The New Encyclopædia BritannicaEncyclopædia Britannica, 1983 - Encyclopedias and dictionaries |
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Page 32
... sediments are those originating in proglacial lakes , which are formed at the terminus of a stagnant or retreating glacier . Silt and clay are carried by streams from a melting glacier into its associated lake during the spring and ...
... sediments are those originating in proglacial lakes , which are formed at the terminus of a stagnant or retreating glacier . Silt and clay are carried by streams from a melting glacier into its associated lake during the spring and ...
Page 34
... sediments of those lake stages . The Green River lakes became permanently stratified during the deeper water stages , and during those stages varved laminae of microgranular carbonates and struc- tureless organic matter formed on the ...
... sediments of those lake stages . The Green River lakes became permanently stratified during the deeper water stages , and during those stages varved laminae of microgranular carbonates and struc- tureless organic matter formed on the ...
Page 36
... Sediments and Their Importance for the Study of Sedimentary Rocks , " Soc . Nat . Moscow Bull . , Sec . Ge- ology , N.S. , 35 : 264-289 ( 1927 ) ; s.E. CALVERT , " Factors Af- fecting Distribution of Laminated Diatomaceous Sediments in ...
... Sediments and Their Importance for the Study of Sedimentary Rocks , " Soc . Nat . Moscow Bull . , Sec . Ge- ology , N.S. , 35 : 264-289 ( 1927 ) ; s.E. CALVERT , " Factors Af- fecting Distribution of Laminated Diatomaceous Sediments in ...
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