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SOTANITO D,E AHUACAYLAN Sierra Madre Oriental Jalpan

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SOTANITO D,E AHUACAYLAN Sierra Madre Oriental Jalpan ,. , SOTANITO D,E AHUACAYLAN Sierra Madre Oriental Jalpan Ahuacatl~n I "t J I GU [ " ,. ASSOCIATION FOR MEXICAN CAVE STUDIES ,y. CAVE REPORT SERIES Number 1 t r ~:.iffI'i"Y..)" ~, ". lioN D '" RA: j,rl , ... __ ,. I'" ~, tr " ASSOCIATION FOR MEXICAN CAVE STUDIES CAVE REPORT SERIES Number 1 SOTANITO DE AHUACATLAN Sierra Madre Oriental; Jalpan; Ahuacatlan by TERRY W. RAINES The Speleo Press • Austin • 1972 The Association for Mexican Cave Studies is a non-profit, volunteer organization whose goals are the collection and dissemination of infor­ mation concerning Mexican caves. The AMCS publishes a Newsletter, Bulletin, and Cave Report Series which are available to any sincerely interested, conservation-minded person. Prices are available by writing. Some of the persons responsible for the continued success of the Association's endeavours are the following: Publications Editor Terry W. Raines Cave Files . William H. Russell Secretary-Treasurer Jan E. Lewis Coordinating Biologist James R. Reddell Photo Editor . Carl E. Kunath Production Manager. Ronald G. Fieseler ASSOCIATlON FOR MEXICAN CAVE STUDIES P. O. Box 7672, Austin, Texas 78712 Frontispiece: Craig Sainsott views the entrance of the 288.3 m (946 ft) drop within Sotanito de Ahuacatlan. Copyright ©1972 by the Association for Mexican Cave Studies Printed in the United States of America The Spe1eo Press P. O. Box 7037 Austin, Texas 78712 ASSOCIATION FOR MEXICAN CAVE STUDIES P. O. Box 7672, University Station Austin, Texas 78712 USA Price of this issue - $2.50 US INTRODUCTION the mid 1960's this right-of-way consisted solely of a single lane road paved with cob­ Of the 18 physiographic provinces in bles which was built in 1910. Branching off Mexico (Russell, 1969, Assoc. Mex. Cave the highway at innumerable points is a com­ Stud. News., 3: 27), the Sierra Madre Oriental plex network of both primary and secondary has been the most productive in terms of trails which provide the really basic means caves and other karst features to date. For the of travel. These trails date from the 1500's past ten years the AMCS has been conducting and even earlier, and can lead one to almost field investigations in this rugged terrain of any point desired. Access to the Sotanito is thick limestone sequences. The Sierra Madre by way of one of these primary routes that is extensive, measuring roughly 200 km by leaves Ahuacatlan and continues to the north­ 550 km, with few roads to allow access. These west indefinitely. Presently, this particular logistics problems, coupled with the lack of trail is being widened to road-size which will manpower, have limited extensive detailed ex­ allow passage of trucks to Puerto Guilotla and ploration and certainly in many locations then on to Santa Agueda, a small village west large caves only a few minutes' hike from the of the Area. road have not been entered. As a result, To reach the Sotanito, follow the main AMCS cavers have directed their efforts from trail, which trends generally northwest, out of one area of concentrated karst development town. It roughly parallels the arroyo in the to another. Most recently initiated has been valley below but climbs continuously. Less the Ahuacatlan Area, located within the Jal­ than 1 km from Ahuacatlan the first hillside pan Region of the SMO Province. The Jalpan arroyo is crossed. Continue on, up over a Region lies almost entirely within the state of broad ridge, until reaching a second arroyo. Queretaro and to the northwest of Jalpan, From this point the cave entrance is directly Qro. The small town of Ahuacatlan gives its up the arroyo, requiring a steep, one hour name to the Area, which consists primarily of hike. It would be impossible to describe ex­ the Cerro de la Tinaja north of the highway actly where the entrance can be found from (see map, p. 7 ). It is within this area that here as it is so small and insignificant. The Sotanito de Ahuacatlan is situated. upper photograph on page 16 is a view from For the most part, volunteer manpower the cave which may give some aid. This field to produce this report was supplied by the is crossed immediately before arrival at the ever-present, hard-core group of Austin cavers, entrance, located in an area of undergrowth. with, of course, help from our friends. Per­ Also, the town of Ahuacatlan lies hidden in sons who should be recognized are: Chuck the main valley directly above the caver. The Bryan, Arthur Cleaves, de de Esparza, Ronnie last leg of the journey is most comfortably Fieseler, Blake Harrison, Roy Jameson, James traversed under the direction of a local guide, Jasek, Orion Knox, Carl Kunath, Jan Lewis, who would be more than willing to help out Neal Morris, James Reddell, Olga Reyes, Jim if