Bankfull width is the maximum width the stream attains and is typically marked by a change in vegetation, topography, or texture of sediment (Herrelson and others 1994).
The dominant channel forming discharge is often assumed to be the bankfull flow. For example Knighton (1998) argued that "since it seems reasonable to suppose that river channels are adjusted on average to a flow which just fills the available cross-section, dominant discharge has been equated with bankfull flow, thereby giving it additional morphogenetic significance." The dominant discharge is supposed to give the same effects as the whole range of discharges occurring (Brandt, 2000). --- Brandt, S.A., 2000: Classification of geomorphological effects downstream of dams. Catena, vol. 40(4), pp. 375-401. doi:10.1016/S0341-8162(00)00093-X Knighton, D., 1998. Fluvial Forms and Processes: A New Perspective. Arnold, London, xv+383 pp.
535meters in width of the new dome.
Thew width of Neptune is exactly 72.9m long
Width is a length or distance. The unit of length is the meter.
Because width doesn't matter in a tsunami. The width is typically the length of the shore. It would be extremely difficult to classify a tsunami based upon height and width when the width is simply incomparable.
It depends how far along the river course it is. In theory as you move further down the river's course the bankfull width should increase.
The dominant channel forming discharge is often assumed to be the bankfull flow. For example Knighton (1998) argued that "since it seems reasonable to suppose that river channels are adjusted on average to a flow which just fills the available cross-section, dominant discharge has been equated with bankfull flow, thereby giving it additional morphogenetic significance." The dominant discharge is supposed to give the same effects as the whole range of discharges occurring (Brandt, 2000). --- Brandt, S.A., 2000: Classification of geomorphological effects downstream of dams. Catena, vol. 40(4), pp. 375-401. doi:10.1016/S0341-8162(00)00093-X Knighton, D., 1998. Fluvial Forms and Processes: A New Perspective. Arnold, London, xv+383 pp.
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Sean M. Lawlor has written: 'Determination of channel-morphology characteristics, bankfull discharge, and various design-peak discharges in western Montana' -- subject(s): River channels, Stream measurements
class width is a width width is a width nothing as class width is a width dont be confuse
length 14cm, width 2cm This is worked out by finding the following equations: perimeter = 16 x width length = width + 12 Then working out 16 x width = 2 x (width + 12) + 2 x width -> 14 x width = 2 x (width + 12) -> 14 x width = 2 x width + 24 -> 12 x width = 24 -> width = 2cm Since lendth = width + 12, length = 14cm
perimeter = length + length + width + width = 2*length + 2*width = 36 length = 5*width 2*(5*width) + 2*width = 36 12*width = 36 width = 3 length = 15
length*width = 2*width*width i.e square the width and multiply by 2
Perimeter = length + width + length + width = 2 x (length + width) Given: perimeter = 22in length = width + 3in Thus 22 = 2 x (width + 3 + width) 11 = 2 x width + 3 8 = 2 x width 4 = width So the width is 4in.
there is less friction caused by the bottom of the river bed and banks by sediment and rocks etc. velocities are said to be fastest at the surface of the river because of this less amount of friction acting upon it. it is also fastest at the centre of the river where it is the deepest.
AREA = LENGTH x WIDTH LENGTH = 2 X WIDTH AREA = 2 x WIDTH X WIDTH = 900 900/2 = WIDTH X WIDTH 450 = WIDTH X WIDTH = WIDTH SQUARED WIDTH = SQUARE ROOT (450) = 21.21 FEET LENGTH = 42.42 FEET
no it does not have a width