@article {778,
	title = {Pyroclastic stratigraphy of the Soufriere Hills volcano, Montserrat - Implications for the present eruption},
	journal = {Geophysical Research Letters},
	volume = {25},
	year = {1998},
	note = {119mkTimes Cited:24Cited References Count:9},
	month = {Sep 15},
	pages = {3393-3396},
	abstract = {The stratigraphy of the Soufriere Hills volcano is dominated by dense-andesite block and ash flow deposits. Forty-one radiocarbon ages permit a reconstruction of the eruptive history over the past 31,000 years. A single stratigraphic member yielding radiocarbon ages of 22,000 to 20,000 years B.P. is composed of block and ash flow deposits with semi-vesiculated clasts concentrated in the upper third of each deposit. The present eruption is also producing block and ash flow deposits with both dense and semi-vesiculated clasts. It marks a return to a more explosive driven type of activity as occurred 22,000 to 20,000 years ago. Deposits of this member have a broad sheet-like form and volumes in excess of any produced so far by the present eruption.},
	issn = {0094-8276},
	doi = {10.1029/98gl00643},
	author = {Roobol, M. J. and Smith, A. L.}
}
