Drivers can go west on US 58 from the Atlantic Ocean to Cumberland Gap, paralleling the North Carolina border. Signs on bridges identify when the highway crosses over the Nottoway, Meherrin, Roanoke, New, Holston, Clinch, and Powell rivers, and many smaller streams. Less obvious to travvelers are the crossings of watershed divides, each defining the boundary of a watershed with streams and rivers flowing to the Altantic Ocean or Gulf of Mexico.
There is another continental divide in the Rocky Mountains, separating waters that flow to the Pacific Ocean vs. the Gulf of Mexico. The first Americans to cross that Western Continental Divide were recent immigrants from Russia who had crossed the Bering land bridge. They were headed east, in small hunting and gathering groups.
Roughly 15,000 years later, long after it had become routine for the local Native Americans to go back and forth over the Continental Divide in the Rocky Mountains, Lewis and Clark brought the first citizens of the United States to Lemhi Pass on the current Montana/Idaho border. In 1805, the travelers were headed in the other direction, back towards the west.
Those explorers were looking, in part, for the closest thing to a water-level passage connecting the Mississippi River with the salt water Pacific Ocean. Under the guidance of President Thomas Jefferson, the explorers followed the Missouri River upstream. They never realized that the topography of the Rockies would offer a far-better alternative at South Pass, and no canal would ever connect the Missouri River to the Columbia.
Many emigrants travelling to the west coast, including the '49's rushing to California after the discovery of gold, crossed at South Pass in modern-day Wyoming. Cross it on Interstate 80, and you'll hardly notice the shift from going uphill to downhill. Of course, that's why emigrants with only 4 horses instead of a Sport Utility Vehicle thought South Pass's gentle slopes were such a great choice compare to Lemhi Pass.
The Eastern Continental Divide separates the waters flowing to the Atlantic from those flowing to the Gulf of Mexico. The divide crosses Virginia from Carroll County at the North Carolina line to Giles County at the West Virginia border. Rainwater in southwestern Virginia flows to the Gulf of Mexico.
If you drive north on Route 460 into Blacksburg from I-81, most of that road follows the Eastern Continental Divide until the airport. Rain falling to the east of the highway (and on the new bypass) flows to the North Fork of the Roanoke River and down to Albermarle-Pamlico Sound in North Carolina. Rain to the west will drain into the New River. That water will flow through West Virginia, down the Ohio River, and go with the Mississippi River past New Orleans. After dropping a little bit of sediment from Montgomery County into the birdsfoot delta of the Mississippi River, the runoff from the Blacksburg airport, Gillies and other restaurants in downtown Blacksburg, and the Virginia Tech campus will finally enter the Gulf of Mexico.
Drivers who go from Blacksburg west on US 460 towards West Virginia will first climb to the crest of Brush Mountain, then drop down into a valley on the west side. At the bottom, before the road climbs up Sinking Creek Mountain, is an intersection with a sign for the US Forest Service recreation site at Pandapas Pond. That artificial pond marks the headwaters of Poverty Creek. It flows into Toms Creek and joins the New River at Whitethorne, roughly 500 feet lower in elevation.
At that intersection, Route 460 again marks the continental divide. Rain that falls on the north side of US 460 (on the opposite side of the highway from Pandapas Pond) will flow through Craig Creep, dropping roughly 1,100 feet before reaching the James River just upstream of Eagle Rock (halfway between Clifton Forge and Buchanan). From there, the water will drop another 1,200 feet before reaching sea level at Richmond.
James Pandapas dammed Poverty Creek to create a recreation site for his employees, and then later sold the pond to the US Forest Service
Craig Creek and Poverty Creek are both eroding away at the ridge which separates them, the ridge on which US 460 runs. Craig Creek is likely to erode faster than Poverty Creek. The distance from the divide on US 460 to sea level (313 miles) is far less than the distance to the Gulf of Mexico (2,000 miles), but Craig Creek's capacity to etch into bedrock might be greater primarily because hard-to-erode layers in the bedrock of the New River reduce the erosive power of Poverty Creek. US Geological Survey (USGS), "National Atlas Streamer," Stream Trace Detailed Reports for Craig Creek and confluence of Poverty Creek/New River, http://nationalatlas.gov/streamer/Streamer/streamer.html (last checked August 3, 2013)
At some point in the future, after Craig Creek carves its valley more than 500 feet deeper, it could intercept the New River. The upper New River will then be diverted to flow into the James River and on to the Atlantic Ocean, rather than to the Gulf of Mexico.
That act of "stream piracy," diverting the upper New River into the Chesapeake Bay watershed, will shift the Eastern Continental Divide. The headwaters of the Tennessee River (the Holston, Clinch, and Powell rivers) will still carry water to the Gulf of Mexico, but in nearly all of Virginia the "pirated" New River will become part of the Chesapeake Bay watershed.
The new Eastern Continental Divide will become the watershed divide between the New/Tennessee river drainages. That divide on US 11 is hard to recognize today. The crest is at Rural Retreat, where the soft drink Dr. Pepper was invented, in Wythe County. It is the highest elevation on the original Virginia and Tennessee Railroad connecting Lynchburg and Knoxville, but such a gentle crest that even a bicyclist on Route 11 would have to be paying close attention to notice the exact location of when uphill becomes downhill.
The hypothetical transformation of the watershed boundaries by piracy of the New River will not occur for thousands or even millions of years, if it ever does. However, such a shift in the continental divide has already occurred more than once.
US 58 climbs up the Blue Ridge at the Meadows of Dan and reaches the crest - not at the Blue Ridge Parkway, but east of the parkway at the Patrick/Floyd county line. That crossing is the Eastern Continental Divide. To the east, raindrops flow downhill to the Atlantic Ocean. To the west, water drains to the Gulf of Mexico via the New River or tributaries of the Tennessee River, ultimately flowing into the Mississippi River and going past New Orleans.
