Velocity is the mean speed of flow over time (metres per second) measured either at a
point in a river channel or over a set distance.
Stream velocity refers to the speed at which water flows in a stream or river. It is typically measured in meters per second or feet per second and can vary depending on factors such as channel geometry, slope, and discharge. Stream velocity is an important parameter in hydrology and river engineering for understanding water movement and erosion processes.
The process by which the material carried by a stream or river settles or is dropped is called deposition. This occurs when the velocity of the water decreases, causing it to lose the energy needed to carry sediment, which then settles to the riverbed.
A river's power to erode depends on its flow velocity, the volume of water it carries, the type and size of sediment it transports, and the slope of the river channel. These factors influence the force and effectiveness of erosion by the river.
Yes, a stream can flow below sea level. Streams that flow below sea level are typically found in areas with low elevations, such as large river deltas or regions with significant subsidence. These streams often rely on levees or other engineering measures to prevent flooding.
A point bar is a depositional feature found on the inside bend of a meandering river, characterized by coarser sediment accumulation due to decreased water velocity. In contrast, a channel bar forms in the middle of a river channel and is composed of sediment deposited within the active channel due to changes in flow velocity or sediment supply.
velocity
The velocity and discharge volume of the stream or river.
Stream velocity refers to the speed at which water flows in a stream or river. It is typically measured in meters per second or feet per second and can vary depending on factors such as channel geometry, slope, and discharge. Stream velocity is an important parameter in hydrology and river engineering for understanding water movement and erosion processes.
the competence and capacity of a steam depend on a streams velocity and discharge. Because the velocity and discharge of a given stream are not constant , the competence and capacity of a stream are not constant . competence and capacity vary along a stream and change throughout the year.
The ultimate base level of a stream is sea level. A base level is the lowest point to which a stream can erode its channel.
river
Stream velocity is the speed at which water flows in a stream or river. It is typically measured in units of distance per time (e.g. meters per second) and can vary based on factors such as gradient, channel shape, and discharge.
The velocity of a river is the speed at which the water in the river is flowing in a particular direction. It is typically measured in meters per second or feet per second. Velocity can vary at different points along a river depending on factors such as stream gradient, channel width, and flow volume.
The base level of a river is the lowest place where it can flow, generally it's mouth. Therefore if a river or stream flows into another river, then the first river's base level is the point where it joins the other river.
The elevation down to which a river has the ability to erode its bed everywhere along its course.
A stream or river called that flows into a larger stream or river is called a tributary.
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