Geography of the United States
 |
| Relief map of the
48 states of the U.S. mainland |
|
Area |
| Total |
3,717,813 sq mi
9.63 Mm² |
| Land |
3,536,294 sq mi
9.16 Mm² |
| Water |
181,519 sq mi
470,131 km² |
| Latitude |
38°0' N |
| Longitude |
97°0'W |
|
Borders |
| Canada |
5,526 miles8.89 Mm |
| Mexico |
2,067 miles3.33 Mm |
| Coastlines |
12,380 miles
1.99 Mm |
|
Maritime claims |
| Contiguous zone |
24 nautical miles
(44 km) |
| Economic zone |
200 nautical miles (370 km) |
| Territorial sea |
12 nautical miles (22 km) |
The
United
States
is a country in the Western
Hemisphere
. It consists of forty-eight contiguous
states on the North American continent; Alaska
, an enormous
peninsula which forms the northwestern
most part of North America, and Hawaii
, an archipelago in the Pacific Ocean
. It also holds several United States territories in the
Pacific and Caribbean
. The term "United States",... when used in
the geographical sense,means the continental United States, Alaska,
Hawaii, Puerto Rico,Guam, and the Virgin Islands of the United
States.
The country shares land borders with Canada
and Mexico
and water
borders with Russia
, the
United
Kingdom
, and The
Bahamas
.
Area
By
total area including water, the United States is either
slightly larger or smaller than the People's
Republic of China
, making it the world's third largest
country. Its rank depends on whether one includes two
territories claimed by India
but governed
by China when calculating China's size. Both China and the
United States follow behind Canada
and Russia
in total
area, and are followed by Brazil
. By
land area (exclusive of waters), the United States is the world's
third largest country, following Russia and China.
In total area
(including inland water), Russia
and Canada
are larger than the United States. Ranking for third-largest
status is disputed.
Some sources (including Encyclopædia Britannica
and all publications of the People's Republic of China
), list China as larger than the U.S. Many
other sources list the U.S. as larger. The dispute appears to
hinge on Taiwan, without
which China takes fourth place. Total U.S. area is 3,718,711 square
miles (9.63 Mm²), of which land is 3,537,438 square miles
(9.16 Mm²) and water is 181,273 square miles
(469,495 km²). Ranked by land area, the top countries in order
are Russia, China, the U.S., Canada and Brazil.
General characteristics
The
United States shares land borders with Canada
(to the
north) and Mexico
(to the
south), and a territorial water
border with Russia
in the
northwest. The contiguous forty-eight states are
otherwise bounded by the Pacific Ocean
on the west, the Atlantic Ocean
on the east, and the Gulf of Mexico
to the southeast. Alaska borders the
Pacific
Ocean
to the south, the Bering Strait
to the west, and the Arctic Ocean
to the north, while Hawaii
lies far to
the southwest of the mainland in the Pacific Ocean.
Forty-eight of the States are in the single region between Canada
and Mexico; this group is referred to, with varying precision and
formality, as the
continental or
contiguous
United States, and as the
Lower
48.
Alaska
, which is
not included in the term contiguous United States, is at
the northwestern end of North America,
separated from the Lower 48 by Canada. The State of Hawaii
is an
archipelago in the Pacific Ocean
. The capital city, Washington,
District of Columbia
, is a federal district located on land donated by
the state of Maryland
. (Virginia
had also donated land, but it was returned in
1847.) The United States also has
overseas territories with varying levels of independence and
organization.
Physiographic divisions
The eastern United States has a varied topography. A broad, flat
coastal plain lines the Atlantic and Gulf shores from the
Texas-Mexico border to New York City, and includes the Florida
peninsula. Areas further inland feature rolling hills and temperate
forests.
The Appalachian Mountains
form a line of low mountains separating the eastern
seaboard from the Great Lakes and the Mississippi Basin.
The five
Great
Lakes
are located in the north-central portion of the
country, four of them forming part of the border with Canada
.
The
southeast United States contain subtropical forests and, near the
gulf coast, mangrove wetlands, especially
in Florida
. West of the Appalachians lies the
Mississippi River basin and two large
eastern tributaries, the
Ohio River and
the
Tennessee River. The
Ohio and
Tennessee Valleys and the
Midwest consist largely of rolling hills and
productive farmland, stretching south to the
Gulf Coast.
