Minnesota is a state in the Upper Midwest and northern regions of the United States. Minnesota was admitted as the 32nd U. S. state on May 11, 1858, created from the eastern half of the Minnesota Territory. The state has a large number of lakes, is known by the slogan the "Land of 10,000 Lakes", its official motto is L'Étoile du Nord. Minnesota is the 12th largest in area and the 22nd most populous of the U. S. states. This area is the center of transportation, industry and government, while being home to an internationally known arts community; the remainder of the state consists of western prairies now given over to intensive agriculture. Minnesota was inhabited by various indigenous peoples for thousands of years prior to the arrival of Europeans. French explorers and fur traders began exploring the region in the 17th century, encountering the Dakota and Ojibwe/Anishinaabe tribes. Much of what is today Minnesota was part of the vast French holding of Louisiana, purchased by the United States in 1803.
Following several territorial reorganizations, Minnesota in its current form was admitted as the country's 32nd state on May 11, 1858. Like many Midwestern states, it remained centered on lumber and agriculture. During the 19th and early 20th centuries, a large number of European immigrants from Scandinavia and Germany, began to settle the state, which remains a center of Scandinavian American and German American culture. In recent decades, immigration from Asia, the Horn of Africa, the Middle East, Latin America has broadened its demographic and cultural composition; the state's economy has diversified, shifting from traditional activities such as agriculture and resource extraction to services and finance. Minnesota's standard of living index is among the highest in the United States, the state is among the best-educated and wealthiest in the nation; the word Minnesota comes from the Dakota name for the Minnesota River: The river got its name from one of two words in the Dakota language,'Mní sóta' which means "clear blue water", or'Mnißota', which means cloudy water.
Native Americans demonstrated the name to early settlers by dropping milk into water and calling it mnisota. Many places in the state have similar names, such as Minnehaha Falls, Minneota, Minnetonka and Minneapolis, a combination of mni and polis, the Greek word for "city". Minnesota is the second northernmost U. S. state and northernmost contiguous state. Its isolated Northwest Angle in Lake of the Woods county is the only part of the 48 contiguous states lying north of the 49th parallel; the state is part of the U. S. region known as part of North America's Great Lakes Region. It shares a Lake Superior water border with Michigan and a land and water border with Wisconsin to the east. Iowa is to the south, North Dakota and South Dakota are to the west, the Canadian provinces of Ontario and Manitoba are to the north. With 86,943 square miles, or 2.25% of the United States, Minnesota is the 12th-largest state. Minnesota has gneisses that are about 3.6 billion years old. About 2.7 billion years ago, basaltic lava poured out of cracks in the floor of the primordial ocean.
The roots of these volcanic mountains and the action of Precambrian seas formed the Iron Range of northern Minnesota. Following a period of volcanism 1.1 billion years ago, Minnesota's geological activity has been more subdued, with no volcanism or mountain formation, but with repeated incursions of the sea, which left behind multiple strata of sedimentary rock. In more recent times, massive ice sheets at least one kilometer thick ravaged the state's landscape and sculpted its terrain; the Wisconsin glaciation left 12,000 years ago. These glaciers covered all of Minnesota except the far southeast, an area characterized by steep hills and streams that cut into the bedrock; this area is known as the Driftless Zone for its absence of glacial drift. Much of the remainder of the state outside the northeast has 50 feet or more of glacial till left behind as the last glaciers retreated. Gigantic Lake Agassiz formed in the northwest 13,000 years ago, its bed created the fertile Red River valley, its outflow, glacial River Warren, carved the valley of the Minnesota River and the Upper Mississippi downstream from Fort Snelling.
