Lv. Benson et al., RADIOCARBON AGES AND ENVIRONMENTS OF DEPOSITION OF THE WONO AND TREGOHOT-SPRINGS TEPHRA LAYERS IN THE PYRAMID LAKE SUBBASIN, NEVADA, Quaternary research, 47(3), 1997, pp. 251-260
Uncalibrated radiocarbon data from core PLC92B taken from Wizards Cove
in the Pyramid Lake subbasin indicate that the Trego Hot Springs and
Wono tephra layers were deposited 23,200+/-300 and 27,300+/-300 C-14 y
r B.P. (uncorrected for reservoir effect). Sedimentological data from
sites in the Pyramid Lake and Smoke Creek-Black Rock Desert subbasins
indicate that the Trego Hot Springs tephra layer was deposited during
a relatively dry period when Pyramid Lake was at or below its spill po
int (1177 m) to the Winnemucca Lake subbasin. The Wono tephra layer wa
s deposited when lake depth was controlled by spill across Emerson Pas
s sill (1207 m) to the Smoke Creek-Black Rock Desert subbasin. O-18 da
ta from core PLC92B also support the concept that the Trego Hot Spring
s tephra fell into a relatively shallow Pyramid Lake and that the Wono
tephra fell into a deeper spilling lake. (C) 1997 University of Washi
ngton.