Information relative to New Zealand /

Includes bibliographical references.

Leila or the seige of Granada ; Calderon the courtier ; and the Pilgrims of the Rhine /

On spine: Bulwer Lytton's novels.

Annual report of the Board of Education and the Superintendent of Public Instruction of New Jersey, with accompanying documents, for the school year ending ...

Title varies slightly.

West coast reporter ... : containing all the decisions as fast as filed of the following courts: United States Circuit and District courts of California, Colorado, Nevada, and Oregon, and the Supreme Courts of Arizona, California, Colorado, Idaho, Montana, Nevada, New Mexico, Oregon, Utah, Washington, and Wyoming ; also legal essays and editorial notes

Editors: 1884, J.N. Pomeroy, C.P. Pomeroy; 1885-86, C.P. Pomeroy

The new administration : containing complete and authentic biographies of Grant and his Cabinet /

Ulysses S. Grant, Schuyler Colfax, James G. Blaine, Hamilton Fish, John A. Rawlins, Jacob D. Cox, George S. Boutwell, Adolph E. Borie, John A.J. Creswell, Ebenezer R. Hoar.

History of Merrimack and Belknap counties, New Hampshire.

Mode of access: Internet.

An old New England school : a history of Phillips Academy Andover /

Mode of access: Internet.

Elements of the differential and integral calculus, by a new method, founded on the true system of Sir Isaac Newton, without the use of infinitesimals or limits.

Mode of access: Internet.

Annual report of the Superintendent of Insurance to the New York Legislature.

Combined report issued for 1977-78.

Transactions of the Linnaean Society of New York.

Publication suspended 1885-1932.

Journal of Daniel Coker, : a descendant of Africa, from the time of leaving New York, in the ship Elizabeth, Capt. Sebor, on a voyage for Sherbro, in Africa, in company with three agents, and about ninety persons of colour. : The Rev. Samuel Bacon, John B. Bankson, Samuel S. Crozer. Agents. : With an appendix.

"Appendix to the Rev. D. Coker's Journal" (pages [41]-52) includes "Letter from Nathaniel Peck to his mother in Baltimore".

Entre el terror y la solidaridad : La influencia de la revolución haitiana en las independencias de Venezuela y Nueva Granada (1804-1825)

En este trabajo me propongo analizar la influencia de la revolución de Haití en las independencias de Venezuela y Colombia durante los años 1804-1825. Miintención es demostrar que las repercusiones del proceso haitiano fueron vastas, complejas y sufrieron importantes cambios durante el transcurso de los años. En líneas generales, la revolución generó pánico entre las elites criollas y peninsulares y esperanzas entre grupos de esclavos y pardos. Inicialmente los sectores criollos revolucionarios buscaron evitar todo contacto con la isla y eludir el modelo insurgente haitiano por considerar que produciría en la Tierra Firme una "guerra de razas" y una hecatombe similar a la que, en su opinión, allí había acontecido. Sin embargo, a partir de 1812-1813 debido a las dificultades de la guerra de independencia una fracción de la elite criolla comenzó a estrechar vínculos con la República del Sur de Haití a través de contactos diplomáticos y corsarios. Estas primeras relaciones, más bien tímidas, fueron la condición de posibilidad de un cambio importante que sobrevino en 1816. En dicho año, debido a la reconquista de la expedición realista, la mayoría de los líderes independentistas huyeron de Tierra Firme y tuvieron que exiliarse en Haití, uno de los pocos lugares donde encontraron refugio y apoyo. En aquel contexto, se dio el pacto entre Alexandre Petión y Simón Bolívar, por el cual el primero se comprometió a aportar armas, barcos y hombres a la causa patriota a cambio de la emancipación de los esclavos hispanoamericanos. Este acuerdo fue fundamental ya que no sólo posibilitó la exitosa contraofensiva independentista, sino que además le dio un cariz social al proceso revolucionario de Venezuela y Colombia. Así, a partir de 1816 y hasta 1821, se dieron numerosos contactos e incluso el gobierno de Jean Pierre Boyer (sucesor de Alexandre Petión) colaboró con otras dos expediciones a cargo de Gregor Mac Gregor para liberar Panamá y Río Hacha. Sin embargo, el cambio no fue total y aún durante estos años, los líderes criollos continuaron teniendo reparos frente al peligro de la explosión de un nuevo Haití en la Tierra Firme hispana. Por último, el fin de la guerra de independencia abrió un nuevo contexto en el cual aquellos miedos se intensificaron debido a la movilización social interna. Esto derivó en nuevo alejamiento y el gobierno de Colombia no sólo se negó a mantener relaciones con Haití, sino que incluso lo excluyó del Congreso de Panamá.

Requiescat in park: o Central Park de Nova Iorque sob a ótica do cinema Norte - americano

Taking into account the Environmental Restorative Theory (ERT) , created by Fre derick Law Olmsted in mid XIX ce ntury , according which, urban parks can contribute to solve problems arisen from crowding , particularly urban stress, we analize how the ERT arrived at XXI century, having as approach the evaluation of New York Central Park (CP). Considering that the CP and the cinema were born around at the same, we question if the North American cinema produced between 1960 and 2013 show the ideals, which engendered the CP. By answering this question we defend the hypothesis that, even though has existed adjusts and modificati ons in the CP plan through time, it kept reasonably faithful to the ERT premises, propitiating to the XX and XXI centuries cinema identify and bring forth the presence of the Olmsted’s Ideals in the present days. The thesis main objective was nonetheless u nderstand similarities and/or differences between the XIX century ideals (that gave birth to CP) and the way the cinema represents the present uses of the place, taking into account that the Olmstedian ERT proposal have survived to the context changes (soc ial, economic, political and cultural). Methodologically , we drew upon bibliographical and documental analysis to build the first chapters and to the cinema as analytical lenses to investigate the ERT. The results point that although the CP plan has kept r elatively intact and faithful to the ERT – with the presence of natural elements in the films (notably vegetation and water) – many of contemporary behaviors were not foreseen previously, especially in relation to sports practice, the massive feminine pres ence, as well as criminality.

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.