WILLAMETTE VALLEY AVAs: BORN FROM FIRE & WATER

200+ MILLION YEARS IN THE MAKING—VOLCANIC BASALT AND MARINE SEDIMENTARY SOILS DIFFERENTIATE THE VALLEY AND MAKE IT UNIQUELY PERFECT FOR GRAPE GROWING.

This article content was aided by/adapted from information and imagery courtesy of the Oregon Wine Board via a Creative Commons License.

Willamette Valley AVAs Cristom Vineyards & Partners

SUBDUCTION > IRRUPTION

The Willamette Valley is located within the “Ring of Fire,” an area of volcanic activity (75% of the world’s volcanoes and 90% of the world’s earthquakes) surrounding the edges of the Pacific Ocean. Just off the coast of the Pacific Northwest lies the Cascadia Subduction Zone (CSZ) caused by the Juan de Fuca Plate moving east toward the North American Plate (continent) and subducting underneath it. 

The Willamette Valley and its unique soils and topography are the result of hundreds of millions of years of volcanic activity. Over 200 million years ago, Oregon was under the Pacific Ocean. The gradual subduction of the Juan de Fuca tectonic plate created Oregon’s oldest mountains and added land mass. 

Roughly 16-6 million years, the plate continues to subduct, uplifting sedimentary soils, such as Willakenzie and Wellsdale, developed from sandstone and siltstone on the ocean floor to form the Coast Range above water and land mass in the Chehalem Mountains, Ribbon Ridge, and Yamhill-Carlton districts. 

Multiple fissures created one of the largest volcanic events on Earth, and lava flows throughout northern Oregon, creating Basalt bedrock that formed the valley and the Cascade Mountain Range and accumulating enough landmass for Oregon to be above water. Over the millions of years that followed, the weathering of the Columbia River Basalt bedrock created the basalt soils that form a patchwork of volcanic soil series predominantly found in the Chehalem Mountains, Dundee Hills, McMinnville, and Eola-Amity Hills sub-AVAs.

Willamette Valley Subduction of Juan de Fuca plate
Willamette Valley Volcanic Irruptions map 16-10MM Years Ago

THE VALLEY AT LARGE

The Willamette Valley stretches 150 miles (240 km) long – from the Columbia River in Portland in the north to the Calapooya Mountains outside Eugene in the south – and 60 miles (97 km) wide. It is largely protected by the Coast Range to the west and the Cascade Range to the east. The valley experiences damp, cool winters and warm, dry summers. It has an extended growing season due to the northern latitude providing extended daylight hours, which are tempered by a large diurnal temperature shift from day to night. 

The AVA was established in 1983, and subsequently, sub-AVAs were formed within its borders which now total 11.

Willamette Valley AVA_boundary_map_credit Willamette Valley Winery Association

Willamette Valley AVA Map courtesy of the Willamette Valley Wineries Association

45° NORTH: EOLA-AMITY HILLS AVA

Halfway between the North Pole and the Equator, and the same latitude as Burgundy, lies the Eola-Amity Hills (EAH) sub-AVA of the Willamette Valley, home to the 45th parallel North and the Cristom Vineyards Estate. Both experience similar daylight lengths and cool climates. Though, they differ in soil types.

The north and east sides of the AVA and the upper hills are predominantly Basaltic soils, including Jory, Nekia, Witzel, and Gelderman, among others, while the west has a concentration of Sedimentary soils. Missoula Flood Silts can be found along the lower-lying edges surrounding the EAH. It is common to encounter multiple soil types in a single vineyard, depending on its altitude. This JancisRobinson.com article provides more insight on the soil’s impact on the wines of this region.

Soils of the Eola-Amity Hills_Credit Oregon Wine Board

The Eola-Amity Hills AVA is influenced and primarily defined by the predictable, cool afternoon breezes that blow off the Pacific Ocean and enter the valley through the Van Duzer Corridor, which is due west of the region. These winds significantly temper the vineyard temperatures after warm sunny days, cooling the fruit to create small berries with great natural acid retention and thick skins, which leads to a higher skin-to-juice ratio in winemaking.  

Wind in Oregon map

The Cristom Estate is nestled into an east-facing volcanic hillside that rises from 200-800 feet in elevation. We are stewards of five world-renowned estate vineyards – tributes to our founders, Paul and Eileen Gerrie, and family matriarchs – which are unique in their varied aspects, richly diverse soils, clonal diversity, and micro-climate.

Our east-facing orientation allows the morning sun to warm the patchwork of volcanic soils across the Estate, which range from shallow – only 18-24 inches of topsoil before transitioning to fractured Basalt parent material – to deep – over six feet of topsoil. This soil diversity is a true hallmark of our property and lends itself to diverse single-vineyard bottlings and harmonious cuvées, such as our Mt. Jefferson Cuvée Pinot Noir.

