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KANSAS (known as the Sunflower State ")

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Originally appearing in Volume V15, Page 660 of the 1911 Encyclopedia Britannica.
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KANSAS (known as the See also:Sunflower See also:State ")  , the central See also:commonwealth of the See also:United States of See also:America, lying between 370 and 4o° N. See also:lat. and between 940 38' and See also:roe 1' 34" W. See also:long . (i.e . 25° W. long. from See also:Washington) . It is bounded on the N. by See also:Nebraska, on the E. by See also:Missouri, on the S. by See also:Oklahoma, and on the W. by See also:Colorado . The See also:state is nearly rectangular in shape, with a breadth of about 210 M. from N. to S. and a length of about 410 M. from E. to W . It contains an See also:area of 82,158 sq. m . (including 384 sq. m. of See also:water See also:surface) . Physiography.—Three physiographic regions may be distinguished within the state—the first, a small portion of the Ozark uplift in the extreme See also:south-See also:east corner; the second, the See also:Prairie Plains, covering approximately the east third of the state; the third, the See also:Great Plains, covering the remaining area . Between the latter-two there is only the most See also:gradual transition . The entire state is indeed practically an undulating See also:plain, gently sloping from See also:west to east at an See also:average of about 7 ft. per mile . There is also an inclination in the eastern See also:half from See also:north to south, as indicated by the course of the See also:rivers, most of which flow south-easterly (the See also:Kansas, with its See also:general easterly course, is the See also:principal exception), the north-west corner being the highest portion of the state . The lowest point in the state in its south-east See also:part, in See also:Montgomery See also:county, is 725 ft. above See also:sea level .

The average See also:

elevation of the east boundary is about 85o ft., while See also:contour lines of 3500—3900 ft. run near the west border . Some-what more than half the See also:total area is below 2000 ft . The gently See also:rolling prairie surface is diversified by an endless See also:succession of broad plains, isolated hills and ridges, and moderate valleys . In places there are terraced uplands, and in others the undulating plain is cut by erosion into See also:low escarpments . The bluffs on the Missouri are in places 200 ft. high, and the valley of the Cimarron, in the south-west, has deep cuts, almost See also:gorges . The west central portion has considerable irregularities of contour, and the north-west is distinctively hilly . In the south-west, below the See also:Arkansas See also:river, is an area of sandhills, and the Ozark See also:Plateau region, as above stated, extends into the south-east corner, though not there much elevated . The great central valley is traversed by the Kansas (or See also:Kaw) river, which, inclusive of the Smoky See also:Hill See also:Branch, extends the entire length of the state, with lateral valleys on the north . Another broad valley is formed in the south half of the state by the Arkansas river, with lateral valleys on the north and south . The south-east portion contains the important Neosho and smaller valleys . In the extreme south-west is the valley of the Cimarron, and along the south boundary is a network of the south tributaries of the Arkansas . Numerous small affluents of the Missouri enrich and diversify the north-east See also:quarter .

The streams of Kansas are usually fed by perennial springs, and, as a See also:

rule, the east and See also:middle portions of the state are well watered . Most of the streams maintain a See also:good flow of water in the driest seasons, and in See also:case of heavy rains many of them " underflow " the adjacent bottom lands, saturating the permeable substratum of the See also:country with the surplus water, which in See also:time drains out and feeds the subsiding streams . This feature is particularly true of the Saline, See also:Solomon and Smoky Hill rivers . The west part is more elevated and water is less abundant . See also:Climate.—The climate of Kansas is exceptionally salubrious . Extremes of See also:heat and See also:cold occur, but as 'a rule the winters are dry and mild, while the summer heats are tempered by the perpetual prairie breezes, and the summer nights are usually cool and refreshing . The average See also:annual temperature of the state for seventeen years preceding 1903 was 54.3° F., the warmest mean being 56•o°, the coldest 52.6° . The extreme variation of yearly means throughout the See also:Year See also:Book of the United States See also:Department of See also:Agriculture, the See also:crop in 1906 was 81,830,611 bushels, almost one-ninth of the crop of the entire country for that year, and much more than the crop of any.other state . In 1909 it was 87,203,000 bushels (less than the crops of either See also:Minnesota or North Dakota) . See also:Winter See also:wheat constitutes almost the entire output . The hard varieties See also:rank in the See also:flour See also:market with the finest Minnesota wheat . The wheat See also:belt crosses the state from north to south in its central third .

