The Fifteenmile Creek watershed in western Maryland and south-central Pennsylvania is approximately 64 square miles in area and is located in a rural part of the Ridge and Valley physiographic province. Fifteenmile Creek originates as a small stream on the flank of Ragged Mountain several miles north of the village of Artemas in Bedford County, Pennsylvania. The creek flows in a southerly direction, crossing into Maryland at the Mason-Dixon Line, and flowing under Scenic Route 144 and Interstate 68. Turning to the east and then to the southeast, the creek continues its 19.3 mile long journey through the Maryland countryside. Near the town of Little Orleans, Maryland—at which point it is a major 4th-order tributary—the creek flows under the Chesapeake and Ohio Canal aqueduct just before reaching its confluence with the Potomac River.
The Fifteenmile Creek watershed contains numerous major tributaries, including: Bear Camp Branch, Pine Lick, Little Pine Lick, Big Divide Run, Piclic Run, White Sulfur Run, Deep Run, Terrapin Run, Mud Lick, Spring Lick, and Flat Run. Fifteenmile Creek is one of the Potomac River’s most pristine tributaries, owing in part to the fact that 92% of its watershed is forested land, of which nearly two-thirds is protected state land: Buchanan State Forest in Pennsylvania, Green Ridge State Forest in Maryland, and Billmeyer Wildlife Management Area in Maryland.
The mainstem of Fifteenmile Creek is presently ungaged, but two major tributaries (Deep Run and Terrapin Run) have been gaged since 2005. Flow records reveal that streamflow in the basin is highly variable in nature. The watershed is capable of producing flash floods in response to intense rainfall and long periods of low (or zero) flow during persistent droughts. Prolonged periods of extremely low flow are relatively common in the hydrologic record, reflecting the combined influences of a rain shadow effect and the underlying bedrock lithology that is unable to sustain baseflow for long periods without rainfall. Under these conditions, much of the creek and its tributaries actually resemble dry cobblestone roads with the only surface water found in a few stagnant pools.
When the early settlers reached the Appalachian Mountains in the 18th century, they were clearly in awe of the size and vastness of the native virgin forest and the potential that it offered. In the middle of the 19th century, John Upton of London, England, described the forest within William Carroll’s huge Town Hill Estate in Allegany County, Maryland (most of its 12,000 acres were located within the Fifteenmile Creek watershed)
The residue of the estate is entirely woodland, containing an immense quantity of oak, and other timber as valuable as any in this part of America. There is the hickory, the white, black, and rock oaks, many of them near one hundred feet high, and fifty to seventy feet from the lower limbs to the ground, with trunks of corresponding magnitude, well adapted for Naval purposes; also the sugar and curly maple, gum, and flowering locust trees, white, yellow, and red pines, one hundred and twenty feet high, exceedingly tough and clean, that will square two feet six inches at the butts when slabbed, and some larger, fit for masts, yards, and spars; also an abundance of sassafras, sumac, and other valuable dyeing and medicinal plants, and thousands of tons of oak and quercitron bark.
The dense and diverse forest at that time provided extensive habitat for a variety of animals, including black bears, woodland bison, mountain lions, timber wolves, elk, white-tailed deer, beaver, foxes, skunks, and wildland birds. Many of the populations of these species were grossly depleted or eliminated as a result of lost habitat as the forest was cut during the 19th century; other species were considered varmints and were hunted to extinction or near extinction. Effective game management and return of the land to forest has allowed many of these populations—such as the white-tailed deer and turkey—to be successfully restored in the watershed.
Humans have played an important role in Fifteenmile Creek for many millennia; the native Americans who arrived in Maryland after the end of the last Ice Age surely found a forest that looked very different from the present one. Some of the earliest European settlers who explored the Potomac River and its tributaries included a surveyor by the name of Peter Jefferson (Thomas Jefferson’s father) who in 1751 was one of the first persons to put Fifteenmile Creek on a map. George Washington was even more familiar with Fifteenmile Creek through his many journeys through the region as a surveyor, military officer, landowner, and later as President of the United States. Historically, Fifteenmile Creek owes its name to the fact that its confluence with the Potomac River is located 15 miles east of Oldtown, Maryland—the site of Colonel Thomas Cresap’s early settlement and trading post.
The first true wagon road into western Maryland—Oldtown Road, constructed in 1758 from Fort Frederick to Fort Cumberland—closely followed the watershed’s southeastern divide. Along this road is famous Point Lookout, used by Union troops during the Civil War to observe Confederate troops intent on destroying the bridges, aqueducts, and railroad tracks along the Potomac River. Visitors to Point Lookout today can enjoy the same view that the Union troops had 150 years ago. From the overlook, one can still see the 243 acres of land across the river in West Virginia that were once owned by George Washington. In the early 1800’s, the “Bank Road” connecting Hancock and Cumberland, Maryland was built as a turnpike to greatly speed east-west travel; today, that road is Route 144 (or Scenic Route 144).
