Hudson Bay; or, Everyday life in the wilds of North America, during six years' residence in the territories of the Hon. Hudson Bay Company.

First edition, Edinburgh, 1848.

Ethnographic bibliography of North America.

Mode of access: Internet.

Ethnographic bibliography of North America.

Mode of access: Internet.

A statistical, political, and historical account of the United States of North America; from the period of their first colonization to the present day.

Brief bibliographies at end of many of the chapters.

Address on the present condition and prospects of the aboriginal inhabitants of North America : with particular reference to the Seneca nation, delivered at Buffalo, New York /

Mode of access: Internet.

An essay on a uniform orthography for the Indian languages of North America, as published in the Memoirs of the American Academy of Arts and Sciences.

"Appendix. Account of Father Râle's ms. Indian dictionary": p. [40]-42.

Address on the present condition and prospects of the aboriginal inhabitants of North America, with particular reference to the Seneca Nation /

Mode of access: Internet.

Some particulars relative to the continuance of the endeavours : on the part of the Society of Friends in the United States of North America, for the improvement and gradual civilization of the Indian natives.

"Advertisement": p. [iii]-v at beginning.

A sketch of the further proceedings of the committees appointed by the Yearly Meetings of Friends of Pennsylvania, &c. and Maryland : for promoting the improvement and gradual civilization of the Indian natives in some parts of North America.

Mode of access: Internet.

A discourse on the religion of the Indian tribes of North America. Delivered before the New-York historical society, December 20, 1819.

Shoemaker 1782.

Voyages from Montreal through the continent of North America to the frozen and Pacific oceans in 1789 and 1793; with an account of the rise and state of the fur trade.

Introduction signed: Robert Waite.

An overview of the labor market problems of Indians and Native Americans /

Item 1089-H

Treaty between the United States of America and the Chippewa Indians of Saginaw, Swan Creek, and Black River, Michigan. Concluded October 18, 1864. Ratification advised, with amendments, May 22, 1866. Amendments accepted June 18, 1866. Proclaimed August 16, 1866.

"Concluded at Isabella ... Michigan."

Cultural and natural areas of native North America,

Cover title.

Molluscan carbonate geochemistry and paleoceanography of the Late Cretaceous western interior seaway of North America

North Amerlc8 W8S inundated by fJ major eplcontlnental sea during ihe C:retaceo.us Period. The sOljihw6rd transgression of th.e northern Boreal See along the ~\festern Interior Seaway resulted in a meetlng with the northward edv6nclng waters from the GUlf of Mexico (Obradovich and Cobban, 1975). Th1s link was 1n eXlstence by late Albien time and 6llowed for the comm1ngl1ng of the prol1ferous Arctic and Gulf rnar1ne faunas (F1g. 1). By early Campanlan time, there was a widening of B6ffln Bay wlth a slrnult8neous subsidence 1n the Arct1c Archlpelago and Sverdrup 6as1n (W11liam and Stelck, 1975). Williams and Burk (1964) found 6 break 1n the marines sedlmentatlon in the f1anltoba area, suggesting Bland corlnectlon from the Dlstrlct of Keewatln through eastern M6fl1toba to the lake Sl~perlor reglon, lmplying that the only dlrect connection between the Interlor Sea with Baffln Bay, was yia the Arct1c. This hiatus was also documented by Meek and Hayden (1861) ln the United states between the Niobrara and Pierre Format1ons. Jeletzky (1971) suggested that the retreat of the sea towards the east was by a serles of strong pulses resultlng in the regression of the Campanlan and M66str1chtlan seas. During ttle Cretaceous1 the r1s1ng Corl1111era caused the western shoreline of the Interlor Sea to migrate eastwards and the Cordillera'l detritus produced deltaic cornplexes from the Mackenzie Valley to Ne\N Mexlcoo The foreland basin was continually subslding and thls down\",arplng aided in the eastward m1gration of the western shorel1ne. Thls also lndicates that trle water 'tIes becom1ng deeper in the central Plains sect10n of the Seaway (Fig. 2).