994 resultados para Benzi, Bernardino, 1688-1768


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T.B. Jervis; the chinese characters and explanations rendered into English were furnished by Mr. Samuel Birch, from a comparison of the above documents and the notes appended to the original by the students in the Missionary College at Naples.

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No more published.

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Tít. en antep.: "Totius latinitatis lexicon opera et studio Aegidi Forcellini ; lucubratum et in hac editione novo ordine digestum amplissime auctum atque emendatum adjecto insuper altera quasi parte Onomastico totius latinus cura et studio Doct. Vicenti de-Vit"

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Advertisement of v. 2 signed: H.W. Torrey.

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Advertisements: p. 46-48.

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"With two additional articles viz. of imposition of hands and singing of Psalms in public worship, also A treatise of church discipline."

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The Valley Mountain 15’ quadrangle straddles the Pinto Mountain Fault, which bounds the eastern Transverse Ranges in the south against the Mojave Desert province in the north. The Pinto Mountains, part of the eastern Transverse Ranges in the south part of the quadrangle expose a series of Paleoproterozoic gneisses and granite and the Proterozoic quartzite of Pinto Mountain. Early Triassic quartz monzonite intruded the gneisses and was ductiley deformed prior to voluminous Jurassic intrusion of diorite, granodiorite, quartz monzonite, and granite plutons. The Jurassic rocks include part of the Bullion Mountains Intrusive Suite, which crops out prominently at Valley Mountain and in the Bullion Mountains, as well as in the Pinto Mountains. Jurassic plutons in the southwest part of the quadrangle are deeply denuded from midcrustal emplacement levels in contrast to supracrustal Jurassic limestone and volcanic rocks exposed in the northeast. Dikes inferred to be part of the Jurassic Independence Dike Swarm intrude the Jurassic plutons and Proterozoic rocks. Late Cretaceous intrusion of the Cadiz Valley Batholith in the northeast caused contact metamorphism of adjacent Jurassic plutonic rocks...