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140-666: The Appalachian Mountains , often called the Appalachians , are a mountain range in eastern to northeastern North America . The term "Appalachian" refers to several different regions associated with the mountain range, and its surrounding terrain. The general definition used is one followed by the United States Geological Survey and the Geological Survey of Canada to describe the respective countries' physiographic regions. The U.S. uses

280-463: A chevron pattern made in Venice for a limited period of time and believed to be indicative of the de Soto expedition. Six metal objects were also found, including a silver pendant and some iron tools. The rarest items were found within what researchers believe was a large council house of the indigenous people whom de Soto was visiting. The expedition continued to present-day South Carolina . There

420-805: A chapel be erected within the Church of San Miguel in Jerez de Los Caballeros, Spain, where De Soto grew up, at a cost of 2,000 ducats, with an altarpiece featuring the Virgin Mary, Our Lady of the Conception , that his tomb be covered in a fine black broadcloth topped by a red cross of the Order of the Knights of Santiago , and on special occasions a pall of black velvet with the De Soto coat of arms be placed on

560-675: A child at each place, De Soto stipulated in his will that his body be interred at Jerez de los Caballeros, where other members of his family were buried. A few years before his birth, the Kingdoms of Castille and Aragon conquered the last Islamic kingdom of the Iberian Peninsula . Spain and Portugal were filled with young men seeking a chance for military fame after the defeat of the Moors . With Christopher Columbus 's discovery of new lands (which he thought to be East Asia ) across

700-591: A consensus (although not total) to end the expedition and try to find a way home, either down the Mississippi River, or overland across Texas to the Spanish colony of Mexico City . They decided that building boats would be too difficult and time-consuming and that navigating the Gulf of Mexico was too risky, so they headed overland to the southwest. Eventually, they reached a region in present-day Texas that

840-452: A fever on 21 May 1542, in the native village of Guachoya . Historical sources disagree as to whether de Soto died near present-day Lake Village, Arkansas McArthur, Arkansas , or Ferriday, Louisiana . Louisiana erected a historical marker at the estimated site on the western bank of the Mississippi River. Before his death, de Soto chose Luis de Moscoso Alvarado , his former maestro de campo (or field commander), to assume command of

980-409: A fortified city in southern Alabama, to receive the women. De Soto gave the chief a pair of boots and a red cloak to reward him for his cooperation. The Mobilian tribe, under chief Tuskaloosa, ambushed de Soto's army. Other sources suggest de Soto's men were attacked after attempting to force their way into a cabin occupied by Tuskaloosa. The Spaniards fought their way out, and retaliated by burning

1120-471: A fragile ecosystem known as the Southern Appalachian spruce–fir forest . Fraser fir rarely occurs below 5,500 ft (1,700 m), and becomes the dominant tree type at 6,200 ft (1,900 m). By contrast, balsam fir is found from near sea level to the tree line in the northern Appalachians, but ranges only as far south as Virginia and West Virginia in the central Appalachians, where it

1260-734: A great thickness of sediment accumulated. Eventually, the tectonic forces pulling the two continents apart became so strong that an ocean formed off the eastern coast of the Laurentian margin. This was called the Iapetus Ocean and was the precursor of the modern Atlantic Ocean. The rocks of the Valley and Ridge province formed over millions of years, in the Iapetus. Shells and other hard parts of ancient marine plants and animals accumulated to form limey deposits that later became limestone. This

1400-565: A month resting the horses while his men searched for gold. De Soto next entered eastern Tennessee . At this point, de Soto either continued along the Tennessee River to enter Alabama from the north (according to John R. Swanton ), or turned south and entered northern Georgia (according to Charles M. Hudson ). Swanton's final report, published by the Smithsonian, remains an important resource  but Hudson's reconstruction of

1540-501: 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 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

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1680-672: A new ocean opened up, the Rheic Ocean , during the Middle to Late Devonian, and subsequently its closure would result in the formation of the Alleghanian orogeny . As the continental plates moved closer together, fragments of oceanic crust, islands, and other continental masses collided with the eastern margin of ancestral North America. By this time, plants had appeared on land, followed by scorpions, insects, and amphibians. The ocean continued to shrink until, about 270 million years ago,

1820-504: A number of deciduous rhododendrons (azaleas), and smaller heaths such as teaberry ( Gaultheria procumbens ) and trailing arbutus ( Epigaea repens ). The evergreen great rhododendron ( Rhododendron maximum ) is characteristic of moist stream valleys. These occurrences are in line with the prevailing acidic character of most oak forest soils. In contrast, the much rarer chinquapin oak ( Quercus muehlenbergii ) demands alkaline soils and generally grows where limestone rock

1960-444: A number of serious insect and disease outbreaks. Among the most conspicuous is that of the introduced spongy moth ( Lymantria dispar ), which infests primarily oaks, causing severe defoliation and tree mortality. But it also has the benefit of eliminating weak individuals, and thus improving the genetic stock, as well as creating rich habitat of a type through accumulation of dead wood. Because hardwoods sprout so readily, this moth

2100-768: A passage between the Atlantic Ocean and the Pacific Ocean to enable trade with the Orient, the richest market in the world. Failing that, and without means to explore further, de Soto, upon Pedro Arias Dávila 's death, left his estates in Nicaragua. Bringing his own men on ships which he hired, de Soto joined Francisco Pizarro at his first base of Tumbes shortly before departure for the interior of present-day Peru . Pizarro quickly made de Soto one of his captains. When Pizarro and his men first encountered

2240-401: A pitched battle with Inca troops in front of the city, but the battle had ended before Pizarro arrived with the rest of the Spanish party. The Inca army withdrew during the night. The Spanish plundered Cuzco, where they found much gold and silver. As a mounted soldier, de Soto received a share of the plunder, which made him very wealthy. It represented riches from Atahualpa's camp, his ransom, and

2380-452: A public office in León, Nicaragua . Brave leadership, unwavering loyalty, and ruthless schemes for the extortion of native villages for their captured chiefs became de Soto's hallmarks during the conquest of Central America . He gained fame as an excellent horseman, fighter, and tactician. During that time, de Soto was influenced by the achievements of Iberian explorers: Juan Ponce de León ,

2520-544: A variety of oaks ( Quercus spp.), hickories ( Carya spp.) and, in the past, by the American chestnut ( Castanea dentata ). The American chestnut was virtually eliminated as a canopy species by the introduced fungal chestnut blight ( Cryphonectaria parasitica ), but lives on as sapling-sized sprouts that originate from roots, which are not killed by the fungus. In present-day forest canopies, chestnut has been largely replaced by oaks. The oak forests of