The
Great
Plains
lie west of the Mississippi River and east of the
Rocky Mountains. A large portion of the country's
agricultural products are grown in the Great Plains. Before their
general conversion to farmland, the Great Plains were noted for
their extensive grasslands, from
tallgrass prairie in the eastern plains to
shortgrass steppe in the western
High Plains. Elevation
rises gradually from less than a few hundred feet near the
Mississippi River to more than a mile high in the High Plains.
The
generally low relief of the plains is broken in several places,
most notably in the Ozark
and Ouachita
Mountains
, which form the U.S. Interior Highlands, the only major
mountainous region between the Rocky
Mountains and the Appalachian Mountains
.The Great Plains come to an abrupt end at
the
Rocky Mountains.
The Rocky Mountains
form a large portion of the Western
U.S., entering from Canada
and
stretching nearly to Mexico
.
The Rocky
Mountains generally contain fairly mild slopes and low peaks
compared to many of the other great mountain ranges, with a few
exceptions (such as the Teton Mountains
in Wyoming
and the Sawatch Range
in Colorado
). In addition, instead of being one
generally continuous and solid mountain range, it is broken up into
a number of smaller, intermittent mountain ranges, forming a large
series of basins and valleys.
West of the Rocky Mountains lies the
Intermontane Plateaus (also known as
the
Intermountain West), a large,
arid desert lying between the Rockies and the
Cascades and
Sierra Nevada ranges. The large
southern portion, known as the
Great
Basin, consists of salt flats, drainage basins, and many small
north-south mountain ranges. The
Southwest is predominantly a
low-lying desert region. A portion known as the
Colorado Plateau, centered around the
Four Corners region, is considered to
have some of the most spectacular scenery in the world.
It is
accentuated in such national parks as Grand
Canyon
, Arches
, and Bryce Canyon
, among others.
The Intermontane Plateaus come to an end at the
Cascade Range and the
Sierra Nevada. The Cascades consist of
largely intermittent, volcanic mountains rising prominently from
the surrounding landscape. The Sierra Nevada, further south, is a
high, rugged, and dense mountain range.
It contains the
highest point in the contiguous 48 states, Mount Whitney
(14,505 ft; 4,421 m). These areas contain
some spectacular scenery as well, as evidenced by such national
parks as Yosemite
and Mount Rainier
. West of the Cascades and Sierra Nevada is a
series of valleys, such as the Central
Valley
in California
and the Willamette
Valley in Oregon
.
Along the coast is a series of low mountain ranges known as the
Pacific Coast Ranges. Much of
the
Pacific Northwest coast is
inhabited by some of the densest vegetation outside of the
Tropics, and also the tallest trees in the world
(the
Redwoods).
Alaska
contains
some of the most dramatic and untapped scenery in the
country. Tall, prominent mountain ranges rise up sharply
from broad, flat tundra plains. On the islands off the south and
southwest coast are many
volcanoes.
Hawaii
, far to the
south of Alaska
in the
Pacific
Ocean
, is a chain of tropical, volcanic islands, popular
as a tourist destination for many from East
Asia and the mainland United States.
The geography of the United States varies across their immense
area. Within the contential U.S.,
eight distinct
physiographic divisions exist, though each is composed of
several smaller physiographic subdivisions. These major divisions
are:
- Laurentian
Upland - part of the Canadian
Shield that extends into the northern United States Great
Lakes
area.
- Atlantic Plain
- the coastal regions of the eastern and southern
parts includes the continental shelf, the Atlantic Coast and the
Gulf Coast.
- Appalachian Highlands
- lying on the eastern side of the United States,
it includes the Appalachian Mountains
, the Watchung
Mountains, the Adirondacks and
New
England
province originally containing the Great Eastern
Forest.
- Interior
Plains - part of the interior contentintal United States, it
includes much of what is called the Great Plains
.
- Interior
Highlands - also part of the interior contentintal United
States, this division includes the Ozark
Plateau.
- Rocky Mountain
System - one branch of the Cordilleran
system lying far inland in the western
states.
- Intermontane
Plateaus - also divided into the Columbia Plateau
, the Colorado
Plateau and the Basin and
Range Province, it is a system of plateaus, basins, ranges and
gorges between the Rocky and Pacific Mountain Systems.
It is the
setting for the Grand
Canyon
, the Great Basin and
Death
Valley
.
- Pacific Mountain System -
the coastal mountain ranges and features in the west coast of the United
States.
Atlantic coast of the United States is, with minor exceptions, low.
