Science: v.1-v.219Moses King, 1965 |
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Page 1108
... present altitudes of former shorelines . 4 ) The late Cenozoic marine beds of western Alaska are interpreted by Hopkins ( 1 , 4 ) as having been de- posited during preglacial and inter- glacial intervals when sea level was approximately ...
... present altitudes of former shorelines . 4 ) The late Cenozoic marine beds of western Alaska are interpreted by Hopkins ( 1 , 4 ) as having been de- posited during preglacial and inter- glacial intervals when sea level was approximately ...
Page 1113
... present position , but the middle part of the Kresta Suite , exposed in many places on the shores of Kresta Bay and Anadyr Gulf , Chukotka , accumulated during a glacial interval when sea level must have been 100 meters lower than at ...
... present position , but the middle part of the Kresta Suite , exposed in many places on the shores of Kresta Bay and Anadyr Gulf , Chukotka , accumulated during a glacial interval when sea level must have been 100 meters lower than at ...
Page 1264
... present in sea water and in the absence of free oxygen the ferrous ion and ammonium salts would also be ex- pected to be present ( 22 ) . The mix- ture of oxidized and reduced salts is somewhat puzzling , though it may be an equilibrium ...
... present in sea water and in the absence of free oxygen the ferrous ion and ammonium salts would also be ex- pected to be present ( 22 ) . The mix- ture of oxidized and reduced salts is somewhat puzzling , though it may be an equilibrium ...
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