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ice ages

46 paragraphs · about 13 minutes

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

59:1.17360,000,000 years ago the land was still ris­ing. North and South Amer­ica were well up. West­ern Eu­rope and the British Isles were emerg­ing, ex­cept parts of Wales, which were deeply sub­merged. There were no great ice sheets dur­ing these ages. The sup­posed glacial de­posits ap­pear­ing in con­nec­tion with these strata in Eu­rope, Africa, China, and Aus­tralia are due to iso­lated moun­tain glaciers or to the dis­place­ment of glacial de­bris of later ori­gin. The world cli­mate was oceanic, not con­ti­nen­tal. The south­ern seas were warmer then than now, and they ex­tended north­ward over North Amer­ica up to the po­lar re­gions. The Gulf Stream coursed over the cen­tral por­tion of North Amer­ica, be­ing de­flected east­ward to bathe and warm the shores of Green­land, mak­ing that now ice-man­tled con­ti­nent a ver­i­ta­ble tropic par­a­dise.

61:5.1By the close of the pre­ced­ing pe­riod the lands of the north­east­ern part of North Amer­ica and of north­ern Eu­rope were highly el­e­vated on an ex­ten­sive scale, in North Amer­ica vast ar­eas ris­ing up to 30,000 feet and more. Mild cli­mates had for­merly pre­vailed over these north­ern re­gions, and the arc­tic wa­ters were all open to evap­o­ra­tion, and they con­tin­ued to be ice-free un­til al­most the close of the glacial pe­riod.

61:5.2Si­mul­ta­ne­ously with these land el­e­va­tions the ocean cur­rents shifted, and the sea­sonal winds changed their di­rec­tion. These con­di­tions even­tu­ally pro­duced an al­most con­stant pre­cip­i­ta­tion of mois­ture from the move­ment of the heav­ily sat­u­rated at­mo­sphere over the north­ern high­lands. Snow be­gan to fall on these el­e­vated and there­fore cool re­gions, and it con­tin­ued to fall un­til it had at­tained a depth of 20,000 feet. The ar­eas of the great­est depth of snow, to­gether with al­ti­tude, de­ter­mined the cen­tral points of sub­se­quent glacial pres­sure flows. And the ice age per­sisted just as long as this ex­ces­sive pre­cip­i­ta­tion con­tin­ued to cover these north­ern high­lands with this enor­mous man­tle of snow, which soon meta­mor­phosed into solid but creep­ing ice.

61:5.3The great ice sheets of this pe­riod were all lo­cated on el­e­vated high­lands, not in moun­tain­ous re­gions where they are found to­day. One half of the glacial ice was in North Amer­ica, one fourth in Eura­sia, and one fourth else­where, chiefly in Antarc­tica. Africa was lit­tle af­fected by the ice, but Aus­tralia was al­most cov­ered with the antarc­tic ice blan­ket.

61:5.4The north­ern re­gions of this world have ex­pe­ri­enced six sep­a­rate and dis­tinct ice in­va­sions, al­though there were scores of ad­vances and re­ces­sions as­so­ci­ated with the ac­tiv­ity of each in­di­vid­ual ice sheet. The ice in North Amer­ica col­lected in two and, later, three cen­ters. Green­land was cov­ered, and Ice­land was com­pletely buried be­neath the ice flow. In Eu­rope the ice at var­i­ous times cov­ered the British Isles ex­cept­ing the coast of south­ern Eng­land, and it over­spread west­ern Eu­rope down to France.

61:5.52,000,000 years ago the first North Amer­i­can glacier started its south­ern ad­vance. The ice age was now in the mak­ing, and this glacier con­sumed nearly one mil­lion years in its ad­vance from, and re­treat back to­ward, the north­ern pres­sure cen­ters. The cen­tral ice sheet ex­tended south as far as Kansas; the east­ern and west­ern ice cen­ters were not then so ex­ten­sive.

