Online Encyclopedia

WATERFALL

Online Encyclopedia
Originally appearing in Volume V28, Page 368 of the 1911 Encyclopedia Britannica.
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WATERFALL  , a point in the course of a stream or

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river where the
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water descends perpendicularly or nearly so . Even a very small stream of water falling from any considerable height is a striking
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object in scenery . Such falls, of small
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volume though often of immense
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depth, are
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common, for a small stream has not the power to
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erode a steady slope, and thus at any considerable irregularity of level in its course it forms a fall . In many mountainous districts a stream may descend into the valley of the larger river to which it is tributary by way of a fall, its own valley having been eroded more slowly and less deeply than the main valley .
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Mechanical considerations apart, the usual cause of the occurrence of a waterfall is a sudden change in
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geological structure . For example, if there be three horizontarl strata, so laid down that a hard stratum occurs between twosoft ones, a river will be able to grade its course through the upper or
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lower soft strata, but not at the same
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rate through the intermediate hard stratum, over a ledge of which it will consequently fall . The same will occur if the course of the river has been interrupted by a hard barrier, such as an intrusive dyke of
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basalt, or by glacial or other deposits . Where a river falls over an escarpment of hard rock overlying softer strata, it powerfully erodes the soft rock at the
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base of the fall and may undermine the hard rock above so that this is broken away . In this way the river gradually cuts back the point of fall, and a
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gorge is
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left below the fall . The classic example of this
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process is provided by the most famous falls in the world—Niagara . WATER-FLEA, a name given by the earlier microscopists (Swammerdam, 1669) to certain minute aquatic
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Crustacea of the order Cladocera, but often applied also to other members of the division
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Entomostraca (q.v.) . The Cladocera are abundant everywhere in fresh water .

One of the commonest

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species, Daphnia pulex, found in ponds and ditches, is less than one-tenth of an inch in length and has the
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body enclosed in a trans-parent bivalved shell . The head, projecting in front of the shell, bears a pair of branched feathery antennae which are the chief swimming
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organs and propel the animal, in a succession of rapid bounds, through the water . There is a single large black eye . In the living animal five pairs of leaf-like limbs acting as gills can be observed in constant motion between the valves of the shell, and the pulsating heart may be seen near the dorsal
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surface, a little way behind the head . The body ends behind in a kind of tail with a double curved claw which can be protruded from the dell . The
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female carries the eggs in a brood-chamber between the back of the body and the shell until hatching takes place . Through-out the greater
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part of the
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year only
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females occur and the eggs develop " parthenogenetically," without fertilization . When the small
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males appear, generally in the autumn, fertilized " winter " or " resting eggs " are produced which are cast adrift in a case of " ephippium " formed by a specially modified part of the shell . These resting eggs enable the
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race to survive the cold of winter or the drying up of the water . For a fuller account of the Cladocera and of other organisms which sometimes share with them the name of " water-fleas," see the article ENTOMOSTRACA . (W . T .

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