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This article describes the location & type of sinkholes occurring in Virginia.
This article series explains what sinkholes are and why they occur, describes their effects on buildings, and gives building and site inspection advice useful in identifying areas where there is an increased risk of sink holes at properties.
The photograph (above-left) of a sinkhole opening in a residential yard in Pennsylvania is from Kochanov, W.E. and illustrates the child hazard or even adult sinkhole hazard that can be formed by storm water drainage.
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Sinkholes in Virginia
The Virginia Department of Mines, Minerals, and Energy reports that sinkholes have been reported in that state since colonial times.
“In the spring of the year 1780, the earth at the
bottom of this sink suddenly gave way and fell into
the cavity below, forming a circular aperture about
the ordinary circumference of a common artificial
well . . .
There being no artificial or natural means
to prevent the earth immediately about the well from
falling in, the aperture is greatly enlarged, forming
a sloping bank, by which a man on foot can easily
descend within eight or ten feet of the water
.... The
whole depth of the cavity is thirty or thirty-five feet”
(Kercheval, 1850, p. 273).
As in several of the other locations of sinkholes around the U.S., Canada, and other countries, in Virginia sinkholes are associated with karst formations. The sinkhole photograph above (from Virginia's DMME) shows a sinkhole that formed in Russell County, Virginia. According to the DMME, [quoting]
In Virginia the formation and modification of sinkholes (also known as sinks, dolines and dolinas) is a natural
process in areas underlain by limestone and other soluble rock. The location and rate at which sinkholes form
can be affected by man’s activities.
Sinkholes are basin-like, funnel shaped, or vertical-sided depressions in the land surface. In general, sinkholes form by the subsidence of unconsolidated materials or soils into voids created by the dissolution of the underlying soluble bedrock.
The rock exposed in a collapsed sinkhole is usually weathered and rounded, but some sinkholes contain freshly broken rock along their steep sides. Freshly broken rock may indicate that the sinkhole has formed by the collapse of a cave (naturally occurring) or a mine (man-made).
Where sinkholes and caves have formed by the dissolution of soluble rock, such as limestone, dolomite, and gypsum, surface water is uncommon and streams may sink into the ground.
This type of topography, formed by dissolution, is referred to as karst terrain. In karst terrain, sinkholes are input points where surface water
enters the groundwater system.
Although a sinkhole can form suddenly and without warning, this list, courtesy of the state's department of geology, lists several specific signs that can signal potential development:
Slumping or falling fence posts
Wilting vegetation
Discolored well water
Structural cracks in walls, floors, or foundations.
Cracks in soil/subsidence.
Location of Sinkholes in Virginia
The VA DMME [and the Virginia Division of Geology and Mineral Resources within the DMME]provides the map showing the location of sinkholes by underlying cause and probability. Quoting:
Sinkholes are most prevalent in karst terrains, but
they occur throughout Virginia. Areas which may contain
sinkholes:
Subsidence/sinkholes are related to mining activity
or soil piping;
Karst, sinkholes are related to the dissolution
of limestone and dolomite (refer to Hubbard, 1983 and 1988, for
more detail) or soil piping;
Sinkholes are very rare and are
related to soil piping;
Sinkholes are rare and are related to soil
piping or dissolution of sparse carbonate rock;
Sinkholes are
related to the dissolution of shell concentrations in sand and soil
piping.
The bare minimum that a property owner needs to know about sinkholes or any other sudden subsidence
of soils at a property is that these conditions might be very dangerous.
Someone falling into a sink hole
or into a collapsing septic tank could be seriously injured or even die.
If a suspicious hole, subsidence,
or depression appears at a property the owner should rope off and prevent access to the area to prevent
anyone from falling into the opening, and then should seek prompt assistance from a qualified expert,
geotechnical engineer, septic contractor, excavator, or the like.
