This is the first in a sequence of five papers dealing with engineerin
g aspects of the surface-wave magnitude M(s) approximate to 6.8, 1988
Armenia earthquake, the devastating effects of which are still being f
elt in Armenia. Although the central theme of our three-year study has
been to assess the role of local soil conditions on the magnitude and
geographic distribution of damage, we have come to recognize that a c
lose link exists among seismological, geological, geotechnical, and st
ructural aspects of the Armenia earthquake. Our field investigations a
nd analysis of various geologic and engineering aspects of the earthqu
ake have culminated in a series of five papers. This and the companion
paper present mostly factual information pertaining to: (1) The mecha
nics of the fault and its surface breakout; (2) some potentially signi
ficant topographic, geologic, and geotechnical features; and (3) the s
tatistics of damage in cities of Spitak, Leninakan (now called Kumayri
), and Kirovakan, Armenia, correlated to geologic and soil profiles. I
n the third and fourth papers of this series, which will appear in a S
ubsequent issue of the journal, theoretical analysis of soil amplifica
tion in Leninakan and Kirovakan are described. The fifth paper, also i
n a later issue of the journal, presents data and analysis of liquefac
tion-induced embankment failure case histories.