Table of Contents
What do streams depends on?
Stream competence depends on stream velocity (as shown on the Hjulstrom diagram above). The faster the current, the heavier the particle that can be transported. Stream capacity is the maximum amount of solid load (bed and suspended) a stream can carry.
How are stream beds formed?
Sediment is transported, eroded and deposited on the stream bed. The majority of sediment washed out in floods is “near-threshold” sediment that has been deposited during normal flow and only needs a slightly higher flow to become mobile again. This shows that the stream bed is left mostly unchanged in size and shape.
What factors affect stream speed?
The velocity of a river is determined by many factors, including the shape of its channel, the gradient of the slope that the river moves along, the volume of water that the river carries and the amount of friction caused by rough edges within the riverbed.
How do streambeds move over time?
At some point in most streams, there are curves or bends in the stream channel called meanders (Figure 10.3). The stream erodes material along its outer banks and deposits material along the inside curves of a meander as it flows to the ocean (Figure 10.4). This causes these meanders to migrate laterally over time.
What makes up a river bed?
Rivers literally “make their beds” (the river bed is the bottom) by eroding and depositing rocks, sand, silt, and organic materials. The energy source for all of this work is flow: water moving downhill. When the river gets out of its banks, it floods land on either side.
What are the factors that affect stream erosion and deposition?
Both natural and human- caused factors affect the amount of erosion a stream may experience. Natural factors include the gradient (or steepness) of the streambed since that affects the speed of the flow of water. Rainfall and snowmelt affect the amount of water in a stream as well as the speed of the flow.
What 3 variables influence the speed of stream flow?
What three variables influence the speed of stream flow? Stream gradient, stream discharge, and channel growth.
Where is the stream most likely flowing the fastest?
Water flow in a stream is primarily related to the stream’s gradient, but it is also controlled by the geometry of the stream channel. As shown in Figure 13.14, water flow velocity is decreased by friction along the stream bed, so it is slowest at the bottom and edges and fastest near the surface and in the middle.
What’s at the bottom of a river?
The bed (also called the river bed) is the bottom of the river (or other body of water).