Cathedra Petri. A political history of the great Latin patriarchate ...

Vols. 3-4 published by Thickbroom Brothers, vol. 5, by William Macintosh.

The climate of England; its meteorological character explained, and the changes of future years revealed. A solution of the great problem which has defied the philosophy of all ages, with meteorological tables from the year 1656 to 1861. With appendix, England's position and England's only hope.

Mode of access: Internet.

Northward over the "great ice" : a narrative of life and work along the shores and upon the interior ice-cap of northern Greenland in the years 1886 and 1891-1897.

Mode of access: Internet.

The great roll of the pipe for the fifth[-thirty-fourth] year of the reign of King Henry the Second, A.D. 1158[-1188]

Prospectus of the society in v. 1; List of members and Reports of the council, in the most of the volumes.

Frederick the Great, the memoirs of his reader, Henri de Catt (1758-1760)

Translation of: Unterhaltungen mit Friedrich dem Grossen.

The life and letters of the great Earl of Cork,

Mode of access: Internet.

The great composers, or Stories of the lives of eminent musicians,

"Fifth edition."

Coregonid Fishes of the Great Lakes /

Bibliography: p. 632-643.

Syllabus for Humanities 151, The Great books in the modern world, first course.

Cover title.

Four thousand miles across Siberia on the great post-road /

Originally published under the title: Across Siberia on the great post road.

The great world's farm; some account of nature's crops and how they are grown,

2d ed.

The great hall, Winchester Castle /

Mode of access: Internet.

State Social Safety Net Programs and the Great Recession: The First Line of Defense and the Last Resort for the Economically Disadvantaged

Thesis (Ph.D.)--University of Washington, 2016-06

Unequally Unemployed: Labor Market Stratification After the Great Recession

Thesis (Ph.D.)--University of Washington, 2016-06

The source of the Great Dyke, Zimbabwe, and its tectonic significance: Evidence from Re-Os isotopes

Re-Os data for chromite separates from 10 massive chromitite seams sampled along the 550-km length of the 2.58-Ga Great Dyke layered igneous complex, Zimbabwe, record initial 187Os/188Os ratios in the relatively narrow range between 0.1106 and 0.1126. This range of initial 187Os/188Os values is only slightly higher than the value for the coeval primitive upper mantle (0.1107) as modeled from the Re-Os evolution of chondrites and data of modern mantle melts and mantle derived xenoliths. Analyses of Archean granitoid and gneiss samples from the Zimbabwe Craton show extremely low Os concentrations (3-9 ppt) with surprisingly unradiogenic present-day 187Os/188Os signatures between 0.167 and 0.297. Only one sample yields an elevated 187Os/188Os ratio of 1.008. Using these data, the range of crustal contamination of the Great Dyke magma would be minimally 0%-33% if the magma source was the primitive upper mantle, whereas the range estimated from Nd and Pb isotope systematics is 5%-25%. If it is assumed that the primary Great Dyke magma derived from an enriched deep mantle reservoir (via a plume), a better agreement can be obtained. A significant contribution from a long-lived subcontinental lithospheric mantle (SCLM) reservoir with subchondritic Re/Os to the Great Dyke melts cannot be reconciled with the Os isotope results at all. However, Os isotope data on pre-Great Dyke ultramafic complexes of the Zimbabwe Craton and thermal modeling show that such an SCLM existed below the Zimbabwe Craton at the time of the Great Dyke intrusion. It is therefore concluded that large melt volumes such as that giving rise to the Great Dyke were able to pass lithospheric mantle keels without significant contamination in the late Archean. Because the ultramafic-mafic melts forming the Great Dyke must have originated below the SCLM (which extends to at least a 200-km depth ), the absence of an SCLM signature precludes a subduction-related magma-generation process.