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volcanoes

36 paragraphs · about 11 minutes

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

57:7.1Through­out these early times the space re­gions of the so­lar sys­tem were swarm­ing with small dis­rup­tive and con­den­sa­tion bod­ies, and in the ab­sence of a pro­tec­tive com­bus­tion at­mo­sphere such space bod­ies crashed di­rectly on the sur­face of Uran­tia. These in­ces­sant im­pacts kept the sur­face of the planet more or less heated, and this, to­gether with the in­creased ac­tion of grav­ity as the sphere grew larger, be­gan to set in op­er­a­tion those in­flu­ences which grad­u­ally caused the heav­ier el­e­ments, such as iron, to set­tle more and more to­ward the cen­ter of the planet.

57:7.22,000,000,000 years ago the earth be­gan de­cid­edly to gain on the moon. Al­ways had the planet been larger than its satel­lite, but there was not so much dif­fer­ence in size un­til about this time, when enor­mous space bod­ies were cap­tured by the earth. Uran­tia was then about one fifth its pres­ent size and had be­come large enough to hold the prim­i­tive at­mo­sphere which had be­gun to ap­pear as a re­sult of the in­ter­nal el­e­men­tal con­test be­tween the heated in­te­rior and the cool­ing crust.

57:7.3Def­i­nite vol­canic ac­tion dates from these times. The in­ter­nal heat of the earth con­tin­ued to be aug­mented by the deeper and deeper burial of the ra­dioac­tive or heav­ier el­e­ments brought in from space by the me­te­ors. The study of these ra­dioac­tive el­e­ments will re­veal that Uran­tia is more than one bil­lion years old on its sur­face. The ra­dium clock is your most re­li­able time­piece for mak­ing sci­en­tific es­ti­mates of the age of the planet, but all such es­ti­mates are too short be­cause the ra­dioac­tive ma­te­ri­als open to your scrutiny are all de­rived from the earth’s sur­face and hence rep­re­sent Uran­tia’s com­par­a­tively re­cent ac­quire­ments of these el­e­ments.

57:7.41,500,000,000 years ago the earth was two thirds its pres­ent size, while the moon was near­ing its pres­ent mass. Earth’s rapid gain over the moon in size en­abled it to be­gin the slow rob­bery of the lit­tle at­mo­sphere which its satel­lite orig­i­nally had.

57:7.5Vol­canic ac­tion is now at its height. The whole earth is a ver­i­ta­ble fiery in­ferno, the sur­face re­sem­bling its ear­lier molten state be­fore the heav­ier met­als grav­i­tated to­ward the cen­ter. This is the vol­canic age. Nev­er­the­less, a crust, con­sist­ing chiefly of the com­par­a­tively lighter gran­ite, is grad­u­ally form­ing. The stage is be­ing set for a planet which can some­day sup­port life.

57:7.6The prim­i­tive plan­e­tary at­mo­sphere is slowly evolv­ing, now con­tain­ing some wa­ter va­por, car­bon monox­ide, car­bon diox­ide, and hy­dro­gen chlo­ride, but there is lit­tle or no free ni­tro­gen or free oxy­gen. The at­mo­sphere of a world in the vol­canic age pre­sents a queer spec­ta­cle. In ad­di­tion to the gases enu­mer­ated it is heav­ily charged with nu­mer­ous vol­canic gases and, as the air belt ma­tures, with the com­bus­tion prod­ucts of the heavy me­te­oric show­ers which are con­stantly hurtling in upon the plan­e­tary sur­face. Such me­te­oric com­bus­tion keeps the at­mo­spheric oxy­gen very nearly ex­hausted, and the rate of me­te­oric bom­bard­ment is still tremen­dous.

57:7.7Pres­ently, the at­mo­sphere be­came more set­tled and cooled suf­fi­ciently to start pre­cip­i­ta­tion of rain on the hot rocky sur­face of the planet. For thou­sands of years Uran­tia was en­veloped in one vast and con­tin­u­ous blan­ket of steam. And dur­ing these ages the sun never shone upon the earth’s sur­face.

