Environment, agriculture, and settlement patterns in a marginal Polynesian landscape.

Beginning ca. A.D. 1400, Polynesian farmers established permanent settlements along the arid southern flank of Haleakala Volcano, Maui, Hawaiian Islands; peak population density (43-57 persons per km(2)) was achieved by A.D. 1700-1800, and it was followed by the devastating effects of European contact. This settlement, based on dryland agriculture with sweet potato as a main crop, is represented by >3,000 archaeological features investigated to date. Geological and environmental factors are the most important influence on Polynesian farming and settlement practices in an agriculturally marginal landscape. Interactions between lava flows, whose ages range from 3,000 to 226,000 years, and differences in rainfall create an environmental mosaic that constrained precontact Polynesian farming practices to a zone defined by aridity at low elevation and depleted soil nutrients at high elevation. Within this productive zone, however, large-scale agriculture was concentrated on older, tephra-blanketed lava flows; younger flows were reserved for residential sites, small ritual gardens, and agricultural temples.

Advising nursing students in a tightened job market.

Although new graduates face a more restricted job market, we continue to need new registered nurses to replenish and renew the profession. As employment settings shift from hospital to community settings and optimal and cost-efficient skill mixes are determined, faculty will need to work closely with students, administrators, and nurse recruiters to assist new graduates to face the challenges evolving in today's practice environments.

Heat flow and hydrothermal circulation in the cascade range, north-central Oregon.

In north-central Oregon a large area of near-zero near-surface conductive heat flow occurs in young volcanic rocks of the Cascade Range. Recent advective heat flux measurements and a heat-budget analysis suggest that ground-water circulation sweeps sufficient heat out of areas where rocks younger than 6 Ma (million years ago) are exposed to account for the anomalously high advective and conductive heat discharge measured in older rocks at lower elevations. Earlier workers have proposed that an extensive midcrustal magmatic heat source is responsible for this anomalously high heat flow. Instead, high heat flow in the older rocks may be a relatively shallow phenomenon caused by regional ground-water flow. Any deeper anomaly may be relatively narrow, spatially variable, and essentially confined to the Quaternary (less than 2 Ma) arc. Magmatic intrusion at a rate of 9 to 33 cubic kilometers per kilometer of arc length per million years can account for the total heat flow anomaly. Deep drilling in the areas of high heat flow in the older rocks could indicate which model is more appropriate for the near-surface heat flow data.

Social skills and the stress-protective role of social support.

Cross-sectional analyses of data collected from a large sample of incoming college freshmen were used to determine whether the perceived availability of social support protects persons from stress-induced depressive affect; whether social competence, social anxiety, and self-disclosure are responsible for the stress-protective effect of perceived social support; and whether these social skill measures discriminate among persons for whom support will help, hinder, or be ineffective in the face of stress. Prospective analyses based on the original testing (beginning of school year) and 11- and 22-week follow-ups of a randomly selected subsample were used to determine how the same social skill factors influence the development and maintenance of support perceptions and of friendships. Evidence is provided for a stress-buffering role of the perceived availability of social support. The stress-buffering effect is unaffected by controls for the possible stress-protective influences of social anxiety, social competence, and self-disclosure. Although these social skill factors do not discriminate among persons for whom support will help, hinder, or be ineffective, they are prospectively predictive of the development of both social support and friendship formation. These prospective relations between social skills and the development of perceived availability of social support are only partly mediated by number of friends.