At the nose of this outcrop, the Huckleberry Ridge tuff is exposed in the upper layers (above the darker flow layer, the Kilgore vitrophyre)
The Kilgore tuff vitrophyre shows displacement along a fault; typical of caldera rim zones.
Spectacular columnar jointing of the very thick Blacktail tuff (though the picture didn't turn out quite as spectacular)
More faulting -this reminds me of a GEOLOGY 101 textbook figure.
These sites are along the dugway near Ririe Reservoir in Idaho.
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