Marble Bluff Bed. Attributed to Mount St. Helens in southwestern Washington because it contains cummingtonite, which is characteristic of Mount St. Helens tephra. Occurs in the Carson Desert and around Pyramid Lake in the Lake Lahontan area, Nevada. Is a graded bed, gray at the base and white at the top, 1 cm thick, and is the lowest tephra layer contained within the lower member of the Sehoo Formation. Underlies the Carson Sink Bed (new) of the Mono Basin Formation (new) and the Pelican Island Bed (new) and Wono Bed (new) of the Pyramid Lake Member (new) of the Mount Mazama Formation. Age is Pleistocene, 35 to 11.5 ka.
Type section: Marble Bluff, in banks of Mud Lake (Winnemucca) Slough, 5.6 km north of Nixon, in NW/4 NW/4 sec. 12, T. 23 N., R. 23 E., Nixon 15-min quadrangle, Washoe Co., NV.
Source: US geologic names lexicon (USGS Bull. 1565, p. 191).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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