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Author Topic:   A series of Questions for our Geologists.
NosyNed
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Posts: 9004
From: Canada
Joined: 04-04-2003


Message 4 of 68 (278964)
01-14-2006 3:31 PM
Reply to: Message 1 by jar
01-14-2006 10:00 AM


Mountain roots
Not a geologist either, but it looks like mountain roots of what is left of the Appalachians. That is the folds caused by the crunching of NA and Europe, when was it? 250 Myrs ago or so.

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NosyNed
Member
Posts: 9004
From: Canada
Joined: 04-04-2003


Message 12 of 68 (279077)
01-14-2006 11:41 PM
Reply to: Message 11 by jar
01-14-2006 11:36 PM


Arc creation
When the old continents collided and pushed up the appalacians?

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NosyNed
Member
Posts: 9004
From: Canada
Joined: 04-04-2003


Message 37 of 68 (284071)
02-04-2006 11:50 PM
Reply to: Message 36 by jar
02-04-2006 11:43 PM


Remains of the mountains
Off the top of my head; there are traces of those mountains across the continent. It seems there were major rivers draining west from them and some sediments are attributed to that.
I suspect that there is a lot more geophysical data than that but haven't a clue.
Oh boy I get to use AIG as a reference LOL
Appalachian Mountain Siliciclastics Source for Navajo Sandstone | Answers in Genesis
and
Page Not Found | Yale University
This message has been edited by NosyNed, 02-04-2006 11:56 PM

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NosyNed
Member
Posts: 9004
From: Canada
Joined: 04-04-2003


Message 40 of 68 (284075)
02-05-2006 12:24 AM
Reply to: Message 39 by jar
02-05-2006 12:04 AM


Re: Remains of the mountains
Sand doesn't flow up hill. If it came from far east and is in the west it needed some help.
There is a LOT of it. That implies a lot eroded too.
This message has been edited by NosyNed, 02-05-2006 12:24 AM

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NosyNed
Member
Posts: 9004
From: Canada
Joined: 04-04-2003


Message 44 of 68 (284111)
02-05-2006 9:41 AM
Reply to: Message 41 by jar
02-05-2006 12:41 AM


Sandstone
Sand is pretty easy to move around. Sandstone also erodes fairly quickly.
There is a possible flaw in thinking here. The sediments laid down have become sandstone. That doesn't mean the source of the sand was sandstone or easily eroded. (might be might not be).

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NosyNed
Member
Posts: 9004
From: Canada
Joined: 04-04-2003


Message 46 of 68 (284133)
02-05-2006 12:36 PM
Reply to: Message 45 by jar
02-05-2006 12:32 PM


more guesses will we await better
We can also see the uplifted parts of the crust in the cores of the mountain ranges.
For one thing if a flat segment of sediment is folded up drastically and then worn down there will be a pretty strong indication of this in the remaining "cores". The two sides of the loop of sediment would remain separated by where the rest of the mountain was.

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