Virginia Sinkhole & Subsidence Resources
Boon, John D., John M. Brubaker, David R. Forrest, CHESAPEAKE BAY LAND SUBSIDENCE AND SEA LEVEL CHANGE,
AN EVALUATION OF PAST AND PRESENT TRENDS AND FUTURE OUTLOOK [PDF] (2010) A report to the
U.S. Army Corps of Engineers,
Norfolk District, Virginia Institute of Marine Science
Special Report No. 425 in Applied Marine
Science and Ocean Engineering, (College of William & Mary), retrieved 2022/08/14, original source: https://www.vims.edu/GreyLit/VIMS/sramsoe425.pdf
VA DMMR SINKHOLES and KARST TERRAIN in VIRGINIA [PDF] Virginia Division of Geology and Mineral Resources, "Geologic Hazards", retrieved 2019/11/19, original source: https://www.dmme.virginia.gov/DGMR/sinkholes.shtml, Current link citation 2022/-08/14: https://www.energy.virginia.gov/geology/sinkholes.shtml
Excerpts:
Sinkholes are bowl-shaped, funnel-shaped, or vertical-sided depressions in the land surface that form over underground voids.
These depressions can range from a few feet to several hundred feet in diameter, and usually result from the natural collapse of soluble bedrock and overlying soil. Sinkholes can also result from mining, groundwater pumping, and leaking water, sewer, and storm water pipes.
Watch out:
Subsidence of the ground is usually gradual, but on occasions it can be sudden and dramatic.
In Virginia, the principal area affected by sinkholes is the Valley and Ridge province, an extensive karst terrain underlain by limestone and dolomite, but narrow marble belts in the Piedmont and some shelly beds in the Coastal Plain are also pocked with sinkholes.
Dramatic collapses that swallow homes or persons have happened in Virginia, but are rare.
The most notable incidents occurred in the City of Staunton: on August 11, 1910, parts of several homes and the firehouse were lost in a series of sinkholes on Baldwin Street and Central Avenue, and on October 28, 2001, a 45-feet deep chasm opened up on Lewis Street.
In April of 2000, thirty-two sinkholes were reported in the upper Shenandoah Valley after seven inches of rain fell after a long dry spell.
Hubbard, David A., Jr., SINKHOLES in VA [PDF] (2014) Virginia Division of Mines, Mineral Resources, & Energy
VA, VIRGINIA RESIDENT'S GUIDE TO SINKHOLES [PDF] (2017) Virginia Cave Board, Virginia Department of Conservation & Recreation, retrived 2022/08/14, original source: https://www.dcr.virginia.gov/natural-heritage/vcbsinkholes
VA, NORTHERN VIRGINIA
HAZARD MITIGATION
PLAN [PDF] (2017), - retrieved 2022/08/14, original source: http://arlington.granicus.com/MetaViewer.php?view_id=2&event_id=1101&meta_id=163110
Pertinent cities & towns in Virginia: Arlington County
Fairfax County
Loudoun County
Prince William County
City of Alexandria
City of Fairfax
City of Falls Church
City of Manassas
City of Manassas Park
Town of Dumfries
Town of Haymarket
Town of Herndon
Town of Leesburg
Town of Lovettsville
Town of Middleburg
Town of Purcellville
Town of Occoquan
Town of Round Hill
Town of Vienna, Virginia.
Excerpt: For the purposes of compliance with the
Disaster Mitigation Act as further specified by Interim Final Rule 44 CFR Section
206.401(c)(2)(i), this Plan addresses in full only the following hazards: Flood, High Wind,
Tornadoes, Winter Storms, Drought, Earthquakes, Landslides, Wildfire, Sinkholes, Dam Failure,
and Extreme Temperatures.
See Section XIV, Sinkholes / Karst / Land Subsidence, beginning on pp. 4-172
Hubbard, D. A., Jr., 2003, Use of regional sinkhole mapping for sinkhole susceptibility maps, in Beck, B. F., ed., ASCE Geotechnical Special Publication No. 122, p. 61-71.
Hubbard, D. A., Jr., 2001, SELECTED KARST FEATURES OF THE CENTRAL VALLEY AND RIDGE PROVINCE, Virginia [PDF] (2001) Virginia Division of Mineral Resources, Publication 167, one sheet.
Sinkholes, cave entrances, springs, and stream insurgences are plotted on a map of the Valley and Ridge province west of 81-degrees of longitude with karst areas subdivided into 5 carbonate units. Text describes karst and karst hazards with photographic illustrations of some karst features and hazards.
Hubbard, D. A., Jr. and Sterrett, R. M., 1994, Groundwater contamination in Virginia karst: Case studies (abs.): Program and Abstracts, 37th Annual Meeting of the Association of Engineering Geologists, Williamsburg, VA, p. 49.
