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¶ Of Rayne.
AFter the generatiō of cloudes is wel knowen, it shall not be hard to learn,* 1.1 from whence the rayne commeth.
For after the matter of the cloud be∣ing drawen vp, and by cold made thick, (as is sayde before) heate followynge, which is moste commenlye of the Sou∣therne wynde, or any other wynde of hotte temper, doth resolue it againe into water, so it falleth in droppes, to geue encrease of fruit to the earth, and moue men to geue thankes to God.
There be small showers, of small droppes, and there be great stormes of great droppes.
The showers with small drops, pro∣ceade either of the small heat, that resol∣ueth the cloudes, or els of the great di∣staunce of the cloudes from the earth.
The streames with great droppes, contrariwyse, doe come of greate heate, resoluing or melting the cloude, or els of smal distaunce from the earth. Wher¦of we sée an experiment when water is powred forth, from an highe place, the droppes are smalle, but if it be not from height, it wyll either haue no droppes