Alien Rainbow Trout Oncorhynchus mykiss in the Balkhash Basin (Kazakhstan, Central Asia): 50 Years of Naturalization. [PDF]
Mamilov NS +11 more
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Description of a new species of <i>Pseudobornella</i> Baba, 1932 (Gastropoda, Nudibranchia, Dendronotidae) from the Yellow Sea. [PDF]
Zhang S, Wang J.
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A possible volcanic origin for the Greenland ice core Pt anomaly near the Bølling-Allerød/Younger Dryas boundary. [PDF]
Green CE +5 more
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Using the EMFIT Sensor in Geophysical Monitoring. [PDF]
Toader VE +3 more
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Stilipedidae Holmes, 1908 (Crustacea, Amphipoda) of the Clarion-Clipperton Zone. [PDF]
Tandberg AHS, Hughes LE.
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Isolation of viruses, including mollivirus, with the potential to infect Acanthamoeba from a Japanese warm temperate zone. [PDF]
Morimoto D +3 more
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Related searches:
The peninsula of Kamchatka in Siberia is situated between the Sea of Okhotsk on the west and Bering Sea and the Pacific Ocean on on the east. This peninsula is about 750 miles long and 80 to 300 miles wide with a mountainous and volcanic interior and a somewhat severe climate.
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Radiogeochemistry of Kamchatka soils
Eurasian Soil Science, 2016Background concentrations of Th and U in volcanic soils (Andosols) of Kamchatka are much lower than their clarkes in continental soils. The dose rate of gamma radiation above the soil surface (10–11.5 µR/h in the south and 8–9.5 [m]R/h in the north of Kamchatka Peninsula) is lower than the natural level of this index for the mountainous areas in the ...
L. V. Zakharikhina, Yu. S. Litvinenko
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The submarine canyons of Kamchatka
Marine Geology, 1984Abstract A system of large submarine canyons on the continental slope off the Kamchatka Peninsula has been studied. These are the Kamachatsky, Storozh, Tyushevsky, Olga, Kronotsky, Zhupanovsky and Avachinsky canyons and they are generally controlled by fault zones and cut the Pre-Miocene basement structural elements in the cross-strike direction ...
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Magnetotelluric sounding of Kamchatka
Journal of Volcanology and Seismology, 2008The MTS data acquired in Kamchatka during the last 30 years have been analyzed and summarized. Our interpretation is based on curves oriented along and across Kamchatka. Longitudinal and transverse curves can be affected by local geoelectric inhomogeneities. These were suppressed by conformal averaging.
Yu. F. Moroz, N. A. Laguta, T. A. Moroz
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