57:7.8Much of the car­bon of the at­mo­sphere was ab­stracted to form the car­bon­ates of the var­i­ous met­als which abounded in the su­per­fi­cial lay­ers of the planet. Later on, much greater quan­ti­ties of these car­bon gases were con­sumed by the early and pro­lific plant life.

57:7.9Even in the later pe­ri­ods the con­tin­u­ing lava flows and the in­com­ing me­te­ors kept the oxy­gen of the air al­most com­pletely used up. Even the early de­posits of the soon ap­pear­ing prim­i­tive ocean con­tain no col­ored stones or shales. And for a long time af­ter this ocean ap­peared, there was vir­tu­ally no free oxy­gen in the at­mo­sphere; and it did not ap­pear in sig­nif­i­cant quan­ti­ties un­til it was later gen­er­ated by the sea­weeds and other forms of veg­etable life.

57:7.10The prim­i­tive plan­e­tary at­mo­sphere of the vol­canic age af­fords lit­tle pro­tec­tion against the col­li­sional im­pacts of the me­te­oric swarms. Mil­lions upon mil­lions of me­te­ors are able to pen­e­trate such an air belt to smash against the plan­e­tary crust as solid bod­ies. But as time passes, fewer and fewer prove large enough to re­sist the ever-stronger fric­tion shield of the oxy­gen-en­rich­ing at­mo­sphere of the later eras.

57:8.2The at­mo­sphere, to­gether with in­ces­sant mois­ture pre­cip­i­ta­tion, fa­cil­i­tated the cool­ing of the earth’s crust. Vol­canic ac­tion early equal­ized in­ter­nal-heat pres­sure and crustal con­trac­tion; and as vol­ca­noes rapidly de­creased, earth­quakes made their ap­pear­ance as this epoch of crustal cool­ing and ad­just­ment pro­gressed.

57:8.3–10 · eight paragraphs not cited here ·

57:8.3The real ge­o­logic his­tory of Uran­tia be­gins with the cool­ing of the earth’s crust suf­fi­ciently to cause the for­ma­tion of the first ocean. Wa­ter-va­por con­den­sa­tion on the cool­ing sur­face of the earth, once be­gun, con­tin­ued un­til it was vir­tu­ally com­plete. By the end of this pe­riod the ocean was world-wide, cov­er­ing the en­tire planet to an av­er­age depth of over one mile. The tides were then in play much as they are now ob­served, but this prim­i­tive ocean was not salty; it was prac­ti­cally a fresh-wa­ter cov­er­ing for the world. In those days, most of the chlo­rine was com­bined with var­i­ous met­als, but there was enough, in union with hy­dro­gen, to ren­der this wa­ter faintly acid.

57:8.4At the open­ing of this far­away era, Uran­tia should be en­vis­aged as a wa­ter-bound planet. Later on, deeper and hence denser lava flows came out upon the bot­tom of the pres­ent Pa­cific Ocean, and this part of the wa­ter-cov­ered sur­face be­came con­sid­er­ably de­pressed. The first con­ti­nen­tal land mass emerged from the world ocean in com­pen­satory ad­just­ment of the equi­lib­rium of the grad­u­ally thick­en­ing earth’s crust.

57:8.5950,000,000 years ago Uran­tia pre­sents the pic­ture of one great con­ti­nent of land and one large body of wa­ter, the Pa­cific Ocean. Vol­ca­noes are still wide­spread and earth­quakes are both fre­quent and se­vere. Me­te­ors con­tinue to bom­bard the earth, but they are di­min­ish­ing in both fre­quency and size. The at­mo­sphere is clear­ing up, but the amount of car­bon diox­ide con­tin­ues large. The earth’s crust is grad­u­ally sta­bi­liz­ing.

