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Eureka Valley Tuff

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Journal Article
Journal: GSA Bulletin
Published: 01 May 1976
GSA Bulletin (1976) 87 (5): 754–762.
...DONALD C. NOBLE; MARJORIE K. KORRINGA; S. E. CHURCH; HARRY R. BOWMAN; MILES L. SILBERMAN; C. E. HEROPOULOS Abstract The Eureka Valley Tuff, erupted from the late Miocene Little Walker volcanic center, east-central California, includes two major ash-flow sheets: the more voluminous, widespread...
Journal Article
Journal: Geology
Published: 01 March 1974
Geology (1974) 2 (3): 139–142.
...Donald C. Noble; David B. Slemmons; Marjorie K. Korringa; William R. Dickinson; Yehya Al-Rawi; Edwin H. McKee Abstract The Eureka Valley Tuff consists of two major ash-flow sheets and a local over-lying sequence of ash-flow tuff erupted from vents within the Little Walker caldera 11 mi west...
Image
Figure 4. Geologic map showing reference section of the <b>Eureka</b> <b>Valley</b> <b>Tuff</b> ...
in > Geosphere
Published: 01 December 2007
Figure 4. Geologic map showing reference section of the Eureka Valley Tuff at Tollhouse Flat, California. Excerpted from King (2006) .
Image
Figure 6. Photograph of the <b>Eureka</b> <b>Valley</b> <b>Tuff</b> reference section. View is e...
in > Geosphere
Published: 01 December 2007
Figure 6. Photograph of the Eureka Valley Tuff reference section. View is eastward with West Walker River and Highway 395 in the foreground. Width of view is ∼800 m.
Journal Article
Journal: Geosphere
Published: 01 December 2007
Geosphere (2007) 3 (6): 646–666.
...Figure 4. Geologic map showing reference section of the Eureka Valley Tuff at Tollhouse Flat, California. Excerpted from King (2006) . ...
FIGURES | View All (16)
Journal Article
Journal: Geosphere
Published: 01 December 2013
Geosphere (2013) 9 (6): 1530–1551.
... this region is apparently devoid of major active strike-slip faults, the presence of Neogene clockwise vertical-axis tectonic block rotations indicates the accommodation of dextral shear. We measured vertical-axis rotation by comparing remanence directions of widespread members of the Eureka Valley Tuff...
FIGURES | View All (11)
Journal Article
Journal: Geosphere
Published: 01 February 2016
Geosphere (2016) 12 (1): 135–175.
... in the graben-vent system to thicknesses 6 times greater than the paleochannel fill, with no reincision surfaces. Sequence 3 ignimbrites of the Stanislaus Group (Eureka Valley Tuff) were erupted from the Little Walker caldera, and mark the course of all three paleochannels, with channel reincision surfaces...
FIGURES | View All (23)
Journal Article
Journal: Geosphere
Published: 07 August 2018
Geosphere (2018) 14 (5): 2068–2117.
... Group, the Table Mountain Latite, is a likely parent to succeeding units of the Stanislaus Group (Eureka Valley Tuff and Dardanelles Formation), but this particular liquid line of descent is otherwise rare in the Mesozoic and Cenozoic history of the Sierra Nevada. Volcano-tectonic activity continued...
FIGURES | View All (34)
Journal Article
Journal: Geosphere
Published: 01 October 2013
Geosphere (2013) 9 (5): 1125–1146.
..., erupted from fault-controlled fissures in the Sierra Crest graben-vent system. (2) The Eureka Valley Tuff consists of three trachydacite ignimbrite members erupted from the Little Walker caldera. These ignimbrites are interstratified with lava flows that continued to erupt from the Sierra Crest graben...
FIGURES | View All (17)
Series: GSA Special Papers
Published: 01 July 2008
DOI: 10.1130/2008.2438(12)
...-polarity cryptochron, C5n.2n-1 at ca. 10.2 Ma, which was previously known only from seafloor magnetic anomalies. High-K volcanism continued with eruption of the three members of the Eureka Valley Tuff (9.3–9.15 Ma). In contrast with previous workers in the southern Sierra, who interpret high-K volcanism...