meanders
A meandering stream is a type of stream with many curves in its path. These curves are caused by erosion and deposition processes along the stream's course, resulting in a winding and zigzagging flow pattern. Meandering streams are common in flat or gently sloping landscapes.
River
Curves in canyons formed by a down-cutting stream are called meanders. These meanders develop as the stream erodes the outer banks of the river bend while depositing sediment on the inner banks, creating a sinuous pattern. Over time, meanders can grow more pronounced and may eventually lead to the formation of oxbow lakes if they become isolated from the main flow of the stream.
an old stream is a deep wide and curvy river stream
Curves in canyons formed by a downcutting stream are known as meanders. These curves develop as the stream erodes the outer banks of the channel, creating a sinuous path as it flows over time. The process is influenced by factors such as water velocity, sediment load, and the geology of the canyon walls. As the stream continues to cut down and erode, meanders can become more pronounced, leading to the characteristic shapes seen in many canyon landscapes.
River
wide and steep
The word 'narrow' describes how wide a river is when it's near its source. The source of a river or stream is called a headwater.
A stream or river called that flows into a larger stream or river is called a tributary.
A stream meanders due to a combination of factors such as the flow of water, the slope of the land, and the type of sediment in the streambed. Erosion and deposition processes also play a role in shaping the curves and bends of a meandering stream.
Option c is correct
A wide bend in a coastline is called a bay. It is an indentation or curved area of land where the coastline curves inward, often forming a sheltered body of water. Bays can range in size from small coves to large, open bays.