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P.O. Box 3066
Newport Beach, California
92659-0620
rshlemon@jps.net
(R.J.S.)
Slosson & Associates
15500 Erwin Street, Ste.
1123
Van Nuys, California
91411
slidings@aol.com
(J.E.S.)
7178 Blue Falls Circle
Reno, Nevada
89511
cgbarney@aol.com
(J.T.B.)
| The first 20% of the full text of this article appears below. |
The 1994 Northridge earthquake in southern California spawned literally hundreds of investigations and their resulting publications. Many investigations are now deemed as paleoseismic, a term now widely used for good old-fashioned trenching and fault dating. Baldwin et al. (2000) continue this tradition by emplacing boreholes, a trench, and test pits across the face of a 2-m-high escarpment that marks the south side of the NWSEtrending Northridge Hills in the northern San Fernando Valley.
The Northridge Hills fault zone underlies the Northridge Hills, and
interest in its ground-rupture potential was set forth over 50 yr ago by
Hazzard (1944), and later by
Slosson and Barnhart (1967),
Barnhart and Slosson (1973),
and Saul (1975), who basically
concluded that fault movement occurred during late Quaternary time and that,
therefore, the fault was likely to be active. In their article Baldwin et
al. (p. 637) asked the rhetorical question: "Is the Northridge
Fault active?" They answer in the affirmative, based mainly on
interpretations of leveling data, on the construction of regional structural
models, and on the
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