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Asia

38 paragraphs · about 13 minutes · 11 chapters

The paragraphs in the index’s own groups, a chapter to each, in the order the index prints them, and in the order of the book within each. A paragraph read in an earlier chapter is named in one line.

Andonites all over central A. in 15,000 B.C. 2 paragraphs

78:3.7The Sa­ha­ran civ­i­liza­tion had been dis­rupted by drought and that of the Med­i­ter­ra­nean basin by flood. The blue races had, as yet, failed to de­velop an ad­vanced cul­ture. The An­don­ites were still scat­tered over the Arc­tic and cen­tral Asian re­gions. The green and or­ange races had been ex­ter­mi­nated as such. The in­digo race was mov­ing south in Africa, there to be­gin its slow but long-con­tin­ued racial de­te­ri­o­ra­tion.

79:1.6In­creas­ing arid­ity in cen­tral Asia fur­ther op­er­ated to re­duce pop­u­la­tion and to ren­der these peo­ple less war­like; and when the di­min­ish­ing rain­fall to the north forced the no­madic An­don­ites south­ward, there was a tremen­dous ex­o­dus of And­ites from Tur­kes­tan. This is the ter­mi­nal move­ment of the so-called Aryans into the Lev­ant and In­dia. It cul­mi­nated that long dis­per­sal of the mixed de­scen­dants of Adam dur­ing which ev­ery Asi­atic and most of the is­land peo­ples of the Pa­cific were to some ex­tent im­proved by these su­pe­rior races.

backbone of A. reached height of 9 miles 1 paragraph

57:8.22With this in­crease in land el­e­va­tion the first cli­matic dif­fer­ences of the planet ap­peared. Land el­e­va­tion, cos­mic clouds, and oceanic in­flu­ences are the chief fac­tors in cli­matic fluc­tu­a­tion. The back­bone of the Asi­atic land mass reached a height of al­most nine miles at the time of the max­i­mum land emer­gence. Had there been much mois­ture in the air hov­er­ing over these highly el­e­vated re­gions, enor­mous ice blan­kets would have formed; the ice age would have ar­rived long be­fore it did. It was sev­eral hun­dred mil­lions of years be­fore so much land again ap­peared above wa­ter.

eastern coast of A. threatens to slide into watery grave 1 paragraph

58:5.8De­pres­sion of the ocean bot­tom dur­ing the pre­life ages had up­thrust a soli­tary con­ti­nen­tal land mass to such a height that its lat­eral pres­sure tended to cause the east­ern, west­ern, and south­ern fringes to slide down­hill, over the un­der­ly­ing semivis­cous lava beds, into the wa­ters of the sur­round­ing Pa­cific Ocean. This so fully com­pen­sated the con­ti­nen­tal pres­sure that a wide break did not oc­cur on the east­ern shore of this an­cient Asi­atic con­ti­nent, but ever since has that east­ern coast line hov­ered over the precipice of its ad­join­ing oceanic depths, threat­en­ing to slide into a wa­tery grave.

eating of executed criminals 1 paragraph

89:5.91. It some­times be­came a com­mu­nal cer­e­mony, the as­sump­tion of col­lec­tive re­spon­si­bil­ity for in­flict­ing the death penalty upon a fel­low tribesman. The blood guilt ceases to be a crime when par­tic­i­pated in by all, by so­ci­ety. The last of can­ni­bal­ism in Asia was this eat­ing of ex­e­cuted crim­i­nals.

geology 21 paragraphs

59:1.8380,000,000 years ago Asia was sub­sid­ing, and all other con­ti­nents were ex­pe­ri­enc­ing a short-lived emer­gence. But as this epoch pro­gressed, the newly ap­pear­ing At­lantic Ocean made ex­ten­sive in­roads on all ad­ja­cent coast lines. The north­ern At­lantic or Arc­tic seas were then con­nected with the south­ern Gulf wa­ters. When this south­ern sea en­tered the Ap­palachian trough, its waves broke upon the east against moun­tains as high as the Alps, but in gen­eral the con­ti­nents were un­in­ter­est­ing low­lands, ut­terly de­void of scenic beauty.

59:2.1The pe­ri­odic phe­nom­ena of land el­e­va­tion and land sink­ing char­ac­ter­is­tic of these times were all grad­ual and non­spec­tac­u­lar, be­ing ac­com­pa­nied by lit­tle or no vol­canic ac­tion. Through­out all of these suc­ces­sive land el­e­va­tions and de­pres­sions the Asi­atic mother con­ti­nent did not fully share the his­tory of the other land bod­ies. It ex­pe­ri­enced many in­un­da­tions, dip­ping first in one di­rec­tion and then an­other, more par­tic­u­larly in its ear­lier his­tory, but it does not pre­sent the uni­form rock de­posits which may be dis­cov­ered on the other con­ti­nents. In re­cent ages Asia has been the most sta­ble of all the land masses.

