Quaternary Nonglacial Geology
DOI: 10.1130/dnag-gna-k2.251
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Quaternary geology and structural history of the Snake River Plain, Idaho and Oregon

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Cited by 50 publications
(78 citation statements)
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“…1, Table 1) was similarly mapped onto the tree to evaluate geographical diversification of Pyrgulopsis. Geographical regions, whose characteristic physiography and structure generally date to the late Tertiary (Stewart, 1998), were chosen as the unit of analysis rather than major western drainage basins, which have been shown to be complex composites (e.g.. Belcher, 1975;Malde, 1991;Young, 2004).…”
Section: Discussionmentioning
confidence: 99%
“…1, Table 1) was similarly mapped onto the tree to evaluate geographical diversification of Pyrgulopsis. Geographical regions, whose characteristic physiography and structure generally date to the late Tertiary (Stewart, 1998), were chosen as the unit of analysis rather than major western drainage basins, which have been shown to be complex composites (e.g.. Belcher, 1975;Malde, 1991;Young, 2004).…”
Section: Discussionmentioning
confidence: 99%
“…Malad Gorge is a tributary to the Snake River Canyon, Idaho, within the Snake River Plain, a broad depression filled by volcanic flows that erupted between ∼15 Ma and ∼2 ka (22,23). The gorge sits at the northern extent of Hagerman Valley, a particularly wide (∼7 km) part of the Snake River Canyon (Fig.…”
mentioning
confidence: 99%
“…Biotic distributions instead have been used to infer that the ancestral Snake River flowed through southeast Oregon to the California Pacific coast, via either the Klamath (Taylor, 1960(Taylor, , 1985 or Sacramento (Miller, 1965) Rivers (also see Wheeler and Cook, 1954). Although this hypothesis is well entrenched in the literature (Christiansen and Yeats, 1992;Malde, 1965Malde, , 1991Smith et al, 2000), its supporting biogeographic evidence has never been rigorously evaluated.…”
Section: Introductionmentioning
confidence: 99%
“…The only reasonably well established geological benchmark that can be associated with this postulated paleodrainage is the capture of the Snake River by the Columbia River, which is generally thought to have occurred about 2.0 Ma (Malde, 1991;Othberg, 1998; Sadler and Link, 1996) in conjunction with the draining of Lake Idaho and incision of Hells Canyon. [Note that some workers have suggested that this shift in drainage occurred earlier in the Pliocene (e.g., Link and Fanning, 1999;Smith, 1999;Wood, 2000) and thus we consider 2.0 Ma to be a minimal date for this event.]…”
Section: Introductionmentioning
confidence: 99%