University of Nebraska - Lincoln DigitalCommons@University of Nebraska - Lincoln U.S. Department of Agriculture: Forest Service -- USDA Forest Service / UNL Faculty Publications National Agroforestry Center September 2004 Historical evidence of riparian forests in the Great Plains and how that knowledge can aid with restoration and management. Elliot West University of Arkansas in Fayetteville, Arkansas Greg Ruark U.S. Department of Agriculture’s National Agroforestry Center in Lincoln, Nebraska Follow this and additional works at: https://digitalcommons.unl.edu/usdafsfacpub Part of the Forest Sciences Commons West, Elliot and Ruark, Greg, "Historical evidence of riparian forests in the Great Plains and how that knowledge can aid with restoration and management." (2004). USDA Forest Service / UNL Faculty Publications. 7. https://digitalcommons.unl.edu/usdafsfacpub/7 This Article is brought to you for free and open access by the U.S. Department of Agriculture: Forest Service -- National Agroforestry Center at DigitalCommons@University of Nebraska - Lincoln. It has been accepted for inclusion in USDA Forest Service / UNL Faculty Publications by an authorized administrator of DigitalCommons@University of Nebraska - Lincoln. a long, long time ago... Elliott West is a professor of history at the University of Arkansas in Fayetteville, Arkansas. Greg Ruark is the director of the U.S. Department of Agriculture’s National Agroforestry Center in Lincoln, Nebraska. Historical evidence of riparian forests in the Great Plains and how that knowledge can aid with restoration and management. Riparian areas—land adja- transcontinental railroad spur lines in the 1860’s; before the 1859 Denver gold cent to a streambank or rush; and before the Great Westward other water body—filtering Movement of the 1840’s along the nonpoint source pollution. Oregon Trail (Ambrose, 2000; West, Unfortunately the riparian 1998). These defining events drew many people into and through the Great Plains areas of today, include only on their way to seek their fortunes and narrow bands of forests, or build their futures. no woody vegetation. This This, then, is a story of the Great Plains greatly minimizes their eco- and how riparian areas along major rivers and their tributaries were once signifi- logical function. In deciding cantly forested. They came under great how to manage these areas, pressure beginning in the mid 1800’s knowing the natural ripari- from the simultaneous and cumulative an makeup before humans impact of Indians, gold seekers, soldiers, railroad crews, and settlers who all played settled in the area is vital. important roles in determining the way Management essentially is riparian areas look today. then restoration. The Story… The Great Plains as a whole hosted far hile some argue that the Great fewer trees than the Missouri valley to Plains were dominated by the east and the Rocky Mountains to the W grasslands and that riparian west. The Arkansas River provides an woodlands were rare, others contend that illustration. Records from the early 19th trees would logically have occurred in century indicate that for 150 miles east of riparian areas due to favorable microen- the current Kansas-Colorado border only vironment conditions. Historically, what an occasional cottonwood would have native plant communities were found in been seen. Three conditions occurred riparian zones of the Great Plains? The that did not favor the persistence of trees: answers to this question depend to a large sandy soil, heavy springtime flooding, and extent on what time period is used as a the low banks that allowed prairie fires to reference of pre-settlement conditions. burn down to the water’s edge (Wells, The U.S. Fish and Wildlife Service 1965). But at the eastern end of this por- (1981) drew upon conditions in 1905 for tion of the river, around present day insight and concluded that trees were Great Bend, Kansas, trees lined the aptly “wholly absent” or consisted of scattered named Walnut and Ash Creeks that emp- cottonwood and willow. However, such tied into the Arkansas. a view rests on a flawed and incomplete Field notes from a 1825 surveying reading of the record. Indeed, by 1900 expedition, describe those streams as well most riparian zones in the Great Plains shaded by stands of hardwoods and report had long since been depleted of their other wooded tributaries downstream natural woody vegetation component. from there (Brown, 1913). At the other However, abundant historical evidence end of that poorly wooded stretch to the from the 1800’s supports a very different west—about where the river today crosses picture, with different ecological implica- from Colorado to Kansas—began one of tions. In fact, to tell the story of this land the best-known woodlands of the Plains, we need to begin a long, long, time the “big timbers” of the Arkansas (See ago. .prior to the construction of the sidebar for additional historical evidence). Reprinted from the Journal