59:2.2 · one paragraph not cited here ·

59:2.2350,000,000 years ago saw the be­gin­ning of the great flood pe­riod of all the con­ti­nents ex­cept cen­tral Asia. The land masses were re­peat­edly cov­ered with wa­ter; only the coastal high­lands re­mained above these shal­low but wide­spread os­cil­la­tory in­land seas. Three ma­jor in­un­da­tions char­ac­ter­ized this pe­riod, but be­fore it ended, the con­ti­nents again arose, the to­tal land emer­gence be­ing fif­teen per cent greater than now ex­ists. The Caribbean re­gion was highly el­e­vated. This pe­riod is not well marked off in Eu­rope be­cause the land fluc­tu­a­tions were less, while the vol­canic ac­tion was more per­sis­tent.

59:2.3340,000,000 years ago there oc­curred an­other ex­ten­sive land sink­ing ex­cept in Asia and Aus­tralia. The wa­ters of the world’s oceans were gen­er­ally com­min­gled. This was a great lime­stone age, much of its stone be­ing laid down by lime-se­cret­ing al­gae.

59:3.3290,000,000 years ago the sea had largely with­drawn from the con­ti­nents, and the bot­toms of the sur­round­ing oceans were sink­ing. The land masses were lit­tle changed un­til they were again sub­merged. The early moun­tain move­ments of all the con­ti­nents were be­gin­ning, and the great­est of these crustal up­heavals were the Hi­malayas of Asia and the great Cale­do­nian Moun­tains, ex­tend­ing from Ire­land through Scot­land and on to Spitzber­gen.

59:4.5Five mil­lion years later the land ar­eas of North and South Amer­ica, Eu­rope, Africa, north­ern Asia, and Aus­tralia were briefly in­un­dated, in North Amer­ica the sub­mer­gence at one time or an­other be­ing al­most com­plete; and the re­sult­ing lime­stone lay­ers run from 500 to 5,000 feet in thick­ness. These var­i­ous De­vo­nian seas ex­tended first in one di­rec­tion and then in an­other so that the im­mense arc­tic North Amer­i­can in­land sea found an out­let to the Pa­cific Ocean through north­ern Cal­i­for­nia.

59:4.6–14 · nine paragraphs not cited here ·

59:4.6260,000,000 years ago, to­ward the end of this land-de­pres­sion epoch, North Amer­ica was par­tially over­spread by seas hav­ing si­mul­ta­ne­ous con­nec­tion with the Pa­cific, At­lantic, Arc­tic, and Gulf wa­ters. The de­posits of these later stages of the first De­vo­nian flood av­er­age about one thou­sand feet in thick­ness. The coral reefs char­ac­ter­iz­ing these times in­di­cate that the in­land seas were clear and shal­low. Such coral de­posits are ex­posed in the banks of the Ohio River near Louisville, Ken­tucky, and are about one hun­dred feet thick, em­brac­ing more than two hun­dred va­ri­eties. These coral for­ma­tions ex­tend through Canada and north­ern Eu­rope to the arc­tic re­gions.

59:4.7Fol­low­ing these sub­mer­gences, many of the shore lines were con­sid­er­ably el­e­vated so that the ear­lier de­posits were cov­ered by mud or shale. There is also a red sand­stone stra­tum which char­ac­ter­izes one of the De­vo­nian sed­i­men­ta­tions, and this red layer ex­tends over much of the earth’s sur­face, be­ing found in North and South Amer­ica, Eu­rope, Rus­sia, China, Africa, and Aus­tralia. Such red de­posits are sug­ges­tive of arid or semi­arid con­di­tions, but the cli­mate of this epoch was still mild and even.

59:4.8Through­out all of this pe­riod the land south­east of the Cincin­nati Is­land re­mained well above wa­ter. But very much of west­ern Eu­rope, in­clud­ing the British Isles, was sub­merged. In Wales, Ger­many, and other places in Eu­rope the De­vo­nian rocks are 20,000 feet thick.

59:4.9250,000,000 years ago wit­nessed the ap­pear­ance of the fish fam­ily, the ver­te­brates, one of the most im­por­tant steps in all pre­hu­man evo­lu­tion.

