Difference between revisions of "57:8 Crustal Stabilization-The Age of Earthquakes-The World Ocean and The First Continent"

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57:8.1 1,000,000,000 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]].
 
57:8.1 1,000,000,000 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]].
  
57:8.2 The [[atmosphere]], [[together]] with incessant moisture [[precipitation]], [[facilitated]] the cooling of the [http://en.wikipedia.org/wiki/Earth%27s_crust earth's crust]. [http://en.wikipedia.org/wiki/Volcano Volcanic] action early [[equalized]] internal-[[heat]] [[pressure]] and crustal contraction; and as volcanoes rapidly decreased, [http://en.wikipedia.org/wiki/Earthquakes earthquakes] made their [[appearance]] as this [[epoch]] of crustal cooling and [[adjustment]] [[progressed]].
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57:8.2 The [[atmosphere]], [[together]] with incessant moisture [[precipitation]], [[facilitated]] the cooling of the [https://en.wikipedia.org/wiki/Earth%27s_crust earth's crust]. [https://en.wikipedia.org/wiki/Volcano Volcanic] action early [[equalized]] internal-[[heat]] [[pressure]] and crustal contraction; and as volcanoes rapidly decreased, [https://en.wikipedia.org/wiki/Earthquakes earthquakes] made their [[appearance]] as this [[epoch]] of crustal cooling and [[adjustment]] [[progressed]].
  
57:8.3 The real [[geologic]] [[history]] of [[Urantia]] begins with the cooling of the [http://en.wikipedia.org/wiki/Earth%27s_crust 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 [http://en.wikipedia.org/wiki/Salt_water salty]; it was practically a [http://en.wikipedia.org/wiki/Fresh_water fresh-water] covering for the world. In those days, most of the [http://en.wikipedia.org/wiki/Chlorine chlorine] was combined with various metals, but there was enough, in [[union]] with [http://en.wikipedia.org/wiki/Hydrogen hydrogen], to render this [[water]] faintly acid.
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57:8.3 The real [[geologic]] [[history]] of [[Urantia]] begins with the cooling of the [https://en.wikipedia.org/wiki/Earth%27s_crust 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 [https://en.wikipedia.org/wiki/Salt_water salty]; it was practically a [https://en.wikipedia.org/wiki/Fresh_water fresh-water] covering for the world. In those days, most of the [https://en.wikipedia.org/wiki/Chlorine chlorine] was combined with various metals, but there was enough, in [[union]] with [https://en.wikipedia.org/wiki/Hydrogen hydrogen], to render this [[water]] faintly acid.
  
57:8.4 At the opening of this faraway era, [[Urantia]] should be envisaged as a [[water]]-bound planet. Later on, deeper and hence denser [http://en.wikipedia.org/wiki/Lava lava] flows came out upon the bottom of the present [http://en.wikipedia.org/wiki/Pacific_Ocean 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 [http://en.wikipedia.org/wiki/Earth%27s_crust earth's crust].
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57:8.4 At the opening of this faraway era, [[Urantia]] should be envisaged as a [[water]]-bound planet. Later on, deeper and hence denser [https://en.wikipedia.org/wiki/Lava lava] flows came out upon the bottom of the present [https://en.wikipedia.org/wiki/Pacific_Ocean 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 [https://en.wikipedia.org/wiki/Earth%27s_crust earth's crust].
  
57:8.5 950,000,000 years ago [[Urantia]] presents the picture of [http://en.wikipedia.org/wiki/Pangaea one great continent] of [[land]] and one large body of [[water]], the [http://en.wikipedia.org/wiki/Pacific_Ocean Pacific Ocean]. [http://en.wikipedia.org/wiki/Volcanoes Volcanoes] are still widespread and [http://en.wikipedia.org/wiki/Earthquakes 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 [http://en.wikipedia.org/wiki/Carbon_dioxide carbon dioxide] continues large. The earth's crust is gradually [[stabilizing]].
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57:8.5 950,000,000 years ago [[Urantia]] presents the picture of [https://en.wikipedia.org/wiki/Pangaea one great continent] of [[land]] and one large body of [[water]], the [https://en.wikipedia.org/wiki/Pacific_Ocean Pacific Ocean]. [https://en.wikipedia.org/wiki/Volcanoes Volcanoes] are still widespread and [https://en.wikipedia.org/wiki/Earthquakes 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 [https://en.wikipedia.org/wiki/Carbon_dioxide carbon dioxide] continues large. The earth's crust is gradually [[stabilizing]].
  
