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Through the Looking Glass

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Through the Looking Glass Through the Lookingone Glass The Environment of the Ancient Mesa Verdeans Karen R. Adams For Alice in Wonderland, the task was easy. All she Despite the region’s suitability for farming, we had to do was step through a magic looking glass know that ancestral Pueblo people also experienced into a wonderful new world that was not only clear times of hardship caused by agricultural failures. but also in full color. Our archaeological looking More than once they watched their crops wither glass, on the other hand, is fogged, and the images from lack of rain or succumb to killing frosts. we peer at seem blurry at first. Plant remains and Sometimes hunger and malnutrition pitted groups animal bones in archaeological sites usually are bro- against each other, resulting in warfare and emigra- ken up, and plant fragments are often black from tion. The more we know about the environment of charring. Yet as we archaeologists continue to the past, the better we can understand population assemble evidence from many sources, the haze in spikes and declines, the movements of people, and our looking glass clears, and we see in increasing the ways they coped with food shortages. detail the environment of the ancient Puebloans of The diverse biotic communities of the Mesa the Mesa Verde region. Little by little, we under- Verde region have long included many plants and stand better how they went about growing crops, animals that humans have found useful. Studies of foraging for wild plants, and hunting animals. preserved pack rat middens (nests) tell us that the We now know that for centuries farmers have present plant and animal communities of the considered the Mesa Verde country of southwestern American Southwest have been in place for the past Colorado and southeastern Utah to be a great place 4,000 years. The archaeological record verifies that to settle down and raise a family. Well suited to ancestral Pueblo landscapes hosted many of the agriculture, the region receives sediment carried by same wild plants and animals we see today. winds blowing regularly from the southwest, sedi- Still, our ability to envision earlier landscapes ment that has formed thick layers of loose, nutrient- has been inhibited by the appearance over the last rich farmland. In addition, nature has obliged many century of invasive species originating on other a Mesa Verdean farmer’s need for enough moisture continents. Tumbleweeds, summer cypress, and and frost-free days to enable crops to mature. For clovers, for example, now crowd out native plants. much of the time between 500 and 1300 CE (the In addition, commercial farming, logging, and live- Basketmaker III through Pueblo III periods), farm- stock grazing have cleared vast areas that once sup- ers raised corn (maize), beans, and squash, and they ported piñon and juniper woodlands and parklands grew or traded for gourds. More recently, farmers in of sagebrush and native grasses. Along with deep southwestern Colorado have experienced a century plowing and fire suppression, these historic activi- of successful dryland farming (farming by natural ties have altered the proportions and, in some precipitation alone), particularly of splotchy red- instances, the natural groupings of plants and ani- and-white common beans similar to those grown by mals. The role that ancient people played in altering ancient farmers. their environment must also be acknowledged. Copyrighted Material Figure 1.2. Ancestral Pueblo farmers built agricultural terraces such as these in Mesa Verde National Park to contain runoff and stabilize soil. The Modern Environment have long been critical water sources for both Seven major biotic communities grace the Mesa animals and people. Over the centuries, Puebloans Verde regional landscape. Each consists of a certain also constructed check dams, water diversion sys- group of plants and animals that is affected by and tems, and reservoirs to make water more accessible adapted to local temperature, precipitation, and soil. (fig 1.2). From the valleys, at some 4,000 feet in elevation, to All farmers know how critical moisture is to mountain peaks above 12,000 feet, these plant com- their crops. In the Mesa Verde region, mean annual munities are characterized by, respectively, sage- precipitation ranges from 7.8 inches near Kayenta, brush and saltbush shrubs; grasses; piñon and Arizona, to more than 18.3 inches in and around juniper woodlands; Gamble oak scrubland; pon- Durango, Colorado. Moisture from snowmelt allows derosa pine and Douglas fir woodlands; spruce and corn kernels to germinate and sustains tiny true fir woodlands; and low-growing alpine tundra. seedlings through the normally dry weeks of late Piñon-juniper woodlands, expanses of sage- spring and early summer. Later, sporadic summer brush and saltbush, and grasslands abound in the rains spur rapid plant growth and ear