57:8.6It was at about this time that Uran­tia was as­signed to the sys­tem of Sa­ta­nia for plan­e­tary ad­min­is­tra­tion and was placed on the life reg­istry of Nor­la­ti­adek. Then be­gan the ad­min­is­tra­tive rec­og­ni­tion of the small and in­signif­i­cant sphere which was des­tined to be the planet whereon Mi­chael would sub­se­quently en­gage in the stu­pen­dous un­der­tak­ing of mor­tal be­stowal, would par­tic­i­pate in those ex­pe­ri­ences which have since caused Uran­tia to be­come lo­cally known as the “world of the cross.”

57:8.7900,000,000 years ago wit­nessed the ar­rival on Uran­tia of the first Sa­ta­nia scout­ing party sent out from Je­ru­sem to ex­am­ine the planet and make a re­port on its adap­ta­tion for a life-ex­per­i­ment sta­tion. This com­mis­sion con­sisted of twenty-four mem­bers, em­brac­ing Life Car­ri­ers, La­non­an­dek Sons, Mel­chiz­e­deks, ser­a­phim, and other or­ders of ce­les­tial life hav­ing to do with the early days of plan­e­tary or­ga­ni­za­tion and ad­min­is­tra­tion.

57:8.8Af­ter mak­ing a painstak­ing sur­vey of the planet, this com­mis­sion re­turned to Je­ru­sem and re­ported fa­vor­ably to the Sys­tem Sov­er­eign, rec­om­mend­ing that Uran­tia be placed on the life-ex­per­i­ment reg­istry. Your world was ac­cord­ingly reg­is­tered on Je­ru­sem as a dec­i­mal planet, and the Life Car­ri­ers were no­ti­fied that they would be granted per­mis­sion to in­sti­tute new pat­terns of me­chan­i­cal, chem­i­cal, and elec­tri­cal mo­bi­liza­tion at the time of their sub­se­quent ar­rival with life trans­plan­ta­tion and im­plan­ta­tion man­dates.

57:8.9In due course ar­range­ments for the plan­e­tary oc­cu­pa­tion were com­pleted by the mixed com­mis­sion of twelve on Je­ru­sem and ap­proved by the plan­e­tary com­mis­sion of sev­enty on Eden­tia. These plans, pro­posed by the ad­vi­sory coun­selors of the Life Car­ri­ers, were fi­nally ac­cepted on Sal­ving­ton. Soon there­after the Neb­a­don broad­casts car­ried the an­nounce­ment that Uran­tia would be­come the stage whereon the Life Car­ri­ers would ex­e­cute their six­ti­eth Sa­ta­nia ex­per­i­ment de­signed to am­plify and im­prove the Sa­ta­nia type of the Neb­a­don life pat­terns.

57:8.10Shortly af­ter Uran­tia was first rec­og­nized on the uni­verse broad­casts to all Neb­a­don, it was ac­corded full uni­verse sta­tus. Soon there­after it was reg­is­tered in the rec­ords of the mi­nor and the ma­jor sec­tor head­quar­ters plan­ets of the super­uni­verse; and be­fore this age was over, Uran­tia had found en­try on the plan­e­tary-life reg­istry of Uversa.

57:8.11This en­tire age was char­ac­ter­ized by fre­quent and vi­o­lent storms. The early crust of the earth was in a state of con­tin­ual flux. Sur­face cool­ing al­ter­nated with im­mense lava flows. Nowhere can there be found on the sur­face of the world any­thing of this orig­i­nal plan­e­tary crust. It has all been mixed up too many times with ex­trud­ing lavas of deep ori­gins and ad­mixed with sub­se­quent de­posits of the early world-wide ocean.

57:8.12–15 · four paragraphs not cited here ·

57:8.12Nowhere on the sur­face of the world will there be found more of the mod­i­fied rem­nants of these an­cient pre­o­cean rocks than in north­east­ern Canada around Hud­son Bay. This ex­ten­sive gran­ite el­e­va­tion is com­posed of stone be­long­ing to the pre­o­ceanic ages. These rock lay­ers have been heated, bent, twisted, up­crum­pled, and again and again have they passed through these dis­tort­ing meta­mor­phic ex­pe­ri­ences.

