Thirty days later on February 28, 1861, outgoing U.S. President James Buchanan signed an Act of Congress organizing the free Territory of Colorado. The original boundaries of Colorado remain unchanged except for government survey amendments. The name Colorado was chosen because it was commonly believed that the Colorado River originated in the territory. In 1776, Spanish priest Silvestre Vélez de Escalante recorded that Native Americans in the area knew the river as el Rio Colorado for the red-brown silt that the river carried from the mountains. In 1859, a U.S. Army topographic expedition led by Captain John Macomb located the confluence of the Green River with the Grand River in what is now Canyonlands National Park in Utah. The Macomb party designated the confluence as the source of the Colorado River.
On April 12, 1861, South Carolina artillery opened fire on Fort Sumter to start the American Civil War. While many gold seekers held sympathies for the Confederacy, the vast majority remained fiercely loyal to the Union cause.
In 1862, a force of Texas cavalry invaded the Territory of New Mexico and captured Santa Fe on March 10. The object of this Western Campaign was to seize or disrupt the gold fields of Colorado and California and to seize ports on the Pacific Ocean for the Confederacy. A hastily organized force of Colorado volunteers force-marched from Denver City, Colorado Territory, to Glorieta Pass, New Mexico Territory, in an attempt to block the Texans. On March 28, the Coloradans and local New Mexico volunteers stopped the Texans at the Battle of Glorieta Pass, destroyed their cannon and supply wagons, and dispersed 500 of their horses and mules. The Texans were forced to retreat to Santa Fe. Having lost the supplies for their campaign and finding little support in New Mexico, the Texans abandoned Santa Fe and returned to San Antonio in defeat. The Confederacy made no further attempts to seize the Southwestern United States.
In 1864, Territorial Governor John Evans appointed the Reverend John Chivington as Colonel of the Colorado Volunteers with orders to protect white settlers from Cheyenne and Arapaho warriors who were accused of stealing cattle. Colonel Chivington ordered his men to attack a band of Cheyenne and Arapaho encamped along Sand Creek. Chivington reported that his troops killed more than 500 warriors. The militia returned to Denver City in triumph, but several officers reported that the so-called battle was a blatant massacre of Indians at peace, that most of the dead were women and children, and that bodies of the dead had been hideously mutilated and desecrated. Three U.S. Army inquiries condemned the action, and incoming President Andrew Johnson asked Governor Evans for his resignation, but none of the perpetrators was ever punished. This event is now known as the Sand Creek massacre.
In the midst and aftermath of the Civil War, many discouraged prospectors returned to their homes, but a few stayed and developed mines, mills, farms, ranches, roads, and towns in Colorado Territory. On September 14, 1864, James Huff discovered silver near Argentine Pass, the first of many silver strikes. In 1867, the Union Pacific Railroad laid its tracks west to Weir, now Julesburg, in the northeast corner of the Territory. The Union Pacific linked up with the Central Pacific Railroad at Promontory Summit, Utah, on May 10, 1869, to form the First Transcontinental Railroad. The Denver Pacific Railway reached Denver in June the following year, and the Kansas Pacific arrived two months later to forge the second line across the continent. In 1872, rich veins of silver were discovered in the San Juan Mountains on the Ute Indian reservation in southwestern Colorado. The Ute people were removed from the San Juans the following year.


Colorado (/ˌkɒləˈrædoʊ, -ˈrɑːdoʊ/ (listen), other variants) is a state in the Mountain West subregion of the Western United States. It encompasses most of the Southern Rocky Mountains, as well as the northeastern portion of the Colorado Plateau and the western edge of the Great Plains. Colorado is the eighth most extensive and 21st most populous U.S. state. The 2020 United States Census enumerated the population of Colorado at 5,773,714, an increase of 14.80% since the 2010 United States Census.
The region has been inhabited by Native Americans for more than 13,000 years, with the Lindenmeier site containing artifacts dating from approximately 9200 to 1000 BC; the eastern edge of the Rocky Mountains was a major migration route for early peoples who spread throughout the Americas. "Colorado" is the Spanish adjective meaning "ruddy", the color of red sandstone. The Territory of Colorado was organized on February 28, 1861, and on August 1, 1876, U.S. President Ulysses S. Grant signed Proclamation 230 admitting Colorado to the Union as the 38th state. Colorado is nicknamed the "Centennial State" because it became a state one century after the signing of the United States Declaration of Independence.
Colorado is bordered by Wyoming to the north, Nebraska to the northeast, Kansas to the east, Oklahoma to the southeast, New Mexico to the south, and Utah to the west, as well as touching Arizona to the southwest at the Four Corners. Colorado is noted for its vivid landscape of mountains, forests, high plains, mesas, canyons, plateaus, rivers, and desert lands. Colorado is one of the Mountain States, and is a part of the western and southwestern United States.
Denver is the capital of and most populous city in Colorado. Residents of the state are known as Coloradans, although the antiquated "Coloradoan" is occasionally used. Colorado is a comparatively wealthy state, ranking eighth in household income in 2016, and 11th in per capita income in 2010. It also ranks highly in the nation's standard of living index. Major parts of the economy include government and defense, mining, agriculture, tourism, and increasingly other kinds of manufacturing. With increasing temperatures and decreasing water availability, Colorado's agriculture, forestry, and tourism economies are expected to be heavily affected by climate change.


Roughly 70% of Colorado's population resides along the eastern edge of the Rocky Mountains in the Front Range Urban Corridor between Cheyenne, Wyoming, and Pueblo, Colorado. This region is partially protected from prevailing storms that blow in from the Pacific Ocean region by the high Rockies in the middle of Colorado. The "Front Range" includes Denver, Boulder, Fort Collins, Loveland, Castle Rock, Colorado Springs, Pueblo, Greeley, and other townships and municipalities in between. On the other side of the Rockies, the significant population centers in Western Colorado (which is not considered the "Front Range") are the cities of Grand Junction, Durango, and Montrose.


To the south and east is the Gulf of Maine, and to the west is the state of New Hampshire. The Canadian province of New Brunswick is to the north and northeast, and the province of Québec is to the northwest. Maine is the northernmost state in New England and the largest, accounting for almost half of the region's entire land area. Maine is the only state to border exactly one other American state (New Hampshire).
Maine is the easternmost state in the United States both in its extreme points and in its geographic center. The town of Lubec is the easternmost organized settlement in the United States. Its Quoddy Head Lighthouse is also the closest place in the United States to Africa and Europe. Estcourt Station is Maine's northernmost point, as well as the northernmost point in New England. (For more information see extreme points of the United States.)
Maine's Moosehead Lake is the largest lake wholly in New England, since Lake Champlain is located between Vermont, New York and Québec. A number of other Maine lakes, such as South Twin Lake, are described by Thoreau in The Maine Woods (1864). Mount Katahdin is the northern terminus of the Appalachian Trail, which extends southerly to Springer Mountain, Georgia, and the southern terminus of the new International Appalachian Trail which, when complete, will run to Belle Isle, Newfoundland and Labrador.
Machias Seal Island and North Rock, off the state's Downeast coast, are claimed by both Canada and the American town of Cutler, and are within one of four areas between the two countries whose sovereignty is still in dispute, but it is the only one of the disputed areas containing land. Also in this easternmost area in the Bay of Fundy is the Old Sow, the largest tidal whirlpool in the Western Hemisphere.
Maine is the least densely populated U.S. state east of the Mississippi River. It is called the Pine Tree State; over 80% of its total land is forested or unclaimed, the most forest cover of any U.S. state. In the wooded areas of the interior lies much uninhabited land, some of which does not have formal political organization into local units (a rarity in New England). The Northwest Aroostook unorganized territory in the northern part of the state, for example, has an area of 2,668 square miles (6,910 km²) and a population of 10, or one person for every 267 square miles (690 km²).
Maine is in the temperate broadleaf and mixed forests biome. The land near the southern and central Atlantic coast is covered by the mixed oaks of the Northeastern coastal forests. The remainder of the state, including the North Woods, is covered by the New England–Acadian forests.
Maine has almost 230 miles (400 km) of ocean coastline (and 3,500 miles (5,600 km) of tidal coastline). West Quoddy Head in Lubec is the easternmost point of land in the 48 contiguous states. Along the famous rock-bound coast of Maine are lighthouses, beaches, fishing villages, and thousands of offshore islands, including the Isles of Shoals which straddle the New Hampshire border. There are jagged rocks and cliffs and many bays and inlets. Inland are lakes, rivers, forests, and mountains. This visual contrast of forested slopes sweeping down to the sea has been summed up by American poet Edna St. Vincent Millay of Rockland and Camden, in "Renascence":
All I could see from where I stood

Was three long mountains and a wood;

I turned and looked the other way,

And saw three islands in a bay.
Geologists describe this type of landscape as a "drowned coast", where a rising sea level has invaded former land features, creating bays out of valleys and islands out of mountain tops. A rise in land elevation due to the melting of heavy glacier ice caused a slight rebounding effect of underlying rock; this land rise, however, was not enough to eliminate all the effect of the rising sea level and its invasion of former land features.
Much of Maine's geomorphology was created by extended glacial activity at the end of the last ice age. Prominent glacial features include Somes Sound and Bubble Rock, both part of Acadia National Park on Mount Desert Island. Carved by glaciers, Somes Sound reaches depths of 175 feet (50 m). The extreme depth and steep drop-off allow large ships to navigate almost the entire length of the sound. These features also have made it attractive for boat builders, such as the prestigious Hinckley Yachts.
Bubble Rock, a glacial erratic, is a large boulder perched on the edge of Bubble Mountain in Acadia National Park. By analyzing the type of granite, geologists discovered that glaciers carried Bubble Rock to its present location from near Lucerne, 30 miles (48 km) away. The Iapetus Suture runs through the north and west of the state, being underlain by the ancient Laurentian terrane, and the south and east underlain by the Avalonian terrane.
Acadia National Park is the only national park in New England. Areas under the protection and management of the National Park Service include:
Acadia National Park near Bar Harbor
Appalachian National Scenic Trail
Maine Acadian Culture in St. John Valley
Roosevelt Campobello International Park on Campobello Island in New Brunswick, Canada, operated by both the U.S. and Canada, just across the Franklin Delano Roosevelt Bridge from Lubec
Saint Croix Island International Historic Site at Calais
Katahdin Woods and Waters National Monument
Lands under the control of the state of Maine include:
Maine State Parks
Maine Wildlife Management Areas (WMA)


