The Urantia Book

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continents

47 paragraphs · about 14 minutes

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

57:8.11,000,000,000 years ago is the date of the ac­tual be­gin­ning of Uran­tia his­tory. The planet had at­tained ap­prox­i­mately its pres­ent size. And about this time it was placed upon the phys­i­cal reg­istries of Neb­a­don and given its name, Uran­tia.

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.

57:8.3The 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.

57:8.12Nowhere 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.

57:8.17Vol­canic 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.

57:8.19800,000,000 years ago wit­nessed the in­au­gu­ra­tion of the first great land epoch, the age of in­creased con­ti­nen­tal emer­gence.

57:8.20Since the con­den­sa­tion of the earth’s hy­dro­sphere, first into the world ocean and sub­se­quently into the Pa­cific Ocean, this lat­ter body of wa­ter should be vi­su­al­ized as then cov­er­ing nine tenths of the earth’s sur­face. Me­te­ors falling into the sea ac­cu­mu­lated on the ocean bot­tom, and me­te­ors are, gen­er­ally speak­ing, com­posed of heavy ma­te­ri­als. Those falling on the land were largely ox­i­dized, sub­se­quently worn down by ero­sion, and washed into the ocean basins. Thus the ocean bot­tom grew in­creas­ingly heavy, and added to this was the weight of a body of wa­ter at some places ten miles deep.

57:8.21The in­creas­ing down­thrust of the Pa­cific Ocean op­er­ated fur­ther to up­thrust the con­ti­nen­tal land mass. Eu­rope and Africa be­gan to rise out of the Pa­cific depths along with those masses now called Aus­tralia, North and South Amer­ica, and the con­ti­nent of Antarc­tica, while the bed of the Pa­cific Ocean en­gaged in a fur­ther com­pen­satory sink­ing ad­just­ment. By the end of this pe­riod al­most one third of the earth’s sur­face con­sisted of land, all in one con­ti­nen­tal body.

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.

57:8.23750,000,000 years ago the first breaks in the con­ti­nen­tal land mass be­gan as the great north-and-south crack­ing, which later ad­mit­ted the ocean wa­ters and pre­pared the way for the west­ward drift of the con­ti­nents of North and South Amer­ica, in­clud­ing Green­land. The long east-and-west cleav­age sep­a­rated Africa from Eu­rope and sev­ered the land masses of Aus­tralia, the Pa­cific Is­lands, and Antarc­tica from the Asi­atic con­ti­nent.

57:8.24700,000,000 years ago Uran­tia was ap­proach­ing the ripen­ing of con­di­tions suit­able for the sup­port of life. The con­ti­nen­tal land drift con­tin­ued; in­creas­ingly the ocean pen­e­trated the land as long fin­ger­like seas pro­vid­ing those shal­low wa­ters and shel­tered bays which are so suit­able as a habi­tat for ma­rine life.

57:8.25650,000,000 years ago wit­nessed the fur­ther sep­a­ra­tion of the land masses and, in con­se­quence, a fur­ther ex­ten­sion of the con­ti­nen­tal seas. And these wa­ters were rapidly at­tain­ing that de­gree of salti­ness which was es­sen­tial to Uran­tia life.

57:8.26It was these seas and their suc­ces­sors that laid down the life rec­ords of Uran­tia, as sub­se­quently dis­cov­ered in well-pre­served stone pages, vol­ume upon vol­ume, as era suc­ceeded era and age grew upon age. These in­land seas of olden times were truly the cra­dle of evo­lu­tion.

57:8.27[Pre­sented by a Life Car­rier, a mem­ber of the orig­i­nal Uran­tia Corps and now a res­i­dent ob­server.]

58:4.3500,000,000 years ago prim­i­tive ma­rine veg­etable life was well es­tab­lished on Uran­tia. Green­land and the arc­tic land mass, to­gether with North and South Amer­ica, were be­gin­ning their long and slow west­ward drift. Africa moved slightly south, cre­at­ing an east and west trough, the Med­i­ter­ra­nean basin, be­tween it­self and the mother body. Antarc­tica, Aus­tralia, and the land in­di­cated by the is­lands of the Pa­cific broke away on the south and east and have drifted far away since that day.

58:4.4We had planted the prim­i­tive form of ma­rine life in the shel­tered tropic bays of the cen­tral seas of the east-west cleav­age of the break­ing-up con­ti­nen­tal land mass. Our pur­pose in mak­ing three ma­rine-life im­plan­ta­tions was to in­sure that each great land mass would carry this life with it, in its warm-wa­ter seas, as the land sub­se­quently sep­a­rated. We fore­saw that in the later era of the emer­gence of land life large oceans of wa­ter would sep­a­rate these drift­ing con­ti­nen­tal land masses.

