2016
DOI: 10.1016/j.quascirev.2015.11.011
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A mid to late Holocene cryptotephra framework from eastern North America

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Cited by 45 publications
(49 citation statements)
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“…Depositional and grain size analysis indicate that the eruptive plume was 40-45 km in height and was distributed by ~10 m/s winds that were sustained at this velocity for ~2 days (Lerbekmo, 2008). The presence of the WRAe as a cryptotephra was also recently recognized in Maine, Nova Scotia, and Newfoundland (Jensen et al 2014;Mackay, et al, 2016;Pyne-O'Donnell et al, 2012). Geochemical and morphological evidence has also shown that the WRAe correlates with the "AD860B" ash (A.D. 846-848) found in Greenland and northern Europe (Jensen et al, 2014).…”
Section: Introductionmentioning
confidence: 89%
“…Depositional and grain size analysis indicate that the eruptive plume was 40-45 km in height and was distributed by ~10 m/s winds that were sustained at this velocity for ~2 days (Lerbekmo, 2008). The presence of the WRAe as a cryptotephra was also recently recognized in Maine, Nova Scotia, and Newfoundland (Jensen et al 2014;Mackay, et al, 2016;Pyne-O'Donnell et al, 2012). Geochemical and morphological evidence has also shown that the WRAe correlates with the "AD860B" ash (A.D. 846-848) found in Greenland and northern Europe (Jensen et al, 2014).…”
Section: Introductionmentioning
confidence: 89%
“…WRAe is the most widely distributed of the two deposits, having been correlated across to eastern Canada (Pyne-O'Donnell et al, 2012), the northeastern Unites States (Mackay et al, 2016), Greenland and Europe (Jensen et al, 2014a). It should be noted that within northwestern North America it had significant effects on the lives and migration patterns of the ancestral Athapaskan people of the area (e.g.…”
Section: Wraementioning
confidence: 99%
“…Lowe et al, 2007;Lowe et al, 2012;Lane et al, 2013;Streeter and Dugmore, 2014). The recent discovery of Pacific northwest tephra more than 5000 km from their source in eastern Canada (Pyne-O'Donnell et al, 2012), Europe (Jensen et al, 2014a) and the eastern United States (Jensen et al, 2014b;Mackay et al, 2016;Pyne-O'Donnell et al, 2016), demonstrates the excellent potential for developing a cryptotephra framework across northern North America.…”
Section: Introductionmentioning
confidence: 99%
“…This new dataset includes proximal deposits of the 1980 MSH eruption (UA 3005, UA 3006), layer T (UA 2305/6, UA 3326; dated to ad 1799–1800 via tree ring analysis) (Lawrence, ; Yamaguchi, ; Mackay et al ., ), and a previously undescribed tephra (UA 3008) collected on the southern flank of the volcano. We include analyses of the crystal‐rich light‐gray dacite from the 1980 cryptodome (UA 3109), which was the most abundant lithology (~72%) erupted by the 18 May 1980 lateral blast (e.g.…”
Section: Introductionmentioning
confidence: 99%