Difference between revisions of "61:4 The Recent Continental-Elevation Stage-The Last Great Mammalian Migration"

From Nordan Symposia
Jump to navigationJump to search
m (Text replacement - "http://" to "https://")
 
(One intermediate revision by the same user not shown)
Line 1: Line 1:
 
[[File:lighterstill.jpg]][[File:The_eye_of_all_ur60.jpg|right|frame]]
 
[[File:lighterstill.jpg]][[File:The_eye_of_all_ur60.jpg|right|frame]]
  
61:4.1 This is the period of pre-[http://en.wikipedia.org/wiki/Glacier glacial] land elevation in [http://en.wikipedia.org/wiki/North_America North America], [http://en.wikipedia.org/wiki/Europe Europe], and [http://en.wikipedia.org/wiki/Asia Asia]. The land was greatly altered in [[topography]]. [[Mountain]] ranges were born, [[streams]] changed their [[courses]], and isolated [http://en.wikipedia.org/wiki/Volcanoes volcanoes] broke out all over the world.
+
61:4.1 This is the period of pre-[https://en.wikipedia.org/wiki/Glacier glacial] land elevation in [https://en.wikipedia.org/wiki/North_America North America], [https://en.wikipedia.org/wiki/Europe Europe], and [https://en.wikipedia.org/wiki/Asia Asia]. The land was greatly altered in [[topography]]. [[Mountain]] ranges were born, [[streams]] changed their [[courses]], and isolated [https://en.wikipedia.org/wiki/Volcanoes volcanoes] broke out all over the world.
  
61:4.2 10,000,000 years ago began an age of widespread local [[land]] deposits on the lowlands of the [http://en.wikipedia.org/wiki/Continents continents], but most of these sedimentations were later removed. Much of Europe, at this time, was still under [[water]], including parts of England, Belgium, and France, and the [[Mediterranean]] Sea covered much of northern Africa. In North America extensive depositions were made at the [[mountain]] bases, in [[lakes]], and in the great [[land]] basins. These deposits average only about two hundred feet, are more or less colored, and [[fossils]] are rare. Two great fresh-water [[lakes]] existed in western North America. The [http://en.wikipedia.org/wiki/Sierras Sierras] were elevating; [http://en.wikipedia.org/wiki/Mt._Shasta Shasta], [http://en.wikipedia.org/wiki/Mt._Hood Hood], and [http://en.wikipedia.org/wiki/Mt._Ranier Rainier] were beginning their [[mountain]] [[careers]]. But it was not until the subsequent [http://en.wikipedia.org/wiki/Ice_Age ice age] that North America began its creep toward the Atlantic depression.
+
61:4.2 10,000,000 years ago began an age of widespread local [[land]] deposits on the lowlands of the [https://en.wikipedia.org/wiki/Continents continents], but most of these sedimentations were later removed. Much of Europe, at this time, was still under [[water]], including parts of England, Belgium, and France, and the [[Mediterranean]] Sea covered much of northern Africa. In North America extensive depositions were made at the [[mountain]] bases, in [[lakes]], and in the great [[land]] basins. These deposits average only about two hundred feet, are more or less colored, and [[fossils]] are rare. Two great fresh-water [[lakes]] existed in western North America. The [https://en.wikipedia.org/wiki/Sierras Sierras] were elevating; [https://en.wikipedia.org/wiki/Mt._Shasta Shasta], [https://en.wikipedia.org/wiki/Mt._Hood Hood], and [https://en.wikipedia.org/wiki/Mt._Ranier Rainier] were beginning their [[mountain]] [[careers]]. But it was not until the subsequent [https://en.wikipedia.org/wiki/Ice_Age ice age] that North America began its creep toward the Atlantic depression.
  
