Kushendratno James Stimac Cecilia F. Avendano Rodriguez de Harpel Sofyan Primulyana Christopher Harpel 2019 <div id="Abs1-section" class="c-article-section"><div id="Abs1-content" class="c-article-section__content"><p>A VEI 5 dacite eruption emplaced the Orange Tuff about between 34.3&nbsp;cal&nbsp;kBP and 17.2&nbsp;cal&nbsp;kBP. Gunung Salak is the unit’s source and the Orange Tuff represents the most recent such eruption from any of the volcanoes southwest of Bogor, Indonesia. The Orange Tuff is the region’s first such documented tephra-fall deposit whose characteristics and phenocryst geochemistry make it readily identifiable over at least 1250&nbsp;km². Magnetite compositions and temperature and<span>&nbsp;</span><i>f</i>O₂<span>&nbsp;</span>estimates inferred from Fe-Ti oxide compositions are particularly useful for identifying the unit. Deposit characteristics suggest that the eruption lasted 1–11&nbsp;h with mass eruption rates of 1.0–8.3 × 10⁸&nbsp;kg/s and a column height of 31–40&nbsp;km. The eruption’s column height and the deposit’s 2.5–11&nbsp;km³<span>&nbsp;</span>volume suggest that the unit was dispersed over a much wider area than mapped. The unit is a marker bed throughout its mapped distribution and has potential to be applied over a much broader area as a regional marker bed. The large population and infrastructure proximal to Salak suggest that the unit should be considered in hazards assessments despite its age and the lack of subsequent similar eruptions.</p></div></div><div id="Sec1-section" class="c-article-section"><br></div> application/pdf 10.1007/s00445-019-1292-y en Springer The Orange Tuff: A Late Pleistocene tephra-fall deposit emplaced by a VEI 5 silicic Plinian eruption in West Java, Indonesia article