Places & People

The Latest Crop in the Local Food Movement? Wheat

Kristan Lawson from modernfarmer.com published a remarkably important article last summer discussing how wheat is experiencing a renaissance with small farmers revolutionizing the local food movement by growing heirloom and landrace grains with unique terroir. The article so effectively conveys the message we at Palouse Heritage champion that we wanted to feature it here in our blog. The author quotes our dear grains scientist from Washington State University, Steve Lyon and even mentions two landrace grain varieties we are growing, Red Fife and Sonoran Gold! Here are the highlights. You can read the full article on modernfarmer.com here.

Ripe wheat on Camas Country Mill in Central Oregon, Courtesy Tom Hunton and modernfarmer.com

Ripe wheat on Camas Country Mill in Central Oregon, Courtesy Tom Hunton and modernfarmer.com

Until very recently, small farms have tended to avoid planting wheat because it's not very profitable per acre. Commercially, wheat is grown in such vast quantities that it's usually sold not by the pound but by the ton. For centuries, society has considered wheat a faceless "commodity" like iron ore or cotton, every sack anonymous and interchangeable.

But that’s all about to change. Wheat is experiencing a renaissance as chefs, food writers, and savvy consumers discover that each kernel holds a universe of long-forgotten flavors, a terroir: Wheat from one area tastes different from the wheat in another, and each varietal has a different flavor profile from the one down the road.

And when wheat is no longer treated as a high-volume/low-price commodity, small farmers can start commanding top dollar for unique grain grown in a unique way on their unique land.

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But is it really possible to tell the difference between heirloom wheat hand-tended in small plots and nameless factory wheat? When you come right down to it, it’s all just … wheat, a flavor that’s always in the background, never the star. In fact, in blind taste tests, even top wine experts can’t tell different wines apart. Aren’t wheat terroirs just as indistinguishable?

No, says Dr. Stephen Jones at the Washington State University Bread Lab. As a leading expert in wheat genetics, he’s proven that different wheat strains and growing conditions do produce unique flavor profiles. “We do taste tests all the time in our lab with bakers, chefs, students, and even random visitors. People notice big differences in wheat flavor based on where it’s grown—especially when it’s fresh-milled 100-percent whole wheat. That’s where the flavors are.”

Although wine connoisseurs have developed an entire vocabulary to describe the subtle aromas hidden in a glass of Zinfandel or Chardonnay, the specialty wheat dialect is still in its infancy. “Sadly, we don’t yet have terms for all the different flavors in wheat,” says Klein. “But we’re working on it.” Taste-testers at the Bread Lab have volunteered such expressions as “nutty,” “earthy,” “bright,” “chewy,” “warm,” and “gratifying.” It’s a start.

Modern American farmers did not invent the notion that specific varietals of wheat from various geographic regions have different flavors; you can trace the concept back to Italy centuries ago, where each Italian region championed the quality, texture, and taste of their own wheat pasta over all others. The recent rise of major nationally distributed pasta brands eroded the regionalism, but now Italian pasta terroir is making a comeback, too. Companies like Rustichella d’Abruzzo have begun to release pastas made exactly as they were in the 19th century, such as their “PrimoGrano” line which exclusively uses hyper-localized ancient wheat strains only discovered in the hills of the Abruzzo region; a handful of acres are harvested and processed using traditional methods to make a single batch of pasta once per year, released to connoisseurs like the rarest of wines.

Just as there is no “best” type of grape, there is no single all-purpose heritage wheat “better” than the others. Small farmers are re-discovering that ancient wheat strains, known as “landraces,” each excel in different culinary contexts: Red Fife, originally from prehistoric Anatolia but perfected in Canada, is unbeatable for bread flour, for example; Sonora Wheat, the first wheat brought to the Americas by Spanish conquistadors, makes the perfect tortilla; Mesopotamian Durum, the grand-daddy of them all, dating back 9,000 years, is the basis for impeccable pasta.

