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  2. Hydraulic jump - Wikipedia

    en.wikipedia.org/wiki/Hydraulic_jump

    A tidal bore is a hydraulic jump which occurs when the incoming tide forms a wave (or waves) of water that travel up a river or narrow bay against the direction of the current. [16] As is true for hydraulic jumps in general, bores take on various forms depending upon the difference in the waterlevel upstream and down, ranging from an undular ...

  3. Hydraulic jumps in rectangular channels - Wikipedia

    en.wikipedia.org/wiki/Hydraulic_Jumps_in...

    1. y 2 /y 1 > 1: depth increases over the jump so that y 2 > y 1 2. Fr 2 < 1: downstream flow must be subcritical 3. Fr 1 > 1: upstream flow must be supercritical. Table 2 shows the calculated values used to develop Figure 8. The values associated with a y 1 = 1.5 ft are not valid for use since they

  4. Armor (hydrology) - Wikipedia

    en.wikipedia.org/wiki/Armor_(hydrology)

    Armour of basalt blocks. In hydrology and geography, armor is the association of surface pebbles, rocks or boulders with stream beds or beaches.Most commonly hydrological armor occurs naturally; however, a man-made form is usually called riprap, when shorelines or stream banks are fortified for erosion protection with large boulders or sizable manufactured concrete objects.

  5. File:River Chart.svg - Wikipedia

    en.wikipedia.org/wiki/File:River_Chart.svg

    English: Charting a river - measuring its width at a given location using the intercept theorem. The intercept theorem can be used to determine a distance that cannot be measured directly, such as the width of a river or a lake, the height of tall buildings or similar. The graphic to the right illustrates measuring the width of a river.

  6. Stream competency - Wikipedia

    en.wikipedia.org/wiki/Stream_competency

    Stream power is the rate of potential energy loss per unit of channel length. [7] This potential energy is lost moving particles along the stream bed. = where is the stream power, is the density of water, is the gravitational acceleration, is the channel slope, and is the discharge of the stream.

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  8. Dickerson Whitewater Course - Wikipedia

    en.wikipedia.org/wiki/Dickerson_Whitewater_Course

    A final 100-foot (30 m) section ends in the river, with or without a drop, depending on the river level. Overall slope adds another seven feet of drop, for a total course drop of 15 feet (4.6 m), plus zero to four feet (0 to 1.2 meters) into the river at the end. The following map shows the arrangement of the visible and submerged features.

  9. Northern Warfare Training Center - Wikipedia

    en.wikipedia.org/wiki/Northern_Warfare_Training...

    Junior Leaders Course (discontinued): Two week basic mountaineering, plus greeley phase and river phase: geography, climate, and phenomenon of northern area of operations, living in the field, hazards to movement, medical problems, inland waterways, river training, boat operations, river charting, reading and navigation, and stream crossing.