Origin and Distribution of Glauconites and Related Clay Aggregates on Sea Floor off Southern California: ABSTRACT

Author(s):  
W. L. Pratt
2017 ◽  
Vol 2017 ◽  
pp. 1-13 ◽  
Author(s):  
Milton S. Love ◽  
Mary M. Nishimoto ◽  
Linda Snook ◽  
Donna M. Schroeder ◽  
Ann Scarborough Bull

Increasing reliance on deep-water renewable energy has increased concerns about the effects of the electromagnetic fields (EMFs) generated by submarine power cables on aquatic organisms. Off southern California, we conducted surveys of marine organisms living around energized and unenergized submarine power cables and nearby sea floor during 2012–2014 at depths between 76 and 213 m. In general, EMFs declined to background levels about one meter from the cable. We found no statistical difference in species composition between the fish assemblages along the energized and unenergized cables. The natural habitat community statistically differed from both energized and unenergized cable communities. Within species (or species groups), we found no differences in densities between energized and unenergized cables. Total fish densities were significantly higher around the cables than over the natural habitat. We found that invertebrate communities were structured by habitat type and depth and, similar to the fishes, there was no statistical difference between the energized and unenergized cables. Individually, the densities of four invertebrate species or species groups (Metridium farcimen, Luidia spp., unidentified black Crinoidea, and Urticina spp.) differed between energized and unenergized cables, but this difference was not significant across all depth strata. The invertebrate community inhabiting the natural habitat strongly differed from the energized and unenergized cable community exhibiting the fewest species and individuals.


1942 ◽  
Vol 53 (6) ◽  
pp. 815-848 ◽  
Author(s):  
R. S. DIETZ ◽  
K. O. EMERY ◽  
F. P. SHEPARD

2017 ◽  
Vol 116 (2) ◽  
pp. 61-87 ◽  
Author(s):  
Milton S. Love ◽  
Mary M. Nishimoto ◽  
Scott Clark ◽  
Merit McCrea ◽  
Ann Scarborough Bull

2004 ◽  
Vol 20 (3) ◽  
pp. 917-950 ◽  
Author(s):  
Mark R. Legg ◽  
Jose C. Borrero ◽  
Costas E. Synolakis

We investigate the tsunami hazard associated with the Catalina Fault offshore of southern California. Realistic faulting parameters are used to match coseismic displacements to existing sea floor topography. Several earthquake scenarios with moment magnitudes ranging between 7.0 and 7.6 are used as initial conditions for tsunami simulations, which predict runup of up to 4 m. Normalizing runup with the maximum uplift identifies areas susceptible to tsunami focusing and amplification. Several harbors and ports in southern California lie in areas where models predict tsunami amplification. Return periods are estimated by dividing the modeled seafloor uplift per event by the observed total uplift of the Santa Catalina Island platform multiplied by the time since the uplift began. The analysis yields return periods between 2,000 to 5,000 years for the Catalina Fault alone, and 200 to 500 years when all offshore faults are considered.


1947 ◽  
Vol 37 (4) ◽  
pp. 307-313
Author(s):  
Thomas Clements ◽  
K. O. Emery

ABSTRACT The positions of submarine epicenters of seismic shocks occurring during a twelve and one-quarter year period were plotted on a bathymetric chart of the area off southern California. The data show: (1) that the sea floor is active seismically, and (2) that the seismic activity and the topography are related. It appears that the major topographic features are of tectonic origin and that the forces which brought them about are still active.


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