New England in the republic, 1776-1850.

Mode of access: Internet.

An Anglo-Chinese calendar for the years 1892-1911.

Mode of access: Internet.

The story of the life of MacKay of Uganda told for boys by his sister.

Mode of access: Internet.

Ancient towers and doorways; being pictorial representations and restorations of masoncfraft relating to Celtic and Norman ecclesiology in Scotland from pen drawings by the late Alexander Galletly ...

"The edition of this work consists of 300 copies, which this is no. ."

The poetical works of Alexander Pope.

Mode of access: Internet.

The record of a happy life : being memorials of Franklin Whitall Smith, a student of Princeton College /

Mode of access: Internet.

A.M. Mackay : pioneer missionary of the Church Missionary Society to Uganda /

Includes index.

Post-mortem use of wealth, including a consideration of ante-mortem gifts;

Mode of access: Internet.

John Bright: born November 16, 1811, died March 27, 1889. An address delivered at Rochdale on November 16, 1911.

Mode of access: Internet.

University of Michigan Football Team, 1911

Back Row: mngr. William Learmonth, Clement Quinn, George Thomson, Stanfield Wells, captain Fred Conklin, Thomas Bogle, William Otis, Richard Meek, Miller Pontius, Neil McMillan

Middle Row: George Paterson, Herschel Smith, Allen Garrells, Grover Herrington, Raymon Cooper, Herbert Hueble, Howard Kayner

Front Row: Otto Carpell, Henry Wenner, Ernest Allmendinger, Roy Torbert, Lawrence Roblee, Frank Picard

1911 UM Track Team

Back Row: Benjamin Reck, ? Smith, George Lawton, Robert Hammond, H.C. Smith, Cole

3rd Row: st. mngr. Herbert Goetz, John Otte, XX Elliott, Roger Waring, Louis Haller, ? Crossman, James Angell McLaughlin, XX White, Ath. Dir. Philip Bartelme

2nd Row: Charles Hall. Edmond Hanavan, Raymond Haimbaugh, Ralph Craig, Carroll Haff, Hugh Gamble, Fred Ross

Front Row (on floor): Charles Kime, Frederick(?) Beardsley, Walter Willits, Cleon Spangler, XX Pierce,

The works of Alexander Hamilton,

First edition (500 copies) in 9 vols., published 1885-86.

The theories of inspiration of the Rev. Daniel Wilson, Rev. Dr. Pye Smith, and the Rev. Dr. Dick, proved to be erroneous : with remarks on the Christian observer, & Eclectic review,

Mode of access: Internet.

Briefe über Alexander von Humboldt's Kosmos. Ein Commentar zu diesem Werke für gebildete Laien.

Vols. 1 and 3 edited by Bernhard von Cotta; v. 2. by Julius Schaller.

Fossil associations from the middle and upper Eocene strata of the Pamplona Basin and surrounding areas (Navarre, western Pyrenees)

Fossil associations from the middle and upper Eocene (Bartonian and Priabonian) sedimentary succession of the Pamplona Basin are described. This succession was accumulated in the western part of the South Pyrenean peripheral foreland basin and extends from deep-marine turbiditic (Ezkaba Sandstone Formation) to deltaic (Pamplona Marl, Ardanatz Sandstone and Ilundain Marl formations) and marginal marine deposits (Gendulain Formation). The micropalaeontological content is high. It is dominated by foraminifera, and common ostracods and other microfossils are also present. The fossil ichnoasssemblages include at least 23 ichnogenera and 28 ichnospecies indicative of Nereites, Cruziana, Glossifungites and ?Scoyenia-Mermia ichnofacies. Body macrofossils of 78 taxa corresponding to macroforaminifera, sponges, corals, bryozoans, brachiopods, annelids, molluscs, arthropods, echinoderms and vertebrates have been identified. Both the number of ichnotaxa and of species (e. g. bryozoans, molluscs and condrichthyans) may be considerably higher. Body fossil assemblages are comparable to those from the Eocene of the Nord Pyrenean area (Basque Coast), and also to those from the Eocene of the west-central and eastern part of South Pyrenean area (Aragon and Catalonia). At the European scale, the molluscs assemblages seem endemic from the Pyrenean area, although several Tethyan (Italy and Alps) and Northern elements (Paris basin and Normandy) have been recorded. Palaeontological data of studied sedimentary units fit well with the shallowing process that throughout the middle and late Eocene occurs in the area, according to the sedimentological and stratigraphical data.