Preliminary geologic map of the Raymond quadrangle, Pacific County, Washington

Preliminary estimates of recurrence intervals for great earthquakes of the past 3500 years at northeastern Willapa Bay, Washington

“…This structural high, which extends about 40 Ian in a northnorthwestward direction, is defined mainly by an exposed core of Crescent Formation-Eocene pillow basalt, basaltic breccia, and basaltic sedimentary rock (Wagner, 1967a(Wagner, , 1967b. Near the northern and southern ends of the antiform the Crescent is flanked to the east and west by younger sedimentary strata of Eocene and Oligocene age.…”

Molluscan paleontology of the lower Miocene Clallam Formation, northwestern Washington

“…This shoaling is the concluding phase of an Eocene to Miocene depositional cycle in which maximum deepening took place during the Oligocene. Elsewhere in western Washington the concluding phase of the transgressive-regressive cycle is represented by the middle Miocene part of the Astoria Formation (Rau, 1967, p. 25;Wagner, 1967).…”

Well stratigraphy and correlations, western Washington and northwestern Oregon

“…2), with key species including Cibicides e/maensis, Sphaeroidina bulloides, Lenticulina brevispinosus, and Cassidulina crassipunctata. Strata in this lower biostratigraphic unit represent the upper part of the Lincoln Creek Formation as mapped in this area by Wagner (1967). These assemblages were probably deposited at lower to lower-middle bathyal water depths as suggested by the consistent occurrence of the lower bathyal Gyroidina so/danii (table 25; Ingle, 1980).…”

“…It is located in the southem part of the Grays Harbor basin ( fig. 3) on the crest of a gentle anticline bounded to the northwest and south by normal faults (Wagner, 1967). Surface exposures at the well site have been assigned to the upper part of the Astoria (?)…”

“…This biostratigraphic unit corresponds to the upper and middle units of the Astoria (?) Formation mapped in this area by Wagner (1967).…”