The Appalachian Mountains are a vast mountain range situated in eastern North America, extending roughly from central Alabama to Newfoundland along a generally southwest–northeast axis. Alongside the Appalachian Plateau province—with which they are not entirely synonymous—the mountains form a wider system comprising the region's backbone. The range's highest peak is Mount Mitchell in the Black Mountains subrange of North Carolina, which themselves are part of the larger Blue Ridge Mountains. Saint Pierre and Miquelon, an overseas collectivity of France, is part of the range, meaning it technically spans portions of three countries. It is geologically related to the Scottish Highlands, Atlas Mountains, Scandinavian Mountains, and Ouachitas, as these ranges all originally belonged to the sprawling Central Pangean Mountains before plate tectonics tore them apart.
The geologic processes that led to the formation of the Appalachian Mountains started around 1.1billion years ago with the creation of supercontinent Rodinia, and many Precambrian rocks and minerals created via this process remain visible today in the range's outcrops. The modern Appalachians and their relatives themselves were created by a series of three distinct orogenies beginning approximately 480million years ago, making them one of the oldest surviving mountain ranges in the world. The young Appalachians reached elevations similar to today's Alps and Rockies—both of which are significantly younger mountain ranges—before 240million years of natural erosion by water, wind, ice, and gravity gradually morphed them into the lower, rugged peaks typically seen today.
Considering their extensive length, the Appalachians contain a diverse selection of biomes ranging from the temperate broadleaf and mixed Appalachian-Blue Ridge forest in the south to the boreal Eastern Canadian forest in the north. Conifers like red spruce and balsam fir dominate the north and high elevations, while deciduous trees like sugar maple and beech are more prevalent further south and oak-chestnut forests reign between. The climate ranges from humid subtropical to subarctic, with a few peaks in the Presidential Range of New Hampshire's White Mountains having a true tundra climate; many locations are also oceanic or humid continental. Mammals like black bear, white-tailed deer, squirrels, raccoons, and skunks are common throughout the range, while others like moose are more regionally limited. Birds, fish, shellfish, amphibians like salamanders, and other invertebrates are also abound in the profoundly ecologically diverse region. Once-largely extirpated species like the bobcat and coyote have also made a resurgence in recent years.
The Appalachian Mountains are a barrier to east–west travel, as they form a series of alternating ridgelines and valleys oriented in opposition to most highways and railroads running east–west. This barrier was extremely important in shaping the expansion of the United States in the colonial era. Much of the range's economy was historically based on logging and coal mining, which attracted many migrants who contributed to the genesis of a new cultural region. Though the decline of these industries was an economic detriment, many communities have pivoted to manufacturing and services. Tourism has also become increasingly prevalent: the mountains are home to the very popular Appalachian Trail, a hiking trail that runs from Mount Katahdin in Maine to Springer Mountain in Georgia. The International Appalachian Trail is an extension of this hiking trail into the Canadian portion of the Appalachian range in New Brunswick and Quebec.
Etymology While exploring inland along the northern coast of Florida in 1528, the members of the Narváez expedition, including Álvar Núñez Cabeza de Vaca, found a Native American village near present-day Tallahassee, Florida, the name of which they transcribed as or (). The name was soon altered by the Spanish to Apalachee and used as a name for the tribe and region spreading well inland to the north. Pánfilo de Narváez's expedition first entered Apalachee territory on June 15, 1528, and applied the name. Now spelled "Appalachian", it is the fourth-oldest surviving European place-name in the US.After Florida, Cape Canaveral, and Dry Tortugas:
After the 1540 expedition of Hernando de Soto, Spanish cartographers began to apply the name of the tribe to the mountains themselves. The first cartographic appearance of is on Diego Gutiérrez's map of 1562; the first use for the mountain range is the map of Jacques le Moyne de Morgues in 1565.Walls, David (1978), "On the Naming of Appalachia" In An Appalachian Symposium, pp. 56–76.
The name was not commonly used for the whole mountain range until the late 19th century. A competing and often more popular name was the "Allegheny Mountains", "Alleghenies", and even "Alleghania". In the early 19th century, Washington Irving proposed renaming the United States either Appalachia or Alleghania.Stewart, George R. (1967). Names on the Land. Boston: Houghton Mifflin Company. 173.