The Appalachian Highland owes its oblique northeast-southwest trend
to crustal deformations which in very early geological time gave a
beginning to what later came to be the Appalachian mountain system.
This system had its climax of deformation so long ago (probably in
Permian time) that it has since then been
very generally reduced to moderate or low relief. It owes its
present day altitude either to renewed elevations along the earlier
lines or to the survival of the most resistant rocks as residual
mountains. The oblique trend of this coast would be even more
pronounced but for a comparatively modern crustal movement, causing
a depression in the northeast resulting in an encroachment of the
sea upon the land. Additionally, the southeastern section has
undergone an elevation resulting in the advance of the land upon
the sea.
The following map, known as a
physiographical map, shows
geographical and
terrain
information about the regions of the contiguous 48 states of the
U.S. used by
earth scientists. The map
indicates the age of the exposed surface as well as the type of
terrain. More information about the regions is covered in several
sub articles found in the additional topics subsection below.
While the Atlantic coast is relatively low, the Pacific coast is,
with few exceptions, hilly or mountainous. This coast has been
defined chiefly by geologically recent crustal deformations, and
hence still preserves a greater relief than that of the
Atlantic.
The low Atlantic coast and the hilly or mountainous Pacific coast
foreshadow the leading features in the distribution of mountains
within the United States. The east coast Appalachian system,
originally forest covered, is relatively low and narrow and is
bordered on the southeast and south by an important coastal plain.
The
Cordilleran
system
on the western side of the continent is lofty,
broad and complicated having two branches, the Rocky Mountain
System and the Pacific Mountain System. In between these,
lie the Intermontaine Plateaus. Heavy forests cover the northwest
coast, but elsewhere trees are found only on the higher ranges
below the Alpine region. The
intermontane valleys, plateaus and basins range
from treeless to desert with the very arid region being in
thesouthwest.
Both the
Columbia River and Colorado
River
rise far inland near the easternmost members of the
Cordilleran system, and flow through plateaus and intermontaine
basins to the ocean.
The
Laurentian Highlands, the Interior Plains and the Interior
Highlands lie between the two coasts, stretching from the Gulf of
Mexico
northward, far beyond the national boundary, to the
Arctic
Ocean
. The central plains are divided by a hardly
perceptible height of land into a Canadian
and a United States portion. It is from the
United States side, that the great
Mississippi system discharges southward to
the Gulf of Mexico. The upper Mississippi and some of the
Ohio basin is the semi-arid prairie region, with
trees originally only along the watercourses. The uplands towards
the Appalachians were included in the great eastern forested area,
while the western part of the plains has so dry a climate that its
native plant life is scanty, and in the south it is practically
barren.
See also:
List of North
American deserts
Elevation extremes:
Climate

Climate zones of the lower 48 United
States.

Average precipitation
Due to its large size and wide range of geographic features, the
United States contains examples of nearly every global climate.
The
climate is temperate in most areas, tropical in Hawaii
and southern
Florida
, polar in Alaska
, semiarid in
the Great
Plains
west of the 100th
meridian, Mediterranean in coastal California
and arid in the Great
Basin. Its comparatively generous climate contributed
(in part) to the country's rise as a world power, with infrequent
severe drought in the major agricultural regions, a general lack of
widespread flooding, and a mainly temperate climate that receives
adequate precipitation.
The main
influence on U.S. weather is the polar jet
stream, which brings in large low pressure systems from the
northern Pacific
Ocean
. The
Cascade
Range,
Sierra Nevada, and
Rocky Mountains pick up most of the
moisture from these systems as they move eastward. Greatly
diminished by the time they reach the
High Plains, much of the
moisture has been sapped by the
orographic
effect as it is forced over several mountain ranges.
However,
once it moves over the Great Plains
, uninterrupted flat land allows it to reorganize
and can lead to major clashes of air masses. In addition, moisture
from the Gulf of
Mexico
is often drawn northward. When combined with
a powerful jet stream, this can lead to violent thunderstorms,
especially during spring and summer.
Sometimes during late
winter and spring these storms can combine with another low
pressure system as they move up the East Coast and into the
Atlantic
Ocean
, where they intensify rapidly. These storms are
known as Nor'easters and often bring widespread, heavy snowfall to
the Mid-Atlantic and New England
. The uninterrupted flat grasslands of the
Great
Plains
also leads to some of the most extreme climate
swings in the world. Temperatures can rise or drop rapidly
and winds can be extreme, and the flow of heat waves or Arctic air
masses often advance uninterrupted through the plains.
