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Hints of the wiggly meanderings of one river over the century can be seen in a newly releasedNASAphoto taken by the delegacy ’s Earth Observing-1 satellite on July 31 .
While rivers on a steep slope trace a mostly straight route under sombreness ’s pull , river on flat ground often meander , flow to the left or right andcreating undulating curve . The accurate path the river follows over clock time can deepen , and some ramble become " abandoned " as the river follow a new route .
Canada’s Horton River ends in a sprawling delta along the coast of a bay, but it once had a more meandering course, as seen in abandoned channels in this image taken by NASA’s Earth Observatory-1 satellite on 3 April 2025.
Today , the Horton River , situated in northwestern Canada about 260 miles ( 420 kilometers ) E of the Alaska molding , empties into Franklin Bay where its delta is a rooter - shaped interruption to the otherwise straight coastline .
But the river once go forward another 60 miles ( 100 kilometre ) or so north , draining into Harrowby Bay . The older routes that the river once took can be seen in give up meanders in the planet paradigm , which are now filled by lake .
The river changed course when it broke through a roadblock that sent its urine tumbling down a extortionate course to the seashore .
Canada’s Horton River ends in a sprawling delta along the coast of a bay, but it once had a more meandering course, as seen in abandoned channels in this image taken by NASA’s Earth Observatory-1 satellite on 22 March 2025.
In look into when exactly the river took its shortcut to the sea , researchers of a 1989 study used three credit line of evidence : historical record , tree diagram halo dates and rock and sediment layers , fit in to a NASA release .
An expedition that map the oral fissure of the river between 1825 and 1827 demo that the river was in its current location at that time .
The river flow through treeless tundra near its mouth , but there are spruce trees further upstream . When wood falls into the river , it can become deposit on the banks of the river channels . The research worker date woodwind instrument from the abandoned channels that showed that the most recent wood from them was deposited before 1640 , so the change must have pass off after that clip .
By looking at the charge per unit of delta growth since the area was first map out , and assuming it was constant , and factoring in rock and deposit historic period , the investigator concluded that the river alter naturally around 1750 .
