intervall N22NOMPN que CONJ mont N33GENPM maxi ADJ11VOCSMSUPER recipi V31PRESACTIVEIND3P imbr N31NOMPM et CONJ propter PREPACC silv N11GENPF crebritat N31ACCSF niv N33NOMPF ab PREPABL umbr N11LOCPF arbor N31GENPF et CONJ mont N33GENPM ibi ADVPOS diutius ADVCOMP conserv V11PRESPASSIVEIND3P deinde ADVPOS liquat VPAR11GENSFPERFPASSIVEPPL per PREPACC terr N11GENSF ven N11ACCPF col V11PRESPASSIVEIND3P et CONJ it VPAR61NOMSFPERFPASSIVEPPL perveni V41PRESACTIVEIND3P ad ADVPOS infi ADJ11ACCPFSUPER mont N33GENPM radic V11PRESACTIVESUB2S ex PREPABL qu PRON10DATPX proflu VPAR31NOMPCPRESACTIVEPPL font N33GENPM erump V31PRESACTIVEIND3P fruct VPAR31NOMSMPERFPPL
Valleys between mountains are subject to much rain, and because of the dense forests, snow stands there longer under the shadow of the trees and the hills. Then it melts and percolates through the interstices of the earth and so reaches to the lowest spurs of the mountains, from which the product of the springs flows and bursts forth.
final_alignments\Vitruvius_Architecture_Book_8.json