2660-641: A variety of other destructive activities continue, albeit in diminished forms; and thus far only a few ecologically based management practices have taken hold. Appalachian bogs are boreal ecosystems , which occur in many places in the Appalachians, particularly the Allegheny and Blue Ridge subranges. Though popularly called bogs , many of them are technically fens . Mountain range Mountain ranges are usually segmented by highlands or mountain passes and valleys . Individual mountains within

2800-483: Is a boreal species that forms a few high elevation outliers as far south as West Virginia. All of these species except white pine tend to occupy sandy, rocky, poor soil sites, which are mostly acidic in character. White pine, a large species valued for its timber, tends to do best in rich, moist soil, either acidic or alkaline in character. Pitch pine is also at home in acidic, boggy soil, and Table Mountain pine may occasionally be found in this habitat as well. Shortleaf pine

2940-538: Is at work while the mountains are being uplifted until the mountains are reduced to low hills and plains. The early Cenozoic uplift of the Rocky Mountains of Colorado provides an example. As the uplift was occurring some 10,000 feet (3,000 m) of mostly Mesozoic sedimentary strata were removed by erosion over the core of the mountain range and spread as sand and clays across the Great Plains to

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3080-455: Is disputed only in minor details. His route beyond Mabila is contested. Swanton reported the de Soto trail ran from there through Mississippi , Arkansas , and Texas . Historians have more recently considered archeological reconstructions and the oral history of the various Native American peoples who recount the expedition. Most historical places have been overbuilt and much evidence has been lost. More than 450 years have passed between

3220-403: Is found at high elevations in the northern Appalachians, and in bogs as far south as Pennsylvania. The Appalachians are also home to two species of fir, the boreal balsam fir ( Abies balsamea ), and the southern high elevation endemic, Fraser fir ( Abies fraseri ). Fraser fir is endemic to the highest parts of the southern Appalachian Mountains, where along with red spruce it forms

3360-533: Is generally found in warmer habitats and at lower elevations than the other species. All the species listed do best in open or lightly shaded habitats, although white pine also thrives in shady coves, valleys, and on floodplains. The Appalachians are characterized by a wealth of large, beautiful deciduous broadleaf (hardwood) trees. Their occurrences are best summarized and described in E. Lucy Braun 's 1950 classic, Deciduous Forests of Eastern North America (Macmillan, New York). The most diverse and richest forests are

3500-414: Is near the surface. Hence no ericaceous shrubs are associated with it. The Appalachian flora also include a diverse assemblage of bryophytes (mosses and liverworts), as well as fungi . Some species are rare and/or endemic. As with vascular plants , these tend to be closely related to the character of the soils and the thermal environment in which they are found. Eastern deciduous forests are subject to

3640-525: Is not as harmful as the hemlock woolly adelgid . Perhaps more serious is the introduced beech bark disease complex, which includes both a scale insect ( Cryptococcus fagisuga ) and fungal components. During the 19th and early 20th centuries, the Appalachian forests were subject to severe and destructive logging and land clearing, which resulted in the designation of the national forests and parks as well many state-protected areas. However, these and

3780-497: Is not known. According to one source, de Soto's men hid his corpse in blankets weighted with sand and sank it in the middle of the Mississippi River during the night. De Soto's expedition had explored La Florida for three years without finding the expected treasures or a hospitable site for colonization. They had lost nearly half their men, and most of the horses. By this time, the soldiers were wearing animal skins for clothing. Many were injured and in poor health. The leaders came to

3920-476: Is now the southern United States, the Ococee Basin was formed. Seawater filled the basin. Rivers from the surrounding countryside carried clay, silt, sand, and gravel to the basin, much as rivers today carry sediment from the midcontinent region to the Gulf of Mexico. The sediment spread out in layers on the basin floor. The basin continued to subside, and over a long period of time, probably millions of years,

4060-530: 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. In U.S. dialects in

4200-550: Is possible that the cratons of Kalahari , and Rio Plato , were also part of that early collision since they were present as Rodinia broke up). Mountain-building referred to as the Grenville Orogeny occurred along the boundaries of the cratons. The present Appalachian Mountains have at least two areas which are made from rock formations that were formed during this orogeny - the Blue Ridge Mountains and

4340-506: 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

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4480-645: Is subject to the hemlock woolly adelgid ( Adelges tsugae ), an introduced insect, that is rapidly extirpating it as a forest tree. Less abundant, and restricted to the southern Appalachians, is Carolina hemlock ( Tsuga caroliniana ). Like Canada hemlock, this tree suffers severely from the hemlock woolly adelgid. Several species of pines characteristic of the Appalachians are eastern white pine ( Pinus strobus ), Virginia pine ( Pinus virginiana ), pitch pine ( Pinus rigida ), Table Mountain pine ( Pinus pungens ) and shortleaf pine ( Pinus echinata ). Red pine ( Pinus resinosa )

4620-531: Is the first European documented as having crossed the Mississippi River . De Soto's North American expedition was a vast undertaking. It ranged throughout what is now the southeastern United States , searching both for gold, which had been reported by various Native American tribes and earlier coastal explorers, and for a passage to China or the Pacific coast. De Soto died in 1542 on the banks of

4760-458: 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. 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

4900-505: Is the same process by which limestone forms in modern oceans. The weathering of limestone, now exposed at the land surface, produces the lime-rich soils that are so prevalent in the fertile farmland of the Valley and Ridge province. During this continental break-up, around 600 million to 560 million years ago, volcanic activity was present along the tectonic margins. There is evidence of this activity in today's Blue Ridge Mountains. Mount Rogers , Whitetop Mountain , and Pine Mountain are all

5040-464: Is usually confined above 3,900 ft (1,200 m) asl, except in cold valleys. Curiously, it is associated with oaks in Virginia. The balsam fir of Virginia and West Virginia is thought by some to be a natural hybrid between the more northern variety and Fraser fir. While red spruce is common in both upland and bog habitats, balsam fir, as well as black spruce and tamarack, are more characteristic of

5180-628: The Adirondacks . After the Grenville orogeny, the direction of the continental drift reversed, and the single supercontinent Rodinia began to break up. The mountains formed during the Grenvillian era underwent erosion due to weathering, glaciation, and other natural processes, resulting in the leveling of the landscape. The eroded sediments from these mountains contributed to the formation of sedimentary basins and valleys. For example, in what

