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01-22-2002, 09:09 PM | #11 |
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Awesome as always Patrick: "You da man!"
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01-23-2002, 08:30 AM | #12 | ||
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Thanks for the links Patrick. My sarcastic rant wasn't terribly informative. He finds a local occurrance and makes up some process to explain it. Then he assumes that this process was flood linked. When his assertions are tested globally by observation, since a flood would have global consequenses, they fail miserably. Others have already addressed his diatoms and chronology problems.
Then there is his concept of stream terracing. He doesn't seem to understand how sea level changes affect base level. Onlap sequences are laid down on the coastal plain during high stand sea level during glacial minima. This is especially evident on passive margins such as the mid-Atlantic East Coast of the US. He interprets depositional phases as occuring during ice maxima when the land is warped downward. The depostional sequenses are truncated when ice retreats and the land "warps" upward and gradient is increased. Quote:
His interpretation of isostacy would also dicate that there should be high mountains in the Hudson Bay area since the unloading of all that ice. The Coastal Range of Alaska should be squished into the ground under the load of all those glaciers. Volcanic activity should exist in the northern Appalachians since they were under a huge ice burden and must be lifting rapidly. The crust should fracture due to the distortion from the ocean basin sinking while the adjacent land mass rises rapidly. Quote:
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01-24-2002, 02:21 PM | #13 |
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Morpho-
I found some good papers today. I'm gonna set Wmscott straight on the diatoms this weekend. Patrick |
01-24-2002, 09:18 PM | #14 | |
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Quote:
No one's really challenged him hard on the actual theory (instantaneous isostatic rebound). I don't know enough about the mechanisms. That might be interesting... [Edited to add: Okay, I see you've already started your assault. Ignore my last. "You da man"! <img src="graemlins/notworthy.gif" border="0" alt="[Not Worthy]" /> [ January 24, 2002: Message edited by: Morpho ]</p> |
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