Let Your Story Shine – Flights of Foundry 2024
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Secrets and Mysteries of Rafting the Grand CanyonSecrets and Mysteries of Rafting the Grand Canyon
So, for the next month and more, this blog, or at least most of its available posting space, has been claimed by a fan of the Grand Canyon. Yes, a fan of a really big hole in the ground. It’s not as big as Valles Marinaris, but there is still a river at the bottom of the Grand Canyon, which greatly facilitates travel by river raft. The goal is to take you along on a fourteen-day expedition, from Kaibab Sandstone to Vishnu Schist, through rapids, slot canyons, waterfalls, and thunderstorms, and along the way reveal a few of the deep dark secrets of these trips so few of us take. We’ll cover over 180 miles on the river plus many miles afoot on canyon trailways. Why use up a month to take you on a two-week trip? Because that’s what it feels like. You forget what day it is, how long you’ve been gone, how much time is left. If you don’t keep a journal, you’re lost.
I kept a journal.
I also took about 3,000 photographs and an hour of video.
Yes, there will be a fair amount of “what we did”, but I also want to share the background information the guides (and other travelers) shared with us, the additional tidbits I’ve gleaned from research (the addiction of the Ph.D.), and perhaps even paint the picture well enough that if you can’t go on this trip you can claim you did and provide your friends with a verisimilitudinous description. Just pick one of the falsified names in the diary segments & say “yeah, that’s me”. Also, if you’re a well-heeled adventure traveler planning your own expedition, I’d hope you’ll come away with enough information to know where you should not take short-cuts—and with some clues about how to find experienced, capable guides to get you through safely.
In the meantime, I don’t want to wear out your eyeballs with more than a few photos and a thousand words of gushing per post. There will be directions to see more photos, but, I promise, this won’t be a session of “Watch my Vacation Slideshow”.
Time for the first installment of Secrets of Grand Canyon River Rafting.
Deep, dark secret #1. Not everyone wants to go on this trip. Three husbands who could have joined their wives refused the chance to walk away from work, television, and electronic connectedness for a week. A young backbacker—who had completed the climb of Mount Whitney with his mother just a few months previously—turned down a free ticket and sent his retirement-age Mom on her own. She said he didn’t like the idea of not being in control on the trip. Another traveller’s wife sent him off with a (female) friend he’d recently reconnected with after a thirty-year hiatus, because the wife just can’t stand camping. His son, a golf enthusiast, only agreed to chaperone them if they took the shorter trip, to be sure he’d be home in time to watch the Master’s. Me? No, actually, I didn’t want to go on this trip. The only person who couldn’t tell was my husband, he was so excited about going. Why would this nature/science/ancient-peoples-loving photographer want to sit this out?
First of all, it’s frightfully expensive—if you want to travel the Canyon and not spend a fortune, you need to be able to work there. I am not the correct age or physical type to start a new career as a river guide. Nor do I have the right background or training to get hired by (or even volunteer for) the Park Service or any of the scientific research teams with feet on the water down there. So when my husband Clark declared that it had “always” been his wish to make this trip and that he had, after all, a big landmark birthday coming up, I made him pay for it out of his IRA. That was the only place we had enough money set by.
Second, Clark got the idea from a friend of his, a childhood friend who’s facing the same landmark birthday this year. When these two get together, they tend to devote a significant amount of our time to recalling those good-old-days. Days I did not share. Oh, great, my jealous heart predicted: two weeks of traipsing along behind while they play “remember when.” Well, I did end up trailing along behind, but not quite the way predicted. You’ll see.
And the third and most sensible reason: I broke my shoulder in January and my orthopedist’s solid opinion about my going river-rafting in April was: “I wouldn’t recommend doing that.” The bone knitted on schedule, but shoulders are complicated messes of tendons and muscles that don’t take kindly to the whole process. I was told it would be a year or more before I’d be back from this injury. My physical therapist did what he could to get some of my range-of-motion restored and added a couple of exercises to build back a little strength, but I went off with one arm fully-qualified to hang on tight and one that complained bitterly about any extension beyond a basic stretch while it simply refused to raise my hand beyond about 80 degrees. One upside was that Clark got to haul all my gearbags, because I just couldn’t handle them.
The other upside is that I would not want to have missed out on this trip. Even though we couldn’t afford it, it was worth it. Does that make any sense at all? Well, it will.
So, all right already, let’s go. For a teasing sneak-peek, here is a picture from Day 5. Oh, aye, it’s the Grand Canyon.
Chasing CometsChasing Comets
As a re-entry activity, let’s fall right into the project which inspired the overarching theme for this so-called blog: cometary tails. That is, in this instance, we’ll be “studying” the behavior of the tails of actual comets falling along their orbits about a star. But of course, this is a “Messy Monday” project, so it involves running, arguing, and playing with scissors (not all at the same time).
