SHEAR-WAVE VELOCITY FROM TWO 150 M BOREHOLES IN SEATTLE, WA
Volunteer Park (VPD) and Beacon Hill Park (BHP) boreholes have some similarities; both have thick outwash near the ground surface, and both have thick glaciolacustrine clay near the middle depths of the boreholes. The surficial unit, Vashon advance outwash (Qva-"Esperance Sand"), varies in thickness from 51 m at VPD to 26 m at BHP, 5 km to the south. Comparisons made between lithology, standard borehole geophysical logs and a series of borehole Vs models reveal that the Qva unit can be sub-divided into an upper, clean, well graded, interbedded, gravel-rich sand layer and a lower, dense, silty to clayey sand layer. Shear-wave velocity models at both sites show an increase in average velocity of 30 to 33% respectively between the layers (415 to 580 m/s at VPD and 450 to 675 m/s at BHP).
Interpretation of borehole cuttings and regional geology indicate that the Beacon Hill borehole penetrates a more complete sequence of Vashon Drift, deposits from the Olympia nonglacial interval (Qob), glaciolacustrine deposits from the Possession glaciation, and even older glacial diamict deposits. In general, shear-wave velocity of glaciolacustrine deposits are slower with an average of 500 m/s (480 to 520 m/s) at VPD and 450 m/s (390 to 520 m/s) at BHP. Older glacial units at BHP (125 m to bottom of hole) have the highest shear (930 m/s) and compressional-wave (2255 m/s) velocities measured at either site.