From Columbus to Cooperation - Trade and Shipping Policies from 1492 to 1992

This Article summarizes the history of international trade agreements from the time of Columbus to the present

From Columbus to Cooperation - Trade and Shipping Policies from 1492 to 1992

This Article summarizes the history of international trade agreements from the time of Columbus to the present

Introduction- Twenty-Five Years of the Fordham International Law Journal

A review of the history of the Fordham ILJ. It is a partial reprint of an essay published in 20 FORDHAM INT\u27L L.J. 1 (1996). The essay attempts to briefly summarize the purpose of the ILJ and past volumes

The United Nations: Reflections on Fifty Years, 1945-1995

Introduction in relation to the 50th anniversary of the United Nations

Guantanamo and U.S. Law

This Article deals with the United States\u27 presence at Guantanamo Bay, Cuba, the domestic and international law issues that have arisen, and the nature of the jurisdiction exercised there by the United States. It does not deal with the operation of the prison facility. Guantanamo Bay is near the eastern end of Cuba, 628 miles (1000 km) from the capital, Havana. It is a deep-water harbor, protected by hills from the extremes of Caribbean weather; but it has an unhealthy tropical climate. The forty-five square miles of the Guantanamo Naval Base have been occupied by the United States since the Spanish-American War in 1898. Originally a coaling station, it had been utilized for training, repairs, anti-submarine warfare, and humanitarian rescue before its present uses. Its continued presence is deeply resented in the island State of almost twelve million people, but the persistence of the communist dictatorship of Fidel Castro has strengthened U.S. determination to hold on, even though the base no longer serves a military purpose

Fiscal Year 2007

This annual report documents the locations, magnitudes, and geologic interpretations of earthquakes recorded for the Hanford monitoring region of south-central Washington in fiscal year 2007 (October 2006 through September 2007). The report provides summaries of seismic events recorded during the first three quarters of fiscal year 2007 and contains a more comprehensive discussion of seismic events for the fourth quarter of the fiscal year

Third Quarter Hanford Seismic Report for Fiscal Year 2008

The Hanford Seismic Assessment Program (HSAP) provides an uninterrupted collection of high-quality raw and processed seismic data from the Hanford Seismic Network for the U.S. Department of Energy and its contractors. The Hanford Seismic Assessment Team locates and identifies sources of seismic activity and monitors changes in the historical pattern of seismic activity at the Hanford Site. The data are compiled, archived, and published for use by the Hanford Site for waste management, natural phenomena hazards assessments, and engineering design and construction. In addition, the seismic monitoring organization works with the Hanford Site Emergency Services Organization to provide assistance in the event of a significant earthquake on the Hanford Site. The Hanford Seismic Network and the Eastern Washington Regional Network consist of 44 individual sensor sites and 15 radio relay sites maintained by the Hanford Seismic Assessment Team. For the Hanford Seismic Network, fourteen local earthquakes were recorded during the third quarter of fiscal year 2008. The largest event recorded by the network during the third quarter (May 18, 2008 - magnitude 3.7 Mc) was located approximately 17 km east of Prosser at a depth of 20.5 km. With regard to the depth distribution, five earthquakes occurred at shallow depths (less than 4 km, most likely in the Columbia River basalts), six earthquakes at intermediate depths (between 4 and 9 km, most likely in the pre-basalt sediments), and three earthquakes were located at depths greater than 9 km, within the crystalline basement. Geographically, eight earthquakes occurred in swarm areas and six earthquakes were classified as random events. The largest event recorded by the network during the third quarter occurred on May 18 (magnitude 3.7 Mc) and was located approximately 17 km east of Prosser at a depth of 20.5 km. This earthquake was the highest magnitude event recorded in the 46-47 N. latitude / 119-120 W. longitude sector since 1975. The May 18 event, not reported as being felt on the Hanford site or causing any damage, was communicated to the PNNL Operations Center per HSAP communications procedures. The event is not considered to be significant with regard to site safety and not unprecedented given the site’s seismic history. The Hanford strong motion accelerometer (SMA) stations at the 200 East Area, 300 Area, and the 400 Area were triggered by the May 18 event. The reportable action level of 2% g for Hanford facilities is approximately 12 times larger than the peak acceleration (0.17%) observed at the 300 Area SMA station and no action was required