphotographic paper is <strong>the</strong> same as that used in <strong>the</strong> Vela project.The Wiechert seismograph started operation again at <strong>the</strong> beginning of 1943. Thehorizontal seismograph (ordered <strong>from</strong> Sprengne<strong>the</strong>r to replace <strong>the</strong> Masing- Wilip)reached Bogoti in 1946; one component had to be repaired, and <strong>the</strong>refore <strong>the</strong> wholeinstrument installation was made in July of 1947.This equipment is composed of two horizontal components, Sprengne<strong>the</strong>r modelH, galvanometers by Leeds & Northrup of Philadelphia (U.S.A.), and a triple drumfor photographic paper of 30 cm by 90 cm. The drum rotation is 30 cm per minute.The natural period of this seismograph was 16 sec, and <strong>the</strong> components orientationwas N-S and EW; o<strong>the</strong>r constants, such as damping, polarity, and magnification,were unknown.

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