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Attractions normally visited before or after visiting Wild Waters. Wild Waters Tour Reviews. All Questions. Zandile Nov Ayanda Nobuhle Nov Sphiwe Oct Alinah Oct Mbali Oct Family day out.
Great spot for just relaxing or having braais. The kids love the water and slides. Great spot overall. Date of experience: December Boksburg, South Africa 2 contributions 5 helpful votes.
It's a lovely place when go at summertime with kids who love water and love to swim. Always take food with to avoid looking shops while entertaining kids on a hot day.
Date of experience: March Benoni, South Africa 10 contributions 5 helpful votes. Unfortunately they don't have all the slides they use to have.
Date of experience: October Previous Next 1 2 3 4 5 6 7. Frequently Asked Questions about Wild Waters. What hotels are near Wild Waters?
Four factors, separately or in combination, can create rapids: gradient, constriction, obstruction, and flow rate. Gradient, constriction, and obstruction are streambed topography factors and are relatively consistent.
Flow rate is dependent upon both seasonal variation in precipitation and snowmelt and upon release rates of upstream dams. Streambed topography is the primary factor in creating rapids, and is generally consistent over time.
Increased flow, as during a flood or high-rainfall season, can make permanent changes to the streambed by displacing rocks and boulders, by deposition of alluvium , or by creating new channels for flowing water.
The gradient of a river is the rate at which it changes elevation along its course. This loss determines the river's slope, and to a large extent its rate of flow velocity.
Shallow gradients produce gentle, slow rivers, while steep gradients are associated with raging torrents. Constrictions can form a rapid when a river's flow is forced into a narrower channel.
This pressure causes the water to flow more rapidly and to react to riverbed events rocks, drops, etc. A boulder or ledge in the middle of a river or near the side can obstruct the flow of the river, and can also create a "pillow"; when water flows backwards upstream of the obstruction, or a "pour over" over the boulder ; and "hydraulics" or "holes" where the river flows back on itself—perhaps back under the drop—often with fearful results for those caught in its grasp.
Holes, or hydraulics, are so-called because their foamy, aerated water provides less buoyancy and can feel like an actual hole in the river surface.
If the flow passes next to the obstruction, an eddy may form behind the obstruction; although eddies are typically sheltered areas where boaters can stop to rest, scout, or leave the main current, they may be swirling and whirlpool-like.
In large rivers with high flow rates next to an obstruction, "eddy walls" can occur. An eddy wall is formed when the height of the river is substantially higher than the level of the water in the eddy behind the obstruction.
This can make it difficult for a boater, who has stopped in that particular eddy, to re-enter the river due to a wall of water that can be several feet high at the point at which the eddy meets the river flow.
A marked increase or decrease in flow can create a rapid, "wash out" a rapid decreasing the hazard , or make safe passage through previously navigable rapids more difficult or impossible.
Flow rate is measured in volume per unit of time. The most widely used [ citation needed ] grading system is the International Scale of River Difficulty , where whitewater either an individual rapid, or the entire river is classed in six categories from class I the easiest and safest to class VI the most difficult and most dangerous.
The grade reflects both the technical difficulty and the danger associated with a rapid, with grade I referring to flat or slow-moving water with few hazards, and grade VI referring to the hardest rapids, which are very dangerous even for expert paddlers, and are rarely run.
Harder rapids for example a grade-V rapid on a mainly grade-III river are often portaged , a French term for carrying.
A portaged rapid is where the boater lands and carries the boat around the hazard. A rapid's grade is not fixed, since it may vary greatly depending on the water depth and speed of flow.
Rapids that would have meant almost certain death a hundred years ago may now be considered only a Class IV or V rapid, due to the development of certain safety features.
Although some rapids may be easier at high flows because features are covered or "washed-out", high water usually makes rapids more difficult and dangerous.
At flood stage, even rapids that are usually easy can contain lethal and unpredictable hazards briefly adapted from the American version  of the International Scale of River Difficulty.
On any given rapid, a multitude of different features can arise from the interplay between the shape of the riverbed and the velocity of the water in the stream.
Strainers are formed when an object blocks the passage of larger objects, but allows the flow of water to continue - like a big food strainer or colander.
These objects can be very dangerous, because the force of the water will pin an object or body against the strainer and then pile up, pushing it down under water.
For a person caught in this position, getting to safety will be difficult or impossible, often leading to a fatal outcome. Strainers are formed by many natural or man-made objects, such as storm grates over tunnels, trees that have fallen into a river "log jam" , bushes by the side of the river that are flooded during high water, wire fence, rebar from broken concrete structures in the water, or other debris.
Strainers occur naturally most often on the outside curves of rivers where the current undermines the shore, exposing the roots of trees and causing them to fall into the river and form strainers.
In an emergency, climbing on top of a strainer may be better so as not to be pinned against the object under the water.
In a river, swimming aggressively away from the strainer and into the main channel is recommended. If avoiding the strainer is not possible, one should swim hard towards it and try to get as much of one's body up and over it as possible.
Sweepers are trees fallen in or heavily leaning over the river, still rooted on the shore and not fully submerged. Their trunks and branches may form an obstruction in the river like strainers.
Since it is an obstruction from above, it often does not contribute to whitewater features, but may create turbulence. Thanks for helping!
Share another experience before you go. Full view. Best nearby. Li's Chinese Restaurant. Mombasa Marine National Park.
Get to know the area. Walking Tours Mombasa City Tour 4 reviews. Our tour focusses on client satisfaction. Write a review. Traveler rating.
Selected filters. All reviews floater. Dee wrote a review Apr Nairobi, Kenya 13 contributions. Fun for all ages. Was here for my birthday weekend and I had a lot of fun.
Could not get enough of the rides and was exhausted by the end of the day.Recent News. This open-top mat slide is one of our original and still most popular slides. Carribean Plunge Cool off in this giant 30, sq. Welcome to Wild Water Adventures! For 29 years, guests from Champions League Spielplan Heute the world have enjoyed our fun, exciting, enriching Canadian Rockies rafting trips on the world famous Kicking Horse River.