61:5.61,500,000 years ago the first great glacier was re­treat­ing north­ward. In the mean­time, enor­mous quan­ti­ties of snow had been falling on Green­land and on the north­east­ern part of North Amer­ica, and ere­long this east­ern ice mass be­gan to flow south­ward. This was the sec­ond in­va­sion of the ice.

61:5.7These first two ice in­va­sions were not ex­ten­sive in Eura­sia. Dur­ing these early epochs of the ice age North Amer­ica was over­run with mastodons, woolly mam­moths, horses, camels, deer, musk oxen, bi­son, ground sloths, gi­ant beavers, saber-toothed tigers, sloths as large as ele­phants, and many groups of the cat and dog fam­i­lies. But from this time for­ward they were rapidly re­duced in num­bers by the in­creas­ing cold of the glacial pe­riod. To­ward the close of the ice age the ma­jor­ity of these an­i­mal species were ex­tinct in North Amer­ica.

61:5.8Away from the ice the land and wa­ter life of the world was lit­tle changed. Be­tween the ice in­va­sions the cli­mate was about as mild as at pres­ent, per­haps a lit­tle warmer. The glaciers were, af­ter all, lo­cal phe­nom­ena, though they spread out to cover enor­mous ar­eas. The coast­wise cli­mate var­ied greatly be­tween the times of glacial in­ac­tion and those times when enor­mous ice­bergs were slid­ing off the coast of Maine into the At­lantic, slip­ping out through Puget Sound into the Pa­cific, and thun­der­ing down Nor­we­gian fiords into the North Sea.

61:6.1The great event of this glacial pe­riod was the evo­lu­tion of prim­i­tive man. Slightly to the west of In­dia, on land now un­der wa­ter and among the off­spring of Asi­atic mi­grants of the older North Amer­i­can lemur types, the dawn mam­mals sud­denly ap­peared. These small an­i­mals walked mostly on their hind legs, and they pos­sessed large brains in pro­por­tion to their size and in com­par­i­son with the brains of other an­i­mals. In the sev­en­ti­eth gen­er­a­tion of this or­der of life a new and higher group of an­i­mals sud­denly dif­fer­en­ti­ated. These new mid-mam­mals—al­most twice the size and height of their an­ces­tors and pos­sess­ing pro­por­tion­ately in­creased brain power—had only well es­tab­lished them­selves when the Pri­mates, the third vi­tal mu­ta­tion, sud­denly ap­peared. (At this same time, a ret­ro­grade de­vel­op­ment within the mid-mam­mal stock gave ori­gin to the simian an­ces­try; and from that day to this the hu­man branch has gone for­ward by pro­gres­sive evo­lu­tion, while the simian tribes have re­mained sta­tion­ary or have ac­tu­ally ret­ro­gressed.)

61:6.21,000,000 years ago Uran­tia was reg­is­tered as an in­hab­ited world. A mu­ta­tion within the stock of the pro­gress­ing Pri­mates sud­denly pro­duced two prim­i­tive hu­man be­ings, the ac­tual an­ces­tors of man­kind.

61:6.3This event oc­curred at about the time of the be­gin­ning of the third glacial ad­vance; thus it may be seen that your early an­ces­tors were born and bred in a stim­u­lat­ing, in­vig­o­rat­ing, and dif­fi­cult en­vi­ron­ment. And the sole sur­vivors of these Uran­tia abo­rig­ines, the Es­ki­mos, even now pre­fer to dwell in frigid north­ern climes.

61:6.4Hu­man be­ings were not pres­ent in the West­ern Hemi­sphere un­til near the close of the ice age. But dur­ing the in­ter­glacial epochs they passed west­ward around the Med­i­ter­ra­nean and soon over­ran the con­ti­nent of Eu­rope. In the caves of west­ern Eu­rope may be found hu­man bones min­gled with the re­mains of both tropic and arc­tic an­i­mals, tes­ti­fy­ing that man lived in these re­gions through­out the later epochs of the ad­vanc­ing and re­treat­ing glaciers.

