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10.1). tem- heat materials the to upwelling a 211
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of surface function a is Earth, the within of ability rates flow igneous (young Earth of the “N Heat Heat flow refers to the amount crosses the amount of time. The 0.08 W/m’. equivalent to 107~* cal/cem?/s, or 1.9
temperate), the
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R47 [|OE. hatu), the quality of being hot; energy manifest by < L. |< degree of hotness; the amount of heat per unit mass of a matcrial. adj., having to do thar'm'l gra’ the from a across production the the of regions 10.2). shallow at material through
Poe Flow the accelerated vibration of molecules vi., |OE. heat flow (het fld) n., the rate of transfer of heat from (tem' prachar) n., < 5). (Gr. ged- n., (gra'dé ant) |< of a road: the rate of change of a parameter. (je' 6 in temperature with increasing depth outward flow heat Earth, the different (Fig. heat material hot of cold cooling of material ridge).
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i
Earth's NJ: Cliffs, E. W. mag- and to Blackwell Earth's pp. and Monograph Magnetic ridge. tecton- and Geophysical A. D. Cambridge: anom-
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