... >6.5), both historical and those measured instrumentally in Mexico, is not yet available. The tectonic setting where the Jalisco‐Colima coast is located is prone to large earthquakes and tsunamis, but only two large tsunamis that occurred in 1932 have been cataloged. This can be explained...

.... Gerl. Beitr. z. Geophys. , 38 : 228 - 256 (1933) . T H E E U R E K A E A R T H Q U A K E OF JUNE 6, 1932" By NEIL R. SPARKS ON THE MOR~I~CGof June 6, 1932, about 44 minutes past midnight, the region about Humboldt Bay was severely shaken by an earthquake which attained a maximum intensity...

... of this triggered earthquake on the LTV Fault would affect the estimate of the recurrence rate for moderate to large onshore events, changing the hazard estimates for the Lisbon area. We propose an alternative interpretation for the very high intensities (MMI X according to Sousa [ 1932 ]; MMI IX–X and IX...

... of large shallow earthquakes, 1897-1912 , Phys. Earth Planet. Interiors 33 , 1 - 11 . Galvan Rivera D. M. (1950) . Coleccion de las efemerides publicadas en el calendario del mas antiguo Galvan desde su Fundacion haste el 30 de...

...​/JB093iB12p15085 . Peltzer , G. , Tapponnier , P. , Gaudemer , Y. , Meyer , B. , Guo , S.M. , Yin , K. , Chen , Z.T. , and Dai , H.G. , 1988 , Offsets of late quaternary morphology, rate of slip, and occurrence of large earthquakes on the Chang Ma fault (Gansu, China...

... at the Pacific harbor settlement of Puerto de la Navidad and caused severe damage to structures up to ∼ 100 km from the coast. The macroseismic intensity distribution for the 1563 earthquake is practically identical to that of the 3 June 1932 M s 8.2 earthquake, which ruptured the Rivera–North America plate...

... earthquake ( M 8.0), the 1932 Changma earthquake ( M 7.6), and the 1954 Shandan earthquake ( M 7.3). They are predominantly reverse slip, except for the 1932 Changma and the 1954 Shandan earthquakes. The Changma earthquake is characterized by left-lateral faulting with a reverse component, while the Shandan...

... =LONGVALE o| LK CREEK I BRAGS ~ WILLITS ,oi o-o EARTHQUAKE ERIVEI~COt~PTCHE ORE(} JA~N,~2,~1935 .FELT =sHL,u ELKNA AMS ¢1 NOT FELT "~ ,I:~T~? ' UI.PAPoRKtE SI%RiNSS. . . . . o A).MA( ~_ c~eOONVILLE °LAKEPORT =MANCHE~TER °H,OPU MID PT ARENA [] YORKVtLLE - - ~ oAN4OLIS Fig. 4. Questionnaire coverage after...

... 20, 1932 , Trans. Am. Geophys. Union , 14th Ann. Mtg. , 471 - 475 (1933) 3 Leggette R. M. Taylor G. H. Earthquakes Instrumentally Recorded in Artesian Wells , Bull...

...” was perhaps too concise in its geographical locations to meet with the need of the parametric catalogs to systematically assign geographical epicentral coordinates. The celebrity position among the global earthquake lists of the early twentieth century is without any doubt occupied by Sieberg (1932...

... composite earthquake catalog for the High Asia region ( Fig. 1 ) counted 3033 solutions for M b = 3.0–8.0 earthquakes between 1932 to 2016, with origin depths of 0 to 70 km, including the filtered catalog for the period 01.1976–05.1994 plus the recent data from the Global CMT catalog for 05.1994...

... and apparently confused A.H. with A.D. As a result of this, thirty entries in his list are dated about six centuries too early. Willis's list was copied in part by Sieberg (1932 a, b) and others without checking the mistake, with the effect that many earthquake catalogues now contain non-existent events. We...

... that the aftershocks cluster around areas of high slip and high moment release ( e.g., 1992 Landers earthquake, Wald and Heaton, 1994 ; 1994 Northridge earthquake, Thio and Kanamori, 1996 ; 1999 Chi-Chi earthquake, Ma et al., 2001). The 2002 Denali Fault earthquake sequence offers an unprecedented...

... of major scientific importance, such as fossil leaves, later identified as Glossopteris indica . He then worked in Egypt, Palestine and New Zealand, and was Acting Director of the New Zealand Geological Survey when he died suddenly in 1932. Little has been acknowledged about Ferrar’s other contributions...

.... There are earthquakes with n equal to 5 for which the curve has an inflection point at some distance. This change in slope is explained by the arrival of totally reflected body waves from some discontinuity within the crust the M-discontinuity and discontinuities within the upper mantle as well as the concentration...

... , Chiron 17 , 343 – 360 . Claudian (circa 399) . Against Eutropius 1.4-5, 2.24-30 , in M. Platnauer (editor), Loeb Classical Library , Vol. 135 , Cambridge, MA , 1922 . Degterev , A. K. ( 2001 ). Earthquake effect on hydrogen sulfide contamination of the Black Sea , Russian...

... the Fairview Peak earthquake and subsequent triggering of the Dixie Valley earthquake. Right-lateral offsets of more than a meter occurred along both the West Gate and Louder-back Mountains faults. Slip was limited to normal motion of 1 m or less along the Gold King fault. The change from right-oblique motion...

... and tectonics of the Rivera plate and implications for the 1932 Jalisco, Mexico, earthquake , J. Geophys. Res. 89 , 4520 – 4530 . Escobedo D. Pacheco J. F. , and Suárez G. 1998 . Teleseismic body‐wave analysis of the October 1995 ( M w = 8.0 ), Colima‐Jalisco, Mexico earthquake...

... +0.0038  MPa (∼52%) and +0.0014  MPa (∼19%), respectively. Around the epicenter of the 1932 M ∼7.6 Changma earthquake, the total change of Coulomb failure stress, just prior to its occurrence, reached about +0.0052  MPa (Fig.  4b ), to which the regional tectonic loading and the coseismic...

.... 1935 . Erdbebenherde und Tektonik im Gebiete der Schwäbischen Alb , Zeitschr. f. Geophysik , 11 : 15 - 19 . Ishimoto M. 1932 . Echelle d'intensité sismique et accélération maxima , Bull. Earthquake Research Inst. (Tokyo...