Seismological Research Letters; May/June 2008; v. 79; no. 3;
p. 426-437; DOI: 10.1785/gssrl.79.3.426
© 2008 Seismological Society of America
Tom La Touche and the Great Assam Earthquake of 12 June 1897: Letters from the Epicenter
Roger Bilham
University of Colorado at Boulder
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Richard Dixon Oldham's classic memoir on the great Mw =
8.1 Assam earthquake of 1897 is seminal for its seismological observations,
insights, and conclusions (Oldham
1899). Teleseismic arrivals of waves from Shillong led Oldham
(1858–1936) to distinguish the three types of seismic waves and
eventually to recognize from them the distinctive presence of the Earth's
core. Oldham, however, did not feel the earthquake. He had left the Calcutta
office of the Geological Survey of India (GSI) in the care of his colleague
Thomas Henry Digges La Touche (1856–1938) two weeks previously (see
figure 1). Now recently
discovered letters written by La Touche from Calcutta and the epicentral
region to his wife, Nancy, provide a firsthand, day-by-day account of the
post-earthquake investigation and include a seismogram from an instrument that
he constructed in the field at a cost of "less than sixpence" from
pieces of tin, a suspended boulder, a glass bead, and a bamboo needle that
scratched a glass plate (LaTouche papers,
1880–1913).
In his memoir Oldham notes that he focused his team of geologists on the
physics of the earthquake. Their reports were submitted "under specific
instructions to report only on the facts observed, and to refrain from any
expressions of opinion as to the conclusions to be drawn, as this could only
be profitably done after a review of the whole of the facts, of which only
part could become known to each individually."
(Oldham 1899, p.257). He
deduced from their observations that local accelerations in the earthquake had
exceeded 1 g, that velocities had exceeded 3 m/s, that electrical currents in
the ground had accompanied aftershocks, that postseismic crustal deformation
continued to deform the plateau in the year following the earthquake, and that
many of the largest aftershocks lay 15 . . . [Full Text of this Article]
University of Colorado at Boulder
Department of Geological
Sciences
Campus Box 399
Boulder, Colorado 80309-0399
USA
roger.bilham@colorado.edu
Copyright © 2009 by Seismological Society of America