Book, Paragraph

  1   I,  7 |             when frequent foreshadow wind and drought must be taken
  2   I,  7 |             had been carried up by a wind and fell down in the daytime-then
  3   I,  7 |              For in the gulf a north wind blew and outside it a violent
  4   I,  7 |           outside it a violent south wind. Again in the archonship
  5   I,  10|             is clear and there is no wind. For the vapour could not
  6   I,  10|             sky were clear, and if a wind were blowing it could not
  7   I,  10|           not in cold. For the south wind brings warm, and the north,
  8   I,  10|        wintry weather. For the north wind is cold and so quenches
  9   I,  10|              But in Pontus the south wind does not bring warmth enough
 10   I,  10|            the coldness of the north wind concentrates the heat by
 11   I,  10|              a north than in a south wind. Only the north winds quench
 12   I,  10|           gathered, while in a south wind the evaporation is allowed
 13   I,  13|              in motion and flows, is wind, and that this same air
 14   I,  13|          implying that the nature of wind and water is the same. So
 15   I,  13|             the same. So they define wind as a motion of the air.
 16   I,  13|           that all the winds are one wind, because the air that moves
 17   I,  13| investigation is this: the nature of wind and how it originates, its
 18   I,  13|            one ought to think of the wind as issuing from a sort of
 19  II,  3 |              it is originally a cold wind, for it becomes warm on
 20  II,  3 |              passes over.) The north wind, on the other hand, comb
 21  II,  3 |           just as the south is a dry wind in Libya. So the south wind
 22  II,  3 |          wind in Libya. So the south wind charges the rain that falls
 23  II,  4 |           are specifically distinct, wind and rain obviously differ
 24  II,  4 |           same air when in motion is wind, but when it condenses again
 25  II,  4 |           surrounds us should become wind when in motion, whatever
 26  II,  4 |     interchange.~Further, after rain wind generally rises in those
 27  II,  4 |            when rain has come on the wind ceases. These are necessary
 28  II,  4 |            be the material cause of. wind. Again, suppose this secretion
 29  II,  4 |             secretion is present and wind prevails; the heat is continually
 30  II,  4 |             upper region, and so the wind ceases; then the fall in
 31  II,  4 |             are the causes that make wind cease on the advent of rain,
 32  II,  4 |             fall on the cessation of wind.~The cause of the predominance
 33  II,  4 |            since this evaporation is wind, it is natural that the
 34  II,  4 |            above: before we feel the wind blowing the air betrays
 35  II,  4 |          their motion shows that the wind has begun to blow before
 36  II,  4 |            winds is above. But since wind is defined as "a quantity
 37  II,  4 |         matter and the generation of wind come from below. The oblique
 38  II,  4 |            its generation and origin wind plainly derives from the
 39  II,  4 |          oozes from the earth. Every wind is weakest in the spot from
 40  II,  4 |          observation becomes a great wind as it passes on.~We have
 41  II,  4 |             the nature and origin of wind, the occurrence of drought
 42  II,  4 |            the reason why rain stops wind and wind rises after rain,
 43  II,  4 |              why rain stops wind and wind rises after rain, the prevalence
 44  II,  4 |             south winds and also why wind moves in the way it does.~
 45  II,  5 |           for this is that the north wind I from the arctic regions
 46  II,  5 |           from that time onwards the wind tends to blow continuously.)
 47  II,  5 |         continuously.) But the south wind blows from the tropic of
 48  II,  5 |              just as we have a north wind here, they must have a corresponding
 49  II,  5 |            must have a corresponding wind from the antarctic. This
 50  II,  5 |             from the antarctic. This wind cannot reach us since our
 51  II,  5 |         reach us since our own north wind is like a land breeze and
 52  II,  5 |              is clear that the south wind is not the wind that blows
 53  II,  5 |            the south wind is not the wind that blows from the south
 54  II,  5 |              is neither that nor the wind from the winter tropic.
 55  II,  5 |       symmetry would require another wind blowing from the summer
 56  II,  5 |          since we know that only one wind blows from that quarter.
 57  II,  5 |           that quarter. So the south wind clearly blows from the torrid
 58  II,  5 |         extensive and open the south wind is greater and stronger
 59  II,  5 |             the north than the north wind does to the south.~The origin
 60  II,  6 |           are these. Zephyrus is the wind that blows from A, this
 61  II,  6 |            rises at the equinox. The wind blowing from H, the north,
 62  II,  6 |             north, is the true north wind, called Aparctias: while
 63  II,  6 |              Its contrary is not the wind blowing from E but Lips
 64  II,  6 |          Lips blowing from G but the wind that blows from E which
 65  II,  6 |            solstice, and is the only wind that is diametrically opposite
 66  II,  6 |              have no contraries. The wind they call Thrascias, which
 67  II,  6 |     Aparctias, blows from I; and the wind called Meses, which lies
 68  II,  6 |             or else there would be a wind blowing from the point M
