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CRATER

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Originally appearing in Volume V07, Page 381 of the 1911 Encyclopedia Britannica.
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CRATER , the cavity at the mouth of a volcanic duct, usually See also:

funnel-shaped or presenting the See also:form of a bowl, whence the name, from the Gr. Kpari]p, a bowl. A volcanic See also:hill may have a single crater at, or near, its See also:summit, or it may have several See also:minor craters on its flanks: the latter are sometimes called " See also:adventitious craters " or " craterlets." Much of the loose ejected material, falling in the neighbourhood of the vent, rolls down the inner See also:wall of the crater, and thus produces a stratification with an inward See also:dip. The crater in an active See also:volcano is kept open by intermittent explosions, but in a volcano which has become dormant or See also:extinct the vent may become plugged, and the bowl-shaped cavity may subsequently be filled with See also:water, forming a crater-See also:lake, or as it is called in the See also:Eifel a Maar. In some basaltic cones, like those of the See also:Sandwich Islands, the crater may be a broad shallow See also:pit, having almost perpendicular walls, with See also:horizontal stratification. Such hollows are consequently called pit-craters. The name caldera (Sp. for cauldron) was suggested for such pits by Capt. C. E. Dutton, who regarded them as having been formed by subsidence of the walls. The See also:term caldera is often applied to bowl-shaped craters in See also:Spanish-speaking countries.

End of Article: CRATER

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