Fluvial Geomorphology

is a rock layer that cannot hold water

is a rock layer that can hold water

is impermeable

is a soil layer that is not porous

is another name for a levee

is the land between two rivers

is the meeting of two rivers

is the source of a river

is the crust water in the rainy season

is the ground water

is the upper-most level of the ground water

is the ability of the ground to hold water

will be above the wet season water table

will be below the wet season water table

The place where a river starts

Where the river flows into the sea

Where two river channels meet

The land next to the river channel

watershed

river source

main channel of a river

wetland

run off the occurs in layers

run off the occurs in streams

the ground is saturated

the gradient is gentle

the is sparse vegetation

the rainfall is heavy

the ground is unsaturated

the gradient is gentle

the is sparse vegetation

the rainfall is gentle

the river mouth

the confluence

the watershed