About 1,000 square miles of the western part of the Taupo Volcanic Zone is covered by the Whakamaru Ignimbrites, a formation consisting of more than a dozen coarse-textured tuff sheets. They are of Pleistocene age, and were erupted over an irregular topographic surface after a prolonged pause in acid ignimbrite volcanism in this province. Locally their total thickness exceeds 1,000 ft. The rocks are generally lightly welded and contain from 10 to 45% of phenocrysts-andesine, quartz, hypersthene, sanidine, magnetite, biotite, and hornblende.