Lake Drummond is named for a former North Carolina governor who had been an ally of Governor Berkeley of Virginia, but then chose the wrong side in Bacon's Rebellion in 1676. After the rebellion collapsed, the last words of Governor Berkeley to William Drummond were "Mr. Drummond, you are very welcome. I am more glad to see you than any man in Virginia. Mr. Drummond, you shall be hanged in half an hour."1
The lake is one of just two natural lakes in Virginia. Mountain Lake (in Giles County) may have formed on Salt Pond Mountain by eroding a basin into an unusual structure in the Clinch Sandstone formation. There, cracks in the sandstone have formed a depression allowing water to seep underground, etching a lake basin in the bedrock. Intermittently, the cracks are opened (allowing Mountain Lake to drain and be replaced by a meadow) or blocked (causing the lake to reform).
The creation of Lake Drummond is even more mysterious. Geologically, Lake Drummond is an unusually large (3,108 acre) open body of water on the Coastal Plain, east of the Suffolk Scarp. At normal water levels, the lake is 6-7 feet deep and the surface is 18 feet above sea level. There is little topographic relief in the area; elevation drops at one foot per mile near the lake.2
There's no obvious reason for one big lake to exist in the middle of the Great Dismal Swamp, which extended all the way to Back Bay/Albemarle Sound in the colonial era. There is no network of streams draining a watershed upstream and emptying into the lake. Lake Drummond is a high point in the middle of the remnants of the swamp.
In fact, ditches - including some dug during the time when Virginia was a colony, such as "Washington Ditch" initiated by George Washington - are supplied naturally with water that drains by gravity out of the lake. When lake level drops to 15.75 feet, the U.S. Army Corps of Engineers stops releasing water from Lake Drummond to supply the Dismal Swamp Canal. As described by the US Fish and Wildlife Service:3
The origin of the swamp dates back to the end of the last ice Age:4
Source: US Fish and Wildlife Service
Geologically, the swamp and lake formed on top of coarse sand that is very permeable, but with layers of clay and silt that block water flow. An organic layer of peat has accumulated at the surface, and is up to five feet thick. Underneath the peat is the Sandbridge Formation, with upper layer of silty clay and a lower layer of sand. the next layer down is the London Bridge Formation, mostly clay silt, and then layers of sand and silt called the Norfolk Formation. The Norfolk Formation is exposed to the west of the swamp at the Suffolk Scarp:5
One possibility: Lake Drummond was formed when a natural fire burned a "hole" in the peat of the Great Dismal Swamp. In 2011, during a severe drought, one of the largest wildfires in the modern history of Virginia burned 6,500 acres of the swamp. The "Great Conflagration" of 1923-26 was probably even more significant.6
Perhaps 9,000 years ago, a lightning strike triggered an extraordinary fire that burned hot enough to destroy the peat layer, down to the clay confining layer that keeps the water in the swamp from draining into the sand underneath. Such a fire could have carved out a bowl within the deep peat, creating a hole that developed into Lake Drummond.
Lake Drummond resembles may other elliptical "bays" or small lakes on the Coastal Plain of the Eastern United States, from Florida to New Jersey, with a southeast-northwest orientation. They might have formed naturally in the Pleistocene as the climate changed, perhaps comparable to the formation of modern lakes on the Arctic Coastal Plain. The elliptical pattern could have been caused by winds blowing from the southwest and forming sand ridges, which have since been vegetated - and in some cases flooded to form lakes - as rainfall increased in the last 20,000 years.7
Another possible cause is that Lake Drummond was formed by an icy comet/meteor that broke up in the atmosphere and peppered the Coastal Plain. Meteorite fragments are rare in the area, so there is insufficient evidence to claim the lake is a meteor crater. However, shock waves from a comet exploding above the surface of the earth could have carved out the initial depressions, which then filled with water and have been covered with vegetation.
Fragmentation of an extra-terrestrial comet in the atmosphere might explain the regular pattern of the ellipses, their large number (roughly 500,000), and the absence of meteorite fragments. (Comets, because of their icy composition, leave no trail of "meteorites" to record their impact or disintegration in the lower atmosphere.) The Younger Dryas period of global cooling, 12,800 years ago, could have been triggered by a comet's impact. Lake Drummond could be a larger-than-usual Carolina Bay, formed recently as earth's surface was disturbed by a dying comet.8
The ground surrounding Lake Drummond includes dry land as well as swamp. The dry land is typically peat (dead vegetation that has not decomposed yet, or been compressed into lignite/coal) with sand underneath. Such soil is unsuitable for agriculture, but Atlantic White Cedar (Chamaecyparis thyoides) thrives in places high enough for plant roots to grow above the water table.
