RADIOCARBON AGES AND ENVIRONMENTS OF DEPOSITION OF THE WONO AND TREGOHOT-SPRINGS TEPHRA LAYERS IN THE PYRAMID LAKE SUBBASIN, NEVADA

Citation
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
Citations number
17
Categorie Soggetti
Geosciences, Interdisciplinary
Journal title
ISSN journal
00335894
Volume
47
Issue
3
Year of publication
1997
Pages
251 - 260
Database
ISI
SICI code
0033-5894(1997)47:3<251:RAAEOD>2.0.ZU;2-P
Abstract
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.