A stream or river typically follows a downhill path from its source in the mountains or highlands to its mouth where it meets a larger body of water, such as a lake or ocean. Along the way, it may meander, forming curves and bends, and sometimes split into smaller channels or tributaries before converging again.
The wearing down of soil and bedrock of a river or stream creates a channel, which is a trough or groove formed by the flow of water. This channel path is where the river or stream flows and carries sediment downstream. Over time, erosion can widen and deepen the channel, shaping the landscape.
Headward erosion is a fluvial process of erosion that lengthens a stream, a valley or a gully at its head and also enlarges its drainage basin. The stream erodes away at the rock and soil at its headwaters in the opposite direction that it flows. Once a stream has begun to cut back, the erosion is sped up by the steep gradient the water is flowing down. As water erodes a path from its headwaters to its mouth at a standing body of water, it tries to cut an ever-shallower path. This leads to increased erosion at the steepest parts, which is headward erosion. (wikipedia)When this happens, the erosion can break through into another stream and the water from the stream is diverted. So the stream is "stealing" the other stream's water.
An entrenched meander is a curved bend in a river that has eroded deeply into the landscape, creating a steep, narrow channel. This process typically occurs over a long period of time as the river flows through the landscape, cutting into the underlying rock or soil. Entrenched meanders are often seen in areas where the river has limited space to move laterally due to surrounding topography.
Meanders, or curved loops in a river, can be found in various river systems around the world. They are commonly seen in larger rivers with gentle slopes, such as the Mississippi River in the United States or the Amazon River in South America. Meanders form as the river erodes the outer bank and deposits sediment on the inner bank, causing the river channel to shift and create a looping pattern.
A stream transitions into a river when it reaches a certain size and flow rate. This transition is not clearly defined and can vary depending on the region and specific characteristics of the waterway.
The path that a stream follows is a channel.
A meander is described to as a river or stream with eroded banks such that it no longer flows in a relatively straight path, but instead is a winding path.
The Black River is an inland river and the course followed by the Nautilus as it began its voyage with Aronnax, Land, and Conseil. It is not one of the five Gulf Stream Currents.
The path that a stream follows is a channel.
To "meander" means "to follow a winding or bending path" - meandered is the past tense of this; "The river meandered towards Cambridge." (The river followed a winding path towards Cambridge.)
A stream or river called that flows into a larger stream or river is called a tributary.
The wearing down of soil and bedrock of a river or stream creates a channel, which is a trough or groove formed by the flow of water. This channel path is where the river or stream flows and carries sediment downstream. Over time, erosion can widen and deepen the channel, shaping the landscape.
The stream is a tributary of the river.
The bed of the stream.
A stream or brook can get bigger and become a river.
Lakes are found in the path of a stream/brook and small river. They are found over nearly all of the world depending on the climate.
its a tributary stream which set its path along a underlying non resistant rock...... if already the main drainage pattern is established.