59:4.10The arthro­pods, or crus­taceans, were the an­ces­tors of the first ver­te­brates. The fore­run­ners of the fish fam­ily were two mod­i­fied arthro­pod an­ces­tors; one had a long body con­nect­ing a head and tail, while the other was a back­bone­less, jaw­less pre­fish. But these pre­lim­i­nary types were quickly de­stroyed when the fishes, the first ver­te­brates of the an­i­mal world, made their sud­den ap­pear­ance from the north.

59:4.11Many of the largest true fish be­long to this age, some of the teeth-bear­ing va­ri­eties be­ing twenty-five to thirty feet long; the pres­ent-day sharks are the sur­vivors of these an­cient fishes. The lung and ar­mored fishes reached their evo­lu­tion­ary apex, and be­fore this epoch had ended, fishes had adapted to both fresh and salt wa­ters.

59:4.12Ver­i­ta­ble bone beds of fish teeth and skele­tons may be found in the de­posits laid down to­ward the close of this pe­riod, and rich fos­sil beds are sit­u­ated along the coast of Cal­i­for­nia since many shel­tered bays of the Pa­cific Ocean ex­tended into the land of that re­gion.

59:4.13The earth was be­ing rapidly over­run by the new or­ders of land veg­e­ta­tion. Here­to­fore few plants grew on land ex­cept about the wa­ter’s edge. Now, and sud­denly, the pro­lific fern fam­ily ap­peared and quickly spread over the face of the rapidly ris­ing land in all parts of the world. Tree types, two feet thick and forty feet high, soon de­vel­oped; later on, leaves evolved, but these early va­ri­eties had only rudi­men­tary fo­liage. There were many smaller plants, but their fos­sils are not found since they were usu­ally de­stroyed by the still ear­lier ap­pear­ing bac­te­ria.

59:4.14As the land rose, North Amer­ica be­came con­nected with Eu­rope by land bridges ex­tend­ing to Green­land. And to­day Green­land holds the re­mains of these early land plants be­neath its man­tle of ice.

59:4.15240,000,000 years ago the land over parts of both Eu­rope and North and South Amer­ica be­gan to sink. This sub­si­dence marked the ap­pear­ance of the last and least ex­ten­sive of the De­vo­nian floods. The arc­tic seas again moved south­ward over much of North Amer­ica, the At­lantic in­un­dated a large part of Eu­rope and west­ern Asia, while the south­ern Pa­cific cov­ered most of In­dia. This in­un­da­tion was slow in ap­pear­ing and equally slow in re­treat­ing. The Catskill Moun­tains along the west bank of the Hud­son River are one of the largest ge­o­logic mon­u­ments of this epoch to be found on the sur­face of North Amer­ica.

59:5.4210,000,000 years ago the warm-wa­ter arc­tic seas cov­ered most of North Amer­ica and Eu­rope. The south po­lar wa­ters in­un­dated South Amer­ica and Aus­tralia, while both Africa and Asia were highly el­e­vated.

59:5.5–19 · 15 paragraphs not cited here ·

59:5.5When the seas were at their height, a new evo­lu­tion­ary de­vel­op­ment sud­denly oc­curred. Abruptly, the first of the land an­i­mals ap­peared. There were nu­mer­ous species of these an­i­mals that were able to live on land or in wa­ter. These air-breath­ing am­phib­ians de­vel­oped from the arthro­pods, whose swim blad­ders had evolved into lungs.

59:5.6From the briny wa­ters of the seas there crawled out upon the land snails, scor­pi­ons, and frogs. To­day frogs still lay their eggs in wa­ter, and their young first ex­ist as lit­tle fishes, tad­poles. This pe­riod could well be known as the age of frogs.

59:5.7Very soon there­after the in­sects first ap­peared and, to­gether with spi­ders, scor­pi­ons, cock­roaches, crick­ets, and lo­custs, soon over­spread the con­ti­nents of the world. Dragon flies mea­sured thirty inches across. One thou­sand species of cock­roaches de­vel­oped, and some grew to be four inches long.

59:5.8Two groups of echin­o­derms be­came es­pe­cially well de­vel­oped, and they are in re­al­ity the guide fos­sils of this epoch. The large shell-feed­ing sharks were also highly evolved, and for more than five mil­lion years they dom­i­nated the oceans. The cli­mate was still mild and equable; the ma­rine life was lit­tle changed. Fresh-wa­ter fish were de­vel­op­ing and the trilo­bites were near­ing ex­tinc­tion. Corals were scarce, and much of the lime­stone was be­ing made by the crinoids. The finer build­ing lime­stones were laid down dur­ing this epoch.

