Railroad accident report : Southern Pacific Transportation Co. freight train 2nd BSM 22 munitions explosion, Benson, Arizona, May 24, 1973 /

Mode of access: Internet.

In the Circuit Court of the United States. The County of San Mateo vs. The Southern Pacific Railroad Company. Argument of

Mode of access: Internet.

In the District Court of the United States for the Southern District of California, Northern Division, before Hon. Benjamin F. Bledsoe, United States District Judge : United States of America, plaintiff, vs. Southern Pacific Company, et al., Defendants. In Equity No.46 Civil, A-16, A-24, A-25, A-26, A-28.

Cover title.

Southern Pacific Company and Oregon and California Railroad Company v. Interstate Commerce Commission. Appendix to Brief for the Interstate Commerce Commission.

Cover-title.

Before the Interstate Commerce Commission. In the matter of the transportation of salt from Hutchinson, Kans. Hearing at Hutchinson, Kans., December 5, 1903. Present: Commissioner Charles A. Prouty. Appearances: Mr. J.H. Richards, general attorney, Missouri Pacific Railway Company. Mr. H. Whiteside, counsel, Atchison, Topeka and Santa Fe Railway Company. Mr. F.L. Martin, counsel, Chicago, Rock Island and Pacific Railway Company. Mr. John T. Marchand and Mr. W.G. Fairchilds, for the Commission.

Mode of access: Internet.

In the Circuit Court of the United States for the Southern District of New-York. Before the Honorable Samuel Nelson and the Honorable Samuel Blatchford. May 5, 1870. James Fisk, Jr., vs. the Union Pacific Railroad Company and others ... Argument of Samuel J. Tilden for defendants, in reply to Mr. Stoughton and Mr. Field.

Mode of access: Internet.

Southern Pacific company, a corporation, petitioner vs. A.J. Pillsbury, Will J. French and Harris Weinstock, as members of and constituting the Industrial Accident Commission of the State of California, Respondents : Brief for respondents, statement of facts and issues.

At head of title: S.F. no. 6993. In the Supreme Court of the State of California.

Before the Interstate commerce commission. In the matter of the application of the Great northern railway company, etc., Finance docket no. 7439. In the matter of the application of the Western Pacific railroad company, etc. Finance docket no. 7440. In the matter of the application of the Great northern railway company and the Western Pacific railroad company, etc. Finance docket no. 7781 ...

Vol. [1]-[2]. Applicants' opening brief. F.G. Dorety, F.M. Angellotti [and others], attorneys.--v. [3]-[5] Brief for Southern Pacific company, Union Pacific railroad company, Oregon short line railroad company, Oregon-Washington railroad & navigation company and Los Angeles & Salt Lake railroad company, interveners. B.C. Dey, G.V. Shoup [and others] attorneys.

Pendleton Artificial Reef: annual progress report presented to Southern California Edison Company

(PDF contains 82 pages.)

The new California Line via Atchison, Topeka and Santa Fe Railroad and Southern Pacific Railroad

The new California Line via Atchison, Topeka and Santa Fe Railroad and Southern Pacific Railroad. This schedule is torn. This does not affect text, n.d.

(Table 2) Integrated concentration, production and dissolution of silica in the water column of the southern Pacific

An intense diatom bloom developed within a strong meridional silicic acid gradient across the Antarctic Polar Front at 61°S, 170°W following stratification of the water column in late October/early November 1997. The region of high diatom biomass and the silicic acid gradient propogated southward across the Seasonal Ice Zone through time, with the maximum diatom biomass tracking the center of the silicic acid gradient. High diatom biomass and high rates of silica production persisted within the silicic acid gradient until the end of January 1998 (ca. 70 d) driving the gradient over 500 km to the south of its original position at the Polar Front. The bloom consumed 30 to >40 µM Si(OH)4 in the euphotic zone between about 60 and 66°S leaving near surface concentrations <2.5 µM and occasionally <1.0 µM in its wake. Integrated biogenic silica concentrations within the bloom averaged 410 mmol Si/m**2 (range 162-793 mmol Si/m**2). Average integrated silica production on two consecutive cruises in December 1997 and January 1998 that sampled the bloom while it was well developed were 27.5±6.9 and 22.6±20 mmol Si/m**2/d, respectively. Those levels of siliceous biomass and silica production are similar in magnitude to those reported for ice-edge diatom blooms in the Ross Sea, Antarctica, which is considered to be among the most productive regions in the Southern Ocean. Net silica production (production minus dissolution) in surface waters during the bloom was 16-21 mmol Si/m**2/d, which is sufficient for diatom growth to be the cause of the southward displacement of the silicic acid gradient. A strong seasonal change in silica dissolution : silica production rate ratios was observed. Integrated silica dissolution rates in the upper 100-150 m during the low biomass period before stratification averaged 64% of integrated production. During the bloom integrated dissolution rates averaged only 23% of integrated silica production, making 77% of the opal produced available for export to depth. The bloom ended in late January apparently due to a mixing event. Dissolution : production rate ratios increased to an average of 0.67 during that period indicating a return to a predominantly regenerative system. Our observations indicate that high diatom biomass and high silica production rates previously observed in the marginal seas around Antarctica also occur in the deep ocean near the Polar Front. The bloom we observed propagated across the latitudinal band overlying the sedimentary opal belt which encircles most of Antarctica implying a role for such blooms in the formation of those sediments. Comparison of our surface silica production rates with new estimates of opal accumulation rates in the abyssal sediments of the Southern Ocean, which have been corrected for sediment focusing, indicate a burial efficiency of <=4.6% for biogenic silica. That efficiency is considerably lower than previous estimates for the Southern Ocean.

Chemical composition of manganese nodules from the Southern Pacific

Deep sea manganese nodules from the Southern Ocean have been studied using chemical analysis, X-ray diffraction, optical mineragraphic and electron probe microanalysis techniques. The nodules were lower in manganese, iron and associated elements than the average grade of manganese nodules from other localities. A number of chemical relationships have been observed. Nickel, copper, cobalt, barium, zinc, molybdenum, strontium, sulphur and phosphorus are associated with the manganese rich phases and titanium with the iron rich phases. X-ray diffraction analysis and electron probe microanalysis results indicate that the manganese phases are similar to the disordered delta-MnO2 and "manganite" phases reported by other workers.