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| Alphabetical [« »] refutation 1 regard 1 regards 2 region 53 regions 15 regular 3 regularity 1 | Frequency [« »] 54 vapour 53 kind 53 part 53 region 53 why 52 nature 52 salt | Aristotle Meteorology IntraText - Concordances region |
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1 I, 1 | They take place in the region nearest to the motion of 2 I, 3 | our treatment of the upper region, but we may return to the 3 I, 3 | why the stars in the upper region impart heat to the earth 4 I, 3 | earth and the colder that region is. For it is neither appreciably 5 I, 3 | if the whole of that vast region is vapour, the amount of 6 I, 3 | already been said. The upper region as far as the moon we affirm 7 I, 3 | not formed in the upper region to be this: that it is filled 8 I, 3 | of clouds in that upper region is also prevented by the 9 I, 3 | squeezed out into the upper region and it sinks, and other 10 I, 3 | exhalation. Thus the one region is always full of air and 11 I, 3 | not occur in that upper region but below: yet the more 12 I, 4 | phenomenon is formed in the upper region it is due to the combustion 13 I, 6 | water to itself because that region is dried up by the sun on 14 I, 7 | begins to gather in the lower region independently the comet 15 I, 7 | this stuff collects in the region of the milky way.~ 16 I, 8 | this circle and that this region was scorched or met with 17 I, 8 | and especially in that region in which the stars are biggest 18 I, 8 | tropic circles. Besides the region is full of the biggest and 19 I, 8 | off and gathered into this region.~We have now explained the 20 I, 8 | affections that appear in that region.~ 21 I, 9 | us go on to treat of the region which follows next in order 22 I, 9 | surrounds the earth. It is the region common to water and air, 23 I, 9 | dispersing to the higher region, in part quenched through 24 I, 10| way that it does in the region of the clouds.~ 25 I, 11| amount of vapour, for the region from which and the time 26 I, 11| hand is found in the upper region, but the corresponding phenomenon 27 I, 11| phenomenon in the vaporous region near the earth is lacking. 28 I, 11| said, to snow in the upper region corresponds hoar-frost in 29 I, 11| and to rain in the upper region, dew in the lower. But there 30 I, 11| correspond to hail in the upper region. Why this is so will be 31 I, 12| water freezing in the upper region. It cannot have frozen before 32 I, 12| thrust up into the cold upper region.~Now we see that warm and 33 I, 13| appear to differ owing to the region from which the air may happen 34 I, 13| height and extent about that region. In the extreme north, beyond 35 I, 13| sufficient (any more than the region of the clouds would be) 36 I, 14| advantage to them for the whole region to have become navigable; 37 I, 14| been flowing, but that the region whence they flow was once 38 II, 2 | of fire is in the upper region; that of air occupies the 39 II, 2 | the place next inside the region of fire; while the mass 40 II, 2 | vapour and rises to the upper region, where it is condensed again 41 II, 4 | off, rising to the upper region, and so the wind ceases; 42 II, 5 | and not from the antarctic region.~There are two inhabitable 43 II, 5 | Crown, too, moves over this region: for it is in the zenith 44 II, 5 | we see that the inhabited region is limited in breadth, while 45 II, 5 | the whole breadth of the region we dwell in up to the uninhabited 46 II, 5 | Now since there must be a region bearing the same relation 47 II, 5 | reach the limits of the region we live in. The prevalence 48 II, 5 | clearly blows from the torrid region. Now the sun is so near 49 II, 5 | the sun is so near to that region that it has no water, or 50 II, 6 | reason for this is that the region in which we live lies nearer 51 II, 9 | heat escapes to the upper region and leaves them. This explains 52 II, 9 | escapes disperses to the up region. But if any of the dry exhalation 53 III, 6 | various effects in the upper region, so here it causes two varieties