59:5.9The wa­ters of many of the in­land seas were so heav­ily charged with lime and other min­er­als as greatly to in­ter­fere with the prog­ress and de­vel­op­ment of many ma­rine species. Even­tu­ally the seas cleared up as the re­sult of an ex­ten­sive stone de­posit, in some places con­tain­ing zinc and lead.

59:5.10The de­posits of this early Car­bonif­er­ous age are from 500 to 2,000 feet thick, con­sist­ing of sand­stone, shale, and lime­stone. The old­est strata yield the fos­sils of both land and ma­rine an­i­mals and plants, along with much gravel and basin sed­i­ments. Lit­tle work­able coal is found in these older strata. These de­po­si­tions through­out Eu­rope are very sim­i­lar to those laid down over North Amer­ica.

59:5.11To­ward the close of this epoch the land of North Amer­ica be­gan to rise. There was a short in­ter­rup­tion, and the sea re­turned to cover about half of its pre­vi­ous beds. This was a short in­un­da­tion, and most of the land was soon well above wa­ter. South Amer­ica was still con­nected with Eu­rope by way of Africa.

59:5.12This epoch wit­nessed the be­gin­ning of the Vos­ges, Black For­est, and Ural moun­tains. Stumps of other and older moun­tains are to be found all over Great Britain and Eu­rope.

59:5.13200,000,000 years ago the re­ally ac­tive stages of the Car­bonif­er­ous pe­riod be­gan. For twenty mil­lion years prior to this time the ear­lier coal de­posits were be­ing laid down, but now the more ex­ten­sive coal-for­ma­tion ac­tiv­i­ties were in pro­cess. The length of the ac­tual coal-de­po­si­tion epoch was a lit­tle over twenty-five mil­lion years.

59:5.14The land was pe­ri­od­i­cally go­ing up and down due to the shift­ing sea level oc­ca­sioned by ac­tiv­i­ties on the ocean bot­toms. This crustal un­easi­ness—the set­tling and ris­ing of the land—in con­nec­tion with the pro­lific veg­e­ta­tion of the coastal swamps, con­tributed to the pro­duc­tion of ex­ten­sive coal de­posits, which have caused this pe­riod to be known as the Car­bonif­er­ous. And the cli­mate was still mild the world over.

59:5.15The coal lay­ers al­ter­nate with shale, stone, and con­glom­er­ate. These coal beds over cen­tral and east­ern United States vary in thick­ness from forty to fifty feet. But many of these de­posits were washed away dur­ing sub­se­quent land el­e­va­tions. In some parts of North Amer­ica and Eu­rope the coal-bear­ing strata are 18,000 feet in thick­ness.

59:5.16The pres­ence of roots of trees as they grew in the clay un­der­ly­ing the pres­ent coal beds demon­strates that coal was formed ex­actly where it is now found. Coal is the wa­ter-pre­served and pres­sure-mod­i­fied re­mains of the rank veg­e­ta­tion grow­ing in the bogs and on the swamp shores of this far­away age. Coal lay­ers of­ten hold both gas and oil. Peat beds, the re­mains of past veg­etable growth, would be con­verted into a type of coal if sub­jected to proper pres­sure and heat. An­thracite has been sub­jected to more pres­sure and heat than other coal.

59:5.17In North Amer­ica the lay­ers of coal in the var­i­ous beds, which in­di­cate the num­ber of times the land fell and rose, vary from ten in Illi­nois, twenty in Penn­syl­va­nia, thirty-five in Al­abama, to sev­enty-five in Canada. Both fresh- and salt-wa­ter fos­sils are found in the coal beds.

59:5.18Through­out this epoch the moun­tains of North and South Amer­ica were ac­tive, both the An­des and the south­ern an­ces­tral Rocky Moun­tains ris­ing. The great At­lantic and Pa­cific high coastal re­gions be­gan to sink, even­tu­ally be­com­ing so eroded and sub­merged that the coast lines of both oceans with­drew to ap­prox­i­mately their pres­ent po­si­tions. The de­posits of this in­un­da­tion av­er­age about one thou­sand feet in thick­ness.

59:5.19190,000,000 years ago wit­nessed a west­ward ex­ten­sion of the North Amer­i­can Car­bonif­er­ous sea over the pres­ent Rocky Moun­tain re­gion, with an out­let to the Pa­cific Ocean through north­ern Cal­i­for­nia. Coal con­tin­ued to be laid down through­out the Amer­i­cas and Eu­rope, layer upon layer, as the coast­lands rose and fell dur­ing these ages of seashore os­cil­la­tions.