Minnesota is geologically quiet today. The state's high point is Eagle Mountain at 2,301 feet, only 13 miles away from the low of 601 feet at the shore of Lake Superior. Notwithstanding dramatic local differences in elevation, much of the state is a rolling peneplain. Two major drainage divides meet in Minnesota's northeast in rural Hibbing, forming a triple watershed. Precipitation can follow the Mississippi River south to the Gulf of Mexico, the Saint Lawrence Seaway east to the Atlantic Ocean, or the Hudson Bay watershed to the Arctic Ocean; the state's nickname, "Land of 10,000 Lakes", is apt, as there are 11,842 Minnesota lakes over 10 acres in size. Minnesota's portion of Lake Superior is the largest at 962,700 acres and deepest body of wate
U.S. Route 75
U. S. Route 75 is a major north–south U. S. Highway that extends 1,239 miles in the central United States; the highway's northern terminus is in Noyes, Minnesota, at the Canada–US border, where it once continued as Manitoba Highway 75 on the other side of the now-closed border crossing. Its southern terminus is at Interstate 30 and Interstate 45 in Dallas, where it is known as North Central Expressway. U. S. 75 was a cross-country route, from Canada to the Gulf of Mexico at Texas. However, the entire segment south of Dallas has been decommissioned in favor of Interstate 45, a cutoff section of town-to-town surface road having become Texas State Highway 75; the first freeway in Texas was a several-mile stretch of US 75 --The Gulf Freeway, opened to Houston traffic on October 1, 1948. The stretch of US 75 between Interstate 30 and the Oklahoma state line has exits numbered consecutively from 1 to 75, excluding 9-19. All other Texas freeways that have exit numbers are coordinated with mile markers. From Denison north to the Oklahoma border, US 75 is concurrent to U.
S. Route 69. US-75 remains concurrent to US-69 from the Texas border north to Atoka. While US-69 continues to the northeast as a multilane highway, US-75 turns north to serve several small communities between Atoka and Henryetta. Through travellers bypass this segment of US-75 via US-69 and the Indian Nation Turnpike, where the speed limit is 75 miles per hour. From Henryetta through Tulsa and on through Bartlesville to the Kansas State Line, US-75 is once again a multilane highway. In the early 1990s, some portions of US-75 in Oklahoma were slated to become part of the Interstate Highway System; the 1991 Intermodal Surface Transportation Efficiency Act states that "upon the request of the Oklahoma State highway agency, the Secretary shall designate the portion of United States Route 69 from the Oklahoma-Texas State line to Checotah in the State of Oklahoma as a part of the Interstate System." This would have created an Interstate route from Interstate 40 south to the Texas line, including the portion of US-75 co-signed with US-69 south of Atoka.
The legislation was unclear whether the route would enter Texas to connect with or become an extension of Interstate 45. A current plan is to construct a new segment of the Oklahoma Turnpike along the US-69 corridor to bring it to corridor standards. A major north–south artery in Kansas, US-75 enters the state at Caney, it crosses Interstate 35 south of Olivet at the BETO Junction. From I-35 to Melvern Lake, US-75 is a Super-2 highway, with controlled access interchanges at Township Road, K-278, K-31 southbound. From Melvern Lake to just north of Lyndon, US-75 and K-31 share a long concurrency. At U. S. Route 56 near Scranton US-75 becomes a freeway. There is no direct access to the Kansas Turnpike from US-75, but the highway joins with Interstate 470 less than 1 mile from 470's interchange with the turnpike. US-75 and Interstate 470 run together along the west side of Topeka to Interstate 70. US-75 turns east along Interstate 70 for about 3 miles before exiting northbound as a freeway; this freeway segment runs to Elmont becomes an expressway to Holton.
The remainder of US-75 in Kansas is two lanes. The highway exits the state north of Sabetha. There was a US-75 Alternate in Kansas, it was on Topeka Boulevard and was the route US-75 took through Topeka. U. S. 75 enters Nebraska south of Dawson. From Nebraska City northward, it parallels the Missouri River. A brief section which serves as a bypass for Nebraska City is an expressway called the J. Sterling Morton Beltway. Nebraska City itself is served with Business Route U. S. 75. U. S. 75 and U. S. Route 34 overlap from Union to Plattsmouth. North of Plattsmouth, U. S. 75 becomes the Kennedy Freeway, serving as an arterial highway through Bellevue and the South Omaha neighborhood of Omaha. It follows Interstate 480 through central Omaha before branching off as the North Omaha Freeway. From Interstate 680 northward to Nashville U. S. 75 is an expressway. North of Nashville it becomes a two-lane road again, it is concurrent with U. S. Route 30 in Blair, it joins with U. S. Route 77 at Winnebago; the two highways run together until their junction with Interstate 129 and U.