5320-865: The Alpide belt . The Pacific Ring of Fire includes the Andes of South America, extends through the North American Cordillera , the Aleutian Range , on through Kamchatka Peninsula , Japan , Taiwan , the Philippines , Papua New Guinea , to New Zealand . The Andes is 7,000 kilometres (4,350 mi) long and is often considered the world's longest mountain system. The Alpide belt stretches 15,000 km across southern Eurasia , from Java in Maritime Southeast Asia to

5460-517: The Alps and the Rockies before natural erosion occurred over the last 240 million years leading to what is present today. 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

5600-551: The Annamite Range . If the definition of a mountain range is stretched to include underwater mountains, then the Ocean Ridge forms the longest continuous mountain system on Earth, with a length of 65,000 kilometres (40,400 mi). The position of mountain ranges influences climate, such as rain or snow. When air masses move up and over mountains, the air cools, producing orographic precipitation (rain or snow). As

5740-643: The Caddo River , where they clashed with a Native American tribe called the Tula in October 1541. The Spaniards characterized them as the most skilled and dangerous warriors they had encountered. This may have happened in the area of present-day Caddo Gap, Arkansas (a monument to the de Soto expedition was erected in that community). Eventually, the Spaniards returned to the Mississippi River. De Soto died of

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5880-594: The Coal Region of northeastern Pennsylvania . The bituminous coal fields of western Pennsylvania , western Maryland , southeastern Ohio, eastern Kentucky, southwestern Virginia , and West Virginia contain the sedimentary form of coal. The mountain top removal method of coal mining , in which entire mountain tops are removed, is currently threatening vast areas and ecosystems of the Appalachian Mountain region. The surface coal mining that started in

6020-518: The Gulf of Mexico to meet two ships bearing fresh supplies from Havana . De Soto demanded women and servants, and when Tuskaloosa refused, the European explorers took him hostage. The expedition began making plans to leave the next day, and Tuskaloosa gave in to de Soto's demands, providing bearers for the Spaniards. He informed de Soto that they would have to go to his town of Mabila (or Mauvila ),

6160-707: The Gulf of Mexico . In the central section, north of the New River, the rivers, rising in or just beyond the Valley Ridges, flow through great gorges to the Great Valley, and then across the Blue Ridge to tidal estuaries penetrating the coastal plain via the Roanoke River, James River , Potomac River , and Susquehanna River . In the northern section the height of land lies on the inland side of

6300-732: The Iapetus Ocean , from the North America/Europe collision (See Caledonian orogeny ). By the end of the Mesozoic Era , the Appalachian Mountains had been eroded to an almost flat plain. It was not until the region was uplifted during the Cenozoic Era that the distinctive topography of the present formed. Uplift rejuvenated the streams, which rapidly responded by cutting downward into the ancient bedrock. Some streams flowed along weak layers that define

6440-687: The Iberian Peninsula in Western Europe , including the ranges of the Himalayas , Karakoram , Hindu Kush , Alborz , Caucasus , and the Alps . The Himalayas contain the highest mountains in the world, including Mount Everest , which is 8,848 metres (29,029 ft) high. Mountain ranges outside these two systems include the Arctic Cordillera , Appalachians , Great Dividing Range , East Siberians , Altais , Scandinavians , Qinling , Western Ghats , Vindhyas , Byrrangas , and

6580-683: The Mithrim Montes and Doom Mons on Titan, and Tenzing Montes and Hillary Montes on Pluto. Some terrestrial planets other than Earth also exhibit rocky mountain ranges, such as Maxwell Montes on Venus taller than any on Earth and Tartarus Montes on Mars . Jupiter's moon Io has mountain ranges formed from tectonic processes including the Boösaule , Dorian, Hi'iaka and Euboea Montes . Hernando de Soto Hernando de Soto ( / d ə ˈ s oʊ t oʊ / ; Spanish: [eɾˈnando ðe ˈsoto] ; c. 1497 – 21 May 1542)

6720-490: The North American craton . Volcanoes grew along the continental margin coincident with the initiation of subduction . Thrust faulting uplifted and warped older sedimentary rock laid down on the passive margin. As the mountains rose, erosion began to wear them down over time. Streams carried rock debris downslope to be deposited in nearby lowlands. The Taconic orogeny ended after about 60 million years, but built much of

6860-581: The Pánuco River and the Spanish frontier town of Pánuco . There they rested for about a month. During this time many of the Spaniards, having safely returned and reflecting on their accomplishments, decided they had left La Florida too soon. There were some fights within the company, leading to some deaths. But, after they reached Mexico City and the Viceroy Don Antonio de Mendoza offered to lead another expedition to La Florida , few of

7000-492: The Rocky Mountains of the west. Some of the outcrops in the Appalachians contain rocks formed during the Precambrian era. The geologic processes that led to the formation of the Appalachian Mountains started 1.1 billion years ago. The first mountain range in the region was created when the continents of Laurentia and Amazonia collided, creating a supercontinent called Rodinia . The collision of these continents caused

7140-576: The Spanish conquest of the Inca Empire . He was admitted into the prestigious Order of Santiago and "granted the right to conquer Florida". His share was awarded to him by the King of Spain, and he received 724 marks of gold, and 17,740 pesos. He married Isabel de Bobadilla , daughter of Pedrarias Dávila and a relative of a confidante of Queen Isabella . De Soto petitioned King Charles to lead

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7280-596: The Uzita while searching for the lost Narváez expedition ; he later escaped to Mocoso . Ortiz had learned the Timucua language and served as an interpreter to de Soto as he traversed the Timucuan-speaking areas on his way to Apalachee . Ortiz developed a method for guiding the expedition and communicating with the various tribes, who spoke many dialects and languages. He recruited guides from each tribe along

7420-544: The anthropologist John R. Swanton published The Final Report of the United States De Soto Expedition Commission in 1939. Among other locations, Manatee County, Florida , claims an approximate landing site for de Soto and has a national memorial recognizing that event. In the early 21st century, the first part of the expedition's course, up to de Soto's battle at Mabila (a small fortress town in present-day central Alabama ),

7560-722: The eastern seaboard of the United States and the Midwest region of the country. The Eastern Continental Divide follows the Appalachian Mountains from Pennsylvania to Georgia. The Appalachians, particularly the Central and Southern regions, is one of the most biodiverse places in North America. The north–south orientation of the long ridges and valleys contributes to the high number of plant and animal species. Species were able to migrate through these from either direction during alternating periods of warming and cooling, settling in

