REVEGETATION OF TAAL VOLCANO 



203 



Vae«tr-.tea 



shadtd crith 

 ilngls liTtfs: 

 #1 Indicates 



#t InJlCites -v-v 



pTtng (thicketf), ^3 



or btaboo. 



Ar«A« vtiich are 

 cross lined \r*re 

 tnor.x ovsr In ?«hru- 

 »rji or *ftrch 1?13. 



Intrrrv.pteA 

 lines within 

 th« er»t«r 

 lAka tnelofe 

 btttblln* 



«*nt In 

 »*ren 1?18. 



Th» COTtenar lines royrcff»nt conditions e— ^b .ri,e,«r,a.,<, 



previottf to ths oruytion off If 11. Only in co..o«r .^..rv.i is , 



^5!2*v?^ '^ *** ■'^^J Tw-^hsld go^d. Con- =»-<"-«*';«"«»» 



sldjTAbla ohan«o hfts taken piwe east and w«3t 



SLiS.rt^'I'v^'*^ *'^*=''* **"* ^"^8 b«en ehn7i«<i 

 ,fOf»»i9\at by ffubiDtrgsnce, * 



Fig. 3. Map of Taal Volcano, showing the area revegetated up to March, 

 1915. 



The development of the dipterocarp forest, normal for such 

 altitudes in this region, is possible, although very improbable, 

 for accidents in the shape of eruptions are likely to intervene, 

 before it has had sufficient time to develop. Dipterocarps are 