S. Route 20 at South Sioux City. U. S. 75 follows I-129 and U. S. 20 towards the Missouri River and Iowa. U. S. 75 is a major north–south artery in the northwestern corner of Iowa. It enters the state by a Missouri River crossing at Sioux City concurrent with Interstate 129 and U. S. Route 20. U. S. 75 and U. S. 20 run together on a freeway bypass around the southeast side of Sioux City before U. S. 20 turns east at Gordon Drive. U. S. 75 continues as a freeway to the Woodbury County/Plymouth County line, where it becomes an expressway. This expressway becomes a freeway bypass of Le Mars. North of Le Mars, U. S. 75 exits off the freeway bypass, which continues on as Iowa Highway 60, turns north. U. S. 75 continues as a two-lane, undivided highway passing through Sioux Center and Rock Rapids before leaving the state north of Iowa Highway 9. The segment from the Missouri River to LeMars is part of a larger expressway project which will provide a direct connection between Sioux City and the Twin Cities region in Minnesota.
In Minnesota, U. S. 75 stays close to the state's western border. It passes through few large towns. U. S. 75 enters Minnesota south of Luverne near Ash Creek and Steen, passes though Pipestone and Breckenridge. It is the main north–south route through Moorhead. North of Moorhead, the route turns northeast to pass through Crookston turns northwest towards the Red River of t
North Dakota is a U. S. state in northern regions of the United States. It is the nineteenth largest in area, the fourth smallest by population, the fourth most sparsely populated of the 50 states. North Dakota was admitted to the Union on November 3, 1889, along with its neighboring state, South Dakota, its capital is Bismarck, its largest city is Fargo. In the 21st century, North Dakota's natural resources have played a major role in its economic performance with the oil extraction from the Bakken formation, which lies beneath the northwestern part of the state; such development has led to reduced unemployment. North Dakota contains the tallest human-made structure in the KVLY-TV mast. North Dakota is a Midwestern state of the United States, it lies at the center of the North American continent. The geographic center of North America is near the town of Rugby. Bismarck is the capital of North Dakota, Fargo is the largest city. Soil is North Dakota's most precious resource, it is the base of the state's great agricultural wealth.
But North Dakota has enormous mineral resources. These mineral resources include billions of tons of lignite coal. In addition, North Dakota has large oil reserves. Petroleum was discovered in the state in 1951 and became one of North Dakota's most valuable mineral resources. In the early 2000's, the emergence of hydraulic fracturing technologies enabled mining companies to extract huge amounts of oil from the Bakken shale rock formation in the western part of the state. North Dakota's economy is based more on farming than are the economies of most other states. Many North Dakota factories manufacture farm equipment. Many of the state’s merchants rely on agriculture. Farms and ranches cover nearly all of North Dakota, they stretch from the flat Red River Valley in the east, across rolling plains, to the rugged Badlands in the west. The chief crop, wheat, is grown in nearly every county. North Dakota flaxseed, it is the country’s top producer of barley and sunflower seeds and a leader in the production of beans, lentils, oats and sugar beets.
Few white settlers came to the North Dakota region before the 1870's because railroads had not yet entered the area. During the early 1870's, the Northern Pacific Railroad began to push across the Dakota Territory. Large-scale farming began during the 1870's. Eastern corporations and some families established huge wheat farms covering large areas of land in the Red River Valley; the farms made such enormous profits. White settlers, attracted by the success of the bonanza farms, flocked to North Dakota increasing the territory's population. In 1870, North Dakota had 2,405 people. By 1890, the population had grown to 190,983. North Dakota was named for the Sioux people; the Sioux called meaning allies or friends. One of North Dakota's nicknames is the Peace Garden State; this nickname honors the International Peace Garden, which lies on the state's border with Manitoba, Canada. North Dakota is called the Flickertail State because of the many flickertail ground squirrels that live in the central part of the state.
North Dakota is in the U. S. region known as the Great Plains. The state shares the Red River of the North with Minnesota to the east. South Dakota is to the south, Montana is to the west, the Canadian provinces of Saskatchewan and Manitoba are to the north. North Dakota is near the middle of North America with a stone marker in Rugby, North Dakota marking the "Geographic Center of the North American Continent". With an area of 70,762 square miles, North Dakota is the 19th largest state; the western half of the state consists of the hilly Great Plains as well as the northern part of the Badlands, which are to the west of the Missouri River. The state's high point, White Butte at 3,506 feet, Theodore Roosevelt National Park are in the Badlands; the region is abundant in fossil fuels including crude oil and lignite coal. The Missouri River forms Lake Sakakawea, the third largest artificial lake in the United States, behind the Garrison Dam; the central region of the state is divided into the Missouri Plateau.
