By Bruce McCune, James Grace
Research of Ecological groups bargains a motive and tips for choosing acceptable, potent, analytical equipment in neighborhood ecology.
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In Papua New Guinea the glaciated mountains remained isolated ice-covered peaks scattered through the highland areas, along the Owen Stanley Range and the eastern parts of the northern coastal ranges (Fig. 1). The Late Pleistocene glacial snowline was at about 3550-3600 m on most mountains but there were some variations due to local climatic or tectonic conditions. This snowline corresponds to a temperature depression of about 5-6°C in the mountain areas assuming that the lapse rate was similar to the present.
Miner. Resour. Aust. Rec. ). Johnson, T. and P. Molnar. 1972. Focal mechanisms and plate tectonics of the southwest Pacific. J. Geophys. Res. 77, 5000-32. Mackenzie, D. E. 1973. Quaternary volcanoes of the central and Southern Highlands of Papua New Guinea. Bur. Miner. Resour. Aust. Rec. ). Manser, W. 1974. Earth science abstracts, Papua New Guinea, to 1971. Bur. Miner. Resour. Aust. Bull. 143. Mutter, J. C. 1975. A structural analysis of the Gulf of Papua and northwest Coral Sea region. Bur. Miner Resour.
Resour. Aust. explan. Notes SB/54-7. Davies, H. L. and I. E. Smith. 1974. Tufi-Cape Nelson, Papua New Guinea-I :250,000 Geological Series. Bur. Miner. Resour. Aust. explan. Notes SCj55-8, 4. Dow, D. , J. A. J. Smith and R. W. Page. 1974. Wau, Papua New Guinea-l:250,000 Geological Series. Bur. Miner. Resour. Aust. explan. Notes SB/55-14. Pieters, P. E. 1979. Port Moresby-Kalo-Aroa, Papua New Guinea-I:250,000 Geological Series. Bur. Miner. Resour. Aust. explan. Notes SCj55-7, 11,6. Robinson, G. P.