The
Great Basin and Columbia
Plateau
(the Intermontane
Plateaus) are arid or semiarid regions that lie in the rain
shadow of the Cascades and
Sierra Nevada.
Precipitation averages less than 15 inches (38 cm). The
Southwest is a hot desert, with
temperatures exceeding 100°F (38°C) for several weeks at a time in
summer.
The Southwest and the Great Basin are also
affected by the monsoon from the Gulf of
California
from July-September, which brings localized but
often severe thunderstorms to the region.
Much of
California
consists of a Mediterranean climate, with sometimes
excessive rainfall from October-April and nearly no rain the rest
of the year. In the
Pacific
Northwest rain falls year-round, but is much heavier during
winter and spring. The mountains of the west receive abundant
precipitation and very heavy snowfall. The Cascades are one of the
snowiest places in the world, with some places averaging over
600 inches (1,520 cm) of snow annually, but the lower
elevations closer to the coast receive very little snow.
Another
significant (but localized) weather effect is lake-effect snow that falls south and east
of the Great
Lakes
, especially in the hilly portions of the Upper
Peninsula
of
Michigan
and on the Tug Hill
Plateau in New
York
.The lake effect dumped well over 5 feet of snow in
the Buffalo, New York area throughout the 2006-2007 winter The
Wasatch Front and Wasatch Range in Utah
can also
receive significant lake effect accumulations off of the Great Salt
Lake
.
Extremes
In northern Alaska,
tundra and
arctic conditions predominate, and the temperature
has fallen as low as minus -80 °
F
(−62 °
C).
On the other end of
the spectrum, Death Valley, California
once reached 134 °F (56.7 °C), the
second-highest temperature ever recorded on Earth.
On average, the mountains of the western states receive the highest
levels of snowfall on Earth.
The greatest annual snowfall level is at
Mount
Rainier
in Washington
, at 692 inches (17,580 mm); the record
there was 1,122 inches (28,500 mm) in the winter of
1971–72. This record was broken by the Mt. Baker Ski Area in
northwestern Washington which reported 1,140 inches of
snowfall for the 1998-99 snowfall season.
Other places with
significant snowfall outside the Cascade Range are the Wasatch Mountains, near the Great Salt
Lake
, and the Sierra
Nevada, near Lake
Tahoe
. In the east, while snowfall does not
approach western levels, the region near the Great Lakes and the
mountains of the Northeast receive the most. Along the northwestern
Pacific coast, rainfall is greater than anywhere else in the
continental U.S., with
Quinault
Ranger in Washington having an average of 137 inches
(3480 mm).
Hawaii receives even more, with
460 inches (11,680 mm) measured annually on Mount
Waialeale
, in
Kauai
. The
Mojave
Desert, in the southwest, is home to the driest locale in the
U.S.
Yuma, Arizona
, has an average of 2.63 inches (66.8 mm)
of precipitation each
year.
In central portions of the U.S.,
tornadoes
are more common than anywhere else on Earth and touch down most
commonly in the spring and summer. Deadly and destructive
hurricanes occur almost every year along the
Atlantic seaboard and the Gulf of Mexico. The Appalachian region
and the Midwest experience the worst floods, though virtually no
area in the U.S. is immune to flooding. The Southwest has the worst
droughts; one is thought to have lasted over 500 years and to have
decimated the
Anasazi people. The West is
affected by large wildfires each year.
Natural disasters
The United States is affected by a large variety of natural
disasters yearly. Although severe drought is rare, it has
occasionally caused major problems, such as during the
Dust Bowl (1931-1942), which coincided with the
Great Depression. Farmland failed
throughout the Plains, entire regions were virtually depopulated,
and dust storms ravaged the land.
More recently, the western U.S.
experienced widespread drought from 1999-2004, and signs of a
major, long-term drought across the Great Plains
have developed.[5657] In the past year, drought has spread
from the Southern Plains westward through the Southwest and east
along the Gulf Coast to Florida.

A powerful tornado near Dimmitt, Texas
on June 2, 1995
The United States also experience, by a large margin, the most
frequent and powerful
tornadoes in the
world. The Great Plains and Midwest, due to the contrasting air
masses, sees frequent severe thunderstorms and tornado outbreaks
during spring and summer.
