Mountains And Mountain Ranges Codexery

Appalachian Mountains

Ancient mountain range spanning eastern North America.

Appalachian Mountains

The Appalachian Mountains stretch about 2,050 miles (3,300 kilometers) across eastern North America, running from central Alabama northeast to Newfoundland. They form the region’s backbone, though they are not exactly the same as the Appalachian Plateau province, which is part of a larger system. The highest point is Mount Mitchell, which rises 6,684 feet (2,037 meters) in North Carolina’s Black Mountains, a subrange of the Blue Ridge Mountains. The range also includes Saint Pierre and Miquelon, a French overseas collectivity, so it technically crosses three countries. Geologically, the Appalachians are linked to the Scottish Highlands, Atlas Mountains, Scandinavian Mountains, and Ouachitas—all once part of the ancient Central Pangean Mountains before plate tectonics split them apart.

The mountains’ formation began about 1.1 billion years ago with the creation of the supercontinent Rodinia, and Precambrian rocks and minerals from that time still appear in outcrops today. The modern Appalachians and their relatives took shape through three distinct orogenies starting around 480 million years ago, making them one of the world’s oldest surviving mountain ranges. In their youth, they reached heights similar to today’s Alps and Rockies, which are much younger. Over 240 million years, erosion from water, wind, ice, and gravity wore them down into the lower, rugged peaks seen now.

Given their great length, the Appalachians host a wide range of biomes. Southern areas feature temperate broadleaf and mixed Appalachian-Blue Ridge forests, while northern parts have boreal Eastern Canadian forests. Conifers like red spruce and balsam fir dominate the north and high elevations; farther south, deciduous trees such as sugar maple and beech are common, with oak-chestnut forests in between. Climate varies from humid subtropical to subarctic, and a few peaks in New Hampshire’s Presidential Range (White Mountains) have true tundra climates; many locations are oceanic or humid continental. Common mammals include black bear, white-tailed deer, squirrels, raccoons, and skunks, while moose are more regionally limited. Birds, fish, shellfish, amphibians like salamanders, and other invertebrates thrive in this ecologically diverse region. Species like bobcat and coyote, once largely extirpated, have rebounded in recent years.

The Appalachians act as a barrier to east–west travel, with alternating ridgelines and valleys running opposite to most east–west highways and railroads. This obstacle heavily shaped U.S. colonial expansion. Historically, the range’s economy relied on logging and coal mining, drawing many migrants who helped create a distinct cultural region. As those industries declined, many communities shifted to manufacturing and services. Tourism has grown, especially around the Appalachian Trail, a 2,175-mile (3,500 km) hiking path from Mount Katahdin in Maine to Springer Mountain in Georgia. The International Appalachian Trail extends this route into the Canadian portion of the range in New Brunswick and Quebec.

**Etymology** In 1528, while exploring inland along Florida’s northern coast, members of the Narváez expedition—including Álvar Núñez Cabeza de Vaca—found a Native American village near present-day Tallahassee, Florida. They transcribed its name as *Apalchen* or *Apalachen* (pronounced [a.paˈla.tʃɛn] in Apalachee). The Spanish soon altered it to *Apalachee* and used it for the tribe and the surrounding region, which spread inland to the north. Pánfilo de Narváez’s expedition entered Apalachee territory on June 15, 1528, applying the name. Now spelled “Appalachian,” it is the fourth-oldest surviving European place-name in the United States. After Hernando de Soto’s 1540 expedition, Spanish cartographers began applying the tribe’s name to the mountains. The first cartographic appearance of *Apalchen* is on Diego Gutiérrez’s 1562 map; the first use for the mountain range itself appears on Jacques le Moyne de Morgues’s 1565 map. The name wasn’t commonly used for the entire range until the late 19th century. A competing name, often more popular, was “Allegheny Mountains,” “Alleghenies,” or “Alleghania.” In the early 19th century, Washington Irving proposed renaming the United States either Appalachia or Alleghania. In most U.S. dialects across the Appalachians, the word is pronounced with the third syllable sounding like “latch.” In some northern parts, especially Pennsylvania, it is pronounced with the third syllable like “lay” and the fourth like “chins” or “shins.” Residents often debate the correct pronunciation. Elsewhere, a common pronunciation for the adjective “Appalachian” has the last two syllables (“-ian”) pronounced like in “Romanian.”

