The Works of Benjamin Franklin: Containing Several Political and Historical Tracts Not Included in Any Former Edition, and Many Letters Official and Private Not Hitherto Published : with Notes and a Life of the Author, Band 6Tappan, Whittemore, and Mason, 1838 |
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Seite 107
... upper end of the race , where the water is last in motion . We have on this continent a long ridge of mountains running from northeast to south- west ; and the coast runs the same course . These may , perhaps , contribute towards the ...
... upper end of the race , where the water is last in motion . We have on this continent a long ridge of mountains running from northeast to south- west ; and the coast runs the same course . These may , perhaps , contribute towards the ...
Seite 131
... upper air may be more condensed by cold , than the lower air by pressure ; the lower more ex- panded by heat than the upper , for want of pressure In such case the upper air will become the heavier , the lower the lighter . The lower ...
... upper air may be more condensed by cold , than the lower air by pressure ; the lower more ex- panded by heat than the upper , for want of pressure In such case the upper air will become the heavier , the lower the lighter . The lower ...
Seite 148
... upper region , they may indeed descend in the spout or whirl- wind ; but then , when the united current reached the earth or water , it would spread , and , probably , blow every way from the centre . There may be whirlwinds of both ...
... upper region , they may indeed descend in the spout or whirl- wind ; but then , when the united current reached the earth or water , it would spread , and , probably , blow every way from the centre . There may be whirlwinds of both ...
Seite 150
... upper ; consequently , specifically lighter . The coldness of the upper region is manifested by the hail , which sometimes falls from it in a hot day . 2. That heated air may be very moist , and yet the moisture so equally diffused and ...
... upper ; consequently , specifically lighter . The coldness of the upper region is manifested by the hail , which sometimes falls from it in a hot day . 2. That heated air may be very moist , and yet the moisture so equally diffused and ...
Seite 153
... upper end it becomes visible , by the warm air brought up to the cooler region , where its moisture begins to be con- densed into thick vapor by the cold , and is seen first at A , the highest part , which being now cooled , con- denses ...
... upper end it becomes visible , by the warm air brought up to the cooler region , where its moisture begins to be con- densed into thick vapor by the cold , and is seen first at A , the highest part , which being now cooled , con- denses ...
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air-box appears ascending boat body bottom CADWALLADER COLDEN cause chimney cloud cold air common condensed conductor continually Copley Medal DEAR SIR degree descending distance earth EDITOR effect electricity England equal experiments fire fire-place fluid force FRANKLIN give glass heat humble servant hygrometer inches ingenious JARED ELIOT JOHN PERKINS JOSEPH PRIESTLEY kind less letter light London magic squares matter mentioned mercury miles moisture motion move nature observed occasion paper particles pass perhaps perspirable Philadelphia Philosophical piece plate pleasure present printed putrid quantity rain rarefied received red clover rising river round Royal Society sail salt ship side Sir John Pringle smoke sound specific gravity spout stoves suppose surface thing tion Transit of Mercury transit of Venus vapor vessel warm water-spouts waves weight whirl whirlwind whole wind wood