So far, the only star whose comets we’ve observed have been those of our own Sun, but as our star is not particularly unusual, it’s likely that comets ply their trade throughout the cosmos. We’ll not be delving too deeply into astrophysics, instead we’ll be building fun models of comets and playing games which illustrate the apparent motion of a typical comet’s tail. If you’re running this project as part of a school science program, you can double-count the activity as a P.E. session, as the central game involves more than a bit of running, though not likely moving as fast as a comet.
Just as a reminder, what I want to give you in these “Messy Monday” project descriptions is 1) enough background on the science that you’ll be prepared for questions and have resources to draw on if your own curiosity is triggered, 2) a play-by-play description of running the project with a group, recognizing that your time and resources are limited and your participants will vary in both interest and prior knowledge, and 3) a shopping list detailed enough to help you minimize your costs as well the time you have to spend assembling supplies.
So, What Do You Want to Know?
For thousands of years, humans have wondered at the strange visitations of comets.
In our time, people now understand that comets are not harbingers of doom or annunciations of the births of kings but fellow travelers in our solar system, icy bodies wheeling in towards the sun and shedding a fraction of their substance as they approach the sun. However, a key aspect of the comet’s tail remains counterintuitive to us earthbound air-dwelling creatures. The tail of a running horse flows behind her as she gallops, so we naturally expect that the tail of comet simply flies behind it as it plunges along its course. But a comet’s behavior plays tricks with such expectations.
Where do comets come from? The Solar System is a big place, but for most of us, the territory ends with Pluto, the Object Formerly Known as The Ninth Planet.
However, if you’re a fan of Cosmos (either Carl Sagan’s or Neil DeGrasse Tyson’s version) or if your school is lucky enough to have new textbooks, then you’ll know about the Oort Cloud , that sphere of orbiting material from which most comets emerge. Do you realize how much farther out this region is? On a scale of one inch per 100,000 miles, in which the orbit of Pluto would be one mile across, the distance from the Sun to the Oort Cloud would be the length of the state of California. It’s even been hypothesized that the Oort clouds of neighboring stars may physically interact, exchanging comets.
The Oort cloud is a long way out, but it’s still a part of the Solar System, because the objects there are still subject to the Sun’s gravity. Occasionally, a piece of this clutter is jostled from its orbit and begins the long fall towards the sun. Depending on the path it takes as it zooms around the sun, the comet may slingshot out of the solar system entirely or it may settle into a new orbit, returning to loop around the sun on a regular schedule. For instance, Comet Halley returns every 86 years. The last time round, it actually came in ’86–1986 that is. I was lucky enough to visit New Zealand that year, so I can confirm that Comet Halley was extremely unspectacular that year–only just barely visible. Fortunately, New Zealand itself is spectacular every single day of any given year. NASA was more successful, having a noticeable advantage in telescope access.
But why do comets even have tails? We don’t see shiny tails glowing in the wakes of our planets. Well, it all has to do with the change in environmental conditions as the comet moves towards the Sun. Comets are composed of water ice, frozen gases, rocky matter, and even traces of organic compounds. As this frozen jumble approaches the sun, it warms up enough that the various ices in the outer layers of the comet become gaseous—water vapor, ammonia, carbon dioxide. These gases bubble and boil into a misty cloud, so the comet will have an atmosphere of sorts, called the coma, for the duration of its passage through the inner Solar System. The gas expulsions may even shoot out of the comet’s rocky layers like jets, causing the comet itself to tumble as it falls along its inward path. At the same time, very small-scale “dust” particles are swept from the cometary nucleus. This is not the heavily-organic dust we find under our furniture here on Earth (if you really want to know what’s in household dust don’t use “Google images”; stick to text searches or just ask your friendly neighborhood allergist). What we mean is that the particle size—a few microns—is extremely fine, about the same size as the particles in cigarette smoke.
We get our fabulous cometary tail once these newly-ejected gases and dust of the coma approach the sun just a bit closer, enough that the various solar emissions can have their ways with the comet’s atmosphere. First, there is sunlight itself, which acts in several ways to provide us with the visual spectacle of the comet’s tail.
The simplest role of sunlight is to shine on the cloud of dust ejected from the nucleus. That’s the main tail we see. But that still doesn’t explain why the dust forms a tail at all: the secret is that light, as electromagnetic radiation, actually exerts pressure on objects, and with tiny objects like cometary dust this radiation pressure force is enough to fan that material out from the core. Plus, there is a cool bonus “secret”: that most comets actually have two tails—one formed by the gases and one formed by the dust. The ultraviolet radiation in sunlight blasts the gas particles, stripping away electrons, and so creating a mass of ionized gas, which fluoresces (mostly blue) in sunlight. Then those glowing blue ions are blasted in a straight line away from the sun by the solar wind, a stream of high-energy particles hurtling at supersonic speeds through the solar system. The solar wind is a wonderfully intricate system in its own right, but for our purposes here it is most important to convey that, like earthly winds, it consists of particles moving at high speeds and that its direction is away from the Sun.