58:5.1The con­ti­nen­tal land drift con­tin­ued. The earth’s core had be­come as dense and rigid as steel, be­ing sub­jected to a pres­sure of al­most 25,000 tons to the square inch, and ow­ing to the enor­mous grav­ity pres­sure, it was and still is very hot in the deep in­te­rior. The tem­per­a­ture in­creases from the sur­face down­ward un­til at the cen­ter it is slightly above the sur­face tem­per­a­ture of the sun.

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.

58:5.3The 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.

58:5.6The sea bot­toms are more dense than the land masses, and this is what keeps the con­ti­nents above wa­ter. When the sea bot­toms are ex­truded above the sea level, they are found to con­sist largely of basalt, a form of lava con­sid­er­ably heav­ier than the gran­ite of the land masses. Again, if the con­ti­nents were not lighter than the ocean beds, grav­ity would draw the edges of the oceans up onto the land, but such phe­nom­ena are not ob­serv­able.

58:5.7The weight of the oceans is also a fac­tor in the in­crease of pres­sure on the sea beds. The lower but com­par­a­tively heav­ier ocean beds, plus the weight of the over­ly­ing wa­ter, ap­prox­i­mate the weight of the higher but much lighter con­ti­nents. But all con­ti­nents tend to creep into the oceans. The con­ti­nen­tal pres­sure at ocean-bot­tom lev­els is about 20,000 pounds to the square inch. That is, this would be the pres­sure of a con­ti­nen­tal mass stand­ing 15,000 feet above the ocean floor. The ocean-floor wa­ter pres­sure is only about 5,000 pounds to the square inch. These dif­fer­en­tial pres­sures tend to cause the con­ti­nents to slide to­ward the ocean beds.

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.

59:1.7Within a few mil­lion years the Pa­cific Ocean be­gan to in­vade the Amer­i­can con­ti­nents. The sink­ing of the land was prin­ci­pally due to crustal ad­just­ment, al­though the lat­eral land spread, or con­ti­nen­tal creep, was also a fac­tor.

59:4.1In the age­long strug­gle be­tween land and wa­ter, for long pe­ri­ods the sea has been com­par­a­tively vic­to­ri­ous, but times of land vic­tory are just ahead. And the con­ti­nen­tal drifts have not pro­ceeded so far but that, at times, prac­ti­cally all of the land of the world is con­nected by slen­der isth­muses and nar­row land bridges.

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.

60:3.2Near 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.

60:3.3–10 · eight paragraphs not cited here ·

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.

60:3.790,000,000 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.

60:3.1275,000,000 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.

60:4.1The great Cre­ta­ceous pe­riod was draw­ing to a close, and its ter­mi­na­tion marks the end of the great sea in­va­sions of the con­ti­nents. Par­tic­u­larly is this true of North Amer­ica, where there had been just twenty-four great in­un­da­tions. And though there were sub­se­quent mi­nor sub­mer­gences, none of these can be com­pared with the ex­ten­sive and lengthy ma­rine in­va­sions of this and pre­vi­ous ages. These al­ter­nate pe­ri­ods of land and sea dom­i­nance have oc­curred in mil­lion-year cy­cles. There has been an age­long rhythm as­so­ci­ated with this rise and fall of ocean floor and con­ti­nen­tal land lev­els. And these same rhyth­mi­cal crustal move­ments will con­tinue from this time on through­out the earth’s his­tory but with di­min­ish­ing fre­quency and ex­tent.

60:4.2This pe­riod also wit­nesses the end of the con­ti­nen­tal drift and the build­ing of the mod­ern moun­tains of Uran­tia. But the pres­sure of the con­ti­nen­tal masses and the thwarted mo­men­tum of their age­long drift are not the ex­clu­sive in­flu­ences in moun­tain build­ing. The chief and un­der­ly­ing fac­tor in de­ter­min­ing the lo­ca­tion of a moun­tain range is the pre-ex­is­tent low­land, or trough, which has be­come filled up with the com­par­a­tively lighter de­posits of the land ero­sion and ma­rine drifts of the pre­ced­ing ages. These lighter ar­eas of land are some­times 15,000 to 20,000 feet thick; there­fore, when the crust is sub­jected to pres­sure from any cause, these lighter ar­eas are the first to crum­ple up, fold, and rise up­ward to af­ford com­pen­satory ad­just­ment for the con­tend­ing and con­flict­ing forces and pres­sures at work in the earth’s crust or un­der­neath the crust. Some­times these up­thrusts of land oc­cur with­out fold­ing. But in con­nec­tion with the rise of the Rocky Moun­tains, great fold­ing and tilt­ing oc­curred, cou­pled with enor­mous over­thrusts of the var­i­ous lay­ers, both un­der­ground and at the sur­face.

Onward

Cited alongside: Rocky Mountains, Europe, oceans, Urantia, evolution, mountains, North America, South America