The cedar is a pioneer species, capable of regrowing from seed after fires/storms and forming dense stands. It is not an "old growth" species that replaces itself, perpetuating Atlantic White Cedar forests indefinitely. Without disturbance, other species such as red maple ultimately dominate land originally covered by Atlantic White Cedar trees.
As one researcher noted:9
Atlantic White Cedar has a grain that makes it easy to split/saw. The high resistance to rot also made the species a high-value target for lumber companies. Most forested areas east of the Great Dismal Swamp were harvested in the 1700-1900's, and much of the remaining timber was burned by wildfires.
Forest regeneration was blocked where land was timbered, then ditched and drained for planting crops. Efforts to drain swamps altered the hydrologic regime, triggering the growth of hardwoods and blocking reproduction of Atlantic White Cedar. By one description, the cedar forest were "mined" rather than "managed."10 By the 1950's, the Great Dismal Swamp was one of the last remaining areas with a substantial Atlantic White Cedar forest.
The Union Camp Corporation, a lumber company, donated 49,000 acres of logged-over swampland to The Nature Conservancy in 1973, and the non-government organization then transferred the property to the Federal government. Today, Lake Drummond is in the middle of the Dismal Swamp National Wildlife Refuge, managed by the US Fish and Wildlife Service in the Department of the Interior. Further land acquisition has expanded the refuge to over 110,000 acres, but that is only 10% of the size of the original swampland existing before European colonization.11
One goal of the US Fish and Wildlife Service is to restore the natural flow of water in the swamp, undoing the effects of ditches and logging roads that have created drier-than-natural and wetter-than-natural areas. The organic soils in the swamp are normally 85-95% water. When they dry out, the soil particles alter into a granular form that will not absorb water even after water levels rise again, and oxidize away. Keeping the soils saturated is essential for minimizing the intensity and size of wildfires in the Great Dismal Swamp.12
Hurricanes and major forest fires, influenced by the altered drainage, alter the ecosystem even more rapidly. In 2003, Hurricane Isabel flattened 80% of the purest cedar stands in the refuge. Fires - and prevention of fires - threaten the continued existence of the Atlantic white cedar plant community:13
forest with Atlantic White Cedar at Dismal Swamp
Source: US Fish and Wildlife Service National Digital Library
Dismal Swamp is excellent habitat for beeding mosquitoes in the summer; visitors to the 113,000-acre wildlife refuge get to experience annoying as well as attractive critters. The mosquitoes are considered wildlife, like bears and birds.
Water levels of the lake and swamp are controlled by Federal land managers, and bear/deer hunting is authorized, so the "natural" character of the refuge is modified by human action, but insects are protected as part of the natural food chain. Because the Great Dismal Swamp National Wildlife Refuge is Federally-protected, the City of Suffolk is not allowed to spray chemicals within the refuge to kill the mosquitoes.14
The effect of that prohibition extends beyond the refuge boundaries. Mosquitoes are the primary vector that transfers Eastern equine encephalitis (EEE) and West Nile virus from birds in the refuge to horses and humans in the cities of Suffolk and Chesapeake. There is a tradeoff between protecting natural processes in natural areas vs. protecting human health...