The eastern part of the state consists of the flat Red River Valley, the bottom of glacial Lake Agassiz. Its fertile soil, drained by the meandering Red River flowing northward into Lake Winnipeg, supports a large agriculture industry. Devils Lake, the largest natural lake in the state, is found in the east. Eastern North Dakota is overall flat. Most of the state is covered in grassland. Natural trees in North Dakota are found where there is good drainage, such as the ravines and valley near the Pembina Gorge and Killdeer Mountains, the Turtle Mountains, the hills around Devil's Lake, in the dunes area of McHenry County in central North Dakota, along the Sheyenne Valley slopes and the Sheyenne delta; this diverse terrain supports nearly 2,000 species of plants. North Dakota has a continental climate with cold winters; the temperature differences are significant because of its far inland position and being in the center of the Northern Hemisphere, with equal distances to the North Pole and the Equator.
As such, summers are subtropical, but winters are cold enough to ensure plant hardiness is low. Native American peoples lived in what is now North Dakota for thousands of year
Red River of the North
The Red River is a North American river. Originating at the confluence of the Bois de Sioux and Otter Tail rivers between the U. S. states of Minnesota and North Dakota, it flows northward through the Red River Valley, forming most of the border of Minnesota and North Dakota and continuing into Manitoba. It empties into Lake Winnipeg, whose waters join the Nelson River and flow into Hudson Bay. Several urban areas have developed on both sides of the Red River, including those of Fargo-Moorhead and Grand Forks-East Grand Forks in states of North Dakota and Minnesota in the United States and Winnipeg in Canada; the Red is about 885 kilometres long, of which about 635 kilometres are in the United States and about 255 kilometres are in Canada. The river falls 70 metres on its trip to Lake Winnipeg, where it spreads into the vast deltaic wetland known as Netley Marsh. In the United States, the Red River is sometimes called the Red River of the North; this distinguishes it from the so-called Red River of the South, a tributary of the Atchafalaya River that forms part of the border between Texas and Arkansas.
Long a highway for trade, the Red has been designated as a Canadian Heritage River. The watershed of the Red River was part of Rupert's Land, the concession established by the British Hudson's Bay Company in north central North America; the Red was a key trade route for the company, contributed to the settlement of British North America. The river was long used by fur traders, including the French and the Métis people, who established a community in this area before the British defeated France in the Seven Years' War. Following that, they took over French territory in Canada. Settlers of the Red River Colony established farming along the river, their primary settlement developed as Winnipeg, Manitoba. What became known as the Red River Trails, nineteenth-century oxcart trails developed by the Métis, supported the fur trade and these settlements, they contributed to further development of the region on both sides of the international border. The Red River begins at the confluence of the Bois de Sioux and Otter Tail rivers, on the border of Wahpeton, North Dakota and Breckenridge, Minnesota.
Downstream, it is bordered by the twin cities of Fargo, North Dakota – Moorhead and Grand Forks, North Dakota – East Grand Forks, Minnesota. It continues north to the province of Manitoba in Canada. Manitoba's capital, Winnipeg, is at the Red's confluence with the Assiniboine River, at a point called The Forks. Together with the Assiniboine, the Red River encloses the endorheic basin of Devils' Lake and Stump Lake; the Red flows further north before draining into Lake Winnipeg which drains through the Nelson River into Hudsons Bay, both part of the Hudson Bay watershed. The mouth of the Red River forms; the Netley Marsh is west of the Red and the Libau Marsh is east, forming a 26,000-hectare wetland. Southern Manitoba has a comparatively long frost-free season, between 120 and 140 days in the Red River Valley; the Red River flows across the flat lake bed of the ancient glacial Lake Agassiz, an enormous glacial lake created at the end of the Wisconsin glaciation from meltwaters of the Laurentide ice sheet.
