The New Encyclopędia BritannicaEncyclopędia Britannica, 1983 - Encyclopedias and dictionaries |
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Page 32
... varves of the type just described . Under circumstances where varves do form in brackish waters , the varve boundaries tend to be nongradational because of the greater tendency for the particles to flocculate . The proof of the annual ...
... varves of the type just described . Under circumstances where varves do form in brackish waters , the varve boundaries tend to be nongradational because of the greater tendency for the particles to flocculate . The proof of the annual ...
Page 33
varve thickness ( centimetres ) 876543210 543210 240 240 Problems and discrep- ancies Varves in the Todilto Limestone and the Green River shales The Castile anhydrites. New Haven , Connecticut mean 23.24 millimetres 250 260 270 280 290 ...
varve thickness ( centimetres ) 876543210 543210 240 240 Problems and discrep- ancies Varves in the Todilto Limestone and the Green River shales The Castile anhydrites. New Haven , Connecticut mean 23.24 millimetres 250 260 270 280 290 ...
Page 34
Barstow and Searles Lake varves alkaline or saline , and varved deposits are common in the deeper water sediments of those lake stages . The Green River lakes became permanently stratified during the deeper water stages , and during ...
Barstow and Searles Lake varves alkaline or saline , and varved deposits are common in the deeper water sediments of those lake stages . The Green River lakes became permanently stratified during the deeper water stages , and during ...
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