approached in a friendly manner. The eleva­ and Julie Rodemaker, Bill and Carol Russell, tion gained between Ahuacatlan and the cave Craig Sainsott, Joe Simo, Richard M. Smith, is about 400 m over a distance of 2.5 km. The Bob Stockton, and Hugo Victoria. Undoubt­ weather is usually hot and the trail steepens as edly, others will appear in the latter stages of one nears the cave. There is absolutely no wa­ production who can not be credited at this ter once you get there, so be prepared. time. As mentioned before, the Ahuacatlan Area and Cerro de la Tinaja are essentially one GEOGRAPHY and the same. Extending to the north beyond the map, the range is ultimately terminated Primary vehicular travel through the by the Rio Ayutla. Total dimensions are 5 km Ahuacatlan Area is via a hard-surfaced high­ by 20 km. To the southeast of the Sotanito, way which borders the southern edge. Until the greatest elevation difference is 500 to 600 m. It is measured between the crest of necessarily contemporaneous, they are said to the Cerro de la Tinaja and the base level at be homotaxial, and therefore rock-stratigraph­ Ahuacathln. The crestal area is broad, giving ical units. However, on the basis of fossil evi­ way on the southwestern flank to a dip slope dence, certain time intervals can be assigned of 30°. In the vicinity of the linear peak a at specific locations. number of shallow stream courses head. These channels are in general oriented directly down­ LAS TRANCAS FORMATION slope and coalesce with a base level arroyo The lower-most formation exposed in the which is parallel to the range. Because of in­ Ahuacatlan Area is a splintery-weathering, ternal drainage, the channels very rarely carry slightly phyllitic gray shale interbedded with a water and are consequently poorly developed. dark-gray argillaceous limestone. These thin On the other hand, the usually dry base level beds contain small quartz grains and the for­ arroyos do flood after intensive summer rains, mation has scattered beds of impure calcare­ in this case conducting the torrent through nite. Ahuacatlan into the RIO Jalpan drainage sys­ The photograph on page 9 is a good ex­ tem. ample of the splintery-weathering exhibited The climate of the AhuacaWm Area is by the Las Trancas formation, while on page rather harsh on visitors as well as local resi­ 10 is iJlustrated the characteristic thin bed­ dents. The winter and spring months are quite ding. A small thrust fault can also be seen in dry, receiving only 10% of the annual 600 mm this photograph with accompanying drag folds. rainfall. Then, during the summer months, Fossil evidence found by Segerstrom heavy rains erode quantities of loose topsoil 1961 indicates the Las Trancas formation in from bare corn fields. At all times good water the immediate Ahuacatlan area is considered for drinking can usually only be found along to be late Callovian to late Oxfordian age. the base level arroyos because the above lime­ These, of course, are stages of the Late Juras­ stone terrain readily consumes all precipita­ sic System. tion quickly. EL DOCTOR FORt\1AnON The El Doctor is the principal rock unit GEOLOGY OF THE AHUACATLAN AREA exposed in the area. To the west of the region, the EI Doctor overlies the Las Trancas with by Richard M. Smith great disconformity, however, the exposed contact between these two formations near LOCATION Ahuacatlan is extremely gradational as can be The author, aided by several other mem­ seen on page 11 . The lithologic characteristics bers of AMCS, mapped the area during 1971­ change from slightly phyllitic gray shale and 1972. It should be noted that the mapping dark-gray argillaceous limestone in the upper was reconnaissance in nature and because of Las Trancas to shaly limestone interstitially the difficulty of access and poor exposures, bedded with calcareous shales. These beds much reliance was placed on the geologic map range from 15 em to 20 em thick. compiled by Segerstrom in 1961. The few mi­ In turn, these beds grade into a thick­ nor errors found in the remarkable Segerstrom bedded, fine grained, dove micrite. Further work were corrected on the included map. in the section, a rudistid facies appears turning the hitherto unfossiliferous micrite into a vir­ LITHOSTRATIGRAPHIC UNITS tual coquina. The extent of this facies could The rocks exposed in the Ahuacatlan not be determined, but certainly constitutes area have been subdivided into formations on a major portion of the middle El Doctor. the basis of lithologic characteristics. Since The middle EI Doctor quickly changes these formations have a similar order of ar­ within a few feet from massive limestone to rangement in different locations, but are not thin-bedded limestone with some interbeds of 2 brown calcareous shale. been intensely folded with the axial plane Along the highway, just south of Esca­ trend from northwest to southeast.
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