7700-1552: The mixed-mesophytic or medium-moisture types, which are largely confined to rich, moist montane soils of the southern and central Appalachians, particularly in the Cumberland and Allegheny Mountains, but also thrive in the southern Appalachian coves. Characteristic canopy species are white basswood ( Tilia heterophylla ), yellow buckeye ( Aesculus octandra ), sugar maple ( Acer saccharum ), American beech ( Fagus grandifolia ), tuliptree ( Liriodendron tulipifera ), white ash ( Fraxinus americana ) and yellow birch ( Betula alleganiensis ). Other common trees are red maple ( Acer rubrum ), shagbark and bitternut hickories ( Carya ovata and C. cordiformis ) and black or sweet birch ( Betula lenta ). Small understory trees and shrubs include paw paw ( Asimina tribola ), flowering dogwood ( Cornus florida ), hophornbeam ( Ostrya virginiana ), witch-hazel ( Hamamelis virginiana ) and spicebush ( Lindera benzoin ). There are also hundreds of perennial and annual herbs, among them such herbal and medicinal plants as American ginseng ( Panax quinquefolius ), goldenseal ( Hydrastis canadensis ), bloodroot ( Sanguinaria canadensis ) and black cohosh ( Cimicifuga racemosa ). The foregoing trees, shrubs, and herbs are also more widely distributed in less rich mesic forests that generally occupy coves, stream valleys and flood plains throughout

7840-596: The 1940s has significantly impacted the central Appalachian Mountains in Kentucky , Tennessee , Virginia and West Virginia. Early mining methods were unregulated and mined land reclamation research, including acid base reaction , was led by the West Virginia University in the 1960s and 1970s. West Virginia developed rigorous mine reclamation standards for state coal mines in the late 1960s. Regulations were introduced by most federal states to protect

7980-498: The 96-square-mile (248.6 km) archipelago of Saint Pierre and Miquelon , an overseas collectivity of France , meaning it is technically in three countries. The highest peak of the mountain range is Mount Mitchell in North Carolina at 6,684 feet (2,037 m), which is also the highest point in the United States east of the Mississippi River . The range is older than the other major mountain range in North America,

8120-418: The Appalachian Basin. Some plateaus of the Appalachian Mountains contain metallic minerals such as iron and zinc . There are many geological issues concerning the rivers and streams of the Appalachians. In spite of the existence of the Great Appalachian Valley, many of the main rivers are transverse to the mountain system axis. The drainage divide of the Appalachians follows a tortuous course that crosses

8260-487: The Appalachian Mountains by the late 1960s. Social and political activism brought about the Surface Mining Control and Reclamation Act of 1977 . The 1859 discovery of commercial quantities of petroleum in the Appalachian Mountains of western Pennsylvania started the modern United States petroleum industry . Recent discoveries of commercial natural gas deposits in the Marcellus Shale formation and Utica Shale formations have once again focused oil industry attention on

8400-434: The Appalachian range in New Brunswick and Quebec . 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 whose name they transcribed as Apalchen or Apalachen [a.paˈla.tʃɛn] . The name was soon altered by the Spanish to Apalachee and used as

8540-419: The Blue Ridge again reaches 2,000 ft (600 m) and higher. In the Virginia Blue Ridge, the following are some of the highest peaks north of the Roanoke River : Stony Man 4,031 ft (1,229 m), Hawksbill Mountain 4,066 ft (1,239 m), Apple Orchard Mountain 4,225 ft (1,288 m) and Peaks of Otter 4,001 and 3,875 ft (1,220 and 1,181 m). South of the Roanoke River, along

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8680-439: The Blue Ridge, are Virginia's highest peaks including Whitetop Mountain 5,520 ft (1,680 m) and Mount Rogers 5,729 ft (1,746 m), the highest point in the Commonwealth. Chief summits in the southern section of the Blue Ridge are located along two main crests, the Western or Unaka Front along the Tennessee - North Carolina border and the Eastern Front in North Carolina, or one of several "cross ridges" between

8820-491: The Great Balsams. The Western Blue Ridge Front is subdivided into the Unaka Range , the Bald Mountains , the Great Smoky Mountains , and the Unicoi Mountains , and its major peaks include Roan Mountain 6,285 ft (1,916 m) in the Unakas, Big Bald 5,516 ft (1,681 m) and Max Patch 4,616 ft (1,407 m) in the Bald Mountains, Kuwohi 6,643 ft (2,025 m), Mount Le Conte 6,593 feet (2,010 m), and Mount Guyot 6,621 ft (2,018 m) in

8960-555: The Great Smokies, and Big Frog Mountain 4,224 ft (1,287 m) near the Tennessee- Georgia -North Carolina border. Prominent summits in the cross ridges include Waterrock Knob (6,292 ft (1,918 m)) in the Plott Balsams . Across northern Georgia, numerous peaks exceed 4,000 ft (1,200 m), including Brasstown Bald , the state's highest, at 4,784-and-4,696 ft (1,458-and-1,431 m) Rabun Bald . In north-central Alabama , Mount Cheaha rises prominently to 1,445 feet (440 m) over its surroundings, as part of

9100-483: The Gulf of Mexico. From their winter location in the western panhandle of Florida, having heard of gold being mined "toward the sun's rising", the expedition turned northeast through what is now the modern state of Georgia . Based on archaeological finds made in 2009 at a remote, privately owned site near the Ocmulgee River , researchers believe that de Soto's expedition stopped in Telfair County . Artifacts found here include nine glass trade beads , some of which bear

9240-420: The Mississippi River; sources disagree on the exact location, whether it was what is now Lake Village, Arkansas , or Ferriday, Louisiana . Hernando de Soto was born around the late 1490s or early 1500s in Extremadura , Spain, to parents who were both hidalgos , nobility of modest means. The region was poor and many people struggled to survive; young people looked for ways to seek their fortune elsewhere. He

9380-422: The Napituca Massacre, the first large-scale massacre by Europeans in the current United States. One of Soto’s most important battles with the natives, along his conquest of Florida, was a 1539 battle with Chief Vitachuco. Unlike other native chiefs who entered into peace with the Spanish, Vitachuco did not trust them and had secretly plotted to kill Soto and his army, but he was betrayed by interpreters who told Soto

