Washington Wine Country

From afar, many believe the Evergreen State is a vast region blanketed entirely with majestic forests and days of endless rain and clouds. If you're west of the jagged Cascade Mountains, most of the area is forested with lush vegetation and a moderate, maritime climate. However, the spine of the Cascades causes a remarkable weather change, acting as a barrier that stops all but a few inches of rain east of the mountains. Envision then, a terrain covered mostly in sage and bunchgrass. In places, miles of wheat fields gently wave in the wind, hop-yards thrive, and large fruit orchards of apples, pears and cherries abound. Other than primarily the northeast corner of the State, much of Eastern Washington is an expansive upland desert.

The singular exception to this setting is the majestic Columbia River, flowing larger and larger as it meanders south through central Washington. It takes a dramatic curve to the west, cutting through the Cascades, forming the breathtaking Columbia River Gorge then finally reaching the Pacific Ocean north of Portland, Oregon. Were it not for the Columbia and its myriad irrigation canal tributaries, the wheat, hops, fruit trees, wine and table grapes and all of the many crops farmed in the State, simply couldn't survive.

In contemporary times, the Cascades, the Columbia River and the northern latitude are the essential influential factors affecting our State's unique climate, and ultimately, the burgeoning wine industry. But the story becomes more fascinating when considering several cataclysmic events that occurred over eons of time in the past.

No other grape growing region resembles Washington State. The land has been hewn from the 'Pacific Ring of Fire' and specifically the meeting of two tremendous tectonic plates, the Pacific Oceanic Plate and the North American Continental Plate. The eruption of Mt. Saint Helens was a poignant example of the tremendous colliding forces. From our home and winery, we have an outstanding view of Mt. Rainier, only 32 miles due east, certainly one of the word's most majestic volcanoes. Yet it's a contradiction in beauty and potential disaster. Below the thin crust of the earth, huge forces are at play. The Oceanic Plate is driving beneath the Continental Plate causing monumental pressure that when released, has resulted in the great volcanoes as well as the Cascade Mountain range. The primary mineral that dominates Washington's vineyards is igneous Basalt, a by-product of the tectonic phenomenon.

But the story of Washington's vineyard land is not complete without the knowledge of another remarkable event that happened about 17 to 20 million years ago. A volcano of immense proportion, the Grand Ronde (which today is most of southeastern Washington), spread immense lava flows, creating what is now the Columbia Valley. Much of central Washington is actually the remaining gentle slope of this vast ancient crater. Within the last 10 million years, the northward movement of the west coast (the Oceanic Plate influence) has caused the lava to buckle and form large folds, creating (for example) the Yakima Valley, one of the State's most important wine regions. The Valley's north and south rims are actually basalt folds, defining the Valley and separating it from the rest of the great Columbia basin.

The final cataclysmic entry in the history influencing Washington's vineyards occurred about 13 to 17 thousand years ago when a massive glacier, called the Cordilleran Ice Sheet pushed south from Canada, damming the Clark Fork River and backing up the waters into the high mountain valleys of western Montana. It formed Lake Missoula, a two thousand foot deep monster of some 500 cubic miles of water. Inevitably, the glacial dam broke, releasing possibly the world's greatest flood. It raced across what is now Eastern Washington, scouring away the soil and exposing the ancient basalt lava while forming deep ripples many feet high. The floodwaters dammed up behind a barrier close to today's Tri-Cities in south-central Washington, creating a temporary lake thousands of feed deep. The still water gradually released sediment in the Columbia Basin, depositing silt loam and pebbly quartzite carried by the great waters from as far away as the Artic Circle. This phenomenon reoccurred scores of times, possibly as many as one hundred.

The wines of Washington are the product of several cataclysmic events, ancient and powerful primordial events, coupled with today's dynamic tectonic interplay. Together, they have sculpted the essence of what is the foundation for a remarkably singular wine region, rapidly on its way to world acclaim.