Editing 2887: Minnesota

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The Midwestern states, particularly in areas like the {{w|New Madrid Seismic Zone}}, are subject to the movement of tectonic plates well within a tectonic plate boundary. While these areas are typically less active than boundary zones, they can still experience significant seismic activity. The flexible way the Earth's crust in these regions responds to tectonic stresses – gently stretching and flexing over centuries in response to deep stresses – could imaginatively be described as "supple."
 
The Midwestern states, particularly in areas like the {{w|New Madrid Seismic Zone}}, are subject to the movement of tectonic plates well within a tectonic plate boundary. While these areas are typically less active than boundary zones, they can still experience significant seismic activity. The flexible way the Earth's crust in these regions responds to tectonic stresses – gently stretching and flexing over centuries in response to deep stresses – could imaginatively be described as "supple."
  
Minnesota's northern border is legally defined in part by reference to geographical features, most notably {{w|Lake of the Woods}} and a chain of rivers and lakes connecting it to {{w|Lake Superior}}. As such, movement of these features due to glacial rebound may indeed be reducing Minnesota's size at a very gradual rate. Minnesota's southern border, in contrast, is legally defined as a line running at 43º 30′ N, which would not be affected by the motion of the land. Indeed, it is possible that glacial rebound is effectively moving land out of Minnesota and into Iowa, again at a very gradual rate.
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Minnesota's northern border is legally defined in part by reference to geographical features, most notably {{w|Lake of the Woods}} and a chain of rivers and lakes connecting it to {{w|Lake Superior}}. As such, movement of these features due to glacial rebound may indeed be reducing Minnesota's size at a very gradual rate. Minnesota's southern border, in contrast, is legally defined as a line running at 43º 30′ N, which would not be affected by the motion of the land. Indeed, it is possible that glacial rebound is effectively moving land out of Iowa and into Minnesota, again at a very gradual rate.
  
 
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