Maine (/meɪn/ (listen)) is a state in the New England region of the United States, bordered by New Hampshire to the west; the Gulf of Maine to the southeast; and the Canadian provinces of New Brunswick and Quebec to the northeast and northwest, respectively. Maine is the 12th-smallest by area, the 9th-least populous, the 13th-least densely populated, and the most rural of the 50 U.S. states. It is also the northeasternmost among the contiguous United States, the northernmost state east of the Great Lakes, the only state whose name consists of a single syllable, and the only state to border exactly one other US state. Approximately half the area of Maine lies on each side of the 45th parallel north in latitude. The most populous city in Maine is Portland, while its capital is Augusta.
Maine has traditionally been known for its jagged, rocky Atlantic Ocean and bayshore coastlines; smoothly contoured mountains; heavily forested interior; picturesque waterways; and its wild lowbush blueberries and seafood cuisine, especially lobster and clams. Coastal and Down East Maine, especially in the vicinity of Portland, have emerged as an important center for the creative economy, which is also bringing gentrification.
For thousands of years after the glaciers retreated during the last ice age, indigenous peoples were the only inhabitants of the territory that is now Maine. At the time of European arrival, several Algonquian-speaking peoples inhabited the area. The first European settlement in the area was by the French in 1604 on Saint Croix Island, founded by Pierre Dugua, Sieur de Mons. The first English settlement was the short-lived Popham Colony, established by the Plymouth Company in 1607. A number of English settlements were established along the coast of Maine in the 1620s, although the rugged climate and conflict with the local indigenous people caused many to fail.
As Maine entered the 18th century, only a half dozen European settlements had survived. Loyalist and Patriot forces contended for Maine's territory during the American Revolution. During the War of 1812, the largely undefended eastern region of Maine was occupied by British forces with the goal of annexing it to Canada via the Colony of New Ireland, but returned to the United States following failed British offensives on the northern border, mid-Atlantic and south which produced a peace treaty that restored the pre-war boundaries. Maine was part of the Commonwealth of Massachusetts until 1820 when it voted to secede from Massachusetts to become a separate state. On March 15, 1820, under the Missouri Compromise, it was admitted to the Union as the 23rd state.


Formal secession from Massachusetts and admission of Maine as the 23rd state occurred on March 15, 1820, as part of the Missouri Compromise, which geographically limited the spread of slavery and enabled the admission to statehood of Missouri the following year, keeping a balance between slave and free states.
Maine's original state capital was Portland, Maine's largest city, until it was moved to the more central Augusta in 1832. The principal office of the Maine Supreme Judicial Court remains in Portland.
The 20th Maine Volunteer Infantry Regiment, under the command of Colonel Joshua Lawrence Chamberlain, prevented the Union Army from being flanked at Little Round Top by the Confederate Army during the Battle of Gettysburg.
Four U.S. Navy ships have been named USS Maine, most famously the armored cruiser USS Maine (ACR-1), whose sinking by an explosion on February 15, 1898 precipitated the Spanish–American War.


The original inhabitants of the territory that is now Maine were Algonquian-speaking Wabanaki peoples, including the Passamaquoddy, Maliseet, Penobscot, Androscoggin, and Kennebec. During the later King Philip's War, many of these peoples would merge in one form or another to become the Wabanaki Confederacy, aiding the Wampanoag of Massachusetts and the Mahican of New York. Afterwards, many of these people were driven from their natural territories, but most of Maine's tribes continued, unchanged, until the American Revolution. Before this point, however, most of these people were considered separate nations. Many had adapted to living in permanent, Iroquois-inspired settlements, while those along the coast tended to be semi-nomadic—traveling from settlement to settlement on a yearly cycle. They would usually winter inland and head to the coasts by summer.
European contact with what is now called Maine may have started around 1200 CE when Norwegians are believed to have interacted with the native Penobscot in present-day Hancock County, most likely through trade. If confirmed, this would make Maine the site of the earliest European discovery in the entire US. About 200 years earlier, from the settlements in Iceland and Greenland, Norwegians first identified America and attempted to settle areas such as Newfoundland, but failed to establish a permanent settlement. Archeological evidence suggests that Norwegians in Greenland returned to North America for several centuries after the initial discovery to trade and collect timber, with the most relevant evidence being the Maine Penny, an 11th-century Norwegian coin found at a Native American dig site in 1954.
The first European confirmed settlement in modern-day Maine was in 1604 on Saint Croix Island, led by French explorer Pierre Dugua, Sieur de Mons. His party included Samuel de Champlain, noted as an explorer. The French named the entire area Acadia, including the portion that later became the state of Maine. The Plymouth Company established the first English settlement in Maine at the Popham Colony in 1607, the same year as the settlement at Jamestown, Virginia. The Popham colonists returned to Britain after 14 months.
The French established two Jesuit missions: one on Penobscot Bay in 1609, and the other on Mount Desert Island in 1613. The same year, Claude de La Tour established Castine. In 1625, Charles de Saint-Étienne de la Tour erected Fort Pentagouet to protect Castine. The coastal areas of eastern Maine first became the Province of Maine in a 1622 land patent. The part of western Maine north of the Kennebec River was more sparsely settled and was known in the 17th century as the Territory of Sagadahock. A second settlement was attempted in 1623 by English explorer and naval Captain Christopher Levett at a place called York, where he had been granted 6,000 acres (24 km²) by King Charles I of England. It also failed.
The 1622 patent of the Province of Maine was split at the Piscataqua River into the Province of New Hampshire to the south and New Somersetshire to the north. A disputed 1630 patent split off the area around present-day Saco as Lygonia. Justifying its actions with a 1652 geographic survey that showed an overlapping patent, the Massachusetts Bay Colony had seized New Somersetshire and Lygonia by force by 1658. The Territory of Sagadahock between the Kennebec River and St. Croix River notionally became Cornwall County, Province of New York under a 1664 grant from Charles II of England to his brother James, at the time the Duke of York. Some of this land was claimed by New France as part of Acadia. All of the English settlements in the Massachusetts Bay Colony and the Province of New York became part of the Dominion of New England in 1686. All of present-day Maine was unified as York County, Massachusetts under a 1691 royal patent for the Province of Massachusetts Bay.
Central Maine was formerly inhabited by the Androscoggin tribe of the Abenaki nation, also known as Arosaguntacook. They were driven out of the area in 1690 during King William's War. They were relocated to St. Francis, Canada, which was destroyed by Rogers' Rangers in 1759, and is now Odanak. The other Abenaki tribes suffered several severe defeats, particularly during Dummer's War, with the capture of Norridgewock in 1724 and the defeat of the Pequawket in 1725, which significantly reduced their numbers. They finally withdrew to Canada, where they were settled at Bécancour and Sillery, and later at St. Francis, along with other refugee tribes from the south.
Maine was much fought over by the French, English, and allied natives during the 17th and 18th centuries. These natives conducted raids against settlers and each other, taking captives for ransom or, in some cases, kidnapped for adoption by Native American tribes. A notable example was the early 1692 Abenaki raid on York, where about 100 English settlers were killed and another estimated 80 taken hostage. The Abenaki took captives taken during raids of Massachusetts in Queen Anne's War of the early 1700s to Kahnewake, a Catholic Mohawk village near Montreal, where some were adopted and others ransomed.
After the British defeated the French in Acadia in the 1740s, the territory from the Penobscot River east fell under the nominal authority of the Province of Nova Scotia, and together with present-day New Brunswick formed the Nova Scotia county of Sunbury, with its court of general sessions at Campobello. American and British forces contended for Maine's territory during the American Revolution and the War of 1812, with the British occupying eastern Maine in both conflicts via the Colony of New Ireland. The territory of Maine was confirmed as part of Massachusetts when the United States was formed following the Treaty of Paris ending the revolution, although the final border with British North America was not established until the Webster–Ashburton Treaty of 1842.
Maine was physically separate from the rest of Massachusetts. Long-standing disagreements over land speculation and settlements led to Maine residents and their allies in Massachusetts proper forcing an 1807 vote in the Massachusetts Assembly on permitting Maine to secede; the vote failed. Secessionist sentiment in Maine was stoked during the War of 1812 when Massachusetts pro-British merchants opposed the war and refused to defend Maine from British invaders. In 1819, Massachusetts agreed to permit secession, sanctioned by voters of the rapidly growing region the following year.


Maine has a humid continental climate (Köppen climate classification Dfb), with warm and sometimes humid summers, and long, cold and very snowy winters. Winters are especially severe in the Northern and Western parts of Maine, while coastal areas are moderated slightly by the Atlantic Ocean, resulting in marginally milder winters and cooler summers than inland regions. Daytime highs are generally in the 75–80 °F (24–27 °C) range throughout the state in July, with overnight lows in the high 50s °F (around 15 °C). January temperatures range from highs near 30 °F (−1 °C) on the southern coast to overnight lows averaging below 0 °F (−18 °C) in the far north.
The state's record high temperature is 105 °F (41 °C), set in July 1911, at North Bridgton.
Precipitation in Maine is evenly distributed year-round, but with a slight summer maximum in northern/northwestern Maine and a slight late-fall or early-winter maximum along the coast due to "nor'easters" or intense cold-season rain and snowstorms. In coastal Maine, the late spring and summer months are usually driest—a rarity across the Eastern United States. Maine has fewer days of thunderstorms than any other state east of the Rockies, with most of the state averaging fewer than twenty days of thunderstorms a year. Tornadoes are rare in Maine, with the state averaging two per year, although this number is increasing. Most severe thunderstorms and tornadoes occur in the Sebago Lakes & Foothills region of the state. Maine rarely sees the effect of tropical cyclones, as they tend to pass well east and south or are greatly weakened by the time they reach Maine.
In January 2009, a new record low temperature for the state was set at Big Black River of −50 °F (−46 °C), tying the New England record.
Annual precipitation varies from 35.8 in (909 mm) in Presque Isle to 56.7 in (1,441 mm) in Acadia National Park.