Cristom partners with several esteemed neighboring vineyards that contribute to our flagship Pinot Noir. Additionally, the 2021 vintage included single-vineyard designates from Eola Springs and Seven Springs vineyards, and the 2022 vintage sees the launch of a single-vineyard Pinot Noir from nearby Björnson Vineyard, from whom we also source Gamay fruit for our AVA blend. Witness Tree, our direct neighbor to the north, and Five Points vineyard have provided the Pinot Noir we use to craft our Rosé. Beginning with the 2021 vintage, we crafted single-vineyard Chardonnay from Royer and Seven Springs vineyards.

The wines from the Eola-Amity Hills AVA are bright, fresh, and structured, with a slightly darker and edgier personality creating a balance of tension and generosity. 

THE ‘RED HILLS OF DUNDEE’: DUNDEE HILLS AVA

The Dundee Hills are defined by the ancient (15 millon years), deep Jory volcanic soil, volcanic basalt known for excellent drainage and the oxidized red coloring – famously known as the “red hills of Dundee.”

Additionally, the climate is slightly warmer than other Willamette Valley AVAs due to its position between the Coast Range and Chehalem Mountains, which shelters it from Pacific Ocean breezes.

Dundee Hills AVA map

Oregon wine pioneers David Lett of The Eyrie Vineyards, Dick Erath, Erath Winery, and Susan Sokol and Bill Blosser planted many of Oregon’s first vineyards in the mid-1960s to early 1970s in what would later be established as the Dundee Hills AVA in 2004. 

Cristom has a partnership with pioneering Arcus and Durant Vineyards, both established in 1973. The fruit we source comprises our Dundee Hills AVA Pinot Noir blend, as well as our Durant Vineyard Pinot Noir.

The wines from this AVA are pure and elegant, offering distinctly bright, penetrating red fruit and florals in cooler vintages to notes of plum, earth and chocolate in warmer vintages.

COAST RANGE FOOTHILLS: McMINNVILLE AVA

Vines in the McMinnville AVA are planted in some of Oregon’s oldest and most geologically complex soils. Thin topsoil on top of unique marine bedrock, called the Nestucca Formation, forces vine roots deep into the earth, causing them to struggle and resulting in dark, complex flavor profiles.

Similar to the Eola-Amity Hills, the region is influenced by the cool ocean winds blowing through the Van Duzer Cooridor to the south. The effect is the same – the cool and dry microclimate leads longer hangtimes, producing distinctly pronounced wines with bright acidity, great structure, and increased tannins.

McMinnville AVA map

Cristom has a partnership with pioneering Hyland Vineyard (est. 1971, one of the oldest vineyards in Willamette Valley) and Meredith Mitchell Vineyard (est. 1988 with own-rooted vines). The fruit we source comprises our McMinnville AVA Pinot Noir blend, as well as our Meredith Mitchell Vineyard Pinot Noir.

The wines from the McMinnville AVA are intense, with powerful tannins, high acidity, and fruit-forward profiles displaying flavors of dark fruit, spice, earthy, and mineral notes. 

AN EXPRESSION OF TIME & PLACE

Cristom Vineyards was established in 1992 by the Gerrie family to grow and craft distinguished wines of place that honor individual sites and traditional techniques – which extends beyond our own estate vineyards. Since our founding, we’ve also sourced fruit from world-class vineyard sites across sub-AVAs within the Willamette Valley. 

This fruit is vinified using the same neo-classical methods — whole-cluster fermentation (Pinot Noir) or whole-cluster pressed (Chardonnay) and native yeast fermentations — indicative of our hallmark style. Barrels are selected to add complexity, texture, and layers to our Mt. Jefferson Cuvée Pinot Noir and Eola-Amity Hills Chardonnays and our AVA Series Pinot Noir. Some barrels are designated to craft dynamic single-vineyard Pinot Noir and Chardonnay expressions that translate a specific site and vintage. All of these wines offer the opportunity to explore structured, cool-climate, volcanic Pinot Noir and Chardonnay from the Willamette Valley of Oregon.

Cristom flagship Mt Jeff Pinot Noir + EAH Chardonnay

AN EXPLORATION IN TERROIR

Cristom’s flagship 2022 Mt. Jefferson Cuvée Pinot Noir and flagship 2022 Eola-Amity Hills Chardonnay as well as our single vineyard Chardonnay, Winery Exclusive Pinot Noir, 2022 Gamay Noir, and Gathering Kits featuring our AVA Series and Single Vineyard Partner Grower Pinot Noir highlight the distinctive profiles of three of Oregon’s premier AVAs mentioned above. Many of these are winery-exclusive wines, available for purchase in our online shop or in our tasting room.

Cristom Vineyards AVA Series Pinot Noir 2021
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