North Dakota Highway 200
North Dakota Highway 200 is a major east–west state highway in the U. S. state of North Dakota. It runs from Minnesota State Highway 200 at the Minnesota border near Halstad, Minnesota to Montana Highway 200 near Fairview, Montana. At nearly 416 miles, it is the longest state highway in North Dakota; this state highway is part of a continuous chain of numbered state highways that stretch from Minnesota to Idaho. The North Dakota Highways Page by Chris Geelhart
Interstate 29 is an Interstate Highway in the Midwestern United States. I-29 runs from Kansas City, Missouri, at a junction with Interstate 35 and Interstate 70, to the Canada–US border near Pembina, North Dakota, where it connects with Manitoba Highway 75; the road follows the course of three major rivers, all of which form the borders of U. S. states. The southern portion of I-29 parallels the Missouri River from Kansas City northward to Sioux City, where it crosses and parallels the Big Sioux River. For the northern third of the highway, it follows the Red River of the North; the major cities that I-29 connects to includes Iowa. Near its southern terminus, I-29 is concurrent with I-35 and U. S. Route 71; the interstate diverts from U. S. 71 just north of St. Joseph and follows a sparsely populated corridor along the Missouri River to Council Bluffs. During the design phase there was an alternative sending the route further along U. S. 71 through the bigger towns of Maryville and Clarinda, Iowa.
During the Great Flood of 1993 the Missouri River flooded this section and traffic was rerouted to U. S. 71 through Maryville and Clarinda. I-29 was closed again for about two months during the 2011 Missouri River Flood. All of I-29 in Missouri is in an area called the Platte Purchase, not part of Missouri when it entered the Union. Interstate 29 begins in Iowa near Hamburg, it goes northwest to an interchange with Iowa Highway 2 goes north until Council Bluffs. It runs concurrent with Interstate 80 until separating from I-80 less than a mile east of Omaha, Nebraska to follow the Missouri River north, winding its way along the western and northern edges of Council Bluffs. North of Council Bluffs, I-29 runs concurrent with Interstate 680 between Exits 61 and 71. After Interstate 680 separates, I-29 continues on a northwesterly path toward Sioux City. At Sioux City, Interstate 129 spurs off of I-29 to go west toward Nebraska. After continuing toward downtown Sioux City on a northerly route, I-29 turns west and enters South Dakota.
Interstate 29 enters South Dakota at North Sioux City by crossing over the Big Sioux River. It runs northwest until its interchange with South Dakota Highway 50 near Vermillion, where it turns north; the highway alignment is due north until just before Sioux Falls. In the Sioux Falls area, I-29 serves the western part of Sioux Falls while I-229 spurs off and serves eastern Sioux Falls. In northwestern Sioux Falls, I-29 meets Interstate 90. After that, it continues north past Brookings and an intersection with US 14. At the intersection with South Dakota Highway 28, I-29 turns northwest toward Watertown. After Watertown, the highway continues north and passes an intersection with US 12 before continuing into North Dakota. Interstate 29 enters North Dakota from the south, near Hankinson. At Fargo, it continues north along the Red River toward Grand Forks. At its northern terminus, I-29 enters Canada and becomes Manitoba Provincial Trunk Highway 75, which leads to Winnipeg; the portion from Fargo, North Dakota, to the Canada–US border was considered for designation as Interstate 31 in 1957 for present-day I-29.
No freeway was planned south of Fargo. However, it was subsequently decided in 1958 to connect I-31 between Sioux Falls and Fargo; the entire freeway was built and numbered as I-29. Residents of Missouri and Louisiana began campaigning in 1965 via, the "US 71 - I-29 Association," to extend Interstate 29 all the way to New Orleans, Louisiana following the US 71 corridor; the campaign would create a limited access highway from New Orleans on to Winnipeg. That extension came to be called Interstate 49, not part of the 1957 master plan, it was named I-49 instead of I-29 because the interstate naming rules mandate that north-south roads are odd numbered and named in increasing order from west to east. North of their concurrence, I-29 is west of I-35, but south of Kansas City Interstate 35 and Interstate 45 are to the west of the proposed route, Interstate 55 is to the east. Interstate 49 was the number chosen; when Interstate 49 is complete, the goal of the Association will have been accomplished, with only a brief gap and name change in Kansas City.
