Some people fall in love and find quicksand

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Cm Ab It won't rest until there's nothing left. Quicksand tabs Tabs. About the artist behind Quicksand Chords : Incubus is a Grammy-nominated alternative rock band based out of Calabasas, California. They are known for their eclectic sound, balancing experimental and progressive qualities with pop appeal, earning praise for their ability to change and evolve their music with every subsequent release. Their lyrics touch on a number of different subjects, from their earliest works which touch on drugs and anti-conformity to the later albums where they often sing about politics and romance, although they primarily stress an optimistic view.

Incubus has received both high critical acclaim and commercial success, reaching multi-platinum sales, as well as releasing several highly successful singles. The band started branching out creatively and earned mainstream recognition with the release of their album Make Yourself. By , Incubus became hugely successful with the single "Drive" and their follow up album Morning View. Today they remain one of the world's most popular rock acts, with their latest studio album, Light Grenades , reaching Gold certification and reaching 1 in the U.

Their music has also appeared in other media, such as the video games Halo 2 and Guitar Hero , and the films Stealth and Final Destination 2. Indexed at Wikipedia.

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Show us your talent, perform Quicksand Chords! Certainly, the physix of the whole thing has a lot in common with the dry form of quicksand. Corn kernels, soy beans, or wheat grain are much larger than your typical grain of sand, and have much smaller contact area from which a force chain can result. So a heavy weight placed at the top of a pile of grain can quickly displace the grain below and sink quickly. And those accidents seem to happen more often when the grain is being transferred out of a bin; usually an auger pulls the grain from the bottom of the bin as gravity keeps the grain flowing.

Pockets can develop in the bin as grain is pulled out from the bottom; to break up the pockets and keep the grain flowing people will sometimes jump into the bin, and they can find themselves buried very quickly. Growing up in farm country, I was always told if you fell into a wagon or bin of grain to not try to stand up; instead lie flat to distribute the weight over a greater area. Then again, I get no kicks from Champagne.

I saw something on Discovery channel…there is a similar phenomena in water when excess air or other gasas are released from the sea floor. The density of water is reduced and therefore, once buoyant objects…sink. The soil is beyond its saturation point, but because of the way it is stacked, it does not become a liquid.


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  5. Given an earthquake, or such, however, it will, and it poses a pretty big threat. One such example, from Japan, I think:. As I understand it, they got the buildings righted again afterward, and since all the oversaturated soil was gone, there was no longer a threat. When I lived in Vegas, some friends and I would go off-road trucking. There were certain places in the desert that if the truck slowed below about 30 m.

    It was a layer of superfine dust on top of the clay, just a few inches deep. From what I understand from the Mythbusters show on quicksand, the water has to be coming up continuously — an Artesian spring which comes up through sand. Sand on a beach is simply wet, there is nothing forcing additional water between the sand grains. The bay of Mt Saint Michel is a beautiful place and it is really tempting to go for a walk when the tide is low. If you careless you can find yourself trap in the quicksand and this is when troubles start, because if, for sure, you are not about to sank in the sand and if nobody helps you to get out , it will be difficult to extract yourself of it.

    Anyway you can visit the bay with a guide by feet or by horse and it is, somehow, a mystic experience due to presence of the Mont itself.


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    Beaches are not quicksand because the water migrates up into the sand after it has already been deposited by liquid force and consolidated due to wave action and the weight of the sand. If you have a water pocket in the depositional sequence it could theoretically become quicksand, but I have never seen anything like this. Although, a mobile dune could migrate into tidal pools or such and probably create quicksand. Depending on the sands mineral composition, it can cause it to have some buoyancy. Most river sand is sub-angular mature quartz.

    It is mature, because most of the softer minerals have been eroded into silts and clays feldspars in particularly.

    I suppose the current could probably undercut a bank or something and form quicksand at a deeper level also. Most alluvial sands have a dry density of about pcf within a few feet of the surface. Maximum dry density of alluvial sands by the Standard Proctor Method is usually around pcf. That tells you several things, mostly that the sand is relatively consolidated to begin with, and the pores between the sand grains are most likely in a state of positive pore pressure, not allowing water to migrate into the sediment package.

    In the case of water loss, the sands are going to remain compacted, but they are going to exhibit negative pore pressure, allowing water to migrate back into the package when it becomes available. The overburden of the existing sediment will keep the sand compacted though, even against the buoyancy of the sand grains.

