THERE HAILSTORMS START!
point of a hail-storm hi of air laden with waterj Wwes rapidly through varygrees of temperature, which l * le P arl ‘ L 'les of water and I* them and re-freeze them, rj other particles as the jourIJtoinues. . *"4ones, m falling, are some,rrie(l h< !ow the central part t’.fc’tn which gave birth to successive layers of i w!| j°h accounts for la, ‘ resulant stone is k, a nu| nb**r of disrinct coat- . ® kinS ° f Itn onioneDtly hai>{»en.s ihat a con»h U ? nti ' l - iis froz ‘n vaby ,hf * ac tion of the to th. n \ r “ n,r “ 01 ,l “* tornado, n* f • f ° rr ° rf * asf * s abrupfV r ,lcl “ s become too heavy 1 Ue d l,y - ,h ' ; wind. they to * ear th in an almost solid l*,;""' 1 ;'" boiween hail'>Pid'y Un< h T f SI " r "‘ S ' S becaus, ‘ . f ‘- s h'f'tng degrees of “'I f,,,, "'' !l accompany the also explains V. / ms occur usually In the wh "' lhe oer -slornis take place.
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Bibliographic details
Waipawa Mail, Volume XXXVIII, Issue 8513, 5 August 1921, Page 5 (Supplement)
Word Count
167THERE HAILSTORMS START! Waipawa Mail, Volume XXXVIII, Issue 8513, 5 August 1921, Page 5 (Supplement)
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