The strip of land from north Texas
north to
Kansas
and east
into Tennessee
is known as Tornado
Alley, where many houses have tornado shelters and many towns
have tornado sirens. Another natural disaster that frequents the
country are hurricanes, which can hit
anywhere along the Gulf Coast or the
Atlantic Coast as well as Hawaii
in the
Pacific
Ocean
. Particularly at risk are the central and
southern Texas
coasts,
the area from southeastern Louisiana
east to the Florida
Panhandle, the east coast of Florida
, and the Outer Banks
of North
Carolina
, although
any portion of the coast could be struck. Hurricane season
runs from June 1 to November 30, with a peak from mid-August
through early October.
Some of the more devastating hurricanes have
included the Galveston Hurricane of 1900
, Hurricane
Andrew in 1992, and Hurricane
Katrina in 2005. The remnants of tropical cyclones from
the Eastern Pacific also occasionally impact the southwestern
United States, bringing sometimes heavy rainfall.
Like drought, widespread severe flooding is rare. Some exceptions
include the
Great
Mississippi Flood of 1927, the
Great Flood of 1993, and widespread
flooding and mudslides caused by the 1982-1983
El
Niño event in the western United States. Localized flooding
can, however, occur anywhere, and mudslides from heavy rain can
cause problems in any mountainous area, particularly the Southwest.
Large stretches of desert shrub in the west can fuel the spread of
wildfires. The narrow canyons of many
mountain areas in the west and severe thunderstorm activity during
the
monsoon season in summer leads to
sometimes devastating
flash floods as
well, while Nor'Easter snowstorms can bring activity to a halt
throughout the Northeast (although heavy snowstorms can occur
almost anywhere).
The West
Coast of the continental United States and areas of Alaska
(including the Aleutian
Islands
, the Alaskan Peninsula
and southern Alaskan coast) make up part of the
Pacific Ring of Fire, an area
of heavy tectonic and volcanic activity that is the source of 90%
of the world's earthquakes. The American Northwest sees the highest
concentration of active volcanoes in the United States, in Washington
, Oregon
and
northern California along the
Cascade Mountains.
There are
several active volcanoes located in the islands of Hawaii
, including
Kilauea in ongoing eruption since 1983, but they do not typically
adversely affect the inhabitants of the islands. There has
not been a major life-threatening eruption on the Hawaiian islands
since the 17th century.
Volcanic eruptions can occasionally be
devastating, such as in the 1980
eruption of Mount St. Helens
in Washington.
The Ring
of Fire makes California
and southern Alaska
particularly
vulnerable to earthquakes.
Earthquakes can cause extensive damage, such
as the 1906 San Francisco
Earthquake or the 1964 Good
Friday Earthquake near Anchorage, Alaska
. California is well known for seismic
activity, and requires large structures to be
earthquake resistant to minimize loss
of life and property. Outside of devastating earthquakes,
California experiences minor earthquakes on a regular basis.
Other
natural disasters include: tsunamis around Pacific Basin, mud
slides in California
, and forest fires in the west. your
Public lands
The United States holds many areas for the use and enjoyment of the
public. These include
National Parks,
National Monuments,
National Forests,
Wilderness areas, and other areas.
For lists of areas, see the following articles:
See also
References
- Yahoo's chart of countries by land area based on the CIA World
Factbook
http://education.yahoo.com/reference/factbook/countrycompare/area/3d.html;_ylt=As1XMsN8kgSx746VWazy_s7PecYF
- Williams, Jack Each
state's low temperature record, USA today, URL
accessed 13 June, 2006.
- National Atlas, Average Annual Precipitation, 1961-1990, URL
accessed 15 June 2006.
- Hereford, Richard, et al., Precipitation
History of the Mojave Desert Region, 1893–2001, U.S.
Geological Survey, Fact Sheet 117-03, URL accessed 13 June
2006.
- NOVA, Tornado Heaven, Hunt for the Supertwister,
URL accessed 15 June 2006.
- O'Connor, Jim E. and John E. Costa, Large
Floods in the United States: Where Thley Happen and Why,
U.S. Geological Survey Circular 1245, URL accessed 13
June 2006.
Further reading
- Brown, Ralph Hall, Historical Geography of the United
States, New York : Harcourt, Brace, 1948
- Stein, Mark, How the States Got Their Shapes, New York
: Smithsonian Books/Collins, 2008. ISBN 9780061431388
External links