9520-411: The Richardson/UF Village site (8AL100) in Alachua County , west of Orange Lake , appears to have been accepted by archaeologists as the site of the town of Potano visited by the de Soto expedition. The 17th-century mission of San Buenaventura de Potano is believed to have been founded here. Many archaeologists believe the Parkin Archeological State Park in northeast Arkansas was the main town for

9660-411: The Spanish held Atahualpa captive in Cajamarca for months while his subjects paid for his ransom by filling a room with gold and silver objects. During this captivity, de Soto became friendly with Atahualpa and taught him to play chess . By the time the ransom had been completed, the Spanish became alarmed by rumors of an Inca army advancing on Cajamarca. Pizarro sent de Soto with 200 soldiers to scout for

9800-426: 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

9940-575: The air descends on the leeward side, it warms again (following the adiabatic lapse rate ) and is drier, having been stripped of much of its moisture. Often, a rain shadow will affect the leeward side of a range. As a consequence, large mountain ranges, such as the Andes, compartmentalize continents into distinct climate regions . Mountain ranges are constantly subjected to erosional forces which work to tear them down. The basins adjacent to an eroding mountain range are then filled with sediments that are buried and turned into sedimentary rock . Erosion

10080-632: The altar; that a chaplain be hired at the salary of 12,000 maravedis to perform five masses every week for the souls of De Soto, his parents, and wife; that thirty masses be said for him the day his body was interred, and twenty for our Lady of the Conception, ten for the Holy Ghost , sixty for souls in purgatory and masses for many others as well; that 150000 maravedis be given annually to his wife Isabel for her needs and an equal amount used yearly to marry off three orphan damsels...the poorest that can be found," to assist his wife and also serve to burnish

10220-516: The army of Inca Atahualpa at Cajamarca , Pizarro sent de Soto with fifteen men to invite Atahualpa to a meeting. When Pizarro's men attacked Atahualpa and his guard the next day (the Battle of Cajamarca ), de Soto led one of the three groups of mounted soldiers. The Spanish captured Atahualpa. De Soto was sent to the camp of the Inca army, where he and his men plundered Atahualpa's tents. During 1533,

10360-484: The boats. They survived through the winter, and the spring floods delayed them another two months. By July they set off on their makeshift boats down the Mississippi for the coast. Taking about two weeks to make the journey, the expedition encountered hostile fleets of war canoes along the whole course. The first was led by the powerful paramount chief Quigualtam , whose fleet followed the boats, shooting arrows at

10500-640: The colonial era. The range is the home of a very popular recreational feature, the Appalachian Trail . This is a 2,175-mile (3,500 km) hiking trail that runs all the way from Mount Katahdin in Maine to Springer Mountain in Georgia , passing over or past a large part of the Appalachian range. The International Appalachian Trail is an extension of this hiking trail into the Canadian portion of

10640-456: The continent that are now exposed. The first mountain-building tectonic plate collision that initiated the construction of what are today the Appalachians occurred at least a billion years ago when the pre-North American craton called Laurentia collided with at least one other craton - Amazonia . All the other cratons of the earth also collided at about this time to form the supercontinent Rodinia and were surrounded by one single ocean. (It

10780-668: The continents that were ancestral to North America and Africa collided during the formation of the supercontinent Pangea . Because North America and Africa were once geographically connected, the Appalachians formed part of the same mountain chain as the Little Atlas in Morocco . This mountain range, known as the Central Pangean Mountains , extended into Scotland , before the Mesozoic Era opening of

10920-412: The deciduous needle-leaf conifer, the tamarack , or eastern larch ( Larix laricina ). The dominant northern and high elevation conifer is the red spruce ( Picea rubens ), which grows from near sea level to above 4,000 ft (1,200 m) above sea level (asl) in northern New England and southeastern Canada. It also grows southward along the Appalachian crest to the highest elevations of

11060-529: The driest sites are dominated by chestnut oak, or sometimes by scarlet or northern red oaks. In the northern Appalachians the oaks, except for white and northern red, drop out, while the latter extends farthest north. The oak forests generally lack the diverse small tree, shrub and herb layers of mesic forests. Shrubs are generally ericaceous , and include the evergreen mountain laurel ( Kalmia latifolia ), various species of blueberries ( Vaccinium spp.), black huckleberry ( Gaylussacia baccata ),

11200-485: The east. This mass of rock was removed as the range was actively undergoing uplift. The removal of such a mass from the core of the range most likely caused further uplift as the region adjusted isostatically in response to the removed weight. Rivers are traditionally believed to be the principal cause of mountain range erosion, by cutting into bedrock and transporting sediment. Computer simulation has shown that as mountain belts change from tectonically active to inactive,

11340-513: The events and current history tellers, but some oral histories have been found to be accurate about historic events that have been otherwise documented. The Governor Martin Site at the former Apalachee village of Anhaica , located about a mile east of the present Florida capital in Tallahassee , has been documented as definitively associated with de Soto's expedition. The Governor Martin Site

11480-487: The expedition recorded being received by a female chief ( The Lady of Cofitachequi ), who gave her tribe's pearls, food and other goods to the Spanish soldiers. The expedition found no gold, however, other than pieces from an earlier coastal expedition (presumably that of Lucas Vázquez de Ayllón .) De Soto headed north into the Appalachian Mountains of present-day western North Carolina , where he spent

11620-468: The expedition. At the time of death, de Soto owned four Indian slaves, three horses, and 700 hogs. De Soto had deceived the local natives into believing that he was a deity, specifically an "immortal Son of the Sun ," to gain their submission without conflict. Some of the natives had already become skeptical of de Soto's deity claims, so his men were anxious to conceal his death. The actual site of his burial

11760-524: The first European to reach Florida ; Vasco Núñez de Balboa , the first European to reach the Pacific Ocean coast of the Americas (he called it the "South Sea" on the south coast of Panama ); and Ferdinand Magellan , who first sailed that ocean to East Asia . In 1530, de Soto became a regidor of León, Nicaragua . He led an expedition up the coast of the Yucatán Peninsula searching for

11900-425: The folds and faults created many millions of years earlier. Other streams downcut so rapidly that they cut right across the resistant folded rocks of the mountain core, carving canyons across rock layers and geologic structures. The Appalachian Mountains contain major deposits of anthracite coal as well as bituminous coal . In the folded mountains the coal is in metamorphosed form as anthracite , represented by

