美国华盛顿州港口系统的开发及其对我国的启示

本文在分析70年代以来美国华盛顿州港口系统开发的特征、措施及其效果基础上，总结出华盛顿州港口系统抓住亚太地区经济腾飞的良机，统一规划沿海各港口群区的地位、功能和作用，大力发展集装箱多式联运等经验，均可作为发展我国沿海港口系统的借鉴。     

Spawning sockeye salmon fossils in Pleistocene lake beds of Skokomish Valley, Washington

An assemblage of fossil sockeye salmon was discovered in Pleistocene lake sediments along the South Fork Skokomish River, Olympic Peninsula, Washington. The fossils were abundant near the head of a former glacial lake at 115 m elevation. Large adult salmon are concentrated in a sequence of death assemblages that include individuals with enlarged breeding teeth and worn caudal fins indicating migration, nest digging, and spawning prior to death. The specimens were 4 yr old and 45-70 cm in total length, similar in size to modern sockeye salmon, not landlocked kokanee. The fossils possess most of the characteristics of sockeye salmon, Oncorhynchus nerka, but with several minor traits suggestive of pink salmon, O. gorbuscha. This suggests the degree of divergence of these species at about 1 million yr ago, when geological evidence indicates the salmon were deposited at the head of a proglacial lake impounded by the Salmon Springs advance of the Puget lobe ice sheet. Surficial geology and topography record a complicated history of glacial damming and river diversion that implies incision of the modern gorge of the South Fork Skokomish River after deposition of the fossil-bearing sediments.     

Source Investigation and Comparison of the 1939, 1946, 1949 and 1965 Earthquakes,Cascadia Subduction Zone,Western Washington

Over the past ~65 years intraslab earthquakes have caused the most significant damage in the western Washington region. This study examines regional and teleseismic seismograms for four historic, suspected intraslab events of M > 5.5 occurring within the Cascadia Subduction zone in 1939 (South Seattle), 1946 (Puget Sound), 1949 (Olympia) and 1965 (Sea-Tac) to better determine the source locations, mechanisms and rupture histories of these events. Our study is aided by digital seismograms of post-1990 intraslab events with well-determined focal depths and focal mechanisms that were recorded in the same locations as the historic events. Thus the recent events were used as empirical Greens functions to study the historic events. Our results suggest that the 1946 earthquake is not an intraslab event, that the 1939 event closely resembles the 1965 event, and that the 1949 event is similar to the 2001 Nisqually earthquake, although the 1949 event appears to have ruptured toward the south, causing significantly more damage than the Nisqually event. These results suggest that earthquakes periodically rupture along the same or similarly oriented faults within the subducting slab.     

IDENTITY AND ASSIMILATION AMONG YOUNG ETHIOPIAN IMMIGRANTS IN METROPOLITAN WASHINGTON*

ABSTRACT. Ethiopians are a recent immigrant group in the United States, having entered the country in significant numbers during the 1980s and 1990s. This preliminary study examines the ethnic and racial identities of children of first‐generation Ethiopian immigrants living in the Washington, D.C. metropolitan area. The results of twenty in‐depth interviews demonstrate that race is a much more fluid and contested form of identification than is ethnicity to the young immigrants, who equate the latter unilaterally with their Ethiopian heritage. Immigrants also adopt different subject identities in various locales, favoring those that are most in accordance with their needs and sense of self.     

Seismic tomography constrained by bouguer gravity anomalies: Applications in western Washington

Tomographic inversions for velocity variations in western Washington indicate a high correlation with surface geology and geophysical measurements, including gravity observations. By assuming a simple linear relationship between density and velocity (Birch's law) it is possible to calculate the gravity field predicted from the velocity perturbations obtained by local tomographic inversion. While the predicted gravity matches observations in parts of the model, the overall correlation is not satisfactory. In this paper we suggest a method of constraining the tomographic inversion to fit the gravity observations simultaneously with the seismic travel time data. The method is shown to work well with synthetic data in 3 dimensions where the assumption of Birch's law holds strictly. If the sources of the gravity anomalies are assumed to be spatially localized, integration can be carried out over a relatively small volume below the observation points and sparse matrix techniques can be applied. We have applied the constrained inversion method to western Washington using 4,387 shallow earthquakes, to depths of 40.0 km, (36,865 raypaths) convering a 150×250 km region and found that the gravitational constraints may be satisfied with minor effect on the degree of misfit to the seismic data.     

The Afternoon Creek rockslide near Newhalem, Washington

A series of mass wasting events occurred above a Washington, USA, highway in the Cascade Mountains in November and December 2003. The largest event was a rockslide involving approximately 750,000 m³ that occurred on November 9, 2003. The source zone for this event was located at the crest of a ridge. Most of the debris fell to the east of the sharp ridge and was deposited in the relatively shallow sloping Afternoon Creek without causing damage to the highway. Lesser amounts of debris fell to the west of the ridge, sliding 600 m down the steeper Falls Creek and impacting the road. There is an evidence of one or more historical rock avalanches at this location. Displacement of reference points, ground vibration, crack extension, and tilting are being monitored due to concerns that future slope failures or remobilization of debris might again damage or block the highway.     

Gulf of Mexico dissolved hydrocarbons associated with the Ixtoc I mousse

Increased levels of dissolved hydrocarbons were observed in the western Gulf of Mexico during the late summer of 1979. This period was associated with heightened levels of surface tar and oil/water emulsion (mousse) directly resulting from the blowout of the Ixtoc I oil well in the Bay of Campeche on 3 June 1979. The observed concentrations of total dissolved hydrocarbons (up to 656.9 ng l^?1, n-alkanes) were one to two orders of magnitude above levels observed at control stations (5.2 ng l^?1, n-alkanes) and stations in the same area during the earlier Bureau of Land Management (BLM) baseline study. The highest concentrations observed were approximately of the same level as those obtained in an artificial spill/weathering experiment.