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Hence, instead of broad deposit framework, determining the newest remobilised Mazama tephra dumps away from primary Mazama tephra is actually difficult. That is compared to the new well-known sedimentary formations inside the remobilised YTT which might be demonstrably caused by transport by-water (Gatti et al. 2013). Which supports our translation that the downslope processes you to triggered the brand new significantly overthickened places (Fig. 3) might have been relatively dead. Yet not, pollen advise that the brand new Mazama emergence occurred in northern hemisphere autumn (Mehringer et al. 1977).
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- The real history displayed from the caldera wall space begins with structure from the fresh andesitic Phantom Cone ∼ 400,000 year B.P.
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Remobilised tephra inside river cores will likely be acknowledged by diffuse top or lower connections to the record sediments, changed GSDs and you may anomalous radiocarbon times surrounding the newest layer (Hopkins et al. 2015). Such as, Swiftcurrent River (web site 150) in the Montana include forty-eight cm out of Mazama tephra however with to twenty-five% clastic contaminants (MacGregor et al. 2011), suggesting the newest coating counted is a mix of number one and you may reworked issue. Sadly, a number of the lake core localities run out of intricate findings of your own tephra coating so it’s difficult to confidently categorize the new tephra while the remobilised or primary. Head community observations from remobilised places identify well-known attributes of non-number 1 Mazama tephra, for example discontinuous beds, lens and you can lover-molded outcrops as well as the co-occurrence with alluvial places (Fig. 3). In which i observed remobilised Mazama tephra, however, there are no visible sedimentary formations; which is different from the newest remobilised YTT places that contain great scale cross-beds (Gatti et al. 2013). The fresh remobilised YTT as well as shows various other GSDs versus primary YTT (Gatti et al. 2011, 2013); however, the fresh GSD of one’s remobilised and you will first Mazama tephra are practically the same, no less than ~ 150–500 kilometres away from origin (Fig. 5).