The United States Census Bureau estimates that the population of Maine was 1,344,212 on July 1, 2019, a 1.19% increase since the 2010 United States census. At the 2020 census, 1,362,359 people lived in the state. The state's population density is 41.3 people per square mile, making it the least densely populated state east of the Mississippi River. As of 2010, Maine was also the most rural state in the Union, with only 38.7% of the state's population living within urban areas. As explained in detail under "Geography", there are large tracts of uninhabited land in some remote parts of the interior of the state, particularly in the North Maine Woods.
The mean population center of Maine is located in Kennebec County, just east of Augusta. The Greater Portland metropolitan area is the most densely populated with nearly 40% of Maine's population. This area spans three counties and includes many farms and wooded areas; the 2016 population of Portland proper was 66,937.
Maine has experienced a very slow rate of population growth since the 1990 census; its rate of growth (0.57%) since the 2010 census ranks 45th of the 50 states. The modest population growth in the state has been concentrated in the southern coastal counties; with more diverse populations slowly moving into these areas of the state. However, the northern, more rural areas of the state have experienced a slight decline in population from 2010 to 2016.
According to the 2010 Census, Maine has the highest percentage of non-Hispanic whites of any state, at 94.4% of the total population. In 2011, 89.0% of all births in the state were to non-Hispanic white parents. Maine also has the second-highest residential senior population.
The table below shows the racial composition of Maine's population as of 2016.
According to the 2016 American Community Survey, 1.5% of Maine's population were of Hispanic or Latino origin (of any race): Mexican (0.4%), Puerto Rican (0.4%), Cuban (0.1%), and other Hispanic or Latino origin (0.6%). The five largest ancestry groups were: English (20.7%), Irish (17.3%), French (15.7%), German (8.1%), and American (7.8%).
People citing that they are American are of overwhelmingly English descent, but have ancestry that has been in the region for so long (often since the 17th century) that they choose to identify simply as Americans.
Maine has the highest percentage of French Americans of any state. Most of them are of Canadian origin, but in some cases have been living there since prior to the American Revolutionary War. There are particularly high concentrations in the northern part of Maine in Aroostook County, which is part of a cultural region known as Acadia that goes over the border into New Brunswick. Along with the Acadian population in the north, many French-Canadians came from Quebec as immigrants between 1840 and 1930.
The upper Saint John River valley area was once part of the so-called Republic of Madawaska, before the frontier was decided in the Webster-Ashburton Treaty of 1842. Over a quarter of the population of Lewiston, Waterville, and Biddeford are Franco-American. Most of the residents of the Mid Coast and Down East sections are chiefly of British heritage. Smaller numbers of various other groups, including Irish, Italian and Polish, have settled throughout the state since the late 19th and early 20th century immigration waves.


Southern Oregon generally supports candidates of the Republican Party; besides Jackson County, which is considered a swing county, no Democrat has won any county of Southern Oregon in presidential elections since 1996 using the seven-county definition, or since 1964 using the four-county definition. Josephine County has not supported a Democrat for president since 1936.


Southern Oregon is a region of the U.S. state of Oregon south of Lane County and generally west of the Cascade Range, excluding the southern Oregon Coast. Counties include Douglas, Jackson, Klamath, and Josephine. It includes the Southern Oregon American Viticultural Area, which consists of the Umpqua and Rogue River drainages. As of 2015, the population in the four counties is about 471,000, and in the greater, seven-county definition, it is about 564,000.


Amaranthaceae is a widespread and cosmopolitan family from the tropics to cool temperate regions. The Amaranthaceae (sensu stricto) are predominantly tropical, whereas the former Chenopodiaceae have their centers of diversity in dry temperate and warm temperate areas. Many of the species are halophytes, tolerating salty soils, or grow in dry steppes or semi-deserts.


The basic chromosome number is (rarely 6) mostly 8–9 (rarely 17).


Amaranthaceae is a family of flowering plants commonly known as the amaranth family, in reference to its type genus Amaranthus. It includes the former goosefoot family Chenopodiaceae and contains about 165 genera and 2,040 species, making it the most species-rich lineage within its parent order, Caryophyllales.


Widespread in the Amaranthaceae is the occurrence of betalain pigments. The former Chenopodiaceae often contain isoflavonoids.
In phytochemical research, several methylenedioxyflavonols, saponins, triterpenoids, ecdysteroids, and specific root-located carbohydrates have been found in these plants.


The state is named for the Missouri River, which was named after the indigenous Missouri Indians, a Siouan-language tribe. It is said they were called the ouemessourita (wimihsoorita), meaning "those who have dugout canoes", by the Miami-Illinois language speakers. In the language of the Miami-Illinois's close neighbors, the Ojibwe, it could mean "You Ought to Go Downriver & Visit Those People."
Assuming Missouri were deriving from the Siouan language, it could come from "Maya Sunni" (MAH-yah SOO-nee), which translates as "It connects to the side of it", in reference to the river itself. Most likely, though, the name Missouri comes from Chiwere, a Siouan language spoken by people who resided in the modern-day states of Wisconsin, Iowa, South Dakota, Missouri, and Nebraska.
The name Missouri has several different pronunciations even among its present-day natives, the two most common being /mɪˈzɜːri/ (listen) mə-ZUR-ee and /mɪˈzɜːrə/ (listen) mə-ZUR-ə. Further pronunciations also exist in Missouri or elsewhere in the United States, involving the realization of the medial consonant as either /z/ or /s/; the vowel in the second syllable as either /ɜːr/ or /ʊər/; and the third syllable as /i/ (phonetically [i] (listen), [ɪ] (listen), or [ɪ̈] (listen)) or /ə/. Any combination of these phonetic realizations may be observed coming from speakers of American English. In British received pronunciation, the preferred variant is /mɪˈzʊəri/, with /mɪˈsʊəri/ being a possible alternative.
The linguistic history was treated definitively by Donald M. Lance, who acknowledged that the question is sociologically complex, but no pronunciation could be declared "correct", nor could any be clearly defined as native or outsider, rural or urban, southern or northern, educated or otherwise. Politicians often employ multiple pronunciations, even during a single speech, to appeal to a greater number of listeners. In informal contexts respellings of the state's name, such as "Missour-ee" or "Missour-uh", are occasionally used to distinguish pronunciations phonetically.


Archaeological excavations along river valleys have shown continuous habitation since about 9000 BCE. Beginning before 1000 CE, the people of the Mississippian culture created regional political centers at present-day St. Louis and across the Mississippi River at Cahokia, near present-day Collinsville, Illinois. Their large cities included thousands of individual residences. Still, they are known for their surviving massive earthwork mounds, built for religious, political and social reasons, in platform, ridgetop and conical shapes. Cahokia was the center of a regional trading network that reached from the Great Lakes to the Gulf of Mexico. The civilization declined by 1400 CE, and most descendants left the area long before the arrival of Europeans. St. Louis was at one time known as Mound City by the European Americans because of the numerous surviving prehistoric mounds since lost to urban development. The Mississippian culture left mounds throughout the middle Mississippi and Ohio river valleys, extending into the southeast and the upper river.
The land that became the state of Missouri was part of numerous different territories possessed changing and often indeterminate borders and had many different Native American and European names between the 1600s and statehood. For much of the first half of the 1700s, the west bank of the Mississippi River that would become Missouri was mostly uninhabited, something of a no man's land that kept peace between the Illinois on the east bank of the Mississippi River and to the North, and the Osage and Missouri Indians of the lower Missouri Valley. In the early 1700s, French traders and missionaries explored the whole of the Mississippi Valley, named the region “Louisiana.” Around the same time, a different group of French Canadians who established five villages on the east bank of the Mississippi River placed their settlements in the le pays des Illinois, “the country of the Illinois.” When habitants – settlers of French Canadian descent – began crossing the Mississippi River to establish settlements such as Ste. Genevieve, they continued to place their settlements in the Illinois Country. At the same time, the French settlements on both sides of the Mississippi River were part of the French province of Louisiana. To distinguish the settlements in the Middle Mississippi Valley from French settlements in the lower Mississippi Valley around New Orleans, French officials and inhabitants referred to the Middle Mississippi Valley as La Haute Louisiane, “The High Louisiana,” or “Upper Louisiana.”
The first European settlers were mostly ethnic French Canadians, who created their first settlement in Missouri at present-day Ste. Genevieve, about an hour south of St. Louis. They had migrated about 1750 from the Illinois Country. They came from colonial villages on the east side of the Mississippi River, where soils were becoming exhausted, and there was insufficient river bottom land for the growing population. The early Missouri settlements included many enslaved Africans and Native Americans, and slave labor was central to both commercial agriculture and the fur trade. Sainte-Geneviève became a thriving agricultural center, producing enough surplus wheat, corn and tobacco to ship tons of grain annually downriver to Lower Louisiana for trade. Grain production in the Illinois Country was critical to the survival of Lower Louisiana and especially the city of New Orleans.
St. Louis was founded soon after by French fur traders, Pierre Laclède and stepson Auguste Chouteau from New Orleans in 1764. From 1764 to 1803, European control of the area west of the Mississippi to the northernmost part of the Missouri River basin, called Louisiana, was assumed by the Spanish as part of the Viceroyalty of New Spain, due to Treaty of Fontainebleau (in order to have Spain join with France in the war against England). The arrival of the Spanish in St. Louis was in September 1767.
St. Louis became the center of a regional fur trade with Native American tribes that extended up the Missouri and Mississippi rivers, which dominated the regional economy for decades. Trading partners of major firms shipped their furs from St. Louis by river down to New Orleans for export to Europe. They provided a variety of goods to traders for sale and trade with their Native American clients. The fur trade and associated businesses made St. Louis an early financial center and provided the wealth for some to build fine houses and import luxury items. Its location near the confluence of the Illinois River meant it also handled produce from the agricultural areas. River traffic and trade along the Mississippi were integral to the state's economy. As the area's first major city, St. Louis expanded greatly after the invention of the steamboat and the increased river trade.


