Besides the necessity of river transportation, the goound near the rivers and old river channels contained the best agricultural land, where the sandy and silty soil settled, increasing the height of the natural levees.
32.
The height of these natural levees, formed from overbank deposits of sediments deposited by annual river floods, ranged from above mean high tide at Staten and Tyler Islands, located further east near the Mokelumne River.
33.
From Kampong Cham Province the gradient slopes very gently, and inundation of areas along the river occurs at flood stage June through November through breaks in the natural levees that have built up along its course.
34.
The street was laid out atop a slight rise, the remains of an old natural levee, in connection with the construction of the New Orleans and Carrollton Railroad, which became the St . Charles Streetcar Line.
35.
If the river breaches its natural levees ( i . e ., during a flood ), it spills out onto a new course with a shorter route to the ocean, thereby obtaining a more stable steeper slope.
36.
The lower reaches of the Latrobe River, Thomson River and Mitchell River flow into the Gippsland Lakes and have extensive floodplains in which there are large wetlands, often separated by natural levees from the main river channels.
37.
This spillway and an imperfect natural levee about 4 6 meters ( 12 to 20 feet ) high are all that prevents the Mississippi from taking a new, shorter course through Lake Pontchartrain to the Gulf of Mexico.
38.
If the river could breach its natural levees ( i . e ., during a flood ), it would spill out onto a new course with a shorter route to the ocean, thereby obtaining a more stable steeper slope.
39.
Located on Lafayette Street, a bluff that works as the river's natural levee, the new LaSalle office building and a separate 540, 000-square-foot parking garage will look out over the river, nearly a mile wide as it passes downtown.
40.
The leftover higher locations, typically natural levees at the margins of the flood channel, will themselves be eroded by lateral stream erosion and from local rainfall and possibly wind transport if the climate is arid and does not support soil-holding grasses.
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