of Soil and Water Conservation Volume 59, Number 5 S|O 2004 VOLUME 59 NUMBER 5 105A Copyright © 2004 Soil and Water Conservation Society 1. Platte River 2. Arkansasa River 3. Republican River 4. Smoky Hill River 5. Kansas River 6. Lodgepole Creek 7. North Platte River 8. South Platte River 9. Purgatory River 10. Walnut Creek 11. Pawnee Creek 12. Big Timber of Arkansas 13. Big Timbers of Smoky 14. Big Timbers of Republic OPPOSITE The locations for the specifc rivers discussed are indicated on the map. SELECTED HISTORICAL EVIDENCE FOR WOODED RIPARIAN ZONES So while the soil and lay of the land 1806 – When Lt. Zebulon Montgomery Pike ascended the Arkansas River, he gave trees little or no chance to take hold reported that “the river banks began to be entirely covered with woods on both along some streams, conditions on many sides” just west of the present Colorado border (Jackson, 1966, vol. 2, Pp. 344- others encouraged healthy stands of 345). For about sixty miles upstream cottonwoods abounded. trees—mostly cottonwoods, willows, and hackberries on the western Plains and to 1821 – Jacob Fowler wrote of thickly wooded islands and “Points of [timber] in the east, a mixture of deciduous species. the bends more plenty” (Coues, 1970, pp. 44). During the next forty years many These woodlands could be a striking sources remarked on the considerable (although, dwindling) cottonwood groves along the Arkansas, especially below the mouth of Sand (or Big Sandy) Creek. sight after a long crossing of the treeless highlands between watersheds. An Irish This large stand, was one of three “big timbers” of the Central Plains. The sec- private in 1849, after four days of crossing ond was on the Smoky Hill River in present Wallace County in far western Kansas. The third was on the Republican River not far south of present McCook, the sea of shortgrass in eastern Colorado, Nebraska. All are well documented. greeted the treetops of the Republican’s wooded bottoms with a joyful cry: “Be 1835 – Henry Dodge wrote in 1835 that the Platte River above the heavily timbered Jesus we’re in sight of land again” Grand Island had abundant trees on the south bank while feeder ravines were “cov- (Mattes, 1953). ered with timber of small growth.” From a hill at the confluence of the North and The analogy was insightful, for these South Platte, he could see the hills above the river downstream “covered with scat- riparian groves were safe harbors for tered groves” while at “an immense distance” were “the feathery outline of some tall trees...above the horizon.” (Report of the Secretary of War, 1835) some Plains inhabitants during winter, when sudden blizzards and bitterly cold 1857 – Two Buttes Creek, which enters the Arkansas near present Holly, temperatures threatened any warm- Colorado, was named Piles of Driftwood by Southern Cheyennes for the great blooded creature caught in the open. For tangle of dead trees at its mouth. Lt. Francis Bryan reported that a similar sight at the mouth of a tributary of the Republican suggested flourishing timber Plains grazers—bison, deer, pronghorns, along this creek: “indeed, a quantity [of trees] could be seen from the point and elk—the even slightly lower eleva- where we crossed it” (Report of the Secretary of War, 1857, pp. 472). tion of a stream bottom provided some shelter from the wintery blasts. More 1860 – Like Walnut and Ash Creeks, many tributaries of larger watercourses protective were the stands of timber, which were well wooded. J.E.B. Stuart wrote of the Purgatory River that flowed into broke the force of the wind and conserved the Arkansas from the south that “timber [is] heavy and abundant near the some heat. river.” (Hafen, 1959, pp. 235) From the Quaking Asp River on the northern Plains comes a vivid account of the value of these natural shelters. When a storm caught Alexander Toppance’s freighting outfit in January, 1866, they took shelter in groves along the river and soon were joined by hundreds of bison. So crowded were men and beasts that many bison remained exposed. They 106A JOURNAL OF SOIL AND WATER CONSERVATION S|O 2004 froze where they stood, and the next developments help us understand what spring Toppance found that their bones happened. First, the spread of horses out formed a bleached border to the stand of of the Southwest and the rise of the timber. (Toppance, 1923) Plains horse culture led to an increase in The dependence of people and animals Native American population, which in on shelters like these, once understood, is turn wore away at the resources of the further evidence for timber along Plains river valleys. In 1821, Jacob Fowler esti- watercourses.The year-round presence of mated that a winter camp in the big tim- people, horses and bison on the high bers of the Arkansas hosted twenty thou- Plains supports the existence of riparian sand horses; twenty-seven years later an woodlands simply because the one could Indian agent reported Cheyenne and not have survived without the other.