North Carolina was inhabited for at least ten thousand years by succeeding prehistoric indigenous cultures. The Hardaway Site saw major periods of occupation dating to 10,000 years BCE. Before 200 AD, the people were building earthwork platform mounds, which were used for ceremonial and religious purposes. Succeeding peoples, including those of the South Appalachian Mississippian culture, established by 1000 AD in the Piedmont and mountain region, continued to build this style of mounds. In contrast to some of the larger centers of the classic Mississippian culture (as noted below), in what became known as the western Carolinas, northeastern Georgia and southeastern Tennessee, most of the larger towns had only one central platform mound. The smaller settlements had none but developed close to the more prominent towns. This area became known as the homelands of the historic Cherokee people, who are believed to have migrated over time from the Great Lakes area.
In the 500–700 years preceding European contact, the Mississippian culture built large, complex cities and maintained far-flung regional trading networks. Its largest city was Cahokia, which had numerous mounds for different purposes, a highly stratified society, and was located in present-day southwestern Illinois near the Mississippi River. The Native polities of the Mississippian culture fell apart and reformed as new groups, such as the Catawba, due to a series of destabilizing events known as the "Mississippian shatter zone". As described by anthropologist Robbie Ethridge, the Mississippian shatter zone was an area of great instability, in what is now the American South, caused by the instability of Mississippian chiefdoms, high mortality from new Eurasian diseases, construction of a global capitalistic economy based on trading of Native American slaves, and the emergence of Native "militaristic slaving societies".
Historically documented tribes in the North Carolina region include the Carolina Algonquian-speaking tribes of the coastal areas, such as the Chowanoke, Roanoke, Pamlico, Machapunga, Coree, and Cape Fear Indians, who were the first encountered by the English; the Iroquoian-speaking Meherrin, Cherokee, and Tuscarora of the interior; and Southeastern Siouan tribes, such as the Cheraw, Waxhaw, Saponi, Waccamaw, and Catawba of the Piedmont.
In the late 16th century, the first Spanish explorers traveling inland recorded meeting  Mississippian culture people at Joara, a regional chiefdom near what later developed as Morganton. Records of Hernando de Soto attested to his meeting with them in 1540. In 1567, Captain Juan Pardo led an expedition to claim the area for the Spanish colony and to establish another route to reach silver mines in Mexico. Pardo made a winter base at Joara, which he renamed Cuenca. His expedition built Fort San Juan and left a contingent of 30 men there, while Pardo traveled further. His forces built and garrisoned five other forts. He returned by a different route to Santa Elena on Parris Island, South Carolina, then a center of Spanish Florida. In the spring of 1568, natives killed all but one of the Spanish soldiers and burned the six forts in the interior, including the one at Fort San Juan. Although the Spanish never returned to the interior, this effort marked the first European attempt at colonization of the interior of what became the United States. A 16th-century journal by Pardo's scribe Bandera, and archaeological findings since 1986 at Joara, have confirmed the settlement.


In 1860, North Carolina was a slave state, in which one-third of the state's total population were African-American slaves. The state did not vote to join the Confederacy until President Abraham Lincoln called on it to invade its sister state, South Carolina, becoming the last or penultimate state to officially join the Confederacy. The title of "last to join the Confederacy" has been disputed; although Tennessee's informal secession on May 7, 1861, preceded North Carolina's official secession on May 20, the Tennessee legislature did not formally vote to secede until June 8, 1861.
Around 125,000 troops from North Carolina served in the Confederate Army, and about 15,000 North Carolina troops (both black and white) served in Union Army regiments, including men who left the state to join Union regiments elsewhere. Over 30,000 North Carolina troops died from combat or disease during the war. Elected in 1862, Governor Zebulon Baird Vance tried to maintain state autonomy against Confederate President Jefferson Davis in Richmond. The state government was reluctant to support the demands of the national government in Richmond, and the state was the scene of only small battles. In 1865, Durham County saw the largest single surrender of Confederate soldiers at Bennett Place, when Joseph E. Johnston surrendered the Army of Tennessee and all remaining Confederate forces still active in North Carolina, South Carolina, Georgia, and Florida, totalling 89,270 soldiers.
After secession, some North Carolinians refused to support the Confederacy. Some of the yeoman farmers chiefly in the state's mountains and western Piedmont region remained neutral during the Civil War, with others covertly supporting the Union cause during the conflict. Approximately 15,000 North Carolinians (both black and white) from across the state would enlist in the Union Army. Numerous slaves would also escape to Union lines, where they became essentially free.
Confederate troops from all parts of North Carolina served in virtually all the major battles of the Army of Northern Virginia, the Confederacy's most famous army. The largest battle fought in North Carolina was at Bentonville, which was a futile attempt by Confederate General Joseph Johnston to slow Union General William Tecumseh Sherman's advance through the Carolinas in the spring of 1865. In April 1865, after losing the Battle of Morrisville, Johnston surrendered to Sherman at Bennett Place, in what is today Durham. North Carolina's port city of Wilmington, was the last Confederate port to fall to the Union, in February 1865, after the Union won the nearby Second Battle of Fort Fisher, its major defense downriver.
The first Confederate soldier to be killed in the Civil War was Private Henry Wyatt from North Carolina, in the Battle of Big Bethel in June 1861. At the Battle of Gettysburg in July 1863, the 26th North Carolina Regiment participated in Pickett/Pettigrew's Charge and advanced the farthest into Union lines of any Confederate regiment. During the Battle of Chickamauga, the 58th North Carolina Regiment advanced farther than any other regiment on Snodgrass Hill to push back the remaining Union forces from the battlefield. At Appomattox Court House in Virginia in April 1865, the 75th North Carolina Regiment, a cavalry unit, fired the last shots of the Confederate Army of Northern Virginia in the Civil War.  The phrase "First at Bethel, Farthest at Gettysburg and Chickamauga, and Last at Appomattox", later became used through much of the early 20th century.


After the Spanish in the 16th century, the first permanent European settlers of North Carolina were English colonists who migrated south from Virginia. The latter had grown rapidly and land was less available. Nathaniel Batts was documented as one of the first of these Virginian migrants. He settled south of the Chowan River and east of the Great Dismal Swamp in 1655. By 1663, this northeastern area of the Province of Carolina, known as the Albemarle Settlements, was undergoing full-scale English settlement. During the same period, the English monarch Charles II gave the province to the Lords Proprietors, a group of noblemen who had helped restore him to the throne in 1660. The new Province of Carolina was named in honor and memory of his father, Charles I (Latin: Carolus). A large revolt happened in the state in 1711, known as Cary's Rebellion. In 1712, North Carolina became a separate colony. Except for the Earl Granville holdings, it became a royal colony seventeen years later.
In June 1718, the pirate Blackbeard ran his flagship, the Queen Anne's Revenge, aground at Beaufort Inlet, North Carolina, in present-day Carteret County. After the grounding her crew and supplies were transferred to smaller ships. In November 1718, after appealing to the governor of North Carolina, who promised safe-haven and a pardon, Blackbeard was killed in an ambush by troops from Virginia. In 1996 Intersal, Inc., a private firm, discovered the remains of a vessel likely to be the Queen Anne's Revenge, which was added to the U.S. National Register of Historic Places.
North Carolina became one of the English Thirteen Colonies and with the territory of South Carolina was originally known as the Province of North Carolina. The northern and southern parts of the original province separated in 1712, with North Carolina becoming a royal colony in 1729. Originally settled by small farmers, sometimes having a few slaves, who were oriented toward subsistence agriculture, the colony lacked large cities or towns. Pirates menaced the coastal settlements, but by 1718 the pirates had been captured and killed. Growth was strong in the middle of the 18th century, as the economy attracted Scots-Irish, Quaker, English and German immigrants. A majority of the North Carolina colonists generally supported the American Revolution, although there were some Loyalists. Loyalists in North Carolina were smaller in number than in some other colonies such as Georgia, South Carolina, Delaware, and New York.
During colonial times, Edenton served as the state capital beginning in 1722, followed by New Bern becoming the capital in 1766. Construction of Tryon Palace, which served as the residence and offices of the provincial governor William Tryon, began in 1767 and was completed in 1771. In 1788, Raleigh was chosen as the site of the new capital, as its central location protected it from coastal attacks. Officially established in 1792 as both county seat and state capital, the city was named after Sir Walter Raleigh, sponsor of Roanoke, the "lost colony" on Roanoke Island. The population of the colony more than quadrupled from 52,000 in 1740 to 270,000 in 1780 from high immigration from Virginia, Maryland and Pennsylvania, plus immigrants from abroad.
North Carolina did not have any printer or print shops  until 1749, when the North Carolina Assembly commissioned James Davis from Williamsburg Virginia to act as their official printer.  Before this time the laws and legal journals of North Carolina were handwritten and were largely kept in a disorganized manner, prompting them to hire Davis. Davis settled in New Bern, became married and in 1755 was appointed by Benjamin Franklin as North Carolina's first postmaster. In October of that year the North Carolina Assembly awarded Davis the contract to carry the mail between Wilmington, North Carolina and Suffolk, Virginia. He was also  active in North Carolina's politics, as a member of the Assembly and later as the Sheriff. Davis also founded and printed the North-Carolina Gazette, North Carolina's first newspaper, printed in his printing house in New Bern.
Differences in the settlement patterns of eastern and western North Carolina, or the Atlantic coastal plain and uplands, affected the political, economic, and social life of the state from the 18th until the 20th century. Eastern North Carolina was settled chiefly by immigrants from rural England and Gaelic speakers from the Scottish Highlands. The Piedmont upcountry and western mountain region of North Carolina was settled chiefly by Scots-Irish, English, and German Protestants, the so-called "cohee". Arriving during the mid-to-late 18th century, the Scots-Irish, people of Scottish descent who migrated to and then emigrated from what is today Northern Ireland, were the largest non-English immigrant group before the Revolution; English indentured servants were overwhelmingly the largest immigrant group before the Revolution.
During the American Revolutionary War, the English and Gaelic speaking Highland Scots of eastern North Carolina tended to remain loyal to the British Crown, because of longstanding business and personal connections with Great Britain. The English, Welsh, Scots-Irish, and German settlers of western North Carolina tended to favor American independence from Britain. On April 12, 1776, the colony became the first to instruct its delegates to the Continental Congress to vote for independence from the British Crown, through the Halifax Resolves passed by the North Carolina Provincial Congress. The date of this event is memorialized on the state flag and state seal. Throughout the Revolutionary War, fierce guerrilla warfare erupted between bands of pro-independence and pro-British colonists. In some cases the war was also an excuse to settle private grudges and rivalries.


