Terrestrial Magnetism And Atmospheric Electricity

Cover Terrestrial Magnetism And Atmospheric Electricity
Terrestrial Magnetism And Atmospheric Electricity
L a Louis Agricola Bauer
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In Figure 4 is reproduced a portion of a continuous record sev- MAv(9.l90fl ItCnoQH) iA/ »!►« k »*.r^.
• An: PiGUXlB 4 eral meters in length, showing the magnetic storm of May 19, 1906.
The scale value is about 1.2 minutes per millimeter on the original trace, and dots were printed at the rate of one per minute, giving a time scale of twenty millimeters per hour. Increasing ordinates cor- respond to increasing westerly declination.
Wesleyan University^ Middletown^ Connecticut, Digitized by Goog
...le LETTERS TO EDITOR MAGNETIC OBSERVATIONS ON THE HILL OF SAN MIGUEL, D. F., MEXICO.
The hill of San Miguel lies W. S .W. of the City of Mexico, at a dis- tance of about 60 kilometers, and corresponding nearly to the vertex formed by the junction of the Sierras de las Cruces and Monte Alto, the Valley of Mexico being bounded on the West by the former which runs from N. W. to S. E. and enclosed by the latter on the South, nearly from due West to East. The geographical coordinates of the hill are as follows : latitude, 19° i(/ N., and longitude, 99° 19^ 17^'' W.


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