Answer :
H and i were located in Mexico in 1936.
They were located in the United States of America in 1992.
River water because of high energy and very less friction and low energy and high friction in the water at both the banks of the river, erodes one side and deposits sediments on the other side. Oxbow lakes usually form in plains or flat lands close to the river. Meanwhile, meander rivers that form oxbow lakes have two pairs of curves: one curving away from the river and the other curving back into the straight path of the river. Corners of banks closest to both of these are called concave banks. Banks opposite to them are convex banks. Erosion and deposition caused a new channel to be cut through the small piece of land at the end of the meander, making a shortcut path. Oxbow lakes are the remaining land/bend of the river. These principles of oxbow and meander rivers might have caused the change of location of h and i.
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