meteorology-第8章
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neighbourhood of mountains and of high ground; whereas if we except
rivers; water rarely appears in the plains。 For mountains and high
ground; suspended over the country like a saturated sponge; make the
water ooze out and trickle together in minute quantities but in many
places。 They receive a great deal of water falling as rain (for it
makes no difference whether a spongy receptacle is concave and
turned up or convex and turned down: in either case it will contain
the same volume of matter) and; they also cool the vapour that rises
and condense it back into water。
Hence; as we said; we find that the greatest rivers flow from the
greatest mountains。 This can be seen by looking at itineraries: what
is recorded in them consists either of things which the writer has
seen himself or of such as he has compiled after inquiry from those
who have seen them。
In Asia we find that the most numerous and greatest rivers flow from
the mountain called Parnassus; admittedly the greatest of all
mountains towards the south…east。 When you have crossed it you see the
outer ocean; the further limit of which is unknown to the dwellers
in our world。 Besides other rivers there flow from it the Bactrus; the
Choaspes; the Araxes: from the last a branch separates off and flows
into lake Maeotis as the Tanais。 From it; too; flows the Indus; the
volume of whose stream is greatest of all rivers。 From the Caucasus
flows the Phasis; and very many other great rivers besides。 Now the
Caucasus is the greatest of the mountains that lie to the northeast;
both as regards its extent and its height。 A proof of its height is
the fact that it can be seen from the so…called 'deeps' and from the
entrance to the lake。 Again; the sun shines on its peaks for a third
part of the night before sunrise and again after sunset。 Its extent is
proved by the fact that thought contains many inhabitable regions
which are occupied by many nations and in which there are said to be
great lakes; yet they say that all these regions are visible up to the
last peak。 From Pyrene (this is a mountain towards the west in
Celtice) there flow the Istrus and the Tartessus。 The latter flows
outside the pillars; while the Istrus flows through all Europe into
the Euxine。 Most of the remaining rivers flow northwards from the
Hercynian mountains; which are the greatest in height and extent about
that region。 In the extreme north; beyond furthest Scythia; are the
mountains called Rhipae。 The stories about their size are altogether
too fabulous: however; they say that the most and (after the Istrus)
the greatest rivers flow from them。 So; too; in Libya there flow
from the Aethiopian mountains the Aegon and the Nyses; and from the
so…called Silver Mountain the two greatest of named rivers; the
river called Chremetes that flows into the outer ocean; and the main
source of the Nile。 Of the rivers in the Greek world; the Achelous
flows from Pindus; the Inachus from the same mountain; the Strymon;
the Nestus; and the Hebrus all three from Scombrus; many rivers;
too; flow from Rhodope。
All other rivers would be found to flow in the same way; but we have
mentioned these as examples。 Even where rivers flow from marshes;
the marshes in almost every case are found to lie below mountains or
gradually rising ground。
It is clear then that we must not suppose rivers to originate from
definite reservoirs: for the whole earth; we might almost say; would
not be sufficient (any more than the region of the clouds would be) if
we were to suppose that they were fed by actually existing water
only and it were not the case that as some water passed out of
existence some more came into existence; but rivers always drew
their stream from an existing store。 Secondly; the fact that rivers
rise at the foot of mountains proves that a place transmits the
water it contains by gradual percolation of many drops; little by
little; and that this is how the sources of rivers originate。 However;
there is nothing impossible about the existence of such places
containing a quantity of water like lakes: only they cannot be big
enough to produce the supposed effect。 To think that they are is
just as absurd as if one were to suppose that rivers drew all their
water from the sources we see (for most rivers do flow from
springs)。 So it is no more reasonable to suppose those lakes to
contain the whole volume of water than these springs。
That there exist such chasms and cavities in the earth we are taught
by the rivers that are swallowed up。 They are found in many parts of
the earth: in the Peloponnesus; for instance; there are many such
rivers in Arcadia。 The reason is that Arcadia is mountainous and there
are no channels from its valleys to the sea。 So these places get
full of water; and this; having no outlet; under the pressure of the
water that is added above; finds a way out for itself underground。
In Greece this kind of thing happens on quite a small scale; but the
lake at the foot of the Caucasus; which the inhabitants of these parts
call a sea; is considerable。 Many great rivers fall into it and it has
no visible outlet but issues below the earth off the land of the
Coraxi about the so…called 'deeps of Pontus'。 This is a place of
unfathomable depth in the sea: at any rate no one has yet been able to
find bottom there by sounding。 At this spot; about three hundred
stadia from land; there comes up sweet water over a large area; not
all of it together but in three places。 And in Liguria a river equal
in size to the Rhodanus is swallowed up and appears again elsewhere:
the Rhodanus being a navigable river。
14
The same parts of the earth are not always moist or dry; but they
change according as rivers come into existence and dry up。 And so
the relation of land to sea changes too and a place does not always
remain land or sea throughout all time; but where there was dry land
there comes to be sea; and where there is now sea; there one day comes
to be dry land。 But we must suppose these changes to follow some order
and cycle。 The principle and cause of these changes is that the
interior of the earth grows and decays; like the bodies of plants
and animals。 Only in the case of these latter the process does not
go on by parts; but each of them necessarily grows or decays as a
whole; whereas it does go on by parts in the case of the earth。 Here
the causes are cold and heat; which increase and diminish on account
of the sun and its course。 It is owing to them that the parts of the
earth come to have a different character; that some parts remain moist
for a certain time; and then dry up and grow old; while other parts in
their turn are filled with life and moisture。 Now when places become
drier the springs necessarily give out; and when this happens the
rivers first decrease in size and then finally become dry; and when
rivers change and disappear in one part and come into existence
correspondingly in another; the sea must needs be affected。
If the sea was once pushed out by rivers and encroached upon the
land anywhere; it necessarily leaves that place dry when it recedes;
again; if the dry land has encroached on the sea at all by a process
of silting set up by the rivers when at their full; the time must come
when this place will be flooded again。
But the whole vital process of the earth takes place so gradually
and in periods of time which are so immense compared with the length
of our life; that these changes are not observed; and before their
course can be recorded from beginning to end whole nations perish
and are destroyed。 Of such destructions the most utter and sudden
are due to wars; but pestilence or famine cause th