Deep-sea corehead camera photography and piston coring

Cameras were mounted in a newly designed corehead of a piston corer and used to photograph coring operations during 36 stations on CHAIN cruise 75 and 28 stations on ATLANTIS II cruise 42. Through the analysis of these photographs, the deep-water operation of a piston corer during its descent, tripping, impact with the bottom, and ascent has been studied, providing information on the corer's stability, effectiveness in obtaining a bottom sample, and influence on the nearby sea-floor. Accurate determinations of the amount of penetration were possible, allowing comparisons to be made with the more indirect methods of determining penetration and with the length of core recovered. Sediment clouds produced by bottom currents were noticed in many of the bottom photographs. A number of suggestions are made for future piston coring operations. The corer descends with little rotation and swinging. Free-fall and penetration generally take place in less than 5 seconds, with a rotation of 20-60° and an increase of about 6° in vertical deviation. During penetration, the corer disturbs the surrounding sea floor, producing both mounds and depressions around the core barrels. While resting in the bottom, the corer is very stable although some wobbling does occur. Considerable rotation takes place during both pull-out and ascent; frequent sediment discharges from the piston corer occur. No consistent relationship was found between the amount of penetration and the length of core recovered, and thus with the degree of core shortening. Comparisons between piston and pilot cores indicate that the piston cores have been shortened and disturbed relative to the pilot cores, and that as much as a meter of the upper portion of the piston core has been lost. The position of the mud-mark appears to be a reliable indicator of the amount of penetration; estimates by extrapolation of the thermal gradient to the surface are less reliable. The vertical deviation of the corer in the bottom does not influence the amount of penetration. Stratigraphic dips in the recovered cores correspond poorly to this vertical deviation in the bottom.The National Science Foundation Grants GA-1077 and GA-1209 and submitted to the Office of Naval Research under Contract Nonr-4029(00); NR 260-101, and N00014-66-C0241; NR 083- 004

Book Reviews

Book Reviews: Overthrow: America's Century of Regime Change From Hawaii to Iraq by Stephen Kinzer ; Longitude and Empire: How Captain Cook's Voyages Changed the World by Brian W. Richardson ; Pacific Encounters: Art & Diversity in Polynesia 1760-1860 by Steven Hooper ; All Men Are Brothers: The Life & Times of Francis Williams Damon by Paul Berry ; Broken Trust: Greed, Mismanagement, & Political Manipulation at America's Largest Charitable Trust by Samuel P. King and Randall W. Roth ; Crowning the Nice Girl: Gender, Ethnicity, and Culture in Hawai'i's Cherry Blossom Festival by Christine R. Yano ; Combat Chaplain: The Personal Story of the World War II Chaplain of the Japanese American 100th Battalion by Israel A. S. Yost ; Hawaiian Volcanoes by Clarence Edward Dutton ; Reworking Race: The Making of Hawaii's Interracial Labor Movement by Moon-Kie Jung ; Islands in a Far Sea: The Fate of Nature in Hawai'i by John L. Culliney

Arctic passages: liminality, Iñupiat Eskimo mothers and NW Alaska communities in transition

Background. While the primary goal of the NW Alaska Native maternal transport is safe deliveries for mothers from remote villages, little has been done to question the impact of transport on the mothers and communities involved. This study explores how presence of Iñupiat values influences the desire of indigenous women of differing eras and NW Alaska villages to participate in biomedical birth, largely made available by a tribal health-sponsored transport system. Objective. This paper portrays how important it is (and why) for Alaska Native families and women of different generations from various areas of Iñupiat villages of NW Alaska to get to the hospital to give birth. This research asks: How does a community’s presence of Iñupiat values influence women of different eras and locations to participate in a more biomedical mode of birth? Design. Theoretical frameworks of medical anthropology and maternal identity work are used to track the differences in regard to the maternal transport operation for Iñupiat mothers of the area. Presence of Iñupiat values in each of the communities is compared by birth era and location for each village. Content analysis is conducted to determine common themes in an inductive, recursive fashion. Results. A connection is shown between a community’s manifestation of Iñupiat cultural expression and mothers’ acceptance of maternal transport in this study. For this group of Iñupiat Eskimo mothers, there is interplay between community expression of Iñupiat values and desire and lengths gone to by women of different eras and locations. Conclusions. The more openly manifested the Iñupiat values of the community, the more likely alternative birthing practices sought, lessening the reliance on the existing transport policy. Conversely, the more openly western values are manifested in the village of origin, the less likely alternative measures are sought. For this study group, mothers from study villages with openly manifested western values are more likely to easily acquiesce to policy, and “make the best” of their prenatal travel

The Geology of the Manu'a Islands, Samoa

The Manu'a Islands are a group of three islands-Ta'u, Ofu, and Olosega-that were built by volcanic activity along the crest of the easternmost portion of the Samoan Ridge. Ta'u Island represents the largest volcanic center, where aa and pahoehoe flows of non-porphyritic basalt, olivine basalt, pierite basalt, and feldspar-phyric basalts constructed a volcanic shield more than 3,000 feet above sea level. The present-day total thickness of this volcanic material is over 12,000 feet, as measured from the ocean floor to the summit of Ta'u, Lata Mountain (3,056 feet). Dips of the lava flows frequently exceed 30°, but average 20-25°. Summit collapse formed a caldera that became partially filled with ponded lavas and pyroclastic deposits which accumulated to a thickness of over 1,000 feet. From the summit area, two rift zones radiate to the northeast and northwest, the latter coinciding with the trend of the Samoan Ridge. Two smaller shields are located along these rift zones. Following a period of extensive erosion, the northeast corner of the island was built out by dunite-bearing lava flows, upon which the village of Fitiiuta now stands. A tuff complex containing large dunite xenoliths and coral blocks extended the northwest corner of the island near the village of Faleasao, burying a former sea cliff