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.

59:6.8Among the land an­i­mals the frogs reached their cli­max in the pre­ced­ing age and rapidly de­clined, but they sur­vived be­cause they could long live even in the dry­ing-up pools and ponds of these far-dis­tant and ex­tremely try­ing times. Dur­ing this de­clin­ing frog age, in Africa, the first step in the evo­lu­tion of the frog into the rep­tile oc­curred. And since the land masses were still con­nected, this pre­rep­til­ian crea­ture, an air breather, spread over all the world. By this time the at­mo­sphere had been so changed that it served ad­mirably to sup­port an­i­mal res­pi­ra­tion. It was soon af­ter the ar­rival of these pre­rep­til­ian frogs that North Amer­ica was tem­porar­ily iso­lated, cut off from Eu­rope, Asia, and South Amer­ica.

60:1.6As this era opens, the east­ern and cen­tral parts of North Amer­ica, the north­ern half of South Amer­ica, most of Eu­rope, and all of Asia are well above wa­ter. North Amer­ica for the first time is ge­o­graph­i­cally iso­lated, but not for long as the Bering Strait land bridge soon again emerges, con­nect­ing the con­ti­nent with Asia.

60:1.7–11 · five paragraphs not cited here ·

60:1.7Great troughs de­vel­oped in North Amer­ica, par­al­lel­ing the At­lantic and Pa­cific coasts. The great east­ern-Con­necti­cut fault ap­peared, one side even­tu­ally sink­ing two miles. Many of these North Amer­i­can troughs were later filled with ero­sion de­posits, as also were many of the basins of the fresh- and salt-wa­ter lakes of the moun­tain re­gions. Later on, these filled land de­pres­sions were greatly el­e­vated by lava flows which oc­curred un­der­ground. The pet­ri­fied forests of many re­gions be­long to this epoch.

60:1.8The Pa­cific coast, usu­ally above wa­ter dur­ing the con­ti­nen­tal sub­mer­gences, went down ex­cept­ing the south­ern part of Cal­i­for­nia and a large is­land which then ex­isted in what is now the Pa­cific Ocean. This an­cient Cal­i­for­nia sea was rich in ma­rine life and ex­tended east­ward to con­nect with the old sea basin of the mid­west­ern re­gion.

60:1.9140,000,000 years ago, sud­denly and with only the hint of the two pre­rep­til­ian an­ces­tors that de­vel­oped in Africa dur­ing the pre­ced­ing epoch, the rep­tiles ap­peared in full-fledged form. They de­vel­oped rapidly, soon yield­ing croc­o­diles, scaled rep­tiles, and even­tu­ally both sea ser­pents and fly­ing rep­tiles. Their tran­si­tion an­ces­tors speed­ily dis­ap­peared.

60:1.10These rapidly evolv­ing rep­til­ian di­no­saurs soon be­came the monar­chs of this age. They were egg lay­ers and are dis­tin­guished from all an­i­mals by their small brains, hav­ing brains weigh­ing less than one pound to con­trol bod­ies later weigh­ing as much as forty tons. But ear­lier rep­tiles were smaller, car­niv­o­rous, and walked kan­ga­roo­like on their hind legs. They had hol­low avian bones and sub­se­quently de­vel­oped only three toes on their hind feet, and many of their fos­sil foot­prints have been mis­taken for those of gi­ant birds. Later on, the her­biv­o­rous di­no­saurs evolved. They walked on all fours, and one branch of this group de­vel­oped a pro­tec­tive ar­mor.

60:1.11Sev­eral mil­lion years later the first mam­mals ap­peared. They were non­pla­cen­tal and proved a speedy fail­ure; none sur­vived. This was an ex­per­i­men­tal ef­fort to im­prove mam­malian types, but it did not suc­ceed on Uran­tia.

60:1.12The ma­rine life of this pe­riod was mea­ger but im­proved rapidly with the new in­va­sion of the sea, which again pro­duced ex­ten­sive coast lines of shal­low wa­ters. Since there was more shal­low wa­ter around Eu­rope and Asia, the rich­est fos­sil beds are to be found about these con­ti­nents. To­day, if you would study the life of this age, ex­am­ine the Hi­malayan, Siberian, and Med­i­ter­ra­nean re­gions, as well as In­dia and the is­lands of the south­ern Pa­cific basin. A promi­nent fea­ture of the ma­rine life was the pres­ence of hosts of the beau­ti­ful am­monites, whose fos­sil re­mains are found all over the world.

