Discover Virginia


Virginia overview

The Commonwealth of Virginia is a state inVirginia's long east-west axis means that
the Southern United States. Named after Queenmetropolitan northern Virginia lies as close
Elizabeth I of England, who was known as theto New York City and New England as to its
Virgin Queen, this commonwealth was one ofown rural western panhandle. Conversely, Lee
the thirteen colonies that revolted againstCounty, at the tip of the panhandle, is
British rule in the American Revolution.closer to eight other state capitals than it
Virginia was the first part of the Americasis  to  Richmond,  Virginia's  own  capital.
to be continuously inhabited by British
colonists from its founding as a EuropeanVirginia has a number of National Park
colony up to the American Revolution. ItService units, including one national park,
included area explored by the 1584 expeditionthe Shenandoah National Park. For a list of
of Sir Walter Raleigh along the coast ofall areas managed by the National Park
North America, and at one time it alsoService within Virginia, see: List of areas
included Bermuda (or Virgineola). The Londonin the National Park System of the United
Virginia Company became incorporated as aStates  in  Virginia.
joint stock company by a proprietary charter
drawn up on April 10, 1606. The charterClimate
granted lands stretching from approximately
the 34th parallel (North Carolina) north toThe climate is considered mild compared to
approximately the 45th parallel (New York)other areas of the United States. Most of the
and from the Atlantic Ocean westwardstate east of the Blue Ridge, plus the
(although the Third Charter of 1612 extendedsouthern part of the Shenandoah Valley, has a
its boundaries far enough across the Atlantichumid subtropical climate (Koppen climate
to incorporate Bermuda, which the company hadclassification Cfa). In the mountainous areas
been in possession of since 1609). Thewest of the Blue Ridge, the climate becomes
capital is Richmond and the most populoushumid  continental  (Koppen  Dfa).
city  is  Virginia  Beach.
However, substantial variations occur because
Virginia is known as the "Mother ofof the state's significant relief. Elevations
Presidents", because it is the birthplace ofin Virginia vary from sea level to Mount
eight U.S. presidents (George Washington,Rogers at 5,729 ft (1,746 m) above sea level
Thomas Jefferson, James Madison, Jameswith major gradations occurring at the edges
Monroe, William Henry Harrison, John Tyler,of the Atlantic Ocean, the end of the
Zachary Taylor, and Woodrow Wilson), exceededPiedmont, and the Blue Ridge and Allegheny
by no other state. Most of the United States'chains of the Appalachian Mountains. The
early presidents were from the state.usually moderating influence of the ocean
Virginia has also been known as the "Motherfrom the east, powered by the Gulf Stream, is
of States", because portions of the originalinterspersed with brief moments of danger due
Colony subsequently became Kentucky, Indiana,to the potential for hurricanes near the
Illinois, and West Virginia as well as somemouth of Chesapeake Bay. On the other hand,
portions of Ohio. Additionally, most of whatcold air masses arrive over the mountains,
is now Wisconsin and Michigan was alsoespecially in winter, leading to significant
briefly claimed by Virginia during thesnowfalls. However, in something of an
Revolutionary  War.anomaly, much of the state south of Northern
Virginia has not had over one foot of snow in
Virginia is bordered by West Virginia,a single storm since the Blizzard of 1996.
Maryland, and the District of ColumbiaThe interaction of these elements with the
(across the Potomac River) to the north; bystate's topography create micro-climates in
Chesapeake Bay and the Atlantic Ocean to thethe Shenandoah Valley, the mountainous
east; by North Carolina and Tennessee to thesouthwest, and the coastal plains that are
south; and by Kentucky and West Virginia toslightly but noticeably distinct from each
the  west.other.[2] An additional element in recent
years is the expansion of the southern
The Chesapeake Bay divides the commonwealth,suburbs of Washington into Northern Virginia,
with Virginia's Eastern Shore, a part of thecreating an urban heat island due to the
Delmarva Peninsula, completely separate (anincreased energy output of the city. However,
exclave) from the rest of the Commonwealth.aside from the urban stations, no global
Geographically, Virginia is divided into thewarming effects have been noted by Virginia
following  six  regions:weather  stations  by  2001.
Ridge and Valley—between theSevere weather is occasionally a concern in
Appalachian Plateau and Allegheny Plateau toVirginia. As mentioned above, hurricanes make
the west and the Blue Ridge Mountains to thethe coastal area of Virginia somewhat
east. Sometimes referred to as Valley andvulnerable, although it is rare for a major
Ridge.hurricane to threaten the Virginia coast as
hurricanes this far north tend to become
Shenandoah Valley—located within thesomewhat weakened. More often, Virginia is
Ridge and Valley Region; it is referred tostruck with the remnants of systems which hit
geographically—and culturally—further south bringing torrential rain to the
as  its  own  region.state. Thunderstorms are an occasional
concern with the state averaging anywhere
Blue Ridge Mountains—between the Ridgefrom 30-50 days of thunderstorm activity
and Valley Region to the west and theannually, with the highest area of occurrence
Piedmont  region  to  the  east.going towards the west. Conversely, eastern
Virginia has a lower rate of tornadoes, and
Foothills—area now recognized directlythe state averages around 2 tornadoes per
between the Piedmont and the Blue Ridgeyear. The last tornado that Virginia
Mountains. Pertaining to the counties ofexperienced  was  around  November  2006.
Madison, Green, Albemarle, and Nelson.
Denotes a region just west of the CartersFaults  and  quakes
Mountain range and north of the James river
subject  to  its  own  unique  microclimate.Virginia has not had a history of major
seismic activity: earthquakes here are rarely
Piedmont—between the Blue Ridgeabove 4.5 on the Richter magnitude scale.
Mountains to the west and the TidewaterThere is no volcanic activity in the state,
region  to  the  east.and it is located centrally on the North
American Plate—where the Earth's crust
Tidewater—between the fall line to theis thicker than at the edges—which
west and the Atlantic coast to the east; itleads to fewer strong earthquakes. The
includes  the  Eastern  Shore.largest, at 6.0 magnitude, came in 1897 in
Blacksburg.



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