**Geography** Because the range runs through large portions of both the United States and Canada, and because it formed over numerous geologic periods—one of which is sometimes called the Appalachian orogeny—writing communities struggle to agree on an encyclopedic definition of the mountain range. However, each government has an agency that informs the public about the major landforms that make up the country.

Length
2,050 mi (3,300 km)
Highest peak
Mount Mitchell, 6,684 ft (2,037 m)
Countries spanned
United States, Canada, France (Saint Pierre and Miquelon)
Oldest rocks
Precambrian, dating to ~1.1 billion years ago
Major orogenies
Three, starting ~480 million years ago
Notable trail
Appalachian Trail, 2,175 mi (3,500 km)

Lore & Background

The name 'Appalachian' originates from a Native American village near present-day Tallahassee, Florida, encountered by the Narváez expedition in 1528. The name was transcribed as Apalchen or Apalachen and soon altered by the Spanish to Apalachee, used for the tribe and region spreading inland. After Hernando de Soto's 1540 expedition, Spanish cartographers began applying the name to the mountains. The first cartographic appearance of Apalchen is on Diego Gutiérrez's map of 1562; the first use for the mountain range is on Jacques le Moyne de Morgues's map of 1565. The name was not commonly used for the whole range until the late 19th century; a competing name was the 'Allegheny Mountains' or 'Alleghenies'. In the early 19th century, Washington Irving proposed renaming the United States either Appalachia or Alleghania.

Reader's Guide

The Appalachian Mountains are a barrier to east–west travel, forming 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 2,175-mile (3,500 km) hiking trail that runs from Mount Katahdin in Maine to Springer Mountain in Georgia. The International Appalachian Trail is an extension into the Canadian portion of the range in New Brunswick and Quebec. The range is ecologically diverse, containing biomes from temperate broadleaf and mixed Appalachian-Blue Ridge forest in the south to boreal Eastern Canadian forest in the north. 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. Geologically, the Appalachians are related to the Scottish Highlands, Atlas Mountains, Scandinavian Mountains, and Ouachitas, as these ranges all originally belonged to the Central Pangean Mountains.

Did You Know?

Deep-Time Origins and the Long Erosion

The geologic processes that led to the formation of the Appalachian Mountains started around 1.1 billion 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 were created by a series of three distinct orogenies beginning approximately 480 million 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 240 million years of natural erosion by water, wind, ice, and gravity gradually morphed them into the lower, rugged peaks typically seen today. The range 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.

A Living Tapestry of Biomes and Wildlife

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.

Shaping a Nation and Forging a Culture

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 2,175-mile (3,500 km) 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.

A Name Born from First Contact

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 Apalchen or Apalachen. 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. 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 Apalchen 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. 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.

Frequently Asked Questions

What are the Appalachian Mountains?

The Appalachian Mountains are a major mountain system running through eastern North America, stretching from central Alabama to Newfoundland along a southwest-to-northeast axis. They are considered one of the oldest surviving mountain ranges on the planet.

How long are the Appalachian Mountains?

The range spans approximately 2,050 miles (3,300 km) in total length. This makes it one of the longest continuous mountain systems in North America.

What is the highest peak in the Appalachian Mountains?

Mount Mitchell, situated in the Black Mountains subrange of North Carolina within the broader Blue Ridge system, tops out at 6,684 feet (2,037 m) as the range's tallest summit.

How old are the Appalachian Mountains?

The range was built up through three major orogenies that began roughly 480 million years ago, making it among the oldest mountain systems still standing. Some of its oldest rock formations are Precambrian in origin, dating back around 1.1 billion years.

Which countries do the Appalachian Mountains span?

The range crosses through the United States and Canada, with a small extension reaching France's territory of Saint Pierre and Miquelon. It is most commonly associated with the eastern United States.

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