I have been fascinated by quicksand since I can remember. It was likely back in Moose Jaw, Saskatchewan, in the early 70's, something on tv that caught my attention when I was very young, perhaps the Ron Ely Tarzan episodes. I remember standing in some gooey mud in my rubbers in some bushes below an embankment north of our home, loving the feeling of the pressure it exerted on my rubbers, imagining what it would be like to sink into quicksand. I remember once when there was an ad on tv for some movie or show, I heard a baby crying, and then I heard one of my parents making a statement about a baby sinking into quicksand!
I rushed to the tv, only to see a woman yelling "You killed my baby!", and then showing a man spitting something white (saliva? phlegm?) out of his mouth. I never seen the ad again, so I don't know what it was from.
Years later, when we lived in Beausejour, Manitoba in the mid to late 70's, I read a Reader's Digest book that had a section devoted to quicksand, with stories, experiments, and explanations (I also frequently looked it up in various encyclopedias, finding limited description). Following what I learned from the Reader's Digest book, I began to start making my own quicksand using sand in a funnel attached to a hose, and then a pail with a hose stuck in it. Then, a friend of mine introduced me to a sand quarry (The Sand Pit), where they pumped fine silica sand from a man(quarry)-made lake into an area surrounded by a dike of sand, which was steadily built up into a hill, to be later trucked away to be made into glass. The top of that area had nice quicksand, only a foot or so deep at the high spot where the pipe was, but deeper at the edges closer to the circular dike, where the water pooled, making the water in the sand there slow to drain away. When my friend first took me there, I had no idea what it was going to be like. When I saw him start to sink, I got scared and yelled for him to get out, fearing that he would disappear!
After seeing him only sink a foot or so down, I was still apprehensive about trying it out. But a week or so later, I tried it out, and was hooked!
I got familiar with the characteristics of the area, such as what I had described above, and noticed how it would settle quickly. I found it to be the best way to spend my summers!
Then, I sexually matured, and found new "feelings" coming over me when I played in it, as well as in sticky clay north of Gimli, Manitoba, along Lake Winnipeg, and walking through some peat mud in southeastern Manitoba, with me "wetting my shorts" before I got out of those spots!
I also began to have "wet dreams" about it
, forcing me to "relieve" myself in a controlled manner to end those embarrassing episodes.
When the sand sucking operation halted for a while, I began going biking and hiking in search for new spots, but wasn't getting any luck, except for around Gimli (hadn't gone far enough from Beausejour yet).
After we moved away, to Kamloops, BC in 1980, I tried to put it behind me, to start with a clean slate. But after a month or so, I decided to walk along a section of the South Thompson River, where I encountered clay mud!
It was too close to civilization for playing in, but seeing it (can't remember if I tested it out, bus saw another kid walking through it) opened a gigantic floodgate, my feelings went into overdrive!
It was almost like a sickness, and it took weeks for things to calm down. After that, I began scouting for mud locations, first around Kamloops, then around Vernon BC after moving here in 1988, and over the years, have become quite expert at it.
I like quicksand for the way it locks up when you tug at it, and its perceived suffocating threat by common folklore. But, in a practical sense, the fact that it has a very short "shelf life" when disturbed, namely the settling and packing of the sand grains as the water rises out of it, makes it not as good as other substances. It also has a high density, making it harder to sink deep.
But, if it is deep and loose enough (
really loose deeper down), then the experience could perhaps be more fun!
I love quicksilt, because it has the same locking properties as quicksand, but has a finer texture and doesn't settle as quickly if there is some clay mixed in. Some silts do seem to pack quickly, but I have some that takes weeks to get hard. It feels smoother, and when looser, it can be mushed into a claylike consistency.
But, just like quicksand, it is of a higher density, reducing the amount you can sink. But still, its longer "shelf life" makes it much more enjoyable!
Clay is also a very wonderful sinking substance that I love, being all sticky and gooey, with a really smooth texture!
It doesn't pack hard, unless it dries out. Also being a mineral-based sinking substance like quicksand and quicksilt, it also has a high density, making it more difficult to go deep, although it can be done if the clay is thick enough to hold you in place past your buoyancy point (but you may have to go in at an angle).
Organic mud is another of my favorites, ranging from coarse peat to really fine stuff, with the finer stuff being the best!
Finer organic mud can have a sticky texture like clay, but being organic, is of a lower density, and therefore is easy to go under in if it isn't too stiff.
Being organic, it also undergoes decomposition, forming swamp gas which bubbles or farts out of it, adding to the experience/effect!
It doesn't pack, unless it dries out.
I tend to currently find most access to quicksilt, organic mud, and quicksand. I find quicksilt best for a slow sink and getting stuck in a wonderful-feeling substance that you have to fight with to escape, while I find organic mud best for deep sinks, especially vertical submergences, and prefer the finer textured, better feeling, stuff over the coarser stuff. Pure quicksand, I find too limiting, although if I find stuff with enough water content to sink past my stomach, then it may be more fun.
I have yet to locate a good clay spot locally, but unfortunately, it is in limited supply in the mountains where there are fewer people, and is mostly in the valleys, where all the population is.