950 resultados para Blake, William, 1757-1827.
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"Dedicated to the Shakspearean club"-verso of t.-p.
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Mode of access: Internet.
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Bound with other Friends' pamphlets.
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vol. 1. Poems referring to the period of childhood. Juvenile pieces. Poems founded on the affections. Poems of the fancy.--vol. 2. Poems of the fancy. Poems of the imagination. Miscellaneous sonnets.--vol. 3. Memorials of a tour in Scotland, 1803. Memorial of a tour in Scotland, 1814. Poems on the naming of places. Inscriptions. Sonnets dedicated to liberty. Memorials of a tour on the continent, 1820. Ecclesiastical sketches.--vol. 4. The white doe of Rylstone. The prioress's tale. The river Duddon. Poems of sentiment and reflection. Poems referring to the period of old age. Epitaphs and elegiac poems.--vol. 5. The excursion.
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Issued in five parts, 1884-93.
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Mode of access: Internet.
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Mode of access: Internet.
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"An abridgement of Dallas, Cranch, and Wheaton, on the same general plan as the subsequent condensation by Curtis."--Soule, Lawyer's ref. manual, 1884.
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Caption title.
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v. 1. On the principles and character of American institutions, and the duties of American citizens, 1856-1891.--v. 2. Addresses and reports on the reform of the civil service of the United States.--v. 3. Historical and memorial addresses.
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Mode of access: Internet.
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An answer to Huskisson's speech.
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v. 1. Political and ethical.--v. 2. Aesthetical and literary.--v. 3. Critical and ethical.
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Mode of access: Internet.
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An area of about 22,000 km² on the northern Blake Plateau, off the coast of South Carolina, contains an estimated 2 billion metric tons of phosphorite concretions, and about 1.2 billion metric tons of mixed ferromanganese-phosphorite pavement. Other offshore phosphorites occur between the Blake Plateau and known continental deposits, buried under variable thicknesses of sediments. The phosphorite resembles other marine phosphorites in composition, consisting primarily of carbonate-fluorapatite, some calcite, minor quartz and other minerals. The apatite is optically pseudo-isotropic and contains about 6% [CO3]**2- replacing [PO4]**3- in its structure. JOIDES drillings and other evidence show that the phosphorite is a lag deposit derived from Miocene strata correlatable with phosphatic Middle Tertiary sediments on the continent. It has undergone variable cycles of erosion, reworking, partial dissolution and reprecipitation. Its present form varies from phosphatized carbonate debris, loose pellets, and pebbles, to continuous pavements, plates, and conglomeratic boulders weighing hundreds of kilograms. No primary phosphatization is currently taking place on the Blake Plateau. The primary phosphate-depositing environment involved reducing conditions and required at least temporary absence of the powerful Gulf Stream current that now sweeps the bottom of the Blake Plateau and has eroded away the bulk of the Hawthorne-equivalent sediments with which the phosphorites were once associated.