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The Not-So-New River and Its Past
Stand at the overlook at Canyon Rim Visitor Center and look southeastward. Here the panorama of the gorge best presents itself, revealing the character of its natural sculpture and landscaping. From this point the valley sides fall away steeply, almost 900 vertical feet, prescribing the river's course through a V-shaped gorge whose sides are softened by luxuriant Appalachian vegetation. I stood here in the fading light of a summer evening reflecting on the river, its roar diminished by distance, and on the gorge, its walls darkening in the twilight, and I wondered about the scene before me and how it came about.
The answer to my questions come from the geologists, whose science is not as simple or precise as we might wish. But we will get past these difficulties and focus on some easy-to-understand and intriguing parts of New River's geologic history.
The River Today
Let's start with the scene today. If you stand on the river bank, you see and hear a river in motion whose headsprings are in the Blue Ridge Mountains near Boone, North Carolina, sometimes called the 'Roof of Eastern America' because four great river systems start close by.
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Here the headwaters of the New River start on their more than 2,000 mile journey that takes them north into Virginia, there to be joined by the Little River, north further into West Virginia to be joined by the Greenbrier, through the New River Gorge, then losing identity as the New River at the confluence of the Gauley to become the Kanawha, westward to the Ohio River near Point Pleasant, continuing as part of the Ohio to join with the Mississippi at Cairo, Illinois, then moving sharply to the south cutting through the nation's mid-section and finally emptying into the Gulf of Mexico near New Orleans.
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The entire journey take about 110 days, sometimes more, sometimes less, based on the fluctuating speed of river flow. Some of this water may repeat the same trip or part of it sometime in the future, as it has in the past through the age-old cycle of evaporation, transportation, precipitation, and run-off.
Water Resources
The primary thrust of the natural resource management activities at New River Gorge National River is the protection of the water resources. The quality of the surface water resources of the New River has been studied in recent years by both the State of West Virginia and park Resource Management staff. Data from these studies suggest the presence of metals, organic contaminants and influx of raw sewage are common in many tributaries of the New River. Metals contamination, resulting from mining activities and or urban surface flows, are present in most tributaries, with four streams, Wolf Creek, Arbuckle Creek, Dunloup Creek and Piney Creek, showing pronounced values. Other sources of pollutants within park boundaries include unlined landfills, illegal dumps, pesticide sprayed directly into the New River, agricultural runoff, road salt runoff, direct discharge of residential sewage, inadequate municipal sewage treatment facilities, recreation waste streams, and industrial discharges.
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Pollution of rural streams by fecal coliform bacteria is a widespread issue. Since fecal coliform bacteria live in the gut of warm-blooded animals, fecal contamination of rural streams can come not only from humans, but also from livestock, pets, and wildlife (including birds). Several research efforts have been made to understand the role of these various potential sources of bacteria. One of these studies was conducted in New River Gorge by the U.S. Geological Survey, in cooperation with the National Park Service. The results indicate that human caused wastewater pollution is present in each of the four New River Gorge tributaries sampled. The report also found other sources of contamination in some streams, and noted the need for additional research to bolster the findings and refine the methods.