When applied to wheat, the term “landrace” refers to any ancient variety cultivated so far in the past and for so long that it evolved to thrive in a specific ecosystem; nowadays these primitive types are cherished as the source of wheat’s genetic diversity, which is otherwise being lost as modern high-yield strains dominate all others. The very word “landrace” is appropriate here as well, since “land-” in this context means both “regional area” and “the ground” (while in botany “-race” means “distinctive sub-variety”), so “landrace” is the native English word closest in meaning to the French terroir.

For American farmers, the difficult part about marketing these heirloom strains is convincing consumers to give wheat a second look. You can only charge a premium for specialty wheat if customers are willing to pay. Paul Muller, co-owner of Full Belly Farm in Guinda, California—who grows the heirloom Iraqi Durum used by Community Grains to make its fettuccine—is excited about the wheat renaissance.

“I’ve grown up around wheat all my life,” Muller says, “and until recently no one has really talked about flavor. But now food writers and chefs are saying, ‘Hey, we love this wheat.’ People are finally paying attention to it. We as wheat farmers are now growing a food, not a commodity.”

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Klein is convinced that the flavors of these heirloom and landrace wheat varieties are only as good as the soil in which they’re sown. “Wheat like ours from small farms tastes superior because it’s grown in very good nutrient-rich soil,” he says. “Most generic wheat, conversely, comes from nutrient-depleted soil, because in the United States we usually grow wheat where the land is cheap, which is not great nutrient-wise. The better farmland is normally reserved for more profitable crops. But wheat from good soil gives a more ‘animated’ flavor, especially in fresh-baked bread.”

WSU’s Jones agrees that wheat grown in more desirable areas produces a vastly superior grain: “With grapes, the big flavors come from intentionally stressing the vines, but with wheat we have discovered it’s the opposite—the big flavors do not come from stress but from cool and moist conditions.”

Tom Hunton of Camas Country Mill in central Oregon is spearheading the wheat terroir movement in the Pacific Northwest, not only growing specialty wheats such as Edison Hard White (described as “buttery” and “golden”) but also inviting a growing community of local grain farmers to share his new state-of-the-art stone grist mill; without this access, they’d have to sell their high-end wheat at much lower prices on the commodity market, where its terroir would be lost.

From this small cooperative beginning, Hunton has big dreams: “We desire to bring taste and flavor to as large a population as possible, at an affordable price point,” he says.“We want to move beyond food for the elite and share these phenomenal flavorful varietals with a broader audience.”

The Eastern Palouse Uplands

"Morning Mist" curtesy of John Clement (photo taken at the eastern Palouse uplands)

"Morning Mist" curtesy of John Clement (photo taken at the eastern Palouse uplands)

The Palouse River headwaters are born in the clear stony brooks of Idaho's Hoodoo and Clearwater mountains and fed by tributaries emerging from the Thatuna Range located between the river's north and south forks. These eastern uplands are composed of the western buttes' parent belt quartzites and argillites that rose with the Rocky Mountains when the Cascade Range had not yet emerged above the Pacific waters. In the formative processes of this early Mesozoic Age of explosive Rocky Mountain strato-volcanoes, hot magmatic fluids under great pressure penetrated this younger earth's crust and brought certain metals in gaseous state nearer the surface to form soluble compounds like gold chloride and aluminum-iron silicate. In places where water penetrated to great depth these compounds dissolved, mixed with the magma, and were forced through fissures with other solubles like silicon dioxide, or quartz, to create veins containing precious metals and alamandine garnet crystals.

Where this petrographic drama transpired under ancient weathered surfaces as in the Hoodoos, these deposits were worn by water until soft yellow flakes, larger nuggets, and violet-red gemstones fell out into streams which usually held these heavy particles near their sources. As in other high places along the Pacific Slope, indications of this placer gold in North Idaho resulted in nineteenth century regional rushes as prospectors flocked to the rumored El Dorados. Dodecahedron-faced garnets and rainbow-colored "harlequin" opals have also been sought in the eastern Palouse as the region's only semi-precious stones. 

