单词 | katavothron |
释义 | katavothronn. A subterranean channel or deep chasm formed by the action of water. ΘΚΠ the world > the earth > water > rivers and streams > stream > [noun] > underground swallet1668 katavothron1820 under-runner1921 the world > the earth > land > landscape > low land > hole or pit > [noun] > pot-hole or swallow-hole water sink1553 swallow1610 swallow-hole1660 estuary1665 swallet1668 cockpit1683 sinkhole1772 sink1791 pot1797 water-swallow1811 shake-hole1823 pothole1826 fleet-hole1839 spout hole1849 katavothron1869 ponor1890 sump1951 1820 T. S. Hughes Trav. Sicily II. xii. 311 A lake whose superfluous waters are carried off by a catabothron or subterranean channel. 1833 C. Lyell Princ. Geol. III. 144 The gulphs (katavothrons) of the plain of Tripolitza have swallowed up of late years thousands of human bones. 1846 G. Grote Hist. Greece II. ii. viii. 596 Tegea and Mantineia—conterminous towns..separated by one of those capricious torrents which only escapes through katabothra. 1869 H. F. Tozer Res. Highlands of Turkey I. vii. 160 The Mediævals..had the idea of there being a catavothra from the lake. 1878 Encycl. Brit. VIII. 685/2 The subterranean course of the streams is frequently indicated by peculiar vents or pits caused by the subsidence of the soil; they are popularly known in Greece as catavothra. 1892 A. J. Jukes-Browne Student's Handbk. Physical Geol. (ed. 2) xi. 197 The torrents of the Morea are usually charged with reddish mud, sand, and pebbles, when they enter the katavothra, but are pure and limpid when they flow out again. 1892 Proc. Royal Geogr. Soc. 14 466 (heading) The katavothræ of the Morea. 1892 Proc. Royal Geogr. Soc. 14 467 All these basins are drained by underground channels, to the entrance of which the name katavothra is given. 1937 Geogr. Jrnl. 90 448 Since the water was drawn off, the mouths of twenty-five large katavothrai..have appeared in the sides of the surrounding hills. 1957 G. E. Hutchinson Treat. Limnol. I. i. 107 Though these variations [in level] can in part depend on rainfall, they are largely independent of it and may be attributed to the silting of the katavothrai or sinks which drain the lake. 1970 Water-Supply Paper U.S. Geol. Surv. No. 1899 -K. 11/2 Katavothron, a closed depression or swallow hole. 1971 J. N. Jennings Karst v. 74 The French name estavelle is commonly used for these alternating orifices but they are also well known by the Greek katavothre. This entry has not yet been fully updated (first published 1976; most recently modified version published online March 2021). < |
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