Titlebook: Long-term Limnological Research and Monitoring at Crater Lake, Oregon; A benchmark study of G. L. Larson,R. Collier,M. W. Buktenica Book 20

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Mark W. Buktenica,Scott F. Girdner,Gary L. Larson,C. David McIntire oberfl?chlich nach ventral, lateral der Mandibula bzw. des M. masseter. Dorso-caudal der Parotis liegen der hintere Bauch des M. digastricus sowie die Stylomuskeln. Weiters reicht ein unterschiedlich gro?er Anteil medial der Mandibula (retromandibul?rer Anteil). In der Drüse verl?uft longitudinal,

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Long-term limnological research and monitoring at Crater Lake, Oregon,n of 1882 m and a maximum depth of 594 m. Limited studies of this ultraoligotrophic lake conducted between 1896 and 1981, lead to a 10-year limnological study to evaluate any potential degradation of water quality. No long-term variations in water quality were observed that could be attributed to an

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Thermal, chemical, and optical properties of Crater Lake, Oregon,m. There is no outlet stream and surface inflow is limited to small streams and springs. Owing to its great volume and heat, the lake is not covered by snow and ice in winter unlike other lakes in the Cascade Range. The lake is isothermal in winter except for a slight increase in temperature in the

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