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The andesitic dome-building eruption of the Soufriere Hills Volcano wreaked havoc at the small Caribbean island of Montserrat. approximately half this 'emerald Isle' was once rendered barren and uninhabitable, nearly two-thirds of the unique inhabitants needed to go away, and 19 lives have been misplaced, all as an instantaneous results of the volcanic task.
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Extra info for Advances in Jurassic Research 2000. Proceedings of the Fifth International Symposium on the Jurassic System. R.L. Hall and P.L. Smith (Eds.), GeoResearch Forum 6
6 topotypes, all from the type locality and horizon, including SMC X29336 (plate 2, figure 8) (Sedgwick Museum Cambridge collections). Diagnosis. - Vermiceras with extremely dense ribbing throughout ontogeny. Remarks. - The development of ribbing (Fig. 4) resembles that of V palmeri (Fig. 5), but the rib numbers are far higher. In the density of ribbing the species resembles certain echioceratids from the Upper Sinemurian. Vermiceras elegans Remark on Metophioceras sp. indet. A Scarce fragments (PI.
JELETZKYI + ? A. CF. SALTFUENSE + AFINIOCERAS SP. +A. AS A. RETUSUM A . SP. AFF. MAAGAFIT I A + ARNIOCERAS SP. ASTEROCERAS SP. , HIU£BPANOT 1987 ARNIOCERAS SP. f :A. P. �=A ASTEAOCERAS ? SP. A f ...... 12 fih Jurassic Symposium, Vancouver HILLEBRANDT, A. v. 1 98 1 . Faunas de amonites del Liasico Inferior y Medio (Hettangiano hasta Pliensbachiano) de America del Sur (excluyendo Argentina), p. 499-537. In Comite Sudamericano del Jurasico: Cuncas sedimentarias del Jurasico y Cretacico de America del Sur, 2.
The sequence passes from the cliff into the ledges on the foreshore so that the identification of individual beds on the foreshore is easy. The facies is typical "Blue Lias", a sequence of marls and bituminous shales and intercalated marly limestone beds. Detailed sections on this part of the coast were first provided by Palmer ( 1 972, p. 70-7 1 , 73). The bed numbers of Whittaker and Green are used here, with Palmer's notation in brackets. lvimey-Cook and Donovan ( 1 983, p. 1 28- 1 29) gave a brief account of the ammonite fauna which did not permit a subdivision of the Angulata Zone, and details of the ammonite succession in the Conybeari Subzone remained uncertain.