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St. Lawrence River

3 paragraphs · about 1 minute

Every paragraph the index cites under St. Lawrence River, once, in the order of the book. Beside each stand the entries that cite it.

59:4.16230,000,000 years ago the seas were con­tin­u­ing their re­treat. Much of North Amer­ica was above wa­ter, and great vol­canic ac­tiv­ity oc­curred in the St. Lawrence re­gion. Mount Royal, at Mon­treal, is the eroded neck of one of these vol­ca­noes. The de­posits of this en­tire epoch are well shown in the Ap­palachian Moun­tains of North Amer­ica where the Susque­hanna River has cut a val­ley ex­pos­ing these suc­ces­sive lay­ers, which at­tained a thick­ness of over 13,000 feet.

61:7.5In North Amer­ica the ad­vanc­ing fifth glacier con­sisted of a com­bined in­va­sion by all three ice cen­ters. The east­ern lobe, how­ever, ex­tended only a short dis­tance be­low the St. Lawrence val­ley, and the west­ern ice sheet made lit­tle south­ern ad­vance. But the cen­tral lobe reached south to cover most of the state of Iowa. In Eu­rope this in­va­sion of the ice was not so ex­ten­sive as the pre­ced­ing one.

61:7.6–9 · four paragraphs not cited here ·

61:7.6250,000 years ago the sixth and last glacia­tion be­gan. And de­spite the fact that the north­ern high­lands had be­gun to sink slightly, this was the pe­riod of great­est snow de­po­si­tion on the north­ern ice fields.

61:7.7In this in­va­sion the three great ice sheets co­a­lesced into one vast ice mass, and all of the west­ern moun­tains par­tic­i­pated in this glacial ac­tiv­ity. This was the largest of all ice in­va­sions in North Amer­ica; the ice moved south over fif­teen hun­dred miles from its pres­sure cen­ters, and North Amer­ica ex­pe­ri­enced its low­est tem­per­a­tures.

61:7.8200,000 years ago, dur­ing the ad­vance of the last glacier, there oc­curred an episode which had much to do with the march of events on Uran­tia—the Lu­cifer re­bel­lion.

61:7.9150,000 years ago the sixth and last glacier reached its far­thest points of south­ern ex­ten­sion, the west­ern ice sheet cross­ing just over the Cana­dian bor­der; the cen­tral com­ing down into Kansas, Mis­souri, and Illi­nois; the east­ern sheet ad­vanc­ing south and cov­er­ing the greater por­tion of Penn­syl­va­nia and Ohio.

61:7.10This is the glacier that sent forth the many tongues, or ice lobes, which carved out the pres­ent-day lakes, great and small. Dur­ing its re­treat the North Amer­i­can sys­tem of Great Lakes was pro­duced. And Uran­tian ge­ol­o­gists have very ac­cu­rately de­duced the var­i­ous stages of this de­vel­op­ment and have cor­rectly sur­mised that these bod­ies of wa­ter did, at dif­fer­ent times, empty first into the Mis­sis­sippi val­ley, then east­ward into the Hud­son val­ley, and fi­nally by a north­ern route into the St. Lawrence. It is thirty-seven thou­sand years since the con­nected Great Lakes sys­tem be­gan to empty out over the pres­ent Ni­a­gara route.