57:8.13Through­out the oceanic ages, enor­mous lay­ers of fos­sil-free strat­i­fied stone were de­posited on this an­cient ocean bot­tom. (Lime­stone can form as a re­sult of chem­i­cal pre­cip­i­ta­tion; not all of the older lime­stone was pro­duced by ma­rine-life de­po­si­tion.) In none of these an­cient rock for­ma­tions will there be found ev­i­dences of life; they con­tain no fos­sils un­less, by some chance, later de­posits of the wa­ter ages have be­come mixed with these older pre­life lay­ers.

57:8.14The earth’s early crust was highly un­sta­ble, but moun­tains were not in pro­cess of for­ma­tion. The planet con­tracted un­der grav­ity pres­sure as it formed. Moun­tains are not the re­sult of the col­lapse of the cool­ing crust of a con­tract­ing sphere; they ap­pear later on as a re­sult of the ac­tion of rain, grav­ity, and ero­sion.

57:8.15The con­ti­nen­tal land mass of this era in­creased un­til it cov­ered al­most ten per cent of the earth’s sur­face. Se­vere earth­quakes did not be­gin un­til the con­ti­nen­tal mass of land emerged well above the wa­ter. When they once be­gan, they in­creased in fre­quency and sever­ity for ages. For mil­lions upon mil­lions of years earth­quakes have di­min­ished, but Uran­tia still has an av­er­age of fif­teen daily.

57:8.16850,000,000 years ago the first real epoch of the sta­bi­liza­tion of the earth’s crust be­gan. Most of the heav­ier met­als had set­tled down to­ward the cen­ter of the globe; the cool­ing crust had ceased to cave in on such an ex­ten­sive scale as in for­mer ages. There was es­tab­lished a bet­ter bal­ance be­tween the land ex­tru­sion and the heav­ier ocean bed. The flow of the sub­crustal lava bed be­came well-nigh world-wide, and this com­pen­sated and sta­bi­lized the fluc­tu­a­tions due to cool­ing, con­tract­ing, and su­per­fi­cial shift­ing.

57:8.17 · one paragraph not cited here ·

57:8.17Vol­canic erup­tions and earth­quakes con­tin­ued to di­min­ish in fre­quency and sever­ity. The at­mo­sphere was clear­ing of vol­canic gases and wa­ter va­por, but the per­cent­age of car­bon diox­ide was still high.

57:8.18Elec­tric dis­tur­bances in the air and in the earth were also de­creas­ing. The lava flows had brought to the sur­face a mix­ture of el­e­ments which di­ver­si­fied the crust and bet­ter in­su­lated the planet from cer­tain space-en­er­gies. And all of this did much to fa­cil­i­tate the con­trol of ter­res­trial en­ergy and to reg­u­late its flow, as is dis­closed by the func­tion­ing of the mag­netic poles.

58:5.2The outer one thou­sand miles of the earth’s mass con­sists prin­ci­pally of dif­fer­ent kinds of rock. Un­der­neath are the denser and heav­ier metal­lic el­e­ments. Through­out the early and preat­mo­spheric ages the world was so nearly fluid in its molten and highly heated state that the heav­ier met­als sank deep into the in­te­rior. Those found near the sur­face to­day rep­re­sent the ex­u­date of an­cient vol­ca­noes, later and ex­ten­sive lava flows, and the more re­cent me­te­oric de­posits.

58:5.3–4 · two paragraphs not cited here ·

58:5.3The outer crust was about forty miles thick. This outer shell was sup­ported by, and rested di­rectly upon, a molten sea of basalt of vary­ing thick­ness, a mo­bile layer of molten lava held un­der high pres­sure but al­ways tend­ing to flow hither and yon in equal­iza­tion of shift­ing plan­e­tary pres­sures, thereby tend­ing to sta­bi­lize the earth’s crust.