In 1584, Elizabeth I granted a charter to Sir Walter Raleigh, for whom the state capital is named, for land in present-day North Carolina (then part of the territory of Virginia). It was the second American territory which the English attempted to colonize. Raleigh established two colonies on the coast in the late 1580s, but both failed. The fate of the "Lost Colony" of Roanoke Island remains one of the most widely debated mysteries of American history. Virginia Dare, the first English child to be born in North America, was born on Roanoke Island on August 18, 1587; Dare County is named for her.
As early as 1650, settlers from the Virginia colony had moved into the area of Albemarle Sound. By 1663, King Charles II of England granted a charter to start a new colony on the North American continent; this would generally establish North Carolina's borders. He named it Carolina in honor of his father, Charles I. By 1665, a second charter was issued to attempt to resolve territorial questions. In 1712 owing to disputes over governance, the Carolina colony split into North Carolina and South Carolina. North Carolina would become a crown colony in 1729.
Most of the English colonists had arrived as indentured servants, hiring themselves out as laborers for a fixed period to pay for their passage. In the early years the line between indentured servants and African slaves or laborers was fluid. Some Africans were allowed to earn their freedom before slavery became a lifelong status. Most of the free colored families formed in North Carolina before the Revolution were descended from unions or marriages between free white women and enslaved or free African or African-American men. Because the mothers were free, their children were born free. Many had migrated or were descendants of migrants from colonial Virginia. As the flow of indentured laborers to the colony decreased with improving economic conditions in Great Britain, planters imported more slaves, and the state's legal delineations between free and slave status tightened, effectively hardening the latter into a racial caste. The economy's growth and prosperity was based on slave labor, devoted primarily to the production of tobacco.
In 1738–1739, smallpox would cause high fatalities among the Native Americans, who had no immunity to the new disease (it had become endemic over centuries in Europe). According to the historian Russell Thornton, "The 1738 epidemic was said to have killed one-half of the Cherokee, with other tribes of the area suffering equally."


Following the collapse of the Confederacy in 1865, North Carolina, along with other former Confederate States (except Tennessee), was put under direct control by the U.S. military and was relieved of its constitutional government and representation within the United States Congress in what is now referred to as the Reconstruction era. In order to earn back its rights, the state had to make concessions to Washington, one of which was ratifying the Thirteenth Amendment. Congressional Republicans during Reconstruction, commonly referred to as "radical Republicans", constantly pushed for new constitutions for each of the Southern states that emphasized equal rights for African-Americans. In 1868, a constitutional convention restored the state government of North Carolina. Though the Fifteenth Amendment was also adopted that same year, it remained in most cases ineffective for almost a century, not to mention paramilitary groups and their lynching with impunity.
The elections in April 1868 following the constitutional convention led to a narrow victory for a Republican-dominated government, with 19 African-Americans holding positions in the North Carolina State Legislature. In attempt to put the reforms into effect, the new Republican Governor William W. Holden declared martial law on any county allegedly not complying with law and order using the passage of the Shoffner Act.
A Republican Party coalition of black freedmen, northern carpetbaggers and local scalawags controlled state government for three years. The white conservative Democrats regained control of the state legislature in 1870, in part by Ku Klux Klan violence and terrorism at the polls, to suppress black voting. Republicans were elected to the governorship until 1876, when the Red Shirts, a paramilitary organization that arose in 1874 and was allied with the Democratic Party, helped suppress black voting. More than 150 black Americans were murdered in electoral violence in 1876.
Post civil war-debt cycles pushed people to switch from subsistence agriculture to commodity agriculture. Among this time the notorious Crop-Lien system developed and was financially difficult on landless whites and blacks, due to high amounts of usury. Also due to the push for commodity agriculture, the free range was ended. Prior to this time people fenced in their crops and had their livestock feeding on the free range areas. After the ending of the free range people now fenced their animals and had their crops in the open.
Democrats were elected to the legislature and governor's office, but the Populists attracted voters displeased with them. In 1896 a biracial, Populist-Republican Fusionist coalition gained the governor's office and passed laws that would extend the voting franchise to blacks and poor whites. The Democrats regained control of the legislature in 1896 and passed laws to impose Jim Crow and racial segregation of public facilities. Voters of North Carolina's 2nd congressional district elected a total of four African-American congressmen through these years of the late 19th century.
Political tensions ran so high a small group of white Democrats in 1898 planned to take over the Wilmington government if their candidates were not elected. In the Wilmington Insurrection of 1898, more than 1,500 white men attacked the black newspaper and neighborhood, killed an estimated 60 to 300 people, and ran off the white Republican mayor and aldermen. They installed their own people and elected Alfred M. Waddell as mayor, in the only coup d'état in United States history.
In 1899, the state legislature passed a new constitution, with requirements for poll taxes and literacy tests for voter registration which disenfranchised most black Americans in the state. Exclusion from voting had wide effects: it meant black Americans could not serve on juries or in any local office. After a decade of white supremacy, many people forgot North Carolina had ever had thriving middle-class black Americans. Black citizens had no political voice in the state until after the federal Civil Rights Act of 1964 and Voting Rights Act of 1965 were passed to enforce their constitutional rights. It was not until 1992 that another African American was elected as a U.S. Representative from North Carolina.


After 1800, cotton and tobacco became important export crops. The eastern half of the state, especially the Coastal Plain region, developed a slave society based on a plantation system and slave labor. Planters owning large estates wielded significant political and socio-economic power in antebellum North Carolina. They placed their interests above those of the generally non-slave-holding "yeoman" farmers of North Carolina. While slaveholding was slightly less concentrated compared to some other Southern states, according to the 1860 census, more than 330,000 people, or 33% of the population out of 992,622 people in total, were enslaved African Americans. They lived and worked chiefly on plantations in the Piedmont and Coastal Plain regions of the state. In addition, 30,463 free people of color lived in the state. They were also mainly concentrated in the eastern coastal plain, especially at port cities such as Wilmington and New Bern, where a variety of jobs were available. Most were descendants from free African Americans who had migrated along with neighbors from Virginia during the 18th century. The majority were the descendants of unions in the working classes between white women, indentured servants or free, and African men, indentured, slave or free.
After the American Revolution, Quakers and Mennonites worked to persuade slaveholders to free their slaves. Some were inspired by their efforts and the language of the Revolution to arrange for manumission of their slaves. The number of free people of color rose markedly in the first couple of decades after the Revolution. Many free people of color migrated to the frontier, along with their European-American neighbors, where the social system was looser. By 1810, nearly three percent of the free population consisted of free people of color, who numbered slightly more than 10,000. The western areas of North Carolina were mainly white families of European descent, especially Scotch-Irish, who operated small subsistence farms. In the early national period, the state became a center of Jeffersonian and Jacksonian democracy, with a strong Whig presence, especially in the western part of the state. After Nat Turner's slave uprising in 1831, North Carolina and other southern states reduced the rights of free blacks. In 1835, the legislature withdrew their right to vote.
In mid-century, the state's rural and commercial areas were connected by the construction of a 129 mi (208 km) wooden plank road, known as a "farmer's railroad", from Fayetteville in the east to Bethania (northwest of Winston-Salem). On October 25, 1836, construction began on the Wilmington and Raleigh Railroad to connect the port city of Wilmington with the state capital of Raleigh. In 1840, the state capitol building in Raleigh was completed, and still stands today.
In 1849, the North Carolina Railroad was created by act of the legislature to extend that railroad west to Greensboro, High Point, and Charlotte. During the Civil War, the Wilmington-to-Raleigh stretch of the railroad would be vital to the Confederate war effort; supplies shipped into Wilmington would be moved by rail through Raleigh to the Confederate capital of Richmond, Virginia.


North Carolina (/ˌkærəˈlaɪnə/ (listen)) is a state in the Southeastern region of the United States. The state is the 28th largest and 9th-most populous of the 50 United States. It is bordered by Virginia to the north, the Atlantic Ocean to the east, Georgia and South Carolina to the south, and Tennessee to the west. Raleigh is the state's capital and Charlotte is its largest city. The Charlotte metropolitan area, with a population of 2,595,027 in 2020, is the most-populous metropolitan area in North Carolina, the 21st-most populous in the United States, and the largest banking center in the nation after New York City. The Raleigh-Durham-Cary combined statistical area is the second-largest metropolitan area in the state and 32nd-most populous in the United States, with a population of 2,043,867 in 2020, and is home to the largest research park in the United States, Research Triangle Park.
The earliest evidence of human occupation in North Carolina dates back 10,000 years, found at the Hardaway Site. North Carolina was inhabited by Carolina Algonquian, Iroquoian, and Siouan speaking tribes of Native Americans prior to the arrival of Europeans. North Carolina was established as a royal colony in 1729 and was one of the Thirteen Colonies. North Carolina is named in honor of King Charles I of England who first formed the English colony, Carolus being Latin for "Charles". In 1755 colonial North Carolina received its first postmaster, James Davis, appointed by Benjamin Franklin.  The Halifax Resolves resolution adopted by North Carolina on April 12, 1776, was the first formal call for independence from Great Britain among the American Colonies during the American Revolution.
On November 21, 1789, North Carolina became the 12th state to ratify the United States constitution. In the run-up to the American Civil War, North Carolina declared its secession from the Union on May 20, 1861, becoming the tenth of eleven states to join the Confederate States of America. Following the Civil War, the state was restored to the Union on July 4, 1868. On December 17, 1903, Orville and Wilbur Wright successfully piloted the world's first controlled, sustained flight of a powered, heavier-than-air aircraft at Kitty Hawk in North Carolina's Outer Banks. North Carolina uses the slogan "First in Flight" on state license plates to commemorate this achievement, alongside a newer alternative design bearing the slogan "First in Freedom" in reference to the Mecklenburg Declaration and Halifax Resolves.
North Carolina is defined by a wide range of elevations and landscapes. From west to east, North Carolina's elevation descends from the Appalachian Mountains to the Piedmont and Atlantic coastal plain. North Carolina's Mount Mitchell at 6,684 feet (2,037 m) is the highest point in North America east of the Mississippi River. Most of the state falls in the humid subtropical climate zone; however, the western, mountainous part of the state has a subtropical highland climate.


