“…The Huckleberry Ridge Tuff (HRT), the oldest and largest ash-flow tuff of the Yellowstone Plateau volcanic field, has long been associated with the Réunion event based on a common transitional paleomagnetic direction determined from tuff members A, B, and C (Reynolds, 1977). Numerous K-Ar and 40 Ar/ 39 Ar ages between 2.0 and 2.1 Ma have been obtained from HRT members A, B, and C (Gansecki et al, 1998;Lanphere et al, 2002, and references within). Gansecki et al (1998) measured 21 sanidine grains from sample 2R577 collected near the middle of member B, which is the most voluminous of the three members.…”