| 释义 |
lapiés, n. pl. Geomorphol.|ˈlæpjeɪz, ˈlæpɪeɪz|
Also lapiaz, lapies, lapiez.
[a. F. dial. lapiaz, lapiés pl. (used in the Jura), f. pop.L. *lapida f. L. lapis stone.]
a. (Const. as pl.) = karren, Karren n. pl.; also (const. as sing.), a karrenfeld.
1902, etc. [see karren, Karren]. 1903Geogr. Jrnl. XXI. 328 The surface formation met with most commonly in limestone districts, which is usually known by the German term Karren, or the French Lapiaz. 1921Geogr. Rev. XI. 594 The identification of ‘karren’ and ‘lapiez’ is taken from Eugène Renevier's ‘Monographie des Hautes Alpes Vaudoises’ (Matériaux pour la carte géol. Suisse), p. 499. Ibid. 598 The name adopted by Professor Cvijič is ‘lapiez’, which is the term used in the French Jura. 1924J. Cvijič in Geogr. Rev. XIV. 27 Lapiés are found at all altitudes from sea level to lofty mountain summits. They were first observed and described in the limestone alps of Switzerland, where in the cantons of German speech they are called Karren or Schratten and in districts of French speech lapiéz or lapiaz or lapiés. Ibid. 40 Lapiés are formed principally by chemical erosion of limestone surfaces by meteoric water. Ibid. 44 Typical lapiés occur chiefly on moderately steep slopes. Ibid., Scattered limestone monoliths are rapidly formed out of the lapiés ridges. 1954W. D. Thornbury Princ. Geomorphol. xiii. 319 Where relief is considerable, limestone surfaces are bare of terra rossa and there is exposed an etched, pitted, grooved, fluted and otherwise rugged surface to which the name lapiés is most commonly applied. Cvijić (1924) has described..the amazing diversity of surface and form which lapiés exhibits in the Dalmatian karst region. He maintained that lapiés is found chiefly on outcrops of naked rock. 1968R. W. Fairbridge Encycl. Geomorphol. 645/1 Well developed lapiés with pinnacles standing up to 5 meters high are common in emerged limestone reefs, particularly in the South Pacific. 1972Bauer & Zötl in Herak & Stringfield Karst vii. 236 At these altitudes [in Austria] lapies are dominant karst phenomena, covering wide areas. Ibid. 237 Where the surface of limestones is exposed by recent soil erosion, irregularly shaped, more or less rounded rills and lapies of different depth are found.
b. Used in the sing. form lapié. rare.
1968R. W. Fairbridge Encycl. Geomorphol. 644/2 (caption) Lapiés formed in limestone covered by residual clay... When the lapié ridges are destroyed, a dolina will be formed, filled with clay. |