61:7.1Through­out the glacial pe­riod other ac­tiv­i­ties were in prog­ress, but the ac­tion of the ice over­shad­ows all other phe­nom­ena in the north­ern lat­i­tudes. No other ter­res­trial ac­tiv­ity leaves such char­ac­ter­is­tic ev­i­dence on the to­pog­ra­phy. The dis­tinc­tive boul­ders and sur­face cleav­ages, such as pot­holes, lakes, dis­placed stone, and rock flour, are to be found in con­nec­tion with no other phe­nom­e­non in na­ture. The ice is also re­spon­si­ble for those gen­tle swells, or sur­face un­du­la­tions, known as drum­lins. And a glacier, as it ad­vances, dis­places rivers and changes the whole face of the earth. Glaciers alone leave be­hind them those tell­tale drifts—the ground, lat­eral, and ter­mi­nal moraines. These drifts, par­tic­u­larly the ground moraines, ex­tend from the east­ern seaboard north and west­ward in North Amer­ica and are found in Eu­rope and Siberia.

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.

61:7.3In 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.

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.

61:7.17The ice age is the last com­pleted ge­o­logic pe­riod, the so-called Pleis­tocene, over two mil­lion years in length.

61:7.1835,000 years ago marks the ter­mi­na­tion of the great ice age ex­cept­ing in the po­lar re­gions of the planet. This date is also sig­nif­i­cant in that it ap­prox­i­mates the ar­rival of a Ma­te­rial Son and Daugh­ter and the be­gin­ning of the Adamic dis­pen­sa­tion, roughly cor­re­spond­ing to the be­gin­ning of the Holocene or post­glacial pe­riod.

61:7.19This nar­ra­tive, ex­tend­ing from the rise of mam­malian life to the re­treat of the ice and on down to his­toric times, cov­ers a span of al­most fifty mil­lion years. This is the last—the cur­rent—ge­o­logic pe­riod and is known to your re­searchers as the Ceno­zoic or re­cent-times era.

61:7.20[Spon­sored by a Res­i­dent Life Car­rier.]

64:1.4These events oc­curred dur­ing the times of the third glacier, the first ac­cord­ing to the reck­on­ing of ge­ol­o­gists. The first two glaciers were not ex­ten­sive in north­ern Eu­rope.

64:4.4750,000 years ago the fourth ice sheet was well on its way south. With their im­proved im­ple­ments the Ne­an­derthalers made holes in the ice cov­er­ing the north­ern rivers and thus were able to spear the fish which came up to these vents. Ever these tribes re­treated be­fore the ad­vanc­ing ice, which at this time made its most ex­ten­sive in­va­sion of Eu­rope.

64:4.5In these times the Siberian glacier was mak­ing its south­ern­most march, com­pelling early man to move south­ward, back to­ward the lands of his ori­gin. But the hu­man species had so dif­fer­en­ti­ated that the dan­ger of fur­ther min­gling with its non­pro­gres­sive simian rel­a­tives was greatly less­ened.

64:4.6700,000 years ago the fourth glacier, the great­est of all in Eu­rope, was in re­ces­sion; men and an­i­mals were re­turn­ing north. The cli­mate was cool and moist, and prim­i­tive man again thrived in Eu­rope and west­ern Asia. Grad­u­ally the forests spread north over land which had been so re­cently cov­ered by the glacier.

64:4.7Mam­malian life had been lit­tle changed by the great glacier. These an­i­mals per­sisted in that nar­row belt of land ly­ing be­tween the ice and the Alps and, upon the re­treat of the glacier, again rapidly spread out over all Eu­rope. There ar­rived from Africa, over the Si­cil­ian land bridge, straight-tusked ele­phants, broad-nosed rhinoceroses, hye­nas, and African li­ons, and these new an­i­mals vir­tu­ally ex­ter­mi­nated the saber-toothed tigers and the hip­popota­muses.

