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By Tamia Nelson May 10, 2005
The Schoharie Creek ran high and fast, swollen
with snowmelt and spring rains. The current surged against the trunks of
partially submerged willows and
sycamores. Looking up as I hurtled past, I spotted shopping carts,
countless plastic bags, one seemingly intact Volkswagen Beetle, and a dead deer
all high in the trees, all ensnared in the tangle of naked branches. It
was a salutary lesson in the force of moving water. The planet's surface bears
witness to this power everywhere, displaying the scars of giant waves
and surging
floodwaters, from deluges both ancient and modern.
Moving water always leaves change in its wake. On a river, nothing lasts
forever, but that's
The Tao of Flowing Water
A rising river first fills its channel from one bank to the other and then
spills out over the surrounding land. Even a bankfull river is fast and
powerful, but the Force is really with a river in flood abandoned cars
and shopping carts don't end up in trees without some doing. There's a lot
going on underneath the surface, too. From microscopic flecks of clay to
boulders the size of cottages, sediments are plucked from their resting places
and dumped somewhere else. And moving water doesn't just eat away at soft
earthen banks. Armed with the cutting tools that suspended sediments provide,
it erodes solid rock as well. A low, slow river also reshapes its channel, but
this work is done at a measured, leisurely pace. A lazy river approaches the
job with the laid-back attitude of a teen-ager, confident that there'll always
be another day to do what needs to be done. A river in flood is something else.
It's like an old man in a hurry. Change comes fast and furious. That's why the first paddling
trips of the season are often voyages of discovery,
even on familiar streams.
Hopefully, you won't be on many rivers while they're in flood. If
nothing else, it's a little disconcerting to hear a distant rumble and realize
belatedly that you're hearing boulders banging together on the
river bottom. But you don't have to ride the flood to see what the water's been
up to. You can read a river's history in the landscape, long after the
floodwaters have receded. It's a new way to
Read the Water
One frequently encountered relic of past floods is the sweeper, a toppled
tree whose branches hang down into the water, while its roots still cling to
the land. You'll most likely find sweepers at the outside of bends, where
floodwaters have undercut a bank. I use the word "encountered" figuratively, by
the way. Sweepers are best viewed from a downstream vantage point. The current
passes easily through the submerged branches, but paddlers don't. An unlucky
boater can be trapped in this vegetable snare like a moth on the grill of a
speeding car, and in a worst-case scenario the boater's chances aren't a whole
lot better than the moth's. Don't bet against the odds. The gentle susurration
of water as it washes through a sweeper is the sound of whispering
death.
Sweepers aren't confined to river bends, though. Nor are they always
solitary pickets. Sometimes especially on big rivers many
sweepers are
well
swept away from the land altogether, piling up in
great drifts of dead wood in the shallows. These driftwood islands, too, are
best avoided. Approach them, if you must, from downstream. R.M. Patterson,
whose Dangerous
River remains a paddling classic more than 50 years after it was
written, speaks feelingly of watching whole trees speeding by in the grip of
the muscular Nahanni current, now vanishing below the surface, now vaulting
free of the water altogether. Later, while camping on a gravel bar in midriver,
he clambered out onto a driftwood pile built up from many such wayward
sweepers. The trunks of the grounded trees quivered and thrummed as the Nahanni
swept relentlessly beneath them. Dangerous river, indeed! Had Patterson been
unfortunate enough to dump upriver of that deadly trap, he'd probably never
have lived to tell his story.
Moving water carries more than trees, of course. The gravel bar that
Patterson camped on was itself a legacy of past floods. Rivers are always
rearranging the dust, building new islands, raising new banks, extending sandy
spits and bars, and making beaches. Look
for these landmarks anywhere the current takes a breather: the insides of
bends, say, or the gentler reaches between major drops. But beware. Not every
river is a Nahanni. Streams in more "sivilized" latitudes transport almost as
much trash as natural sediment. That attractive-looking beach you're eyeing for
a lunch stop is likely to have broken beer bottles, strands of rusty barbed
wire, and splintered wood from discarded shipping pallets embedded in the warm,
inviting sands. The days of barefoot beachcombing are over. Be sure to go properly shod
whenever you explore afoot.
And that's not all. Nothing comes from nothing. For every new island or
beach, there's a new channel, eroded bank, or deeper cut somewhere upstream. If
the sandy spit you remember from last year is now an island, chances are good
that a flood is responsible. Each spring, rivers grind deeper into their banks
at the outside of every bend. Contractors and homeowners do their best to armor
"their" stretches of shoreline against the floodwater's annual assault, to be
sure, but it's a holding action at best, and doomed to failure. Whatever it may
say in the deeds registered at the courthouse, a river retains title to all the
land along its banks.
Sweepers. New islands. New channels. The ancient Greeks were right: you'll
never find a river the same as you left it. That's where scouting
comes in, and scouting puts us right
On the Riverbank
In some places the great rivers of the James Bay lowlands come to
mind, as do the coastal bayous of the American South and at some times,
it isn't always easy to tell where the water ends and the land begins. Yet most
rivers flow between well-defined banks, at least after the spring floods
subside. In the High Peaks of the Adirondack Mountains, for example, many
streams are constrained by rock walls for at least a part of their journey. But
even mountain torrents have to slow down eventually, and as they spill out onto
the plains, these lively streams dig deep into glacial till, sand, and clay.
Here they have a free hand to remodel the landscape. As we've already noted, a
river's appetite is most easily satisfied at the outside of bends. Even when
it's not in flood, it gnaws away at the bank, undermining the overlying earth.
To get a handle on what happens next, think back to the time before siege
howitzers and bunker-buster bombs, when stone walls were the ultimate in
fortification. If you wanted to bring a stone fort down in those days, there
was just one way to do it: dig tunnels under the walls and then blow the
shoring timbers out. The all but inevitable result? The walls came a-tumbling
down.
A river attacks the banks at the outside of its bends in the same way,
tearing at the underlying props. And sooner or later the riverbank, too, comes
a-tumbling down. You don't want to be standing on it when it does. Whenever you
scout a river, therefore, avoid the temptation to walk right out to the very
edge of a high cutbank in order to get a better view. You just might take more
of a trip than you bargained on.
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