The diary of General Grow as exposed by Major Richard Squires /

Cover title.

Indenture between William Kingsmill and Peter Buchanan, Isaac Buchanan, Robert W. Harris and I. Young

Indenture (vellum) between William Kingsmill, Sheriff of Niagara regarding the sale of goods and chattels of Darius Ball including buildings and improvements in Lot no. 4 near Grand River to Peter Buchanan, Isaac Buchanan, Robert W. Harris and I. Young, July 22, 1844.

Dra. Celia Ortiz Arrigos de Montoya : (1895-1985)

Fil: Pró, Diego F.. Universidad Nacional de Cuyo. Facultad de Filosofía y Letras. Instituto de Filosofía Argentina y Americana

Schembechler Hall reception, Bo Schembechler, Robert W. Brown

[at President's House]

Schembechler Hall reception, Bo Schembechler, Robert W. Brown

[at President's House]

Robert W. Barbour : letters, poems, and pensées /

Preface [by] Henry Drummond---Memorial chronology [by] James Stalker--Pensées--Poems--Letters--Biographical notices.

Proceedings of the United States senate and the House of representatives in the trial of impeachment of Robert W. Archbald, additional circuit judge of the United States from the third judicial circuit and designated a judge of the Commerce court.

Mode of access: Internet.

(Table 1) Geochemistry of upper Paleocene and upper Eocene glass particles at DSDP Hole 80-549

Two ash horizons have been identified in Hole 549, one in the upper Paleocene (basal NP9), the other in the upper Eocene (NP18); both are mixed lithic crystal tuffs of rhyolitic composition. These tuffs are absent in Hole 550 owing to unconformities, but the basal Eocene (NP10) of Hole 550 includes a series of over 50 thin bentonite layers. Intermediate plagioclase associated with these bentonites indicates that the original ash was of basaltic to andesitic composition. The bentonites are absent in Hole 549, probably because of an unconformity, but they have been identified in Hole 401 (Leg 48, Bay of Biscay). Two of the pyroclastic phases can be matched with phases previously reported for the North Sea Basin. The bentonites of Site 550 are probably equivalent to the widespread "ash series" of northwestern Europe, which may therefore be regarded as being lower Eocene in terms of Martini's calcareous nannoplankton zonation.