61:4.3 For a short time all the [[land]] of the world was again joined excepting [http://en.wikipedia.org/wiki/Australia Australia], and the last great world-wide [[animal]] migration took place. [http://en.wikipedia.org/wiki/North_America North America] was connected with both [http://en.wikipedia.org/wiki/South_America South America] and [http://en.wikipedia.org/wiki/Asia Asia], and there was a free exchange of [[animal]] life. Asiatic sloths, armadillos, antelopes, and bears entered North America, while North American camels went to [http://en.wikipedia.org/wiki/China China]. Rhinoceroses migrated over the whole world except Australia and South America, but they were [[extinct]] in the [http://en.wikipedia.org/wiki/Western_Hemisphere Western Hemisphere] by the close of this period.
+
61:4.3 For a short time all the [[land]] of the world was again joined excepting [https://en.wikipedia.org/wiki/Australia Australia], and the last great world-wide [[animal]] migration took place. [https://en.wikipedia.org/wiki/North_America North America] was connected with both [https://en.wikipedia.org/wiki/South_America South America] and [https://en.wikipedia.org/wiki/Asia Asia], and there was a free exchange of [[animal]] life. Asiatic sloths, armadillos, antelopes, and bears entered North America, while North American camels went to [https://en.wikipedia.org/wiki/China China]. Rhinoceroses migrated over the whole world except Australia and South America, but they were [[extinct]] in the [https://en.wikipedia.org/wiki/Western_Hemisphere Western Hemisphere] by the close of this period.
  
61:4.4 In general, the life of the preceding period continued to [[evolve]] and spread. The [http://en.wikipedia.org/wiki/Cat cat] family [[dominated]] the [[animal]] life, and [[marine]] life was almost at a standstill. Many of the [http://en.wikipedia.org/wiki/Horses horses] were still three-toed, but the modern types were arriving; llamas and giraffelike camels mingled with the horses on the grazing plains. The [http://en.wikipedia.org/wiki/Giraffe giraffe] appeared in [http://en.wikipedia.org/wiki/Africa Africa], having just as long a neck then as now. In South America sloths, armadillos, anteaters, and the South American type of primitive [http://en.wikipedia.org/wiki/Monkeys monkeys] evolved. Before the [http://en.wikipedia.org/wiki/Continents continents] were finally [[isolated]], those massive [[animals]], the [http://en.wikipedia.org/wiki/Mastodons mastodons], migrated everywhere except to Australia.
+
61:4.4 In general, the life of the preceding period continued to [[evolve]] and spread. The [https://en.wikipedia.org/wiki/Cat cat] family [[dominated]] the [[animal]] life, and [[marine]] life was almost at a standstill. Many of the [https://en.wikipedia.org/wiki/Horses horses] were still three-toed, but the modern types were arriving; llamas and giraffelike camels mingled with the horses on the grazing plains. The [https://en.wikipedia.org/wiki/Giraffe giraffe] appeared in [https://en.wikipedia.org/wiki/Africa Africa], having just as long a neck then as now. In South America sloths, armadillos, anteaters, and the South American type of primitive [https://en.wikipedia.org/wiki/Monkeys monkeys] evolved. Before the [https://en.wikipedia.org/wiki/Continents continents] were finally [[isolated]], those massive [[animals]], the [https://en.wikipedia.org/wiki/Mastodons mastodons], migrated everywhere except to Australia.
  
61:4.5 5,000,000 years ago the [http://en.wikipedia.org/wiki/Horse horse] evolved as it now is and from [http://en.wikipedia.org/wiki/North_America North America] migrated to all the world. But the horse had become [[extinct]] on the continent of its origin long before the [http://nordan.daynal.org/wiki/index.php?title=Paper_64#64:6._THE_SIX_SANGIK_RACES_OF_URANTIA red man] arrived.
+
61:4.5 5,000,000 years ago the [https://en.wikipedia.org/wiki/Horse horse] evolved as it now is and from [https://en.wikipedia.org/wiki/North_America North America] migrated to all the world. But the horse had become [[extinct]] on the continent of its origin long before the [https://nordan.daynal.org/wiki/index.php?title=Paper_64#64:6._THE_SIX_SANGIK_RACES_OF_URANTIA red man] arrived.
  
