erosion
deposition
weathering
and a lot more...
An increase in gradient will generally increase stream velocity.
The water in the stream will also rise.
This occurs in the small intestine by deffusion into the blood stream.
Its really simple if you think about it. if you have a bacterial infection your white blood cell count would increase because as the wbc's are fighting off the infection they die off releasing a chemical into the blood stream that tells your body to increase production of white blood cells. so the hematocrit would have a thicker buffer layer. the buffer layer being the white blood cells. With a higher production of white blood cells the rbc production would very slightly decrease which would decrease the ratio of rbc to whole blood volume.
Precautions for landslide - (I) if you remain or arecaught suddenly at home move to a second story if possible (II) if you are near a stream or channel , be alert for any sudden decrease or increase of water flow and for a change from clear to muddy water (III) be especially alert if you are driving (IV) whenever you are in the path of landslide or debris flow , move away as quickly as possible
increase
Decrease. The source of the river is usually in a mountainous area with a steep gradient.
pressure, temperature, possibly somethign else
An increase in gradient will generally increase stream velocity.
Yea
Stream discharge would increase if additional water enters it, such as from a rain storm or from melting snow.
Decrease in stream velocity
Decrease in stream velocity
Decrease in stream velocity
Decrease in stream velocity
The width of the stream will increase as the order increases
The discharge for a single stream should not change much from the headwater to the mouth. The exceptions to the mouth would be if another stream joined the main stream, which would increase the discharge or if you loose a significant amount of water to infilitration, which would decrease the discharge. The gradient should be high at the headwaters and gradually decrease downstream where it should be low at the mouth. Of course differences in lithologies or secondary streams can change the gradient for a short distance, thought the overall profile should fit the expected model.