12040-775: The government of Guatemala , with "permission to create discovery in the South Sea." He was granted the governorship of Cuba instead. De Soto was expected to colonize the North American continent for Spain within 4 years, for which his family would be given a sizable piece of land. Fascinated by the stories of Cabeza de Vaca , who had survived years in North America after becoming a castaway and had just returned to Spain, de Soto selected 620 Spanish and Portuguese volunteers, including some of mixed-race African descent known as Atlantic Creoles, to accompany him to govern Cuba and colonize North America. Averaging 24 years of age,

12180-445: The indigenous province of Casqui , which de Soto had recorded. They base this on similarities between descriptions from the journals of the de Soto expedition and artifacts of European origin discovered at the site in the 1960s. Theories of de Soto's route are based on the accounts of four chroniclers of the expedition. Milanich and Hudson warn that older translations of the chronicles are often "relatively free translations in which

12320-525: The land as Espíritu Santo after the Holy Spirit . The ships carried priests, craftsmen, engineers, farmers, and merchants; some with their families, some from Cuba, most from Europe and Africa. Few of the men had traveled before outside of Spain, or even away from their home villages. Near de Soto's port, the party found Juan Ortiz , a Spaniard living with the Mocoso people. Ortiz had been captured by

12460-483: The land mass that is now New England and southwestward to Pennsylvania. The Taconic Orogeny was the second of four mountain building plate collisions that contributed to the formation of the Appalachians, culminating in the collision of North America and Africa (see Alleghanian orogeny ). The third mountain-building event was the Acadian orogeny which occurred between 375 and 359 million years ago. The Acadian orogeny

12600-468: The latter. However, balsam fir also does well in soils with a pH as high as 6. Eastern or Canada hemlock ( Tsuga canadensis ) is another important evergreen needle-leaf conifer that grows along the Appalachian chain from north to south but is confined to lower elevations than red spruce and the firs. It generally occupies richer and less acidic soils than the spruce and firs and is characteristic of deep, shaded and moist mountain valleys and coves . It

12740-477: The memory of De Soto as a man of charity and substance. Historians have worked to trace the route of de Soto's expedition in North America, a controversial process over the years. Local politicians vied to have their localities associated with the expedition. The most widely used version of "De Soto's Trail" comes from a study commissioned by the United States Congress . A committee chaired by

12880-463: The men embarked from Havana on seven of the King's ships and two caravels of de Soto's. With tons of heavy armor and equipment, they also carried more than 500 head of livestock, including 237 horses and 200 pigs, for their planned four-year continental expedition. De Soto wrote a new will upon arriving in what is now the Tampa Bay area of Florida. On 10 May 1539, he wrote in his will: That

13020-539: The microclimates that best suited them. The flora of the Appalachians are diverse and vary primarily in response to geology, latitude, elevation and moisture availability. Geobotanically, they constitute a floristic province of the North American Atlantic Region . The Appalachians consist primarily of deciduous broad-leaf trees and evergreen needle-leaf conifers, but also contain the evergreen broad-leaf American holly ( Ilex opaca ), and

13160-788: 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 2,000 ft (600 m) in Pennsylvania. South Mountain achieves its highest point just below the Mason-Dixon line in Maryland at Quirauk Mountain 2,145 ft (654 m) and then diminishes in height southward to the Potomac River . Once in Virginia ,

13300-655: The mountainous belt just north of the New River in Virginia. South of the New River, rivers head into the Blue Ridge, cross the higher Unakas, receive important tributaries from the Great Valley, and traversing the Cumberland Plateau in spreading gorges ( water gaps ), escape by way of the Cumberland River and the Tennessee River rivers to the Ohio River and the Mississippi River, and thence to

13440-549: The mountainous belt, and thus the main lines of drainage run from north to south, exemplified by the Hudson River . However, the valley through which the Hudson River flows was cut by the gigantic glaciers of the ice ages —the same glaciers that deposited their terminal moraines in southern New York and formed the east–west Long Island . The Appalachian region is generally considered the geographical divide between

13580-507: The natural geography has not changed much since de Soto's time, scholars have analyzed those journals with modern topographic intelligence , to develop a more precise account of the De Soto Trail. In May 1539, de Soto landed nine ships with over 620 men and 220 horses in an area generally identified as south Tampa Bay . Historian Robert S. Weddle has suggested that he landed at either Charlotte Harbor or San Carlos Bay . He named

13720-531: 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. The Appalachian belt includes

13860-520: The ocean to the west, young men were attracted to rumors of adventure, glory and wealth. De Soto sailed to the New World with Pedro Arias Dávila , appointed as the first Governor of Panama . In 1520 he participated in Gaspar de Espinosa 's expedition to Veragua , and in 1524, he participated in the conquest of Nicaragua under Francisco Hernández de Córdoba . There he acquired an encomienda and

14000-424: The oceans, but there were no plants or animals on land. Then, during the middle Ordovician Period about 500 to 470 million years ago, the motion of the crustal plates changed, and the continents began to move back toward each other. The once-quiet Appalachian passive margin changed to a very active plate boundary when a neighboring Iapetus oceanic plate containing a volcanic arc collided with and began sinking beneath

14140-490: The plan. So, Soto struck first and, in the process, killed thousands of natives. Those that survived were surrounded and cornered by woods and water. Thousands were killed during the 3 hours battle and 900 survivors took refuge in the pond, specifically Two-mile Pond in Melrose, where they continued to fight, while swimming. Most eventually surrendered, but after 30 hours in the water, 7 men remained and had to be dragged out of

14280-675: 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

14420-532: The plunder from Cuzco. On the road to Cuzco, Manco Inca Yupanqui , a brother of Atahualpa, had joined Pizarro. Manco had been hiding from Atahualpa in fear of his life, and was happy to gain Pizarro's protection. Pizarro arranged for Manco to be installed as the Inca leader. De Soto joined Manco in a campaign to eliminate the Inca armies under Quizquiz , a general who had been loyal to Atahualpa. By 1534, de Soto

14560-490: The process of the Columbian Exchange . For instance, some of the swine brought by de Soto escaped and became the ancestors of feral razorback pigs in the southeastern United States . De Soto was instrumental in contributing to the development of a hostile relationship between many Native American tribes and Europeans. When his expedition encountered hostile natives in the new lands, more often than not it

14700-627: The rate of erosion drops because there are fewer abrasive particles in the water and fewer landslides. Mountains on other planets and natural satellites of the Solar System, including the Moon , are often isolated and formed mainly by processes such as impacts, though there are examples of mountain ranges (or "Montes") somewhat similar to those on Earth. Saturn 's moon Titan and Pluto , in particular, exhibit large mountain ranges in chains composed mainly of ices rather than rock. Examples include

