continental shelf
Yes, at the surface but the full Gulf Stream is a cycle. It includes a flow of cold water in the opposite direction and which travels at depth.
Any Type Of water as long as it flows down stream(north, south,east,west) the sources can flow in to other streams! Any Type Of water as long as it flows down stream(north, south,east,west) the sources can flow in to other streams!
Water will flow downhill. Weeds often grow and lean downstream. Ripples and floating debris will show flow direction.
A contour map shows lines which connect areas equal in height. These lines are called contours and should be labelled to show the height that each contour represents. A stream flows downhill, this is due to gravity. Thus, to determine which way a stream flows, find contours, at least two, that intersect the path of the stream, then look at the heights these contours represents(their labels). The stream will flow from the contour labelled with the higher number towards the contour labelled with the lower number. PS. sometimes not all the contours are numbered, but only say every fith contour is numbered, then you can assume that all contours are equally incremented i.e. the height difference from one contour to the next stays equal.
Wetted width is a term used in fluvial geomorphology. It is the width of a stream at the time of the field measurements indicating the width of the current flow and is generally below bankful width.
stream channel
The continental slope is the steep transition between the continental shelf and the deep ocean floor, marking a distinct boundary in underwater topography. This area typically descends at an angle of 2 to 5 degrees, leading to the abyssal plain. It serves as a critical ecological zone where nutrients from the shelf can flow into deeper waters, supporting diverse marine life. Additionally, the slope is important for geological studies and resource exploration, including oil and gas deposits.
yes through surface run-off or groundwater flow
Changing the slope of the stream table affects the speed and direction of water flow. A steeper slope creates faster water flow, which can result in more erosion and deposition. Conversely, a flatter slope slows down water flow, leading to less erosion and deposition. These changes in flow dynamics can cause differences in the shape and size of channels, as well as the amount and distribution of sediment carried by the water.
A steeper slope typically leads to a faster flow velocity in a stream. This is because gravity plays a larger role in pulling the water downhill, increasing the speed of the water flow. Conversely, a gentler slope results in a slower velocity as the force of gravity is not as strong.
Gravity and the slope of the land combine to create the force that moves water in a stream. Gravity pulls the water downhill, and the slope of the land determines the direction and speed of the flow.
Water flows downhill. Contour lines show the slope of the landscape, and the direction a stream must flow.
False a steep shelf slows the surge. while a slopping shelf will let the water flow.
The great heaps of unconsolidated sediment at the base of the continental slope are known as submarine fans. These fans are typically formed by the deposition of sediment transported by turbidity currents that flow down the continental slope. Submarine fans are important features in understanding sediment transport processes in deep-sea environments.
Stream gradient, or the slope of the stream channel, affects stream velocity by influencing the speed at which water flows downstream. A steeper stream gradient typically results in a faster water flow velocity, as the force of gravity pulls water downhill more strongly. Conversely, a gentler stream gradient leads to slower water flow velocity.
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.
A steeper gradient generally results in a faster flow velocity, while a shallower gradient typically leads to slower flow velocity in a stream. This is because the slope of the streambed determines how quickly water can move downstream due to gravity.