58:5.4Even to­day the con­ti­nents con­tinue to float upon this non­crys­tal­lized cush­iony sea of molten basalt. Were it not for this pro­tec­tive con­di­tion, the more se­vere earth­quakes would lit­er­ally shake the world to pieces. Earth­quakes are caused by slid­ing and shift­ing of the solid outer crust and not by vol­ca­noes.

58:5.5The lava lay­ers of the earth’s crust, when cooled, form gran­ite. The av­er­age den­sity of Uran­tia is a lit­tle more than five and one-half times that of wa­ter; the den­sity of gran­ite is less than three times that of wa­ter. The earth’s core is twelve times as dense as wa­ter.

59:2.5330,000,000 years ago marks the be­gin­ning of a time sec­tor of com­par­a­tive quiet all over the world, with much land again above wa­ter. The only ex­cep­tion to this reign of ter­res­trial quiet was the erup­tion of the great North Amer­i­can vol­cano of east­ern Ken­tucky, one of the great­est sin­gle vol­canic ac­tiv­i­ties the world has ever known. The ashes of this vol­cano cov­ered five hun­dred square miles to a depth of from fif­teen to twenty feet.

59:3.2No fire rocks or lava are found in the stone lay­ers of this pe­riod ex­cept those of the great vol­ca­noes of south­ern Eu­rope and east­ern Maine and the lava flows of Que­bec. Vol­canic ac­tion was largely past. This was the height of great wa­ter de­po­si­tion; there was lit­tle or no moun­tain build­ing.

59:3.3–5 · three paragraphs not cited here ·

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.

59:3.4It is in the de­posits of this age that much of the gas, oil, zinc, and lead are found, the gas and oil be­ing de­rived from the enor­mous col­lec­tions of veg­etable and an­i­mal mat­ter car­ried down at the time of the pre­vi­ous land sub­mer­gence, while the min­eral de­posits rep­re­sent the sed­i­men­ta­tion of slug­gish bod­ies of wa­ter. Many of the rock salt de­posits be­long to this pe­riod.

59:3.5The trilo­bites rapidly de­clined, and the cen­ter of the stage was oc­cu­pied by the larger mol­lusks, or ceph­a­lop­ods. These an­i­mals grew to be fif­teen feet long and one foot in di­am­e­ter and be­came mas­ters of the seas. This species of an­i­mal ap­peared sud­denly and as­sumed dom­i­nance of sea life.

59:3.6The great vol­canic ac­tiv­ity of this age was in the Eu­ro­pean sec­tor. Not in mil­lions upon mil­lions of years had such vi­o­lent and ex­ten­sive vol­canic erup­tions oc­curred as now took place around the Med­i­ter­ra­nean trough and es­pe­cially in the neigh­bor­hood of the British Isles. This lava flow over the British Isles re­gion to­day ap­pears as al­ter­nate lay­ers of lava and rock 25,000 feet thick. These rocks were laid down by the in­ter­mit­tent lava flows which spread out over a shal­low sea bed, thus in­ter­spers­ing the rock de­posits, and all of this was sub­se­quently el­e­vated high above the sea. Vi­o­lent earth­quakes took place in north­ern Eu­rope, no­tably in Scot­land.

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.

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.

60:1.3These de­posits vary in thick­ness from 3,000 to 10,000 feet, even be­ing 18,000 on the Pa­cific coast. Lava was later forced in be­tween many of these lay­ers. The Pal­isades of the Hud­son River were formed by the ex­tru­sion of basalt lava be­tween these Tri­as­sic strata. Vol­canic ac­tion was ex­ten­sive in dif­fer­ent parts of the world.

60:3.1The great Cre­ta­ceous pe­riod de­rives its name from the pre­dom­i­nance of the pro­lific chalk-mak­ing foraminifers in the seas. This pe­riod brings Uran­tia to near the end of the long rep­til­ian dom­i­nance and wit­nesses the ap­pear­ance of flow­er­ing plants and bird life on land. These are also the times of the ter­mi­na­tion of the west­ward and south­ward drift of the con­ti­nents, ac­com­pa­nied by tremen­dous crustal de­for­ma­tions and con­comi­tant wide­spread lava flows and great vol­canic ac­tiv­i­ties.