 
57:8.6 It 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 [https://nordan.daynal.org/wiki/index.php?title=Paper_119#119:7._THE_SEVENTH_AND_FINAL_BESTOWAL mortal bestowal], would [[participate]] in those [[experiences]] which have since caused [[Urantia]] to become locally known as the "[https://nordan.daynal.org/wiki/index.php?title=Paper_188#188:4._MEANING_OF_THE_DEATH_ON_THE_CROSS world of the cross]."
 
57:8.6 It 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 [https://nordan.daynal.org/wiki/index.php?title=Paper_119#119:7._THE_SEVENTH_AND_FINAL_BESTOWAL mortal bestowal], would [[participate]] in those [[experiences]] which have since caused [[Urantia]] to become locally known as the "[https://nordan.daynal.org/wiki/index.php?title=Paper_188#188:4._MEANING_OF_THE_DEATH_ON_THE_CROSS world of the cross]."
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57:8.10 Shortly 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 [https://nordan.daynal.org/wiki/index.php?title=Paper_15#15:13._THE_SECTOR_GOVERNMENTS 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]].
 
57:8.10 Shortly 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 [https://nordan.daynal.org/wiki/index.php?title=Paper_15#15:13._THE_SECTOR_GOVERNMENTS 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]].
  
57:8.11 This entire [[age]] was characterized by frequent and [[violent]] [http://en.wikipedia.org/wiki/Storm storms]. The early [http://en.wikipedia.org/wiki/Earth_crust crust of the earth] was in a state of continual [[flux]]. [[Surface]] cooling alternated with immense [http://en.wikipedia.org/wiki/Lava lava] [[flows]]. Nowhere can there be found on the [[surface]] of the world anything of this [[original]] [http://en.wikipedia.org/wiki/Earth_crust 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]].
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57:8.11 This entire [[age]] was characterized by frequent and [[violent]] [https://en.wikipedia.org/wiki/Storm storms]. The early [https://en.wikipedia.org/wiki/Earth_crust crust of the earth] was in a state of continual [[flux]]. [[Surface]] cooling alternated with immense [https://en.wikipedia.org/wiki/Lava lava] [[flows]]. Nowhere can there be found on the [[surface]] of the world anything of this [[original]] [https://en.wikipedia.org/wiki/Earth_crust 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 Nowhere on the [[surface]] of the world will there be found more of the [[modified]] remnants of these ancient preocean [http://en.wikipedia.org/wiki/Rocks rocks] than in northeastern Canada around [http://en.wikipedia.org/wiki/Hudson_Bay Hudson Bay]. This extensive [http://en.wikipedia.org/wiki/Granite 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]].
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57:8.12 Nowhere on the [[surface]] of the world will there be found more of the [[modified]] remnants of these ancient preocean [https://en.wikipedia.org/wiki/Rocks rocks] than in northeastern Canada around [https://en.wikipedia.org/wiki/Hudson_Bay Hudson Bay]. This extensive [https://en.wikipedia.org/wiki/Granite 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]].
  
57:8.13 Throughout the [[ocean]]ic ages, enormous layers of [[fossil]]-free stratified stone were deposited on this ancient [[ocean]] bottom. ([http://en.wikipedia.org/wiki/Limestone 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.
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57:8.13 Throughout the [[ocean]]ic ages, enormous layers of [[fossil]]-free stratified stone were deposited on this ancient [[ocean]] bottom. ([https://en.wikipedia.org/wiki/Limestone 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.
  
57:8.14 The [[earth]]'s early [http://en.wikipedia.org/wiki/Earth_crust crust] was highly unstable, but [http://en.wikipedia.org/wiki/Mountains 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.
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57:8.14 The [[earth]]'s early [https://en.wikipedia.org/wiki/Earth_crust crust] was highly unstable, but [https://en.wikipedia.org/wiki/Mountains 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.
  
57:8.15 The [http://en.wikipedia.org/wiki/Pangea continental land mass] of this [[era]] increased until it covered almost ten per cent of the [[earth]]'s [[surface]]. Severe [http://en.wikipedia.org/wiki/Earthquakes 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 [http://en.wikipedia.org/wiki/Earthquakes earthquakes] have diminished, but [[Urantia]] still has an average of fifteen daily.
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57:8.15 The [https://en.wikipedia.org/wiki/Pangea continental land mass] of this [[era]] increased until it covered almost ten per cent of the [[earth]]'s [[surface]]. Severe [https://en.wikipedia.org/wiki/Earthquakes 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 [https://en.wikipedia.org/wiki/Earthquakes earthquakes] have diminished, but [[Urantia]] still has an average of fifteen daily.
  
