CLIMATE OF LOWER DIVISIO^ST OF COAST PINE BELT. 



Ill 



a height of from l'20 to 300 feet above the tiat woods and marshes and 

 alluvial forests of the tide-watev region. Where the level table-h\nds, 

 devoid of surface drainage, are underlaid by impervious olavs, spongy 

 bogs surround the iieads of water courses. On the rolling uplands 

 with a porous siliceous soil the copious rainfall is readily absorbed, 

 giving rise to innumerable springs, the feeders of the numerous limpid 

 brooks and creeks by which this region is traversed. The area of the 

 lower pine region is estimated to embrace a little over 7,000 square 

 miles, including the following counties and parts of counties: Geneva, 

 part of Covington. Escambia, part of Monroe, ami all oi Baldwin, 

 Mobile, and AVashington. 



Both the climate and topography oi this region exhibit great uni- 

 formity. Under the moderating influences of the proximity of the 

 sea, the climate is generally mild. According to the records of the 

 Mobile station of the United States Weather Bureau, extending over 

 a period of twenty-three years, the mean annual temperature for that 

 period was 66.9°, with the highest temperature 101 . observed in 

 July, lS8-t. and the lowest lU. in January, 1886.' 



Mean inoiitldi/ tciupernture irith miu'ima atid mim7»a. 



Dafa of tempcraiure by seasons for period of twetitiHhrec years. 



The latest killing frost for the juM-iod occurred .V]>iil I'l. 1884. The 

 average date of last frost in spring was Mar»ii 'JO. TJic :i\ (Mage date 

 of earliest frost in autumn was November i*(». 



The following data were obtained from Mr. J. A. Barrv. observer 

 for the Weather Bureau at Mobile: 



Jhila of rainfall aixl clouds. 



'See footnote ', p. 26. 