Source: US Geological Survey (USGS),
Source: Virginia Department of Conservation and Recreation (DCR), Virginia Hydrologic Unit Explorer
the Dan River pirated the headwaters of Reed Island Creek, diverting the water to the Atlantic Ocean and altering the Eastern Continental Divide
The headwaters of the Dan River used to flow westward into Reed Island Creek. The Dan River eroded the east side of the Blue Ridge faster than Reed Island Creek eroded the west side. Near the Pinnacles of Dan, the headwaters of the Dan River intercepted the headwaters of Reed Island Creek, and the location of the Eastern Continental Divide shifted when the watershed boundaries shifted.
John T. Hack, "Physiographic Divisions and Differential Uplift in the Piedmont and Blue Ridge," US Geological Survey (USGS), Professional Paper 1265, pp.38-40, http://pubs.usgs.gov/pp/1265/report.pdf (last checked August 4, 2013)
A more substantial change in the location of the Eastern Continental Divide occurred when the headwaters of the Potomac River were pirated about 5 million years ago. The beginning of the Potomac River used to be on the east side of the Blue Ridge. When erosion opened a gap through the Blue Ridge at Harpers Ferry, the Shenandoah River and the upper Potomac River were able to flow directly east to the Atlantic Ocean. The location of the Eastern Continental Divide moves by the natural process of erosion - the same process that created the divide in the first place.
The geological basis for the existence of the Eastern Continental Divide is still poorly understood. For 200+ million years, the Applachians have eroded away. Why is there still an escarpment (the Blue Ridge) with significant topographic relief, instead of a flat eroded peneplain, between the Atlantic Ocean and the Midwest?
Some force has lifted up the Appalachians faster than erosion has cut down the mountains. Uplift has been fast enough so no river flows completely across the Appalachians. (The New River starts in the midddle of the Blue Ridge at Blowing Rock, NC and does not completely bisect the Blue Ridge.)
It appears that for 200 million+ years, an Eastern Continental Divide has separated streams flowing westward towards the Mississippi River from streams flowing east to the Atlantic Ocean. Watershed boundaries have migrated as streams etched new paths and deposited sediments downstream, but the divide has not disappeared.
watershed boundaries reveal that, in most of Virginia, the Eastern Continental Divide separating Gulf of Mexico/Atlantic Ocean watersheds does not match up with the crest of the Blue Ridge
Source: US Geological Survey (USGS), National Atlas
The continental divide along the Blue Ridge south of 40° latitude apparently has been present for many millions of years, perhaps since the Cretaceous Period. At that time, when dinosaurs were wandering across the landscape, the Blue Ridge in southern Virginia may have been 13,000 feet high. Erosion has lowered the mountain heights, but the divide has remained essentially in the same place.
John Tilton Hack, "Rock control and tectonism: their importance in shaping the Appalachian Highlands," p.22, pp.27-31 (last checked August 3, 2013)
Different rates of erosion of different bedrock layers is a key reason some version of the Eastern Continental Divide has survived for so long, just like the Blue Ridge escarpment. Limestone formations, exposed in valleys to the west of the Blue Ridge, erode faster than the crystalline bedrock of the Blue Ridge.
Many watershed divides in the Valley and Ridge physiographic province owe their existence to the contrasting ability of rain/wind to erode hard sandstone layers vs. limestone. The hard sandstone mountains today (such as Massanutten Mountain east of Harrisonburg) are eroding, but eroding at a rate slower that the limestones. The valleys west of the Blue Ridge are etched out of softer rock than the adjacent mountains.
North of Roanoke, differential erosion can also explain the topographic relief of the Blue Ridge vs. the Piedmont to the east. The Blue Ridge is formed from volcanic/metamorphic formations that are substantially more resistant to erosion that the Piedmont bedrock. However, south of Roanoke, the bedrock in the Piedmont physiographic province erodes at essentially the same rate as the Blue Ridge, but there is a clear difference between the rolling hills of the Piedmont and the "ridge" to the west:
Why? Theories include asymmetric uplift by tectonic forces along a fault at the base of the Blue Ridge, more-rapid erosion by streams draining east to the Atlantic Ocean, and "flexural isostasy" as sediments deposited along the Atlantic Ocean shoreline pushed down the crust there and triggered an uplift further inland. Gregory C. Bank, "Testing the Origins of the Blue Ridge Escarpment," Masters Thesis, Virginia Tech, July 27, 2001, pp.1-3, http://scholar.lib.vt.edu/theses/available/etd-08272001-112622/unrestricted/Thesis-ETD.pdf
The East Coast has tilted towards the Atlantic Ocean since Africa pulled away and the ocean first formed. It appears the crust has warped during the tilting, so the Blue Ridge has been lifted higher than the Piedmont. There is a distinctive area of low gravity in the central and southern Appalachians, due perhaps to a change in thickness of the deep crust dating back a billion or so years to the Grenville orogeny.
the watershed divide between the Shenandoah and James rivers at Raphine/Steeles Tavern is not obvious, in contrast to the Blue Ridge or subwatersheds defined by individual ridges in the Valley and Ridge physiographic province
Source: USGS Earth Resources Observation and Science (EROS) Center, National Elevation Dataset - Shaded Relief Map of Virginia
A tiny portion of Virginia drains into South Carolina. The Yadkin River watershed in Patrick and Carroll counties is on the eastern side of the Eastern Continental Divide, but the Ararat River and other streams flow through North Carolina into the Pee Dee River of South Carolina. Drivers on I-77 from North Carolina to Fancy Gap cross the only part of Virginia where rainwater flows 376 miles to reach the Atlantic Ocean in South Carolina, north of Charleston.1