1124 



OHIO 



the state, in most localities the products being for the 

 home demand only, but large concerns at Painesville, 

 Oalla, Springfield and Dayton have an immense ship- 

 ping trade of plants, the mailing trade being particu- 

 larly largo. Out-flowers are grown in considerable 

 quantities also, the principal ctiitcrs being Cleveland 

 and Cincinnati. Large iiur-o, ..iii.r. . xist at Paines- 

 ville, on the lake short-, afi! n !' ^1 m mi valley, near 

 Dayton and Troy. Th< -: i !i-^e and other 



nurseries of the state c»'ii-i -I - m ^ ..i Iruit trees and 



small fruit plants. Oruum. iiuJ un,-. and plants are 

 grown in comparatively limited quantities, for the rea- 

 son that landscape gardening and ornamental planting 

 have not been given due attention. More or less pre- 

 tentious park systems are in a state of development in 

 some of the larger cities, Cincinnati, Cleveland and 

 Toledo leading in this i-espect. A number of cemeteries 

 show considerable care in maintenance and some skill 

 in planting, but well-arranged private grounds are rare. 

 Spring Grove cemetery, in Cincinnati, was one of the 

 first large landscape cemeteries in the world. Mount 

 Auburn, in Cambridge, was the first rural cemetery in 

 this country. See Laiidsrftpe Gardening and Strauch. 



While landscape art i^ in a rather backward condition 

 within the state, tli. v i^ rpnt.- a fund of accumulated 

 knowledge retiai-.liTi- ili.- .fliptaliility of species and 

 varieties of trei-^ .niil i-i^mi- i-- this climate. It would 

 be too broad a .--tat. m, nt t,, ^ay that foreign species do 

 not succeed here, but so manv have been disappointing 

 that there seems to be little 'of any value left. Fortu- 

 nately there is an abundance of suitable material in our 

 own and neighboring states. 



Ohio is a great agricultural state, and this fact has 

 somewhat retarded horticultural development, but, on 

 the other hand, large manufacturing Interests have had. 

 and will continue to have, the opposite effect, and Ohio 

 will in the near future take high rank as a horticul- 

 tural state. -Rr, J. (Jkkkn. 



OELAHOHA. HOKTICULTUBAL POSSIBILITIES 



OF. Fig. 131i). The northern boiindars- ..f Okial,..ina 



is X7° north latitude. The southern 



boundary is an irregular line, bm 



does not extend far .south of the S.'itli 



parallel. Except a small strip which 



extends to the I03d meridian, most of 



the territory lies between 96° 30' west 



and 100° west longitude. The greater 



portion of the country has an altitude 



of 800 to 1,400 feet. The surface of 



the country is rolling prairie, with 



numerous small rivers and creeks 



flowing east. The longer streams are 



wide, shallow, and very sandy. The 



shorter streams are narrow and have 



high, steep banks. In the eastern 



half there are considerable areas 



covered with timber, the greater part 



of which is black-jack and post-oak. 



Elm. Cottonwood, pecan, hickory, red 



cedar, walnut, hackberry and honey 



locust are common, but do not form 



separate forests as the oaks do. In 



the western part timber belts follow 



the streams, and in the extreme western part only brush 



and small trees are found. The soil is usually a fine 



sand, the particles lying very compactly. 



Previous to the settlement of the country, in 1889, the 

 prairies were burned off each year. This kept the soil 

 poor in humus. There is very little clay soil in the terri- 

 tory except along the small streams, the bottomlands of 

 which contain considerable clay. The soil is fertile and 

 contains a good supply of plant-food. The subsoil is 

 very compact, usually joint-clay, where the surface soil 

 is a black or gray color: but the red or brown loam sur- 

 face soil is usually underlaid with a more loose and 

 mellow subsoil. The black and gray soils are usually 

 found at greater altitudes, and are seldom covered with 

 timber. Often these soils contain large quantities of 

 alkali, and the well and spring water in such localities is 

 very poor. Stone is abundant in some sections and 

 very scarce in others, but there is not enough surface 

 rock to be a factor in controlling the .amount of till- 



OKLAHOMA 



able land. Red and gray sandstone are the most abuii- 



The extremes of temperatun- l>.-t«.-. u summer and 

 winter are great. In soint- |.1;m-i-- iIh- t.-mperature 

 reaches zero during the most ^.-\.-rt- -ri.mis nf winter. 

 Except during occasional stc.nn^. th. --, m'. i is mild and 

 usually dry. A snowfall of ih'-ji -' ■: - li>-s indepth 

 is arre.and soon melts. PI" > t, . t i ,, t such farm 

 work may be done nearly ail ' -l' the sum- 

 mer a maximum of 100°'F. i- I i. , , hcd. The 



high temperature is nearly al...i_v.> .i. , ..lupauied by a 

 dry wind. In the hottest weather the nights are cool 

 and refreshing. The average mean temperature is 

 about 00°. The wind is a prominent factor in the climate 

 of Oklahoma. The prevailing wind is from the south 

 during most of the year. The air is dry, and the wind 

 and hot sun dry the soil rapidly. The rainfall usually 

 is light during July and August, and the warm, dry 

 winds from the south and southwest make this the most 

 tryiiiiT sea-nii fur vegetation. The wind is so strong and 

 ,-i.ii-i:iiit til It it 1I...-S considerable damage to young trees 

 ami \ ill- - mill -- they are protected by some form of 

 wiiict I.]. Ml^. .Miiiry snow and rain storms are accom- 

 pauit-tl by Uarti winds, which are seldom destructive. 



The average annual rainfall for the territory is about 

 30 in. For the eastern half it is about 33 in., and gradu- 

 ally decreases to about 20 in. in the extreme western 

 part. The rainfall for any one year varies greatly in 

 different localities, and these areas of light and heavy 

 precipitation are variable in size, shape and location 

 from year to year. The line of average equal rainfall 

 runs almost north and south, bearing to the west in the 

 southirii |.art of the territory. The winter and late 

 sutiiiiii r ate i!ry. Light snows fall during January, 

 Fi-lri-iiaiy and .March, but usually melt in two or three 

 .Itiy- Sui.w -ti.rnis seldom reach the southern portion, 

 tiiiiii-- ';-lii ■■ inn they do. The rain and snow storms, 



■ liii 1- M-tption, travel from west and north to 



I- riiey travel very rapidly and last only 



1 lieavicst rains last only a few hours. 



^li-\' - iin 111 r:(i-i_-, and ctmie only during the colder 



1519. Geographical features of Oklahoma. 



part of the year. In 1897 there were about 230 days of 

 sunshine, which is about the average. There is very 

 little .lark. foETtry weather; and heavy dews, though 



coiiiinoTi, ar-.- )niii-li lii.'lit.-iied by the almost 



Im- lii-i.t i-t tMsiaii a may be said to be a mixture 



111- i|..r-;i- lit' Kansas ami Texas, there being few spe- 



■ t.-un.| li' r. that are not found in one or both of 



-' 1 r- - Fin- predominance of yellow flowers is 



i-t it- ni'-t prnininent characteristics. The botani- 



!l : - I the country are far from complete, 



I - - '-iiitugh to justify the statement that 



' I very extensive one. The number of 



- is very small, and only a small por- 



. I III iit-es. "The trees are usually low and 



i-ii i.iai,, lji.tl. and give a poor quality of lumber, 



ch i.s, no doubt, partly due to the annual burning, 



, neither represents the quality or quantity of tini- 



which the country is capable of producing when 