In the late 19th and early 20th centuries, the Fifteenmile Creek watershed was valued primarily for its timber resources and for unknown mineral resources (e.g., coal, iron ore) that the land might hold. William Carroll, grandson of Daniel Carroll—one of America’s Founding Fathers—was an early investor in western Maryland who sought to take advantage of opportunities provided by construction of a canal (the “C&O”) connecting Georgetown and Cumberland, Maryland or possibly by one of the nation’s first railroad lines (the “B&O”) that would eventually connect Baltimore and Cumberland.
William Carroll’s ventures in the watershed ended in personal failure and he was forced to leave his Town Hill Estate in 1843—60 years old and bankrupt. Eventually, the same land that Carroll had invested in provided enough sawtimber to sustain several generations of “Timber Barons” operating in the watershed. In the late 1800’s, Frederick Mertens—a Cumberland businessman—was involved in house and canal boat construction that required large quantities of lumber. Mertens’ demand for sawtimber was so great that he constructed a narrow gauge railroad from one of his sawmills at Darkey’s Lock into the Big Run and Deep Run watersheds. Mertens used two locomotives purchased from the Mount Savage Locomotive Works in Frostburg, Maryland to move his freight. By 1896, the Green Ridge Railroad was 26 miles in length and had a passenger car for its owners and for paying customers. The rail bed of much of the former Green Ridge Railroad is now occupied by the Green Ridge Hiking Trail.
By the end of the 19th century, the devastation inflicted by the “Timber Barons” on the watershed was nearly complete. Depleted of its valuable sawtimber, the land was virtually worthless—considered wasteland and simply left to the ravages of water and fire. Yet the Fifteenmile Creek watershed would sustain yet another grandiose venture at the hands of Fred Mertens’ sons: creation of the “largest apple orchard in the universe”. Before going bankrupt in 1918, the Mertens brothers and their Green Ridge Valley Orchard Company would subdivide their massive landholdings in the watershed and amass a proverbial fortune—nearly $3 million—by selling 10-acre parcels in their cooperative orchard venture for $150 to $250 an acre. Planting, growing, and maintaining a productive apple orchard in this harsh dry climate turned out to be far less profitable than the Mertenses had ever imagined.
The most recent chapter in the human history of the watershed began with establishment of Green Ridge State Forest under the direction of Maryland’s first state forester, Fred W. Besley, in 1931. Some of the earliest work performed in the new state forest by the Civilian Conservation Corps (CCC) not only helped to establish new forests, perpetuate existing forests, prevent soil erosion, and fight forest fires, but the experience instilled confidence in a group of young men shaken by unemployment and other hardships of the Great Depression.
The Fifteenmile Creek watershed is truly a place of national significance; it includes many landmarks of cultural significance such as: the Mason Dixon Line (the most famous boundary line in the nation); the Chesapeake and Ohio Canal National Historical Park; the Potomac Heritage National Scenic Trail.
While the presence of Green Ridge State Forest in Maryland and Buchanan State Forest in Pennsylvania afford significant protection of a large portion of the Fifteenmile Creek basin, the watershed is still threatened by problems associated with commercial and residential development. The urbanization pressure is largely attributable to the fact that the watershed is bisected by Interstate 68 that provides a major transportation corridor to the urban and suburban growth centers in eastern Maryland. Presently, a proposed 4,300 home development on a 935 acre subdivision in the Terrapin Run subwatershed of Fifteenmile Creek is being held up by a civil court case involving the developer, Allegany County, and two state of Maryland departments.
The impacts of the proposed development on surface and groundwater resources are major issues that have yet to be resolved. This issue is further complicated by two other facts: (1) several reaches of Fifteenmile Creek and its tributaries are considered Tier II (i.e., high quality) waters—ostensibly providing them with additional protection under the anti-degradation rules of the Clean Water Act; and (2) the presence of the federally-endangered Harperella plant along reaches of the mainstem of Fifteenmile Creek.
Erosion and sedimentation from a variety of sources, including timber harvesting, a relatively extensive network of maintained gravel roads, and an ATV trail, are perceived as major threats to water quality. Future development of natural gas resources within the Marcellus shale also represent a significant threat to water quality.
Finally, invasive species and pests—such as the gypsy moth caterpillar, can have severe consequences for the productivity and composition of the second-growth forest itself.