64:4.8650,000 years ago wit­nessed the con­tin­u­a­tion of the mild cli­mate. By the mid­dle of the in­ter­glacial pe­riod it had be­come so warm that the Alps were al­most de­nuded of ice and snow.

64:4.9600,000 years ago the ice had reached its then north­ern­most point of re­treat and, af­ter a pause of a few thou­sand years, started south again on its fifth ex­cur­sion. But there was lit­tle mod­i­fi­ca­tion of cli­mate for fifty thou­sand years. Man and the an­i­mals of Eu­rope were lit­tle changed. The slight arid­ity of the for­mer pe­riod less­ened, and the alpine glaciers de­scended far down the river val­leys.

64:7.1When the col­ored de­scen­dants of the San­gik fam­ily be­gan to mul­ti­ply, and as they sought op­por­tu­nity for ex­pan­sion into ad­ja­cent ter­ri­tory, the fifth glacier, the third of ge­o­logic count, was well ad­vanced on its south­ern drift over Eu­rope and Asia. These early col­ored races were ex­traor­di­nar­ily tested by the rig­ors and hard­ships of the glacial age of their ori­gin. This glacier was so ex­ten­sive in Asia that for thou­sands of years mi­gra­tion to east­ern Asia was cut off. And not un­til the later re­treat of the Med­i­ter­ra­nean Sea, con­se­quent upon the el­e­va­tion of Ara­bia, was it pos­si­ble for them to reach Africa.

64:7.2–7 · six paragraphs not cited here ·

64:7.2Thus it was that for al­most one hun­dred thou­sand years these San­gik peo­ples spread out around the foothills and min­gled to­gether more or less, not­with­stand­ing the pe­cu­liar but nat­u­ral an­tipa­thy which early man­i­fested it­self be­tween the dif­fer­ent races.

64:7.3Be­tween the times of the Plan­e­tary Prince and Adam, In­dia be­came the home of the most cos­mopoli­tan pop­u­la­tion ever to be found on the face of the earth. But it was un­for­tu­nate that this mix­ture came to con­tain so much of the green, or­ange, and in­digo races. These sec­ondary San­gik peo­ples found ex­is­tence more easy and agree­able in the south­lands, and many of them sub­se­quently mi­grated to Africa. The pri­mary San­gik peo­ples, the su­pe­rior races, avoided the trop­ics, the red man go­ing north­east to Asia, closely fol­lowed by the yel­low man, while the blue race moved north­west into Eu­rope.

64:7.4The red men early be­gan to mi­grate to the north­east, on the heels of the re­treat­ing ice, pass­ing around the high­lands of In­dia and oc­cu­py­ing all of north­east­ern Asia. They were closely fol­lowed by the yel­low tribes, who sub­se­quently drove them out of Asia into North Amer­ica.

64:7.5When the rel­a­tively pure-line rem­nants of the red race for­sook Asia, there were eleven tribes, and they num­bered a lit­tle over seven thou­sand men, women, and chil­dren. These tribes were ac­com­pa­nied by three small groups of mixed an­ces­try, the largest of these be­ing a com­bi­na­tion of the or­ange and blue races. These three groups never fully frat­er­nized with the red man and early jour­neyed south­ward to Mex­ico and Cen­tral Amer­ica, where they were later joined by a small group of mixed yel­lows and reds. These peo­ples all in­ter­mar­ried and founded a new and amal­ga­mated race, one which was much less war­like than the pure-line red men. Within five thou­sand years this amal­ga­mated race broke up into three groups, es­tab­lish­ing the civ­i­liza­tions re­spec­tively of Mex­ico, Cen­tral Amer­ica, and South Amer­ica. The South Amer­i­can off­shoot did re­ceive a faint touch of the blood of Adam.