Greater even than wheat in See also:

absolute output, though not relatively to the output of other states, is See also:Indian See also:corn . In 1906 the crop was 195,075,000 bushels, and in 1909 it was 154,225,000 . The crop is very variable, according to seasons and prospective markets; ranging e.g. in the See also:decade 1892-1901 from 42'6 (1901) to 2251 (1899) million bushels . The Indian corn belt is mainly in the eastern third of the state . In the five years 1896-1900 the combined value of the crops of Indian corn and wheat exceeded the value of the same crops in any other state of the See also:Union (See also:Illinois being a See also:close second) . In the western third See also:irrigation has been tried, in the earlier years unsuccessfully; in all Kansas, in 1899, there were 23,620 acres irrigated, of which 8939 were in Finney and 7071 in See also:Kearney county . In this western third the rainfall is insufficient for Indian corn; but Kafir corn, an exceptional drought-resisting cereal, has made extraordinary progress in this region, and indeed generally over the state, since 1893, its acreage increasing 416.1 % In the decade 1895-1904 . With the saccharine variety of See also:sorghum, which increased greatly In the same See also:period, this See also:grain is replacing Indian corn . Oats are the third great cereal crop, the yield being 24,780,000 bushels in 1906 and 27,185,000 in 1909 . See also:Alfalfa showed an increased acreage in 1895-1904 of 310.8 %; it is valuable in the west for the same qualities as the Kafir corn . The See also:hay crop in 1909 was 2,652,000 tons . Alfalfa, the See also:Japanese soy See also:bean and the wheat See also:fields—which furnish the finest of pasture in the See also:early See also:spring and ordinarily well into the winter See also:season—are the props of a prosperous See also:dairy See also:industry .

In the early 'eighties the organization of creameries and See also:

cheese factories began in the county-seats; they depended upon gathered cream . About 1889 separators and the whole-See also:milk See also:system were introduced, and about the same time began the service of refrigerator cars on the See also:railways ; the See also:hand separator became See also:common about 1901 . Western Kansas is the dairy country . Its great ranges, whose insufficient rainfall makes impossible the certain, and therefore the profitable, cultivation of cereals, or other settled agriculture, lend themselves with profit to stock and dairy farming . Dairy products increased 60'6 % in value from 1895 to 1904, amounting in the latter year to $16,420,095 . This value was almost equalled by that of eggs and poultry ($14,050,727), which increased 79.7 % in the same decade . The livestock See also:interest is stimulated by the enormous demand for See also:beef-See also:cattle at Kansas See also:City . See also:Sugar-See also:beet culture was tried in the years following 1890 with indifferent success until the introduction of bounties in 1901 . It has extended along the Arkansas valley from the Colorado beet See also:district and into the north-western counties . There is a large beet-sugar factory at See also:Garden City, Finney county . Experiments have been made unsuccessfully in sugar See also:cane (1885) and See also:silk culture (1885 seq.) . The See also:bright climate and pure See also:atmosphere are admirably adapted to the growth of the See also:apple, See also:pear, See also:peach, See also:plum, See also:grape-and See also:cherry .

The smaller fruits also, with scarce an exception, flourish finely . The See also:

fruit product of Kansas ($2,431,773 in 1899) is not, however, as yet particularly notable when compared with that of various other states . According to the estimates of the state department of agriculture, of the total value of all agricultural products in the twenty years 1885-1904 ($3,078,999,855), Indian corn and wheat together represented more than two-fifths (821'3 and 518'1 million dollars respectively), and livestock products nearly one-third (1024.9 millions) . The aggregate value of all agricultural products in 1903-1904 was $754,954,208 . Minerals.—In the east portion of the state are immense beds of bituminous See also:coal, often at shallow depths or cropping out on the surface . In 1907 more than 95 % of the coal came from See also:Crawford, See also:Cherokee, Leavenworth and Osage counties, and about 91'5 % from the first two . The total value of the See also:production of coal in 1905 (6,423,979 tons) was $9,350,542, and in 1908 (6,245,508 tons) $9,292,222 .. In the central portion, which belongs to the Triassic formation, magnesian See also:limestone, ferruginous See also:sandstone and See also:gypsum are representative rocks . Gypsum (in beautiful crystalline See also:form) is found in an almost continuous See also:bed across the state See also:running north-east and south-west with three principal areas, the See also:northern in See also:Marshall county, the central in See also:Dickinson and Saline counties, and the See also:southern (the heaviest, being 3 to 40 ft. thick) in See also:Barber and See also:Comanche counties . The product in 1908 was valued at $281,339• Magnesian limestone, or See also:dolomite, is especially plentiful along the See also:Blue, Republican and Neosho rivers and their tributaries . This beautiful See also:stone, resembling See also:white, See also:grey and cream-coloured See also:marble, is exceedingly useful for See also:building purposes . It crops out in the bluffs in endless quantities, and is easily worked .

