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Alps

7 paragraphs · about 2 minutes

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

60:1.4Over Eu­rope, es­pe­cially Ger­many and Rus­sia, may be found de­posits of this pe­riod. In Eng­land the New Red Sand­stone be­longs to this epoch. Lime­stone was laid down in the south­ern Alps as the re­sult of a sea in­va­sion and may now be seen as the pe­cu­liar dolomite lime­stone walls, peaks, and pil­lars of those re­gions. This layer is to be found all over Africa and Aus­tralia. The Car­rara mar­ble comes from such mod­i­fied lime­stone. Noth­ing of this pe­riod will be found in the south­ern re­gions of South Amer­ica as that part of the con­ti­nent re­mained down and hence pre­sents only a wa­ter or ma­rine de­posit con­tin­u­ous with the pre­ced­ing and suc­ceed­ing epochs.

60:3.6Great vol­canic ac­tions oc­curred south of the Alps and along the line of the pres­ent Cal­i­for­nia coast-range moun­tains. The great­est crustal de­for­ma­tions in mil­lions upon mil­lions of years took place in Mex­ico. Great changes also oc­curred in Eu­rope, Rus­sia, Japan, and south­ern South Amer­ica. The cli­mate be­came in­creas­ingly di­ver­si­fied.

61:1.12Dur­ing the lat­ter part of this epoch most of Eu­rope was sub­merged. Fol­low­ing a slight land rise the con­ti­nent was cov­ered by lakes and bays. The Arc­tic Ocean, through the Ural de­pres­sion, ran south to con­nect with the Med­i­ter­ra­nean Sea as it was then ex­panded north­ward, the high­lands of the Alps, Carpathi­ans, Apen­nines, and Pyre­nees be­ing up above the wa­ter as is­lands of the sea. The Isth­mus of Panama was up; the At­lantic and Pa­cific Oceans were sep­a­rated. North Amer­ica was con­nected with Asia by the Bering Strait land bridge and with Eu­rope by way of Green­land and Ice­land. The earth cir­cuit of land in north­ern lat­i­tudes was bro­ken only by the Ural Straits, which con­nected the arc­tic seas with the en­larged Med­i­ter­ra­nean.

61:1.13Con­sid­er­able foraminiferal lime­stone was de­posited in Eu­ro­pean wa­ters. To­day this same stone is el­e­vated to a height of 10,000 feet in the Alps, 16,000 feet in the Hi­malayas, and 20,000 feet in Ti­bet. The chalk de­posits of this pe­riod are found along the coasts of Africa and Aus­tralia, on the west coast of South Amer­ica, and about the West In­dies.

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.

61:7.4–15 · twelve paragraphs not cited here ·

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.

61:7.11100,000 years ago, dur­ing the re­treat of the last glacier, the vast po­lar ice sheets be­gan to form, and the cen­ter of ice ac­cu­mu­la­tion moved con­sid­er­ably north­ward. And as long as the po­lar re­gions con­tinue to be cov­ered with ice, it is hardly pos­si­ble for an­other glacial age to oc­cur, re­gard­less of fu­ture land el­e­va­tions or mod­i­fi­ca­tion of ocean cur­rents.

61:7.12This last glacier was one hun­dred thou­sand years ad­vanc­ing, and it re­quired a like span of time to com­plete its north­ern re­treat. The tem­per­ate re­gions have been free from the ice for a lit­tle over fifty thou­sand years.

61:7.13The rig­or­ous glacial pe­riod de­stroyed many species and rad­i­cally changed nu­mer­ous oth­ers. Many were sorely sifted by the to-and-fro mi­gra­tion which was made nec­es­sary by the ad­vanc­ing and re­treat­ing ice. Those an­i­mals which fol­lowed the glaciers back and forth over the land were the bear, bi­son, rein­deer, musk ox, mam­moth, and mastodon.

61:7.14The mam­moth sought the open prairies, but the mastodon pre­ferred the shel­tered fringes of the for­est re­gions. The mam­moth, un­til a late date, ranged from Mex­ico to Canada; the Siberian va­ri­ety be­came wool cov­ered. The mastodon per­sisted in North Amer­ica un­til ex­ter­mi­nated by the red man much as the white man later killed off the bi­son.

61:7.15In North Amer­ica, dur­ing the last glacia­tion, the horse, tapir, llama, and saber-toothed tiger be­came ex­tinct. In their places sloths, ar­madil­los, and wa­ter hogs came up from South Amer­ica.

61:7.16The en­forced mi­gra­tion of life be­fore the ad­vanc­ing ice led to an ex­traor­di­nary com­min­gling of plants and of an­i­mals, and with the re­treat of the fi­nal ice in­va­sion, many arc­tic species of both plants and an­i­mals were left stranded high upon cer­tain moun­tain peaks, whither they had jour­neyed to es­cape de­struc­tion by the glacier. And so, to­day, these dis­lo­cated plants and an­i­mals may be found high up on the Alps of Eu­rope and even on the Ap­palachian Moun­tains of North Amer­ica.

64:2.3They were fol­lowed in Eu­rope by a some­what su­pe­rior and pro­lific peo­ple, whose de­scen­dants soon spread over the en­tire con­ti­nent from the ice in the north to the Alps and Med­i­ter­ra­nean in the south. These tribes are the so-called Hei­del­berg race.

Onward

Cited alongside: Europe, Asia, South America, Australia, limestone, Russia, volcanoes, Africa