Is
it frozen yet? Every morning for the past few weeks, I’ve peered into the gray
dawn, looking for the absence of waves on the lake. If there wasn’t a choppy
surface, then I stared harder still, trying to determine if the reflection was
due to calm water, or a skim of ice. One morning the pink clouds reflected on
both ice and liquid, as a thin sheet filled my bay. The next morning, I
couldn’t see any open water.
I
gave the ice another frigid day and night before venturing down to its edge. Wind
had piled that first layer of ice up against the shore, and now the round
pancakes of ice chunks were frozen together in a jumbled mess. Cautiously, I
stepped out away from the shore, and stopped a minute to listen for cracking,
and feel for shifting. Solid. I shuffled out toward the smooth ice.
Two
inches of clear ice covered the deeper water. Silvery bubbles and crystalline
patterns decorated the black surface. Just under the ice, little blobs of
mint-green algae bobbed gently, barely moving in a gentle current. Even as the
ice was freezing, these little producers had been carrying out photosynthesis
and releasing oxygen bubbles, which left shimmering vertical paths in the ice
as they rose toward (but never reaching) the surface.
Strange
as it may seem, the surface of my lake has just become a mineral. Mineral is a geologic term, describing
solid substances with certain characteristics. Minerals are all around us, but
mostly overlooked. Let’s take a closer look at ice to see how it fits.
The
first criterion in the definition of a mineral is that it must be a natural
occurring, inorganic substance. The ice on my lake is natural occurring, of
course, but the ice cubes in my freezer are not. Diamonds made in laboratories
are not technically minerals, either. Ice doesn’t contain carbon and is not
derived from living things, which means it is also inorganic.
Minerals
must be crystalline solids, meaning that they have to have an orderly internal
arrangement of atoms. This means that water is not a mineral, the same way that
volcanic lava is not a mineral, since they are both liquids. As they cool,
though, their molecules arrange themselves into distinct geometric patterns.
You can see this in the hexagonal symmetry of snowflakes.
Each
mineral is made of a particular mix of chemical elements, and has a definite
chemical composition. The chemical composition of ice is, of course, two
hydrogen atoms and one oxygen atom per molecule, written as H2O. Apatite,
a mineral in your tooth enamel, is more complicated, and contains set amounts of
three elements, plus variable amounts of four more.
Speaking
of appetite, we are surrounded by minerals not only on a frozen lake, but also
at the dinner table (especially if we relax the definition of mineral to
include human-altered forms). The salt in your shaker is tiny crystals of the
mineral halite (also called sodium chloride, NaCl,). The leavening in your
pumpkin bread is sodium bicarbonate (NaHCO3). Both the pumpkin and
the turkey contain small amounts of calcium and iron.
As
you dig into the food on your plate (ceramic plate containing feldspar and
silica), with your grandmother’s set of heirloom flatware (silver) or your regular
silverware (made of iron, nickel, molybdenum, chrome, strontium, and neodymium),
be careful not to chip a tooth filling (gold)!
Give
thanks for the screws (iron and zinc) that hold the feasting table together,
the drywall (gypsum) that forms your cozy room, and the insulation (vermiculite)
that keeps you warm. Don’t forget the electric wires (copper) that power your
light bulbs (tungsten, silica), and the plumbing (copper) that carries the
remains of the feast away.
As
you settle your stomach onto the couch with a swig of pepto (bismuth), and
maybe crack a beer can (aluminum), I encourage you to give minerals a second
thought. They are all around us, bringing the beauty of snowflakes, the fun of
ice fishing, and the grace of good health.
“When
we cut the ripe [pumpkin], should we not give it thanks? And should we not
thank the knife also? We do not live in a simple world.”
From “At the River
Clarion,” by Mary Oliver.
For
over 45 years, the Cable Natural History Museum has served to connect you to
the Northwoods. Come visit us in Cable, WI, at 13470 County Highway M. The
current exhibit, “Deer Camp: A Natural and Cultural History of White-tailed
Deer,” opened in May 2013 and will remain open until April 2014.
Find
us on the web at www.cablemuseum.org to learn more about our exhibits and
programs. Discover us on Facebook, or at our blogspot,
http://cablemuseumnaturalconnections.blogspot.com/.
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