60:3.1180,000,000 years ago great dis­tur­bances oc­curred in the earth’s crust. The west­ern ad­vance of the con­ti­nen­tal drift was com­ing to a stand­still, and the enor­mous en­ergy of the slug­gish mo­men­tum of the hin­ter con­ti­nen­tal mass up­crum­pled the Pa­cific shore line of both North and South Amer­ica and ini­ti­ated pro­found reper­cus­sional changes along the Pa­cific shores of Asia. This cir­cum­pa­cific land el­e­va­tion, which cul­mi­nated in pres­ent-day moun­tain ranges, is more than twenty-five thou­sand miles long. And the up­heavals at­ten­dant upon its birth were the great­est sur­face dis­tor­tions to take place since life ap­peared on Uran­tia. The lava flows, both above and be­low ground, were ex­ten­sive and wide­spread.

60:3.12–14 · three paragraphs not cited here ·

60:3.1275,000,000 years ago marks the end of the con­ti­nen­tal drift. From Alaska to Cape Horn the long Pa­cific coast moun­tain ranges were com­pleted, but there were as yet few peaks.

60:3.13The back­thrust of the halted con­ti­nen­tal drift con­tin­ued the el­e­va­tion of the west­ern plains of North Amer­ica, while in the east the worn-down Ap­palachian Moun­tains of the At­lantic coast re­gion were pro­jected straight up, with lit­tle or no tilt­ing.

60:3.1470,000,000 years ago the crustal dis­tor­tions con­nected with the max­i­mum el­e­va­tion of the Rocky Moun­tain re­gion took place. A large seg­ment of rock was over­thrust fif­teen miles at the sur­face in British Columbia; here the Cam­brian rocks are obliquely thrust out over the Cre­ta­ceous lay­ers. On the east­ern slope of the Rocky Moun­tains, near the Cana­dian bor­der, there was an­other spec­tac­u­lar over­thrust; here may be found the pre­life stone lay­ers shoved out over the then re­cent Cre­ta­ceous de­posits.

60:3.15This was an age of vol­canic ac­tiv­ity all over the world, giv­ing rise to nu­mer­ous small iso­lated vol­canic cones. Sub­ma­rine vol­ca­noes broke out in the sub­merged Hi­malayan re­gion. Much of the rest of Asia, in­clud­ing Siberia, was also still un­der wa­ter.

60:4.3The old­est moun­tains of the world are lo­cated in Asia, Green­land, and north­ern Eu­rope among those of the older east-west sys­tems. The mid-age moun­tains are in the cir­cum­pa­cific group and in the sec­ond Eu­ro­pean east-west sys­tem, which was born at about the same time. This gi­gan­tic up­ris­ing is al­most ten thou­sand miles long, ex­tend­ing from Eu­rope over into the West In­dies land el­e­va­tions. The young­est moun­tains are in the Rocky Moun­tain sys­tem, where, for ages, land el­e­va­tions had oc­curred only to be suc­ces­sively cov­ered by the sea, though some of the higher lands re­mained as is­lands. Sub­se­quent to the for­ma­tion of the mid-age moun­tains, a real moun­tain high­land was el­e­vated which was des­tined, sub­se­quently, to be carved into the pres­ent Rocky Moun­tains by the com­bined artistry of na­ture’s el­e­ments.

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.

61:3.715,000,000 years ago the moun­tain re­gions of Eura­sia were ris­ing, and there was some vol­canic ac­tiv­ity through­out these re­gions, but noth­ing com­pa­ra­ble to the lava flows of the West­ern Hemi­sphere. These un­set­tled con­di­tions pre­vailed all over the world.

61:4.3For a short time all the land of the world was again joined ex­cept­ing Aus­tralia, and the last great world-wide an­i­mal mi­gra­tion took place. North Amer­ica was con­nected with both South Amer­ica and Asia, and there was a free ex­change of an­i­mal life. Asi­atic sloths, ar­madil­los, an­telopes, and bears en­tered North Amer­ica, while North Amer­i­can camels went to China. Rhinoceroses mi­grated over the whole world ex­cept Aus­tralia and South Amer­ica, but they were ex­tinct in the West­ern Hemi­sphere by the close of this pe­riod.

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.

61:5.4–6 · three paragraphs not cited here ·

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.