Coahuila is subdivided into five regions and 38 municipalities (municipios).


Coahuila ([koaˈwila] (listen)), formally Coahuila de Zaragoza (American Spanish: [koaˈwila ðe saɾaˈɣosa] (listen)), officially the Free and Sovereign State of Coahuila de Zaragoza (Spanish: Estado Libre y Soberano de Coahuila de Zaragoza), is one of the 32 states of Mexico.
Coahuila borders the Mexican states of Nuevo León to the east, Zacatecas to the south, and Durango and Chihuahua to the west. To the north, Coahuila accounts for a 512 kilometres (318 mi) stretch of the Mexico–United States border, adjacent to the U.S. state of Texas along the course of the Rio Grande (Río Bravo del Norte). With an area of 151,563 square kilometres (58,519 sq mi), it is the nation's third-largest state. It comprises 38 municipalities (municipios). In 2020, Coahuila's population is 3,146,771 inhabitants.
The largest city and State Capital is the city of Saltillo; the second largest is Torreón (largest metropolitan area in Coahuila and 9th largest in Mexico); the third largest is Monclova (a former state capital); the fourth largest is Ciudad Acuña; and the fifth largest is Piedras Negras.


Basic education
Basic public education in Coahuila is mainly managed by the state's Secretary of Education, but federal-sustained schools are also very common. There are also a lot of private schools in the main cities of the state.
Higher education
Some of the most recognized universities in Coahuila include:
Iberoamerican University of Torreón|Iberoamerican University (Universidad Iberoamericana)
A private university part of the Jesuit University System with a campus in Torreón and a university extension center in Saltillo.
Technological Institute of La Laguna (Instituto Tecnológico de la Laguna)
The most recognized public technological university of La Laguna Region located in the city of Torreón.
Technological Institute of Saltillo (Instituto Tecnológico de Saltillo)
Monterrey Institute Of Technology and Higher Studies
It is the most known technological university in Mexico with two campuses: one in Saltillo and another one in Torreón.
Autonomous University of La Laguna
Antonio Narro Agrarian Autonomous University (UAAAN)
Autonomous University of Coahuila (Universidad Autónoma de Coahuila)
It is considered the best public university of the states and it has campuses and schools all across Coahuila.


Cismontane chaparral ("this side of the mountain") refers to the chaparral ecosystem in the Mediterranean forests, woodlands, and scrub biome in California, growing on the western (and coastal) sides of large mountain range systems, such as the western slopes of the Sierra Nevada in the San Joaquin Valley foothills, western slopes of the Peninsular Ranges and California Coast Ranges, and south-southwest slopes of the Transverse Ranges in the Central Coast and Southern California regions.


In its natural state, chaparral is characterized by infrequent fires, with natural fire return intervals ranging between 30 years and over a hundred years. Mature chaparral (at least 50 years since time of last fire) is characterized by nearly impenetrable, dense thickets (except the more open chaparral of the desert).  These plants are flammable during the late summer and autumn months when conditions are characteristically hot and dry.  They grow as woody shrubs with thick, leathery, and often small leaves, contain green leaves all year (are evergreen), and are typically drought resistant (with some exceptions).  After the first rains following a fire, the landscape is dominated by small flowering herbaceous plants, known as fire followers, which die back with the summer dry period.
Similar plant communities are found in the four other Mediterranean climate regions around the world, including the Mediterranean Basin (where it is known as maquis), central Chile (where it is called matorral), the South African Cape Region (known there as fynbos), and in Western and Southern Australia (as kwongan).  According to the California Academy of Sciences, Mediterranean shrubland contains more than 20 percent of the world's plant diversity. The word chaparral is a loanword from Spanish chaparro, meaning place of the scrub oak, which itself comes from a Basque word, txapar, that has the same meaning.
Conservation International and other conservation organizations consider chaparral to be a biodiversity hotspot – a biological community with a large number of different species – that is under threat by human activity.


Chaparral (/ˌʃæpəˈræl, ˌtʃæp-/ SHAP-ə-RAL, CHAP-) is a shrubland plant community and geographical feature found primarily in the U.S. state of California, in southern Oregon, and in the northern portion of the Baja California Peninsula in Mexico. It is shaped by a Mediterranean climate (mild wet winters and hot dry summers) and infrequent, high-intensity crown fires. Chaparral features summer-drought-tolerant plants with hard sclerophyllous evergreen leaves, as contrasted with the associated soft-leaved, drought-deciduous, scrub community of coastal sage scrub, found often on drier, southern facing slopes within the chaparral biome. Three other closely related chaparral shrubland systems occur in central Arizona, western Texas, and along the eastern side of central Mexico's mountain chains (mexical), all having summer rains in contrast to the Mediterranean climate of other chaparral formations. Chaparral comprises 9% of California's wildland vegetation and contains 20% of its plant species. The name comes from the Spanish word chaparro, which translates to "place of the scrub oak".


For the numerous individual plant and animal species found within the California chaparral and woodlands ecoregion, see:
Flora of the California chaparral and woodlands
Fauna of the California chaparral and woodlands.
Some of the indicator plants of the California chaparral and woodlands ecoregion include:
Quercus species – oaks:
Quercus agrifolia – coast live oak
Quercus berberidifolia – scrub oak
Quercus chrysolepis – canyon live oak
Quercus douglasii – blue oak
Quercus wislizeni – interior live oak
Artemisia species – sagebrush:
Artemisia californica – California sagebrush,  coastal sage brush
Arctostaphylos species – manzanitas:
Arctostaphylos glauca – bigberry manzanita
Arctostaphylos manzanita – common manzanita
Ceanothus species – California lilacs:
Ceanothus cuneatus – buckbrush
Ceanothus megacarpus – bigpod ceanothus
Rhus species – sumacs:
Rhus integrifolia – lemonade berry
Rhus ovata – sugar bush
Eriogonum species – buckwheats:
Eriogonum fasciculatum – California buckwheat
Salvia species – sages:
Salvia mellifera – black sage
Chaparral soils and nutrient composition
Chaparral characteristically is found in areas with steep topography and shallow stony soils, while adjacent areas with clay soils, even where steep, tend to be colonized by annual plants and grasses.  Some chaparral species are adapted to nutrient-poor soils developed over serpentine and other ultramafic rock, with a high ratio of magnesium and iron to calcium and potassium, that are also generally low in essential nutrients such as nitrogen.


The complex ecology of chaparral habitats supports a very large number of animal species. The following is a short list of birds which are an integral part of the cismontane chaparral ecosystems.
Characteristic chaparral bird species include:
Wrentit (Chamaea fasciata)
California thrasher (Toxostoma redivivum)
California towhee (Melozone crissalis)
Spotted towhee (Pipilo maculatus)
California scrub jay (Aphelocoma californica)
Other common chaparral bird species include:
Anna's hummingbird (Calypte anna)
Bewick's wren (Thryomanes bewickii)
Bushtit (Psaltriparus minimus)
Costa's hummingbird (Calypte costae)
Greater roadrunner (Geococcyx californianus)


The California chaparral and woodlands ecoregion, of the Mediterranean forests, woodlands, and scrub biome, has three sub-ecoregions with ecosystem—plant community subdivisions:
California coastal sage and chaparral:
In coastal Southern California and northwestern coastal Baja California, as well as all of the Channel Islands off California and Guadalupe Island (Mexico).
California montane chaparral and woodlands:
In southern and central coast adjacent and inland California regions, including covering some of the mountains of the California Coast Ranges, the Transverse Ranges, and the western slopes of the northern Peninsular Ranges.
California interior chaparral and woodlands:
In central interior California surrounding the Central Valley, covering the foothills and lower slopes of the northeastern Transverse Ranges and the western Sierra Nevada range.


The Sonoran desert has an arid subtropical climate. In the lower-elevation portions of the desert, temperatures are warm year-round, and rainfall is infrequent and irregular, often less than 90 mm annually. The Arizona uplands are also warm year-round, but they receive 100–300 mm of average annual rainfall, which falls in a more regular bi-seasonal pattern.