The result of all these combined forces is that a complex, continuously shifting cloud of gases and dust streams out from a comet during its time in the inner solar system and that tail—or, rather, pair of tails—points away from the sun, even when the comet is on its way back out to its origin. (If you’re a die-hard comet enthusiast, you’ll know that the dust tail does curve inward a bit, as the small particles of dust battle with the solar forces, striving to curl into their own individual orbits about the sun, but from our earthly perspective, the outward forces have the upper hand.)
In the next installment, we’ll get down to the nitty-gritty of building our own comet models and playing a game of As the Comet Tail Flies.
Oh, yeah, and I’m not making things up about radiation pressure. Consider the prospects for spaceflight under the power of light!
On Aisle 42, Universe Components: The Atomic Marshmallow ProjectOn Aisle 42, Universe Components: The Atomic Marshmallow Project
Now that you have all of your supplies ready, it’s time to guide your group through the construction of a model atom.
Start by handing out the marshmallows and ice-cream topping pieces. With younger participants, it can maintain focus if you mention that there are extra supplies for snacking on afterwards.
Start with the marshmallow. Most of an atom is empty space. And most of a marshmallow is nothing but air frothed into sugar. So this marshmallow represents the “empty” space of an atom. For older participants, you can encourage them to think of the sugar of the marshmallow as representing not only the energy that permeates what we call “empty” space but also the forces that hold the atom together.
For a very long time, the atom was believed to be more-or-less of uniform density, an amorphous mixture of tiny negative particles called electrons swirling around in a positively-charged “pudding.” In 1911, Ernst Rutherford and his team completed a series of experiments that shocked the physics community by revealing that most of the mass of an atom is concentrated in a tiny, central nucleus containing all of the positive charge. For our model, in honor of Rutherford, we’ll build a helium (He) atom, which has a nucleus containing two protons and two neutrons. (Much of Rutherford’s research focused on the alpha particle–which happens to be exactly the same as a helium nucleus.)
Let your dark-colored candies be protons and your light-colored candies be neutrons. (It doesn’t really matter, but textbooks often draw protons as dark dots and neutrons as white dots.)
Using the wooden skewer or toothpick, drill a small hole in the side of the marshmallow. Now use the same toothpick or skewer to push those nucleons (a word which here means “candy pieces representing protons and neutrons”) into the center of the marshmallow.
This is a good time in the activity to stop lecturing and instead gather suggestions from the participants and sketch their ideas on a board if you have one, or to gather around some sketching paper for discussion purposes. You can expect to see pictures that look much like a planetary system, because that’s the way the atom often (still!) is drawn in textbooks. You might have a knowledgeable participant who’ll shout out something like, “Shells! The electrons are in shells!” or “They’re in the Cloud!” Regardless, during the discussion, build on these volunteered suggestions to reach a description of the electrons as whirling around the nucleus in a cloud, going so fast that you can’t really tell exactly where they are, only that you know roughly how far they are from the nucleus.
At this point, we have a positively charged ion, because we haven’t added any electrons yet. A helium atom needs two electrons, negatively-charged particles, to balance out the two positively-charged protons. Once it was established that the positive charge is concentrated in the nucleus, where did researchers decide that the electrons belong?
Our helium atom’s two electrons do indeed share an electron “shell”, a layer of electrons a known distance from the nucleus. So let’s put a very thin, energetic, sparkly shell around our atom.
Before setting up the shell supplies, pause to demonstrate the procedure. If you’re working with younger students, you may need to stress that everyone will get their turn. If the “mess” part of the activity is an issue, set up a protected area where the messy activity is OK and let the participants queue up to build their atoms in assembly-line fashion.
To create the “electron shell” skewer the marshmallow firmly on the wooden stick, then very briefly dunk it into the water, then tap off any excess water into the water container. Tapping off excess water is important, because otherwise the marshmallow can get soggy, which makes for a less-attractive candy atom.
Each group needs a container with about a cup of water in it and another container with a packet of dry gelatin mix emptied into it. (For fun, choose a gelatin color in keeping with whatever events are ongoing, or a local sports team’s colors…anything to drive interest.)
Finally, gently swirl the damp marshmallow in the gelatin mix.
Set the decorated marshmallows aside on a sheet of waxed paper or a plate.
As time permits, participants can make other atoms…stuffing different numbers of protons or neutrons into marshmallows and adding a shell of electrons.