12MB PDF - Association for Mexican Cave Studies

12MB PDF - Association for Mexican Cave Studies 12MB PDF - Association for Mexican Cave Studies

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Stream passage in Cueva Tecolo.(Ernie Garza)Sistema Cuetzalan:the resurgence?A trip into Chichicasapan to dosome photography was very enjoyable.A look at the boulder choke at thebottom of the Resistol Stream Passageseemed to reveal that this isnot just a simple stopping. As farup as one can climb into the breakdownit is covered with silt, whichseems to be coming from above. Onemight conclude that there is a higher68level crossing as this point, and, ifit could be entered, it might leadback to the stream and onward anddown. It should be noted that dryupper levels seem to be COmmon andare found at least in Jonotla, Teco­10, and Chichicasapan. Where thesecan be seen to have collapsed toform~n unusually large chamber inthe lower stream level, one finds

ENTRADACANONACUEVATECOLOESTADA DE PUEBLA, MEXICOPLANO POR CINTA PARA MEDIR Y COMPASASOCIACION PARA ESTUDIOS DE CUEVAS MEXICANAS4-2-79 W. ANDERSON. D. JOHNSON. B. LIEBMAN, N. PACE4-4-79 W. ANDE RSON, E. GARZA. D. JOHNSON, S. KNUTSON,B. LIEBMAN, A. VILLAGOMEZ4-6-79 S. KNUTSON. D. LAFORGE. N. PACETOTAL DE LARGO ES 1830 METROSTOTAL DE HONDURA ES 52.5 METROSuElINEACION POR STEVE KNUTSON, MAYO, 1979SECCION TRANSVERSAL ES DOS VECES ESCALA?MAG.NENTRADASUPERIORo 50 1001:-:-:...t:. -.::::.±=-:_:-=:.:==_.:..:.::::f METERS~?~~~~TERRENAAPROXIMADACANONZEMPOALA(TECUANTEPEC) r,~r-"t:.:..to20?=~----:~?~~~--::::~~_~~rz:t-20METROS4060PROYECCI6N AL LADO DE RUMBO ~AGNETICO DE 120 GRADOS

Stream passage in Cueva Tecolo.(Ernie Garza)Sistema Cuetzalan:the resurgence?A trip into Chichicasapan to dosome photography was very enjoyable.A look at the boulder choke at thebottom of the Resistol Stream Passageseemed to reveal that this isnot just a simple stopping. As farup as one can climb into the breakdownit is covered with silt, whichseems to be coming from above. Onemight conclude that there is a higher68level crossing as this point, and, ifit could be entered, it might leadback to the stream and onward anddown. It should be noted that dryupper levels seem to be COmmon andare found at least in Jonotla, Teco­10, and Chichicasapan. Where thesecan be seen to have collapsed to<strong>for</strong>m~n unusually large chamber inthe lower stream level, one finds

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