61:7.3In 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.

homeland of human race 1 paragraph

79:0.1Asia is the home­land of the hu­man race. It was on a south­ern penin­sula of this con­ti­nent that An­don and Fonta were born; in the high­lands of what is now Afghanistan, their de­scen­dant Bado­nan founded a prim­i­tive cen­ter of cul­ture that per­sisted for over one-half mil­lion years. Here at this east­ern fo­cus of the hu­man race the San­gik peo­ples dif­fer­en­ti­ated from the An­donic stock, and Asia was their first home, their first hunt­ing ground, their first bat­tle­field. South­west­ern Asia wit­nessed the suc­ces­sive civ­i­liza­tions of Dala­ma­tians, Nod­ites, Adamites, and And­ites, and from these re­gions the po­ten­tials of mod­ern civ­i­liza­tion spread to the world.

most animals suitable for domestication found in 1 paragraph

81:2.11Most of the an­i­mals best suited to do­mes­ti­ca­tion were found in Asia, es­pe­cially in the cen­tral to south­west re­gions. This was one rea­son why civ­i­liza­tion pro­gressed faster in that lo­cal­ity than in other parts of the world. Many of these an­i­mals had been twice be­fore do­mes­ti­cated, and in the And­ite age they were re­tamed once again. But the dog had re­mained with the hunters ever since be­ing adopted by the blue man long, long be­fore.

red race left imprint 1 paragraph

64:6.5About eighty-five thou­sand years ago the com­par­a­tively pure rem­nants of the red race went en masse across to North Amer­ica, and shortly there­after the Bering land isth­mus sank, thus iso­lat­ing them. No red man ever re­turned to Asia. But through­out Siberia, China, cen­tral Asia, In­dia, and Eu­rope they left be­hind much of their stock blended with the other col­ored races.

Salem missionaries penetrated to remotest tribes of 1 paragraph

94:0.1The early teach­ers of the Salem re­li­gion pen­e­trated to the re­motest tribes of Africa and Eura­sia, ever preach­ing Ma­chi­venta’s gospel of man’s faith and trust in the one uni­ver­sal God as the only price of ob­tain­ing di­vine fa­vor. Mel­chiz­e­dek’s covenant with Abra­ham was the pat­tern for all the early pro­pa­ganda that went out from Salem and other cen­ters. Uran­tia has never had more en­thu­si­as­tic and ag­gres­sive mis­sion­ar­ies of any re­li­gion than these no­ble men and women who car­ried the teach­ings of Mel­chiz­e­dek over the en­tire East­ern Hemi­sphere. These mis­sion­ar­ies were re­cruited from many peo­ples and races, and they largely spread their teach­ings through the medium of na­tive con­verts. They es­tab­lished train­ing cen­ters in dif­fer­ent parts of the world where they taught the na­tives the Salem re­li­gion and then com­mis­sioned these pupils to func­tion as teach­ers among their own peo­ple.

yellow race drove Andonites from 4 paragraphs

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.

78:1.53. The An­don­ites main­tained five or six fairly rep­re­sen­ta­tive set­tle­ments to the north and east of the Adam­son head­quar­ters. They were also scat­tered through­out Tur­kes­tan, while iso­lated is­lands of them per­sisted through­out Eura­sia, es­pe­cially in moun­tain­ous re­gions. These abo­rig­ines still held the north­lands of the Eurasian con­ti­nent, to­gether with Ice­land and Green­land, but they had long since been driven from the plains of Eu­rope by the blue man and from the river val­leys of far­ther Asia by the ex­pand­ing yel­low race.

78:1.64. The red man oc­cu­pied the Amer­i­cas, hav­ing been driven out of Asia over fifty thou­sand years be­fore the ar­rival of Adam.

78:1.75. The yel­low race. The Chi­nese peo­ples were well es­tab­lished in con­trol of east­ern Asia. Their most ad­vanced set­tle­ments were sit­u­ated to the north­west of mod­ern China in re­gions bor­der­ing on Ti­bet.

yellow race drove red race from 4 paragraphs, 1 read above

64:6.4In later times they had se­ri­ous and pro­longed trou­ble with their yel­low breth­ren in Asia. They were aided by their early in­ven­tion of the bow and ar­row, but they had un­for­tu­nately in­her­ited much of the ten­dency of their an­ces­tors to fight among them­selves, and this so weak­ened them that the yel­low tribes were able to drive them off the Asi­atic con­ti­nent.

64:6.5–13 · nine paragraphs not cited here ·

64:6.5 read above, under red race left imprint

64:6.6When the red man crossed over into Amer­ica, he brought along much of the teach­ings and tra­di­tions of his early ori­gin. His im­me­di­ate an­ces­tors had been in touch with the later ac­tiv­i­ties of the world head­quar­ters of the Plan­e­tary Prince. But in a short time af­ter reach­ing the Amer­i­cas, the red men be­gan to lose sight of these teach­ings, and there oc­curred a great de­cline in in­tel­lec­tual and spir­i­tual cul­ture. Very soon these peo­ple again fell to fight­ing so fiercely among them­selves that it ap­peared that these tribal wars would re­sult in the speedy ex­tinc­tion of this rem­nant of the com­par­a­tively pure red race.

