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OK shut up with the balloon stuff OK listen to me I'm twelve :). first you have to have a full sink of water then empty your mind only think of your inner chi flowing through your body just like water then imagine it coming out of your hands now keep it in your mind slowly stand up with your eyes closed and imagine the chi still coming out of your hands and connect it with the water and move your hands very slowly back and forth and if that don't work write back and i have other things and Ive water bended before and i still do and it does work keep your hopes up

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12y ago
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13y ago

You can't really "bend" water. As a solid (ice), the hydrogen bonds make it pretty rigid and brittle. It tends to break before bending. The liquid has an extremely low resistance to shear forces. It won't hold its shape so that you can try to bend it. And as a gas, the same logic applies as it did to the liquid form. The bottom line is that you can't bend water. To be a bit more "scientific" here, bending something speaks to the ability of a material to plastically deform. Water does not have a phase that will permit plastic deformation. You can't bend water.

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Q: How do you water bend?
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dfg sdfg


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Steep undercut area on the outside of a river bend?

As the river flows around the outside of the bend, it accelerates just like when a car goes around a bend. The water, like a car, is pulled toward the outside of the bend through centripetal force (which is why road bends are often banked). The same thing happens to the water surface. It actually rises around the outside of the bend. This higher elevation of the water surface means that the water on the outside of the bend is slightly deeper than the inside. Since water always tries to seek a level surface, the water on the outside of the bend actually flows downward, along the bottom and comes back up on the inside of the bend. This secondary current pushes material from the outside of the bend back up on the inside of the bend - and that's where sand bars come from. So the combination of accelerated flow around the outside combined with the secondary current moving downward erodes the outside of the river bend.


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