14840-672: The region level. The lowest level of classification is "section". 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

14980-453: The residents of the regions regarding the correct pronunciation. Elsewhere, a commonly accepted pronunciation for the adjective Appalachian is / ˌ æ p ə ˈ l æ tʃ i ə n / , with the last two syllables "-ian" pronounced as in the word "Romanian". 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

15120-486: The result of volcanic activity that occurred around this time. Evidence of subsurface activity, dikes and sills intruding into the overlying rock, is present in the Blue Ridge as well. For instance, mafic rocks have been found along the Fries Fault in the central Blue Ridge area of Montgomery County, VA. The Iapetus continued to expand and during that time bacteria, algae, and many species of invertebrates flourished in

15260-617: The river, the expedition continued traveling westward through modern-day Arkansas, Oklahoma, and Texas. They wintered in Autiamique , on the Arkansas River . After a harsh winter, the Spanish expedition decamped and moved on more erratically. Their interpreter Juan Ortiz had died, making it more difficult for them to get directions and food sources, and generally to communicate with the Natives. The expedition went as far inland as

15400-401: The river, which in his view was an obstacle to his mission. There has been considerable research into the exact location where de Soto crossed the Mississippi River. A commission appointed by Franklin D. Roosevelt in 1935 determined that Sunflower Landing, Mississippi , was the "most likely" crossing place. De Soto possibly traveled down Charley's Trace , which had been used as a trail through

15540-462: The rocks to be folded and faulted, creating the first mountains in the region. Many of the rocks and minerals that were formed during that event can currently be seen at the surface of the present Appalachian range. Around 480 million years ago, geologic processes began that led to three distinct orogenic eras that created much of the surface structure seen in today's Appalachians. During this period, mountains once reached elevations similar to those of

15680-532: The route was conducted 40 years later and benefited from considerable advances in archaeological methods. De Soto's expedition spent another month in the Coosa chiefdom a vassal to Tuskaloosa , who was the paramount chief , believed to have been connected to the large and complex Mississippian culture , which extended throughout the Mississippi Valley and its tributaries. De Soto turned south toward

15820-431: The route. A chain of communication was established whereby a guide who had lived in close proximity to another tribal area was able to pass his information and language on to a guide from a neighboring area. Because Ortiz refused to dress as a hidalgo Spaniard, other officers questioned his motives. De Soto remained loyal to Ortiz, allowing him the freedom to dress and live among his native friends. Another important guide

15960-540: The rumored army. While de Soto was gone, the Spanish in Cajamarca decided to kill Atahualpa to prevent his rescue. De Soto returned to report that he found no signs of an army in the area. After executing Atahualpa, Pizarro and his men headed to Cuzco , the capital of the Incan Empire. As the Spanish force approached Cuzco, Pizarro sent his brother Hernando and de Soto ahead with 40 men. The advance guard fought

16100-531: The same mountain range do not necessarily have the same geologic structure or petrology . They may be a mix of different orogenic expressions and terranes , for example thrust sheets , uplifted blocks , fold mountains, and volcanic landforms resulting in a variety of rock types . Most geologically young mountain ranges on the Earth's land surface are associated with either the Pacific Ring of Fire or

16240-724: The same side of the Great Valley, south of the Potomac, are the Pinnacle 3,007 feet (917 m) and Pidgeon Roost 3,400 ft (1,000 m). In West Virginia, more than 150 peaks rise above 4,000 ft (1,200 m), including Spruce Knob 4,863 ft (1,482 m), the highest point in the Allegheny Mountains . A number of other points in the state rise above 4,800 ft (1,500 m). Cheat Mountain ( Snowshoe Mountain ) at Thorny Flat 4,848 ft (1,478 m) and Bald Knob 4,842 ft (1,476 m) are among

16380-408: 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 2,500 ft (800 m); the summits of Mount Davis and Blue Knob rise over 3,000 ft (900 m). In Maryland, Eagle Rock and Dans Mountain are conspicuous points reaching 3,162 and 2,882 ft (964 and 878 m) respectively. On

16520-545: The ships at Mobile Bay , de Soto led them away from the Gulf Coast. He moved into inland Mississippi , most likely near present-day Tupelo , where they spent the winter. In the spring of 1541, de Soto demanded 200 men as porters from the Chickasaw . They refused his demand and attacked the Spanish camp during the night. On 8 May 1541, de Soto's troops reached the Mississippi River . De Soto had little interest in

16660-450: The soldiers for days as they drifted through their territory. The Spanish had no effective offensive weapons on the water, as their crossbows had long since ceased working. They relied on armor and sleeping mats to block the arrows. About 11 Spaniards were killed along this stretch and many more wounded. On reaching the mouth of the Mississippi, they stayed close to the Gulf shore heading south and west. After about 50 days, they made it to

16800-487: 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

16940-416: The southern Appalachians, as in North Carolina and Tennessee . In the central Appalachians it is usually confined above 3,000 ft (900 m) asl, except for a few cold valleys in which it reaches lower elevations. In the southern Appalachians, it is restricted to higher elevations. Another species is the black spruce ( Picea mariana ), which extends farthest north of any conifer in North America,

17080-413: The southern and central Appalachians consist largely of black , northern red , white , chestnut and scarlet oaks ( Quercus velutina, Q. rubra, Q. alba, Q. prinus and Q. coccinea ) and hickories, such as the pignut ( Carya glabra ) in particular. The richest forests, which grade into mesic types, usually in coves and on gentle slopes, have predominantly white and northern red oaks, while

17220-511: The southern and central Appalachians at low and intermediate elevations. In the northern Appalachians and at higher elevations of the central and southern Appalachians these diverse mesic forests give way to less diverse northern hardwood forests with canopies dominated only by American beech, sugar maple, American basswood ( Tilia americana ) and yellow birch and with far fewer species of shrubs and herbs. Drier and rockier uplands and ridges are occupied by oak–chestnut forests dominated by

17360-409: The southern regions of the Appalachians, the word is pronounced / ˌ æ p ə ˈ l æ tʃ ɪ n z / , with the third syllable sounding like "latch". In northern parts of the mountain range, it is pronounced / ˌ æ p ə ˈ l eɪ tʃ ɪ n z / or / ˌ æ p ə ˈ l eɪ ʃ ɪ n z / ; the third syllable is like "lay", and the fourth "chins" or "shins". There is often great debate between

