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Therefore, as opposed to greater deposit perspective, pinpointing the fresh remobilised Mazama tephra dumps from number one Mazama tephra is actually tough. This can be in contrast to the fresh popular sedimentary structures in the remobilised YTT which can be demonstrably caused by transportation by-water (Gatti et al. 2013). That it helps our very own interpretation the downslope processes you to lead to the new significantly overthickened dumps (Fig. 3) has been seemingly lifeless. Although not, pollen recommend that the new Mazama eruption took place northern hemisphere trip (Mehringer et al. 1977).

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Remobilised tephra inside the river cores might be recognized by diffuse higher otherwise all the way down connectivity to your history sediments, altered GSDs and anomalous radiocarbon schedules surrounding the new covering (Hopkins et al. 2015). Such as, Swiftcurrent River (site 150) inside Montana includes forty eight cm from Mazama tephra but with up to 25% clastic toxic contamination (MacGregor et al. 2011), recommending the newest covering mentioned are a mixture of number one and you can reworked thing. Sadly, many of the river core localities run out of intricate observations of your own tephra level so it’s tough to confidently classify the brand new tephra as the remobilised or number 1. Direct community findings of remobilised deposits identify common attributes of non-number one Mazama tephra, including discontinuous beds, lens and you can lover-formed outcrops and the co-thickness which have alluvial dumps (Fig. 3). Where i seen remobilised Mazama tephra, but not, there had been zero noticeable sedimentary structures; so it differs from the newest remobilised YTT dumps which contain good measure cross-beds (Gatti et al. 2013). The fresh remobilised YTT and exhibits various other GSDs versus primary YTT (Gatti et al. 2011, 2013); on the other hand, the fresh GSD of the remobilised and you can first Mazama tephra are almost identical, at least ~ 150–500 km away from source (Fig. 5).