 69  II,  6 |            for then there would be a wind blowing from N, the point
 70  II,  6 |       opposite. (But perhaps a local wind which the inhabitants of
 71  II,  6 |     described Aparctias is the north wind in the strict sense. Thrascias
 72  II,  6 |            south and Lips. East, the wind from the rising of the sun
 73  II,  6 |             and half east. West, the wind from the true west and that
 74  II,  8 |           give rise to a quantity of wind both outside and inside
 75  II,  8 |          outside and inside it. This wind sometimes flows outwards
 76  II,  8 |            naturally moves farthest. Wind satisfies these conditions
 77  II,  8 |         flame and moves rapidly when wind accompanies it): so that
 78  II,  8 |          that some take place when a wind is blowing, but this presents
 79  II,  8 |            an earthquake attended by wind. Only these earthquakes
 80  II,  8 |              inwards the quantity of wind in the earth is greater
 81  II,  8 |          great and therefore violent wind is developed, which would
 82  II,  8 |           they have room for so much wind.~For the same reason earthquakes
 83  II,  8 |           drought the air is full of wind; drought is just the predominance
 84  II,  8 |           the cavities. Thus a great wind is compressed into a smaller
 85  II,  8 |            suppose the action of the wind in the earth to be analogous
 86  II,  8 |            in us by the force of the wind contained in our bodies.
 87  II,  8 |           after passing water as the wind returns inwards from without
 88  II,  8 |             in one volume.~The force wind can have may be gathered
 89  II,  8 |            and spasms are motions of wind, and their force is such
 90  II,  8 |              has continued until the wind that caused it burst through
 91  II,  8 |        finally it burst, and a great wind came out of it and threw
 92  II,  8 |         small particles and then the wind is beaten about and so catches
 93  II,  8 |              the earth. When a south wind is going to blow there is
 94  II,  8 |              back into the earth the wind that was issuing from it.
 95  II,  8 |             being driven on that the wind slips away into the void
 96  II,  8 |             rule be calm because the wind flows back into the earth:
 97  II,  8 |            earthquakes, for when the wind is not part outside earth,
 98  II,  8 |   essentially hot enters the earth. (Wind is not recognized to be
 99  II,  8 |          cold for the same reason as wind.) Well, when this evaporation
100  II,  8 |            line. This is because the wind is leaving the air and dying
101  II,  8 |           sea is to the shore so the wind is to the cloudy air; so,
102  II,  8 |             cloudy air; so, when the wind drops, this very straight
103  II,  8 |           air but is dying away, the wind which causes the earthquake
104  II,  8 |            the air moves again and a wind rises, and does so later,
105  II,  8 |        determined by the quantity of wind and the shape of the passages
106  II,  8 |              from which it forms the wind which we call an earthquake.
107  II,  8 |          noises, too, are due to the wind; sometimes they portend
108  II,  8 |             things more readily than wind. But when the wind is too
109  II,  8 |              than wind. But when the wind is too weak by reason of
110  II,  8 |         cause of the earthquake. The wind is the efficient cause whether
111  II,  8 |                the true cause is the wind.~The combination of a tidal
112  II,  8 |            winds. It occurs when the wind which is shaking the earth
113  II,  8 |            off the sea which another wind is bringing on, but pushes
114  II,  8 |            it follows that when this wind gives way the whole body
115  II,  8 |               driven on by the other wind, will burst out and overwhelm
116  II,  8 |             in Achaea. There a south wind was blowing, but outside
117  II,  8 |         blowing, but outside a north wind; then there was a calm and
118  II,  8 |             there was a calm and the wind entered the earth, and then
119  II,  8 |           sea allowed no exit to the wind that had entered the earth,
120  II,  8 |        struggle with one another the wind caused the earthquake, and
121  II,  8 |              one direction.~When the wind is present in sufficient
122  II,  9 |           say that the same stuff is wind on the earth, and earthquake
123  II,  9 |         flows in one direction it is wind, in another it causes earthquakes;
124 III,  1 |              like those found when a wind is forced from an open into
125 III,  1 |         contrary current, and so the wind forms a circle and eddy.
126 III,  1 |             and becomes a continuous wind) the cloud follows the exhalation
127 III,  1 |             all these phenomena are "wind", and wind is a dry and
128 III,  1 |            phenomena are "wind", and wind is a dry and warm evaporation.
129 III,  1 |               It moves things by its wind in the direction in which
130 III,  3 |               if it is broken up, of wind. For if it does not fade
131 III,  3 |             darkest. It is a sign of wind when it is broken up because
132 III,  3 |              breaking up is due to a wind which exists there but has
133 III,  3 |         support in the fact that the wind blows from the quarter in
134 III,  3 |           calmer: for where there is wind it is clear that no halo
135 III,  4 |           when there is a south-east wind, and everything seems bigger,
136  IV,  9 |             moist nor does it become wind (which is a continuous flow