17500-542: The southernmost spur of the Blue Ridge Mountains. Sources written prior to the recognition of the concept of physiographic regions divided the Appalachian Mountains into three major sections: Plate tectonics over the period dating back at least 1 billion years led to geological creation of the land that is now the Appalachian Mountain range. The continental movement led to collisions that built mountains and they later pulled apart creating oceans over parts of

17640-563: The survivors volunteered. Of the recorded 700 participants at the start, between 300 and 350 survived (311 is a commonly accepted figure). Most of the men stayed in the New World, settling in Mexico, Peru, Cuba, and other Spanish colonies. The Spanish believed that de Soto's excursion to Florida was a failure. They acquired neither gold nor prosperity and founded no colonies. But the expedition had several major consequences. It contributed to

17780-730: The swamps of the Mississippi Delta , to reach the Mississippi River. De Soto and his men spent a month building flatboats, and crossed the river at night to avoid the Native Americans who were patrolling the river. De Soto had hostile relations with the native people in this area. In the late 20th century, research suggests other locations may have been the site of de Soto's crossing, including three locations in Mississippi: Commerce , Friars Point , and Walls , as well as Memphis, Tennessee . Once across

17920-589: The term Appalachian Highlands and Canada uses the term Appalachian Uplands ; the Appalachian Mountains are not synonymous with the Appalachian Plateau , which is one of the provinces of the Appalachian Highlands. The Appalachian range runs from the Island of Newfoundland in Canada, 2,050 mi (3,300 km) southwestward to Central Alabama in the United States; south of Newfoundland, it crosses

18060-633: The town to the ground. During the nine-hour encounter, about 200 Spaniards died, and 150 more were badly wounded, according to the chronicler Elvas. Twenty more died during the next few weeks. They killed an estimated 2,000–6,000 Native Americans at Mabila, making the battle one of the bloodiest in recorded North American history. The Spaniards won a Pyrrhic victory , as they had lost most of their possessions and nearly one-quarter of their horses. The Spaniards were wounded and sickened, surrounded by enemies and without equipment in an unknown territory. Fearing that word of this would reach Spain if his men reached

18200-518: The translators took considerable liberty with the Spanish and Portuguese text." The chronicles describe de Soto's trail in relation to Havana , from which they sailed; the Gulf of Mexico , which they skirted while traveling inland then turned back to later; the Atlantic Ocean , which they approached during their second year; high mountains, which they traversed immediately thereafter; and dozens of other geographic features along their way, such as large rivers and swamps, at recorded intervals. Given that

18340-691: The two main crests. Major subranges of the Eastern Front include the Black Mountains , Great Craggy Mountains , and Great Balsam Mountains , and its chief summits include Grandfather Mountain 5,964 ft (1,818 m) near the Tennessee-North Carolina border, Mount Mitchell 6,684 ft (2,037 m) in the Blacks, and Black Balsam Knob 6,214 ft (1,894 m) and Cold Mountain 6,030 ft (1,840 m) in

18480-530: The water by the Spanish. De Soto's first winter encampment was at Anhaica , the capital of the Apalachee people. It is one of the few places on the route where archaeologists have found physical traces of the expedition. The chroniclers described this settlement as being near the "Bay of Horses" . The bay was named for events of the 1527 Narváez expedition , the members of which, dying of starvation, killed and ate their horses while building boats for escape by

18620-403: The way. Hernando de Soto's army seized the food stored in the villages, captured women to be used as slaves for the soldiers' sexual gratification, and forced men and boys to serve as guides and bearers. The army fought two battles with Timucua groups, resulting in heavy Timucua casualties. After defeating the resisting Timucuan warriors, Hernando de Soto had 200 executed, in what was to be called

18760-700: Was a Spanish explorer and conquistador who was involved in expeditions in Nicaragua and the Yucatan Peninsula . He played an important role in Francisco Pizarro 's conquest of the Inca Empire in Peru, but is best known for leading the first European expedition deep into the territory of the modern-day United States (through Florida , Georgia , Alabama , North Carolina , South Carolina , Mississippi , and most likely Arkansas ). He

18900-490: Was born in the current province of Badajoz. Three towns— Badajoz , Barcarrota and Jerez de los Caballeros —each claim to be his birthplace. Historian Ursula Lamb writes that the Barcarrota claim can be traced to Inca Garcilaso de la Vega and is probably incorrect, having been written down 45 years after De Soto's death. According to Lamb, his birthplace is most likely Jerez de los Caballeros. Although he spent time as

19040-661: Was caused by a series of collisions of pieces of crust from the Avalonia Terrane, sections broken off from continent of Gondwana , with the North American Plate. The collision initiating this orogeny resulted in the closing of the southern Iapetus Ocean and the formation of a high mountain belt. After the Acadian collision took place, Gondwana began to retreat from Laurentia with the newly accreted Avalonian terranes left behind. As Gondwana moved away,

19180-685: Was discovered by archaeologist B. Calvin Jones in March 1987. It has been preserved as the DeSoto Site Historic State Park . The Hutto/Martin Site, 8MR3447, in southeastern Marion County, Florida , on the Ocklawaha River , is the most likely site of the principal town of Acuera referred to in the accounts of the entrada , as well as the site of the seventeenth-century mission of Santa Lucia de Acuera. As of 2016,

19320-439: Was dry. The native populations were made up mostly of subsistence hunter-gatherers. The soldiers found no villages to raid for food, and the army was still too large to live off the land. They were forced to backtrack to the more developed agricultural regions along the Mississippi, where they began building seven bergantines , or pinnaces . They melted down all the iron, including horse tackle and slave shackles, to make nails for

19460-585: Was serving as lieutenant governor of Cuzco while Pizarro was building his new capital on the coast; it later became known as Lima . In 1535 King Charles awarded Diego de Almagro , Francisco Pizarro's partner, the governorship of the southern portion of the Inca Empire. When de Almagro made plans to explore and conquer the southern part of the Inca empire (now Chile ), de Soto applied to be his second-in-command, but de Almagro turned him down. De Soto packed up his treasure and returned to Spain. De Soto returned to Spain in 1536, with wealth gathered from plunder in

19600-455: Was the seventeen-year-old boy Perico , or Pedro, from what is now Georgia . He spoke several of the local tribes' languages and could communicate with Ortiz. Perico was taken as a guide in 1540. The Spanish had also captured other Indians, whom they used as slave labor. Perico was treated better due to his value to the Spaniards. The expedition traveled north, exploring Florida's West Coast, and encountering native ambushes and conflicts along

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