development. southwestern corner of Colorado, where ancient On the Colorado Plateau, corn agriculture requires human populations were once large. Although the at least 12 to 14 inches of annual precipitation to be region includes both major rivers (the San Juan, successful, and some developmental stages of corn Animas, La Plata, and Dolores) and smaller rivers growth, such as pollination and grain development, and creeks (the Mancos, McElmo, Piedra, and especially need water. Yellow Jacket), the springs and ephemeral drainages Pueblo farmers learned long ago that they could 2 Karen R. Adams / Copyrighted Material direct runoff from intense summer showers to their centuries. He then combined the annual tempera- fields by aligning stones, dirt, and brush debris. ture and precipitation data to construct a 2,000- They also placed their fields in locations best suited year time line of conditions critical to agriculture. to receiving storm runoff, such as at the bases of To add to this, Timothy A. Kohler (see chapter 8) gentle slopes. Sometimes they also hand-carried and his associates from Washington State University water from reservoirs (“pot irrigation”), especially recently assembled a broad range of environmental to drought-intolerant crops such as squash. data, information about corn yields, and estimates Temperatures, too, play an important role in of human population to form the basis of a sophisti- growing crops successfully. Most varieties of corn cated, multicentury model of periods of farming need at least 120 frost-free days and a minimum success and failure for the Mesa Verde region. amount of summertime heat in order to mature. The latter is measured in “corn-growing degree day” Agricultural Success and Failure, Population (CGDD) units; at least 2,500 units are required dur- Spikes and Declines ing a growing season. Farmers in the Mesa Verde region began growing corn, a Mexican import, sometime in the first few CGDD units are calculated by summing the centuries of the first millennium CE. Before long it difference between each day’s average tempera- became both a dietary staple and an integral compo- nent in ceremonies. Why did this happen? Corn is ture and a set base temperature (50 degrees unique among grain crops in having both large ker- Fahrenheit). One CGDD unit is accumulated for nels and high yields. By planting a single kernel, a each degree by which the average exceeds the farmer could grow a plant that produced 300 to 600 base temperature. A minimum of 50 degrees and kernels. Studies have shown that Puebloans in the a maximum of 86 degrees have been set as last century routinely set aside approximately 350 thresholds below and above which corn crops pounds of corn kernels for one person’s annual con- will not thrive. sumption (fig. 1.3). Under favorable circumstances, three to four acres of land could yield enough corn My colleagues and I have examined modern to feed a family of three to four people for a year, temperature and precipitation records for the Mesa assuming that wild plants and animals provided Verde region to assess the locations best (and worst) additional calories, critical vitamins and minerals, suited for farming. Our research shows that despite and protein missing from corn. Also, around 600 being above 7,000 feet in elevation, Mesa Verde CE, Pueblo people began growing common beans. proper currently has enough CGDD units, frost- When added to corn in their diet, beans gave them free days, and precipitation to farm successfully in all the amino acids of a complete protein. most years, enhanced by the fact that the broad, After corn became a staple, the successes and sediment-covered mesas tilt gently south, toward failures of corn harvests paralleled the rises and the warming sun. The Yellow Jacket, Cortez, and declines of the native population. By the 600s, pop- Blanding areas, too, receive enough moisture and ulation was on the increase, but a drought in the summer heat to grow corn, so it is no surprise that late 800s made dryland farming too risky. they were all densely populated in prehistoric times. Throughout the 900s, Pueblo farmers seem to have Tree-ring samples obtained from ancient roof hung on by tending small fields along drainages or beams, stands of very old living trees, and even by clearing fields at the bases of slopes to benefit older wood lying on rocky landscapes provide data from storm runoff. By the middle and late 1000s, on precipitation in the past. Dendrochronologist while living in dispersed farmsteads and walking Matthew Salzer, working in the San Francisco Peaks daily to their nearby cornfields, they were again area, near Flagstaff, Arizona, used bristlecone pine reaping successful harvests. Between 1130 and records to reconstruct periods of relatively higher 1180, however, drought again placed its curse on and lower temperatures for the ancestral Pueblo agriculture. We see its reflection in tree rings, in a Copyrighted Material / The Ancient Environment 3 Figure 1.3.
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