Missouri I‑35 / I‑70 / US 24 / US 40 / US 71 in Kansas City. I-29/I-35 travels concurrently through Kansas City. I-29/US 71 travels concurrently to east of Amazonia. US 69 on the Gladstone–Kansas City city line US 169 on the Gladstone–Kansas City city line I‑635 in Kansas City I‑435 in Kansas City; the highways travel concurrently to Platte City. I‑229 south-southeast of St. Joseph US 169 in St. Joseph US 36 in St. Joseph US 169 in St. Joseph US 59 north-northeast of St. Joseph; the highways travel concurrently to east of Amazonia. I‑229 / US 59 / US 71 North of St. Joseph US 59 northwest of Amazonia; the highways travel concurrently for 1.8 miles. US 59 north of Oregon US 159 south-southeast of Mound City US 59 east of Craig US 136 in Rock Port Iowa US 34 / US 275 west of Glenwood. I-29/US 275 travels concurrently to Council Bluffs. I‑80 in Council Bluffs; the highways travel concurrently through Council Bluffs. I‑480 / US 6 in Council Bluffs I‑680 west-southwest of Crescent; the highways travel concurrently to west-southwest of Loveland.
US 30 in Missouri Valley I‑129 / US 20 / US 75 in Sioux City US 77 in Sioux City South Dakota US 18 south-southwest of Worthing. The highways travel concurrently for 3.02 miles. I‑229 in Sioux Falls I‑90 in Sioux Falls US 14 in Brookings US 212 in Watertown US 81 n
Population density is a measurement of population per unit area or unit volume. It is applied to living organisms, most of the time to humans, it is a key geographical term. In simple terms population density refers to the number of people living in an area per kilometer square. Population density is population divided by total land water volume, as appropriate. Low densities may lead to further reduced fertility; this is called the Allee effect after the scientist. Examples of the causes in low population densities include: Increased problems with locating sexual mates Increased inbreeding For humans, population density is the number of people per unit of area quoted per square kilometer or square mile; this may be calculated for a county, country, another territory or the entire world. The world's population is around 7,500,000,000 and Earth's total area is 510,000,000 square kilometers. Therefore, the worldwide human population density is around 7,500,000,000 ÷ 510,000,000 = 14.7 per km2. If only the Earth's land area of 150,000,000 km2 is taken into account human population density is 50 per km2.
This includes all continental and island land area, including Antarctica. If Antarctica is excluded population density rises to over 55 people per km2. However, over half of the Earth's land mass consists of areas inhospitable to human habitation, such as deserts and high mountains, population tends to cluster around seaports and fresh-water sources. Thus, this number by itself does not give any helpful measurement of human population density. Several of the most densely populated territories in the world are city-states and dependencies; these territories have a small area and a high urbanization level, with an economically specialized city population drawing on rural resources outside the area, illustrating the difference between high population density and overpopulation The potential to maintain the agricultural aspects of deserts is limited as there is not enough precipitation to support a sustainable land. The population in these areas are low. Therefore, cities in the Middle East, such as Dubai, have been increasing in population and infrastructure growth at a fast pace.
Cities with high population densities are, by some, considered to be overpopulated, though this will depend on factors like quality of housing and infrastructure and access to resources. Most of the most densely populated cities are in Southeast Asia, though Cairo and Lagos in Africa fall into this category. City population and area are, however dependent on the definition of "urban area" used: densities are invariably higher for the central city area than when suburban settlements and the intervening rural areas are included, as in the areas of agglomeration or metropolitan area, the latter sometimes including neighboring cities. For instance, Milwaukee has a greater population density when just the inner city is measured, the surrounding suburbs excluded. In comparison, based on a world population of seven billion, the world's inhabitants, as a loose crowd taking up ten square feet per person, would occupy a space a little larger than Delaware's land area; the Gaza Strip has a population density of 5,046 pop/km.
Although arithmetic density is the most common way of measuring population density, several other methods have been developed to provide a more accurate measure of population density over a specific area. Arithmetic density: The total number of people / area of land Physiological density: The total population / area of arable land Agricultural density: The total rural population / area of arable land Residential density: The number of people living in an urban area / area of residential land Urban density: The number of people inhabiting an urban area / total area of urban land Ecological optimum: The density of population that can be supported by the natural resources Demography Human geography Idealized population Optimum population Population genetics Population health Population momentum Population pyramid Rural transport problem Small population size Distance sampling List of population concern organizations List of countries by population density List of cities by population density List of city districts by population density List of English districts by population density List of European cities proper by population density List of United States cities by population density List of islands by population density List of U.