Palouse Regional Studies Celebration at WSU

On 4 November 2016, Palouse Heritage had the privilege to participate in an event at Washington State University (WSU) celebrating Palouse regional studies. Specifically, the occasion commemorated Gary Schneimiller's generous gift to WSU Libraries in honor of research related to the Palouse region. Gary is a friend of Palouse Heritage and it was truly a privilege for our co-founder, Richard Scheuerman, to give the keynote speech. We commend Gary for his generosity and shared passion for celebrating the rich history of the Inland Pacific Northwest.

You can view the video of Richard's talk below.

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Land and First Peoples

Looming above the panoramic Palouse near the heart of the region stands a promontory revered by the native peoples known today as Steptoe Butte. To the Palouse Indians it was Yamustas (“Elk’s Abode”), a sacred high place of spirit quests and the abode of mythical Bull Elk. An honored figure in tribal folklore, this creature was said to have found sanctuary during the time of the Animal People in the cleft of the butte's eastern face. Its majestic antlers stretched toward the summit and remain visible today. To the area's first European-American explorers, who dubbed it "Pyramid Peak" for resembling Egypt's great monument to Cheops, the butte served like a mariner's landmark, a strange island in an oceanic maelstrom of earthen waves cresting with wind-pulsed native wheatgrasses and fescues.

Before the sextant and plow demarcated and denuded these fertile swells, they were seasonally transformed from soft springtime viridian hues with wildflowered splashes of bluebells, flaming Indian paintbrush, and bright yellow arrowleaf balsamroot into summer and fall's muted green-brown pastels mixed in the bunchgrass billows. The butte continues to serve as a landmark Palouse portal to Native Americans today. On several occasions while in the company of Nez Perces returning to Lapwai from the Colville Reservation or with Coeur d' Alenes headed east from Warm Springs, I have heard elders say, "When I see Steptoe Butte, I know that I am home."

Elk's Abode - Steptoe Butte (John Clement)

Elk's Abode - Steptoe Butte (John Clement)

The Palouse region covers that part of Eastern Washington and Northern Idaho in the Palouse River basin as well as adjacent lands characterized by a rolling terrain of fertile loess soils. This area covers approximately 4,000 square miles and lies largely in Washington's Whitman and Spokane counties, the eastern third of Adams County, and in Idaho's Latah County. Nearly seventy percent of the land is arable, composed of deep deposits of rich but fragile topsoil which cover immense layers of brown-black basalt. This bedrock shield is up to 10,000 feet thick resulting from successive lava flows through fissures across the Columbia Plateau during the late Miocene Epoch between six and seventeen million years ago when the area of today's Palouse Country, before the Cascade uplift, received as much as fifty inches of annual rainfall to host a mixed forest of conifers, maples, water tupelo, and oak similar to America's southeastern bald cypress swamps of today.

The Palouse is bounded by the Snake and Clearwater rivers on the south and Idaho's imposing Bitterroot and Clearwater Mountains to the east. The evergreen forests of these eastern uplands extend across the northern half of Spokane County along a line roughly corresponding to the deepest penetration of the great Pleistocene glaciers to form the region's northern limit. The Cheney-Palouse lobe of the Channeled Scablands comprises the region's western boundary which extends from the timber line near Tyler, Washington south to the mouth of the Palouse River. Annual rainfall increases from an average of fourteen inches in the western Palouse prairies to eighteen inches in the central Palouse Hills and up to twenty-two inches in the foothills of the eastern mountains.

This pattern corresponds to a rise in elevation from 1,200 feet in the southwest corner of the Palouse prairie to the fringe of the Clearwater Palouse Range at 2,800 feet, almost exactly one inch of precipitation for every hundred feet of elevation. Variations in soil fertility developed over ages due to increasing rainfall eastward led to climax vegetation associated with the Palouse's three climatic life zones: Upper Sonoran in the western Palouse, Arid Transition across the central Palouse Hills, and Canadian in the eastern mountain uplands.