| OCR Text |
Show Inclination 0 30 60 0 30 60 90 i i i- i- i- i- i- i- i- i i- i- i i i i i i i i CO U) < 20 25" 30 35 projection of Wono tephra age onto Lake Russel inclination record using Lake Chewaucan inclination record Mono Lake Excursion Lake Chewaucan Lake Russell Figure 2. Correlation of paleomagnetic inclination feature associated with Wono tephra ( 27,300 ± 300 C- 14 yr B. P.) in Lake Chewaucan sediments with inclination feature from Lake Russell sediments. Wono tephra was deposited under shallow lake conditions in both Lake Lahontan ( Benson et al., 1997) and Lake Chewaucan ( Negrini and Davis, 1992). Paleomagnetic correlation allows climate comparison to be extended to Lake Russell sediments even though the tephra layer is not found in these sediments. |
