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Winter
2001, Premier Issue

by
Tim Steury÷ •÷ Photography by Robert Hubner
It
is early June.
Last evening’s rain has washed the air clean. The morning sun is
warm and assuring. Close-knit rows of grape vines, their young clusters
flush with promise, stretch across a south-facing slope above the
Walla Walla Valley. Chardonnay, Cabernet Franc, Barbera, each in
its appointed place. Here in the Woodward Canyon vineyards all’s
right with the world.
And
here in his vineyard, Rick Small (’69 Agriculture) talks as passionately
about soil as he talks about wine. Because they’re really the same
subject, to hear him tell it. You have to understand Small’s intensity.
He doesn’t slow down. He doesn’t pause. He just...keeps going.

“Winemaking’s
interesting because it’s so broad,” he says, “it keeps you fresh,”
hardly taking a breath, “there’s so much to learn, I’ve done this
for 20 years, now I’m 54, I knew I was going to do this by my late
20s, but I’m continually blown away by how much I don’t know yetÙ
“This
is great soil,” he says, crumbling some in his hand and smelling
it. “Like my dad said, you know what’s good about this soil out
here, it’s clean dirt. It’s got a good earthy smell, not sandy.”
Finally,
he does pause, looking across the valley to the bluffs on the other
side.
“I
would not be anywhere else in the world.”
This
land is his wine. And what we’re looking atæthis breathless sweep
of landscape, this soil beneath our feetæis what the French call
terroir. Place in a bottle.
Terroir.
Tair-WAHR. Whether or not they can pronounce it correctly,
terroir is on the lips of many a Washington winemaker these days.
The idea that the interaction of geology, soil, and climate can
affect the taste, complexity, and character of a fine wine is hardly
new, even within the relatively youthful Washington wine industry.
But the notion was revisited recently in a paper published by WSU
researchers Larry Meinert, a geologist, and Alan Busacca, a soil
scientist, in Geoscience Canada. In “Terroirs of the Walla Walla
Valley AppellationÙ,” Meinert and Busaccaæboth wine devoteesæreport
on their extensive analysis of the appellation and its soils, detailing
various vineyards and their soil, and resulting enological peculiarities.
Some
aspects of terroir, says Meinert, are fairly intuitive. If one slope
gets more sun and is warmer than another slope, it is likely to
produce more vigorous grapevines and better wine. But other aspects,
such as the rocks deep underground and events thousands of years
in the past, are less obvious in how they might influence wine quality.
As Meinert and Busacca explored the geologic terroir of Washington
wines they made some intriguing discoveries. “I was astounded to
find that giant glaciers reaching down from Canada 17,000 years
ago have had more influence on the wines of Washington than the
local volcanic rocks,” Meinert says. “Even more amazing, we are
discovering that many other great wine regions of the world have
also been affected by glacial activity.”
However,
eastern Washington’s terroir is not quite as straightforward as
a glacier. The next time you open a bottle of wine made from grapes
grown in Eastern Washington, think about what gave that wine its
personality. Think, if you will, about floods.
Think
about the greatest floods ever documented on Earthæabout a wave 500
feet high bursting through the ruptured ice dam of Glacial Lake Missoula,
sweeping south across Eastern Washington at 50 miles an hour. Think
about the brunt of 2,500 cubic kilometers of water rushing with a
flow 10 times greater than the combined flow of all the rivers in
the world, scouring the land to its bedrock bonesænot just once, but
as many as 90 times, as the ice dam repeatedly formed and failed,
over intervals of 35 to 55 years, beginning some 15,300 years agoæcreating
an enormously complex geological riddle and hundreds of publication
topics for scores of geologists since J Harlen Bretz first realized
how the tortured landscape of the Channeled Scablands was formed.
The
prevailing southwesterly winds, which still prevail and still continue
the geologic process, lifted the glacial sediments, the loess deposited
by the floods, carrying it back north, distributing it approximately
along the floods’ path, relinquishing finally what remained as the
thick loess dunes of the Palouse.
This
windblown silt deposited over the underlying volcanic basalt, layered
with the ash of intermittent eruptions of Northwest volcanoes from
Mazama to St. Helensæthis is the literal grounding of Eastern Washington’s
terroir.
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these
features in the November 2001 issue of Washington State
Magazine.
Mariner
ManiaA new hero surfaced every game. Ichiro,
Bell, Boone, Martinez, McLemore, Olerud, Cameron, Garcia,
Sele.
The Lagunas Secrets
On the shore of the Laguna Especial, some 30 locals
of all ages watch patiently, no doubt mentally rehearsing
the crazy gringo stories theyll share tonight over dinner.
The archaeologists are the best show on the mountain.
48 Hours with Peter Van SantPeter
Van Sant hasnt seen it all. But he hasnt missed
much either.
State Route 26 RevealedPepto
pig, abandoned barns, dueling windmills, poplar trees that
grow 15 feet a year. Revealing the soul of a highway.
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