The Trail network provides access to many unique ecosystems within five distinct geographic regions. Below are links to some documents to help you explore these special places. To recommend additions, please contact us.
Ecology, Economy and Change
The Potomac Basin has been shaped and reshaped greatly through time as ecosystems have been changed gradually by each resident human society over the last 14,000 years. A slow deterioration, due primarily to the activities of man, has more recently turned into a rapid destruction of habitat coupled with industrialization and over-population. The tides are slowing turning in the other direction, however; for the past 50 years there has been a steady, but slow, repair of natural ecosystems. Today we live in an ever-threatened, fragile and still-recovering structure.
For example, the recent efforts to bring back American shad, a species once economically important, have been successful, but only to a point. The numbers of shad are growing but it is still unlawful to catch and keep shad.
Today there is greater interest in ecology than ever before, but the idea lingers that ecology is a subject important only in the biological sciences. Other groups do include the effects of humans as an innate part of ecology; in the social sciences, however, ecology is viewed as if humanity were the only agent responsible for change.
The effects of time, as another major factor in ecological change, is consistently minimized or ignored by many. In 1886, William Morris Davis of the Pennsylvania Geological Survey published a paper called "Rivers and Valleys of Pennsylvania"; with a few corrections, this paper is still applicable today and describes four major physical factors that shape rivers: 1) the formation of wind and water gaps by erosion; 2) headwater migration of divides; 3) stream piracy; and 4) adjustments to stream structure.
Scientists think that many millions of years ago a super continent, called Pangea, began to break apart to form the modern continents. The topographic changes occurring after the continental split have resulted in the present Chesapeake Bay and Potomac River basin:
• A huge meteorite impacted the earth at what is today the mouth of the Chesapeake Bay, creating a giant crater and further affecting the direction of flow of the proto-rivers (rivers before the Potomac's existence).
• The westward erosion of the headwaters of the ancient Potomac captured other drainage systems, such as the Shenandoah, and thus increased the size of the basin.
• The Potomac River's flow and flooding wore down the heights of the uplifting plateau, resulting in sedimentation and water and wind gaps--spaces eroded from mountains; examples include the Gap in the Blue Ridge where the Potomac and the Shenandoah rivers converge.
Everyday Ecology in the Potomac Basin
The Potomac River corridor can be divided into six physiographic sections: the sediment-covered Coastal Plain, divided from the Piedmont by the fall line; the ancient crystalline rock of the Blue Ridge; the Great Valley, from the Shenandoah Valley south of the River to the Cumberland Valley north of the River; the rippled Ridge and Valley portion of the Appalachian Highlands; and the eastern front of the Allegheny Plateau.
Traveling through these regions is a vast window into geology and geomorphology--the study of the earth's physical makeup and the earth's physical changes, respectively. And this opportunity is a primary reason that Congress authorized the Potomac Heritage National Scenic Trail.
The rock cycle is demonstrated in many places, but nowhere as graphically as Sideling Hill along Interstate 68 in Washington County, Maryland. From the side of the mountain one sees the different levels of rock and deposits and the curvature that sugggests the movement of the earth's plates. We go back in time when studying the rocks of the basin and, fortunately, can also retreat in time by visiting some very special ecosystems. Fossils and pollen allow us to reconstruct the changes in environment over time until the archaeological record begins in the late Pleistocene era.
We still have remnants of ice age ecosystems in the basin today. These are probably best described as "muskegs," an Algonquian word meaning "trembling earth." Locally they are called quaking bogs, glades, swamps, marshes and bogs. Muskegs are at high enough altitudes (ca. 1,000 meters) for frosts to occur in summer, acting as a natural "refrigerator." Cranesville Swamp in Garrett County, Maryland, is a good example. Many arctic plants and animals have their southern-most distribution in these muskegs.
As the continental ice sheet withdrew, a new ecosystem of plants and animals came into play. This complex included caribou and muskoxen as well as several now extinct large ice age mammals. There were few populations of humans at that time in the area, and except for hunting larger mammals, humans probably had little effect on the ecosystem at that time. Over time the area grew into a deciduous forest similar to what we see today, but the trees grew in greatly different proportions to each other.
Many plants have become less prominent since the Pleistocene era. For example, the chestnut and the American elm were two primary tree species hat have been all but wiped out. Some birds have been eliminated including, the passenger pigeon, the Carolina parakeet and the ivory-billed woodpecker. Bison, elk, wolves and mountain lions all used to roam the Potomac basin but are now gone. Game fish and shellfish that provided a commercial fishery, such as sturgeon, shad, striped bass and oysters, have been reduced in numbers and not longer profitable.
Researching Nature at Potomac Heritage Trail
The Potomac Heritage Trail is a natural oasis for visitors and for scientific researchers because of its protected natural landscape. The research done here provides the accurate and current natural resource information we need to provide to best care for the park. Scientists look at what key resources are present in the park, if they are stable or changing, how ecosystems are changing over time, and how much change is normal.
Like a physician monitoring a patient's heartbeat and blood pressure, National Park Service ecologists with the National Capital Region Inventory & Monitoring Network collect long-term data on forest vegetation, bird and amphibian communities, water quality, and other key resources in national parks that make up the Potomac Heritage Trail, analyze the monitoring results, and share them.
Last updated: July 21, 2023