Option c is correct
This is known as an Alluvial Fan. Please see related links.
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.
A mountain chain is called a mountain chain.
A group of mountain ranges is called a mountain range system or a mountain chain.
The tip of a mountain is called a peak.
This is known as an Alluvial Fan. Please see related links.
No, Sediments deposited where a river flows into an ocean or lake builds up a land form called a delta. An alluvial fan is a wide, sloping deposit of sediment formed where a stream leaves a mountain range.
A deposit that forms where a river leaves a mountain range is called an alluvial fan. This fan-shaped deposit is created as the river slows down and deposits sediment and debris that it has carried from the mountains.
This is known as an Alluvial Fan. Please see related links.
An alluvial fan starts at just a build up of sediment at the mouth of a river. As the current moves, more and more sediment is lifted into the stream and carried until it hits a sediment deposit. As the sediment deposit gets bigger, it is exposed to the air and forms a sediment mountain. As the mountain gets bigger it forms an island in the middle of the mouth of a river. This is called an alluvial fan! Hope this was helpful!
Its deposits sediment by picking the sediment up which is called plucking.(weathering)
they wash in the sand at the ocean floor that is then called "deposit" I THINK
A structure built up by stream deposits at the foot of a mountain is called an alluvial fan. Alluvial fans form when rivers or streams carrying sediment from the mountains suddenly lose velocity and deposit the sediment in a fan-shaped pattern.
silt This trianguar deposit of sediment where a river empties into an ocean is called a delta.
The resulting deposit is called loess.
DELTA
A sediment deposit called a windward slope forms when sediment is blown against an obstacle and settles behind it. This deposit is characterized by a gradual slope facing into the prevailing wind direction.