In U.S. dialects in most regions of the Appalachians, the word is pronounced , with the third syllable sounding like "latch". In some northern parts of the mountain range, particularly Pennsylvania, it is pronounced or ; the third syllable is like "lay", and the fourth "chins" or "shins".David Walls, "Appalachia". The Encyclopedia of Appalachia (Knoxville, Tenn.: University of Tennessee Press, 2006), 1006–1007. There is often great debate between the residents of the regions regarding the correct pronunciation. Elsewhere, a commonly accepted pronunciation for the adjective Appalachian is , with the last two syllables "-ian" pronounced as in the word "Romanian".Define "Appalachian". Random House Dictionary, online at Dictionary.com. Retrieved May 15, 2011.
Geography Perhaps partly because the range runs through large portions of both the United States and Canada, and partly because the range was formed over numerous geologic time periods, one of which is sometimes termed the Appalachian orogeny, writing communities struggle to agree on an encyclopedic definition of the mountain range. However, each of the governments has an agency that informs the public about the major landforms that make up the countries, the United States Geological Survey (USGS) and the Geological Survey of Canada (GSC). The landforms are referred to as physiographic regions. The regions create precise boundaries from which maps can be drawn. The Appalachian Highlands is the name of one of the eight physiographic regions of the contiguous 48 United States. The Appalachian Uplands is the name of one of seven physiographic regions of Canada.
Appalachian Highlands of the United States
The second level in the physiographic classification schema for the USGS is "province", the same word as Canada uses to divide its political subdivisions, meaning that the terminology used by the two countries do not match below the region level. The lowest level of classification is "section".
Appalachian Uplands of Canada
The Appalachian Uplands are one of the seven physiographic divisions in Canada. Canada's GSC does not use the same classification system as the USGS below the division level. The agency does break the divisions of the Appalachian Uplands into 13 subsections that are in four different political provinces of Canada.
While the Appalachian Highlands and Appalachian Uplands are generally continuous across the U.S./Canadian border, the St. Lawrence Valley area is handled differently in the physiographic classification schemas. The part of the St. Lawrence Valley in the United States is one of the second-level classifications, part of the Appalachian Highlands. In Canada, the area is part of the first-level classification, the St. Lawrence Lowlands. This includes the area around the city of Montreal, Anticosti Island, and the northwest coastline of Newfoundland. The dissected plateau area, while not actually made up of geological mountains, is popularly called "mountains", especially in eastern Kentucky and West Virginia, and while the ridges are not high, the terrain is extremely rugged. In Ohio and New York, some of the plateau has been glaciated, which has rounded off the sharp ridges and filled the valleys to some extent. The glaciated regions are usually referred to as hill country rather than mountains.
Range characteristics
The Appalachian belt includes the plateaus sloping southward to the Atlantic Ocean in New England, and southeastward to the border of the coastal plain through the central and southern Atlantic states; and on the northwest, the Allegheny and Cumberland plateaus declining toward the Great Lakes and the interior plains. A remarkable feature of the belt is the longitudinal chain of broad valleys, including the Great Appalachian Valley, which in the southerly sections divides the mountain system into two unequal portions, but in the northernmost lies west of all the ranges possessing typical Appalachian features, and separates them from the Adirondack group. The mountain system has no axis of dominating altitudes, but in every portion, the summits rise to rather uniform heights, and, especially in the central section, the various ridges and intermontane valleys have the same trend as the system itself. None of the summits reaches the region of perpetual snow.
In Pennsylvania, there are over sixty summits that rise over ; the summits of Mount Davis and Blue Knob rise over . In Maryland, Eagle Rock and Dans Mountain are conspicuous points reaching respectively. On the same side of the Great Valley, south of the Potomac, are the Pinnacle and Pigeon Roost . In West Virginia, more than 150 peaks rise above , including Spruce Knob , the highest point in the Allegheny Mountains. A number of other points in the state rise above . Cheat Mountain (Snowshoe Mountain) at Thorny Flat and Bald Knob are among the more notable peaks in West Virginia.
The Blue Ridge Mountains, rising in southern Pennsylvania and there known as South Mountain, attain elevations of about in Pennsylvania. South Mountain achieves its highest point just below the Mason-Dixon line in Maryland at Quirauk Mountain and then diminishes in height southward to the Potomac River. Once in Virginia, the Blue Ridge again reaches and higher. In the Virginia Blue Ridge, the following are some of the highest peaks north of the Roanoke River: Stony Man , Hawksbill Mountain , Apple Orchard Mountain and Peaks of Otter . South of the Roanoke River, along the Blue Ridge, are Virginia's highest peaks including Whitetop Mountain and Mount Rogers , the highest point in the Commonwealth.