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|description={{|1=(opposite) Schematic cross-sections showing development of the Scafell Caldera during piecemeal collapse. The sequence of events is greatly simplified (after Branney and Kokelaar, 1994). A Emplacement of the Whorneyside Formation ignimbrite and succeeding phreatoplinian ash. B Onset of piecemeal subsidence causing deformation of the Whorneyside deposits; burial beneath hot silicic ash of the Long Top Tuffs erupted from new vents. C Further collapse causing ductile deformation of the hot ignimbrite. D Paroxysmal eruptions producing very densely welded ignimbrites of the Crinkle Tuffs and causing renewed subsidence and fault-scarp collapse.E Waning eruptions and silicic dome emplacement; sedimentation in a caldera lake. Figure 20 in  Stone, P, Millward, D, Young, B, Merritt, J W, Clarke, S M, McCormac, M and Lawrence, D J D. 2010. British regional geology: Northern England. Fifth edition. Keyworth, Nottingham: British Geological Survey.}}&lt;br /&gt;
|date=2016-04-12 18:08:10&lt;br /&gt;
|source=British Geological Survey&lt;br /&gt;
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