57:8.16 850,000,000 years ago the first real [[epoch]] of the [[stabilization]] of the [http://en.wikipedia.org/wiki/Earth_crust 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 [http://en.wikipedia.org/wiki/Earth_crust subcrustal] lava bed became well-nigh world-wide, and this [[compensated]] and [[stabilized]] the fluctuations due to cooling, contracting, and superficial shifting.
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57:8.16 850,000,000 years ago the first real [[epoch]] of the [[stabilization]] of the [https://en.wikipedia.org/wiki/Earth_crust 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 [https://en.wikipedia.org/wiki/Earth_crust 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 [http://en.wikipedia.org/wiki/Volcanoes Volcanic] [[eruptions]] and [http://en.wikipedia.org/wiki/Earthquakes earthquakes] continued to diminish in [[frequency]] and severity. The [[atmosphere]] was clearing of volcanic [[gases]] and [[water]] vapor, but the percentage of [http://en.wikipedia.org/wiki/Carbon_dioxide carbon dioxide] was still high.
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57:8.17 [https://en.wikipedia.org/wiki/Volcanoes Volcanic] [[eruptions]] and [https://en.wikipedia.org/wiki/Earthquakes earthquakes] continued to diminish in [[frequency]] and severity. The [[atmosphere]] was clearing of volcanic [[gases]] and [[water]] vapor, but the percentage of [https://en.wikipedia.org/wiki/Carbon_dioxide carbon dioxide] was still high.
  
57:8.18 [[Electric]] disturbances in the [[air]] and in the [[earth]] were also decreasing. The [http://en.wikipedia.org/wiki/Lava 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 [http://en.wikipedia.org/wiki/Poles_of_astronomical_bodies magnetic poles].
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57:8.18 [[Electric]] disturbances in the [[air]] and in the [[earth]] were also decreasing. The [https://en.wikipedia.org/wiki/Lava 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 [https://en.wikipedia.org/wiki/Poles_of_astronomical_bodies magnetic poles].
  
 
57:8.19 800,000,000 years ago [[witnessed]] the [[inauguration]] of the first great [[land]] [[epoch]], the age of increased continental [[emergence]].
 
57:8.19 800,000,000 years ago [[witnessed]] the [[inauguration]] of the first great [[land]] [[epoch]], the age of increased continental [[emergence]].
  
57:8.20 Since the [[condensation]] of the [[earth]]'s hydrosphere, first into the world [[ocean]] and subsequently into the [http://en.wikipedia.org/wiki/Pacific_Ocean 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.
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57:8.20 Since the [[condensation]] of the [[earth]]'s hydrosphere, first into the world [[ocean]] and subsequently into the [https://en.wikipedia.org/wiki/Pacific_Ocean 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.
  
57:8.21 The increasing downthrust of the [http://en.wikipedia.org/wiki/Pacific_Ocean Pacific Ocean] operated further to upthrust the continental land mass. [http://en.wikipedia.org/wiki/Europe Europe] and [http://en.wikipedia.org/wiki/Africa Africa] began to rise out of the Pacific depths along with those masses now called [http://en.wikipedia.org/wiki/Australia Australia], [http://en.wikipedia.org/wiki/North_America North] and [http://en.wikipedia.org/wiki/South_America South America], and the continent of [http://en.wikipedia.org/wiki/Antarctica 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.
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57:8.21 The increasing downthrust of the [https://en.wikipedia.org/wiki/Pacific_Ocean Pacific Ocean] operated further to upthrust the continental land mass. [https://en.wikipedia.org/wiki/Europe Europe] and [https://en.wikipedia.org/wiki/Africa Africa] began to rise out of the Pacific depths along with those masses now called [https://en.wikipedia.org/wiki/Australia Australia], [https://en.wikipedia.org/wiki/North_America North] and [https://en.wikipedia.org/wiki/South_America South America], and the continent of [https://en.wikipedia.org/wiki/Antarctica 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.
  
57:8.22 With 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 [http://en.wikipedia.org/wiki/Ice_age ice age] would have arrived long before it did. It was several hundred millions of years before so much [[land]] again appeared above [[water]].
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57:8.22 With 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 [https://en.wikipedia.org/wiki/Ice_age ice age] would have arrived long before it did. It was several hundred millions of years before so much [[land]] again appeared above [[water]].
  
