The Full Wiki

Geography of the United States: Map

  
  
  

Wikipedia article:

Map showing all locations mentioned on Wikipedia article:



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 Statesmarker is a country in the Western Hemispheremarker. It consists of forty-eight contiguous states on the North American continent; Alaskamarker, an enormous peninsula which forms the northwestern most part of North America, and Hawaiimarker, an archipelago in the Pacific Oceanmarker. It also holds several United States territories in the Pacific and Caribbeanmarker. 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 Canadamarker and Mexicomarker and water borders with Russiamarker, the United Kingdommarker, and The Bahamasmarker.

Area

By total area including water, the United States is either slightly larger or smaller than the People's Republic of Chinamarker, making it the world's third largest country. Its rank depends on whether one includes two territories claimed by Indiamarker but governed by China when calculating China's size. Both China and the United States follow behind Canadamarker and Russiamarker in total area, and are followed by Brazilmarker. 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), Russiamarker 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 Chinamarker), 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 Canadamarker (to the north) and Mexicomarker (to the south), and a territorial water border with Russiamarker in the northwest. The contiguous forty-eight states are otherwise bounded by the Pacific Oceanmarker on the west, the Atlantic Oceanmarker on the east, and the Gulf of Mexicomarker to the southeast. Alaska borders the Pacific Oceanmarker to the south, the Bering Straitmarker to the west, and the Arctic Oceanmarker to the north, while Hawaiimarker 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. Alaskamarker, 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 Hawaiimarker is an archipelago in the Pacific Oceanmarker. The capital city, Washington, District of Columbiamarker, is a federal district located on land donated by the state of Marylandmarker. (Virginiamarker 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 Mountainsmarker form a line of low mountains separating the eastern seaboard from the Great Lakes and the Mississippi Basin. The five Great Lakesmarker are located in the north-central portion of the country, four of them forming part of the border with Canadamarker. The southeast United States contain subtropical forests and, near the gulf coast, mangrove wetlands, especially in Floridamarker. 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 Plainsmarker 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 Ozarkmarker and Ouachita Mountainsmarker, which form the U.S. Interior Highlands, the only major mountainous region between the Rocky Mountains and the Appalachian Mountainsmarker.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 Canadamarker and stretching nearly to Mexicomarker. 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 Mountainsmarker in Wyomingmarker and the Sawatch Range in Coloradomarker). 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 Canyonmarker, Archesmarker, and Bryce Canyonmarker, 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 Whitneymarker (14,505 ft; 4,421 m). These areas contain some spectacular scenery as well, as evidenced by such national parks as Yosemitemarker and Mount Rainiermarker. West of the Cascades and Sierra Nevada is a series of valleys, such as the Central Valleymarker in Californiamarker and the Willamette Valley in Oregonmarker. 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).

Alaskamarker 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. Hawaiimarker, far to the south of Alaskamarker in the Pacific Oceanmarker, 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:



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 systemmarker 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 Rivermarker 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 Mexicomarker northward, far beyond the national boundary, to the Arctic Oceanmarker. The central plains are divided by a hardly perceptible height of land into a Canadianmarker 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 Hawaiimarker and southern Floridamarker, polar in Alaskamarker, semiarid in the Great Plainsmarker west of the 100th meridian, Mediterranean in coastal Californiamarker 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 Oceanmarker. 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 Plainsmarker, uninterrupted flat land allows it to reorganize and can lead to major clashes of air masses. In addition, moisture from the Gulf of Mexicomarker 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 Oceanmarker, where they intensify rapidly. These storms are known as Nor'easters and often bring widespread, heavy snowfall to the Mid-Atlantic and New Englandmarker. The uninterrupted flat grasslands of the Great Plainsmarker 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 Plateaumarker (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 Californiamarker from July-September, which brings localized but often severe thunderstorms to the region.

Much of Californiamarker 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 Lakesmarker, especially in the hilly portions of the Upper Peninsulamarker of Michiganmarker and on the Tug Hill Plateau in New Yorkmarker.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 Utahmarker can also receive significant lake effect accumulations off of the Great Salt Lakemarker.

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, Californiamarker 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 Rainiermarker in Washingtonmarker, 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 Lakemarker, and the Sierra Nevada, near Lake Tahoemarker. 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 Waialealemarker, in Kauaimarker. The Mojave Desert, in the southwest, is home to the driest locale in the U.S. Yuma, Arizonamarker, 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 Plainsmarker 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 Texasmarker north to Kansasmarker and east into Tennesseemarker 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 Hawaiimarker in the Pacific Oceanmarker. Particularly at risk are the central and southern Texasmarker coasts, the area from southeastern Louisianamarker east to the Florida Panhandle, the east coast of Floridamarker, and the Outer Banksmarker of North Carolinamarker, 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 1900marker, 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 Islandsmarker, the Alaskan Peninsulamarker 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 Washingtonmarker, Oregonmarker and northern California along the Cascade Mountains. There are several active volcanoes located in the islands of Hawaiimarker, 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. Helensmarker in Washington.

The Ring of Fire makes Californiamarker and southern Alaskamarker particularly vulnerable to earthquakes. Earthquakes can cause extensive damage, such as the 1906 San Francisco Earthquake or the 1964 Good Friday Earthquake near Anchorage, Alaskamarker. 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 Californiamarker, 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

  1. 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
  2. Williams, Jack Each state's low temperature record, USA today, URL accessed 13 June, 2006.
  3. National Atlas, Average Annual Precipitation, 1961-1990, URL accessed 15 June 2006.
  4. 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.
  5. NOVA, Tornado Heaven, Hunt for the Supertwister, URL accessed 15 June 2006.
  6. 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





Embed code:






Got something to say? Make a comment.
Your name
Your email address
Message