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    Ok, about the sand dunes. Wind deposited aeolian sand is typically very mature, has well sorted grain sizes, and is rounded. Wind is a much more efficient erosional force than water, something on the order of about times. It also is very good at sorting sand, because wind can only transport the smaller particles, leaving the gravels behind.

    It also tends to pick up some silt as it is transported and deposited. I will state that aeolian sands are not entirely consistent everywhere. They can be beach or river sands that have been moved by wind, but in some instances they are actually glacial sediments glaciofluvial outwash. Essentially, these blew off the moraines from the last ice age. This is what the sandhills in Nebraska are. Density would increase as depth increased due to consolidation of the sediment from overburden.

    The silt is an important factor here though because ambient moisture will cause it to form a sort of weak matrix with the sand grains in the first 5 or so feet of sediment. Increased contact with moisture or any type of overburden will cause the matrix to collapse, but it makes for larger pore sizes in said upper layer. So aeolian sands have relatively more pore space than alluvial sands due to their small amount of consolidation.

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    This would allow for more water to infiltrate the package, along with increased buoyancy due to smaller particle sizes. The same could be said about a sand dune migrating into a tidal pool or small water pocket along a river. This also implies some things about Peorian Loess that I had not previously though of, but thats for a different time and place.

    Anyway, this was my first post. This is what allows you to build sand castles.

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    This is absolutely wrong. The effect that allows you to build sand castles is surface tension. The first was in south Alabama near a small pool of water found in the woods.

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    I stepped onto a sandy beach and quickly sank up to my waist. Apparently the pool was fed by a spring which flowed under the sand. They pulled me out slowly with quite some effort, and I was barely able to keep my shoes on. The ruins are reputed to be the best preserved anywhere, probably because the site can only be accessed after a strenuous eight mile hike, most of which is along a sandy stream bed.

    The guides warn all visitors of the quicksand, which most often forms on the downstream side of boulders, since the surface water flows around the boulder but the subsurface water is pulled upwards and suspends the sand. The quicksand forms at other spots as well, particularly near the edge of the stream on the inside arcs, and we learned to anticipate it after a while. For the most part, the quicksand is no more than calf or knee deep, and is really just an annoyance. In regards to dry quicksand, I remember my father telling me about a death at his chemical plant that often gave me nightmares as a child.

    An operator was filling a boxcar full of a very fine chemical powder, which my father likened to microbeads used for fiberglass repair. The powder was blown in through a large flexible hose, somewhat like an air conditioning duct. The boxcar was mostly full when the operator somehow fell in and sank to the bottom as if he were falling through air.

    The man apparently suffocated quickly, and was quite dead when they were finally able to fish him out. Clearly this quicksand is all a Chinese conspiracy to steal American shoe technology through the center of the earth. I was backpacking down Paria Canyon in northern Arizona, and repeatedly sank up to my knees. The areas of quicksand were small enough that I was able to get out with a bit of wading and squelching. Eventually I got pretty good at recognizing the good patches of sinking sand, and sometimes I would stand in it intentionally. This is where the shaking caused by an earthquake causes the solid sand layers to behave more like a liquid.

    This is best seen by buildings partially sunk into the ground after an earthquake. One of the phenomena accompanying this liquefaction is geysers of sand blowing upward as the surrounding sand settles, much like the graphic of an apple disappearing into the sand accompanying this article. Dry quicksand would require an outflow of gas, such as methane natural gas to unsettle the sand particles enough to behave as a liquid — not just air. I once fell into quicksand as a kid. The ground in question was super saturated and it was at least five feet deep according to the guys who pulled me out.

    Unlike the movies, I sunk very quickly, barely slower than I would have in water. In about 2 seconds I was chest deep in the stuff and scrabbling at the ground I had just stepped off of trying in vain to pull myself out. Similar to quicksand,sinkholes in bogs and marshes are much more deadly. These marshes are home to Bake Apples,and of course sinkholes,except these are no run of the mill sinkholes….

    Picture that you are on a dirt trail in a bog,and much like quicksand,the top of a sinkhole looks like normal solid ground some are commonly noticeable. You then walk upon some ground,and suddenly you are submersed up to the groins. Unlike quicksand,a sinkhole will suck an object down almost instantaneously depending on how solid the ground is. Of course there are the instances where you can step on the ground without sinking,but with enough effort…you will…almost like playing in the mud.