Receipt from Adam, Meldrum and Anderson, Buffalo, New York

Receipt from Adam, Meldrum and Anderson, Buffalo, New York for sateen, May 17, 1887.

Receipt from A. Cutler and Son, Buffalo, New York

Receipt from A. Cutler and Son, Buffalo, New York for oak chairs in leather and bookcase, Sept. 19, 1887.

Receipt from A. Cutler and Son, Buffalo, New York for oak chairs in leather and bookcase, Sept. 19, 1887

Receipt from A. Cutler and Son, Buffalo, New York for oak chairs in leather and bookcase, Sept. 19, 1887.

Receipt from Lucien Howe, M.D., Buffalo, New York for ear examination

Receipt from Lucien Howe, M.D., Buffalo, New York for ear examination, Sept. 24, 1887.

Receipt from the Genesee, Buffalo, New York for rooms rented

Receipt from the Genesee, Buffalo, New York for rooms rented, Sept. 24, 1887.

Fourth International congress on school hygiene, Buffalo, New York, U.S.A., August 25-30, 1913. Transactions;

Subtitle vol. II-V: Papers.

The breakwater at Buffalo, New York

"Reprinted from Transactions, vol. LII, p. 73 (1904)"

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.

Report of the Buffalo school survey; report of a survey of the public schools of Buffalo, New York, made upon invitation of the Board of education of the city of Buffalo

"The Bureau ... [selected] the United States Office of education ... to survey the 'educational service' of the Buffalo schools ... The more strictly 'business' affairs of the Department of education ... [were] handled by the staff of the Buffalo bureau."-- General introd.

Description and chemical composition of ferromanganese deposits from Oneida Lake, New York

Saucer-shaped iron-manganese crusts occur adjacent to gravel shoal areas in Oneida lake in central New York. The crusts usually have a crude concentric banding owing to an alternation of orange, iron-rich layers and black, iron-poor layers. Materials from both types of layers are x-ray amorphous. The Oneida lake crusts, like most other freshwater manganese nodules, contain about the same Mn concentration as marine manganese nodules, but are usually higher in Fe and lower in trace metals than their marine equivalents. Although Fe and Mn may be precipitating directly from the lake water, it is more likely that the oxidate crusts are the result of precipitation of Fe and Mn when reduced sediment pore water comes in contact with well oxygenated bottom waters. Organisms, particularly bacteria, may play a role in the formation of the crusts, but to date no evidence of this has been found.

An historical review of waterways and canal construction in New York state,

Includes index.

A tour from the City of New-York, to Detroit, in the Michigan Territory, made between the 2d of May and the 22d of September, 1818 : the tour extends from New-York, by Albany, Schenectady, and Utica to Sacket's Harbor, and thence throught Lake Ontario, to St. Lawrence river, and down that stream to Hamilton village. Thence along both banks of the St. Lawrence, from Hamilton to the Thousand Islands; thence to Sacket's Harbor by water; from that place by the route of great Sodus, Geneva, Cananaigua and Batavia, to Buffalo; and from thence to Black Rock, Fort Erie, the Falls of Niagara, Queenston, Lewiston, and the memorable fields of Bridgewater and Chippewa after viewing the interesting place of Niagara, the author traversed the south shore of Lake Erie to the City of Detroit, and visited in the latter range, Dunkirk, Erie, Cleveland, Sandusky, and other places of less note. The tour is accompanied with a map upon which the route will be designated; a particular map of the Falls andRiver of Niagara, and the environs of the City of Detroit /

Errata slip inserted.