The smaller the load a river has the more sediment it can carry is false. When the river has more energy, it is able to carry a larger load, therefore more sediment.
true
My understanding is that every glacier has a certain amount of sediment scraped from the interface of the surrounding bed rock and the moving ice. The total amount of this sediment is the Glacial load. Some significant land features, such as Cape Cod in Massachusetts, are remnants of the load after the ice receded.
none of the above
carrying power
sediment load
sediment load
The smaller the load a river has the more sediment it can carry is false. When the river has more energy, it is able to carry a larger load, therefore more sediment.
The smaller the load a river has the more sediment it can carry is false. When the river has more energy, it is able to carry a larger load, therefore more sediment.
sediment load
It's called transportation.
bedload
James Mirabal has written: 'Suspended-sediment load of Texas streams' -- subject(s): Sediment load
As a river gets older sediment load decreases due to the age of the river and erosion
Stream transport sediment in three ways, dissolved load, (ions in solution being carried downstream), suspended load, (suspended sediment that floats freely downstream) and bed load, (sediment that rolls or scoots along the bottom of the river).
As a river gets older sediment load decreases due to the age of the river and erosion
As a river gets older sediment load decreases due to the age of the river and erosion