The stone resources of the state are largely, but by no means exclusively, confined to the central part . There are See also:

marbles in Osage and other counties, See also:shell marble in Montgomery county, white limestone in See also:Chase county, a valuable bandera flagstone and See also:hydraulic See also:cement See also:rock near Fort See also:Scott, &c . The limestones produced in 1908 were valued at $403,176 and the sandstones at $67,950 . In the central the east, west and middle sections during the same period was very slight, 51'6° to 56'6°, and the greatest variation for any one See also:section was 37° . The absolute extremes were 116° and -34° . The dryness of the See also:air tempers exceedingly to the senses the cold of winter and the heat of summer . The temperature over the state is much more See also:uniform than is the precipitation, which diminishes somewhat regularly westward . In the above period of seventeen years the yearly' means in the west section varied from 11'93 to 29'21 in . (ay . 19'21), in the middle from 18'58 to 34'30 (ay . 26'68), in the east from 26.00 to 45.71 (ay . 34.78); the mean for the state ranging from 20.12 to 3550 (ay .

27'12).1 The precipitation in the west is not sufficient for confident agriculture in any See also:

series of years, since agriculture is practically dependent upon the mean fall; a fact that has been and is of profound importance in the See also:history of the state . The See also:line of 20 in. fall (about the limit of certain agriculture) approximately bisects the state in dry years . The precipitation is very largely in the growing season—at See also:Dodge the fall between See also:April and See also:October is 78 % of that for the year . Freshets and droughts at times See also:work havoc . The former made notable 1844 and 1858; and the latter 1860, 1874 and 1894 . Tornadoes are also a not infrequent infliction, least common in the west . The years 1871, 1879, 1881 and 1892 were made memorable by particularly severe storms . There are 150 to 175 " growing days " for crops between the frosts of spring and autumn, and eight in ten days are bright with See also:sunshine—half of them without a See also:cloud . Winds are prevailingly from the south (in the winter often from the north-west) . See also:Fauna and See also:Flora.—The fauna and flora of the state are those which are characteristic of the plain region generally of which Kansas is a part . The state lies partly in the humid, or Carolinian, and partly in the arid, or Upper Sonoran, area of the Upper Austral See also:life-See also:zone; sod° W. long. is approximately the dividing line between these areas . The bison and See also:elk have disappeared .

A very great variety of birds is found within the state, either as residents or as visitants from the adjoining avifaunal regions—See also:

mountain, plain, northern and southern . In 1886 See also:Colonel N . S . See also:Goss compiled a See also:list of 335 See also:species, of which 175 were known to breed in the state . The See also:wild See also:turkey, once abundant, was near extermination in 1886, and prairie chickens (pinnated See also:grouse) have also greatly diminished in number . The See also:jack-See also:rabbit is characteristic of the prairie . Locusts (" grasshoppers " in See also:local usage) have worked incalculable damage, notably in 1854, 1866, and above all in 1874-1875 . In the last two cases their ravages extended over a great portion of the state . Kansas has no forests . Along the streams there is commonly a fringe of See also:timber, which in the east is fairly heavy . There is an in-creasing scarcity westward .. With the advancing See also:settlement of the state thin See also:wind-break rows become a feature of the prairies .

The lessened ravages of prairie fires have facilitated artificial afforesting, and many cities, in particular, are abundantly and beautifully shaded . Oaks, elms, See also:

hickory, See also:honey-locusts, white ash, sycamore and willows, the rapid growing but miserable See also:box-See also:elder and See also:cotton-See also:wood, are the most common trees . See also:Black See also:walnut was common in the river valleys in Territorial days . The planting of See also:tree reserves by the United States See also:government in the arid counties of this state promises great success . A See also:National See also:Forest of 302,387 acres in Finney, Kearney, See also:Hamilton and See also:Grant counties was set aside in May 1908 . See also:Buffalo and bunch, and other See also:short native prairie See also:grasses, very nutritious ranging See also:food but unavailable as hay, once tovered the plains and pastured immense herds of buffalo and other animals, but with increasing settlement they have given way generally to See also:exotic bladed species, valuable alike for pasture and for hay, except in the western regions . The See also:hardy and ubiquitous See also:sunflower has been chosen as the state See also:flower or floral See also:emblem . See also:Cactus and See also:yucca occur in the west . The See also:soil of the upland prairies is generally a deep See also:rich See also:clay See also:loam of a dark See also:colour . The bottom lands near the streams are a black sandy loam; and the intermediate lands,. or " second bottoms," show a rich and deep black loam, containing very little See also:sand . These soils are all easily cultivated, See also:free from stones, and exceedingly productive . There are exceptional spots on the upland prairies composed of stiff clay, not as easily cultivated, but very productive when properly managed and enriched .