As this continental glacier decayed, its meltwaters formed the lake. Over thousands of years, sediments precipitated to the bottom of the lakebed; these lacustrine soils are the parent soils of today's Red River Valley. The river is young; the word "valley" is a misnomer. While the Red River drains the region, it did not create a valley wider than a few hundred feet; the much wider floodplain is the lake bed of the ancient glacial lake. It is remarkably flat; the river and small in most seasons, does not have the energy to cut a gorge. Instead it meanders across the silty bottomlands in its progress north. In consequence, high water has nowhere to go, except to spread across the old lakebed in "overland flooding". Heavy snows or rains on saturated or frozen soil, have caused a number of catastrophic floods, which are made worse by the fact that snowmelt starts in the warmer south, waters flowing northward are dammed or slowed by ice; these periodic floods have the effect of refilling, in the ancient lake.
Major floods in historic times include those of 1826, 1897, 1950, 1997, 2009, 2011, there has been significant flooding many years in between. Geologists have found evidence of many other floods in prehistoric times of equal or greater size; these "paleofloods" are known from their effects on local landforms, have been the subject of scholarly studies. After the disastrous 1950 flood, which resulted in extensive property damage and losses in Winnipeg, Manitoba Province undertook flood prevention by constructing the Red River Floodway. Completed in 1968, it diverts floodwaters around the city to less settled areas further up the river. Grand Forks, North Dakota, East Grand Forks, suffered widespread destruction in the flood of 1997. 75% of the population in the former city was evacuated, all of the latter. Many of the residential areas along the rivers were inundated and all the homes had to be destroyed. Afterward a massive flood protection project was undertaken to protect both cities. On May 8, 1950 the Red River reached its highest level at Winnipeg since 1861.
Eight dikes protecting Winnipeg g
South Dakota is a U. S. state in the Midwestern region of the United States. It is named after the Lakota and Dakota Sioux Native American tribes, who compose a large portion of the population and dominated the territory. South Dakota is the seventeenth largest by area, but the fifth smallest by population and the 5th least densely populated of the 50 United States; as the southern part of the former Dakota Territory, South Dakota became a state on November 2, 1889 with North Dakota. Pierre is the state capital and Sioux Falls, with a population of about 187,200, is South Dakota's largest city. South Dakota is bordered by the states of North Dakota, Iowa, Nebraska and Montana; the state is bisected by the Missouri River, dividing South Dakota into two geographically and distinct halves, known to residents as "East River" and "West River". Eastern South Dakota is home to most of the state's population, the area's fertile soil is used to grow a variety of crops. West of the Missouri, ranching is the predominant agricultural activity, the economy is more dependent on tourism and defense spending.
Most of the Native American reservations are in West River. The Black Hills, a group of low pine-covered mountains sacred to the Sioux, are in the southwest part of the state. Mount Rushmore, a major tourist destination, is there. South Dakota has a temperate continental climate, with four distinct seasons and precipitation ranging from moderate in the east to semi-arid in the west; the state's ecology features species typical of a North American grassland biome. Humans have inhabited the area for several millennia, with the Sioux becoming dominant by the early 19th century. In the late 19th century, European-American settlement intensified after a gold rush in the Black Hills and the construction of railroads from the east. Encroaching miners and settlers triggered a number of Indian wars, ending with the Wounded Knee Massacre in 1890. Key events in the 20th century included the Dust Bowl and Great Depression, increased federal spending during the 1940s and 1950s for agriculture and defense, an industrialization of agriculture that has reduced family farming.
While several Democratic senators have represented South Dakota for multiple terms at the federal level, the state government is controlled by the Republican Party, whose nominees have carried South Dakota in each of the last 13 presidential elections. Dominated by an agricultural economy and a rural lifestyle, South Dakota has sought to diversify its economy in areas to attract and retain residents. South Dakota's history and rural character still influence the state's culture. South Dakota is in the north-central United States, is considered a part of the Midwest by the U. S. Census Bureau; the culture and geography of western South Dakota have more in common with the West than the Midwest. South Dakota has a total area of 77,116 square miles, making the state the 17th largest in the Union. Black Elk Peak named Harney Peak, with an elevation of 7,242 ft, is the state's highest point, while the shoreline of Big Stone Lake is the lowest, with an elevation of 966 ft. South Dakota is bordered to the north by North Dakota.
