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WATERFALL

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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 See also:

river where the See also:water descends perpendicularly or nearly so. Even a very small stream of water falling from any considerable height is a striking See also:object in scenery. Such falls, of small See also:volume though often of immense See also:depth, are See also:common, for a small stream has not the See also:power to See also: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 See also:main valley. See also:Mechanical considerations apart, the usual cause of the occurrence of a waterfall is a sudden See also:change in See also: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 See also:lower soft strata, but not at the same See also: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 See also:basalt, or by glacial or other deposits. Where a river falls over an escarpment of hard See also:rock overlying softer strata, it powerfully erodes the soft rock at the See also: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 See also:gorge is See also:left below the fall. The classic example of this See also:process is provided by the most famous falls in the See also:worldSee also:Niagara. WATER-See also:FLEA, a name given by the earlier microscopists (See also:Swammerdam, 1669) to certain See also:minute aquatic See also:Crustacea of the See also:order Cladocera, but often applied also to other members of the See also:division See also:Entomostraca (q.v.). The Cladocera are abundant everywhere in fresh water.

One of the commonest See also:

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

End of Article: WATERFALL

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