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. 2011 Sep 27;74(2):511–531. doi: 10.1007/s00445-011-0545-1

Table 1.

Post-depositional processes affecting ignimbrites

Process Time scale Features/effects Example Reference
Internal (lithological) Deaeration Minutes to years Density increase Mt. St. Helens, laboratory experiments Wilson and Head 1981; Rowley et al. 1981; Druitt et al. 2004, 2007
Welding Minutes to days Eutaxitic fabric, fiamme, joints Bishop Tuff, Murga Caldera Ignimbrites Ross and Smith 1961; Sparks et al. 1999
Rheomorphism Minutes to hours to days Flow lineations, deposit thickness variations, eutaxitic fabric Borrowdale Volcanic Group, TL Ignimbrite Schmincke and Swanson 1967; Sumner and Branney 2002; Branney et al. 2004
Compaction Weeks to decades Fracture network, subsidence Grants Ridge Tuff, Lascar pumice flow deposit Keating and Valentine 1998; this work
Cooling Years Joints Bishop Tuff Sheridan 1970
Indurationa Decades to millions of years Hardening, fumarolic incrustations, mounds and ridges Valley of 10,000 Smokes; Bishop Tuff; Akdag-Zelve Ignimbrite; Mazama-Crater Lake Griggs 1922; Sheridan 1970; Schumacher and Mues-Schumacher 1997; Bacon 2008
External (environmental) Aeolian erosion Days to millions of years Yardangs, pits Tara Ignimbrite Bailey et al. 2007
Fluvial erosion Days to decades Gullies, channels Atana Ignimbrite Bailey et al. 2007
Mass wasting Days to millennia Fractures, debris flows, lahars Pinatubo Pierson et al. 1992
Remobilization Days to years Secondary pyroclastic flow deposits Pinatubo Torres et al. 1996
Seismic perturbation Weeks to decades Pyroclast reorganization Gramts Ridge Tuff, Poris Ignimbrite, Lascar pumice flow deposit Keating and Valentine 1998; Brown and Branney 2004; this work
Tectonic deformation Millions of years Lineaments, alluvial fans La Pacana Ignimbrites Riquelme et al. 2003

aPartially controlled by external forcing