منابع مشابه
Rattus exulans in Western Samoa
THE COMMON RAT of Polynesia is Rattus exulans (Peale). It appears to be closely related to, and ptobably derived from Rattus concolor of the Malay region. The concolor group, and its derivatives, occur all over the Pacific, being represented in the Oceanic islands by R. exulans, R. micronesiensis and R. hawaiiensis. Other species have been erected for the Polynesian forms, but it may be simpler...
متن کاملA qualitative study on family meals in Western Samoa with special reference to child nutrition.
Early in 1951 a survey of eating habits was made in Western Samoa by the South Pacific Health Service. The purpose of the study was to observe the factors that influence the nutrition of the young Samoan child. In spite of a rapidly increasing population, the existing indigenous food supplies provide for the adequate nutrition of the people living in most areas. There are a few small islands wh...
متن کاملGEOLOGICAL NOTES Quaternary Glacial-Interglacial Climate Cycles in Hawaii
The upper kilometer of the Hawaiian Scientific Drilling Program core consists of lavas that were emplaced subaerially, burying paleosols. These paleosols were preserved with minimal alteration and are used to construct a ∼330-kyr Quaternary climate record. Within the temporal resolution of this record, there appears to be a ∼100-kyr climate oscillation between cool-dry and warm-wet conditions, ...
متن کاملGeological Notes Diffusion of Water in Silicate Melts
The transport of water in silicate melts is examined from a theoretical point of view, taking into account the presence of both H20 and OH species. It was assumed that only H20 molecules may diffuse and that a constitutive relationship between the number density nH 0 of H20 molecules and the total water content (n:E) exists such that nH,o = g(n:E) . This is related to dissociation or to chemica...
متن کاملNotes on the Cainozoic History of Western Tasmania- " Malanna" Glaciation
The Cainozoic history of the Malanna area included faulting, deposition of sediments by streams or in lakes and swamps, two epochs of planation, and stream erosion. There is no physiographic, depositional or structural evidence for gladation in this area, the type area of Lewis's Malanna Phase of the Pleistocene glaciation. This phase must be considered invalid on the eviaence available in the ...
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ژورنال
عنوان ژورنال: New Zealand Journal of Geology and Geophysics
سال: 1967
ISSN: 0028-8306,1175-8791
DOI: 10.1080/00288306.1967.10423228