The desert's sub-regions include the Colorado Desert of southeastern California; and the Yuma Desert east of the north-to-south section of the Colorado River in southwest Arizona. In the 1957 publication Vegetation of the Sonoran Desert, Forrest Shreve divided the Sonoran Desert into seven regions according to characteristic vegetation: Lower Colorado Valley, Arizona Upland, Plains of Sonora, Foothills of Sonora, Central Gulf Coast, Vizcaíno Region, and Magdalena Region. Many ecologists consider Shreve's Vizcaíno and Magdalena regions, which lie on the western side of the Baja California Peninsula, to be a separate ecoregion, the Baja California Desert.
Within the southern Sonoran Desert in Mexico is found the Gran Desierto de Altar, with the El Pinacate y Gran Desierto de Altar Biosphere Reserve, extending 2,000 square kilometers (770 sq mi) of desert and mountainous regions. The biosphere reserve includes the only active erg dune region in North America. The nearest city to the biosphere reserve is Puerto Peñasco ('Rocky Point') in the state of Sonora, Mexico.
Sub-regions
Sonoran Desert sub-regions include:
Colorado Desert
Gran Desierto de Altar
Lechuguilla Desert
Tonopah Desert
Yuha Desert
Yuma Desert


Many plants not only survive, but thrive in the harsh conditions of the Sonoran Desert. Many have evolved to have specialized adaptations to the desert climate. The Sonoran Desert's bi-seasonal rainfall pattern results in more plant species than any other desert in the world. The Sonoran Desert includes  plant genera and species from the agave family, palm family, cactus family, legume family, and numerous others.
The Sonoran is the only place in the world where the famous saguaro cactus  (Carnegiea gigantea) grows in the wild. Cholla (Cylindropuntia spp.), beavertail (Opuntia basilaris), hedgehog (Echinocereus spp.), fishhook (Ferocactus wislizeni), prickly pear (Opuntia spp.), nightblooming cereus (Peniocereus spp.), and organ pipe (Stenocereus thurberi) are other taxa of cacti found here. Cactus provides food and homes to many desert mammals and birds, with showy flowers in reds, pinks, yellows, and whites, blooming most commonly from late March through June, depending on the species and seasonal temperatures.
Creosote bush (Larrea tridentata) and bur sage (Ambrosia dumosa) dominate valley floors. Indigo bush (Psorothamnus fremontii) and Mormon tea are other shrubs that may be found. Wildflowers of the Sonoran Desert include desert sand verbena (Abronia villosa), desert sunflower (Geraea canescens), and evening primroses.
Ascending from the valley up bajadas, various subtrees such as velvet mesquite (Prosopis velutina), palo verde (Parkinsonia florida), desert ironwood (Olneya tesota), desert willow (Chilopsis linearis ssp. arcuata), and crucifixion thorn (Canotia holacantha) are common, as well as multi-stemmed ocotillo (Fouquieria splendens). Shrubs found at higher elevations include whitethorn acacia (Acacia constricta), fairy duster, and jojoba. In the desert subdivisions found on Baja California, cardon cactus, elephant tree, and boojum tree occur.
The California fan palm (Washingtonia filifera) is found in the Colorado Desert section of the Sonoran Desert, the only native palm in California, among many other introduced Arecaceae genera and species. It is found at spring-fed oases, such as in Anza Borrego Desert State Park, Joshua Tree National Park, and the Kofa National Wildlife Refuge.


The Sonoran desert wraps around the northern end of the Gulf of California, from Baja California Sur (El Vizcaíno Biosphere Reserve in central and Pacific west coast, Central Gulf Coast subregion on east to southern tip), north through much of Baja California, excluding the central northwest mountains and Pacific west coast, through southeastern California and southwestern and southern Arizona to western and central parts of Sonora.
It is bounded on the west by the Peninsular Ranges, which separate it from the California chaparral and woodlands (northwest) and Baja California Desert (Vizcaino subregion, central and southeast) ecoregions of the Pacific slope. The Gulf of California xeric scrub ecoregion lies south of the Sonoran desert on the Gulf of California slope of the Baja California Peninsula.
To the north in California and northwest Arizona, the Sonoran Desert transitions to the colder-winter, higher-elevation Mojave, Great Basin, and Colorado Plateau deserts.
To coniferous Arizona Mountains forests are to the northeast. The Chihuahuan Desert and Sierra Madre Occidental pine–oak forests are at higher elevations to the east. To the south the Sonoran–Sinaloan transition subtropical dry forest is the transition zone from the Sonoran Desert to the tropical dry forests of the Mexican state of Sinaloa.


The Sonoran Desert is home to the cultures of over 17 contemporary Native American tribes, with settlements at  American Indian reservations in California and Arizona, as well as populations in Mexico.
The largest city in the Sonoran Desert is Phoenix, Arizona, with a 2017 metropolitan population of about 4.7 million. Located on the Salt River in central Arizona, it is one of the fastest-growing metropolitan areas in the United States. In 2007 in the Phoenix area, desert was losing ground to urban sprawl at a rate of approximately 4,000 square meters (1 acre) per hour.
The next largest cities are Tucson, in southern Arizona, with a metro area population of just over 1 million, and Mexicali, Baja California, with a similarly sized metropolitan population of around 1,000,000. The metropolitan area of Hermosillo, Sonora, has a population close to 900,000. Ciudad Obregón, Sonora, in the southern part of the desert, has a population of 375,800.


The Sonoran Desert is home to a wide variety of animals, birds and other creatures. such as the Gila monster, bobcat, mule deer, antelope jackrabbit, burrowing owl, greater roadrunner, western diamondback rattlesnake, and elf owl. There are three hundred fifty bird species, 20 amphibian species, over 100 reptile species, 30 native fish species, over 1000 native bee species, and more than 2,000 native plant species found in the desert area. The Sonoran Desert area southeast of Tucson and near the Mexican border is vital habitat for the only population of jaguars living within the United States.  The Colorado River Delta was once an ecological hotspot within the Sonoran desert due to the Colorado river in this otherwise dry area, but the delta has been greatly reduced in extent due to the damming and use of the river upstream. Species that have higher heat tolerance are able to thrive in the conditions of the Sonoran Desert. One such insect species that has evolved a means to thrive in this environment is Drosophila mettleri, a Sonoran Desert fly. This fly contains a specialized P450 detoxification system that enables it to nest in the cool region of exudate moistened soil. Thus, the fly is one of few that can tolerate the high desert temperatures and successfully reproduce.


The Coachella Valley, located in the Colorado Desert section of the Sonoran Desert, has a population of 365,000. Several famous Southern California desert resort cities such as Palm Springs and Palm Desert are located here.
During the winter months, from November to April, the daytime temperatures in the Coachella Valley range from 70 °F (21 °C) to 90 °F (32 °C) and corresponding nighttime lows range from 46 °F (8 °C) to 68 °F (20 °C) making it a popular winter resort destination. Due to its warm year-round climate citrus and subtropical fruits such as mangoes, figs, and dates are grown in the Coachella Valley and adjacent Imperial Valley. The Imperial Valley has a total population of over 180,000 and has a similar climate to that of the Coachella Valley. Other cities include Borrego Springs, Indio, Coachella, Calexico, El Centro, Imperial, and Blythe.


1766 (MDCCLXVI) was a common year starting on Wednesday of the Gregorian calendar and a common year starting on Sunday of the Julian calendar, the 1766th year of the Common Era (CE) and Anno Domini (AD) designations, the 766th  year of the 2nd millennium, the 66th  year of the 18th century, and the  7th   year of the 1760s decade. As of the start of 1766, the Gregorian calendar was 11 days ahead of the Julian calendar, which remained in localized use until 1923.


January 1 – Charles Edward Stuart ("Bonnie Prince Charlie") becomes the new Stuart claimant to the throne of Great Britain, as King Charles III, and figurehead for Jacobitism.
January 14 – Christian VII becomes King of Denmark.
January 20 – Outside of the walls of the Thailand capital of Ayutthaya, tens of thousands of invaders from Burma (under the command of General Ne Myo Thihapate and General Maha Nawatra) are confronted by Thai defenders led by General Phya Taksin. The defenders are overwhelmed and the survivors take refuge inside Ayutthaya. The siege continues for 15 months before the Burmese attackers collapse the walls by digging tunnels and setting fire to debris. The city falls on April 9, 1767, and King Ekkathat is killed.
February 5 – An observer in Wilmington, North Carolina reports to the Edinburgh newspaper Caledonian Mercury that three ships have been seized by British men-of-war, on the charge of carrying official documents without stamps. The strict enforcement causes seven other ships to leave Wilmington for other ports.
February 13 – John Mills is elected a Fellow of the Royal Society, with Benjamin Franklin as one of his sponsors.
February 15 – Protesting against the Stamp Act 1765, members of the New York City Sons of Liberty travel to Pennsylvania and set fire to a British supply of tax stamps before the stamps can be taken to distributors in the province of Maryland.
February 18 – Meermin Slave Mutiny: Captive Malagasy people seize a Dutch East India Company slave ship in the Indian Ocean.
February 20 – The Pennsylvania Gazette reports that a British sloop off Wilmington, North Carolina, has seized a sloop sailing from Philadelphia, and another sailing from Saint Christopher, on the charge of carrying official documents without stamps. In response, local residents threaten to burn a Royal Man-of-War attempting to deliver stamps to Wilmington, forcing the ship to return to the mouth of the Cape Fear River.
February 23 – Lorraine becomes French again, on the death of Stanisław Leszczyński, King of Poland and last Duke of Lorraine.
February – Ferocious wolf attacks occur in France, such as the Beast of Gévaudan or Wolves of Périgord.
March 5 – Antonio de Ulloa, the first Spanish governor of Louisiana, arrives in New Orleans.
March 18 – American Revolution: The British Parliament repeals the Stamp Act, which has been very unpopular in the British colonies; the persuasion of Benjamin Franklin is considered partly responsible. The Declaratory Act asserts the right of Britain to bind the colonies in all other respects.


July 1 – François-Jean de la Barre, a young French nobleman, is tortured and beheaded, before his body is burnt on a pyre, along with a copy of Voltaire's Dictionnaire philosophique nailed to his torso, for the crime of not saluting a Roman Catholic religious procession in Abbeville, and for other sacrileges, including desecrating a crucifix.
August 10 – During the occupation of New York, members of the 28th Foot Regiment of the British Army chop down the liberty pole that was erected by the Sons of Liberty on June 4. The Sons of Liberty put up a second pole the next day, and that pole is cut down on August 22.
August 13 – A hurricane sweeps across the French island colony of Martinique, killing more than 400 people and destroying the plantation owned by Joseph-Gaspard de La Pagerie, the father of the future French Empress Joséphine.
September 1 – The revolt in Quito (at this time part of Spain's  Viceroyalty of Nueva Granada; the modern-day capital of Ecuador) is ended peacefully as royal forces enter the city under the command of Guayaquil Governor Pedro Zelaya. Rather than seeking retribution from the Quito citizens over their insurrection that has broken the monopoly over the sale of the liquor aguardiente, Zeleaya oversees a program of reconciliation.
September 13 – The position of Patriarch of the Serbs, established on April 9, 1346 as the authority over the Serbian Orthodox Church, is abolished by order of Sultan Mustafa III of the Ottoman Empire; the patriarchate is not re-established until 1920 following the creation of Yugoslavia at the end of World War One.
September 23 – John Penn, the Colonial Governor of Pennsylvania and one of the four Penn family owners of the Pennsylvania land grant, issues a proclamation forbidding British American colonist residents from building settlements on lands in the west "not yet purchased of the Nations" of the Iroquois Indians.