The geographical center of the U. S. is 17 miles west of Castle Rock in Butte County. The North American continental pole of inaccessibility is between Allen and Kyle, 1,024 mi from the nearest coastline; the Missouri River is the longest river in the state. Other major South Dakota rivers include the Cheyenne, Big Sioux, White Rivers. Eastern South Dakota has many natural lakes created by periods of glaciation. Additionally, dams on the Missouri River create four large reservoirs: Lake Oahe, Lake Sharpe, Lake Francis Case, Lewis and Clark Lake. South Dakota can be divided into three regions: eastern South Dakota, western South Dakota, the Black Hills; the Missouri River serves as a boundary in terms of geographic and political differences between eastern and western South Dakota. The geography of the Black Hills, long considered sacred by Native Americans, differs from its surroundings to such an extent it can be considered separate from the rest of western South Dakota. At times the Black Hills are combined with the rest of western South Dakota, people refer to the resulting two regions divided by the Missouri River as West River and East River.
Eastern South Dakota features higher precipitation and lower topography than the western part of the state. Smaller geographic regions of this area include the Coteau des Prairies, the Dissected Till Plains, the James River Valley; the Coteau des Prairies is a plateau bordered on the east by the Minnesota River Valley and on the west by the James River Basin. Further west, the James River Basin is low, flat eroded land, following the flow of the James River through South Dakota from north to south; the Dissected Till Plains, an area of rolling hills and fertile soil that covers much of Iowa and Nebraska, extends into the southeastern corner of South Dakota. Layers deposited during the Pleistocene epoch, starting around two million years ago, cover most of eastern South Dakota; these are the youngest rock and sediment layers in the state, the product of several successive periods of glaciation which deposited a large amount of rocks and soil, known as till, over the area. The Great Plains cover most of the western two-thirds of South Dakota.
West of the Missouri Rive
1890 United States Census
The Eleventh United States Census was taken beginning June 2, 1890. It determined the resident population of the United States to be 62,979,766—an increase of 25.5 percent over the 50,189,209 persons enumerated during the 1880 census. The data was tabulated by machine for the first time; the data reported that the distribution of the population had resulted in the disappearance of the American frontier. Most of the 1890 census materials were destroyed in a 1921 fire and fragments of the US census population schedule exist only for the states of Alabama, Illinois, New Jersey, New York, North Carolina, South Dakota, Texas, the District of Columbia; this was the first census in which a majority of states recorded populations of over one million, as well as the first in which multiple cities – New York as of 1880, Philadelphia – recorded populations of over one million. The census saw Chicago rank as the nation's second-most populous city, a position it would hold until 1990, in which Los Angeles would supplant it.
The 1890 census collected the following information: The 1890 census was the first to be compiled using methods invented by Herman Hollerith and was overseen by Superintendents Robert P. Porter and Carroll D. Wright. Data was entered on a machine readable medium, punched cards, tabulated by machine; the net effect of the many changes from the 1880 census: the larger population, the number of data items to be collected, the Census Bureau headcount, the volume of scheduled publications, the use of Hollerith's electromechanical tabulators, was to reduce the time required to process the census from eight years for the 1880 census to six years for the 1890 census. The total population of 62,947,714, the family, or rough, was announced after only six weeks of processing; the public reaction to this tabulation was disbelief, as it was believed that the "right answer" was at least 75,000,000. The United States census of 1890 showed a total of 248,253 Native Americans living in the United States, down from 400,764 Native Americans identified in the census of 1850.
The 1890 census announced that the frontier region of the United States no longer existed, that the Census Bureau would no longer track the westward migration of the U. S. population. Up to and including the 1880 census, the country had a frontier of settlement. By 1890, isolated bodies of settlement had broken into the unsettled area to the extent that there was hardly a frontier line; this prompted Frederick Jackson Turner to develop his Frontier Thesis. The original data for the 1890 Census is no longer available. All the population schedules were damaged in a fire in the basement of the Commerce Building in Washington, D. C. in 1921. Some 25 % of the materials were presumed another 50 % damaged by smoke and water; the damage to the records led to an outcry for a permanent National Archives. In December 1932, following standard federal record-keeping procedures, the Chief Clerk of the Bureau of the Census sent the Librarian of Congress a list of papers to be destroyed, including the original 1890 census schedules.