57:8.23 750,000,000 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 [http://en.wikipedia.org/wiki/North_America North] and [http://en.wikipedia.org/wiki/South_America South America], including [http://en.wikipedia.org/wiki/Greenland Greenland]. The long east-and-west cleavage separated [http://en.wikipedia.org/wiki/Africa Africa] from [http://en.wikipedia.org/wiki/Europe Europe] and severed the [[land]] masses of [http://en.wikipedia.org/wiki/Australia Australia], the [http://en.wikipedia.org/wiki/Pacific_islands Pacific Islands], and [http://en.wikipedia.org/wiki/Antarctica Antarctica] from the [http://en.wikipedia.org/wiki/Asia Asiatic] continent.
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57:8.23 750,000,000 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 [https://en.wikipedia.org/wiki/North_America North] and [https://en.wikipedia.org/wiki/South_America South America], including [https://en.wikipedia.org/wiki/Greenland Greenland]. The long east-and-west cleavage separated [https://en.wikipedia.org/wiki/Africa Africa] from [https://en.wikipedia.org/wiki/Europe Europe] and severed the [[land]] masses of [https://en.wikipedia.org/wiki/Australia Australia], the [https://en.wikipedia.org/wiki/Pacific_islands Pacific Islands], and [https://en.wikipedia.org/wiki/Antarctica Antarctica] from the [https://en.wikipedia.org/wiki/Asia Asiatic] continent.
  
57:8.24 700,000,000 years ago [[Urantia]] was approaching the ripening of conditions suitable for the [[support]] of life. The [http://en.wikipedia.org/wiki/Pangea#Rifting_and_break-up 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.
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57:8.24 700,000,000 years ago [[Urantia]] was approaching the ripening of conditions suitable for the [[support]] of life. The [https://en.wikipedia.org/wiki/Pangea#Rifting_and_break-up 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.
  
57:8.25 650,000,000 years ago [[witnessed]] the [https://nordan.daynal.org/wiki/index.php?title=File:Pangea_animation_03.gif 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 [http://en.wikipedia.org/wiki/Salinity saltiness] which was [[essential]] to [[Urantia]] life.
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57:8.25 650,000,000 years ago [[witnessed]] the [https://nordan.daynal.org/wiki/index.php?title=File:Pangea_animation_03.gif 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 [https://en.wikipedia.org/wiki/Salinity saltiness] which was [[essential]] to [[Urantia]] life.
  
57:8.26 It was these seas and their successors that laid down the life [[records]] of [[Urantia]], as subsequently [[discovered]] in [http://en.wikipedia.org/wiki/Geologic_record well-preserved stone pages],[https://nordan.daynal.org/wiki/index.php?title=Paper_58#58:7._THE_GEOLOGIC_HISTORY_BOOK] volume upon volume, as [[era]] succeeded era and [[age]] grew upon age. These inland seas of olden times were truly the [[cradle]] of [[evolution]].
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57:8.26 It was these seas and their successors that laid down the life [[records]] of [[Urantia]], as subsequently [[discovered]] in [https://en.wikipedia.org/wiki/Geologic_record well-preserved stone pages],[https://nordan.daynal.org/wiki/index.php?title=Paper_58#58:7._THE_GEOLOGIC_HISTORY_BOOK] 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]].][http://books.google.com/books?id=WNplY_v5TP4C&pg=PA228&dq=garden+of+edia&hl=en&ei=tgxfTbbOGJGcgQeQqfnVDQ&sa=X&oi=book_result&ct=result&resnum=1&sqi=2&ved=0CDsQ6AEwAA#v=onepage&q=urantia&f=false]
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57:8.27 [Presented by a [[Life Carrier]], a member of the original Urantia Corps and now a resident [[observer]].][https://books.google.com/books?id=WNplY_v5TP4C&pg=PA228&dq=garden+of+edia&hl=en&ei=tgxfTbbOGJGcgQeQqfnVDQ&sa=X&oi=book_result&ct=result&resnum=1&sqi=2&ved=0CDsQ6AEwAA#v=onepage&q=urantia&f=false]
  
 
<center>[https://nordan.daynal.org/wiki/index.php?title=Paper_57 Go to Paper 57]</center>
 
<center>[https://nordan.daynal.org/wiki/index.php?title=Paper_57 Go to Paper 57]</center>

Latest revision as of 23:38, 12 December 2020

Lighterstill.jpg

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57:8.1 1,000,000,000 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.

57:8.2 The 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 The 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.

57:8.4 At 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.

57:8.5 950,000,000 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.

57:8.6 It 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."

57:8.7 900,000,000 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.

57:8.8 After 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.

57:8.9 In 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.

57:8.10 Shortly 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.

57:8.11 This 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 Nowhere 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.

57:8.13 Throughout 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.

57:8.14 The 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.

57:8.15 The 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.

57:8.16 850,000,000 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 Volcanic 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.

57:8.18 Electric 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.

57:8.19 800,000,000 years ago witnessed the inauguration of the first great land epoch, the age of increased continental emergence.

57:8.20 Since 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.

57:8.21 The 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.

57:8.22 With 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.

57:8.23 750,000,000 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.

57:8.24 700,000,000 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.

57:8.25 650,000,000 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.

57:8.26 It was these seas and their successors that laid down the life records of Urantia, as subsequently discovered in well-preserved stone pages,[1] 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.][2]

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