The south-west section is distinctively sandy . A griculture.—The United States See also:

Census of 1900 shows that of the farming area of the state in 1900 (41,662,970 acres, 79'6 % of the total area), 60'1 % was " improved." The value of all See also:farm See also:property was 3864,100,286—of which See also:land and improvements (including buildings), livestock and implements and machinery represented respectively 74'5, 22.1 and 3'4 % . Almost nine-tenths of all farms derived their principal income from livestock or hay and grain, these two See also:sources being about equally important . Of the total value of farm products in 1899 ($209,895,542), crops represented 537, See also:animal products 45'9 and forest products only o'4 % . In 1899 the wheat crop was 38,778,450 bushels, being less than that of Minnesota, North Dakota, See also:Ohio or South Dakota . According to 1 For the See also:thirty years 187?-1906 the mean rainfall for ten-year periods was: at Dodge, 22'8 in., 18'4 in. and 22'7 in.; and at See also:Lawrence, 35.1 in., 39'2 in. and 367 in. for the first, second and third periods respectively . region See also:salt is produced in immense quantities, within a great north to south belt about See also:Hutchinson . The beds, which are exploited by the brine method at Hutchinson, at See also:Ellsworth (Ellsworth county), at See also:Anthony (Harper county) and at See also:Sterling (See also:Rice county), See also:lie from 400 to 1200 ft. underground, and are in places as much as 350 ft. thick and 99% pure . At . Kanopolis in Ellsworth county, at See also:Lyons in Rice county and at Kingman, Kingman county, the salt is See also:mined and sold as rock-salt . In the south-west salt is found in beds and dry incrustations, varying in thickness from a few inches to 2 ft . The total product from 188o–1899 was valued at $5,538,855; the product of 1908 (when Kansas ranked See also:fourth among the states producing salt) was valued at $882,984 .

The development has been mainly since 1887 at Hutchinson and since about 1890 in the rock-salt mines . In the west portion of the state, which belongs to the Cretaceous formation, chalks and a species of native quicklime are very prominent in the river bluffs . The white and cream-coloured chalks are much used for building purposes, but the blue is usually too soft for exposure to the See also:

weather . The quicklime as quarried from the bluffs slakes perfectly, and with sand makes a fairly good See also:mortar, without calcination or other previous preparation . The See also:lignite found near the Colorado line makes a valuable domestic See also:fuel . Natural See also:gas, oil, See also:zinc and See also:lead have been discovered in south-east Kansas and have given that section an extraordinary growth and prosperity . Indications of gas were found about the time of the See also:Civil See also:War, but only in the early 'seventies were they recognized as unmistakable, and they were not successfully See also:developed until the 'eighties . See also:Iola, in See also:Allen county, is the centre of the See also:field, and the gas yields heat, See also:light, and a cheap fuel for smelters, cement-See also:works and other manufacturing See also:plants throughout a large region . The pools lie from 400 to 950 ft. below the surface; some See also:wells have been drilled 1500 ft. deep . The value of the natural gas produced in the state was $15,873 in 1889, $2,261,836 in 1905 and $7,691,587 in 1908, when there were 1917 producing wells, and Kansas ranked fourth of the states of the United States in the value of the natural gas product, being surpassed by See also:Pennsylvania, West See also:Virginia and Ohio . See also:Petroleum was discovered about 1865 in See also:Miami and See also:Bourbon counties, and about 1892 at Neodesha, See also:Wilson county . There was only slight commercial exploitation before 1900 .