61:4.6 The [[climate]] was [[gradually]] getting cooler; the [[land]] [[plants]] were slowly moving southward. At first it was the increasing cold in the north that stopped [[animal]] migrations over the northern [http://en.wikipedia.org/wiki/Isthmuses isthmuses]; subsequently these North American land bridges went down. Soon afterwards the [[land]] [[connection]] between [http://en.wikipedia.org/wiki/Africa Africa] and [http://en.wikipedia.org/wiki/South_America South America] finally submerged, and the Western Hemisphere was isolated much as it is today. From this time forward [[Different|distinct]] [[types]] of life began to [[develop]] in the [http://en.wikipedia.org/wiki/Eastern_Hemisphere Eastern] and [http://en.wikipedia.org/wiki/Western_Hemisphere Western Hemispheres].
+
61:4.6 The [[climate]] was [[gradually]] getting cooler; the [[land]] [[plants]] were slowly moving southward. At first it was the increasing cold in the north that stopped [[animal]] migrations over the northern [https://en.wikipedia.org/wiki/Isthmuses isthmuses]; subsequently these North American land bridges went down. Soon afterwards the [[land]] [[connection]] between [https://en.wikipedia.org/wiki/Africa Africa] and [https://en.wikipedia.org/wiki/South_America South America] finally submerged, and the Western Hemisphere was isolated much as it is today. From this time forward [[Different|distinct]] [[types]] of life began to [[develop]] in the [https://en.wikipedia.org/wiki/Eastern_Hemisphere Eastern] and [https://en.wikipedia.org/wiki/Western_Hemisphere Western Hemispheres].
  
61:4.7 And thus does this period of almost ten million years' duration draw to a close, and not yet has the [[ancestor]] of [[man]] appeared. This is the time usually designated as the [http://en.wikipedia.org/wiki/Pliocene Pliocene].
+
61:4.7 And thus does this period of almost ten million years' duration draw to a close, and not yet has the [[ancestor]] of [[man]] appeared. This is the time usually designated as the [https://en.wikipedia.org/wiki/Pliocene Pliocene].
  
<center>[http://nordan.daynal.org/wiki/index.php?title=Paper_61 Go to Paper 61]</center>
+
<center>[https://nordan.daynal.org/wiki/index.php?title=Paper_61 Go to Paper 61]</center>
<center>[http://nordan.daynal.org/wiki/index.php?title=The_Urantia_Text_-_Contents Go to Table of Contents]</center>
+
<center>[https://nordan.daynal.org/wiki/index.php?title=The_Urantia_Text_-_Contents Go to Table of Contents]</center>
  
 
[[Category:Paper 61 - The Mammalian Life Era on Urantia]]
 
[[Category:Paper 61 - The Mammalian Life Era on Urantia]]
 
[[Category: Evolution]]
 
[[Category: Evolution]]
 
[[Category: Earth Science/TeaM]]
 
[[Category: Earth Science/TeaM]]

Latest revision as of 23:38, 12 December 2020

Lighterstill.jpg

The eye of all ur60.jpg

61:4.1 This is the period of pre-glacial 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.

61:4.2 10,000,000 years ago began an age of widespread local land deposits on the lowlands of the continents, but most of these sedimentations were later removed. Much of Europe, at this time, was still under water, including parts of England, Belgium, and France, and the Mediterranean Sea covered much of northern Africa. In North America extensive depositions were made at the mountain bases, in lakes, and in the great land basins. These deposits average only about two hundred feet, are more or less colored, and fossils are rare. Two great fresh-water lakes existed in western North America. The Sierras were elevating; Shasta, Hood, and Rainier were beginning their mountain careers. But it was not until the subsequent ice age that North America began its creep toward the Atlantic depression.

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

61:4.4 In general, the life of the preceding period continued to evolve and spread. The cat family dominated the animal life, and marine life was almost at a standstill. Many of the horses were still three-toed, but the modern types were arriving; llamas and giraffelike camels mingled with the horses on the grazing plains. The giraffe appeared in Africa, having just as long a neck then as now. In South America sloths, armadillos, anteaters, and the South American type of primitive monkeys evolved. Before the continents were finally isolated, those massive animals, the mastodons, migrated everywhere except to Australia.

61:4.5 5,000,000 years ago the horse evolved as it now is and from North America migrated to all the world. But the horse had become extinct on the continent of its origin long before the red man arrived.

61:4.6 The climate was gradually getting cooler; the land plants were slowly moving southward. At first it was the increasing cold in the north that stopped animal migrations over the northern isthmuses; subsequently these North American land bridges went down. Soon afterwards the land connection between Africa and South America finally submerged, and the Western Hemisphere was isolated much as it is today. From this time forward distinct types of life began to develop in the Eastern and Western Hemispheres.

61:4.7 And thus does this period of almost ten million years' duration draw to a close, and not yet has the ancestor of man appeared. This is the time usually designated as the Pliocene.

Go to Paper 61
Go to Table of Contents