Dissociated Effigy, a Colima-style Figurine at the Imperial Valley Desert Museum

2021 ◽  
Author(s):  
David Breeckner
Keyword(s):  
Author(s):  
Russell C. Rodríguez

On November 5, 2016, hundreds of people convened at the historical landmark of Chicano Park in Barrio Logan, San Diego, to celebrate the life of one of the community’s most revered elders, Ramón “Chunky” Moroyoqui Sánchez. Nuestro querido maestro falleció el día 28 de octubre de 2016. Sánchez, endearingly known as Chunky, was synonymous with Barrio Logan, Chicano Park, Chicano/a music, and San Diego in general. In this city, an auditorium is named in his honor. His image is incorporated in murals. The Chicano comedy troupe Culture Clash developed a vignette about Chunky, and upon his passing the San Diego Chargers’ website featured him in a blog post that included a photo of him with players and cheerleaders. Chunky was also well known beyond the Imperial Valley. The music of Los Alacranes Mojados (the group he started with his brother, Ricardo Sánchez) continues to be embraced in Mexicano/a and Chicano/a communities throughout California and the Southwest. The news of Sánchez’s passing reverberated throughout California like the violent ripples of a pond into which a boulder has been dropped. Ese vato will be missed.


1984 ◽  
Author(s):  
M.J. Bennett ◽  
P.V. McLaughlin ◽  
J.S. Sarmiento ◽  
T.L. Youd

Hilgardia ◽  
1988 ◽  
Vol 56 (5) ◽  
pp. 17-44 ◽  
Author(s):  
James D. Rhoades ◽  
Frank T. Bingham ◽  
John Letey ◽  
Paul J. Pinter ◽  
Robert D. Lemert ◽  
...  

2000 ◽  
Vol 34 (11) ◽  
pp. 1833-1843 ◽  
Author(s):  
Judith C Chow ◽  
John G Watson ◽  
Mark C. Green ◽  
Douglas H Lowenthal ◽  
Barbara Bates ◽  
...  

1983 ◽  
Vol 73 (4) ◽  
pp. 1203-1224
Author(s):  
J. Langbein ◽  
A. McGarr ◽  
M. J. S. Johnston ◽  
P. W. Harsh

abstract A geodetic trilateration network comprising 54 baselines was established around the northern part of the Imperial fault beginning 12 days after the Imperial Valley earthquake of 15 October 1979, and the line lengths were repeatedly observed during the following 110 days. During the observational period, there was an average of about 10 cm of dextral postseismic fault slip. Geodetic data in conjunction with alignment-array measurements indicate that the postseismic slip U at time t following the main shock is well described by U (t) = (10.96 ± 0.12) cm log(t/1.75 day + 1), a result that implies that it will be approximately 9 to 10 yr before the rate of postseismic displacement diminishes to the ambient rate of creep of 0.5 cm/a. The postseismic strain changes are localized to the east side of the Imperial fault in the southern part of the Mesquite Lake basin, where significant north-south extension occurred at an average rate of 2.7 ± 0.3 × 10−5/a during the observational period. These changes are compatible with dextral fault slip within the top 5 km of the fault.


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