Streams
Ephemeral streams are streams that only have running surface water after a rain storm. During most of the year they are dry gullies or arroyos.
Most of the functionality available for byte streams is also provided for character streams.
If mountain glaciers disappear there will be no source for many mountain streams, which will then dry up. Many rivers will be reduced in size as a result.
Ephemeral deserts streams dry up before they reach the ocean
Streams are merely tributaries of rivers. A river is the wider channel into which smaller creeks, streams and rivers flow. (Streams do not flow out of rivers.) Streams carry water from higher sources, emptying into the river. As more streams empty into a river, it tends to become broader, simply because of the greater volume of water it is carrying.
In Suspension.
in streams and lakes
An ephemeral stream is dry most of the time and ionly holds water suring and after rainfall or snowmelt events. Streams in humid climates generally have water in them at all times.
it continues because some groundwater seeps into the streams
streams that fed the rivers
ions