60:3.2–5 · four paragraphs not cited here ·

60:3.2Near the close of the pre­ced­ing ge­o­logic pe­riod much of the con­ti­nen­tal land was up above wa­ter, al­though as yet there were no moun­tain peaks. But as the con­ti­nen­tal land drift con­tin­ued, it met with the first great ob­struc­tion on the deep floor of the Pa­cific. This con­tention of ge­o­logic forces gave im­pe­tus to the for­ma­tion of the whole vast north and south moun­tain range ex­tend­ing from Alaska down through Mex­ico to Cape Horn.

60:3.3This pe­riod thus be­comes the mod­ern moun­tain-build­ing stage of ge­o­logic his­tory. Prior to this time there were few moun­tain peaks, merely el­e­vated land ridges of great width. Now the Pa­cific coast range was be­gin­ning to el­e­vate, but it was lo­cated seven hun­dred miles west of the pres­ent shore line. The Sier­ras were be­gin­ning to form, their gold-bear­ing quartz strata be­ing the prod­uct of lava flows of this epoch. In the east­ern part of North Amer­ica, At­lantic sea pres­sure was also work­ing to cause land el­e­va­tion.

60:3.4100,000,000 years ago the North Amer­i­can con­ti­nent and a part of Eu­rope were well above wa­ter. The warp­ing of the Amer­i­can con­ti­nents con­tin­ued, re­sult­ing in the meta­mor­phos­ing of the South Amer­i­can An­des and in the grad­ual el­e­va­tion of the west­ern plains of North Amer­ica. Most of Mex­ico sank be­neath the sea, and the south­ern At­lantic en­croached on the east­ern coast of South Amer­ica, even­tu­ally reach­ing the pres­ent shore line. The At­lantic and In­dian Oceans were then about as they are to­day.

60:3.595,000,000 years ago the Amer­i­can and Eu­ro­pean land masses again be­gan to sink. The south­ern seas com­menced the in­va­sion of North Amer­ica and grad­u­ally ex­tended north­ward to con­nect with the Arc­tic Ocean, con­sti­tut­ing the sec­ond great­est sub­mer­gence of the con­ti­nent. When this sea fi­nally with­drew, it left the con­ti­nent about as it now is. Be­fore this great sub­mer­gence be­gan, the east­ern Ap­palachian high­lands had been al­most com­pletely worn down to the wa­ter’s level. The many col­ored lay­ers of pure clay now used for the man­u­fac­ture of earth­en­ware were laid down over the At­lantic coast re­gions dur­ing this age, their av­er­age thick­ness be­ing about 2,000 feet.

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.

60:3.7–10 · four paragraphs not cited here ·

60:3.790,000,000 years ago the an­giosperms emerged from these early Cre­ta­ceous seas and soon over­ran the con­ti­nents. These land plants sud­denly ap­peared along with fig trees, mag­no­lias, and tulip trees. Soon af­ter this time fig trees, bread­fruit trees, and palms over­spread Eu­rope and the west­ern plains of North Amer­ica. No new land an­i­mals ap­peared.

60:3.885,000,000 years ago the Bering Strait closed, shut­ting off the cool­ing wa­ters of the north­ern seas. Thereto­fore the ma­rine life of the At­lantic-Gulf wa­ters and that of the Pa­cific Ocean had dif­fered greatly, ow­ing to the tem­per­a­ture vari­a­tions of these two bod­ies of wa­ter, which now be­came uni­form.

60:3.9The de­posits of chalk and green­sand marl give name to this pe­riod. The sed­i­men­ta­tions of these times are var­ie­gated, con­sist­ing of chalk, shale, sand­stone, and small amounts of lime­stone, to­gether with in­fe­rior coal or lig­nite, and in many re­gions they con­tain oil. These lay­ers vary in thick­ness from 200 feet in some places to 10,000 feet in west­ern North Amer­ica and nu­mer­ous Eu­ro­pean lo­cal­i­ties. Along the east­ern bor­ders of the Rocky Moun­tains these de­posits may be ob­served in the up­tilted foothills.