The production increased from 74,714 barrels in that year to 4,250,779 In 1904; in 1908 it was 1,801,781 barrels . See also:

Chanute has been the most active centre of production . The field was prospected here in the 'nineties, but developed only after 1900 . In 1877 an immense See also:deposit of lead was discovered on land now within the limits of See also:Galena . Rich zinc blendes were at first thrown away among the byproducts of the lead mines . After the See also:discovery of their true nature there was a slow development, and at the end of the See also:century a notable See also:boom in the fields . From 1876 to 1897 the total value of the output of the Galena field was between $25,000,000 and $26,000,000; but at See also:present Kansas is far more important as a smelter than as a miner of zinc and lead, and in 1906 58% of all spelter produced in the United States came from smelters in Kansas . In 1908 the mines' output was 2293 tons of lead valued at $192,612 and 8628 tons of zinc valued at $811,032 . Pottery, See also:fire, ochre and See also:brick See also:clays are abundant, the first two mainly in the eastern part of the state . See also:Coffeyville has large vitrified brick interests . In 1908 the total value of all the See also:mineral products (incompletely reported) of Kansas was $26,162,213 . Industry and See also:Trade.—Manufactures are not characteristic of the state .

The rank of the state in manufactures in 1900 was sixteenth and in farm products seventh in the Union . The value of the manufactured product in 1900, according to the Twelfth United States Census, was $172,129,398, an increase of 56.2% over the output of 1890; of this total value, the part representing establishments under the " factory system " was $154,008,544,1 and in 1905 the value of the factory product was $198,244,992, an increase of 28.7% . Kansas City, See also:

Topeka, See also:Wichita, Leavenworth and See also:Atchison were the only cities which had manufactures whose See also:gross product was valued in 1905 at more than $3,000,000 each; their See also:joint See also:pro-duct was valued at $126,515,804, and that of Kansas City alone was $96473,050, almost half the output of the state . The most important manufacturing industry, both in 1900 and in 1905, was slaughtering and See also:meat-packing—for which Kansas City is the second centre of the country—with a product for the state valued at $77,411,883 in 1900, and $96,375,639 in 1905; in both these years the value of the product of Kansas was exceeded only by that of Illinois . The flour and grist See also:mill industry ranked next, with a product valued at $21,328,747 in 1900 and nearly twice that amount, $42,034,019, in 1905 . In 1900 a quarter of the wheat crop was handled by the See also:mills of the state . Lesser manufacturing interests are railway See also:shop construction (value in 1905, $11,521,144); zinc smelting and refining (value in 1905, $10,999,468); the manufacture of cheese, See also:butter and condensed milk (value in 1905, $3,946,349); and of foundry and See also:machine shop products (value in 1905, $3,756,825) . I All subsequent figures in this See also:paragraph for manufactures in 1900 are given for establishments under the " factory system " only, so as to be comparable with See also:statistics for 1905, which do not include See also:minor establishments . Communications.—Kansas is excellently provided with railways, with an aggregate length in See also:January 1909 of 8914.77 M . (in 1870, 1880, 1890 respectively, 1,501, 3,244 and 8,710 m.) . The most important systems are the Atchison, Topeka & See also:Santa Fe, the Missouri Pacific, the See also:Chicago, Rock See also:Island & Pacific, the Union Pacific, the Missouri, Kansas & See also:Texas, the Chicago, See also:Burlington & See also:Quincy, and the St See also:Louis & See also:San Francisco systems . The first See also:train entered Kansas on the Union Pacific in 1860 .

During the following decade the lines of the Missouri Pacific, the Missouri, Kansas & Texas and the Santa Fe were well under construction . These roads give excellent connexions with Chicago, the Gulf and the Pacific . Kansas has an eastern river front of 15o m. on the Missouri, which is navigable for steamboats of good See also:

size . The See also:internal rivers of the state are not utilized for commercial purposes . See also:Population.—In population Kansas ranked in 1900 and 1910 (1,690,949) twenty-second in the Union . The decennial in-creases of population from 186o to Ig0o were 239.9, 173.4, 43.3 and 3.0%, the population in 1900 being 1,470,495, or 18 to the sq. m2 Of this number 22'5% lived in cities of 2500 or more inhabitants . Nine cities numbered more than Io,000 inhabitants: Kansas City (51,418), Topeka—the state See also:capital (33,608), Wichita (24,671), Leavenworth (20,735), Atchison (15,722), Lawrence—the seat of the state university (1(3,862), Fort Scott (10,322), Galena (10,155) and See also:Pittsburg (10,112) . The life of all of these See also:save the last two goes back to Territorial days; but the importance of Fort Scott, like that of Galena and Pittsburg, is due to the development of the mineral counties in the south-east . Other cities of above 5000 inhabitants were Hutchinson (9379), See also:Emporia (8223), See also: