Annual report of the Buffalo, Rochester and Pittsburgh Railway Company : for year ending ...

Printer varies.

Prospectus of the Buffalo and Washington railway company : with maps of its route and connections with other railroads in Pennsylvania, New Jersey and Maryland. May 1, 1865.

Mode of access: Internet.

Report of Messrs. Johnson and Wood on a central line of railway into Scotland made by them to the directors of the Newcastle-upon-Tyne and Carlisle Railway Company.

Mode of access: Internet.

Delineations of the north western division of the county of Somerset, and of its antediluvian bone caverns, with a geological sketch of the district.

Half-title: Delineations of ... Somerset, and of the Mendip caverns.

Lancashire and Cheshire, past and present: a history and a description of the palatine counties of Lancaster and Chester, forming the North-western division of England, from the earliest ages to the present time (1867).

Added t.-p., engr.

The railways of England : North Western; Midland; Great Northern, Manchester, Sheffield, and Lincoln; North Eastern; South Western; Great Western; Great Eastern; Brighton and South Coast; Chatham and Dover; South Eastern /

Includes index.

Motor and Cars of the Ypsilanti and Ann Arbor Street Railway. - Showing Military Company

Streetcars. On verso: Train and Military Company from Nov. 1895 MichStoner, Claude Thomas, 1899-1977igan Central Magazine, "Headlight"

Presentation in behalf of the shop craft employes, Chesapeake and Ohio Railway Company before the Federal Arbitration Board;

Mode of access: Internet.

In the matter of the arbitration between Transport Workers Union of America, Local 100 and New York City Omnibus Corporation; Fifth Avenue Coach Company; Jamaica Buses, Inc.; Triboro Coach Company; Queens-Nassau Transit Lines, Inc.; Steinway-Omnibus Corporation; Queensboro Bridge Railway Company, Inc.; Avenue B and East Broadway Transit Company, Inc. : opinion and award /

Cover title.

The constitution of the North-Western branch of the American Society for Educating Pious Youth for the Gospel Ministry : with instructions for beneficiaries, directions for agents, and an address to the Christian publick.

Cover title.

Official statement of the Northern Pacific Railway Company, particularly with reference to its preferred and common stock, December 1, 1896.

Mode of access: Internet.

Annual report of the president and directors of the Northern Central Railway Company to the stockholders.

Mode of access: Internet.

Annual report of the board of the directors of the Lake Erie and western railroad company to stockholders

Mode of access: Internet.

Observation of manganese coating and encrustation in different environments of the North-Western Atlantic ocean

The major topographic features, or provinces, beyond the continental slope off the Atlantic coast of the United States are (1) Sohm Plain, (2) Hatteras Plain, (3) Nares Plain, (4) Blake Basin, (5) Blake Plateau-Bahama Banks, and (6) Bermuda Rise. The whole of the described area is commonly referred to as the North American Basin. This basin is bounded on the north by Newfoundland Ridge and on the south by Puerto Rico Trench. Topographic features of note within the basin are the divide and the area of depressions between Sohm and Hatteras Plains, the sharply crested Blake Ridge, and the Puerto Rico Ridge. Recently accumulated data on deep-sea oores has given good evidence that the silt and sand covering the abyssal plains are displaced continental sediments in a virtually quartz-free oceanic environment. These sediments were deposited on a primary volcanic bottom. The primary or volcanic bottom is characterized by abyssal hills and seamounts, and the sediment bottom is characterized by abyssal plains, which extend seaward from the continental margins. On the Blake Plateau, bottom photographs and dredge hauls in the axis of the stream show that locally sediment has been removed and the bottom is paved with crusts and nodules of manganese. Photographs and dredged samples from the outer part of the New England Seamount, Chain and Caryn Peak also indicate extensive encrustations of manganese oxide which acts as a binding agent in areas of ooze or other organic debris and thus helps to stabilize the bottom.

(Table 1) Ice station data during POLARSTERN expeditions ARK-XVIII/2 and ARK-XIX/1 to Fram Strait, the western Barents Sea and north of Svalbard

During two expeditions of the R.V. "Polarstern" to the Arctic Ocean, pack ice and under-ice water samples were collected during two different seasons: late summer (September 2002) and late winter (March/April 2003). Physical and biological properties of the ice were investigated to explain seasonal differences in species composition, abundance and distribution patterns of sympagic meiofauna (in this case: heterotrophs >20 µm). In winter, the ice near the surface was characterized by extreme physical conditions (minimum ice temperature: -22°C, maximum brine salinity: 223, brine volume: <=5%) and more moderate conditions in summer (minimum ice temperature: -5.6°C, maximum brine salinity: 94, most brine volumes: >=5%). Conditions in the lowermost part of the ice did not differ to a high degree between summer and winter. Chlorophyll a concentrations (chl a) showed significant differences between summer and winter: during winter, concentrations were mostly <1.0 µg chl a/l, while chl a concentrations of up to 67.4 µmol/l were measured during summer. The median of depth-integrated chl a concentration in summer was significantly higher than in winter. Integrated abundances of sympagic meiofauna were within the same range for both seasons and varied between 0.6 and 34.1×103 organisms /m**2 in summer and between 3.7 and 24.8×10**3 organisms /m**2 in winter. With regard to species composition, a comparison between the two seasons showed distinct differences: while copepods (42.7%) and rotifers (33.4%) were the most abundant sea-ice meiofaunal taxa during summer, copepod nauplii dominated the community, comprising 92.9% of the fauna, in winter. Low species abundances were found in the under-ice water, indicating that overwintering of the other sympagic organisms did not take place there, either. Therefore, their survival strategy over the polar winter remains unclear.