64:7.6To a cer­tain ex­tent the early red and yel­low men min­gled in Asia, and the off­spring of this union jour­neyed on to the east and along the south­ern sea­coast and, even­tu­ally, were driven by the rapidly in­creas­ing yel­low race onto the penin­su­las and near-by is­lands of the sea. They are the pres­ent-day brown men.

64:7.7The yel­low race has con­tin­ued to oc­cupy the cen­tral re­gions of east­ern Asia. Of all the six col­ored races they have sur­vived in great­est num­bers. While the yel­low men now and then en­gaged in racial war, they did not carry on such in­ces­sant and re­lent­less wars of ex­ter­mi­na­tion as were waged by the red, green, and or­ange men. These three races vir­tu­ally de­stroyed them­selves be­fore they were fi­nally all but an­ni­hi­lated by their en­e­mies of other races.

64:7.8Since the fifth glacier did not ex­tend so far south in Eu­rope, the way was par­tially open for these San­gik peo­ples to mi­grate to the north­west; and upon the re­treat of the ice the blue men, to­gether with a few other small racial groups, mi­grated west­ward along the old trails of the An­don tribes. They in­vaded Eu­rope in suc­ces­sive waves, oc­cu­py­ing most of the con­ti­nent.

64:7.9–16 · eight paragraphs not cited here ·

64:7.9In Eu­rope they soon en­coun­tered the Ne­an­derthal de­scen­dants of their early and com­mon an­ces­tor, An­don. These older Eu­ro­pean Ne­an­derthalers had been driven south and east by the glacier and thus were in po­si­tion quickly to en­counter and ab­sorb their in­vad­ing cousins of the San­gik tribes.

64:7.10In gen­eral and to start with, the San­gik tribes were more in­tel­li­gent than, and in most ways far su­pe­rior to, the de­te­ri­o­rated de­scen­dants of the early An­donic plains­men; and the min­gling of these San­gik tribes with the Ne­an­derthal peo­ples led to the im­me­di­ate im­prove­ment of the older race. It was this in­fu­sion of San­gik blood, more es­pe­cially that of the blue man, which pro­duced that marked im­prove­ment in the Ne­an­derthal peo­ples ex­hib­ited by the suc­ces­sive waves of in­creas­ingly in­tel­li­gent tribes that swept over Eu­rope from the east.

64:7.11Dur­ing the fol­low­ing in­ter­glacial pe­riod this new Ne­an­derthal race ex­tended from Eng­land to In­dia. The rem­nant of the blue race left in the old Per­sian penin­sula later amal­ga­mated with cer­tain oth­ers, pri­mar­ily the yel­low; and the re­sul­tant blend, sub­se­quently some­what up­stepped by the vi­o­let race of Adam, has per­sisted as the swarthy no­madic tribes of mod­ern Arabs.

64:7.12All ef­forts to iden­tify the San­gik an­ces­try of mod­ern peo­ples must take into ac­count the later im­prove­ment of the racial strains by the sub­se­quent ad­mix­ture of Adamic blood.

64:7.13The su­pe­rior races sought the north­ern or tem­per­ate climes, while the or­ange, green, and in­digo races suc­ces­sively grav­i­tated to Africa over the newly el­e­vated land bridge which sep­a­rated the west­ward re­treat­ing Med­i­ter­ra­nean from the In­dian Ocean.

64:7.14The last of the San­gik peo­ples to mi­grate from their cen­ter of race ori­gin was the in­digo man. About the time the green man was killing off the or­ange race in Egypt and greatly weak­en­ing him­self in so do­ing, the great black ex­o­dus started south through Pales­tine along the coast; and later, when these phys­i­cally strong in­digo peo­ples over­ran Egypt, they wiped the green man out of ex­is­tence by sheer force of num­bers. These in­digo races ab­sorbed the rem­nants of the or­ange man and much of the stock of the green man, and cer­tain of the in­digo tribes were con­sid­er­ably im­proved by this racial amal­ga­ma­tion.

