Editing 1449: Red Rover
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In the game portrayed here, an isolated landmass (India in contemporary geography), is the individual charging towards the Laurasian landmass, attempting to break through. We know of course that India failed in this attempt, and as per the games rules joined the Laurasia 'team'. This part of the supercontinent later developed in to {{w|Asia}}. | In the game portrayed here, an isolated landmass (India in contemporary geography), is the individual charging towards the Laurasian landmass, attempting to break through. We know of course that India failed in this attempt, and as per the games rules joined the Laurasia 'team'. This part of the supercontinent later developed in to {{w|Asia}}. | ||
β | It is accepted that the {{w|Himalayas}}, the highest elevated mountain range on earth, formed by the collision of India into what is now Asia. For various reasons, the movement of the Indian plate from its location in Gondwana 90 | + | It is accepted that the {{w|Himalayas}}, the highest elevated mountain range on earth, formed by the collision of India into what is now Asia. For various reasons, the movement of the Indian plate from its location in Gondwana 90 million years ago to its impact point with the rest of Asia 50 million years ago was extremely rapid (as plate movements go) at about 20 cm per year. |
The idea that the landmasses on Earth are sentient and moving about in an incredibly slow game of Red Rover, with India's rapid movement being a result of being "called over", is not one which is currently scientifically accepted{{Citation needed}}. | The idea that the landmasses on Earth are sentient and moving about in an incredibly slow game of Red Rover, with India's rapid movement being a result of being "called over", is not one which is currently scientifically accepted{{Citation needed}}. | ||
β | The title text refers to the {{w|Slide Mountain Ocean}}, which was located between the {{w|Intermontane Islands}} and North America in the Triassic period beginning around 245 | + | The title text refers to the {{w|Slide Mountain Ocean}}, which was located between the {{w|Intermontane Islands}} and North America in the Triassic period beginning around 245 million years ago. The name interests [[Randall]] because oceans (bodies of water), mountains (land masses), and slides (playground equipment) are mutually exclusive concepts when using the most common definitions. In this case, however, "slide" is short for "{{w|landslide}}" which is a common feature of mountains. [http://travelingluck.com/North+America/Canada/British+Columbia/_6149492_Slide+Mountain.html Slide Mountain] is a particular mountain in {{w|British Columbia}}, the result of the remnant of the Slide Mountain {{w|List of tectonic plates#Tertiary plates|microplate}} which {{w|Accretion (geology)|accreted}} onto the continent, becoming the {{w|Slide Mountain Terrane}}, as the majority of the microplate was {{w|Subduction|subducted}}. "Slide Mountain Ocean" refers to the sea between the Slide Mountain microplate before it was subducted under what is now North America. |
==Transcript== | ==Transcript== |