208 FQREST8 OF NORTH CAROLINA. 



on the best soils attain a height of 90 feet, and on the poorer a 

 height not exceeding TO feet ; and many of the soils, on account 

 of their poorness, are much more snited for a growth of pine than 

 of more exacting broad-leaf trees The white and chestnut oaks 

 grown on the crests of the hills will make trees large enough for 

 railway ties and tan-bark but scarcely larger ; on the moister 

 npper slopes the black and white oaks attain sizes which make 

 them suitable for milling-timber; on the cooler and moister lower 

 slopes the white oak, northern red oak and yellow poplar attain 

 moderately large dimensions and form good timber. The Spanish 

 oak generally reaches only a small size and is often defective; 

 and the same is true of the scarlet oak. Sonrw^ood large enongh 

 to be of value commercially is usually defective. The white pine 

 will certainly do fairly well in a few localities along the western 

 limits of the division, and though at this low elevation it fails to 

 clear the stocks, at least in the forest specimens, as it does at a 

 higher elevation, it is worthy of being protected on account of its 

 rapid growth. Thickets of pure growth will probably form 

 cleaner shafts than where single specimens appear in mixed woods. 

 The broad-leaf trees require such care as was indicated for 

 those of the compact red loams (p. 198). The white pine can be 

 treated in the same way as will be given for the groves of that 

 tree occurring in the high mountains (p. 218). 



FORESTS OF THE MOUNTAIN REGION. 



The differences in the character of the forests of the mountain 

 region are not determined so largely either by the kind of soil or 

 by the amount of moisture contained in it as are those of the 

 Piedmont plateau and coastal region. Within short distances 

 among the mountains there are wide variations in elevation. 

 With increased elevation a rapid lowering of the average annual 

 temperature takes place, and a proportional shortening in the 

 growing-season ; increase in the rain-fall and relative humidity, 

 and a decrease in evaporation both directly from the soil and 

 through transpiration. The effect of these factors in limiting the 

 distribution of certain species is more evident than that of the 

 soils; though, between certain limits of elevation, changes in the 



