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, Band 6B. F. Stevens, 1882 |
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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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America appears Aurora Borealis boat body bottom CADWALLADER COLDEN catarrhs cause chimney cloud coals common conductor continued cool Copley Medal DEAR SIR degree descending diameter distance earth EDITOR effect electricity England equal esteem experiment feet fire flame fluid force FRANKLIN funnel give glass Gulf Stream heat hygrometer inches ingenious iron John Pringle JOSEPH PRIESTLEY kind letter light London magic squares matter mentioned mercury miles moisture motion move observed occasion paper particles pass perhaps perspirable Philadelphia Philosophical piece plate pleasure present putrid quantity rarefied received rising river round Royal Society sail salt ship side Sir John Pringle smoke sound specific gravity spout stove suppose surface thermometer thing tion Transit of Mercury transit of Venus upper vapor vessel voyage warm waves weight whirlwind whole wind wood