64:6.7Be­cause of this great ret­ro­gres­sion the red men seemed doomed when, about sixty-five thou­sand years ago, Ona­mo­na­lon­ton ap­peared as their leader and spir­i­tual de­liv­erer. He brought tem­po­rary peace among the Amer­i­can red men and re­vived their wor­ship of the “Great Spirit.” Ona­mo­na­lon­ton lived to be ninety-six years of age and main­tained his head­quar­ters among the great red­wood trees of Cal­i­for­nia. Many of his later de­scen­dants have come down to mod­ern times among the Black­foot In­di­ans.

64:6.8As time passed, the teach­ings of Ona­mo­na­lon­ton be­came hazy tra­di­tions. In­ternecine wars were re­sumed, and never af­ter the days of this great teacher did an­other leader suc­ceed in bring­ing uni­ver­sal peace among them. In­creas­ingly the more in­tel­li­gent strains per­ished in these tribal strug­gles; oth­er­wise a great civ­i­liza­tion would have been built upon the North Amer­i­can con­ti­nent by these able and in­tel­li­gent red men.

64:6.9Af­ter cross­ing over to Amer­ica from China, the north­ern red man never again came in con­tact with other world in­flu­ences (ex­cept the Es­kimo) un­til he was later dis­cov­ered by the white man. It was most un­for­tu­nate that the red man al­most com­pletely missed his op­por­tu­nity of be­ing up­stepped by the ad­mix­ture of the later Adamic stock. As it was, the red man could not rule the white man, and he would not will­ingly serve him. In such a cir­cum­stance, if the two races do not blend, one or the other is doomed.

64:6.102. The or­ange man. The out­stand­ing char­ac­ter­is­tic of this race was their pe­cu­liar urge to build, to build any­thing and ev­ery­thing, even to the pil­ing up of vast mounds of stone just to see which tribe could build the largest mound. Though they were not a pro­gres­sive peo­ple, they prof­ited much from the schools of the Prince and sent del­e­gates there for in­struc­tion.

64:6.11The or­ange race was the first to fol­low the coast line south­ward to­ward Africa as the Med­i­ter­ra­nean Sea with­drew to the west. But they never se­cured a fa­vor­able foot­ing in Africa and were wiped out of ex­is­tence by the later ar­riv­ing green race.

64:6.12Be­fore the end came, this peo­ple lost much cul­tural and spir­i­tual ground. But there was a great re­vival of higher liv­ing as a re­sult of the wise lead­er­ship of Por­shunta, the mas­ter mind of this un­for­tu­nate race, who min­is­tered to them when their head­quar­ters was at Ar­maged­don some three hun­dred thou­sand years ago.

64:6.13The last great strug­gle be­tween the or­ange and the green men oc­curred in the re­gion of the lower Nile val­ley in Egypt. This long-drawn-out bat­tle was waged for al­most one hun­dred years, and at its close very few of the or­ange race were left alive. The shat­tered rem­nants of these peo­ple were ab­sorbed by the green and by the later ar­riv­ing in­digo men. But as a race the or­ange man ceased to ex­ist about one hun­dred thou­sand years ago.

64:6.143. The yel­low man. The prim­i­tive yel­low tribes were the first to aban­don the chase, es­tab­lish set­tled com­mu­ni­ties, and de­velop a home life based on agri­cul­ture. In­tel­lec­tu­ally they were some­what in­fe­rior to the red man, but so­cially and col­lec­tively they proved them­selves su­pe­rior to all of the San­gik peo­ples in the mat­ter of fos­ter­ing racial civ­i­liza­tion. Be­cause they de­vel­oped a fra­ter­nal spirit, the var­i­ous tribes learn­ing to live to­gether in rel­a­tive peace, they were able to drive the red race be­fore them as they grad­u­ally ex­panded into Asia.

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.

78:1.6 read above, under yellow race drove Andonites from

Onward

See also Burma; China; India; Indo-China; Iran; Japan; Kashmir; Malaysia; Mesopotamia; Mongolia; Nepal; Parthia; Russia; Siam; Siberia; Turkestan

Cited alongside: Europe, South America, Africa, Australia, India, North America, red race, yellow race