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Teewinot formation

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Journal Article
Journal: AAPG Bulletin
Published: 01 August 1956
AAPG Bulletin (1956) 40 (8): 1899–1914.
... pyroclastic conglomerate, tuff, sandstone, and claystone of middle Miocene age, unconformably overlying all older rocks and unconformably overlain by rocks of middle Pliocene age. The name Teewinot formation is used for 5,000 feet or more of white limestone, pumicite, tuff, claystone, diatomite...
FIGURES
Image
Fault dip vs distance from the Teton fault. Dip data are from  Love et al. ...
Published: 01 May 2009
Figure 8. Fault dip vs distance from the Teton fault. Dip data are from Love et al. (1992) . Solid circles are dip measurements from the Teewinot Formation; open diamonds are dip measurements from the Colter Formation; pluses are from the mapped Colter Formation in the area north of Signal
Journal Article
Journal: GSA Bulletin
Published: 01 May 2009
GSA Bulletin (2009) 121 (5-6): 837–856.
...Figure 8. Fault dip vs distance from the Teton fault. Dip data are from Love et al. (1992) . Solid circles are dip measurements from the Teewinot Formation; open diamonds are dip measurements from the Colter Formation; pluses are from the mapped Colter Formation in the area north of Signal...
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Journal Article
Journal: GSA Bulletin
Published: 01 March 2005
GSA Bulletin (2005) 117 (3-4): 288–306.
... in the region is the Arbon Valley Tuff Member of the Starlight Formation (10.21 ± 0.03 Ma), which erupted from a caldera source outside of the Heise volcanic field. These results establish the Conant Creek Tuff as a distinct and widespread ignimbrite in the Heise volcanic field, eliminating former confusion...
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Journal Article
Published: 01 January 2014
Rocky Mountain Geology (2014) 49 (2): 191–199.
... of Colorado's highest peaks. Figure 2. Jack Reed on the summit of Teewinot, 1965. In the summer of 1974, however, my luck ran out again. I was summoned east to the new USGS headquarters in Reston, Virginia, to serve as chief of the Office of Environmental Geology. The office was responsible...
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Journal Article
Journal: Geosphere
Published: 11 April 2018
Geosphere (2018) 14 (3): 1008–1030.
... extends from the vicinity of Mount Moran south to the east face of Teewinot, and the southern area extends from Avalanche Canyon to the southern limits of Precambrian outcrop. Figure 5. Structural data from the gneisses of the Teton Range. (A) Poles to foliation from the northern portion...
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Series: GSA Field Guide
Published: 01 January 2008
DOI: 10.1130/2007.fld010(03)
EISBN: 9780813756103
... of the Yellowstone Plateau ( Fig. 5 ) and Heise volcanic fields ( Fig. 6 ). At Heise, the initial caldera-forming eruption produced the Blacktail Creek Tuff at 6.62 Ma from several areas within the caldera and formation of the Blacktail Creek caldera. This eruption signaled the start of the caldera-forming...
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