The parting of the red sea using sonic liquefaction to make water vapor?
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approx. 1600000000Kw hrs of electricity per hour you kept it on\n\nthat would cost a lot of money by the way and you might blow a fuse
579981
Iron and water.  Just wash the sand off the iron.
727784
Earthquakes, use jello full of sand, and observe how it shakes when fractured.  Tsunami, create pool of water with a slope as the shore, and watch waves hit shores.  Volcanoes, build sandy hils and use something like coke and mentos to similate lava under pressure, watch it erupt.  Landslides, build sandy hills with steep sides, and watch how slides can occur.  Using nothing more than sand, jello, water, coke and mentos, and with imagination, you can create all these basic "natural disasters".
217588
Liquefaction occurs when the structure of a loose, saturated sand breaks down due to some rapidly applied loading. As the structure breaks down, the loosely-packed individual soil particles attempt to move into a denser configuration. In an earthquake, however, there is not enough time for the water in the pores of the soil to be squeezed out. Instead, the water is "trapped" and prevents the soil particles from moving closer together. This is accompanied by an increase in water pressure which reduces the contact forces between the individual soil particles, thereby softening and weakening the soil deposit.  \n      Observe how small the contact forces are because of the high water pressure. In an extreme case, the porewater pressure may become so high that many of the soil particles lose contact with each other. In such cases, the soil will have very little strength, and will behave more like a liquid than a solid - hence, the name "liquefaction".
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Water vapor. If all water vaporize u will receive NaCl (crystal)  in vessel.
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stick of dynamite.\n\nOk, I was just being silly, the other two ideas are good.\nA third way might be to create a whirlpool in the water.  I guess you could consider that a hole as well.
700454
One way to do that for relatively small volumes of water is to force the sea water through a special membrane filter under high pressure. The filter membrane must be constructed so that its holes are large enough to just pass a water molecule, but not large enough to pass metal\nmolecules, salt molecules, algae, etc. The result would be fresh clean water with a lot of brine solution left in the pressurized tank that needs to be dumped.\n\nAnother process which is more poractical for large volumes of fresh water production is electrolisis. In that process, electrical current is passed through the water to break it down into its basic elements such as hydrogen and oxygen (and all the other junk that is left over).\n\nOnce the hydrogen and oxygen are collected and recombined, the result is pure fresh water. Again, the vat or tank holding the original sea water now has a heavy brine solution which must be disposed of somehow. Most any use of sea water to produce fresh water will generate a lot of salty brine by-product that could poison sweet earth in the vicinity if it is merely dumped.
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Scientific theories behind the origins of sea salt started with Sir Edmond Halley in 1715, who proposed that salt and other minerals were carried into the sea by rivers, having been leached out of the ground by rainfall runoff. Upon reaching the ocean, these salts would be retained and concentrated as the process of evaporation (see Hydrologic cycle) removed the water. Halley noted that of the small number of lakes in the world without ocean outlets (such as the Dead Sea and the Caspian Sea, see endorheic basin), most have high salt content. Halley termed this process "continental weathering".
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Yes.....apply an electric current to salt water...I think this is the actual commercial method.
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the liquid evaporating
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Yes it did exist. The Mediterranean actually dried up around the end of the Miocene, about 5-6 million years ago. This was known as the Messinian Event. \n\nThere are large thick deposits of evaporite minerals like gypsum and halite (salt) that underlie much of the Mediterranean. These deposits were formed when the water in the Mediterranean dried up. Other evidence exists that shows that the Nile River actually cut down to several hundred feet below present day sea level, which would have been impossible if the sea level were not lowered to that depth. At the start of the Pliocene, about 5.4 million years ago, the barrier at the Strait of Gibraltar broke and the Mediterranean was filled again. \n\nI've studied much of this first hand working around the Mediterranean basin. If you want to see some references go to:\nhttp://www.soton.ac.uk/~imw/messin.htm\nhttp://www.messinianonline.it/
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I don't believe so. That's why it's called 'terminal'. The surface of water when hit at high speeds isn't any 'softer' than actual ground. It just looks more pretty.
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A project on geothermal activity in Indonesia.
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You can observe this yourself by breathing on a mirror. As the condensation evaporates from the mirror, you have completed the water cycle. Water evaporates into the atmosphere from the ocean, lakes, rivers, and from soil and plants, and even from your skin and breath. When the air reaches saturation (100% humidity) due to cooling or changes in atmospheric pressure (or both) the water condenses  from vapor to liquid (or solid) and falls to earth as rain, snow, sleet, hail, or maybe only as dew. This water may then form streams and rivers and return to the ocean where it may evaporate again into the atmosphere or it may sink into the earth where it becomes groundwater that may take many thousands of years to emerge again, or may be pumped to the surface from a well and used for drinking water or irrigation. It is a continuous cycle that may take only seconds or may take thousands of years to complete the cycle depending on the path of the water.   \n\nWhy do I get the feeling I'm answering your homework question? Now if you'd asked about delta O18 (a heavy isotope of oxygen) I could have told you how the water cycle concentrates water composed of hydrogen and heavy oxygen atoms and how this is used to study paleoclimates using ice cores and sea shells. Have a good day.
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if the water is at very very low pressure it can become gaseous.\n\nSee also - the triple point of water
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If it hits sand, it will often make glass.  It makes the ground very hot for a short time, having so much moisture around it draws the heat away quickly.
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You're asking about divining.\n\nWhen divining is tested using anything even remotely resembling a scientific test, it fails.  You can't find underwater pipes (tile in your question) or any other form of underground water that way.\n\nYou might resubmit your question to a group that covers perpetual motion, ghosts, or alien abductions.  You might get an explanation from them.