60:3.10All over the world these strata are per­me­ated with chalk, and these lay­ers of porous semirock pick up wa­ter at up­turned out­crops and con­vey it down­ward to fur­nish the wa­ter sup­ply of much of the earth’s pres­ent arid re­gions.

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.

60:3.1665,000,000 years ago there oc­curred one of the great­est lava flows of all time. The de­po­si­tion lay­ers of these and pre­ced­ing lava flows are to be found all over the Amer­i­cas, North and South Africa, Aus­tralia, and parts of Eu­rope.

61:1.1140,000,000 years ago the land ar­eas of the North­ern Hemi­sphere be­gan to el­e­vate, and this was fol­lowed by new ex­ten­sive land de­posits and other ter­res­trial ac­tiv­i­ties, in­clud­ing lava flows, warp­ing, lake for­ma­tion, and ero­sion.

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.

61:2.335,000,000 years ago marks the be­gin­ning of the age of pla­cen­tal-mam­malian world dom­i­na­tion. The south­ern land bridge was ex­ten­sive, re­con­nect­ing the then enor­mous Antarc­tic con­ti­nent with South Amer­ica, South Africa, and Aus­tralia. In spite of the mass­ing of land in high lat­i­tudes, the world cli­mate re­mained rel­a­tively mild be­cause of the enor­mous in­crease in the size of the tropic seas, nor was the land el­e­vated suf­fi­ciently to pro­duce glaciers. Ex­ten­sive lava flows oc­curred in Green­land and Ice­land, some coal be­ing de­posited be­tween these lay­ers.

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.

61:4.1This is the pe­riod of preglacial land el­e­va­tion in North Amer­ica, Eu­rope, and Asia. The land was greatly al­tered in to­pog­ra­phy. Moun­tain ranges were born, streams changed their courses, and iso­lated vol­ca­noes broke out all over the world.

88:1.1Prim­i­tive man al­ways wanted to make any­thing ex­traor­di­nary into a fe­tish; chance there­fore gave ori­gin to many. A man is sick, some­thing hap­pens, and he gets well. The same thing is true of the rep­u­ta­tion of many medicines and the chance meth­ods of treat­ing dis­ease. Ob­jects con­nected with dreams were likely to be con­verted into fe­tishes. Vol­ca­noes, but not moun­tains, be­came fe­tishes; comets, but not stars. Early man re­garded shoot­ing stars and me­te­ors as in­di­cat­ing the ar­rival on earth of spe­cial vis­it­ing spir­its.

96:1.31. Yah­weh was the god of the south­ern Pales­tinian tribes, who as­so­ci­ated this con­cept of de­ity with Mount Ho­reb, the Sinai vol­cano. Yah­weh was merely one of the hun­dreds and thou­sands of na­ture gods which held the at­ten­tion and claimed the wor­ship of the Semitic tribes and peo­ples.

96:1.4–10 · seven paragraphs not cited here ·

96:1.42. El Elyon. For cen­turies af­ter Mel­chiz­e­dek’s so­journ at Salem his doc­trine of De­ity per­sisted in var­i­ous ver­sions but was gen­er­ally con­noted by the term El Elyon, the Most High God of heaven. Many Semites, in­clud­ing the im­me­di­ate de­scen­dants of Abra­ham, at var­i­ous times wor­shiped both Yah­weh and El Elyon.

96:1.53. El Shad­dai. It is dif­fi­cult to ex­plain what El Shad­dai stood for. This idea of God was a com­pos­ite de­rived from the teach­ings of Amen­emope’s Book of Wis­dom mod­i­fied by Ikh­na­ton’s doc­trine of Aton and fur­ther in­flu­enced by Mel­chiz­e­dek’s teach­ings em­bod­ied in the con­cept of El Elyon. But as the con­cept of El Shad­dai per­me­ated the He­brew mind, it be­came thor­oughly col­ored with the Yah­weh be­liefs of the desert.

