View overlooking the Hutton Sports Complex at Chapman College, Orange, California

View from Hashinger Hall overlooking the Hutton Sports Complex at Chapman College, Orange, California, 1979. Rooftops of residences and trees in the foreground; the stadium and athletics field in the background.

First building of Orange Union High School, Orange, California, now Wilkinson Hall, Chapman University

Orange Union High School, located at 333 N. Glassell Street, Orange, California, 1905. Constructed in 1905 and designed by local architect, C.B. Bradshaw, image shows main building, now called Wilkinson Hall, which moved north prior to 1921. Acquired in 1954 and currently operated by Chapman University; it was renamed Wilkinson Hall in honor of J. E. Wilkinson, a former trustee, chairman of the board, and acting president. View shows front and south elevations across North Glassell Street.

Wilkinson Hall, Chapman College, Orange, California

Wilkinson Hall, 301 N. Orange Street, Chapman College, Orange, California. J.E. Wilkinson was a former trustee, chairman of the board, and acting president. This building was the first on the campus of Orange Union High Schooi, designed by local architect, C.B. Bradshaw and constructed in 1905 by R. J. Noble. In 1921 it was moved 250 feet and turned 90 degrees to its current location. Acquired in 1954 by Chapman College. it houses the Provost’s office, Academic Affairs, English & Comparative Literature, Graduate Studies, and the departments of Religion and Philosophy. It is listed in the National Registry for Historical Buildings.

Letter to S.D. Woodruff from J.J.B. at the National Hotel in East Saginaw, Michigan

Letter to S.D. Woodruff from J.J.B. at the National Hotel in East Saginaw, Michigan. The writer informs Mr. Woodruff that there is about 26,000 of first class board pine which was cut. Mr. Woodruff did not give a receipt to Barton and Bro., Jan. 20, 1880.

Manual of the botany of the Northern United States : including the distriet east of the Mississipi and North of North Carolina and Tennessee

UANL

The Rise and Decline of the East German Economy, 1949-1989.

Why do some organizations decline while other do not? to study this issue , we introduce technological change into a theory of agency proposed by Laffont and Tirole. We show that the optimal organizational form for production depends on the estent of scale ecoomies and on the cost of monitoring workers. When the discrepancy between ideal and actual forms becomes too great, an organization's viability is threatened. We test this structuralist hypothesis for East and west Gemany over the 1949-1989 period. east Germany's relative decline is explained by an institutional structure the proved incompatible with technological change favoring smaller, flatter organizations.

Mixed layer characteristics and hydrography off the west and east coasts of India

In this thesis, a detailed attempt has been made to understand the general hydrography of the upper 300m of the water column, in the eastern Arabian Sea and the western Bay of Bengal, the two contrasting basins in the northern Indian Ocean, using recently collected data sets of Marine Research-Living Resources (MR-LR) assessment programme, funded by Department of Ocean Development, from various cruises, pertaining to different seasons. Initially it discuss the general hydrography of the west and east coasts of India are covered, in the context of mixed layer processes. The study describes the materials and methods . To compare the hydrography of the AS and BOB, a unique MLD(Mixed Layer Depth) definition for AS and BOB is essential, for which the 275 CTD profiles were used. A comparison has been made among the various MLD criteria with the actual MLD. The monthly evolution of MLD, barrier layer thickness and the role of atmospheric forcing on the dynamics of the mixed layer in the AS and BOB were studied. The general hydrography along the west coast of India is described. The upwelling/downwelling, winter cooling processes, in the context of chemical and biological parameters, are also addressed. Finally the general hydrography of the Bay of Bengal is covered. The most striking feature in the hydrography are the signature of an anticyclonic subtropical gyre during spring intermonsoon and a cold core eddy during winter monsoon. The TTS(Typical Tropical Structure) of the euphotic layer was also investigated.

Ecobiogeography, Spatial and Temporal Variations of Microzooplankton Along the East Coast of India

In the present study an attempt has been made to understand the microzooplankton community along the easr coast of India. Most of the earlier studies projected Bay of Bengal as an oligotrophic system where phytoplankton growth is limited by a number of factors among which nutrients are the foremost. Hence it is logical to consider that the most of the primary production in the Bay of Bengal could be contributed by small sized phytoplankton harnessing the available resources, which in turn can be utilized effiency by the microzooplankton only. Hence microzooplankton could play in transferring primary organic carbon to higher tropic levels in this region.