October 1 – Crown Prince Gustav of Sweden weds Princess Sophia Magdalena of Denmark. They become King Gustav III and Queen Consort Sophia of Sweden upon his ascension to the throne in 1771.
October 4 – France formally cedes its rights to the Malouines Islands to Spain. On March 24, Spain renames the islands the Malvinas, and in 1833, the United Kingdom re-colonises the recently abandoned territory and renames it the Falkland Islands.
November – Raja Lumu consolidates his claim to the Selangor Sultanate by marriage to the niece of the Sultan of Perak.
November 10 – The last Colonial governor of New Jersey, William Franklin, signs the charter of Queen's College (later renamed Rutgers University).
November 27 – A British sloop-of-war is searching all vessels passing near Cape Lookout, North Carolina, and some vessels have been seized, according to an observer in New York City, in the Province of New York, reporting to the Pennsylvania Gazette.
November 29 – Wolfgang Amadeus Mozart returns to Salzburg, after the Mozart family grand tour of Europe.
December 2 – The Law on the Freedom of Printing abolishes censorship in Sweden and guarantees freedom of the press, making Sweden the first country of the world to introduce constitutional protection of press freedom, and to pass wide-ranging freedom of information legislation.
December 5 – James Christie holds the first sale at Christie's auction house in London.
December 25 – Mapuches in Chile launch a series of surprise attacks against the Spanish starting the Mapuche uprising of 1766.


This family is cosmopolitan and can be found worldwide except in the Antarctic region. Some species, such as the setaceous Hebrew character (Xestia c-nigrum), can be found in the Arctic Circle, specifically in the Yukon territory of western Canada, with an elevation 1,702 m above sea level, where the temperature fluctuates between 23/-25 °C (73/-13 °F). Many species of dart moths have been recorded in elevations as high as 4,000 m above sea level (e.g. Xestia elisabetha).
Among the places where the number of species has been counted are North America and northern Mexico, with about 2,522 species. 1,576 species are found in Europe, while the other species are distributed worldwide.


The Noctuidae, commonly known as owlet moths, cutworms or armyworms, are a family of moths. They are considered the most controversial family in the superfamily Noctuoidea because many of the clades are constantly changing, along with the other families of the Noctuoidea. It was considered the largest family in Lepidoptera for a long time, but after regrouping Lymantriinae, Catocalinae and Calpinae within the family Erebidae, the latter holds this title now. Currently, Noctuidae is the second largest family in Noctuoidea, with about 1,089 genera and 11,772 species. This classification is still contingent, as more changes continue to appear between Noctuidae and Erebidae.


Herbivory: Caterpillars of most Noctuidae feed on plants; some feed on poisonous plants and are unaffected by their chemical defences; for example, the splendid brocade moth (Lacanobia splendens) feeds on cowbane (Cicuta virosa), a plant that is notoriously toxic to vertebrates.
Predation and cannibalism: During the larval stage, some cutworms readily feed on other insects. One such species is the shivering pinion (Lithophane querquera), whose larvae commonly feed on other lepidopteran larvae. Moreover, many noctuid larvae, such as those of the fall armyworm (Spodoptera frugiperda) and of genera such as Heliothis and Helicoverpa, aggressively eat their siblings and often other species of caterpillar.
Nectarivory and puddling: Like many Lepidoptera, many species of adult Noctuidae visit flowers for their nectar. They also seek other liquid food resources such as plant juices, honeydew, dung, urea and mud, among others.
As is common in members of the order Lepidoptera, courtship in many Noctuidae includes a set of movements in which the female evaluates the male's reproductive fitness.
Most noctuid moths produce pheromones that attract the opposite gender. Female pheromones that attract males occur widely and have long been studied, but the study of male pheromones has further to go.


The word Noctuidae is derived from the name of the type genus Noctua, which is the Latin name for the little owl, and the patronymic suffix -idae used typically to form taxonomic family names in animals.
The common name "owlet" originally means a small or young owl. The names "armyworms" and "cutworms" are based on the behavior of the larvae of this group, which can occur in destructive swarms and cut the stems of plants.


Adult: Most noctuid adults have drab wings, but some subfamilies, such as Acronictinae and Agaristinae, are very colorful, especially those from tropical regions (e.g. Baorisa hieroglyphica). They are characterized by a structure in the metathorax called the nodular sclerite or epaulette, which separates the tympanum and the conjunctiva in the tympanal organ. It functions to keep parasites (Acari) out of the tympanal cavity. Another characteristic in this group is trifine hindwing venation, by reduction or absence of the second medial vein (M2).
Markings present on the wings of noctuid adults can be helpful in distinguishing species.  From the basal location to the outer edge (proximal to distal) on the forewing, there is a claviform (club-shaped) stigma, horizontally oriented with the thicker end closer to the wing's outer edge, located posterior to a discal (round) stigma.  These are followed distally by a reniform (kidney-shaped) stigma, which is typically oriented with its concave side facing the wing's outer edge.  It is often not possible to discern all of the stigmata on all specimens or species.  Crossbands or crosslines may be present, oriented longitudinally from the leading to the trailing edge of the wing.
Larva: Commonly green or brown; some species present bright colors, such as the camphorweed cucullia moth (Cucullia alfarata). Most are pudgy and smooth with rounded short heads and few setae, but there are some exceptions in some subfamilies (e.g. Acronictinae and Pantheinae).
Pupa: The pupae most often range from shiny brown to dark brown. When they newly pupate they are bright brownish orange, but after a few days start to get darker.
Eggs: Vary in colors, but all have a spherical shape.


This group has a wide range of both chemical and physical defenses. Among the chemical defenses three types stand out. First, the pyrrolizidine alkaloid sequestration usually present in Arctiinae is also found in a few species of noctuids, including the Spanish moth (Xanthopastis timais). Another chemical defense is formic acid production, which was thought to be present only in Notodontidae, but later was found in caterpillars of Trachosea champa. Finally, the last type of chemical defense is regurgitation of plant compounds, often used by many insects, but the cabbage palm caterpillar (Litoprosopus futilis) produces a toxin called toluquinone that deters predators.
On the other hand, the main physical defense in caterpillars and adults alike is mimicry. Most owlet moths have drab colors with a variety of patterns suitable to camouflage their bodies. The second physical defense consists in thousands of secondary setae that surround the body. The subfamilies that present this mechanism are Pantheinae and Acronictinae. The third is aposematism, represented by species of Cucullinae. Finally, all adults have another mechanism for defense: a tympanal organ available to hear the echolocation spread out by bats, so the moths can avoid them.


Members of Noctuidae, like other butterflies and moths, perform an important role in plant pollination. Some species have developed a stronger connection with their host plants. For example, the lychnis moth (Hadena bicruris) has a strange mutualistic relationship with pink plants or carnation plants (Caryophyllaceae), in that larvae feed on the plant while the adults pollinate the flowers.


Other forms of the name are: Arabic: الجزائر, romanized: al-Jazāʾir, Algerian Arabic: الدزاير, romanized: al-dzāyīr; Berber languages: Lezzayer; Berber languages: ⵍⴻⵣⴰⵢⴻⵔ; Berber languages: لزّاير; French: Algérie. It is officially the People's Democratic Republic of Algeria (Arabic: الجمهورية الجزائرية الديمقراطية الشعبية, romanized: al-Jumhūriyya al-Jazāʾiriyya ad-Dīmuqrāṭiyya aš-Šaʿbiyya; Berber languages: Tagduda tamegdayt taɣerfant tazzayrit, Berber languages: ⵜⴰⴳⴷⵓⴷⴰ ⵜⴰⵎⴳⴷⴰⵢⵜ ⵜⴰⵖⵔⴼⴰⵏⵜ ⵜⴰⴷⵣⴰⵢⵔⵉⵢⵜ, Berber languages: تڨذوذا تازايريت تاماڨذايت تاغرفانت; French: République algérienne démocratique et populaire, abbreviated as RADP).


The number of European Pied-Noirs who fled Algeria totaled more than 900,000 between 1962 and 1964. The exodus to mainland France accelerated after the Oran massacre of 1962, in which hundreds of militants entered European sections of the city, and began attacking civilians.
Algeria's first president was the Front de Libération Nationale (FLN) leader Ahmed Ben Bella. Morocco's claim to portions of western Algeria led to the Sand War in 1963. Ben Bella was overthrown in 1965 by Houari Boumédiène, his former ally and defence minister. Under Ben Bella, the government had become increasingly socialist and authoritarian; Boumédienne continued this trend. But, he relied much more on the army for his support, and reduced the sole legal party to a symbolic role. He collectivised agriculture and launched a massive industrialisation drive. Oil extraction facilities were nationalised. This was especially beneficial to the leadership after the international 1973 oil crisis.
In the 1960s and 1970s under President Houari Boumediene, Algeria pursued a program of industrialisation within a state-controlled socialist economy. Boumediene's successor, Chadli Bendjedid, introduced some liberal economic reforms. He promoted a policy of Arabisation in Algerian society and public life. Teachers of Arabic, brought in from other Muslim countries, spread conventional Islamic thought in schools and sowed the seeds of a return to Orthodox Islam.
The Algerian economy became increasingly dependent on oil, leading to hardship when the price collapsed during the 1980s oil glut. Economic recession caused by the crash in world oil prices resulted in Algerian social unrest during the 1980s; by the end of the decade, Bendjedid introduced a multi-party system. Political parties developed, such as the Islamic Salvation Front (FIS), a broad coalition of Muslim groups.