S. states by population density List of Australian suburbs by population density Selected Current and Historic City, Ward & Neighborhood Density Duncan Smith / UCL Centre for Advanced Spatial Analysis. "World Population Density". Exploratory map shows data from the Global Human Settlement Layer produced by the European Commission JRC and the CIESIN Columbia University
Caledonia, North Dakota
Caledonia is a census-designated place in Traill County, North Dakota in the United States. A former boomtown of the 1870s and the era of the Hudson's Bay Company steamship trade, the community has now all but disappeared. An unincorporated community, it was designated as part of the U. S. Census Bureau's Participant Statistical Areas Program on March 31, 2010, it was not counted separately during the 2000 Census, but was included in the 2010 Census, where a population of 39 was reported. First called Goose River, the community was established as a post for the Hudson's Bay Company steamships which operated on the Red River of the North. Caledonia became an early boom town in the Red River Valley and became a post for a stagecoach line which lead north to Fort Garry — now called Winnipeg. Upon the creation of Traill County in 1875, Caledonia was designated as the county seat. However, in that same year, the Hudson's Bay Company closed their U. S. posts including the one at Caledonia. When James J. Hill's railroad crossed Traill County, it bypassed Caledonia.
The steamboat industry soon floundered and the county seat was moved to Hillsboro in 1896. Caledonia sits on the banks of the Goose River near the confluence with the Red River of the North
1930 United States Census
The Fifteenth United States Census, conducted by the Census Bureau one month from April 1, 1930, determined the resident population of the United States to be 122,775,046, an increase of 13.7 percent over the 106,021,537 persons enumerated during the 1920 Census. The 1930 Census collected the following information: address name relationship to head of family home owned or rented if owned, value of home if rented, monthly rent whether owned a radio set whether on a farm sex race age marital status and, if married, age at first marriage school attendance literacy birthplace of person, their parents if foreign born: language spoken at home before coming to the U. S. year of immigration whether naturalized ability to speak English occupation and class of worker whether at work previous day veteran status if Indian: whether of full or mixed blood tribal affiliationFull documentation for the 1930 census, including census forms and enumerator instructions, is available from the Integrated Public Use Microdata Series.
The original census enumeration sheets were microfilmed by the Census Bureau in 1949. The microfilmed census is located on 2,667 rolls of microfilm, available from the National Archives and Records Administration. Several organizations host images of the microfilmed census online, digital indices. Microdata from the 1930 census are available through the Integrated Public Use Microdata Series. Aggregate data for small areas, together with electronic boundary files, can be downloaded from the National Historical Geographic Information System. 1930 Census Questions Hosted at CensusFinder.com 1931 U. S Census Report Contains 1930 Census results Historic US Census data 1930Census.com: 1930 United States Census for Genealogy & Family History Research 1930 Interactive US Census Find stories and more attached to names on the 1930 US census
North Dakota's at-large congressional district
North Dakota's At-Large Congressional District is the sole congressional district for the state of North Dakota. Based on size, it is the eighth largest congressional district in the nation; the district is represented by Kelly Armstrong. The district was first created when North Dakota achieved statehood on November 2, 1889, electing a single member. Following the 1900 Census the state was allocated two seats, both of whom were elected from an at large district. Following the 1910 Census a third seat was gained, with the legislature drawing three separate districts; the third district was eliminated after the 1930 Census. After the third seat was lost, North Dakota returned to electing two members At-Large. Following the 1960 Census two separate districts were created. In 1970, the second district was eliminated following the 1970 Census and a single At-Large district was created. Since 1972, North Dakota has retained a single congressional district. Election statistics compiled by the Clerk to the House of Representatives.
Martis, Kenneth C.. The Historical Atlas of Political Parties in the United States Congress. New York: Macmillan Publishing Company. Martis, Kenneth C.. The Historical Atlas of United States Congressional Districts. New York: Macmillan Publishing Company. Congressional Biographical Directory of the United States 1774–present
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