The Librarian was asked by the Bureau to identify any records which should be retained for historical purposes, but the Librarian did not accept the census records. Congress authorized destruction of that list of records on February 21, 1933, the surviving original 1890 census records were destroyed by government order by 1934 or 1935; the other censuses for which some information has been lost are the 1810 enumerations. Few sets of microdata from the 1890 census survive, but aggregate data for small areas, together with compatible cartographic boundary files, can be downloaded from the National Historical Geographic Information System. Mayo-Smith, Richmond, "The Eleventh Census of the United States". In: The Economic Journal, Vol. 1, p. 43 - 58 1891 U. S Census Report Contains 1890 Census results Historical US Census data from the U. S. Census Bureau website Hollerith 1890 Census Tabulator by Columbia University "The Fate of the 1890 Population Census" from the National Archives website
United States Census Bureau
The United States Census Bureau is a principal agency of the U. S. Federal Statistical System, responsible for producing data about the American people and economy; the Census Bureau is part of the U. S. Department of Commerce and its director is appointed by the President of the United States; the Census Bureau's primary mission is conducting the U. S. Census every ten years, which allocates the seats of the U. S. House of Representatives to the states based on their population; the Bureau's various censuses and surveys help allocate over $400 billion in federal funds every year and it helps states, local communities, businesses make informed decisions. The information provided by the census informs decisions on where to build and maintain schools, transportation infrastructure, police and fire departments. In addition to the decennial census, the Census Bureau continually conducts dozens of other censuses and surveys, including the American Community Survey, the U. S. Economic Census, the Current Population Survey.
Furthermore and foreign trade indicators released by the federal government contain data produced by the Census Bureau. Article One of the United States Constitution directs the population be enumerated at least once every ten years and the resulting counts used to set the number of members from each state in the House of Representatives and, by extension, in the Electoral College; the Census Bureau now conducts a full population count every 10 years in years ending with a zero and uses the term "decennial" to describe the operation. Between censuses, the Census Bureau makes population projections. In addition, Census data directly affects how more than $400 billion per year in federal and state funding is allocated to communities for neighborhood improvements, public health, education and more; the Census Bureau is mandated with fulfilling these obligations: the collecting of statistics about the nation, its people, economy. The Census Bureau's legal authority is codified in Title 13 of the United States Code.
The Census Bureau conducts surveys on behalf of various federal government and local government agencies on topics such as employment, health, consumer expenditures, housing. Within the bureau, these are known as "demographic surveys" and are conducted perpetually between and during decennial population counts; the Census Bureau conducts economic surveys of manufacturing, retail and other establishments and of domestic governments. Between 1790 and 1840, the census was taken by marshals of the judicial districts; the Census Act of 1840 established a central office. Several acts followed that revised and authorized new censuses at the 10-year intervals. In 1902, the temporary Census Office was moved under the Department of Interior, in 1903 it was renamed the Census Bureau under the new Department of Commerce and Labor; the department was intended to consolidate overlapping statistical agencies, but Census Bureau officials were hindered by their subordinate role in the department. An act in 1920 changed the date and authorized manufacturing censuses every two years and agriculture censuses every 10 years.
In 1929, a bill was passed mandating the House of Representatives be reapportioned based on the results of the 1930 Census. In 1954, various acts were codified into Title 13 of the US Code. By law, the Census Bureau must count everyone and submit state population totals to the U. S. President by December 31 of any year ending in a zero. States within the Union receive the results in the spring of the following year; the United States Census Bureau defines four statistical regions, with nine divisions. The Census Bureau regions are "widely used...for data collection and analysis". The Census Bureau definition is pervasive. Regional divisions used by the United States Census Bureau: Region 1: Northeast Division 1: New England Division 2: Mid-Atlantic Region 2: Midwest Division 3: East North Central Division 4: West North Central Region 3: South Division 5: South Atlantic Division 6: East South Central Division 7: West South Central Region 4: West Division 8: Mountain Division 9: Pacific Many federal, state and tribal governments use census data to: Decide the location of new housing and public facilities, Examine the demographic characteristics of communities and the US, Plan transportation systems and roadways, Determine quotas and creation of police and fire precincts, Create localized areas for elections, utilities, etc.
Gathers population information every 10 years The United States Census Bureau is committed to confidentiality, guarantees non-disclosure of any addresses or personal information related to individuals or establishments. Title 13 of the U. S. Code establishes penalties for the disclosure of this information. All Census employees must sign an affidavit of non-disclosure prior to employment; the Bureau cannot share responses, addresses or personal information with anyone including United States or foreign government