#Why Midwest Earthquakes
02-Feb-95 17:48:16
Sb: #165602-#Why Midwest Earthquakes
Fm: Jon Woolf 76557,3537
To: Kamron Kirkconnell 73740,2246
Kamron,
>> The water seeks a short cut and once the river had cut lower on one side of
the tower it would never find it easier to return again over the high side let
alone do this over and over back and forth creating the massive tower. <<
Never? Never say never, Kamron — Nature has a funny way of proving such
claims wrong with monotonous regularity. <g>
Consider this scenario: River follows path of least resistance, and cuts a
valley or even a canyon in soft rock to one side of a tower of harder rock,
maybe an igneous intrusion. By and by, you have the river, then the igneous
tower, then sedimentary rock all round the rest of the tower.
Now you have an earthquake — say, a strike-slip type quake with most of the
motion horizontal. Say you get a big fracture right along the border between
the sedimentary rock and the igneous rock. Say that fracture leads into the
riverbed upstream and downstream of the igenous tower, and bottoms out just
below the upstream riverbed. Then the river, always following the path of
least resistance, will quit flowing on the one side of the tower and start
flowing on the other side. Allow another few million years for erosion, and
you wind up with the tower sitting alone with a river on one side and an empty
ex-riverbed on the other side.
Modify this scenario a bit, and you could easily get the river flowing on both
sides of the tower.
Jon W.