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17MB PDF - Association for Mexican Cave Studies

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113in the volcanic detrital deposit. The subterranean streampiracies occured late in the present erosion cycle.Many caves are known to exist in other parts of Guerrero andMorelos l but no theory of speleogenesis is yet available.BIBLIOGRAPHY ANDSELECTED REFERENCESBretz l J. Harlen (1955) <strong>Cave</strong>rn-maki~ in a part of the <strong>Mexican</strong>plateau. Journal of Geology 63(4): 364-375.compania Hulera Euzkadi l S.A. (1966) Caminos de Mexico 1 2nd ed.Mexico. 55 p.Fish l John and Reddell lJames (1965) ~rip repor~ AMCS Newsletter1(8): 73-77.2(4): 82=87.GaYI Carlo E.T. (1967) OldestHistory 76(4): 2~35.(1967) [Trip repor~ AMCS Newsletterpaintings of the New World.NaturalInternational Geological Congress l 20th (1962) Excursion 0-9.Volcanes l rocas volcanicas lsedimentos lacustres y aluvialesdel Pleistoceno y Pliocenoj rocas clasticas y volcanicasterciariasj yeso y caliza no marinos del Terciario inferiorjcalizas y latitas del Cretacico Superior y calizas 1. dolomitasdel Cretacico inferior len el sur de la Cuenca de Mexico y enel Edo. de Morelos. Mexico. 153 p. and 6 geol. maps.Millares lJorge Hernandez and Escribano l Alejandro Carrillo (1966)Atlas Porrua de la Republica <strong>Mexican</strong>a. Editorial Porrua l S.A.:Mexico. 128 p.Sanchez Mejorada l Santiago Hernandez ~ompile~ (1956) Carta geOlOgicade la Republica <strong>Mexican</strong>a. International GeologicalCongress l 20th.

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