64:7.15And so it ap­pears that Egypt was first dom­i­nated by the or­ange man, then by the green, fol­lowed by the in­digo (black) man, and still later by a mon­grel race of in­digo, blue, and mod­i­fied green men. But long be­fore Adam ar­rived, the blue men of Eu­rope and the mixed races of Ara­bia had driven the in­digo race out of Egypt and far south on the African con­ti­nent.

64:7.16As the San­gik mi­gra­tions draw to a close, the green and or­ange races are gone, the red man holds North Amer­ica, the yel­low man east­ern Asia, the blue man Eu­rope, and the in­digo race has grav­i­tated to Africa. In­dia har­bors a blend of the sec­ondary San­gik races, and the brown man, a blend of the red and yel­low, holds the is­lands off the Asi­atic coast. An amal­ga­mated race of rather su­pe­rior po­ten­tial oc­cu­pies the high­lands of South Amer­ica. The purer An­don­ites live in the ex­treme north­ern re­gions of Eu­rope and in Ice­land, Green­land, and north­east­ern North Amer­ica.

64:7.17Dur­ing the pe­ri­ods of far­thest glacial ad­vance the west­ern­most of the An­don tribes came very near be­ing driven into the sea. They lived for years on a nar­row south­ern strip of the pres­ent is­land of Eng­land. And it was the tra­di­tion of these re­peated glacial ad­vances that drove them to take to the sea when the sixth and last glacier fi­nally ap­peared. They were the first ma­rine ad­ven­tur­ers. They built boats and started in search of new lands which they hoped might be free from the ter­ri­fy­ing ice in­va­sions. And some of them reached Ice­land, oth­ers Green­land, but the vast ma­jor­ity per­ished from hunger and thirst on the open sea.

65:2.16In this way the life that was planted on Uran­tia evolved un­til the ice age, when man him­self first ap­peared and be­gan his event­ful plan­e­tary ca­reer. And this ap­pear­ance of prim­i­tive man on earth dur­ing the ice age was not just an ac­ci­dent; it was by de­sign. The rig­ors and cli­matic sever­ity of the glacial era were in ev­ery way adapted to the pur­pose of fos­ter­ing the pro­duc­tion of a hardy type of hu­man be­ing with tremen­dous sur­vival en­dow­ment.

79:5.2While the early Ne­an­derthalers were spread out over the en­tire breadth of Eura­sia, the east­ern wing was the more con­tam­i­nated with de­based an­i­mal strains. These sub­hu­man types were pushed south by the fifth glacier, the same ice sheet which so long blocked San­gik mi­gra­tion into east­ern Asia. And when the red man moved north­east around the high­lands of In­dia, he found north­east­ern Asia free from these sub­hu­man types. The tribal or­ga­ni­za­tion of the red races was formed ear­lier than that of any other peo­ples, and they were the first to mi­grate from the cen­tral Asian fo­cus of the San­giks. The in­fe­rior Ne­an­derthal strains were de­stroyed or driven off the main­land by the later mi­grat­ing yel­low tribes. But the red man had reigned su­preme in east­ern Asia for al­most one hun­dred thou­sand years be­fore the yel­low tribes ar­rived.

80:2.1The early ex­pan­sion of the vi­o­let race into Eu­rope was cut short by cer­tain rather sud­den cli­matic and ge­o­logic changes. With the re­treat of the north­ern ice fields the wa­ter-laden winds from the west shifted to the north, grad­u­ally turn­ing the great open pas­ture re­gions of Sa­hara into a bar­ren desert. This drought dis­persed the smaller-statured brunets, dark-eyed but long-headed dwellers of the great Sa­hara pla­teau.

Onward

See also glaciers

Cited alongside: British Isles, Europe, Greenland, Iceland, Illinois, Mississippi River, Pennsylvania, races