The compositionally zoned eruption of 1912 in the Valley of Ten Thousand Smokes, Katmai National Park, Alaska
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Cited by (218)
Origin of the compositionally zoned Paso Puyehue Tephra, Antillanca Volcanic Complex, Chile
2023, Journal of Volcanology and Geothermal ResearchLate Holocene paleoseismology of Shuyak Island, Alaska
2018, Quaternary Science ReviewsCitation Excerpt :We submitted 43 samples for AMS radiocarbon dating, picking herbaceous macrofossils from the sediment (Table 1). We derive an age model for each site with Oxcal 4.3 (Bronk Ramsey, 2001, 2008), using the P_Sequence model, which allows for a variable sediment rates, building in a hiatus at each sharp boundary between sediment layers, and constrain the model at the base of the distinct Katmai tephra, AD 1912 (Hildreth, 1983). We set the model parameters to generate age estimates at 1 mm intervals and therefore modelled ages for each diatom sample.
Conditions of pinnacle formation and glass hydration in cooling ignimbrite sheets from H and O isotope systematics at Crater Lake and the Valley of Ten Thousand Smokes
2018, Earth and Planetary Science LettersCitation Excerpt :Mt. Mazama is gradationally bimodal, exhibiting andesitic and rhyodacitic pumice clasts throughout the deposit but with an increased proportion of andesitic clasts towards the top (Druitt and Bacon, 1986). Similarly, Novarupta produced abundant initial rhyolite, followed by a mixture of dacite and andesite (Hildreth, 1983). Our study is based on the investigation of this rhyolitic glass in individual pumice clasts collected from pinnacles in both locations that are tied to this inverted stratigraphy.
The origin of a coarse lithic breccia in the 34 ka caldera-forming Sounkyo eruption, Taisetsu volcano group, central Hokkaido, Japan
2018, Journal of Volcanology and Geothermal ResearchCitation Excerpt :We conclude that the occurrence of lithic breccias within small caldera-forming eruption products does not necessarily reflect the presence and the timing of caldera collapse. Besides Ohachidaira, small calderas inferred to have formed by vent widening include Novarupta (Hildreth, 1983) and Caldeira in Faial, Azores (Pimentel et al., 2015), all of which show a detailed stratigraphy of tephra from the caldera-forming eruptions, but do not provide direct insight into subsurface structures. However, some Japanese small calderas, Nigorikawa in southwestern Hokkaido (Ando, 1983; Kurozumi and Doi, 2003), Sunagohara in northeastern Honshu (Mizugaki, 1993, 2000), and Gora in the Hakone volcano group (Mannen, 2008, 2014), are well constrained in three dimensions to have a funnel-shaped conduit by geothermal drilling.