96:1.6One of the dom­i­nant ideas of the re­li­gion of this era was the Egyp­tian con­cept of di­vine Prov­i­dence, the teach­ing that ma­te­rial pros­per­ity was a re­ward for serv­ing El Shad­dai.

96:1.74. El. Amid all this con­fu­sion of ter­mi­nol­ogy and hazi­ness of con­cept, many de­vout be­liev­ers sin­cerely en­deav­ored to wor­ship all of these evolv­ing ideas of di­vin­ity, and there grew up the prac­tice of re­fer­ring to this com­pos­ite De­ity as El. And this term in­cluded still other of the Bed­ouin na­ture gods.

96:1.85. Elo­him. In Kish and Ur there long per­sisted Sume­rian-Chaldean groups who taught a three-in-one God con­cept founded on the tra­di­tions of the days of Adam and Mel­chiz­e­dek. This doc­trine was car­ried to Egypt, where this Trin­ity was wor­shiped un­der the name of Elo­him, or in the sin­gu­lar as Eloah. The philo­sophic cir­cles of Egypt and later Alexan­drian teach­ers of He­braic ex­trac­tion taught this unity of plu­ral­is­tic Gods, and many of Moses’ ad­vis­ers at the time of the ex­o­dus be­lieved in this Trin­ity. But the con­cept of the trini­tar­ian Elo­him never be­came a real part of He­brew the­ol­ogy un­til af­ter they had come un­der the po­lit­i­cal in­flu­ence of the Baby­lo­ni­ans.

96:1.96. Sundry names. The Semites dis­liked to speak the name of their De­ity, and they there­fore re­sorted to nu­mer­ous ap­pel­la­tions from time to time, such as: The Spirit of God, The Lord, The An­gel of the Lord, The Al­mighty, The Holy One, The Most High, Adonai, The An­cient of Days, The Lord God of Is­rael, The Cre­ator of Heaven and Earth, Kyrios, Jah, The Lord of Hosts, and The Fa­ther in Heaven.

96:1.10Je­ho­vah is a term which in re­cent times has been em­ployed to des­ig­nate the com­pleted con­cept of Yah­weh which fi­nally evolved in the long He­brew ex­pe­ri­ence. But the name Je­ho­vah did not come into use un­til fif­teen hun­dred years af­ter the times of Je­sus.

96:1.11Up to about 2000 B.C., Mount Sinai was in­ter­mit­tently ac­tive as a vol­cano, oc­ca­sional erup­tions oc­cur­ring as late as the time of the so­journ of the Is­raelites in this re­gion. The fire and smoke, to­gether with the thun­der­ous det­o­na­tions as­so­ci­ated with the erup­tions of this vol­canic moun­tain, all im­pressed and awed the Bed­ou­ins of the sur­round­ing re­gions and caused them greatly to fear Yah­weh. This spirit of Mount Ho­reb later be­came the god of the He­brew Semites, and they even­tu­ally be­lieved him to be su­preme over all other gods.

96:4.5It does not ap­pear that Moses would ever have suc­ceeded in the es­tab­lish­ment of his some­what ad­vanced cer­e­mo­nial wor­ship and in keep­ing his fol­low­ers in­tact for a quar­ter of a cen­tury had it not been for the vi­o­lent erup­tion of Ho­reb dur­ing the third week of their wor­ship­ful so­journ at its base. “The moun­tain of Yah­weh was con­sumed in fire, and the smoke as­cended like the smoke of a fur­nace, and the whole moun­tain quaked greatly.” In view of this cat­a­clysm it is not sur­pris­ing that Moses could im­press upon his breth­ren the teach­ing that their God was “mighty, ter­ri­ble, a de­vour­ing fire, fear­ful, and all-pow­er­ful.”

Onward

Cited alongside: Europe, Asia, South America, Urantia, Greenland, Mount Sinai, Yahweh, Africa