![](https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEgcu5emd4xsx4Eak_NlUoGOu3qDwWZIXcD4NnP7VTrntSXAFHKIPDZHS8LLv8TocdO4-pzmHG2BJoXwi5-TtK-pd0ebNsGXHlJarITQ31gAw9co5kWgfBMaUdAuuC70rA6WkPdHiEhy81QY/s320/IMG_0429_ed.jpg)
![](https://blogger.googleusercontent.com/img/b/R29vZ2xl/AVvXsEh6C1wkppU_uDb6tJskCY0C8Stkyy_8-NXnqNPGDNmwmGI4ECKhUzHbmuxmCNA_elWo_WxGkZK3p2uhh_zgBW2fp3QA0zVPQQgRUKUx5AekrUlQs37Dr38AA4RAcXq5nqvT8IFUBc6zdLoj/s320/IMG_0428.jpg)
Here are two photos--long overdue--that show the contact relations of the WC lava where I collected sample OWY-19. One shows the modern swale that has eroded around the WC lava that filled the paleo-swale. The other photo shows the nature of the contact between WC and lava flows within the Tertiary section: the WC lava sits on top of the Tertiary section there.
-Spud
Sweet. Thanks. Now about that geotagging concept...
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