A pile of dirt.
An alluvial fan is typically formed at the base of a mountain or hilly area where a river or stream exits a narrow canyon or valley, and the water carrying sediments spreads out onto a flatter, open area. The fan shape is created as the water slows down and deposits the sediment it was carrying.
A fan-shaped formation that develops when a stream deposits its sediment at the base of a steep slope is called an alluvial fan. These features are typically found in arid or semi-arid environments where streams carry a large amount of sediment and quickly lose energy as they reach flat or gently sloping terrain.
The source of a stream is called a headwater or headstream. This is where the stream initially begins, often from a spring or melting snow.
matter
Point bars, cut banks, and levees are common types of deposits in a meandering stream. Point bars are formed on the inside of meander bends where slower flow allows sediment to settle, while cut banks are eroded on the outside of bends where the flow is faster. Levees are built up along the banks of the stream during flooding events.
Where a stream leaves a mountain range is called a Alluvial Fan. An Alluvial Fan is the sediment the streams leave behind as it leaves the range.
You could be describing either headwaters of a stream, or a waterfall.
deltas and placer deposits
Mountain Stream A Mountain Stream Background for Your Television - 2008 was released on: USA: November 2008
It is called deposition. It occurs as friction or gravity overcomes the force of the moving water.
It erodes away the part of the mountain that the stream is on.
Mountain Stream Salamander was created in 1895.
estuary
A five-letter word for "narrow mountain stream" is "brook".
Plateau- it has a horizontal bedrock structure and is a continuation of the Allegheny plateau. It looks like mountains because of stream and glacial erosion.
An alluvial fan is typically formed at the base of a mountain or hilly area where a river or stream exits a narrow canyon or valley, and the water carrying sediments spreads out onto a flatter, open area. The fan shape is created as the water slows down and deposits the sediment it was carrying.
a type of cat