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asscciation for mexican cave studies box 7672 ut station austin ...

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The adrenelin still pumping through my weary bod, we stumbled into La Purisimaand had a few refrescos. ive then sat in the middle of the highway trying to hitcha ride back to Savallo. No luck -- B<strong>ut</strong> the local bartender invited us in and procededto get us totally wasted. (Not that we weren't already!) Around 2 A.M. wemanaged to get some sleep at a nearby house, whose friendly owner also stuffed usfull of beans and tortillas. At 6 A.M. we were awakened by the sho<strong>ut</strong>ing of "thebus is here" and we ran o<strong>ut</strong>. boots untied and gear dragging. 20 min<strong>ut</strong>es of a hecticbus ride later we arrived in Jalpan. A short wait there and we were off to Landade Matamoras. Things were going great till then, when we discovered how few vehicleswent down the dirt road to Saucillo. So another 7 miles later we arrived at thetruck - 29 miles in 24 hours· on foot and 30 miles of bus travel was abo<strong>ut</strong> themost intense sco<strong>ut</strong>ing endeavor I've ever experienced.We split <strong>for</strong> the states the next day as I began my 3rd month in Mexico thissummer.Soledad Area ReportThe latest, I think, issue of the Philadelphia Grotto News, Vol. 12, 1973,contains the long awaited report of the several trips by members of the PhiladelphiaGrotto to the Soledad Area in Veracruz. This moupta~nous; area is located just so<strong>ut</strong>hof Cd. Mendoza, Veracruz. The report contains a location map and a description ofseveral <strong>cave</strong>s written by Bob Kezell and Warren Heller. Cueva de Cerro (= SotanoItamo) was surveyed to a depth of 1437 feet below the entrance. The <strong>cave</strong> has a verticalrange of 1491 feet, and is the largest and deepest so far explored in the SoledadArea. An example of the importance of using the local name <strong>for</strong> a <strong>cave</strong> is illustratedby the remapping of the same <strong>cave</strong> by a group from Austin in June 1974. The Austingroup recorded a depth of 1437 feet -- <strong>for</strong>ty feet less than the Philadelphia groupb<strong>ut</strong> the zero point of the Philadelphia map is above the zero point of the Austin mapso the actual depths are very close. However. with the numerous potentially deepsystems in the Soledad area it is un<strong>for</strong>tunate that a great amount of ef<strong>for</strong>t was duplicatedin producing two maps of the same <strong>cave</strong>.Bill RussellAlpine PaleokarstThe thick cretaceous limestones of northern Mexico have been folded intosharp anticlines and the resultant fracturing has permitted the development oflocalized areas of sinkholes along the crest of the folds. The largest sink areayet investigated was on the Sierra El Laurel Quadrangle (G14C42) west of Saltillo.Along the crest of the Sierra la Concordia at an elevation of 3150 meters. severalsinks up to a kilometer long had developed, b<strong>ut</strong> are now apparently being filledwith alluvium. Another local cluster of sinks has been investigated north of Cuevadel Porvenir on the Re<strong>for</strong>ma Quadrangle (G14A6l). These sinks have developed on thecrest of the Sierra de San Marcos at an elevation of 1600 m. At this lower elevationthe change from the more humid climate that favored the development of sinkholesto the present arid climate is more evident. Large alluvial fans are buildinginto the main dolina, abo<strong>ut</strong> 1 Km. long and 0.5 Km. wide. Several small sinksbordering the main dolina have been completely filled, the alluvium spilling overinto lower sinks. It is apparent that. in the past, climatic conditions were morefavorable <strong>for</strong> the development of surface karst, and karst features developed in thepast are now rapidly being destroyed. Both these areas were investigated on almostthe same day. Making the long climb up to the crest of the Sierra El Laurel wasMaureen Cavanaugh, Blake Harrison, Jill Dorman, Mary Kraska, and Preston Forsythe.Back-packing into the Sierra de San Marcos were Peter Sprouse. Bill Russell, LoganMcNatt and Speleocinematographer Thomas Moore.11

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