I should have … at least said "I agree with the science part of what you said."
That is little different than what you said before. It isn’t just part science. What part do you not agree with that makes the millions of years go away so you can agree with the rest?
It's true that when two plates run into each other, one will most likely be heavier than the other. So if they keep pushing against each other, the heavier one will go under the lighter one.
No, no, no. Every time I have spoken of one plate subducting under another, it has been an oceanic plate that subducts, specifically because only oceanic plates can penetrate the upper mantle and have gravity aiding the subduction process. But if we are dealing with two slabs of continental crust - let me repeat what I posted a couple posts back:
When a slab of continental crust bangs into another slab of continental crust, neither one is even a candidate for subduction. Then it is a pushing match of incredible forces.
Except in very unusual cases, continental crust does not subduct, period. Even if one of the continental slabs is of somewhat lower density than the other, still each is too light for subduction to occur.
As to a heavier continental slab going under a lighter one (but not subducting into the mantle), in a limited sense that could happen. There are well-known processes in geology (called overthrusts and underthrusts) where massive layers of rock can be forced to slide over or under already in-place strata. But those are not unique to colliding plates.
But that's as far as it goes. Because there are problems with the idea that one will slide under the other and lift the other up.
Rather than vague allusions to “problems with the idea”, how about enumerating the issues? “It just can’t happen” is a pretty wimpy argument to make, especially when that very process is being studied and documented as it occurs.
(On the D-10 idea) The idea came from you, if I recall correctly.
It was your use of the D-10 idea, involving what effectively is a cable over a pulley so that gravity assists in the pulling that I see no equivalent of in plate tectonics.
You said there was a combination of the gravity pull from the leading edge of the subducting plate along with the push of the currents in the mantle that could push a plate (without momentum) under another plate.
I don’t think, at least in this thread, that I have said anything about the mantle drag on a plate forcing it along.
I think this idea is wrong on a few levels.
I appreciate the sentiment, but san specifics, this is no more than a doubt in your mind.
OK, I've been referring to the plate that goes underneath another plate as a subducting plate, but that doesn't see to be accurate. So let's call them the plates-that-go-under-other-plates. Seems kind of clunky, but one should be accurate.
Subducting plates are ones that, once started, continue to sink because they are more dense than the medium they are sinking into.
So, these plates-that-go-under-other-plates could either subduct or they could just keep sliding under, as India appears to be doing to the Tibet.
(I have found that Knight is pretty tolerant of long posts, if they are on-subject and pertinent. I hope this qualifies.)
Let me supply some important details that have not been covered about continental crust – continental crust collisions. There are similarities between the continental crust “floating” on the mantle, and icebergs floating in the ocean. When you see the towering wall of iceberg that your ship is about to hit, you know that, impressive as the ice you see is, under the part you see, below the ocean surface, is a vastly bigger mountain of ice actually holding the ice you see above the waterline. This is due to simple laws of hydrodynamics – the ice is only slightly less dense than the water. The difference between the weight of the ice actually below the surface and the weight of the sea water that would have been where the subsurface ice is has to equal the weight of the above water ice. The laws of hydrodynamics still apply.
Similarly continental crust is slightly less dense than the mantle material. And, just like the iceberg, when you climb 10,000 feet high on a mountain, the crust extends 50,000 or 100,000 feet or more below you. Mount Everest is a very minor hill compared to the depths the crust extends below it.
Now think of India pushing into Asia. If some of India is being forced between layers in Asia, causing the upper part to lift, keep in mind that in reality is occurring in the very upper layers of the continental crust.
There are problems with both scenarios. Either the plate that goes under will stop because the pushing power of the mantle isn't enough if the friction of the overlying plate keeps increasing.
Yup, but hasn’t reached that point yet in Tibet.
In the case of the plate subducting, for example at the Andes, where the sediments should be the greatest, which would be the leading edge of the overlying plate, we don't find them.
I am not aware of this, so pending specific data, I will withhold comment.
And secondly, something you mention next, the plate should be pulling the Andes down, not pushing them up. And of course, despite being a little lower in density, such a subtle density difference cannot overcome the not-so-subtle weight of the Andes.
I didn’t say anything about the Nazca Plate or the Andes. But your belief that the Andes should be being pulled down indicates another fundamental misunderstanding of plate tectonics. You do realize that the Andes are part of the “ring of fire”, a nearly continuous string of volcanoes encircling the Pacific Ocean. And that there is an almost perfect correlation between that ring of fire and a nearby ring of deep-ocean trenches caused by subduction zones? That is one place where two apparently dissimilar geological structures – ocean trenches and volcanoes – consistently occur in such close proximity that there almost has to be a causal relationship. And there is.
Side note. I recall seeing several graphics in prior recent TOL threads that I think cover this. I will verbally cover it again, but not a third time. I don’t mind explaining, unless I realize I am covering ground with the same person that they pretended to understand before (which happened with a TOL regular a year or so ago).
Briefly – the Nazca plate subducts under the west coast of South America. As it descends at an angle, the increasing temperature of the mantle around it starts heating it up slowly, and the confining pressure goes up in the plate. When high enough pressures and temperatures are reached, some of the minerals within the descending plate are forced to undergo chemical changes, with one result being that some (a lot of) hydrogen and oxygen atoms are set free. They combine into free water molecules. These water molecules are much lighter than the near-magma they were just set free from, so they begin to rise vertically, as much as the still high viscosity permits. This occurs under areas well inland of the coast, since that is where the angled descent of the subducting plate has carried it.
It is known that the addition of water to high-temperature basaltic magma – mantle rock – lowers its melting temperature. So the part of the mantle just above the descending plate gets an influx of superhot water, and it essentially melts. Its viscosity is now much lower than typical mantle at that depth, and so it starts rising, by sort of melting its way upward. When it finally reaches the bottom of the continental crust, it can melt that too, and it may incorporate some silicates (continental type rock) into the rising mass of magma. If there is sufficient heat, the rising blob may make it all the way to the surface, erupting as a member of the ring of fire. If not enuff heat, then the rising blob may cool off and harden far underground.
So, the Andes are volcanoes, created and fed by subduction processes.
In fact, it appears that the Japan coast when down when the 2011 earthquake happened. That's not what was expected.
So? Lots of specifics about that earthquake were a surprise. You want to see if you can go down 20 miles below the ocean surface and come back with a detailed map of the faults, surface characteristics of the subducting plate, and so on? You find one earthquake that is outside the norm, and that means the hundreds of previous advances in earthquake understanding are bogus? I hope you are not that desperate.