Jerico Ditch, Great Dismal Swamp National Wildlife Refuge
Source: US Fish and Wildlife Service, National Digital Library
References1. Dictionary of Virginia Biography. (2010, June 9). William Drummond (d. 1677). Retrieved September 12, 2010, from Encyclopedia Virginia: http://www.EncyclopediaVirginia.org/Drummond_William_d_1677 (last checked September 12, 2010)
2. "Great Dismal Swamp National Wildlife Refuge and Nansemond National Wildlife Refuge Final Comprehensive Conservation Plan," US Fish and Wildlife Service, July 2006, p.36, p.44, http://library.fws.gov/CCPs/GDS/greatdismalswamp06.pdf (last checked September 9, 2012)
3. "Great Dismal Swamp National Wildlife Refuge and Nansemond National Wildlife Refuge Final Comprehensive Conservation Plan," p.41, p.44
4. "Great Dismal Swamp National Wildlife Refuge and Nansemond National Wildlife Refuge Final Comprehensive Conservation Plan," p.60
5. "Great Dismal Swamp National Wildlife Refuge and Nansemond National Wildlife Refuge Final Comprehensive Conservation Plan," pp.37-38
6. "The Great Dismal Swamp a year after the fire," Chicago Tribune, August 4, 2012, http://www.chicagotribune.com/news/dp-nws-great-dismal-swamp-20120804,0,6818233,full.story; "Great Dismal Swamp wildfire still burning after more than 2 months," The Washington Post, October 6, 2011, http://www.washingtonpost.com/national/health-science/2011/10/05/gIQALlJYRL_story.html (last checked September 9, 2012)
7. Robert E. Carvera, George A. Brook, "Late pleistocene paleowind directions, Atlantic Coastal Plain, U.S.A," Palaeogeography, Palaeoclimatology, Palaeoecology, Volume 74, Issues 3–4 (30 November 1989), http://dx.doi.org/10.1016/0031-0182(89)90061-8 (last checked September 9, 2012)
8. James H. Wittke, James C. Weaver, Ted E. Bunch, James P. Kennett, Douglas J. Kennett, Andrew M. T. Moore, Gordon C. Hillman, Kenneth B. Tankersley, Albert C. Goodyear, Christopher R. Moore, I. Randolph Daniel, Jr., Jack H. Ray, Neal H. Lopinot, David Ferraro, Isabel Israde-Alcántara, James L. Bischoff, Paul S. DeCarli, Robert E. Hermes, Johan B. Kloosterman, Zsolt Revay, George A. Howard, David R. Kimbel, Gunther Kletetschka, Ladislav Nabelek, Carl P. Lipo, Sachiko Sakai, Allen West, and Richard B. Firestone, "Evidence for deposition of 10 million tonnes of impact spherules across four continents 12,800 y ago," Proceedings of the National Academy of Sciences (PNAS), published ahead of print May 20, 2013, http://dx.doi.org/10.1073/pnas.1301760110; J. Ronald Eyton, Judith I. Parkhurst, "A Re-Evaluation Of The Extraterrestrial Origin Of The Carolina Bays," April 1975, http://abob.libs.uga.edu/bobk/cbayint.html; Michael Davias, "Correlating the Orientation of Carolina bays to a Cosmic Impact," http://cintos.org/SaginawManifold/introduction/index.html (last checked May 26, 2013)
9. John E. Kuser, George Zimmermann, "Restoring Atlantic White-Cedar Swamps: A Review of Techniques for Propagation and Establishment," Tree Planters Notes, Volume 46, Number 3, Summer 1995, http://www.stockton.edu/~wcedars/treeplnt.html (last checked July 6, 2013)
10. L. Eric Hinesley, "Research at N. C. State University related to regeneration of Atlantic White Cedar (AWC) and Baldcypress," US Fish and Wildlife Service, August 2002, http://www.fws.gov/nc-es/coastal/plnwrawc/atlanticwhitecedarresearch.html (last checked July 6, 2013)
11. "Great Dismal Swamp National Wildlife Refuge and Nansemond National Wildlife Refuge Final Comprehensive Conservation Plan," p.4; Aimlee D. Laderman, "The Ecology Of Atlantic White Cedar Wetlands: A Community Profile," US Fish and Wildlife Service Biological Report 85, July 1989, p.19, http://www.nwrc.usgs.gov/techrpt/85-7-21.pdf (last checked July 6, 2013)
12. "Great Dismal Swamp National Wildlife Refuge and Nansemond National Wildlife Refuge Final Comprehensive Conservation Plan," pp.38-39
13. "Great Dismal Swamp National Wildlife Refuge and Nansemond National Wildlife Refuge Final Comprehensive Conservation Plan," pp.21-22, p.59
14. "Regulations are barriers to mosquito control in Suffolk," The Virginian-Pilot, July 6, 2013, http://hamptonroads.com/node/682517 (last checked July 6, 2013)
Dismal Swamp National Wildlife Refuge
Source: US Fish and Wildlife Service Great Dismal Swamp National Wildlife Comprehensive Conservation Plan