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17MB PDF - Association for Mexican Cave Studies

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the cave. The spring was running strongly and some travertinepools that have been dry <strong>for</strong> five years are now full.+++Persons: Ed Alexander, Bob Burnett, John Fish, John Kreidler,Charlie Jennings, Tommy McGarrigle, Bill RussellDate: 31 May-IO June 1966Destination: Huautla de Jimenez, OaxacaReported by: John Fish Austin, TexasEd, Bob Charlie, and I left in my car late on Tuesdayafternoon, bound <strong>for</strong> the fabled Huautla plateau in northeasternOaxaca. Bill Russell, John Kreidler, and Tommy McGarrigle gota late start and joined us in Huautla. Despite the many traumasof our drive to Huautla (hole in the gas tank the size of anickel-repaired with a Tootsie Roll, fog along the mountain roads),we arrived there at last only to have to wait a day in Huautlawhile I recovered from a severe intestinal infection. BillRussell and group caught up with us and after puttin~ FelixSeiser,(visiting from Austria and had corne with Bill) on the busback to the U.S., we drove on to the cave area which starts aboutthree miles east of Huautla. On June fourth we got our firstlook at the cave country we were seeking.We had planned to drive to the end of the road and camp,but after passing several large sinkholes, everyone abandonedtheir cars and started checking the sinks near the road. Uponquestioning the local people, Bill was directed to the bottomof a large closed valley in which a small stream dropped intoa pit about 250 feet deep, later named S6tano de San A~ustin.The small town of San Agustin (hence the name of the sotano)lay 500 feet above the s6tano in a divide between two hugedolinas. The San Agustin dolina is approximately one mile longand up to a quarter of a mile wide. It consists of a largecentral dolina with several smaller dolinas or sinks at eachend below the towns of San Andres and San Agustin. The RioIglesia dolina appears to be larger, perhaps the same lengthbut considerably wider and deeper. In both dolinas water runsoff volcanic hills or ridges and sinks into the limestone dolinabottoms.Looking down from San Agustin we could see where the RioIglesia dropped into a fissure below a large opening in themountain. That afternoon Bob, Ed, and Charlie explored theentrance drop of s6tano del RIo Iglesia and found that the mainwater passage, which took several hundred gallons per minute,was impassable. An overflow passage was easily accessible,though, and led to a drop. Since it was virtually dark wedecided not to push the cave then.Meanwhile Tommy and Bill both spotted a large entrancenear San Agust!n on the hill ~bove. This was subsequently calledCueva de San Agustin and goes down a series of slopes and dropsto a deep pool of water. The cave appears to continue.57

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