Hubbard, D. A., Jr., 1999, Highways in Virginia karst: Resource and hazard considerations: 50th Annual Highway Geology Symposium & TRB Karst Meeting, Proc. & Field Trip Guide, 13-22.
Hubbard, D. A., Jr. and Sterrett, R. M., 1994, Groundwater contamination in Virginia karst: Case studies (abs.): Program and Abstracts, 37th Annual Meeting of the Association of Engineering Geologists, Williamsburg, VA, p. 49.
Hubbard, D. A., Jr., 1983, Selected karst features of the northern Valley and Ridge province, Virginia: Virginia Division of Mineral Resources, Publication 44, one sheet.
Virginia DMR, SINKHOLES, Virginia Division of Mineral Resources,
Virginia Department of Mines, Minerals and Energy, www.dmme.virginia.gov Virginia Department of Mines, Minerals and Energy
Division of Mineral Resources 900 Natural Resources Drive, Suite 500 Charlottesville, VA 22903 Sales Office: (434) 951-6341 FAX : (434) 951-6365
Geologic Information: (434) 951-6342 http://www.dmme.virginia.gov/ divisionmineralresources.shtml - Web search 06/09/2010
Weary, D.J., 2008. Preliminary Map of Potentially Karstic Carbonate Rocks in the Central and Southern Appalachian States: USGS Open-File Report 2008-1154 http://pubs.usgs.gov/of/2008/1154/
Daniel Friedman - Florida Suncoast ASHI Educational Seminar - 1 May 2004, updated 2007, 2008, 2014, 2019, 2022.
Question: are there sinkholes in Rockingham County VA?
Arianne Young said:
I heard where Misty and Meadows meet in Rockingham County, Va are over a sink hole. How can I find out if the builders built these duplexes over a sink hole?
Some of us have notices doors don't close tight, windows as well can be difficult to close...this is zip code 22801
Thank you for any direction or guidance you can give us. Thank you.
Image source, VA, DMME, retrieved 2019/11/18 original source: www.dmme.virginia.gov/DGMR/sinkholes.shtml
[Click to enlarge any image]
Reply:
Arianne,
Rockingham county is just north of where I went to school, in Rockbridge County Virgina; by this map provided by the VA Division of Geology and Mineral Resources, both Rockbridge and Rockingham are along the northwestern state border - that RED area in the DMME's map, showing where there are significant karst formations - i.e. in areas of sinkhole risk.
We already know that. There's not "one" or "a" sink hole along that area; rather it's an underlying type of rock formation (karst or limestone) that means there's risk of sinkholes and subsidences.
Beyond that, if there is settlement or signs of settlement where your duplex homes are located, it'd make sense to bring in a local geotechnical engineer who can inspect the properties for patterns of subsidence or movement and if justified, and if a specific sinkhole issue is not already known, she can conduct soil borings to investigate further.
Let me know what you're told as that'll certainly help other Virginia readers in Rockingham and nearby areas.
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Building Pathology, Deterioration, Diagnostics, and Intervention, Samuel Y. Harris, P.E., AIA, Esq., ISBN 0-471-33172-4, John Wiley & Sons, 2001 [General building science-DF] ISBN-10: 0471331724
ISBN-13: 978-0471331728
Building Pathology: Principles and Practice, David Watt, Wiley-Blackwell; 2 edition (March 7, 2008) ISBN-10: 1405161035 ISBN-13: 978-1405161039
Diagnosing & Repairing House Structure Problems, Edgar O. Seaquist, McGraw Hill, 1980 ISBN 0-07-056013-7 (obsolete, incomplete, missing most diagnosis steps, but very good reading; out of print but used copies are available at Amazon.com, and reprints are available from some inspection tool suppliers). Ed Seaquist was among the first speakers invited to a series of educational conferences organized by D Friedman for ASHI, the American Society of Home Inspectors, where the topic of inspecting the in-service condition of building structures was first addressed.
Building Failures, Diagnosis & Avoidance, 2d Ed., W.H. Ransom, E.& F. Spon, New York, 1987 ISBN 0-419-14270-3
"A Foundation for Unstable Soils," Harris Hyman, P.E., Journal of Light Construction, May 1995
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