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Mississippi River

4 paragraphs · about 2 minutes

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

59:3.9280,000,000 years ago the con­ti­nents had largely emerged from the sec­ond Sil­urian in­un­da­tion. The rock de­posits of this sub­mer­gence are known in North Amer­ica as Ni­a­gara lime­stone be­cause this is the stra­tum of rock over which Ni­a­gara Falls now flows. This layer of rock ex­tends from the east­ern moun­tains to the Mis­sis­sippi val­ley re­gion but not far­ther west ex­cept to the south. Sev­eral lay­ers ex­tend over Canada, por­tions of South Amer­ica, Aus­tralia, and most of Eu­rope, the av­er­age thick­ness of this Ni­a­gara se­ries be­ing about six hun­dred feet. Im­me­di­ately over­ly­ing the Ni­a­gara de­posit, in many re­gions may be found a col­lec­tion of con­glom­er­ate, shale, and rock salt. This is the ac­cu­mu­la­tion of sec­ondary sub­si­dences. This salt set­tled in great la­goons which were al­ter­nately opened up to the sea and then cut off so that evap­o­ra­tion oc­curred with de­po­si­tion of salt along with other mat­ter held in so­lu­tion. In some re­gions these rock salt beds are sev­enty feet thick.

59:5.20180,000,000 years ago brought the close of the Car­bonif­er­ous pe­riod, dur­ing which coal had been formed all over the world—in Eu­rope, In­dia, China, North Africa, and the Amer­i­cas. At the close of the coal-for­ma­tion pe­riod North Amer­ica east of the Mis­sis­sippi val­ley rose, and most of this sec­tion has ever since re­mained above the sea. This land-el­e­va­tion pe­riod marks the be­gin­ning of the mod­ern moun­tains of North Amer­ica, both in the Ap­palachian re­gions and in the west. Vol­ca­noes were ac­tive in Alaska and Cal­i­for­nia and in the moun­tain-form­ing re­gions of Eu­rope and Asia. East­ern Amer­ica and west­ern Eu­rope were con­nected by the con­ti­nent of Green­land.

61:7.2750,000 years ago the fourth ice sheet, a union of the North Amer­i­can cen­tral and east­ern ice fields, was well on its way south; at its height it reached to south­ern Illi­nois, dis­plac­ing the Mis­sis­sippi River fifty miles to the west, and in the east it ex­tended as far south as the Ohio River and cen­tral Penn­syl­va­nia.

61:7.3–9 · seven paragraphs not cited here ·

61:7.3In Asia the Siberian ice sheet made its south­ern­most in­va­sion, while in Eu­rope the ad­vanc­ing ice stopped just short of the moun­tain bar­rier of the Alps.

61:7.4500,000 years ago, dur­ing the fifth ad­vance of the ice, a new de­vel­op­ment ac­cel­er­ated the course of hu­man evo­lu­tion. Sud­denly and in one gen­er­a­tion the six col­ored races mu­tated from the abo­rig­i­nal hu­man stock. This is a dou­bly im­por­tant date since it also marks the ar­rival of the Plan­e­tary Prince.

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.

61:7.6250,000 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.

Onward

Cited alongside: Niagara Falls, ice ages